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{{Short description|Hurricane season in the Pacific Ocean}}
{{Short description|none}} <!-- "none" is a legitimate description when the title is already adequate; see [[WP:SDNONE]] -->
{{Use mdy dates|date=February 2012}}
{{Use mdy dates|date=February 2012}}
{{Infobox hurricane season
{{Infobox tropical cyclone season
| Basin=EPac
| Basin = EPac
| Year=1990
| Year = 1990
| Track=1990 Pacific hurricane season summary map.png
| Track = 1990 Pacific hurricane season summary map.png
| First storm formed=May 12, 1990
| First storm formed = May 12, 1990
| Last storm dissipated=November 1, 1990
| Last storm dissipated = November 1, 1990
| Strongest storm name=Trudy
| Strongest storm name = Trudy
| Strongest storm winds=135
| Strongest storm winds = 135
| Strongest storm pressure=924
| Strongest storm pressure = 924
| Average wind speed=1
| Average wind speed = 1
| Total depressions=27
| Total depressions = 27
| Total storms=21
| Total storms = 21
| Total hurricanes=16 <br/>(record high, tied with [[1992 Pacific hurricane season|1992]], [[2014 Pacific hurricane season|2014]] and [[2015 Pacific hurricane season|2015]])
| Total hurricanes = 16 (record high, tied with [[1992 Pacific hurricane season|1992]], [[2014 Pacific hurricane season|2014]] and [[2015 Pacific hurricane season|2015]])
| Total intense=6
| Total intense = 6
| Fatalities=19 total
| Fatalities = 19 total
| Damages=12.5
| Damages = 12.5
| five seasons=[[1988 Pacific hurricane season|1988]], [[1989 Pacific hurricane season|1989]], '''1990''', [[1991 Pacific hurricane season|1991]], [[1992 Pacific hurricane season|1992]]
| five seasons = [[1988 Pacific hurricane season|1988]], [[1989 Pacific hurricane season|1989]], '''1990''', [[1991 Pacific hurricane season|1991]], [[1992 Pacific hurricane season|1992]]
| Season timeline=Timeline of the 1990 Pacific hurricane season
| Season timeline = Timeline of the 1990 Pacific hurricane season
|Atlantic season=1990 Atlantic hurricane season
| Atlantic season = 1990 Atlantic hurricane season
|West Pacific season=1990 Pacific typhoon season
| West Pacific season = 1990 Pacific typhoon season
|North Indian season=1990 North Indian Ocean cyclone season
| North Indian season = 1990 North Indian Ocean cyclone season
}}
}}
The '''1990 Pacific hurricane season''' was a very active season which observed 21 named storms within the basin. The season also produced the fourth highest [[Accumulated cyclone energy|ACE]] index value on record. The season was officially started on May 15 in the eastern Pacific, and on June 1 in the central Pacific, and lasted until November 30. These dates conventionally delimit the period of each year when most tropical cyclones form in the northeastern Pacific Ocean. However, the formation of tropical cyclones is possible at any time of the year, as illustrated in 1990 by the formation of the season's first [[Tropical cyclone naming|named storm]], Hurricane Alma, on May&nbsp;12. At the time, this was the earliest formation of a tropical storm on record in the eastern Pacific
The '''1990 Pacific hurricane season''' was a very active season which observed 21 named storms within the basin. The season also produced the fourth highest [[Accumulated cyclone energy|ACE]] index value on record. The season was officially started on May 15 in the eastern Pacific, and on June 1 in the central Pacific, and lasted until November 30. These dates conventionally delimit the period of each year when most tropical cyclones form in the northeastern Pacific Ocean. However, the formation of tropical cyclones is possible at any time of the year, as illustrated in 1990 by the formation of the season's first [[Tropical cyclone naming|named storm]], Hurricane Alma, on May&nbsp;12. At the time, this was the earliest formation of a tropical storm on record in the eastern Pacific
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== Seasonal summary ==
== Seasonal summary ==
{{center|<timeline>
<div style="text-align: center;">
<timeline>
ImageSize = width:800 height:200
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PlotArea = top:10 bottom:80 right:20 left:20
PlotArea = top:10 bottom:80 right:20 left:20
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ScaleMinor = grid:black unit:month increment:1 start:01/05/1990
ScaleMinor = grid:black unit:month increment:1 start:01/05/1990


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from:24/07/1990 till:26/07/1990 color:TD text:"Eleven-E (TD)"
from:24/07/1990 till:26/07/1990 color:TD text:"Eleven-E (TD)"
from:07/08/1990 till:15/08/1990 color:TS text:"Aka (TS)"
from:07/08/1990 till:15/08/1990 color:TS text:"Aka (TS)"
from:08/08/1990 till:09/08/1990 color:TD text:"[[Hurricane Diana (1990)|Diana (TD)]]"
from:08/08/1990 till:09/08/1990 color:TD text:"[[Hurricane Diana|Diana (TD)]]"
from:10/08/1990 till:13/08/1990 color:TD text:"Two-C (TD)"
from:10/08/1990 till:13/08/1990 color:TD text:"Two-C (TD)"
barset:break
barset:break
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</timeline>
</timeline>
}}
</div>


{{Highest ACE Pacific hurricane seasons}}
{{Highest ACE Pacific hurricane seasons}}
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With the exception of Marie and Polo, these systems developed between [[5th parallel north|5°]] and [[15th parallel north|15°N]], east of the longitude of Baja California Peninsula in the [[climate|climatological]]ly favored area for [[tropical cyclogenesis]] in the basin. After their development, most of the tropical cyclones moved on a west to northwest track and dissipated over cool waters without affecting land. Rachel was the only system to make landfall. In addition, one tropical storm formed in the Central Pacific and eventually crossed the [[International Dateline]] before dissipating.<ref name="Eastern North Pacific Season of 1990"/>
With the exception of Marie and Polo, these systems developed between [[5th parallel north|5°]] and [[15th parallel north|15°N]], east of the longitude of Baja California Peninsula in the [[climate|climatological]]ly favored area for [[tropical cyclogenesis]] in the basin. After their development, most of the tropical cyclones moved on a west to northwest track and dissipated over cool waters without affecting land. Rachel was the only system to make landfall. In addition, one tropical storm formed in the Central Pacific and eventually crossed the [[International Dateline]] before dissipating.<ref name="Eastern North Pacific Season of 1990"/>


The Accumulated Cyclone Energy (ACE) index for the 1990 Pacific hurricane season (Eastern Pacific and Central Pacific combined) as calculated by Colorado State University using data from the National Hurricane Center was 249.5&nbsp;units, the fourth highest ACE on record for a Pacific hurricane season.{{#tag:ref|The total represents the sum of the squares of the maximum sustained wind speed (knots) for every (sub)tropical storm's intensity of over {{convert|33|kn|mph km/h}}, divided by 10,000 while they are above that threshold; therefore, tropical depressions are not included.|group="nb"}}<ref>{{cite web| title=Basin Archives: Northeast Pacific Ocean Historical Tropical Cyclone Statistics|url=http://tropical.atmos.colostate.edu/Realtime/index.php?arch&loc=northeastpacific|publisher=Colorado State University|location=Fort Collins, Colorado|access-date=July 8, 2022}}</ref>
ACE is, broadly speaking, a measure of the power of the hurricane multiplied by the length of time it existed, so storms that last a long time, as well as particularly strong hurricanes, have high ACEs. ACE is only calculated for full advisories on tropical systems at or exceeding 39&nbsp;mph (63&nbsp;km/h) or tropical storm strength.<ref>{{cite web|url=http://www.cpc.noaa.gov/products/outlooks/background_information.shtml|title=Measuring total seasonal activity: The Accumulated Cyclone Energy (ACE) index|publisher=[[Climate Prediction Center]]|access-date=January 3, 2011|archive-url=https://www.webcitation.org/5uGl8BVhE?url=http://www.cpc.noaa.gov/products/outlooks/background_information.shtml|archive-date=November 15, 2010|url-status=dead|df=mdy-all}}</ref> The cumulative ACE for the Eastern Pacific this season fell within the official "Above Normal" grading, being one of the most active. This occurred because the season had many intense storms that lasted for a long period of time. Also it is important to note that this is the fourth highest ACE, only behind the [[1992 Pacific hurricane season|1992]], [[2015 Pacific hurricane season|2015]] and [[2018 Pacific hurricane season|2018]] seasons respectively.<ref name="80columndata"/>


== Systems ==
== Systems ==
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=== Hurricane Alma ===
=== Hurricane Alma ===
{{Infobox Hurricane Small
{{Infobox Hurricane Small
|Basin=EPac
| Basin = EPac
|Image=Hurricane Alma May 15 1990 2101Z.jpg
| Image = Alma 1990-05-15 2101Z.jpg
|Track=Alma 1990 track.png
| Track = Alma 1990 track.png
|Formed=May 12
| Formed = May 12
|Dissipated=May 18
| Dissipated = May 18
|1-min winds=75
| 1-min winds = 75
|Pressure=979
| Pressure = 979
}}
}}
{{See also|List of off-season Pacific hurricanes}}
{{See also|List of off-season Pacific hurricanes}}
A tropical wave emerged from Africa on April 29. It then moved across the Atlantic, crossed northern South America, and entered the Pacific Ocean on May 9. [[Convection]] started to increase with the wave just to the south of [[Panama]]. The wave moved westward and continued to become better organized over the next few days. On May 12, the wave had become organized enough and was designated Tropical Depression One-E.<ref name="almaprelim1">{{cite web|author=Case, Robert|year=1990|title=Hurricane Alma Preliminary Report, Page 1|publisher=National Hurricane Center|access-date=January 2, 2011|url=http://www.nhc.noaa.gov/archive/storm_wallets/epacific/ep1990/alma/prenhc/prelim01.gif}}</ref>
A tropical wave emerged from Africa on April 29. It then moved across the Atlantic, crossed northern South America, and entered the Pacific Ocean on May 9. [[Convection]] started to increase with the wave just to the south of [[Panama]]. The wave moved westward and continued to become better organized over the next few days. On May 12, the wave had become organized enough and was designated Tropical Depression One-E.<ref name="almaprelim1">{{cite web|author=Case, Robert|year=1990|title=Hurricane Alma Preliminary Report, Page 1|publisher=National Hurricane Center|access-date=January 2, 2011|url=http://www.nhc.noaa.gov/archive/storm_wallets/epacific/ep1990/alma/prenhc/prelim01.gif}}</ref>


Tropical Depression One-E moved slowly to the northwest while strengthening slowly due to easterly vertical [[wind shear]]. The depression was upgraded to Tropical Storm Alma on May 14. The storm quickly strengthened once the vertical wind shear relaxed and was near hurricane force by the morning of May 15. Hurricane Alma reached its peak intensity early on May 16 with maximum sustained winds of 85&nbsp;mph (135&nbsp;km/h). The hurricane entered an area of southwesterly wind shear caused by an [[ridge|upper-level ridge]] of [[high pressure]]. The increasing vertical wind shear and [[sea surface temperature|cooler water]] caused Alma to weaken to a tropical storm. On May 17, the storm continued to weaken and became a depression. The next day, the system dissipated as a tropical cyclone well west of mainland Mexico.<ref name="almaprelim1" /><ref name="almadisc1315z">{{cite web|author=Mayfield, Max|date=May 13, 1990|title=Tropical Cyclone Discussion Tropical Depression One-E|publisher=National Hurricane Center|access-date=January 2, 2011|url=http://www.nhc.noaa.gov/archive/storm_wallets/epacific/ep1990/alma/tropdisc/tcd1315z.gif}}</ref><ref name="almadisc1503z">{{cite web|author=Gerrish, Hal|date=May 15, 1990|title=Tropical Cyclone Discussion Tropical Storm Alma|publisher=National Hurricane Center|access-date=January 2, 2011|url=http://www.nhc.noaa.gov/archive/storm_wallets/epacific/ep1990/alma/tropdisc/tcd1503z.gif}}</ref>
Tropical Depression One-E moved slowly to the northwest while strengthening slowly due to easterly vertical [[wind shear]]. The depression was upgraded to Tropical Storm Alma on May 14. The storm quickly strengthened once the vertical wind shear relaxed and was near hurricane force by the morning of May 15. Hurricane Alma reached its peak intensity early on May 16 with maximum sustained winds of {{convert|85|mph|km/h|abbr=on}}. The hurricane entered an area of southwesterly wind shear caused by an [[ridge|upper-level ridge]] of [[high pressure]]. The increasing vertical wind shear and [[sea surface temperature|cooler water]] caused Alma to weaken to a tropical storm. On May 17, the storm continued to weaken and became a depression. The next day, the system dissipated as a tropical cyclone well west of mainland Mexico.<ref name="almaprelim1" /><ref name="almadisc1315z">{{cite web|author=Mayfield, Max|date=May 13, 1990|title=Tropical Cyclone Discussion Tropical Depression One-E|publisher=National Hurricane Center|access-date=January 2, 2011|url=http://www.nhc.noaa.gov/archive/storm_wallets/epacific/ep1990/alma/tropdisc/tcd1315z.gif}}</ref><ref name="almadisc1503z">{{cite web|author=Gerrish, Hal|date=May 15, 1990|title=Tropical Cyclone Discussion Tropical Storm Alma|publisher=National Hurricane Center|access-date=January 2, 2011|url=http://www.nhc.noaa.gov/archive/storm_wallets/epacific/ep1990/alma/tropdisc/tcd1503z.gif}}</ref>
{{clear}}
{{clear}}


=== Hurricane Boris ===
=== Hurricane Boris ===
{{Infobox Hurricane Small
{{Infobox Hurricane Small
|Basin=EPac
| Basin = EPac
|Image=File:Boris 1990-06-05 1400Z.png
| Image = File:Boris 1990-06-05 1400Z.png
|Track=Boris 1990 track.png
| Track = Boris 1990 track.png
|Formed=June 2
| Formed = June 2
|Dissipated=June 8
| Dissipated = June 8
|1-min winds=80
| 1-min winds = 80
|Pressure=977
| Pressure = 977
}}
}}
A tropical wave came off the northwest coast of Africa on May 20. The wave did not significantly develop as it moved west across the Atlantic Ocean and Caribbean Sea. Once it crossed Central America into the eastern Pacific Ocean, cloudiness increased considerably with the system on May 31.<ref name="borisprelim1">{{cite web|author=Mayfield, Max|year=1990|title=Hurricane Boris Preliminary Report, Page 1|publisher=National Hurricane Center|access-date=January 2, 2011|url=http://www.nhc.noaa.gov/archive/storm_wallets/epacific/ep1990/boris/prenhc/prelim01.gif}}</ref> It became well-enough organized to be upgraded to Tropical Depression Two-E on June 2. After becoming a depression, the system moved to the west-northwestward. Upper-level easterly vertical [[wind shear]] limited the amount of the initial strengthening. However, an increase in convective banding led to its upgrade to Tropical Storm Boris on June 4, {{convert|500|mi|km|abbr=on}} southwest of Manzanillo. Further strengthening occurred due to an [[anticyclone]] aloft fostered additional development, and by June 5, Boris became a hurricane. The hurricane began to move to the north-northwest in response to a trough off of the [[West Coast of the United States]]. Strengthening continued, and the storm reached its peak strength with winds of {{convert|90|mph|km/h|abbr=on}} and a minimum central pressure of {{convert|977|mb|inHg|abbr=on}}. The hurricane's cloud pattern became elongated along a southwest-northeast axis on June 6 due to an increased amount of vertical wind shear. Boris was downgraded to a tropical storm later in the day on June 6. The deep convection of the tropical storm decreased, as Boris moved over cooler waters. It was downgraded to a tropical depression on June 7 due to these factors. The depression dissipated as a tropical cyclone on June 8 as the system quickly lost its tropical characteristics. A small circulation remained in the cloud field offshore the northwest coast of Baja California for a few more days.<ref name="borisprelim1"/><ref name="june81421ztcd">{{cite web|author=Lixion, Avila|date=June 8, 1990|title=Tropical Cyclone Discussion: Tropical Depression Boris|publisher=National Hurricane Center|access-date=January 2, 2011|url=http://www.nhc.noaa.gov/archive/storm_wallets/epacific/ep1990/boris/tropdisc/tcd0815z.gif}}</ref>
A tropical wave came off the northwest coast of Africa on May 20. The wave did not significantly develop as it moved west across the Atlantic Ocean and Caribbean Sea. Once it crossed Central America into the eastern Pacific Ocean, cloudiness increased considerably with the system on May 31.<ref name="borisprelim1">{{cite web|author=Mayfield, Max|year=1990|title=Hurricane Boris Preliminary Report, Page 1|publisher=National Hurricane Center|access-date=January 2, 2011|url=http://www.nhc.noaa.gov/archive/storm_wallets/epacific/ep1990/boris/prenhc/prelim01.gif}}</ref> It became well-enough organized to be upgraded to Tropical Depression Two-E on June 2. After becoming a depression, the system moved to the west-northwestward. Upper-level easterly vertical [[wind shear]] limited the amount of the initial strengthening. However, an increase in convective banding led to its upgrade to Tropical Storm Boris on June 4, {{convert|500|mi|km|abbr=on}} southwest of Manzanillo. Further strengthening occurred due to an [[anticyclone]] aloft fostered additional development, and by June 5, Boris became a hurricane. The hurricane began to move to the north-northwest in response to a trough off of the [[West Coast of the United States]]. Strengthening continued, and the storm reached its peak strength with winds of {{convert|90|mph|km/h|abbr=on}} and a minimum central pressure of {{convert|977|mb|inHg|abbr=on}}. The hurricane's cloud pattern became elongated along a southwest–northeast axis on June 6 due to an increased amount of vertical wind shear. Boris was downgraded to a tropical storm later in the day on June 6. The deep convection of the tropical storm decreased, as Boris moved over cooler waters. It was downgraded to a tropical depression on June 7 due to these factors. The depression dissipated as a tropical cyclone on June 8 as the system quickly lost its tropical characteristics. A small circulation remained in the cloud field offshore the northwest coast of Baja California for a few more days.<ref name="borisprelim1"/><ref name="june81421ztcd">{{cite web|author=Lixion, Avila|date=June 8, 1990|title=Tropical Cyclone Discussion: Tropical Depression Boris|publisher=National Hurricane Center|access-date=January 2, 2011|url=http://www.nhc.noaa.gov/archive/storm_wallets/epacific/ep1990/boris/tropdisc/tcd0815z.gif}}</ref>


The winds in the eyewall of Boris ripped off the sails of the Azure Dream sailboat. Outer rainbands from the storm produced moderate rain in several Mexican states. In Mexico, rainfall peaked at {{convert|8.83|in|mm|abbr=on}} near [[San Lucas, Michoacán]]. The remnants of Boris also brought sporadic rainfall over the western United States, with precipitation being reported in Arizona, California, Colorado, Nevada and Wyoming. The remnants of Boris were responsible for causing the wettest June in San Diego since records began in 1850; however, not even {{convert|1|in|mm|abbr=on}} of rain fell at that location. Rainfall from the remnant system in the United States peaked at {{convert|3.28|in|mm|abbr=on}} over the [[Santa Rita Mountains]].<ref name="borisprelim2"/><ref name="borisrain">{{cite web|date=August 12, 2008|access-date=January 2, 2011|url=http://www.wpc.ncep.noaa.gov/tropical/rain/boris1990.html|title=Hurricane Boris – June 4–11, 1990|author=Roth, David|publisher=[[Hydrometeorological Prediction Center]]|author-link=David M. Roth}}</ref> No other direct damages or casualties were reported from Boris.<ref name="borisprelim1"/><ref name="borisprelim2">{{cite web|author=Mayfield, Max|year=1990|title=Hurricane Boris Preliminary Report, Page 2|publisher=National Hurricane Center|access-date=January 2, 2011|url=http://www.nhc.noaa.gov/archive/storm_wallets/epacific/ep1990/boris/prenhc/prelim02.gif}}</ref><ref name="june32031ztcd">{{cite web|author=Avila, Lixion|year=1990|title=Tropical Cyclone Discussion: Tropical Depression Two-E|publisher=National Hurricane Center|access-date=January 2, 2011|url=http://www.nhc.noaa.gov/archive/storm_wallets/epacific/ep1990/boris/tropdisc/tcd0321z.gif}}</ref>
The winds in the eyewall of Boris ripped off the sails of the Azure Dream sailboat. Outer rainbands from the storm produced moderate rain in several Mexican states. In Mexico, rainfall peaked at {{convert|8.83|in|mm|abbr=on}} near [[San Lucas, Michoacán]]. The remnants of Boris also brought sporadic rainfall over the western United States, with precipitation being reported in Arizona, California, Colorado, Nevada and Wyoming. The remnants of Boris were responsible for causing the wettest June in San Diego since records began in 1850; however, not even {{convert|1|in|mm|abbr=on}} of rain fell at that location. Rainfall from the remnant system in the United States peaked at {{convert|3.28|in|mm|abbr=on}} over the [[Santa Rita Mountains]].<ref name="borisprelim2"/><ref name="borisrain">{{cite web|date=August 12, 2008|access-date=January 2, 2011|url=http://www.wpc.ncep.noaa.gov/tropical/rain/boris1990.html|title=Hurricane Boris – June 4–11, 1990|author=Roth, David|publisher=[[Hydrometeorological Prediction Center]]}}</ref> No other direct damages or casualties were reported from Boris.<ref name="borisprelim1"/><ref name="borisprelim2">{{cite web|author=Mayfield, Max|year=1990|title=Hurricane Boris Preliminary Report, Page 2|publisher=National Hurricane Center|access-date=January 2, 2011|url=http://www.nhc.noaa.gov/archive/storm_wallets/epacific/ep1990/boris/prenhc/prelim02.gif}}</ref><ref name="june32031ztcd">{{cite web|author=Avila, Lixion|year=1990|title=Tropical Cyclone Discussion: Tropical Depression Two-E|publisher=National Hurricane Center|access-date=January 2, 2011|url=http://www.nhc.noaa.gov/archive/storm_wallets/epacific/ep1990/boris/tropdisc/tcd0321z.gif}}</ref>


