Climate of Oregon: Difference between revisions
Benryoung23 (talk | contribs) →Snow: Snowfall in the valley rarely exceeds 10 inches per year. NOAA published data has yearly averages for various cities between 5 and 10 inches (Corvallis, Eugene, Portland, Salem, etc.) <ref>https://www.currentresults.com/Weather/Oregon/annual-snowfall.php</ref> |
-11F in Seneca |
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[[File:Köppen Climate Types Oregon.png|thumb|252x252px|[[Köppen climate classification|Köppen climate types]] of Oregon, using 1991-2020 [[Climatological normal|climate normals]].]] |
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[[File:OR trewartha.svg|thumb|250px|[[Trewartha climate classification|Trewartha climate types]] of Oregon]] |
[[File:OR trewartha.svg|thumb|250px|[[Trewartha climate classification|Trewartha climate types]] of Oregon]] |
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According to the [[Köppen climate classification]], most of [[Western Oregon]] has a [[warm-summer Mediterranean climate]] (or Csb type), which features warm, dry summers, and wet winters with frequent overcast and cloudy skies. [[Eastern Oregon]] falls into the [[cold semi-arid climate]] (or BSk type), which features drier weather. |
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⚫ | |||
⚫ | West of the [[Cascade Range]], winters are chilly with frequent rain and occasional snow. Temperatures can get very cold, but only occasionally, as the result of [[Arctic]] [[cold waves]]. The high desert region of the state is much drier, with less rain, more snow, colder winters, and hotter summers.<ref>{{cite web|url=http://www.geog.nau.edu/courses/alew/ggr346/text/chapters/ch10.html|title=The Pacific Coast|author=Lew, Allen A.|publisher=[[Northern Arizona University]]|year=2004|access-date=April 16, 2010|archive-url=https://web.archive.org/web/20090531012223/http://www.geog.nau.edu/courses/alew/ggr346/text/chapters/ch10.html|archive-date=May 31, 2009|url-status=dead}}</ref> |
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==Precipitation== |
==Precipitation== |
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[[File:Oregon Average Annual Precipitation (1961-1990) Map.png|thumb|right|Oregon rainfall varies widely from region to region.]] |
[[File:Oregon Average Annual Precipitation (1961-1990) Map.png|thumb|right|Oregon rainfall varies widely from region to region.]] |
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[[Precipitation (meteorology)|Precipitation]] in the state varies widely: some western coastal slopes approach {{convert|200|in|mm}} annually, while the driest places, such as the [[Alvord Desert]] (in the [[rain shadow]] of [[Steens Mountain]]) in eastern Oregon, get as little as {{convert|5|in|mm}}.{{sfn|Allan|Buckley|Meacham|2001|pp=154–55}}<ref name=WRCC>{{cite web|url=http://www.wrcc.dri.edu/narratives/OREGON.htm|title=Climate of Oregon|author=Western Regional Climate Center|publisher=[[Desert Research Institute]]|date |
[[Precipitation (meteorology)|Precipitation]] in the state varies widely: some western coastal slopes approach {{convert|200|in|mm}} annually, while the driest places, such as the [[Alvord Desert]] (in the [[