{{clear}}
{{clear}}
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=== Tropical Storm Cristina ===
=== Tropical Storm Cristina ===
{{Infobox Hurricane Small
{{Infobox Hurricane Small
|Basin=EPac
| Basin = EPac
|Image=File:Cristina 1990-06-12 1500Z.png
| Image = File:Cristina 1990-06-12 1500Z.png
|Track=Cristina 1990 track.png
| Track = Cristina 1990 track.png
|Formed=June 8
| Formed = June 8
|Dissipated=June 16
| Dissipated = June 16
|1-min winds=55
| 1-min winds = 55
|Pressure=994
| Pressure = 994
}}
}}
A tropical wave emerged into the Atlantic Ocean off the coast of Africa on May 28. The wave moved across Central America into the northeastern Pacific Ocean, where convection organized with the system on June 6. The system became well-enough organized to be upgraded to Tropical Depression Three-E on June 8, while {{convert|920|mi|km|abbr=on}} south of the southern tip of Baja California. The depression continued to strengthen, and was upgraded to Tropical Storm Cristina on June 9.<ref name="cristinaprelim1">{{cite web|author=Avila, Lixion|date=June 22, 1990|title=Tropical Storm Cristina Preliminary Report, Page 1|publisher=National Hurricane Center|access-date=January 2, 2011|url=http://www.nhc.noaa.gov/archive/storm_wallets/epacific/ep1990/cristina/prenhc/prelim01.gif}}</ref><ref name="june81434ztcd">{{cite web|author=Avila, Lixion|date=June 8, 1990|title=Tropical Cyclone Discussion: Tropical Depression Three-E|publisher=National Hurricane Center|access-date=January 2, 2011|url=http://www.nhc.noaa.gov/archive/storm_wallets/epacific/ep1990/cristina/tropdisc/tcd0815z.gif}}</ref>
A tropical wave emerged into the Atlantic Ocean off the coast of Africa on May 28. The wave moved across Central America into the northeastern Pacific Ocean, where convection organized with the system on June 6. The system became well-enough organized to be upgraded to Tropical Depression Three-E on June 8, while {{convert|920|mi|km|abbr=on}} south of the southern tip of Baja California. The depression continued to strengthen, and was upgraded to Tropical Storm Cristina on June 9.<ref name="cristinaprelim1">{{cite web|author=Avila, Lixion|date=June 22, 1990|title=Tropical Storm Cristina Preliminary Report, Page 1|publisher=National Hurricane Center|access-date=January 2, 2011|url=http://www.nhc.noaa.gov/archive/storm_wallets/epacific/ep1990/cristina/prenhc/prelim01.gif}}</ref><ref name="june81434ztcd">{{cite web|author=Avila, Lixion|date=June 8, 1990|title=Tropical Cyclone Discussion: Tropical Depression Three-E|publisher=National Hurricane Center|access-date=January 2, 2011|url=http://www.nhc.noaa.gov/archive/storm_wallets/epacific/ep1990/cristina/tropdisc/tcd0815z.gif}}</ref>
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=== Tropical Storm Douglas ===
=== Tropical Storm Douglas ===
{{Infobox Hurricane Small
{{Infobox Hurricane Small
|Basin=EPac
| Basin = EPac
|Image=File:Douglas 1990-06-20 2230Z.png
| Image = File:Douglas 1990-06-20 2230Z.png
|Track=Douglas 1990 track.png
| Track = Douglas 1990 track.png
|Formed=June 19
| Formed = June 19
|Dissipated=June 23
| Dissipated = June 23
|1-min winds=55
| 1-min winds = 55
|Pressure=992
| Pressure = 992
}}
}}
A tropical wave moved off the northwest coast of Africa on June 5. It continued westward across the tropical North Atlantic and Caribbean Sea without significant development.<ref name="douglasprelim1">{{cite web|author=Gerrish, Hal|year=1990|title=Tropical Storm Douglas Preliminary Report, Page 1|publisher=National Hurricane Center|access-date=January 3, 2011|url=http://www.nhc.noaa.gov/archive/storm_wallets/epacific/ep1990/douglas/prenhc/prelim01.gif}}</ref> The wave entered the northeastern Pacific Ocean on June 16, where it generated an area of increased cloudiness. Organization of thunderstorm activity increased late on June 18 and early on June 19. Tropical Depression Four-E formed on June 19, when it was {{convert|230|mi|km|abbr=on}} south of [[Acapulco]] after evidence of low-level circulation for the past 24&nbsp;hours.<ref name="june192100ztcd">{{cite web|author=Lawrence, Miles|date=June 19, 1990|title=Tropical Cyclone Discussion: Tropical Storm Douglas|publisher=National Hurricane Center|access-date=January 3, 2011|url=http://www.nhc.noaa.gov/archive/storm_wallets/epacific/ep1990/douglas/tropdisc/tcd1921z.gif}}</ref> The depression moved in a west-northwest direction, due to a [[subtropical ridge]] north of the depression. Satellite analysis indicated that the depression had reached tropical storm force strength, and it was upgraded to Tropical Storm Douglas on June 19, while {{convert|230|mi|km|abbr=on}} southwest of Acapulco. Douglas reached peak strength of {{convert|65|mph|km/h|abbr=on}} on June 21<ref name="douglasprelim1"/>
A tropical wave moved off the northwest coast of Africa on June 5. It continued westward across the tropical North Atlantic and Caribbean Sea without significant development.<ref name="douglasprelim1">{{cite web|author=Gerrish, Hal|year=1990|title=Tropical Storm Douglas Preliminary Report, Page 1|publisher=National Hurricane Center|access-date=January 3, 2011|url=http://www.nhc.noaa.gov/archive/storm_wallets/epacific/ep1990/douglas/prenhc/prelim01.gif}}</ref> The wave entered the northeastern Pacific Ocean on June 16, where it generated an area of increased cloudiness. Organization of thunderstorm activity increased late on June 18 and early on June 19. Tropical Depression Four-E formed on June 19, when it was {{convert|230|mi|km|abbr=on}} south of [[Acapulco]] after evidence of low-level circulation for the past 24&nbsp;hours.<ref name="june192100ztcd">{{cite web|author=Lawrence, Miles|date=June 19, 1990|title=Tropical Cyclone Discussion: Tropical Storm Douglas|publisher=National Hurricane Center|access-date=January 3, 2011|url=http://www.nhc.noaa.gov/archive/storm_wallets/epacific/ep1990/douglas/tropdisc/tcd1921z.gif}}</ref> The depression moved in a west-northwest direction, due to a [[subtropical ridge]] north of the depression. Satellite analysis indicated that the depression had reached tropical storm force strength, and it was upgraded to Tropical Storm Douglas on June 19, while {{convert|230|mi|km|abbr=on}} southwest of Acapulco. Douglas reached peak strength of {{convert|65|mph|km/h|abbr=on}} on June 21<ref name="douglasprelim1"/>
Line 184: Line 183:
=== Hurricane Elida ===
=== Hurricane Elida ===
{{Infobox Hurricane Small
{{Infobox Hurricane Small
|Basin=EPac
| Basin = EPac
|Image=Elida 1990-06-28 1801Z.png
| Image = Elida 1990-06-28 1801Z.png
|Track=Elida 1990 track.png
| Track = Elida 1990 track.png
|Formed=June 26
| Formed = June 26
|Dissipated=July 2
| Dissipated = July 2
|1-min winds=70
| 1-min winds = 70
|Pressure=990
| Pressure = 990
}}
}}
A tropical wave came off the coast of Africa into the eastern Atlantic Ocean on June 10 and 11. The system moved across the Atlantic and entered into the northeastern Pacific Ocean.<ref name="elidaprelim1">{{cite web|author=Lawrence, Miles|year=1990|title=Hurricane Elida Preliminary Report, Page 1|publisher=National Hurricane Center|access-date=January 2, 2011|url=http://www.nhc.noaa.gov/archive/storm_wallets/epacific/ep1990/elida/prenhc/prelim01.gif}}</ref> The wave became a significant tropical system, with [[cyclone|cyclonic]] turning in the lower and middle layers of the system's cloudiness on June 25. The center of circulation was located {{convert|345|mi|km|abbr=on}} south of Acapulco, Mexico. The system exhibited sufficient organization to be considered Tropical Depression Five-E on June 26. The depression quickly strengthened and became Tropical Storm Elida later that day. The track of Elida was west-northwestward to northwestward from June 27 through June 28. Some [[rainband]]s moved over the mountainous region of southwestern Mexico, but no flooding, damage, or casualties were reported as a result. Elida continued strengthening and it was upgraded to a hurricane early on June 28 passing directly over [[Socorro Island]] later in the day, right as Elida reached peak strength of {{convert|80|mph|km/h|abbr=on}}, dropping {{convert|3.7|in|mm|abbr=on}} of rain on the island. Some windows broke also as a result, and minor structural damage was reported as a result on the island.<ref name="elidaprelim1"/><ref name="elidaprelim2">{{cite web|author=Lawrence, Miles|year=1990|title=Hurricane Elida Preliminary Report, Page 2|publisher=National Hurricane Center|access-date=January 2, 2011|url=http://www.nhc.noaa.gov/archive/storm_wallets/epacific/ep1990/elida/prenhc/prelim02.gif}}</ref>
A tropical wave came off the coast of Africa into the eastern Atlantic Ocean on June 10 and 11. The system moved across the Atlantic and entered into the northeastern Pacific Ocean.<ref name="elidaprelim1">{{cite web|author=Lawrence, Miles|year=1990|title=Hurricane Elida Preliminary Report, Page 1|publisher=National Hurricane Center|access-date=January 2, 2011|url=http://www.nhc.noaa.gov/archive/storm_wallets/epacific/ep1990/elida/prenhc/prelim01.gif}}</ref> The wave became a significant tropical system, with [[cyclone|cyclonic]] turning in the lower and middle layers of the system's cloudiness on June 25. The center of circulation was located {{convert|345|mi|km|abbr=on}} south of Acapulco, Mexico. The system exhibited sufficient organization to be considered Tropical Depression Five-E on June 26. The depression quickly strengthened and became Tropical Storm Elida later that day. The track of Elida was west-northwestward to northwestward from June 27 through June 28. Some [[rainband]]s moved over the mountainous region of southwestern Mexico, but no flooding, damage, or casualties were reported as a result. Elida continued strengthening and it was upgraded to a hurricane early on June 28 passing directly over [[Socorro Island]] later in the day, right as Elida reached peak strength of {{convert|80|mph|km/h|abbr=on}}, dropping {{convert|3.7|in|mm|abbr=on}} of rain on the island. Some windows broke also as a result, and minor structural damage was reported as a result on the island.<ref name="elidaprelim1"/><ref name="elidaprelim2">{{cite web|author=Lawrence, Miles|year=1990|title=Hurricane Elida Preliminary Report, Page 2|publisher=National Hurricane Center|access-date=January 2, 2011|url=http://www.nhc.noaa.gov/archive/storm_wallets/epacific/ep1990/elida/prenhc/prelim02.gif}}</ref>
Line 199: Line 198:
=== Tropical Depression Six-E ===
=== Tropical Depression Six-E ===
{{Infobox Hurricane Small
{{Infobox Hurricane Small
|Basin=EPac
| Basin = EPac
|Image=Tropical depression 6-E 1990.JPG
| Image = Tropical depression 6-E 1990.JPG
|Track=Temporary cyclone north.svg
| Track = 06E 1990 track.png
|Formed=June 29
| Formed = June 29
|Dissipated=July 3
| Dissipated = July 3
|1-min winds=30
| 1-min winds = 30
|Pressure=1007
| Pressure = 1007
}}
}}
An area of disturbed weather south of Acapulco organized into Tropical Depression Six-E on June 29 and the system began to move northwest. Originally the system was expected to reach [[tropical storm]] strength and near hurricane intensity by late on July 2 or early on July 3,<ref name="6-Edisc1">{{cite web|url=http://www.nhc.noaa.gov/archive/storm_wallets/epacific/ep1990/td6e/tropdisc/tcd2921z.gif|title=Tropical Cyclone Discussion: Tropical Depression Six-E (#1)|last=Avila|first=Lixion|date=June 29, 1990|publisher=National Hurricane Center|access-date=January 2, 2011}}</ref> however persistent vertical wind shear over the system impeded its development.<ref name="6-Edisc3">{{cite web|url=http://www.nhc.noaa.gov/archive/storm_wallets/epacific/ep1990/td6e/tropdisc/tcd3009z.gif|title=Tropical Cyclone Discussion: Tropical Depression Six-E (#3)|last=Avila|first=Lixion|date=June 30, 1990|publisher=National Hurricane Center|access-date=January 2, 2011}}</ref> After convection began to merge into the [[Intertropical Convergence Zone]] (ITCZ), the National Hurricane Center discontinued advisories on Tropical Depression Six-E, stating that the depression dissipated, and regeneration seemed unlikely.<ref name="6-Edisc5">{{cite web|url=http://www.nhc.noaa.gov/archive/storm_wallets/epacific/ep1990/td6e/tropdisc/tcd3021z.gif|title=Tropical Cyclone Discussion: Tropical Depression Six-E (#5)|date=June 30, 1990|publisher=National Hurricane Center|access-date=January 2, 2011}}</ref>
An area of disturbed weather south of Acapulco organized into Tropical Depression Six-E on June 29 and the system began to move northwest. Originally the system was expected to reach [[tropical storm]] strength and near hurricane intensity by late on July 2 or early on July 3,<ref name="6-Edisc1">{{cite web|url=http://www.nhc.noaa.gov/archive/storm_wallets/epacific/ep1990/td6e/tropdisc/tcd2921z.gif|title=Tropical Cyclone Discussion: Tropical Depression Six-E (#1)|last=Avila|first=Lixion|date=June 29, 1990|publisher=National Hurricane Center|access-date=January 2, 2011}}</ref> however persistent vertical wind shear over the system impeded its development.<ref name="6-Edisc3">{{cite web|url=http://www.nhc.noaa.gov/archive/storm_wallets/epacific/ep1990/td6e/tropdisc/tcd3009z.gif|title=Tropical Cyclone Discussion: Tropical Depression Six-E (#3)|last=Avila|first=Lixion|date=June 30, 1990|publisher=National Hurricane Center|access-date=January 2, 2011}}</ref> After convection began to merge into the [[Intertropical Convergence Zone]] (ITCZ), the National Hurricane Center discontinued advisories on Tropical Depression Six-E, stating that the depression dissipated, and regeneration seemed unlikely.<ref name="6-Edisc5">{{cite web|url=http://www.nhc.noaa.gov/archive/storm_wallets/epacific/ep1990/td6e/tropdisc/tcd3021z.gif|title=Tropical Cyclone Discussion: Tropical Depression Six-E (#5)|date=June 30, 1990|publisher=National Hurricane Center|access-date=January 2, 2011}}</ref>
Line 214: Line 213:
=== Hurricane Fausto ===
=== Hurricane Fausto ===
{{Infobox Hurricane Small
{{Infobox Hurricane Small
|Basin=EPac
| Basin = EPac
|Image=Fausto 1990-07-08 2000Z.png
| Image = Fausto 1990-07-08 2000Z.png
|Track=Fausto 1990 track.png
| Track = Fausto 1990 track.png
|Formed=July 6
| Formed = July 6
|Dissipated=July 12
| Dissipated = July 12
|1-min winds=75
| 1-min winds = 75
|Pressure=979
| Pressure = 979
}}
}}
A tropical wave came off the northwest coast of Africa on June 19. The wave crossed the Atlantic Ocean and Caribbean Sea, into the warm waters of the northeastern Pacific Ocean, on July 2. An area of disturbed weather moved northwards towards the [[Gulf of Tehuantepec]] and became Tropical Depression Seven-E early on July 6. The depression moved northwest, and because of increased organization of deep convection, was designated Tropical Storm Fausto on July 7, {{convert|265|mi|km|abbr=on}} south of [[Manzanillo, Colima|Manzanillo]], Mexico. A weakly defined eye formed on July 8, and the storm was upgraded to Hurricane Fausto, {{convert|310|mi|km|abbr=on}} south of [[Cabo San Lucas, Mexico|Cabo San Lucas]].<ref name="faustoprelim1">{{cite web|author=Mayfield, Max|year=1990|title=Hurricane Fausto Preliminary Report, Page 1|publisher=National Hurricane Center|access-date=January 2, 2011|url=http://www.nhc.noaa.gov/archive/storm_wallets/epacific/ep1990/fausto/prenhc/prelim01.gif}}</ref>
A tropical wave came off the northwest coast of Africa on June 19. The wave crossed the Atlantic Ocean and Caribbean Sea, into the warm waters of the northeastern Pacific Ocean, on July 2. An area of disturbed weather moved northwards towards the [[Gulf of Tehuantepec]] and became Tropical Depression Seven-E early on July 6. The depression moved northwest, and because of increased organization of deep convection, was designated Tropical Storm Fausto on July 7, {{convert|265|mi|km|abbr=on}} south of [[Manzanillo, Colima|Manzanillo]], Mexico. A weakly defined eye formed on July 8, and the storm was upgraded to Hurricane Fausto, {{convert|310|mi|km|abbr=on}} south of [[Cabo San Lucas, Mexico|Cabo San Lucas]].<ref name="faustoprelim1">{{cite web|author=Mayfield, Max|year=1990|title=Hurricane Fausto Preliminary Report, Page 1|publisher=National Hurricane Center|access-date=January 2, 2011|url=http://www.nhc.noaa.gov/archive/storm_wallets/epacific/ep1990/fausto/prenhc/prelim01.gif}}</ref>


Fausto peaked in strength with winds of 85&nbsp;mph (140&nbsp;km/h) and a central pressure of {{convert|979|mb|inHg|abbr=on}} on July 9. Fausto passed 40&nbsp;mi (60&nbsp;km) north of Socorro Island causing a northwest wind of 40&nbsp;mph (60&nbsp;km/h), and {{convert|4.3|in|mm|abbr=on}} of rain at that location. The hurricane fluctuated in intensity on July 10,<ref name="faustoprelim1"/><ref name="faustoprelim2">{{cite web|author=Mayfield, Max|year=1990|title=Hurricane Fausto Preliminary Report, Page 2|publisher=National Hurricane Center|access-date=January 2, 2011|url=http://www.nhc.noaa.gov/archive/storm_wallets/epacific/ep1990/fausto/prenhc/prelim02.gif}}</ref> before weakening into a tropical storm later that day, {{convert|403|mi|km|abbr=on}} west of Cabo San Lucas. The weakening Fausto moved over continuing cooler waters, and was downgraded to a tropical depression on July 11, {{convert|690|mi|km|abbr=on}} west of Cabo San Lucas. The depression dissipated as a tropical cyclone on July 13, and its low level circulation of clouds persisted for a few days.<ref name="faustoprelim1"/>
Fausto peaked in strength with winds of {{convert|85|mph|km/h|abbr=on}} and a central pressure of {{convert|979|mb|inHg|abbr=on}} on July 9. Fausto passed {{convert|40|mi|km|abbr=on}} north of Socorro Island causing a northwest wind of {{convert|40|mph|km/h|abbr=on}}, and {{convert|4.3|in|mm|abbr=on}} of rain at that location. The hurricane fluctuated in intensity on July 10,<ref name="faustoprelim1"/><ref name="faustoprelim2">{{cite web|author=Mayfield, Max|year=1990|title=Hurricane Fausto Preliminary Report, Page 2|publisher=National Hurricane Center|access-date=January 2, 2011|url=http://www.nhc.noaa.gov/archive/storm_wallets/epacific/ep1990/fausto/prenhc/prelim02.gif}}</ref> before weakening into a tropical storm later that day, {{convert|403|mi|km|abbr=on}} west of Cabo San Lucas. The weakening Fausto moved over continuing cooler waters, and was downgraded to a tropical depression on July 11, {{convert|690|mi|km|abbr=on}} west of Cabo San Lucas. The depression dissipated as a tropical cyclone on July 13, and its low level circulation of clouds persisted for a few days.<ref name="faustoprelim1"/>
{{clear}}
{{clear}}


=== Hurricane Genevieve ===
=== Hurricane Genevieve ===
{{Infobox Hurricane Small
{{Infobox Hurricane Small
|Basin=EPac
| Basin = EPac
|Image=Hurricane Genevieve Jul 15 1990 1731Z.jpg
| Image = Hurricane Genevieve Jul 15 1990 1731Z.jpg
|Track=Genevieve 1990 track.png
| Track = Genevieve 1990 track.png
|Formed=July 10
| Formed = July 10
|Dissipated=July 18
| Dissipated = July 18
|1-min winds=90
| 1-min winds = 90
|Pressure=970
| Pressure = 970
}}
}}
A tropical wave moved off the coast of Africa on June 25 and moved across the Atlantic Ocean and central Caribbean Sea with little development. Within the western Caribbean Sea, convection developed with the wave on July 7. The system became better organized as it moved into the northeastern Pacific Ocean. The system was upgraded to Tropical Depression Eight-E on July 11. The depression moved west-northwest, with a good outflow to the north, and gradually strengthened into Tropical Storm Genevieve later that day. Genevieve continued to strengthen, reaching hurricane strength on July 13.<ref name="genevieveprelim1">{{cite web|author=Case, Robert|date=August 16, 1990|title=Hurricane Genevieve Preliminary Report 1|publisher=National Hurricane Center|access-date=January 2, 2011|url=http://www.nhc.noaa.gov/archive/storm_wallets/epacific/ep1990/geneviev/prenhc/prelim01.gif}}</ref> The storm approached within {{convert|23|mi|km|abbr=on}} of Socorro Island where a sustained wind of {{convert|44|mph|km/h|abbr=on}} and gust of {{convert|50|mph|km/h|abbr=on}} were reported, before the weather equipment on the island failed.<ref name="genevieveprelim2">{{cite web|author=Case, Robert|date=August 16, 1990|title=Hurricane Genevieve Preliminary Report, Page 2|publisher=National Hurricane Center|access-date=January 3, 2011|url=http://www.nhc.noaa.gov/archive/storm_wallets/epacific/ep1990/geneviev/prenhc/prelim02.gif}}</ref>
A tropical wave moved off the coast of Africa on June 25 and moved across the Atlantic Ocean and central Caribbean Sea with little development. Within the western Caribbean Sea, convection developed with the wave on July 7. The system became better organized as it moved into the northeastern Pacific Ocean. The system was upgraded to Tropical Depression Eight-E on July 11. The depression moved west-northwest, with a good outflow to the north, and gradually strengthened into Tropical Storm Genevieve later that day. Genevieve continued to strengthen, reaching hurricane strength on July 13.<ref name="genevieveprelim1">{{cite web|author=Case, Robert|date=August 16, 1990|title=Hurricane Genevieve Preliminary Report 1|publisher=National Hurricane Center|access-date=January 2, 2011|url=http://www.nhc.noaa.gov/archive/storm_wallets/epacific/ep1990/geneviev/prenhc/prelim01.gif}}</ref> The storm approached within {{convert|23|mi|km|abbr=on}} of Socorro Island where a sustained wind of {{convert|44|mph|km/h|abbr=on}} and gust of {{convert|50|mph|km/h|abbr=on}} were reported, before the weather equipment on the island failed.<ref name="genevieveprelim2">{{cite web|author=Case, Robert|date=August 16, 1990|title=Hurricane Genevieve Preliminary Report, Page 2|publisher=National Hurricane Center|access-date=January 3, 2011|url=http://www.nhc.noaa.gov/archive/storm_wallets/epacific/ep1990/geneviev/prenhc/prelim02.gif}}</ref>


The hurricane began to turn west because of the strengthening and growing ridge to its north. Increasing outflow aloft began to form, and the hurricane reached its peak strength of 105&nbsp;mph (170&nbsp;km/h) with a well-defined eye at its center of circulation.<ref name="genevieveprelim1"/><ref name="july111422ztcd">{{cite web|date=July 11, 1990|title=Tropical Cyclone Discussion: Tropical Depression Eight-E|publisher=National Hurricane Center|access-date=January 3, 2011|url=http://www.nhc.noaa.gov/archive/storm_wallets/epacific/ep1990/geneviev/tropdisc/tcd1115z.gif}}</ref> Genevieve turned northwest on July 16 into an area with strong vertical wind shear and low water temperatures. The hurricane quickly weakened into a tropical storm on July 17 and then into a tropical depression on July 18. Genevieve dissipated as a tropical cyclone later in the day, reduced to a circulation in the [[stratocumulus cloud]] field.<ref name="genevieveprelim1"/>
The hurricane began to turn west because of the strengthening and growing ridge to its north. Increasing outflow aloft began to form, and the hurricane reached its peak strength of {{convert|105|mph|km/h|abbr=on}} with a well-defined eye at its center of circulation.<ref name="genevieveprelim1"/><ref name="july111422ztcd">{{cite web|date=July 11, 1990|title=Tropical Cyclone Discussion: Tropical Depression Eight-E|publisher=National Hurricane Center|access-date=January 3, 2011|url=http://www.nhc.noaa.gov/archive/storm_wallets/epacific/ep1990/geneviev/tropdisc/tcd1115z.gif}}</ref> Genevieve turned northwest on July 16 into an area with strong vertical wind shear and low water temperatures. The hurricane quickly weakened into a tropical storm on July 17 and then into a tropical depression on July 18. Genevieve dissipated as a tropical cyclone later in the day, reduced to a circulation in the [[stratocumulus cloud]] field.<ref name="genevieveprelim1"/>
{{clear}}
{{clear}}


=== Hurricane Hernan ===
=== Hurricane Hernan ===
{{Infobox Hurricane Small
{{Infobox Hurricane Small
|Basin=EPac
| Basin = EPac
|Image=File:Hernan 1990-07-23 0100Z.png
| Image = File:Hernan 1990-07-23 0100Z.png
|Track=Hernan 1990 track.png
| Track = Hernan 1990 track.png
|Formed=July 19
| Formed = July 19
|Dissipated=July 31
| Dissipated = July 31
|1-min winds=135
| 1-min winds = 135
|Pressure=928
| Pressure = 928
}}
}}
A tropical wave that moved off the northwest coast of Africa on July 4 passed through the Atlantic Ocean and Caribbean Sea without significant development.<ref name="hernanprelim1">{{cite web|author=Gerrish, Hal|year=1990|title=Hurricane Hernan Preliminary Report, Page 1|publisher=National Hurricane Center|access-date=January 3, 2011|url=http://www.nhc.noaa.gov/archive/storm_wallets/epacific/ep1990/hernan/prenhc/prelim01.gif}}</ref> The wave moved across Central America into the northeastern Pacific Ocean on July 15. Thunderstorm activity increased in the system between July 16 and 18 before rainbands became present within the tropical disturbance on July 19. Tropical Depression Nine-E formed later that day while 565&nbsp;mi (910&nbsp;km) southwest of Acapulco, Mexico.<ref name="80columndata"/>
A tropical wave that moved off the northwest coast of Africa on July 4 passed through the Atlantic Ocean and Caribbean Sea without significant development.<ref name="hernanprelim1">{{cite web|author=Gerrish, Hal|year=1990|title=Hurricane Hernan Preliminary Report, Page 1|publisher=National Hurricane Center|access-date=January 3, 2011|url=http://www.nhc.noaa.gov/archive/storm_wallets/epacific/ep1990/hernan/prenhc/prelim01.gif}}</ref> The wave moved across Central America into the northeastern Pacific Ocean on July 15. Thunderstorm activity increased in the system between July 16 and 18 before rainbands became present within the tropical disturbance on July 19. Tropical Depression Nine-E formed later that day while {{convert|565|mi|km|abbr=on}} southwest of Acapulco, Mexico.<ref name="80columndata"/>


Tropical Depression Nine-E strengthened into Tropical Storm Hernan on July 21 while 684&nbsp;mi (1,100&nbsp;km) south of Cabo San Lucas. The tropical storm continued to strengthen and as it moved to the northwest, and became a hurricane late on July 21. Hernan continued to strengthen and as it passed 145&nbsp;mi (230&nbsp;km) southwest of [[Clarion Island]]. On July 23, Hernan reached its peak strength of 155&nbsp;mph (250&nbsp;km/h) and minimum pressure of {{convert|928|mb|inHg|abbr=on}} as the center of circulation was 207&nbsp;mi (335&nbsp;km) south-southwest of Clarion Island. On July 24, concentric eyewalls (one eyewall located inside another) formed around the center of Hernan, which was the first time this pattern had been observed with an eastern Pacific hurricane.<ref name="hernanprelim1"/><ref name="hernanprelim2">{{cite web|author=Gerrish, Hal|year=1990|title=Hurricane Hernan Preliminary Report, Page 2|publisher=National Hurricane Center|access-date=January 2, 2011|url=http://www.nhc.noaa.gov/archive/storm_wallets/epacific/ep1990/hernan/prenhc/prelim02.gif}}</ref>
Tropical Depression Nine-E strengthened into Tropical Storm Hernan on July 21 while {{convert|684|mi|km|abbr=on}} south of Cabo San Lucas. The tropical storm continued to strengthen and as it moved to the northwest, and became a hurricane late on July 21. Hernan continued to strengthen and as it passed {{convert|145|mi|km|abbr=on}} southwest of [[Clarion Island]]. On July 23, Hernan reached its peak strength of {{convert|155|mph|km/h|abbr=on}} and minimum pressure of {{convert|928|mb|inHg|abbr=on}} as the center of circulation was {{convert|207|mi|km|abbr=on}} south-southwest of Clarion Island. On July 24, concentric eyewalls (one eyewall located inside another) formed around the center of Hernan, which was the first time this pattern had been observed with an eastern Pacific hurricane.<ref name="hernanprelim1"/><ref name="hernanprelim2">{{cite web|author=Gerrish, Hal|year=1990|title=Hurricane Hernan Preliminary Report, Page 2|publisher=National Hurricane Center|access-date=January 2, 2011|url=http://www.nhc.noaa.gov/archive/storm_wallets/epacific/ep1990/hernan/prenhc/prelim02.gif}}</ref>


Hernan kept Category&nbsp;4 hurricane intensity a few more days and hurricane strength for six days overall. The hurricane weakened into a tropical storm on July 28 as it moved over cooler waters. Hernan turned more to the west as its low level center became separated from its thunderstorm activity and was steering by a surface high-pressure system to its north. Hernan moved over cooler waters, dissipating as a tropical cyclone early on July 31.<ref name="hernanprelim1"/><ref name="july310216ztcd">{{cite web|author=Satchwell, Barry|date=July 31, 1990|title=Tropical Cyclone Discussion: Tropical Depression Hernan|publisher=National Hurricane Center|access-date=January 3, 2011|url=http://www.nhc.noaa.gov/archive/storm_wallets/epacific/ep1990/hernan/tropdisc/tcd3103z.gif}}</ref>
Hernan kept Category&nbsp;4 hurricane intensity a few more days and hurricane strength for six days overall. The hurricane weakened into a tropical storm on July 28 as it moved over cooler waters. Hernan turned more to the west as its low level center became separated from its thunderstorm activity and was steering by a surface high-pressure system to its north. Hernan moved over cooler waters, dissipating as a tropical cyclone early on July 31.<ref name="hernanprelim1"/><ref name="july310216ztcd">{{cite web|author=Satchwell, Barry|date=July 31, 1990|title=Tropical Cyclone Discussion: Tropical Depression Hernan|publisher=National Hurricane Center|access-date=January 3, 2011|url=http://www.nhc.noaa.gov/archive/storm_wallets/epacific/ep1990/hernan/tropdisc/tcd3103z.gif}}</ref>
Line 261: Line 260:
=== Hurricane Iselle ===
=== Hurricane Iselle ===
{{Infobox Hurricane Small
{{Infobox Hurricane Small
|Basin=EPac
| Basin = EPac
|Image=Hurricane Iselle Jul 25 1990 1801Z.jpg
| Image = Hurricane Iselle Jul 25 1990 1801Z.jpg
|Track=Iselle 1990 track.png
| Track = Iselle 1990 track.png
|Formed=July 20
| Formed = July 20
|Dissipated=July 30
| Dissipated = July 30
|1-min winds=105
| 1-min winds = 105
|Pressure=958
| Pressure = 958
}}
}}
A tropical wave moved off the coast of Africa on July&nbsp;7. The wave moved west, but it was not until it moved across the Caribbean Sea that the wave's convection organized.<ref name="iselleprelim1">{{cite web|author=Avila, Lixion|date=August 15, 1990|title=Hurricane Iselle Preliminary Report, Page 1|publisher=National Hurricane Center|access-date=January 2, 2011|url=http://www.nhc.noaa.gov/archive/storm_wallets/epacific/ep1990/iselle/prenhc/prelim01.gif}}</ref> The system entered into the northeastern Pacific Ocean with concentrated convection and a surface center of circulation while southeast of Acapulco. Moving west-northwest, Tropical Depression Ten-E formed on July 20 {{convert|393|mi|km|abbr=on}} south of [[Puerto Ángel]], Mexico. Early on the following day, the depression strengthened into Tropical Storm Iselle. The storm continued strengthening while in the proximity of Hurricane Hernan, becoming a hurricane on July&nbsp;22.<ref name="80columndata"/>
A tropical wave moved off the coast of Africa on July&nbsp;7. The wave moved west, but it was not until it moved across the Caribbean Sea that the wave's convection organized.<ref name="iselleprelim1">{{cite web|author=Avila, Lixion|date=August 15, 1990|title=Hurricane Iselle Preliminary Report, Page 1|publisher=National Hurricane Center|access-date=January 2, 2011|url=http://www.nhc.noaa.gov/archive/storm_wallets/epacific/ep1990/iselle/prenhc/prelim01.gif}}</ref> The system entered into the northeastern Pacific Ocean with concentrated convection and a surface center of circulation while southeast of Acapulco. Moving west-northwest, Tropical Depression Ten-E formed on July 20 {{convert|393|mi|km|abbr=on}} south of [[Puerto Ángel]], Mexico. Early on the following day, the depression strengthened into Tropical Storm Iselle. The storm continued strengthening while in the proximity of Hurricane Hernan, becoming a hurricane on July&nbsp;22.<ref name="80columndata"/>
Line 276: Line 275:
=== Tropical Depression Eleven-E ===
=== Tropical Depression Eleven-E ===
{{Infobox Hurricane Small
{{Infobox Hurricane Small
|Basin=EPac
| Basin = EPac
|Image=Td-11e 1990.JPG
| Image = Td-11e 1990.JPG
|Track=Temporary cyclone north.svg
| Track = 11E 1990 track.png
|Formed=July 24
| Formed = July 24
|Dissipated=July 26
| Dissipated = July 26
|1-min winds=25
| 1-min winds = 25
|Pressure=1009
| Pressure = 1009
}}
}}
On July 24 a tropical disturbance behind Hurricane Hernan strengthened into a [[tropical depression]]. Due to the close proximity of Hernan to its west, the development of the depression was hindered due to vertical wind shear from the outflow of Hernan. This wind shear dissipated the depression on July 26, and its remnants were absorbed by the nearby cyclone. No damages or casualties were caused by the depression as it was well out to sea.<ref name="tropdisc11e">{{cite web|author=National Hurricane Center|year=1990|title=Tropical Discussions on Tropical Depression Eleven-E|publisher=National Hurricane Center|access-date=January 3, 2011|url=http://www.nhc.noaa.gov/archive/storm_wallets/epacific/ep1990/td11e/tropdisc}}</ref>
On July 24 a tropical disturbance behind Hurricane Hernan strengthened into a [[tropical depression]]. Due to the close proximity of Hernan to its west, the development of the depression was hindered due to vertical wind shear from the outflow of Hernan. This wind shear dissipated the depression on July 26, and its remnants were absorbed by the nearby cyclone. No damages or casualties were caused by the depression as it was well out to sea.<ref name="tropdisc11e">{{cite web|author=National Hurricane Center|year=1990|title=Tropical Discussions on Tropical Depression Eleven-E|publisher=National Hurricane Center|access-date=January 3, 2011|url=http://www.nhc.noaa.gov/archive/storm_wallets/epacific/ep1990/td11e/tropdisc}}</ref>
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=== Tropical Storm Aka ===
=== Tropical Storm Aka ===
{{Infobox Hurricane Small
{{Infobox Hurricane Small
|Basin=EPac
| Basin = EPac
|Image=Aka 1990.JPG
| Image = Aka aug 13 1990 0203Z.jpg
|Track=Aka 1990 track.png
| Track = Aka 1990 track.png
|Formed=August 7
| Formed = August 7
|Dissipated=August 13
| Dissipated = August 13 ([[1990 Pacific typhoon season#Tropical Storm Aka|exited basin]])
|1-min winds=55
| 1-min winds = 55
|Pressure=994
| Pressure = 994
}}
}}

Tropical Storm Aka was the only tropical storm to form in the Central North Pacific during 1990. An area of disturbed weather began to organize on August 6. By August 7, the system became well-enough organized to become designated Tropical depression One-C. The depression intensified into a tropical storm while moving west, to the south of the [[Hawaiian Islands]]. On August 10, Tropical Storm Aka peaked with maximum sustained winds of {{convert|60|mph|km/h|abbr=on}}. The storm continued to move west and approached [[Johnston Island]], though the island's weather did not deteriorate. The tropical storm crossed the International Date Line on August 13.<ref name="akareport">{{cite web|year=1990|title=August 7–13, 1990 (Tropical Storm Aka)|publisher=Central Pacific Hurricane Center|access-date=January 2, 2011|url=http://www.prh.noaa.gov/cphc/summaries/1990.php}}</ref> Aka weakened back into a depression and dissipated two days later on August 15.<ref name="80columndata"/>
Tropical Storm Aka was the only tropical storm to form in the Central North Pacific during 1990. An area of disturbed weather began to organize on August 6. By August 7, the system became well-enough organized to become designated Tropical depression One-C. The depression intensified into a tropical storm while moving west, to the south of the [[Hawaiian Islands]]. On August 10, Tropical Storm Aka peaked with maximum sustained winds of {{convert|60|mph|km/h|abbr=on}}. The storm continued to move west and approached [[Johnston Island]], though the island's weather did not deteriorate. The tropical storm crossed the International Date Line on August 13.<ref name="CPHC 90">{{cite report|date=April 1991|title=1990 Tropical Cyclones - Central North Pacific|publisher=Central Pacific Hurricane Center|location=Honolulu, Hawaii|url=https://repository.library.noaa.gov/view/noaa/49714/noaa_49714_DS1.pdf?download-document-submit=Download|access-date=February 3, 2024}}</ref> Aka weakened back into a depression and dissipated two days later on August 15.<ref name="80columndata"/>
{{clear}}
{{clear}}


=== Tropical Depression Diana ===
=== Tropical Depression Diana ===
{{main|Hurricane Diana}}
{{main|Hurricane Diana}}
{{see also|List of Atlantic–Pacific crossover hurricanes}}
{{Infobox Hurricane Small
{{Infobox Hurricane Small
|Basin=EPac
| Basin = EPac
|Formed=August 8
| Formed = August 8
|Dissipated=August 9
| Dissipated = August 9
|Image=Hurricane Diana 07 aug 1990 2004Z.jpg
| Image = Diana 1990-08-07 2004Z.jpg
|Track=Diana 1990 track.png
| Track = Diana 1990 track.png
|1-min winds=30
| 1-min winds = 30
|Pressure=1004
| Pressure = 1004
}}
}}
Hurricane Diana struck eastern Mexico and managed to hold together, remaining a tropical depression as it entered the eastern Pacific Ocean late on August 8. Although Tropical Depression Diana entered the eastern Pacific, the National Hurricane Center did not re-classify the system. No re-intensification occurred after the system entered the eastern Pacific, and it had dissipated as a tropical cyclone by the following day. The remnant tropical disturbance recurved through the [[Gulf of California]] while developing significant convection before it moved into northwest Mexico, which brought rainfall amounts of over {{convert|10|in|mm|abbr=on}} to local areas within the state of [[Sonora]]. The remnant disturbance moved into the American Southwest on August 11.<ref>{{cite web|url=http://www.wpc.ncep.noaa.gov/tropical/rain/diana1990.html|title=Hurricane Diana – August 4–14, 1990|access-date=January 2, 2011|date=January 27, 2007|publisher=Hydrometeorological Prediction Center|author=Roth, David}}</ref>
Atlantic basin Hurricane Diana made landfall on August&nbsp;7 at Category&nbsp;2 strength in [[Tamiahua]], [[Tamaulipas]], along the [[Gulf of Mexico]] coast. The system quickly deteriorated inland while traversing the high terrain of Mexico. Some convection remained as it emerged into the eastern Pacific Ocean late on August&nbsp;8.<ref name="Diana1">{{cite report|chapter-url=http://www.nhc.noaa.gov/archive/storm_wallets/atlantic/atl1990-prelim/diana/prelim01.gif|title=Preliminary Report: Hurricane Diana|chapter=Synoptic History|page=1|author=Avila, Lixion A.|year=1990|publisher=National Hurricane Center|access-date=February 3, 2024|location=Miami, Florida}}</ref> Though Diana crossed between basins, the National Hurricane Center did not re-classify it as an eastern Pacific system. No re-intensification occurred, and by the following day it lost all tropical characteristics. The remnant disturbance turned northward around the eastern periphery of an upper-low and tracked through the [[Gulf of California]]. Convection flared up before it moved into northwest Mexico, bringing rainfall amounts of over {{convert|10|in|mm|abbr=on}} to local areas of [[Sonora]]. Later, after moving into [[Arizona]], the disturbance dissipated by early on August&nbsp;14.<ref name=Diana1990>{{cite web|url=http://www.wpc.ncep.noaa.gov/tropical/rain/diana1990.html|title=Hurricane Diana – August 4–14, 1990|access-date=January 2, 2011|date=January 27, 2007|publisher=Hydrometeorological Prediction Center|author=Roth, David}}</ref>
{{Clear}}
{{Clear}}


=== Tropical Depression Two-C ===
=== Tropical Depression Two-C ===
{{Infobox Hurricane Small
{{Infobox Hurricane Small
|Basin=EPac
| Basin = EPac
|Image=1990 2-C depression.JPG
| Image = 1990 2-C depression.JPG
|Track=Temporary cyclone north.svg
| Track = Two-C 1990 track.png
|Formed=August 10
| Formed = August 10
|Dissipated=August 13
| Dissipated = August 13
|1-min winds=30
| 1-min winds = 30
|Pressure=1000
| Pressure = 1000
}}
}}
Tropical Depression Two-C was the second and last tropical cyclone to develop within the north-central Pacific Ocean in 1990. The depression developed from a tropical disturbance well southeast of Hawaii, which became much better organized on the night of August 10. The tropical depression moved in a west northwest direction for the next 18&nbsp;hours and then changed to a west-southwest track on August 11. As it turned more to the southwest, the depression weakened until it dissipated on August 13 about {{convert|600|mi|km|abbr=on}} south-southeast of [[Hilo, Hawaii]].<ref name="tropdepression2C">{{cite web|year=1990|title=August 10–13, 1990 (Tropical Depression Two-C)|publisher=Central Pacific Hurricane Center|access-date=January 2, 2011|url=http://www.prh.noaa.gov/cphc/summaries/1990.php}}</ref>
Tropical Depression Two-C was the second and last tropical cyclone to develop within the north-central Pacific Ocean in 1990. The depression developed from a tropical disturbance well southeast of Hawaii, which became much better organized on the night of August 10. The tropical depression moved in a west northwest direction for the next 18&nbsp;hours and then changed to a west-southwest track on August 11. As it turned more to the southwest, the depression weakened until it dissipated on August 13 about {{convert|600|mi|km|abbr=on}} south-southeast of [[Hilo, Hawaii]].<ref name="CPHC 90"/>
{{clear}}
{{clear}}


=== Tropical Depression Twelve-E ===
=== Tropical Depression Twelve-E ===
{{Infobox Hurricane Small
{{Infobox Hurricane Small
|Basin=EPac
| Basin = EPac
|Formed=August 16
| Formed = August 16
|Dissipated=August 19
| Dissipated = August 19
|Image=TD12E1990081800zIR.jpg
| Image = TD12E1990081800zIR.jpg
|Track=Temporary cyclone north.svg
| Track = 12E 1990 track.png
|1-min winds=30
| 1-min winds = 30
|Pressure=1009
| Pressure = 1009
}}
}}
A persistent area of thunderstorm activity southwest of [[Puerto Vallarta]] became better organized and strengthened into Tropical Depression Twelve-E on August 16. Moving northwest, the system developed slowly as it was embedded within the [[Intertropical Convergence Zone]]. Easterly [[Wind shear|shear]] kept the system from reaching tropical storm strength and caused its ultimate dissipation on August 19. No damages or fatalities were caused by this depression.<ref name="tropical discussions on 12-E">{{cite web|author=Case|author2=Mayfield|author3=Lawrence|author4=Avila|author5=Gerrish|name-list-style=amp|year=1990|title=Tropical Discussions on 12-E|publisher=NOAA|access-date=December 20, 2006|url=http://www.nhc.noaa.gov/archive/storm_wallets/epacific/ep1990/td12e/tropdisc/}}</ref>
A persistent area of thunderstorm activity southwest of [[Puerto Vallarta]] became better organized and strengthened into Tropical Depression Twelve-E on August 16. Moving northwest, the system developed slowly as it was embedded within the [[Intertropical Convergence Zone]]. Easterly [[Wind shear|shear]] kept the system from reaching tropical storm strength and caused its ultimate dissipation on August 19. No damages or fatalities were caused by this depression.<ref name="tropical discussions on 12-E">{{cite web|author=Case|author2=Mayfield|author3=Lawrence|author4=Avila|author5=Gerrish|name-list-style=amp|year=1990|title=Tropical Discussions on 12-E|publisher=NOAA|access-date=December 20, 2006|url=http://www.nhc.noaa.gov/archive/storm_wallets/epacific/ep1990/td12e/tropdisc/}}</ref>
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=== Hurricane Julio ===
=== Hurricane Julio ===
{{Infobox Hurricane Small
{{Infobox Hurricane Small
|Basin=EPac
| Basin = EPac
|Image=Hurricane Julio Aug 21 1990 1831Z.jpg
| Image = Hurricane Julio Aug 21 1990 1831Z.jpg
|Track=Julio 1990 track.png
| Track = Julio 1990 track.png
|Formed=August 17
| Formed = August 17
|Dissipated=August 24
| Dissipated = August 24
|1-min winds=100
| 1-min winds = 100
|Pressure=960
| Pressure = 960
}}
}}
A tropical wave moved off the western coast of Africa on August 5, moving across the Atlantic Ocean and Caribbean Sea without significant development. The system entered the northeastern Pacific Ocean, and became well-enough organized to be upgraded to Tropical Depression Thirteen-E on August 17 while centered {{convert|404|mi|km|abbr=on}} south of Acapulco, Mexico. The depression moved on a west-northwestward track and strengthened, becoming Tropical Storm Julio on August 18. Strengthening continued and Julio reached hurricane strength on August 19. The cyclone peaked with maximum sustained winds of {{convert|115|mph|km/h|abbr=on}} on August 21. The storm turned westward and began weakening. Julio regained tropical storm status on August 23 and tropical depression status on August 24 before dissipating as a tropical cyclone later that day. No damage was reported from Julio.<ref name="julioprelim1">{{cite web|author=Lawrence, Miles|year=1990|title=Hurricane Julio Preliminary Report, Page 1|publisher=National Hurricane Center|access-date=January 2, 2011|url=http://www.nhc.noaa.gov/archive/storm_wallets/epacific/ep1990/julio/prenhc/prelim01.gif}}</ref>
A tropical wave moved off the western coast of Africa on August 5, moving across the Atlantic Ocean and Caribbean Sea without significant development. The system entered the northeastern Pacific Ocean, and became well-enough organized to be upgraded to Tropical Depression Thirteen-E on August 17 while centered {{convert|404|mi|km|abbr=on}} south of Acapulco, Mexico. The depression moved on a west-northwestward track and strengthened, becoming Tropical Storm Julio on August 18. Strengthening continued and Julio reached hurricane strength on August 19. The cyclone peaked with maximum sustained winds of {{convert|115|mph|km/h|abbr=on}} on August 21. The storm turned westward and began weakening. Julio regained tropical storm status on August 23 and tropical depression status on August 24 before dissipating as a tropical cyclone later that day. No damage was reported from Julio.<ref name="julioprelim1">{{cite web|author=Lawrence, Miles|year=1990|title=Hurricane Julio Preliminary Report, Page 1|publisher=National Hurricane Center|access-date=January 2, 2011|url=http://www.nhc.noaa.gov/archive/storm_wallets/epacific/ep1990/julio/prenhc/prelim01.gif}}</ref>
Line 355: Line 356:
=== Hurricane Kenna ===
=== Hurricane Kenna ===
{{Infobox Hurricane Small
{{Infobox Hurricane Small
|Basin=EPac
| Basin = EPac
|Image=Hurricane Kenna 1990 August 26.JPG
| Image = Hurricane Kenna 1990 August 26.JPG
|Track=Kenna 1990 track.png
| Track = Kenna 1990 track.png
|Formed=August 21
| Formed = August 21
|Dissipated=August 30
| Dissipated = August 30
|1-min winds=75
| 1-min winds = 75
|Pressure=980
| Pressure = 980
}}
}}
A tropical wave moved off the coast of Africa on August 9, and spawned [[1990 Atlantic hurricane season#Tropical Storm Fran|Tropical Storm Fran]] four days later, before it moved through the southern [[Windward Islands]] on August 14. While Fran dissipated shortly after that, the tropical wave progressed into the northeastern Pacific Ocean.<ref name="kennaprelim1">{{cite web|author=Case, Robert|year=1990|title=Hurricane Kenna Preliminary Report, Page 1|publisher=National Hurricane Center|access-date=January 3, 2011|url=http://www.nhc.noaa.gov/archive/storm_wallets/epacific/ep1990/kenna/prenhc/prelim01.gif}}</ref> The wave spawned Tropical Depression Fourteen-E {{convert|808|mi|km|abbr=on}} east-southeast of Hurricane Julio. The depression moved westward for the next several days. As Julio weakened, the depression began to increase in strength. It became Tropical Storm Kenna on August 22 and continued to strengthen into a hurricane on August 25, peaking with winds of {{convert|85|mph|km/h|abbr=on}} the next day. On August 26, a strong [[weather front|frontal trough]] weakened the high pressure system to the storm's north, causing a turn to the north during the next few days. The hurricane weakened in response to cooler water and increasing vertical wind shear, which removed convection from its center. Kenna weakened back to tropical storm strength on August 28,<ref name="august281423ztcd">{{cite web|author=Avila, Lixion|date=August 28, 1990|title=Tropical Cyclone Discussion: Tropical Storm Kenna|publisher=National Hurricane Center|access-date=January 3, 2011|url=http://www.nhc.noaa.gov/archive/storm_wallets/epacific/ep1990/kenna/tropdisc/tcd2815z.gif}}</ref> then into a tropical depression on August 29. The system dissipated as a tropical cyclone on August 30.<ref name="kennaprelim1"/><ref name="august302020ztcd">{{cite web|author=Avila, Lixion|date=August 30, 1990|title=Tropical Cyclone Discussion: Tropical Depression Kenna|publisher=National Hurricane Center|access-date=January 3, 2011|url=http://www.nhc.noaa.gov/archive/storm_wallets/epacific/ep1990/kenna/tropdisc/tcd3021z.gif}}</ref>
A tropical wave moved off the coast of Africa on August 9, and spawned [[1990 Atlantic hurricane season#Tropical Storm Fran|Tropical Storm Fran]] four days later, before it moved through the southern [[Windward Islands]] on August 14. While Fran dissipated shortly after that, the tropical wave progressed into the northeastern Pacific Ocean.<ref name="kennaprelim1">{{cite web|author=Case, Robert|year=1990|title=Hurricane Kenna Preliminary Report, Page 1|publisher=National Hurricane Center|access-date=January 3, 2011|url=http://www.nhc.noaa.gov/archive/storm_wallets/epacific/ep1990/kenna/prenhc/prelim01.gif}}</ref> The wave spawned Tropical Depression Fourteen-E {{convert|808|mi|km|abbr=on}} east-southeast of Hurricane Julio. The depression moved westward for the next several days. As Julio weakened, the depression began to increase in strength. It became Tropical Storm Kenna on August 22 and continued to strengthen into a hurricane on August 25, peaking with winds of {{convert|85|mph|km/h|abbr=on}} the next day. On August 26, a strong [[weather front|frontal trough]] weakened the high pressure system to the storm's north, causing a turn to the north during the next few days. The hurricane weakened in response to cooler water and increasing vertical wind shear, which removed convection from its center. Kenna weakened back to tropical storm strength on August 28,<ref name="august281423ztcd">{{cite web|author=Avila, Lixion|date=August 28, 1990|title=Tropical Cyclone Discussion: Tropical Storm Kenna|publisher=National Hurricane Center|access-date=January 3, 2011|url=http://www.nhc.noaa.gov/archive/storm_wallets/epacific/ep1990/kenna/tropdisc/tcd2815z.gif}}</ref> then into a tropical depression on August 29. The system dissipated as a tropical cyclone on August 30.<ref name="kennaprelim1"/><ref name="august302020ztcd">{{cite web|author=Avila, Lixion|date=August 30, 1990|title=Tropical Cyclone Discussion: Tropical Depression Kenna|publisher=National Hurricane Center|access-date=January 3, 2011|url=http://www.nhc.noaa.gov/archive/storm_wallets/epacific/ep1990/kenna/tropdisc/tcd3021z.gif}}</ref>
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=== Hurricane Lowell ===
=== Hurricane Lowell ===
{{Infobox Hurricane Small
{{Infobox Hurricane Small
|Basin=EPac
| Basin = EPac
|Image=Hurricane Lowell 1990 August 27.JPG
| Image = Hurricane Lowell 1990 August 27.JPG
|Track=Lowell 1990 track.png
| Track = Lowell 1990 track.png
|Formed=August 23
| Formed = August 23
|Dissipated=September 1
| Dissipated = September 1
|1-min winds=65
| 1-min winds = 65
|Pressure=986
| Pressure = 986
}}
}}
A tropical wave moved off the northwestern coast of Africa into the Atlantic Ocean on August 11. After moving across the Atlantic and Caribbean Sea without development, the system moved through the Intertropical Convergence Zone of the northeastern Pacific Ocean.<ref name="lowellprelim1">{{cite web|author=Mayfield, Max|year=1990|title=Hurricane Lowell Preliminary Report, Page 1|publisher=National Hurricane Center|access-date=January 3, 2011|url=http://www.nhc.noaa.gov/archive/storm_wallets/epacific/ep1990/lowell/prenhc/prelim01.gif}}</ref> The cloudiness moved northward toward the [[Gulf of Tehuantepec]] on August 22. The thunderstorm activity organized sufficiently for the system to be upgraded to Tropical Depression Fifteen-E on August 23 while {{convert|298|mi|km|abbr=on}} southeast of Acapulco, Mexico. The depression moved west-northwestward and strengthened into a tropical storm 217&nbsp;mi (350&nbsp;km) south-southwest of Puerto Vallarta on August 25. The storm began to turn more westward due to a strengthening high pressure system to its north and was upgraded to a hurricane on August 27 while {{convert|286|mi|km|abbr=on}} southwest of Cabo San Lucas. As the high to the north continued to strengthen, the hurricane turned west-southwest.<ref name="lowellprelim1"/>
A tropical wave moved off the northwestern coast of Africa into the Atlantic Ocean on August 11. After moving across the Atlantic and Caribbean Sea without development, the system moved through the Intertropical Convergence Zone of the northeastern Pacific Ocean.<ref name="lowellprelim1">{{cite web|author=Mayfield, Max|year=1990|title=Hurricane Lowell Preliminary Report, Page 1|publisher=National Hurricane Center|access-date=January 3, 2011|url=http://www.nhc.noaa.gov/archive/storm_wallets/epacific/ep1990/lowell/prenhc/prelim01.gif}}</ref> The cloudiness moved northward toward the [[Gulf of Tehuantepec]] on August 22. The thunderstorm activity organized sufficiently for the system to be upgraded to Tropical Depression Fifteen-E on August 23 while {{convert|298|mi|km|abbr=on}} southeast of Acapulco, Mexico. The depression moved west-northwestward and strengthened into a tropical storm {{convert|217|mi|km|abbr=on}} south-southwest of Puerto Vallarta on August 25. The storm began to turn more westward due to a strengthening high pressure system to its north and was upgraded to a hurricane on August 27 while {{convert|286|mi|km|abbr=on}} southwest of Cabo San Lucas. As the high to the north continued to strengthen, the hurricane turned west-southwest.<ref name="lowellprelim1"/>


Thunderstorm activity with the hurricane began to weaken and Lowell was downgraded back to tropical storm status on August 28. The tropical storm then turned to a north-northwestward with the storm passing over cooler waters. On August 31, the storm was downgraded to a tropical depression, with only minimal amounts of deep convection remaining within its circulation. Lowell dissipated as a tropical cyclone on September 1, though a low-level circulation of clouds could be seen on satellite imagery for the next few days. No damage or casualties was reported as a result of Lowell.<ref name="lowellprelim1"/><ref name="lowellprelim2">{{cite web|author=Mayfield, Max|year=1990|title=Hurricane Lowell Preliminary Report, Page 2|publisher=National Hurricane Center|access-date=January 3, 2011|url=http://www.nhc.noaa.gov/archive/storm_wallets/epacific/ep1990/lowell/prenhc/prelim02.gif}}</ref>
Thunderstorm activity with the hurricane began to weaken and Lowell was downgraded back to tropical storm status on August 28. The tropical storm then turned to a north-northwestward with the storm passing over cooler waters. On August 31, the storm was downgraded to a tropical depression, with only minimal amounts of deep convection remaining within its circulation. Lowell dissipated as a tropical cyclone on September 1, though a low-level circulation of clouds could be seen on satellite imagery for the next few days. No damage or casualties was reported as a result of Lowell.<ref name="lowellprelim1"/><ref name="lowellprelim2">{{cite web|author=Mayfield, Max|year=1990|title=Hurricane Lowell Preliminary Report, Page 2|publisher=National Hurricane Center|access-date=January 3, 2011|url=http://www.nhc.noaa.gov/archive/storm_wallets/epacific/ep1990/lowell/prenhc/prelim02.gif}}</ref>
Line 383: Line 384:
=== Hurricane Marie ===
=== Hurricane Marie ===
{{Infobox Hurricane Small
{{Infobox Hurricane Small
|Basin=EPac
| Basin = EPac
|Image=Marie 1990-09-11 0130Z.png
| Image = Marie 1990-09-11 0130Z.png
|Track=Marie 1990 track.png
| Track = Marie 1990 track.png
|Formed=September 7
| Formed = September 7
|Dissipated=September 21
| Dissipated = September 21
|1-min winds=120
| 1-min winds = 120
|Pressure=944
| Pressure = 944
}}
}}
A tropical wave moved off the northwestern coast of Africa on August 16. The wave moved west through the Atlantic Ocean and Caribbean Sea without significant development.<ref name="marieprelim1">{{cite web|author=Gerrish, Hal|year=1990|title=Hurricane Marie Preliminary Report, Page 1|publisher=National Hurricane Center|access-date=January 3, 2011|url=http://www.nhc.noaa.gov/archive/storm_wallets/epacific/ep1990/marie/prenhc/prelim01.gif}}</ref> The wave moved across Central America and into the northeastern Pacific Ocean, on August 29. Isolated convection with the system increased while south of the Gulf of Tehuantepec as the system moved northwest parallel to the southwest coast of Mexico. Once convective activity increased, the system was upgraded to Tropical Depression Sixteen-E on September 7 while centered 659&nbsp;mi (1,060&nbsp;km) southwest of Clarion Island.<ref name="marieprelim1"/>
A tropical wave moved off the northwestern coast of Africa on August 16. The wave moved west through the Atlantic Ocean and Caribbean Sea without significant development.<ref name="marieprelim1">{{cite web|author=Gerrish, Hal|year=1990|title=Hurricane Marie Preliminary Report, Page 1|publisher=National Hurricane Center|access-date=January 3, 2011|url=http://www.nhc.noaa.gov/archive/storm_wallets/epacific/ep1990/marie/prenhc/prelim01.gif}}</ref> The wave moved across Central America and into the northeastern Pacific Ocean, on August 29. Isolated convection with the system increased while south of the Gulf of Tehuantepec as the system moved northwest parallel to the southwest coast of Mexico. Once convective activity increased, the system was upgraded to Tropical Depression Sixteen-E on September 7 while centered {{convert|659|mi|km|abbr=on}} southwest of Clarion Island.<ref name="marieprelim1"/>


A weaker than normal high pressure system controlled the movement of the depression, and the system moved slowly to the west through its duration. The depression strengthened into Tropical Storm Marie on September 8, and into a hurricane on September 9, while {{convert|522|mi|km|abbr=on}} south-southwest of Clarion Island. Marie reached its peak intensity of {{convert|140|mph|km/h|abbr=on}} on September 11.<ref name="marieprelim1"/> The hurricane crossed into the central North Pacific on September 14 as a hurricane with maximum sustained winds of {{convert|110|mph|km/h|abbr=on}}. The hurricane weakened thereafter and on September 17 Marie regained tropical storm status. The system weakened into a tropical depression on September 19 and dissipated as a tropical cyclone on September 21 near the Hawaiian coast. No casualties or damages were caused by Marie.<ref name="mariecp">{{cite web|year=1990|title=September 14–21, 1990 (Hurricane Marie)|publisher=Central Pacific Hurricane Center|access-date=January 3, 2011|url=http://www.prh.noaa.gov/cphc/summaries/1990.php}}</ref>
A weaker than normal high pressure system controlled the movement of the depression, and the system moved slowly to the west through its duration. The depression strengthened into Tropical Storm Marie on September 8, and into a hurricane on September 9, while {{convert|522|mi|km|abbr=on}} south-southwest of Clarion Island. Marie reached its peak intensity of {{convert|140|mph|km/h|abbr=on}} on September 11.<ref name="marieprelim1"/> The hurricane crossed into the central North Pacific on September 14 as a hurricane with maximum sustained winds of {{convert|110|mph|km/h|abbr=on}}. The hurricane weakened thereafter and on September 17 Marie regained tropical storm status. The system weakened into a tropical depression on September 19 and dissipated as a tropical cyclone on September 21 near the Hawaiian coast. No casualties or damages were caused by Marie.<ref name="CPHC 90"/>
{{clear}}
{{clear}}


=== Hurricane Norbert ===
=== Hurricane Norbert ===
{{Infobox Hurricane Small
{{Infobox Hurricane Small
|Basin=EPac
| Basin = EPac
|Image=Norbert 1990-09-14 1830Z.png
| Image = Norbert 1990-09-14 1830Z.png
|Track=Norbert 1990 track.png
| Track = Norbert 1990 track.png
|Formed=September 10
| Formed = September 10
|Dissipated=September 19
| Dissipated = September 19
|1-min winds=70
| 1-min winds = 70
|Pressure=983
| Pressure = 983
}}
}}
A tropical wave moved off the coast of Africa and across the Atlantic Ocean and Caribbean Sea without significant development. The wave entered the northeastern Pacific Ocean and began to show signs of organized thunderstorm development. Tropical Depression Seventeen-E formed on September 10 while centered {{convert|758|mi|km|abbr=on}} south-southwest of Cabo San Lucas, Mexico. The depression became better organized and strengthened into Tropical Storm Norbert later in the day.<ref name="norbertprelim1">{{cite web|author=Avila, Lixion|year=1990|title=Hurricane Norbert Preliminary Report, Page 1|publisher=National Hurricane Center|access-date=January 3, 2011|url=http://www.nhc.noaa.gov/archive/storm_wallets/epacific/ep1990/norbert/prenhc/prelim01.gif}}</ref>
A tropical wave moved off the coast of Africa and across the Atlantic Ocean and Caribbean Sea without significant development. The wave entered the northeastern Pacific Ocean and began to show signs of organized thunderstorm development. Tropical Depression Seventeen-E formed on September 10 while centered {{convert|758|mi|km|abbr=on}} south-southwest of Cabo San Lucas, Mexico. The depression became better organized and strengthened into Tropical Storm Norbert later in the day.<ref name="norbertprelim1">{{cite web|author=Avila, Lixion|year=1990|title=Hurricane Norbert Preliminary Report, Page 1|publisher=National Hurricane Center|access-date=January 3, 2011|url=http://www.nhc.noaa.gov/archive/storm_wallets/epacific/ep1990/norbert/prenhc/prelim01.gif}}</ref>
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=== Tropical Depression Eighteen-E ===
=== Tropical Depression Eighteen-E ===
{{Infobox Hurricane Small
{{Infobox Hurricane Small
|Basin=EPac
| Basin = EPac
|Image=Eighteen-E 1990.JPG
| Image = Eighteen-E 1990.JPG
|Track=Temporary cyclone north.svg
| Track = 18E 1990 track.png
|Formed=September 9
| Formed = September 9
|Dissipated=September 12
| Dissipated = September 12
|1-min winds=30
| 1-min winds = 30
|Pressure=1000
| Pressure = 1000
}}
}}
On September 12, satellite images indicated that the eighteenth tropical depression of the season formed southwest of Cabo San Lucas. Located in close proximity to Tropical Storm Norbert, the depression would soon enter a region of colder sea surface temperatures, and the National Hurricane Center noted that only very little intensification was possible.<ref name="TD18-Edisc1">{{cite web|author=Avila, Lixion|date=September 12, 1990|title=Tropical Cyclone Discussion: Tropical Depression Eighteen-E (#1)|publisher=National Hurricane Center|access-date=January 3, 2011|url=http://www.nhc.noaa.gov/archive/storm_wallets/epacific/ep1990/td18e/tropdisc/tcd1203z.gif}}</ref> As predicted, Norbert hindered further intensification of Tropical Depression Eighteen-E. The National Hurricane Center noted six hours later that the depression would likely be absorbed into Norbert.<ref name="TD18-Edisc2">{{cite web|author=Mayfield, Max|date=September 12, 1990|title=Tropical Cyclone Discussion: Tropical Depression Eighteen-E (#2)|publisher=National Hurricane Center|access-date=January 3, 2011|url=http://www.nhc.noaa.gov/archive/storm_wallets/epacific/ep1990/td18e/tropdisc/tcd1209z.gif}}</ref> The National Hurricane Center later believed that Tropical Depression Eighteen-E was "dominating" the interaction between the two systems, and was forecast to absorb Norbert.<ref name="TD18-Edisc3">{{cite web|author1=Pasch, Richard |author2=Lawrence, Miles|date=September 12, 1990|title=Tropical Cyclone Discussion: Tropical Depression Eighteen-E (#3)|publisher=National Hurricane Center|access-date=January 3, 2011|url=http://www.nhc.noaa.gov/archive/storm_wallets/epacific/ep1990/td18e/tropdisc/tcd1215z.gif}}</ref> Unlike the latter prediction, Norbert absorbed Tropical Depression Eighteen-E later that day.<ref name="TD18-Edisc4">{{cite web|author1=Pasch, Richard |author2=Lawrence, Miles|date=September 12, 1990|title=Tropical Cyclone Discussion: Tropical Depression Eighteen-E (#4)|publisher=National Hurricane Center|access-date=January 3, 2011|url=http://www.nhc.noaa.gov/archive/storm_wallets/epacific/ep1990/td18e/tropdisc/tcd1221z.gif}}</ref>
On September 12, satellite images indicated that the eighteenth tropical depression of the season formed southwest of Cabo San Lucas. Located in close proximity to Tropical Storm Norbert, the depression would soon enter a region of colder sea surface temperatures, and the National Hurricane Center noted that only very little intensification was possible.<ref name="TD18-Edisc1">{{cite web|author=Avila, Lixion|date=September 12, 1990|title=Tropical Cyclone Discussion: Tropical Depression Eighteen-E (#1)|publisher=National Hurricane Center|access-date=January 3, 2011|url=http://www.nhc.noaa.gov/archive/storm_wallets/epacific/ep1990/td18e/tropdisc/tcd1203z.gif}}</ref> As predicted, Norbert hindered further intensification of Tropical Depression Eighteen-E. The National Hurricane Center noted six hours later that the depression would likely be absorbed into Norbert.<ref name="TD18-Edisc2">{{cite web|author=Mayfield, Max|date=September 12, 1990|title=Tropical Cyclone Discussion: Tropical Depression Eighteen-E (#2)|publisher=National Hurricane Center|access-date=January 3, 2011|url=http://www.nhc.noaa.gov/archive/storm_wallets/epacific/ep1990/td18e/tropdisc/tcd1209z.gif}}</ref> The National Hurricane Center later believed that Tropical Depression Eighteen-E was "dominating" the interaction between the two systems, and was forecast to absorb Norbert.<ref name="TD18-Edisc3">{{cite web|author1=Pasch, Richard |author2=Lawrence, Miles|date=September 12, 1990|title=Tropical Cyclone Discussion: Tropical Depression Eighteen-E (#3)|publisher=National Hurricane Center|access-date=January 3, 2011|url=http://www.nhc.noaa.gov/archive/storm_wallets/epacific/ep1990/td18e/tropdisc/tcd1215z.gif}}</ref> Unlike the latter prediction, Norbert absorbed Tropical Depression Eighteen-E later that day.<ref name="TD18-Edisc4">{{cite web|author1=Pasch, Richard |author2=Lawrence, Miles|date=September 12, 1990|title=Tropical Cyclone Discussion: Tropical Depression Eighteen-E (#4)|publisher=National Hurricane Center|access-date=January 3, 2011|url=http://www.nhc.noaa.gov/archive/storm_wallets/epacific/ep1990/td18e/tropdisc/tcd1221z.gif}}</ref>
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=== Hurricane Odile ===
=== Hurricane Odile ===
{{Infobox Hurricane Small
{{Infobox Hurricane Small
|Basin=EPac
| Basin = EPac
|Image=File:Odile 1990-09-26 1530Z.png
| Image = File:Odile 1990-09-26 1530Z.png
|Track=Odile 1990 track.png
| Track = Odile 1990 track.png
|Formed=September 23
| Formed = September 23
|Dissipated=October 2
| Dissipated = October 2
|1-min winds=125
| 1-min winds = 125
|Pressure=935
| Pressure = 935
}}
}}
A tropical wave move off the coast of Africa on September 5, and crossed the Atlantic waters, the Caribbean Sea and eventually into the Pacific Ocean as a weak system. An area of convection entered into the northeastern Pacific Ocean a few hundred miles south of Acapulco, Mexico. On September 23, Tropical Depression Nineteen-E formed from this convection, while {{convert|746|mi|km|abbr=on}} south-southeast from the southern tip of Baja California. The depression moved on a west-northwestward track, rounding the southwest side of a strong high pressure system. The depression continued to strengthen and was upgraded to Tropical Storm Odile on September 24 and into a hurricane on September 25. Its intensity peaked with maximum sustained winds of {{convert|145|mph|km/h|abbr=on}} on September 26.<ref name="odileprelim1">{{cite web|author=Lawrence, Miles|year=1990|title=Hurricane Odile Preliminary Report, Page 1|publisher=National Hurricane Center|access-date=January 3, 2011|url=http://www.nhc.noaa.gov/archive/storm_wallets/epacific/ep1990/odile/prenhc/prelim01.gif}}</ref>
A tropical wave move off the coast of Africa on September 5, and crossed the Atlantic waters, the Caribbean Sea and eventually into the Pacific Ocean as a weak system. An area of convection entered into the northeastern Pacific Ocean a few hundred miles south of Acapulco, Mexico. On September 23, Tropical Depression Nineteen-E formed from this convection, while {{convert|746|mi|km|abbr=on}} south-southeast from the southern tip of Baja California. The depression moved on a west-northwestward track, rounding the southwest side of a strong high pressure system. The depression continued to strengthen and was upgraded to Tropical Storm Odile on September 24 and into a hurricane on September 25. Its intensity peaked with maximum sustained winds of {{convert|145|mph|km/h|abbr=on}} on September 26.<ref name="odileprelim1">{{cite web|author=Lawrence, Miles|year=1990|title=Hurricane Odile Preliminary Report, Page 1|publisher=National Hurricane Center|access-date=January 3, 2011|url=http://www.nhc.noaa.gov/archive/storm_wallets/epacific/ep1990/odile/prenhc/prelim01.gif}}</ref>
Line 442: Line 443:
{{Main|Tropical Storm Rachel (1990)}}
{{Main|Tropical Storm Rachel (1990)}}
{{Infobox Hurricane Small
{{Infobox Hurricane Small
|Basin=EPac
| Basin = EPac
|Image=Rachel90bajalandfall.JPG
| Image = Rachel90bajalandfall.JPG
|Track=Rachel 1990 track.png
| Track = Rachel 1990 track.png
|Formed=September 27
| Formed = September 27
|Dissipated=October 3
| Dissipated = October 3
|1-min winds=55
| 1-min winds = 55
|Pressure=994
| Pressure = 994
}}
}}
In mid-September, a weak tropical wave moved off the coast of Northwest Africa. It moved westward and entered the eastern Pacific Ocean early on September 23. Cloudiness became concentrated with the system south of the [[Gulf of Tehuantepec]]. On September 27, the organized thunderstorm area was upgraded to Tropical Depression Twenty One-E while {{convert|230|mi|km|abbr=on}} south of [[Acapulco]]. The depression developed slowly, and became a tropical storm on September 30. As Rachel briefly moved northward, before re-curving and accelerating towards the Mexican coast. The storm passed over the southern portion of [[Baja California Sur]] on October 2. Rachel made its final landfall midway between [[Los Mochis]] and [[Culiacán]], and became the only system to make landfall from the eastern north Pacific Ocean in 1990.<ref name="rachelprelim1">{{cite web|author=Mayfield, Max|year=1990|title=Tropical Storm Rachel Preliminary Report, Page 1|publisher=National Hurricane Center|access-date=January 3, 2011|url=http://www.nhc.noaa.gov/archive/storm_wallets/epacific/ep1990/rachel/prenhc/prelim01.gif }}</ref><ref name="rachelprelim4">{{cite web|author=Mayfield, Max|year=1990|title=Tropical Storm Rachel Preliminary Report, Page 4|publisher=National Hurricane Center|access-date=January 3, 2011|url=http://www.nhc.noaa.gov/archive/storm_wallets/epacific/ep1990/rachel/prenhc/prelim04.gif}}</ref> Rachel decayed rapidly over land, and the final public advisory on Rachel was issued early on October 3.<ref name="oct22357ztcd">{{cite web|author=Mayfield, Max|date=October 2, 1990|title=Tropical Depression Rachel Advisory Number 11A|publisher=National Hurricane Center|access-date=January 3, 2011|url=http://www.nhc.noaa.gov/archive/storm_wallets/epacific/ep1990/rachel/public/tcp0300z.gif}}</ref> its remnants continued accelerating over Texas until they lost their identity.
In mid-September, a weak tropical wave moved off the coast of Northwest Africa. It moved westward and entered the eastern Pacific Ocean early on September 23. Cloudiness became concentrated with the system south of the [[Gulf of Tehuantepec]]. On September 27, the organized thunderstorm area was upgraded to Tropical Depression Twenty One-E while {{convert|230|mi|km|abbr=on}} south of [[Acapulco]]. The depression developed slowly, and became a tropical storm on September 30. As Rachel briefly moved northward, before re-curving and accelerating towards the Mexican coast. The storm passed over the southern portion of [[Baja California Sur]] on October 2. Rachel made its final landfall midway between [[Los Mochis]] and [[Culiacán]], and became the only system to make landfall from the eastern north Pacific Ocean in 1990.<ref name="rachelprelim1">{{cite web|author=Mayfield, Max|year=1990|title=Tropical Storm Rachel Preliminary Report, Page 1|publisher=National Hurricane Center|access-date=January 3, 2011|url=http://www.nhc.noaa.gov/archive/storm_wallets/epacific/ep1990/rachel/prenhc/prelim01.gif }}</ref><ref name="rachelprelim4">{{cite web|author=Mayfield, Max|year=1990|title=Tropical Storm Rachel Preliminary Report, Page 4|publisher=National Hurricane Center|access-date=January 3, 2011|url=http://www.nhc.noaa.gov/archive/storm_wallets/epacific/ep1990/rachel/prenhc/prelim04.gif}}</ref> Rachel decayed rapidly over land, and the final public advisory on Rachel was issued early on October 3.<ref name="oct22357ztcd">{{cite web|author=Mayfield, Max|date=October 2, 1990|title=Tropical Depression Rachel Advisory Number 11A|publisher=National Hurricane Center|access-date=January 3, 2011|url=http://www.nhc.noaa.gov/archive/storm_wallets/epacific/ep1990/rachel/public/tcp0300z.gif}}</ref> its remnants continued accelerating over Texas until they lost their identity.
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=== Hurricane Polo ===
=== Hurricane Polo ===
{{Infobox Hurricane Small
{{Infobox Hurricane Small
|Basin=EPac
| Basin = EPac
|Image=Polo 1990-09-30 1801Z.png
| Image = Polo 1990-09-30 1801Z.png
|Track=Polo 1990 track.png
| Track = Polo 1990 track.png
|Formed=September 28
| Formed = September 28
|Dissipated=October 1
| Dissipated = October 1
|1-min winds=65
| 1-min winds = 65
|Pressure=987
| Pressure = 987
}}
}}
Polo originated from a tropical wave that moved off the African coast on September 2 which spawned [[1990 Atlantic hurricane season#Hurricane Isidore|Hurricane Isidore]] in the [[1990 Atlantic hurricane season|Atlantic basin]]. On September 14, the system increased in convection as it was moving to the west and approaching Central America. The southern extent of the wave crossed into the Pacific Ocean on September 18.<ref name="poloprelim1">{{cite web|author=Case, Robert|year=1990|title=Hurricane Polo Preliminary Report, Page 1|publisher=National Hurricane Center|access-date=January 3, 2011|url=http://www.nhc.noaa.gov/archive/storm_wallets/epacific/ep1990/polo/prenhc/prelim01.gif}}</ref>
Polo originated from a tropical wave that moved off the African coast on September 2 which spawned [[1990 Atlantic hurricane season#Hurricane Isidore|Hurricane Isidore]] in the [[1990 Atlantic hurricane season|Atlantic basin]]. On September 14, the system increased in convection as it was moving to the west and approaching Central America. The southern extent of the wave crossed into the Pacific Ocean on September 18.<ref name="poloprelim1">{{cite web|author=Case, Robert|year=1990|title=Hurricane Polo Preliminary Report, Page 1|publisher=National Hurricane Center|access-date=January 3, 2011|url=http://www.nhc.noaa.gov/archive/storm_wallets/epacific/ep1990/polo/prenhc/prelim01.gif}}</ref>


The wave continued westward and related thunderstorm activity increased during the following week. The convective system organized into Tropical Depression Twenty-E on September 28 nearly midway between Mexico and Hawaii. Initially, the depression drifted toward the northwest due to a large upper-level trough located to its west. Polo strengthened rapidly into a hurricane early on September 30, with its winds peaking at {{convert|75|mph|km/h|abbr=on}}. Since the storm was very small, vertical wind shear caused significant weakening thereafter. On October 1, Polo regained tropical storm strength as it was crossing into the north Central Pacific basin. It dissipated as a tropical cyclone later that day.<ref name="poloprelim1"/> There were no casualties or damages caused by Polo.<ref name="poloprelim1"/>
The wave continued westward and related thunderstorm activity increased during the following week. The convective system organized into Tropical Depression Twenty-E on September 28 nearly midway between Mexico and Hawaii. Initially, the depression drifted toward the northwest due to a large upper-level trough located to its west. Polo strengthened rapidly into a hurricane early on September 30, with its winds peaking at {{convert|75|mph|km/h|abbr=on}}. Since the storm was very small, vertical wind shear caused significant weakening thereafter.<ref name="poloprelim1"/> On October 1, Polo crossed into the Central Pacific basin at tropical storm strength. The storm continued to weaken, becoming a tropical depression and then dissipating southwest of Hawaii later in the day.<ref name="CPHC 90"/> There were no casualties or damages caused by Polo.
{{clear}}
{{clear}}


=== Tropical Storm Simon ===
=== Tropical Storm Simon ===
{{Infobox Hurricane Small
{{Infobox Hurricane Small
|Basin=EPac
| Basin = EPac
|Image=Tropical Storm Simon 1990 October 11.JPG
| Image = Tropical Storm Simon 1990 October 11.JPG
|Track=Simon 1990 track.png
| Track = Simon 1990 track.png
|Formed=October 9
| Formed = October 9
|Dissipated=October 14
| Dissipated = October 14
|1-min winds=60
| 1-min winds = 60
|Pressure=990
| Pressure = 990
}}
}}
A weakly defined tropical wave moved off the northwest coast of Africa on September 20, and crossed the northern portion of the tropical Atlantic and northern South America without significant organization. The wave moved into the northeastern Pacific waters, off the coast of [[Colombia]] on September 30. As the wave passed over southern Central America, rainbands and cloudiness increased with the system between October 1 and October 3, before the system merged with the ITCZ from October 4 to October 6. Signs of convective organization reappeared on October 8, and by October 9, the system was upgraded to Tropical Depression Twenty Two-E {{convert|578|mi|km|abbr=on}} south of Cabo San Lucas, Mexico.<ref name="simonprelim1">{{cite web|author=Gerrish, Hal|year=1990|title=Hurricane Simon Preliminary Report, Page 1|publisher=National Hurricane Center|access-date=January 3, 2011|url=http://www.nhc.noaa.gov/archive/storm_wallets/epacific/ep1990/simon/prenhc/prelim01.gif}}</ref>
A weakly defined tropical wave moved off the northwest coast of Africa on September 20, and crossed the northern portion of the tropical Atlantic and northern South America without significant organization. The wave moved into the northeastern Pacific waters, off the coast of [[Colombia]] on September 30. As the wave passed over southern Central America, rainbands and cloudiness increased with the system between October 1 and October 3, before the system merged with the ITCZ from October 4 to October 6. Signs of convective organization reappeared on October 8, and by October 9, the system was upgraded to Tropical Depression Twenty Two-E {{convert|578|mi|km|abbr=on}} south of Cabo San Lucas, Mexico.<ref name="simonprelim1">{{cite web|author=Gerrish, Hal|year=1990|title=Hurricane Simon Preliminary Report, Page 1|publisher=National Hurricane Center|access-date=January 3, 2011|url=http://www.nhc.noaa.gov/archive/storm_wallets/epacific/ep1990/simon/prenhc/prelim01.gif}}</ref>
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=== Hurricane Trudy ===
=== Hurricane Trudy ===
{{Infobox Hurricane Small
{{Infobox Hurricane Small
|Basin=EPac
| Basin = EPac
|Image=File:Trudy 1990-10-20 1400Z.png
| Image = File:Trudy 1990-10-20 1400Z.png
|Track=Trudy 1990 track.png
| Track = Trudy 1990 track.png
|Formed=October 16
| Formed = October 16
|Dissipated=November 1
| Dissipated = November 1
|1-min winds=135
| 1-min winds = 135
|Pressure=924
| Pressure = 924
}}
}}
The tropical wave that would become future Hurricane Trudy became identifiable on satellite imagery as early as September 30, emerging near the African coast off Cape Verde. However, the wave did not show any signs of development until October 16, when the wave developed into a tropical depression several hundred kilometers south of Acapulco. The tropical depression intensified significantly. The ship ''Maple Ace'' reported gale-force winds about {{convert|140|km|mi|abbr=on|round=5}} from the center at 1800 UTC on October 18. In less than 36 hours, at 1200 UTC on October 20<!-- In the source provided, it said "September" instead of "October", and should be "October". Sorry for the inconvenience for confused readers -->, Trudy became a powerful hurricane with Category 4 equivalent maximum winds of {{convert|135|kn|mph km/h|abbr=on|round=5|sortable=on|order=out}} and a minimum pressure of {{convert|925|mbar|inHg|abbr=on}} according to satellite estimates. Trudy was at least as intense as [[1987 Pacific hurricane season#Hurricane Max|Hurricane Max]] three years earlier and Hurricane Hernan earlier in the year. Estimates state that Trudy may have been the strongest eastern Pacific hurricane since wind estimates have been available from satellite images.<ref name="Eastern North Pacific Season of 1990"/>
The tropical wave that would become future Hurricane Trudy became identifiable on satellite imagery as early as September 30, emerging near the African coast off Cape Verde. However, the wave did not show any signs of development until October 16, when the wave developed into a tropical depression several hundred kilometers south of Acapulco. The tropical depression intensified significantly. The ship ''Maple Ace'' reported gale-force winds about {{convert|140|km|mi|abbr=on|round=5}} from the center at 1800 UTC on October 18. In less than 36 hours, at 1200 UTC on October 20<!-- In the source provided, it said "September" instead of "October", and should be "October". Sorry for the inconvenience for confused readers -->, Trudy became a powerful hurricane with Category 4 equivalent maximum winds of {{convert|135|kn|mph km/h|abbr=on|round=5|sortable=on|order=out}} and a minimum pressure of {{convert|925|mbar|inHg|abbr=on}} according to satellite estimates. Trudy was at least as intense as [[1987 Pacific hurricane season#Hurricane Max|Hurricane Max]] three years earlier and Hurricane Hernan earlier in the year. Estimates state that Trudy may have been the strongest eastern Pacific hurricane since wind estimates have been available from satellite images.<ref name="Eastern North Pacific Season of 1990"/>
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=== Hurricane Vance ===
=== Hurricane Vance ===
{{Infobox Hurricane Small
{{Infobox Hurricane Small
|Basin=EPac
| Basin = EPac
|Image=Vance 1990-10-25 2030Z.png
| Image = Vance 1990-10-25 2030Z.png
|Track=Vance 1990 track.png
| Track = Vance 1990 track.png
|Formed=October 21
| Formed = October 21
|Dissipated=October 31
| Dissipated = October 31
|1-min winds=85
| 1-min winds = 85
|Pressure=975
| Pressure = 975
}}
}}
An area of disturbed weather, possibly related to a tropical wave, organized into Tropical Depression Twenty Four-E on October 21. It strengthened into Tropical Storm Vance early on October 23 and then into a hurricane two days later. Vance moved parallel to the west coast of Mexico and approached the southern tip of the Baja California Peninsula. Before it could strike land, a high-pressure area blocked Vance's path and forced the storm to transcribe a small clockwise loop over a two-day period. During the loop, Vance encountered wind shear and cool waters stirred up by Trudy as well as earlier in its duration. Vance weakened to a tropical storm on October 27 and a depression on October 30. The cyclone dissipated late on October 31.<ref>{{cite web|url=http://www.nhc.noaa.gov/archive/storm_wallets/epacific/ep1990/vance/prenhc/prelim01.gif|title=Hurricane Vance Preliminary Report, Page 1|author=Lawrence, Miles|publisher=National Hurricane Center|year=1991|access-date=January 2, 2011}}</ref>
An area of disturbed weather, possibly related to a tropical wave, organized into Tropical Depression Twenty Four-E on October 21. It strengthened into Tropical Storm Vance early on October 23 and then into a hurricane two days later. Vance moved parallel to the west coast of Mexico and approached the southern tip of the Baja California Peninsula. Before it could strike land, a high-pressure area blocked Vance's path and forced the storm to transcribe a small clockwise loop over a two-day period. During the loop, Vance encountered wind shear and cool waters stirred up by Trudy as well as earlier in its duration. Vance weakened to a tropical storm on October 27 and a depression on October 30. The cyclone dissipated late on October 31.<ref>{{cite web|url=http://www.nhc.noaa.gov/archive/storm_wallets/epacific/ep1990/vance/prenhc/prelim01.gif|title=Hurricane Vance Preliminary Report, Page 1|author=Lawrence, Miles|publisher=National Hurricane Center|year=1991|access-date=January 2, 2011}}</ref>
Line 514: Line 515:


== Storm names ==
== Storm names ==
{{Main|Tropical cyclone naming#Eastern and Central Pacific Ocean}}
The following names were used for named storms that formed in the eastern Pacific in 1990. Names that were not assigned are marked in <span style="color:gray;">gray</span>. Since no names were [[Tropical cyclone naming#Retirement|retired]], no new names were replaced for the [[1996 Pacific hurricane season|1996 season]].<ref>{{cite web|archive-url=https://www.webcitation.org/6n8x2jHtd?url=http://www.nhc.noaa.gov/aboutnames.shtml |url=http://www.nhc.noaa.gov/aboutnames.shtml |title=Tropical Cyclone Names 2016-2021 |publisher=National Oceanic and Atmospheric Administration |work=National Hurricane Center |archive-date=December 30, 2016 |url-status=dead }}</ref> This same list was used in the [[1984 Pacific hurricane season|1984 season]]. ''Wallis'' would trade years with ''Winnie'' in future seasons.
The following list of names was used for named storms that formed in the North Pacific Ocean east of [[140th meridian west|140°W]] in 1990.<ref name="NHOP 90">{{cite report|url=https://www.aoml.noaa.gov/general/lib/lib1/nhclib/Publications/NatHurricaneOpsPlans/1990.pdf|pages=((3{{hyphen}}6{{ndash}}7))|publisher=[[NOAA]] Office of the Federal Coordinator for Meteorological Services and Supporting Research|location=Washington, D.C.|title=National Hurricane Operations Plan|date=May 1990|access-date=January 15, 2024}}</ref> This is essentially the same list used for the [[1984 Pacific hurricane season|1984 season]], though the rotating lists went only to the "W" name at the time.<ref name="NHOP 84">{{cite report|url=https://www.aoml.noaa.gov/general/lib/lib1/nhclib/Publications/NatHurricaneOpsPlans/HOPs-1984.pdf|page=3{{hyphen}}10|publisher=[[NOAA]] Office of the Federal Coordinator for Meteorological Services and Supporting Research|location=Washington, D.C.|title=National Hurricane Operations Plan|date=May 1984|access-date=January 15, 2024}}</ref> It would be used next, with one modification, for the [[1996 Pacific hurricane season|1996 season]], as ''Wallis'' was interchanged with ''Winnie''.<ref name="NHOP 96">{{cite report|url=https://www.aoml.noaa.gov/general/lib/lib1/nhclib/Publications/NatHurricaneOpsPlans/HOPs-1996.pdf|pages=((3{{hyphen}}8{{ndash}}9))|publisher=[[NOAA]] Office of the Federal Coordinator for Meteorological Services and Supporting Research|location=Washington, D.C.|title=National Hurricane Operations Plan|date=May 1996|access-date=January 15, 2024}}</ref> No [[List of retired Pacific hurricane names|names were retired]] from the list following the 1990 season.<ref>{{cite web|title=Tropical Cyclone Naming History and Retired Names|url=https://www.nhc.noaa.gov/aboutnames_history.shtml|publisher=National Hurricane Center|location=Miami, Florida|access-date=January 15, 2024}}</ref>


{| width="90%"
{| width="90%"
Line 531: Line 533:
* Kenna
* Kenna
* Lowell
* Lowell
* Marie
* Marie{{thin space}}*
* Norbert
* Norbert
* Odile
* Odile
* Polo
* Polo{{thin space}}*
|
|
* [[Tropical Storm Rachel (1990)|Rachel]]
* [[Tropical Storm Rachel (1990)|Rachel]]
Line 540: Line 542:
* Trudy
* Trudy
* Vance
* Vance
* {{tcname unused|Wallis}}
* <div style="color: #888;">Wallis (unused)</div>
* {{tcname unused|Xavier}}
* <div style="color: #888;">Xavier (unused)</div>
* {{tcname unused|Yolanda}}
* <div style="color: #888;">Yolanda (unused)</div>
* {{tcname unused|Zeke}}
* <div style="color: #888;">Zeke (unused)</div>
|}
|}


{| width="90%"
=== Central Pacific ===
|
* Additionally, [[Hurricane Diana|Diana]] entered the eastern Pacific basin during the season from the Atlantic basin. Its crossover between basins as an intact tropical cyclone was detected in a post-storm analysis of the system. Thus the National Hurricane Center did not re-classify it as an eastern Pacific system.<ref name="Diana1"/><ref name=Diana1990/>
|}


For storms that form in the [[Central Pacific Hurricane Center]]'s area of responsibility, encompassing the area between [[140th meridian west|140 degrees west]] and the [[International Date Line]], all names are used in a series of [[List of tropical cyclone names#Central Pacific|four rotating lists]].<ref>{{cite web|archive-url=https://www.webcitation.org/6n8wTrpLC?url=http://www.prh.noaa.gov/cphc/pages/names.php |url=http://www.prh.noaa.gov/cphc/pages/names.php |title=Pacific Tropical Cyclone Names 2016-2021 |publisher=National Oceanic and Atmospheric Administration |work=Central Pacific Hurricane Center |date=May 12, 2016 |archive-date=December 30, 2016 |format=PHP |url-status=dead }}</ref> The next four names slated for use are shown below.
For storms that form in the North Pacific from 140°W to the [[International Date Line]], the names come from a series of four rotating lists. Names are used one after the other without regard to year, and when the bottom of one list is reached, the next named storm receives the name at the top of the next list.<ref name="NHOP 90"/><ref>{{cite web|archive-url=https://web.archive.org/web/20170112131437/http://www.nhc.noaa.gov/aboutnames.shtml |url=http://www.nhc.noaa.gov/aboutnames.shtml |title=Tropical Cyclone Names 2016-2021 |publisher=National Oceanic and Atmospheric Administration |work=National Hurricane Center |archive-date=January 12, 2017 |url-status=dead }}</ref> One named storm, listed below, formed in the central North Pacific in 1990. Named storms in the table above that crossed into the area during the year are noted (*).<ref name="CPHC 90"/>


{| style="width:90%;"
{| style="width:50%;"
|
|
* Aka
* Aka
|
* {{tcname unused|Ekeka}}
|
* {{tcname unused|Hali}}
|
* {{tcname unused|Iniki}}
|}
|}


== Season effects ==
== Season effects ==
This is a table of all the storms that have formed in the 1990 Pacific hurricane season. It includes their duration, names, landfall(s), denoted in parentheses, damages, and death totals. Deaths in parentheses are additional and indirect (an example of an indirect death would be a traffic accident), but were still related to that storm. Damage and deaths include totals while the storm was extratropical, a wave, or a low, and all the damage figures are in 1990 USD.
This is a table of all of the tropical cyclones that formed in the 1990 Pacific hurricane season. It includes their name, duration (within the basin), peak classification and intensities, areas affected, damage, and death totals. Deaths in parentheses are additional and indirect (an example of an indirect death would be a traffic accident), but were still related to that storm. Damage and deaths include totals while the storm was extratropical, a wave, or a low, and all of the damage figures are in 1990 USD.


{{Saffir-Simpson small|align=center}}<div style="text-align: center;">
{{Saffir-Simpson small|align=center}}<div style="text-align: center;">
Line 588: Line 587:
{{TC stats cyclone3|cat=depression|name=Eighteen-E|dates=September 10 – 12|max-winds=35 (55)|min-press=1000|areas=None|damage=None|deaths=None}}
{{TC stats cyclone3|cat=depression|name=Eighteen-E|dates=September 10 – 12|max-winds=35 (55)|min-press=1000|areas=None|damage=None|deaths=None}}
{{TC stats cyclone3|cat=cat4|name=Odile|dates=September 23 – October 1|max-winds=145 (230)|min-press=935|areas=None|damage=None|deaths=None}}
{{TC stats cyclone3|cat=cat4|name=Odile|dates=September 23 – October 1|max-winds=145 (230)|min-press=935|areas=None|damage=None|deaths=None}}
{{TC stats cyclone3|cat=storm|name=[[Tropical Storm Rachel (1990)|Rachel]]|dates=September 27 – October 3|max-winds=65 (100)|min-press=994|areas=[[Baja California Peninsula]], [[Texas]]|damage=2.5|deaths=18}}
{{TC stats cyclone3|cat=storm|name=[[Tropical Storm Rachel (1990)|Rachel]]|dates=September 27 – October 3|max-winds=65 (100)|min-press=994|areas=[[Baja California Peninsula]], [[Texas]]|damage=2.5 million|deaths=18}}
{{TC stats cyclone3|cat=cat1|name=Polo|dates=September 28 – October 1|max-winds=75 (120)|min-press=987|areas=None|damage=None|deaths=None}}
{{TC stats cyclone3|cat=cat1|name=Polo|dates=September 28 – October 1|max-winds=75 (120)|min-press=987|areas=None|damage=None|deaths=None}}
{{TC stats cyclone3|cat=storm|name=Simon|dates=October 9 – 14|max-winds=70 (110)|min-press=990|areas=None|damage=None|deaths=None}}
{{TC stats cyclone3|cat=storm|name=Simon|dates=October 9 – 14|max-winds=70 (110)|min-press=990|areas=None|damage=None|deaths=None}}
{{TC stats cyclone3|cat=cat4|name=Trudy|dates=October 16 – November 1|max-winds=155 (250)|min-press=924|areas=None|damage=None|deaths=None}}
{{TC stats cyclone3|cat=cat4|name=Trudy|dates=October 16 – November 1|max-winds=155 (250)|min-press=924|areas=None|damage=None|deaths=None}}
{{TC stats cyclone3|cat=cat2|name=Vance|dates=October 21 – 31|max-winds=100 (155)|min-press=975|areas=Southwestern Mexico, Central America|damage=10|deaths=None}}
{{TC stats cyclone3|cat=cat2|name=Vance|dates=October 21 – 31|max-winds=100 (155)|min-press=975|areas=Southwestern Mexico, Central America|damage=10 million|deaths=None}}
{{TC stats table end3|num-cyclones=27|dates=May 12 – November 1|max-winds=155 (250)|min-press=924|tot-areas=|tot-damage=12.5|tot-deaths=19}}</div>
{{TC stats table end3|num-cyclones=27|dates=May 12 – November 1|max-winds=155 (250)|min-press=924|tot-areas=|tot-damage=12.5 million|tot-deaths=19}}</div>
{{clear}}
{{clear}}


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* Australian region cyclone season: [[1989–90 Australian region cyclone season|1989–90]], [[1990–91 Australian region cyclone season|1990–91]]
* Australian region cyclone season: [[1989–90 Australian region cyclone season|1989–90]], [[1990–91 Australian region cyclone season|1990–91]]
* South Pacific cyclone season: [[1989–90 South Pacific cyclone season|1989–90]], [[1990–91 South Pacific cyclone season|1990–91]]
* South Pacific cyclone season: [[1989–90 South Pacific cyclone season|1989–90]], [[1990–91 South Pacific cyclone season|1990–91]]

== Notes ==
{{reflist|group=nb}}


== References ==
== References ==
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{{1990 Pacific hurricane season buttons}}
{{1990 Pacific hurricane season buttons}}
{{TC Decades|Year=1990|basin=Pacific|type=hurricane}}
{{TC Decades|Year=1990|basin=Pacific|type=hurricane}}
{{Tropical cyclone season|1990}}


{{good article}}
{{good article}}

Latest revision as of 13:18, 16 December 2024

1990 Pacific hurricane season
Season summary map
Seasonal boundaries
First system formedMay 12, 1990
Last system dissipatedNovember 1, 1990
Strongest storm
NameTrudy
 • Maximum winds155 mph (250 km/h)
(1-minute sustained)
 • Lowest pressure924 mbar (hPa; 27.29 inHg)
Seasonal statistics
Total depressions27
Total storms21
Hurricanes16 (record high, tied with 1992, 2014 and 2015)
Major hurricanes
(Cat. 3+)
6
Total fatalities19 total
Total damage$12.5 million (1990 USD)
Related articles
Pacific hurricane seasons
1988, 1989, 1990, 1991, 1992

The 1990 Pacific hurricane season was a very active season which observed 21 named storms within the basin. The season also produced the fourth highest ACE index value on record. The season was officially started on May 15 in the eastern Pacific, and on June 1 in the central Pacific, and lasted until November 30. These dates conventionally delimit the period of each year when most tropical cyclones form in the northeastern Pacific Ocean. However, the formation of tropical cyclones is possible at any time of the year, as illustrated in 1990 by the formation of the season's first named storm, Hurricane Alma, on May 12. At the time, this was the earliest formation of a tropical storm on record in the eastern Pacific

Overall, the impact of this season was minimal. Tropical Storm Rachel made two landfalls in Mexico and brought rain to the United States. Hurricane Boris brought light showers to California.[1]

Seasonal summary

[edit]
Tropical Storm Rachel (1990)Hurricane DianaSaffir-Simpson scale
Most intense Pacific
hurricane seasons[2]
Rank Season ACE value
1 2018 318.1
2 1992 294.3
3 2015 290.2
4 1990 249.5
5 1978 207.7
6 1983 206.2
7 2014 202.4
8 1993 201.8
9 1984 193.7
10 1985 193.1

The 1990 eastern North Pacific hurricane season was active in terms of number of storms that attained at least tropical storm intensity and of Accumulated Cyclone Energy (ACE). All of the tropical cyclones of this year developed from westward-moving African tropical waves. The season established several tropical storm records for this basin and was marked by several strong hurricanes. There were 21 named tropical cyclones, seven below the record established by the 1992 Pacific hurricane season two years later, but four more than the long-term average. Sixteen of those named storms, twice the average and four more than the previous record, reached hurricane intensity. Only Cristina, Douglas, Aka, Rachel, and Simon did not reach hurricane strength. Six of those hurricanes reached Category 3 intensity or higher on the Saffir-Simpson Hurricane Scale. Hurricanes Hernan and Trudy were among the strongest ever observed in this area. Alma became the earliest named storm and hurricane in the satellite era in the eastern Pacific Ocean east of the 140th meridian west at the time; a record subsequently eclipsed by Adrian in 2017.[3][4] The eastern Pacific produced four tropical depressions that did not reach tropical storm status.[5]

With the exception of Marie and Polo, these systems developed between and 15°N, east of the longitude of Baja California Peninsula in the climatologically favored area for tropical cyclogenesis in the basin. After their development, most of the tropical cyclones moved on a west to northwest track and dissipated over cool waters without affecting land. Rachel was the only system to make landfall. In addition, one tropical storm formed in the Central Pacific and eventually crossed the International Dateline before dissipating.[1]

The Accumulated Cyclone Energy (ACE) index for the 1990 Pacific hurricane season (Eastern Pacific and Central Pacific combined) as calculated by Colorado State University using data from the National Hurricane Center was 249.5 units, the fourth highest ACE on record for a Pacific hurricane season.[nb 1][6]

Systems

[edit]

Hurricane Alma

[edit]
Category 1 hurricane (SSHWS)
 
DurationMay 12 – May 18
Peak intensity85 mph (140 km/h) (1-min);
979 mbar (hPa)

A tropical wave emerged from Africa on April 29. It then moved across the Atlantic, crossed northern South America, and entered the Pacific Ocean on May 9. Convection started to increase with the wave just to the south of Panama. The wave moved westward and continued to become better organized over the next few days. On May 12, the wave had become organized enough and was designated Tropical Depression One-E.[3]

Tropical Depression One-E moved slowly to the northwest while strengthening slowly due to easterly vertical wind shear. The depression was upgraded to Tropical Storm Alma on May 14. The storm quickly strengthened once the vertical wind shear relaxed and was near hurricane force by the morning of May 15. Hurricane Alma reached its peak intensity early on May 16 with maximum sustained winds of 85 mph (137 km/h). The hurricane entered an area of southwesterly wind shear caused by an upper-level ridge of high pressure. The increasing vertical wind shear and cooler water caused Alma to weaken to a tropical storm. On May 17, the storm continued to weaken and became a depression. The next day, the system dissipated as a tropical cyclone well west of mainland Mexico.[3][7][8]

Hurricane Boris

[edit]
Category 1 hurricane (SSHWS)
 
DurationJune 2 – June 8
Peak intensity90 mph (150 km/h) (1-min);
977 mbar (hPa)

A tropical wave came off the northwest coast of Africa on May 20. The wave did not significantly develop as it moved west across the Atlantic Ocean and Caribbean Sea. Once it crossed Central America into the eastern Pacific Ocean, cloudiness increased considerably with the system on May 31.[9] It became well-enough organized to be upgraded to Tropical Depression Two-E on June 2. After becoming a depression, the system moved to the west-northwestward. Upper-level easterly vertical wind shear limited the amount of the initial strengthening. However, an increase in convective banding led to its upgrade to Tropical Storm Boris on June 4, 500 mi (800 km) southwest of Manzanillo. Further strengthening occurred due to an anticyclone aloft fostered additional development, and by June 5, Boris became a hurricane. The hurricane began to move to the north-northwest in response to a trough off of the West Coast of the United States. Strengthening continued, and the storm reached its peak strength with winds of 90 mph (140 km/h) and a minimum central pressure of 977 mb (28.9 inHg). The hurricane's cloud pattern became elongated along a southwest–northeast axis on June 6 due to an increased amount of vertical wind shear. Boris was downgraded to a tropical storm later in the day on June 6. The deep convection of the tropical storm decreased, as Boris moved over cooler waters. It was downgraded to a tropical depression on June 7 due to these factors. The depression dissipated as a tropical cyclone on June 8 as the system quickly lost its tropical characteristics. A small circulation remained in the cloud field offshore the northwest coast of Baja California for a few more days.[9][10]

The winds in the eyewall of Boris ripped off the sails of the Azure Dream sailboat. Outer rainbands from the storm produced moderate rain in several Mexican states. In Mexico, rainfall peaked at 8.83 in (224 mm) near San Lucas, Michoacán. The remnants of Boris also brought sporadic rainfall over the western United States, with precipitation being reported in Arizona, California, Colorado, Nevada and Wyoming. The remnants of Boris were responsible for causing the wettest June in San Diego since records began in 1850; however, not even 1 in (25 mm) of rain fell at that location. Rainfall from the remnant system in the United States peaked at 3.28 in (83 mm) over the Santa Rita Mountains.[11][12] No other direct damages or casualties were reported from Boris.[9][11][13]

Tropical Storm Cristina

[edit]
Tropical storm (SSHWS)
 
DurationJune 8 – June 16
Peak intensity65 mph (100 km/h) (1-min);
994 mbar (hPa)

A tropical wave emerged into the Atlantic Ocean off the coast of Africa on May 28. The wave moved across Central America into the northeastern Pacific Ocean, where convection organized with the system on June 6. The system became well-enough organized to be upgraded to Tropical Depression Three-E on June 8, while 920 mi (1,480 km) south of the southern tip of Baja California. The depression continued to strengthen, and was upgraded to Tropical Storm Cristina on June 9.[14][15]

Cristina initially had well-established upper-level outflow. It failed to reach hurricane status, peaking with maximum sustained winds of 65 mph (105 km/h) due to movement of its associated upper-level anticyclone to the north over Mexico which caused Cristina to be exposed to easterly vertical wind shear. Cristina moved generally northwestward, which eventually placed the storm in cooler waters, and caused the deep convection of the system to dissipate. On June 14, Cristina diminished to a tropical depression. Cristina moved west-northwestward with the low-level flow. The depression dissipated as a tropical cyclone on June 16, after a lack of deep convection for 48 hours.[14][16]

Tropical Storm Douglas

[edit]
Tropical storm (SSHWS)
 
DurationJune 19 – June 23
Peak intensity65 mph (100 km/h) (1-min);
992 mbar (hPa)

A tropical wave moved off the northwest coast of Africa on June 5. It continued westward across the tropical North Atlantic and Caribbean Sea without significant development.[17] The wave entered the northeastern Pacific Ocean on June 16, where it generated an area of increased cloudiness. Organization of thunderstorm activity increased late on June 18 and early on June 19. Tropical Depression Four-E formed on June 19, when it was 230 mi (370 km) south of Acapulco after evidence of low-level circulation for the past 24 hours.[18] The depression moved in a west-northwest direction, due to a subtropical ridge north of the depression. Satellite analysis indicated that the depression had reached tropical storm force strength, and it was upgraded to Tropical Storm Douglas on June 19, while 230 mi (370 km) southwest of Acapulco. Douglas reached peak strength of 65 mph (105 km/h) on June 21[17]

A tropical storm warning was issued on June 21, from Punta Tejupan to Cabo Corrientes before being discontinued on June 22. Tropical Storm Douglas brushed the western coast of Mexico. The center of circulation approached within 17 mi (27 km) of the coast of Mexico on June 22. Douglas then began to weaken because of interaction with the mountainous terrain of Mexico. The system continued to weaken despite warm water temperatures and favorable upper-level conditions. Douglas dissipated early on June 24, while 138 mi (222 km) south-southeast off the southern tip of Baja California Sur. The highest rainfall report from Mexico from Douglas totaled 11.07 in (281 mm) at La Huerta.[19] No deaths or damage were reported.[17][20]

Hurricane Elida

[edit]
Category 1 hurricane (SSHWS)
 
DurationJune 26 – July 2
Peak intensity80 mph (130 km/h) (1-min);
990 mbar (hPa)

A tropical wave came off the coast of Africa into the eastern Atlantic Ocean on June 10 and 11. The system moved across the Atlantic and entered into the northeastern Pacific Ocean.[21] The wave became a significant tropical system, with cyclonic turning in the lower and middle layers of the system's cloudiness on June 25. The center of circulation was located 345 mi (555 km) south of Acapulco, Mexico. The system exhibited sufficient organization to be considered Tropical Depression Five-E on June 26. The depression quickly strengthened and became Tropical Storm Elida later that day. The track of Elida was west-northwestward to northwestward from June 27 through June 28. Some rainbands moved over the mountainous region of southwestern Mexico, but no flooding, damage, or casualties were reported as a result. Elida continued strengthening and it was upgraded to a hurricane early on June 28 passing directly over Socorro Island later in the day, right as Elida reached peak strength of 80 mph (130 km/h), dropping 3.7 in (94 mm) of rain on the island. Some windows broke also as a result, and minor structural damage was reported as a result on the island.[21][22]

A high-pressure area to the north forced Elida to move more westward on June 29. Convection began to decrease in the hurricane as it moved into cooler waters, and it weakened to a tropical storm later in the day. It then weakened to a tropical depression on July 1, and dissipated on July 2.[21][23]

Tropical Depression Six-E

[edit]
Tropical depression (SSHWS)
 
DurationJune 29 – July 3
Peak intensity35 mph (55 km/h) (1-min);
1007 mbar (hPa)

An area of disturbed weather south of Acapulco organized into Tropical Depression Six-E on June 29 and the system began to move northwest. Originally the system was expected to reach tropical storm strength and near hurricane intensity by late on July 2 or early on July 3,[24] however persistent vertical wind shear over the system impeded its development.[25] After convection began to merge into the Intertropical Convergence Zone (ITCZ), the National Hurricane Center discontinued advisories on Tropical Depression Six-E, stating that the depression dissipated, and regeneration seemed unlikely.[26]

However, wind shear began to decrease, and convection associated with the remnants of Tropical Depression Six-E quickly began to increase. Although the low-level circulation was near the edge of the deep convection, the National Hurricane Center resumed advisories on Tropical Depression Six-E by July 1. Intensification into a tropical storm was again predicted,[27] but Tropical Depression Six-E remained poorly defined, and eventually dissipated on July 4.[28]

Hurricane Fausto

[edit]
Category 1 hurricane (SSHWS)
 
DurationJuly 6 – July 12
Peak intensity85 mph (140 km/h) (1-min);
979 mbar (hPa)

A tropical wave came off the northwest coast of Africa on June 19. The wave crossed the Atlantic Ocean and Caribbean Sea, into the warm waters of the northeastern Pacific Ocean, on July 2. An area of disturbed weather moved northwards towards the Gulf of Tehuantepec and became Tropical Depression Seven-E early on July 6. The depression moved northwest, and because of increased organization of deep convection, was designated Tropical Storm Fausto on July 7, 265 mi (426 km) south of Manzanillo, Mexico. A weakly defined eye formed on July 8, and the storm was upgraded to Hurricane Fausto, 310 mi (500 km) south of Cabo San Lucas.[29]

Fausto peaked in strength with winds of 85 mph (137 km/h) and a central pressure of 979 mb (28.9 inHg) on July 9. Fausto passed 40 mi (64 km) north of Socorro Island causing a northwest wind of 40 mph (64 km/h), and 4.3 in (110 mm) of rain at that location. The hurricane fluctuated in intensity on July 10,[29][30] before weakening into a tropical storm later that day, 403 mi (649 km) west of Cabo San Lucas. The weakening Fausto moved over continuing cooler waters, and was downgraded to a tropical depression on July 11, 690 mi (1,110 km) west of Cabo San Lucas. The depression dissipated as a tropical cyclone on July 13, and its low level circulation of clouds persisted for a few days.[29]

Hurricane Genevieve

[edit]
Category 2 hurricane (SSHWS)
 
DurationJuly 10 – July 18
Peak intensity105 mph (165 km/h) (1-min);
970 mbar (hPa)

A tropical wave moved off the coast of Africa on June 25 and moved across the Atlantic Ocean and central Caribbean Sea with little development. Within the western Caribbean Sea, convection developed with the wave on July 7. The system became better organized as it moved into the northeastern Pacific Ocean. The system was upgraded to Tropical Depression Eight-E on July 11. The depression moved west-northwest, with a good outflow to the north, and gradually strengthened into Tropical Storm Genevieve later that day. Genevieve continued to strengthen, reaching hurricane strength on July 13.[31] The storm approached within 23 mi (37 km) of Socorro Island where a sustained wind of 44 mph (71 km/h) and gust of 50 mph (80 km/h) were reported, before the weather equipment on the island failed.[32]

The hurricane began to turn west because of the strengthening and growing ridge to its north. Increasing outflow aloft began to form, and the hurricane reached its peak strength of 105 mph (169 km/h) with a well-defined eye at its center of circulation.[31][33] Genevieve turned northwest on July 16 into an area with strong vertical wind shear and low water temperatures. The hurricane quickly weakened into a tropical storm on July 17 and then into a tropical depression on July 18. Genevieve dissipated as a tropical cyclone later in the day, reduced to a circulation in the stratocumulus cloud field.[31]

Hurricane Hernan

[edit]
Category 4 hurricane (SSHWS)
 
DurationJuly 19 – July 31
Peak intensity155 mph (250 km/h) (1-min);
928 mbar (hPa)

A tropical wave that moved off the northwest coast of Africa on July 4 passed through the Atlantic Ocean and Caribbean Sea without significant development.[34] The wave moved across Central America into the northeastern Pacific Ocean on July 15. Thunderstorm activity increased in the system between July 16 and 18 before rainbands became present within the tropical disturbance on July 19. Tropical Depression Nine-E formed later that day while 565 mi (909 km) southwest of Acapulco, Mexico.[5]

Tropical Depression Nine-E strengthened into Tropical Storm Hernan on July 21 while 684 mi (1,101 km) south of Cabo San Lucas. The tropical storm continued to strengthen and as it moved to the northwest, and became a hurricane late on July 21. Hernan continued to strengthen and as it passed 145 mi (233 km) southwest of Clarion Island. On July 23, Hernan reached its peak strength of 155 mph (249 km/h) and minimum pressure of 928 mb (27.4 inHg) as the center of circulation was 207 mi (333 km) south-southwest of Clarion Island. On July 24, concentric eyewalls (one eyewall located inside another) formed around the center of Hernan, which was the first time this pattern had been observed with an eastern Pacific hurricane.[34][35]

Hernan kept Category 4 hurricane intensity a few more days and hurricane strength for six days overall. The hurricane weakened into a tropical storm on July 28 as it moved over cooler waters. Hernan turned more to the west as its low level center became separated from its thunderstorm activity and was steering by a surface high-pressure system to its north. Hernan moved over cooler waters, dissipating as a tropical cyclone early on July 31.[34][36]

Hurricane Iselle

[edit]
Category 3 hurricane (SSHWS)
 
DurationJuly 20 – July 30
Peak intensity120 mph (195 km/h) (1-min);
958 mbar (hPa)

A tropical wave moved off the coast of Africa on July 7. The wave moved west, but it was not until it moved across the Caribbean Sea that the wave's convection organized.[37] The system entered into the northeastern Pacific Ocean with concentrated convection and a surface center of circulation while southeast of Acapulco. Moving west-northwest, Tropical Depression Ten-E formed on July 20 393 mi (632 km) south of Puerto Ángel, Mexico. Early on the following day, the depression strengthened into Tropical Storm Iselle. The storm continued strengthening while in the proximity of Hurricane Hernan, becoming a hurricane on July 22.[5]

The hurricane continued to move west-northwest through its duration, and reached its peak strength of 120 mph (190 km/h) on July 25. Iselle crossed Socorro Island, which recorded a 70 mph (110 km/h) sustained wind and heavy rain on July 25.[37][38][39] The hurricane weakened on following days after it moved over cooler waters, downgraded to a tropical storm on July 28 and subsequently into a tropical depression on July 30. The depression dissipated later that day, after losing its low-level circulation 588 mi (946 km) southwest of San Diego.[37][39][40]

Tropical Depression Eleven-E

[edit]
Tropical depression (SSHWS)
 
DurationJuly 24 – July 26
Peak intensity30 mph (45 km/h) (1-min);
1009 mbar (hPa)

On July 24 a tropical disturbance behind Hurricane Hernan strengthened into a tropical depression. Due to the close proximity of Hernan to its west, the development of the depression was hindered due to vertical wind shear from the outflow of Hernan. This wind shear dissipated the depression on July 26, and its remnants were absorbed by the nearby cyclone. No damages or casualties were caused by the depression as it was well out to sea.[41]

Tropical Storm Aka

[edit]
Tropical storm (SSHWS)
 
DurationAugust 7 – August 13 (exited basin)
Peak intensity65 mph (100 km/h) (1-min);
994 mbar (hPa)

Tropical Storm Aka was the only tropical storm to form in the Central North Pacific during 1990. An area of disturbed weather began to organize on August 6. By August 7, the system became well-enough organized to become designated Tropical depression One-C. The depression intensified into a tropical storm while moving west, to the south of the Hawaiian Islands. On August 10, Tropical Storm Aka peaked with maximum sustained winds of 60 mph (97 km/h). The storm continued to move west and approached Johnston Island, though the island's weather did not deteriorate. The tropical storm crossed the International Date Line on August 13.[42] Aka weakened back into a depression and dissipated two days later on August 15.[5]

Tropical Depression Diana

[edit]
Tropical depression (SSHWS)
 
DurationAugust 8 – August 9
Peak intensity35 mph (55 km/h) (1-min);
1004 mbar (hPa)

Atlantic basin Hurricane Diana made landfall on August 7 at Category 2 strength in Tamiahua, Tamaulipas, along the Gulf of Mexico coast. The system quickly deteriorated inland while traversing the high terrain of Mexico. Some convection remained as it emerged into the eastern Pacific Ocean late on August 8.[43] Though Diana crossed between basins, the National Hurricane Center did not re-classify it as an eastern Pacific system. No re-intensification occurred, and by the following day it lost all tropical characteristics. The remnant disturbance turned northward around the eastern periphery of an upper-low and tracked through the Gulf of California. Convection flared up before it moved into northwest Mexico, bringing rainfall amounts of over 10 in (250 mm) to local areas of Sonora. Later, after moving into Arizona, the disturbance dissipated by early on August 14.[44]

Tropical Depression Two-C

[edit]
Tropical depression (SSHWS)
 
DurationAugust 10 – August 13
Peak intensity35 mph (55 km/h) (1-min);
1000 mbar (hPa)

Tropical Depression Two-C was the second and last tropical cyclone to develop within the north-central Pacific Ocean in 1990. The depression developed from a tropical disturbance well southeast of Hawaii, which became much better organized on the night of August 10. The tropical depression moved in a west northwest direction for the next 18 hours and then changed to a west-southwest track on August 11. As it turned more to the southwest, the depression weakened until it dissipated on August 13 about 600 mi (970 km) south-southeast of Hilo, Hawaii.[42]

Tropical Depression Twelve-E

[edit]
Tropical depression (SSHWS)
 
DurationAugust 16 – August 19
Peak intensity35 mph (55 km/h) (1-min);
1009 mbar (hPa)

A persistent area of thunderstorm activity southwest of Puerto Vallarta became better organized and strengthened into Tropical Depression Twelve-E on August 16. Moving northwest, the system developed slowly as it was embedded within the Intertropical Convergence Zone. Easterly shear kept the system from reaching tropical storm strength and caused its ultimate dissipation on August 19. No damages or fatalities were caused by this depression.[45]

Hurricane Julio

[edit]
Category 3 hurricane (SSHWS)
 
DurationAugust 17 – August 24
Peak intensity115 mph (185 km/h) (1-min);
960 mbar (hPa)

A tropical wave moved off the western coast of Africa on August 5, moving across the Atlantic Ocean and Caribbean Sea without significant development. The system entered the northeastern Pacific Ocean, and became well-enough organized to be upgraded to Tropical Depression Thirteen-E on August 17 while centered 404 mi (650 km) south of Acapulco, Mexico. The depression moved on a west-northwestward track and strengthened, becoming Tropical Storm Julio on August 18. Strengthening continued and Julio reached hurricane strength on August 19. The cyclone peaked with maximum sustained winds of 115 mph (185 km/h) on August 21. The storm turned westward and began weakening. Julio regained tropical storm status on August 23 and tropical depression status on August 24 before dissipating as a tropical cyclone later that day. No damage was reported from Julio.[46]

Hurricane Kenna

[edit]
Category 1 hurricane (SSHWS)
 
DurationAugust 21 – August 30
Peak intensity85 mph (140 km/h) (1-min);
980 mbar (hPa)

A tropical wave moved off the coast of Africa on August 9, and spawned Tropical Storm Fran four days later, before it moved through the southern Windward Islands on August 14. While Fran dissipated shortly after that, the tropical wave progressed into the northeastern Pacific Ocean.[47] The wave spawned Tropical Depression Fourteen-E 808 mi (1,300 km) east-southeast of Hurricane Julio. The depression moved westward for the next several days. As Julio weakened, the depression began to increase in strength. It became Tropical Storm Kenna on August 22 and continued to strengthen into a hurricane on August 25, peaking with winds of 85 mph (137 km/h) the next day. On August 26, a strong frontal trough weakened the high pressure system to the storm's north, causing a turn to the north during the next few days. The hurricane weakened in response to cooler water and increasing vertical wind shear, which removed convection from its center. Kenna weakened back to tropical storm strength on August 28,[48] then into a tropical depression on August 29. The system dissipated as a tropical cyclone on August 30.[47][49]

Hurricane Lowell

[edit]
Category 1 hurricane (SSHWS)
 
DurationAugust 23 – September 1
Peak intensity75 mph (120 km/h) (1-min);
986 mbar (hPa)

A tropical wave moved off the northwestern coast of Africa into the Atlantic Ocean on August 11. After moving across the Atlantic and Caribbean Sea without development, the system moved through the Intertropical Convergence Zone of the northeastern Pacific Ocean.[50] The cloudiness moved northward toward the Gulf of Tehuantepec on August 22. The thunderstorm activity organized sufficiently for the system to be upgraded to Tropical Depression Fifteen-E on August 23 while 298 mi (480 km) southeast of Acapulco, Mexico. The depression moved west-northwestward and strengthened into a tropical storm 217 mi (349 km) south-southwest of Puerto Vallarta on August 25. The storm began to turn more westward due to a strengthening high pressure system to its north and was upgraded to a hurricane on August 27 while 286 mi (460 km) southwest of Cabo San Lucas. As the high to the north continued to strengthen, the hurricane turned west-southwest.[50]

Thunderstorm activity with the hurricane began to weaken and Lowell was downgraded back to tropical storm status on August 28. The tropical storm then turned to a north-northwestward with the storm passing over cooler waters. On August 31, the storm was downgraded to a tropical depression, with only minimal amounts of deep convection remaining within its circulation. Lowell dissipated as a tropical cyclone on September 1, though a low-level circulation of clouds could be seen on satellite imagery for the next few days. No damage or casualties was reported as a result of Lowell.[50][51]

Hurricane Marie

[edit]
Category 4 hurricane (SSHWS)
 
DurationSeptember 7 – September 21
Peak intensity140 mph (220 km/h) (1-min);
944 mbar (hPa)

A tropical wave moved off the northwestern coast of Africa on August 16. The wave moved west through the Atlantic Ocean and Caribbean Sea without significant development.[52] The wave moved across Central America and into the northeastern Pacific Ocean, on August 29. Isolated convection with the system increased while south of the Gulf of Tehuantepec as the system moved northwest parallel to the southwest coast of Mexico. Once convective activity increased, the system was upgraded to Tropical Depression Sixteen-E on September 7 while centered 659 mi (1,061 km) southwest of Clarion Island.[52]

A weaker than normal high pressure system controlled the movement of the depression, and the system moved slowly to the west through its duration. The depression strengthened into Tropical Storm Marie on September 8, and into a hurricane on September 9, while 522 mi (840 km) south-southwest of Clarion Island. Marie reached its peak intensity of 140 mph (230 km/h) on September 11.[52] The hurricane crossed into the central North Pacific on September 14 as a hurricane with maximum sustained winds of 110 mph (180 km/h). The hurricane weakened thereafter and on September 17 Marie regained tropical storm status. The system weakened into a tropical depression on September 19 and dissipated as a tropical cyclone on September 21 near the Hawaiian coast. No casualties or damages were caused by Marie.[42]

Hurricane Norbert

[edit]
Category 1 hurricane (SSHWS)
 
DurationSeptember 10 – September 19
Peak intensity80 mph (130 km/h) (1-min);
983 mbar (hPa)

A tropical wave moved off the coast of Africa and across the Atlantic Ocean and Caribbean Sea without significant development. The wave entered the northeastern Pacific Ocean and began to show signs of organized thunderstorm development. Tropical Depression Seventeen-E formed on September 10 while centered 758 mi (1,220 km) south-southwest of Cabo San Lucas, Mexico. The depression became better organized and strengthened into Tropical Storm Norbert later in the day.[53]

On September 12, Norbert absorbed Tropical Depression Eighteen-E which was in close proximity. Norbert strengthened as it moved north-northwestward. The tropical storm was upgraded to a hurricane on September 14, and formed an eye on September 15. The storm reached its peak strength of 80 mph (130 km/h) sustained winds that day. Turning north of due west,[53] Norbert then weakened as it moved over cooler waters. It was downgraded to a tropical storm later on September 15, and then to a tropical depression on September 18. Norbert dissipated as a tropical cyclone on September 19 after losing all its deep convection.[53][54]

Tropical Depression Eighteen-E

[edit]
Tropical depression (SSHWS)
 
DurationSeptember 9 – September 12
Peak intensity35 mph (55 km/h) (1-min);
1000 mbar (hPa)

On September 12, satellite images indicated that the eighteenth tropical depression of the season formed southwest of Cabo San Lucas. Located in close proximity to Tropical Storm Norbert, the depression would soon enter a region of colder sea surface temperatures, and the National Hurricane Center noted that only very little intensification was possible.[55] As predicted, Norbert hindered further intensification of Tropical Depression Eighteen-E. The National Hurricane Center noted six hours later that the depression would likely be absorbed into Norbert.[56] The National Hurricane Center later believed that Tropical Depression Eighteen-E was "dominating" the interaction between the two systems, and was forecast to absorb Norbert.[57] Unlike the latter prediction, Norbert absorbed Tropical Depression Eighteen-E later that day.[58]

Hurricane Odile

[edit]
Category 4 hurricane (SSHWS)
 
DurationSeptember 23 – October 2
Peak intensity145 mph (230 km/h) (1-min);
935 mbar (hPa)

A tropical wave move off the coast of Africa on September 5, and crossed the Atlantic waters, the Caribbean Sea and eventually into the Pacific Ocean as a weak system. An area of convection entered into the northeastern Pacific Ocean a few hundred miles south of Acapulco, Mexico. On September 23, Tropical Depression Nineteen-E formed from this convection, while 746 mi (1,201 km) south-southeast from the southern tip of Baja California. The depression moved on a west-northwestward track, rounding the southwest side of a strong high pressure system. The depression continued to strengthen and was upgraded to Tropical Storm Odile on September 24 and into a hurricane on September 25. Its intensity peaked with maximum sustained winds of 145 mph (233 km/h) on September 26.[59]

The hurricane began to turn more northwestward in response to a high-pressure system weakening to its north. Odile began to weaken as it moved over cooler waters on September 28. The cyclone regained tropical storm status on September 29 while it slowly progressed northward. The system weakened into a tropical depression status on September 30. Once it lost its deep convection, Odile was steered southwestward by the low-level flow, before it dissipated as a tropical cyclone on October 2. Its remaining low-level circulation of clouds continued on a southwestward course thereafter.[59][60]

Tropical Storm Rachel

[edit]
Tropical storm (SSHWS)
 
DurationSeptember 27 – October 3
Peak intensity65 mph (100 km/h) (1-min);
994 mbar (hPa)

In mid-September, a weak tropical wave moved off the coast of Northwest Africa. It moved westward and entered the eastern Pacific Ocean early on September 23. Cloudiness became concentrated with the system south of the Gulf of Tehuantepec. On September 27, the organized thunderstorm area was upgraded to Tropical Depression Twenty One-E while 230 mi (370 km) south of Acapulco. The depression developed slowly, and became a tropical storm on September 30. As Rachel briefly moved northward, before re-curving and accelerating towards the Mexican coast. The storm passed over the southern portion of Baja California Sur on October 2. Rachel made its final landfall midway between Los Mochis and Culiacán, and became the only system to make landfall from the eastern north Pacific Ocean in 1990.[61][62] Rachel decayed rapidly over land, and the final public advisory on Rachel was issued early on October 3.[63] its remnants continued accelerating over Texas until they lost their identity.

The highest rainfall total from the system in Mexico totaled 9.85 in (250 mm) at Santa Anita near the tip of Baja California.[64] Across northern Mexico, thousands were homeless, and 18 people died.[65] In Texas, Rachel's remnants caused heavy rain. Flooding occurred in the Big Bend area.[61][62][63][66]

Hurricane Polo

[edit]
Category 1 hurricane (SSHWS)
 
DurationSeptember 28 – October 1
Peak intensity75 mph (120 km/h) (1-min);
987 mbar (hPa)

Polo originated from a tropical wave that moved off the African coast on September 2 which spawned Hurricane Isidore in the Atlantic basin. On September 14, the system increased in convection as it was moving to the west and approaching Central America. The southern extent of the wave crossed into the Pacific Ocean on September 18.[67]

The wave continued westward and related thunderstorm activity increased during the following week. The convective system organized into Tropical Depression Twenty-E on September 28 nearly midway between Mexico and Hawaii. Initially, the depression drifted toward the northwest due to a large upper-level trough located to its west. Polo strengthened rapidly into a hurricane early on September 30, with its winds peaking at 75 mph (121 km/h). Since the storm was very small, vertical wind shear caused significant weakening thereafter.[67] On October 1, Polo crossed into the Central Pacific basin at tropical storm strength. The storm continued to weaken, becoming a tropical depression and then dissipating southwest of Hawaii later in the day.[42] There were no casualties or damages caused by Polo.

Tropical Storm Simon

[edit]
Tropical storm (SSHWS)
 
DurationOctober 9 – October 14
Peak intensity70 mph (110 km/h) (1-min);
990 mbar (hPa)

A weakly defined tropical wave moved off the northwest coast of Africa on September 20, and crossed the northern portion of the tropical Atlantic and northern South America without significant organization. The wave moved into the northeastern Pacific waters, off the coast of Colombia on September 30. As the wave passed over southern Central America, rainbands and cloudiness increased with the system between October 1 and October 3, before the system merged with the ITCZ from October 4 to October 6. Signs of convective organization reappeared on October 8, and by October 9, the system was upgraded to Tropical Depression Twenty Two-E 578 mi (930 km) south of Cabo San Lucas, Mexico.[68]

The depression continued to develop and was upgraded to Tropical Storm Simon on October 10 while 604 mi (972 km) south-southwest of Cabo San Lucas. Due to a high-pressure system to the north-northwest, Simon continued on a west-northwestward path. The tropical storm continued to strengthen to its peak intensity of 70 mph (110 km/h) by late on October 11. Simon passed over cooler waters and weakened back into a tropical depression on October 13. The depression moved on a westward course, and the low-level circulation was displaced from its deep convection during the following day. Simon then dissipated as a tropical cyclone early on October 15 across the open waters of the northeast Pacific.[68]

Hurricane Trudy

[edit]
Category 4 hurricane (SSHWS)
 
DurationOctober 16 – November 1
Peak intensity155 mph (250 km/h) (1-min);
924 mbar (hPa)

The tropical wave that would become future Hurricane Trudy became identifiable on satellite imagery as early as September 30, emerging near the African coast off Cape Verde. However, the wave did not show any signs of development until October 16, when the wave developed into a tropical depression several hundred kilometers south of Acapulco. The tropical depression intensified significantly. The ship Maple Ace reported gale-force winds about 140 km (85 mi) from the center at 1800 UTC on October 18. In less than 36 hours, at 1200 UTC on October 20, Trudy became a powerful hurricane with Category 4 equivalent maximum winds of 155 mph (250 km/h) and a minimum pressure of 925 mbar (27.3 inHg) according to satellite estimates. Trudy was at least as intense as Hurricane Max three years earlier and Hurricane Hernan earlier in the year. Estimates state that Trudy may have been the strongest eastern Pacific hurricane since wind estimates have been available from satellite images.[1]

An upper-level trough forced Trudy to move northwards, increasing the risk of hurricane conditions to Baja California Sur residents. The same trough caused an unfavorable environment that caused Trudy to weaken considerably. At that time, dynamically based numeral models predicted Trudy to move northwards over Baja California and make landfall there.[1] Authorities closed five ports on the Baja California peninsula and the Pacific Ocean port of Mazatlán on October 22 as Hurricane Trudy was approaching the Mexican coast with gusts of up to 115 mph (185 km/h).[69] However, the trough progressed eastwards and was replaced by a ridge, sparing a landfall,[1] but still causing locally heavy rainfall and high waves. Socorro Island reported hurricane-force winds for more than 7 hours.[69][70] Moving away from land, Trudy then started to re-intensify, developing an unusually large eye of nearly 90 km (55 mi) in diameter. However, another deep trough approached Trudy and pulled the hurricane northwards, shearing it at the same time. Trudy dissipated on November 1 at 1800 UTC. Its remnant moisture spread over parts of Mexico and the United States.[1]

Hurricane Vance

[edit]
Category 2 hurricane (SSHWS)
 
DurationOctober 21 – October 31
Peak intensity100 mph (155 km/h) (1-min);
975 mbar (hPa)

An area of disturbed weather, possibly related to a tropical wave, organized into Tropical Depression Twenty Four-E on October 21. It strengthened into Tropical Storm Vance early on October 23 and then into a hurricane two days later. Vance moved parallel to the west coast of Mexico and approached the southern tip of the Baja California Peninsula. Before it could strike land, a high-pressure area blocked Vance's path and forced the storm to transcribe a small clockwise loop over a two-day period. During the loop, Vance encountered wind shear and cool waters stirred up by Trudy as well as earlier in its duration. Vance weakened to a tropical storm on October 27 and a depression on October 30. The cyclone dissipated late on October 31.[71]

Storm names

[edit]

The following list of names was used for named storms that formed in the North Pacific Ocean east of 140°W in 1990.[72] This is essentially the same list used for the 1984 season, though the rotating lists went only to the "W" name at the time.[73] It would be used next, with one modification, for the 1996 season, as Wallis was interchanged with Winnie.[74] No names were retired from the list following the 1990 season.[75]

  • Alma
  • Boris
  • Cristina
  • Douglas
  • Elida
  • Fausto
  • Genevieve
  • Hernan
  • Iselle
  • Julio
  • Kenna
  • Lowell
  • Marie*
  • Norbert
  • Odile
  • Polo*
  • Rachel
  • Simon
  • Trudy
  • Vance
  • Wallis (unused)
  • Xavier (unused)
  • Yolanda (unused)
  • Zeke (unused)
  • Additionally, Diana entered the eastern Pacific basin during the season from the Atlantic basin. Its crossover between basins as an intact tropical cyclone was detected in a post-storm analysis of the system. Thus the National Hurricane Center did not re-classify it as an eastern Pacific system.[43][44]

For storms that form in the North Pacific from 140°W to the International Date Line, the names come from a series of four rotating lists. Names are used one after the other without regard to year, and when the bottom of one list is reached, the next named storm receives the name at the top of the next list.[72][76] One named storm, listed below, formed in the central North Pacific in 1990. Named storms in the table above that crossed into the area during the year are noted (*).[42]

  • Aka

Season effects

[edit]

This is a table of all of the tropical cyclones that formed in the 1990 Pacific hurricane season. It includes their name, duration (within the basin), peak classification and intensities, areas affected, damage, and death totals. Deaths in parentheses are additional and indirect (an example of an indirect death would be a traffic accident), but were still related to that storm. Damage and deaths include totals while the storm was extratropical, a wave, or a low, and all of the damage figures are in 1990 USD.

Saffir–Simpson scale
TD TS C1 C2 C3 C4 C5
1990 Pacific hurricane season statistics
Storm
name
Dates active Storm category
at peak intensity
Max 1-min
wind
mph (km/h)
Min.
press.
(mbar)
Areas affected Damage
(USD)
Deaths Ref(s)
Alma May 12 – 18 Category 1 hurricane 85 (140) 979 None None None
Boris June 2 – 8 Category 1 hurricane 90 (150) 978 Baja California Peninsula, Northwestern Mexico Unknown None
Cristina June 8 – 16 Tropical storm 65 (100) 994 None None None
Douglas June 19 – 23 Tropical storm 65 (100) 992 Southwestern Mexico, Central America Minimal 1
Elida June 26 – July 2 Category 1 hurricane 80 (130) 990 Revillagigedo Island None None
Six-E June 29 – July 3 Tropical depression 35 (55) 1007 None None None
Fausto July 6 – 12 Category 1 hurricane 85 (140) 979 None None None
Genevieve July 10 – 18 Category 2 hurricane 105 (165) 970 None None None
Hernan July 19 – 31 Category 4 hurricane 155 (250) 928 None None None
Iselle July 20 – 30 Category 3 hurricane 120 (195) 958 None None None
Eleven-E July 24 – 26 Tropical depression 30 (45) 1009 None None None
Aka August 7 – 13 Tropical storm 65 (100) 991 Hawaiian Islands None None
Diana August 8 – 9 Tropical depression 35 (55) 1004 Southwestern Mexico (after crossover) None None
Two-C August 10 – 13 Tropical depression 35 (55) 1000 None None None
Twelve-E August 16 – 19 Tropical depression 35 (55) 1009 None None None
Julio August 17 – 24 Category 3 hurricane 115 (185) 960 None None None
Kenna August 21 – 30 Category 1 hurricane 85 (140) 980 None None None
Lowell August 23 – September 1 Category 1 hurricane 75 (120) 986 None None None
Marie September 7 – 21 Category 4 hurricane 140 (220) 944 None None None
Norbert September 10 – 19 Category 1 hurricane 80 (130) 983 None None None
Eighteen-E September 10 – 12 Tropical depression 35 (55) 1000 None None None
Odile September 23 – October 1 Category 4 hurricane 145 (230) 935 None None None
Rachel September 27 – October 3 Tropical storm 65 (100) 994 Baja California Peninsula, Texas 2.5 million 18
Polo September 28 – October 1 Category 1 hurricane 75 (120) 987 None None None
Simon October 9 – 14 Tropical storm 70 (110) 990 None None None
Trudy October 16 – November 1 Category 4 hurricane 155 (250) 924 None None None
Vance October 21 – 31 Category 2 hurricane 100 (155) 975 Southwestern Mexico, Central America 10 million None
Season aggregates
27 systems May 12 – November 1   155 (250) 924 12.5 million 19  

See also

[edit]

Notes

[edit]
  1. ^ The total represents the sum of the squares of the maximum sustained wind speed (knots) for every (sub)tropical storm's intensity of over 33 knots (38 mph; 61 km/h), divided by 10,000 while they are above that threshold; therefore, tropical depressions are not included.

References

[edit]
  1. ^ a b c d e f Avila, Lixion (1990). "Eastern North Pacific Season of 1990". Monthly Weather Review. 119 (8). National Hurricane Center: 2034. Bibcode:1991MWRv..119.2034A. doi:10.1175/1520-0493(1991)119<2034:ENPHSO>2.0.CO;2. ISSN 1520-0493.
  2. ^ "Basin Archives: Northeast Pacific Ocean Historical Tropical Cyclone Statistics". Fort Collins, Colorado: Colorado State University. Retrieved July 8, 2022.
  3. ^ a b c Case, Robert (1990). "Hurricane Alma Preliminary Report, Page 1". National Hurricane Center. Retrieved January 2, 2011.
  4. ^ Case, Robert (1990). "Hurricane Alma Preliminary Report, Page 2". National Hurricane Center. Retrieved January 2, 2011.
  5. ^ a b c d "Eastern Pacific Hurricane Database". National Hurricane Center. 2010. Retrieved April 26, 2010.[permanent dead link]
  6. ^ "Basin Archives: Northeast Pacific Ocean Historical Tropical Cyclone Statistics". Fort Collins, Colorado: Colorado State University. Retrieved July 8, 2022.
  7. ^ Mayfield, Max (May 13, 1990). "Tropical Cyclone Discussion Tropical Depression One-E". National Hurricane Center. Retrieved January 2, 2011.
  8. ^ Gerrish, Hal (May 15, 1990). "Tropical Cyclone Discussion Tropical Storm Alma". National Hurricane Center. Retrieved January 2, 2011.
  9. ^ a b c Mayfield, Max (1990). "Hurricane Boris Preliminary Report, Page 1". National Hurricane Center. Retrieved January 2, 2011.
  10. ^ Lixion, Avila (June 8, 1990). "Tropical Cyclone Discussion: Tropical Depression Boris". National Hurricane Center. Retrieved January 2, 2011.
  11. ^ a b Mayfield, Max (1990). "Hurricane Boris Preliminary Report, Page 2". National Hurricane Center. Retrieved January 2, 2011.
  12. ^ Roth, David (August 12, 2008). "Hurricane Boris – June 4–11, 1990". Hydrometeorological Prediction Center. Retrieved January 2, 2011.
  13. ^ Avila, Lixion (1990). "Tropical Cyclone Discussion: Tropical Depression Two-E". National Hurricane Center. Retrieved January 2, 2011.
  14. ^ a b Avila, Lixion (June 22, 1990). "Tropical Storm Cristina Preliminary Report, Page 1". National Hurricane Center. Retrieved January 2, 2011.
  15. ^ Avila, Lixion (June 8, 1990). "Tropical Cyclone Discussion: Tropical Depression Three-E". National Hurricane Center. Retrieved January 2, 2011.
  16. ^ Mayfield, Max (June 16, 1990). "Tropical Cyclone Discussion: Tropical Depression Cristina". National Hurricane Center. Retrieved January 2, 2011.
  17. ^ a b c Gerrish, Hal (1990). "Tropical Storm Douglas Preliminary Report, Page 1". National Hurricane Center. Retrieved January 3, 2011.
  18. ^ Lawrence, Miles (June 19, 1990). "Tropical Cyclone Discussion: Tropical Storm Douglas". National Hurricane Center. Retrieved January 3, 2011.
  19. ^ Roth, David (May 4, 2010). "Tropical Storm Douglas – June 18–23, 1990". Hydrometeorological Prediction Center. Retrieved January 3, 2011.
  20. ^ Gerrish, Hal (1990). "Tropical Storm Douglas Preliminary Report, Page 4". National Hurricane Center. Retrieved January 3, 2011.
  21. ^ a b c Lawrence, Miles (1990). "Hurricane Elida Preliminary Report, Page 1". National Hurricane Center. Retrieved January 2, 2011.
  22. ^ Lawrence, Miles (1990). "Hurricane Elida Preliminary Report, Page 2". National Hurricane Center. Retrieved January 2, 2011.
  23. ^ Mayfield, Max (July 1, 1990). "Tropical Cyclone Discussion: Tropical Depression Elida". National Hurricane Center. Retrieved January 2, 2011.
  24. ^ Avila, Lixion (June 29, 1990). "Tropical Cyclone Discussion: Tropical Depression Six-E (#1)". National Hurricane Center. Retrieved January 2, 2011.
  25. ^ Avila, Lixion (June 30, 1990). "Tropical Cyclone Discussion: Tropical Depression Six-E (#3)". National Hurricane Center. Retrieved January 2, 2011.
  26. ^ "Tropical Cyclone Discussion: Tropical Depression Six-E (#5)". National Hurricane Center. June 30, 1990. Retrieved January 2, 2011.
  27. ^ Gerrish, Hal (July 1, 1990). "Tropical Cyclone Discussion: Tropical Depression Six-E (#6)". National Hurricane Center. Retrieved January 2, 2011.
  28. ^ Gerrish, Hal (July 4, 1990). "Tropical Cyclone Discussion: Tropical Depression Six-E (#18)". National Hurricane Center. Retrieved January 2, 2011.
  29. ^ a b c Mayfield, Max (1990). "Hurricane Fausto Preliminary Report, Page 1". National Hurricane Center. Retrieved January 2, 2011.
  30. ^ Mayfield, Max (1990). "Hurricane Fausto Preliminary Report, Page 2". National Hurricane Center. Retrieved January 2, 2011.
  31. ^ a b c Case, Robert (August 16, 1990). "Hurricane Genevieve Preliminary Report 1". National Hurricane Center. Retrieved January 2, 2011.
  32. ^ Case, Robert (August 16, 1990). "Hurricane Genevieve Preliminary Report, Page 2". National Hurricane Center. Retrieved January 3, 2011.
  33. ^ "Tropical Cyclone Discussion: Tropical Depression Eight-E". National Hurricane Center. July 11, 1990. Retrieved January 3, 2011.
  34. ^ a b c Gerrish, Hal (1990). "Hurricane Hernan Preliminary Report, Page 1". National Hurricane Center. Retrieved January 3, 2011.
  35. ^ Gerrish, Hal (1990). "Hurricane Hernan Preliminary Report, Page 2". National Hurricane Center. Retrieved January 2, 2011.
  36. ^ Satchwell, Barry (July 31, 1990). "Tropical Cyclone Discussion: Tropical Depression Hernan". National Hurricane Center. Retrieved January 3, 2011.
  37. ^ a b c Avila, Lixion (August 15, 1990). "Hurricane Iselle Preliminary Report, Page 1". National Hurricane Center. Retrieved January 2, 2011.
  38. ^ Avila, Lixion (August 15, 1990). "Hurricane Iselle Preliminary Report, Page 2". National Hurricane Center. Retrieved January 2, 2011.
  39. ^ a b Avila, Lixion (August 15, 1990). "Hurricane Iselle Preliminary Report, Page 3". National Hurricane Center. Retrieved January 2, 2011.
  40. ^ Lawrence, Miles (July 30, 1990). "Tropical Cyclone Discussion: Tropical Depression Iselle". National Hurricane Center. Retrieved January 3, 2011.
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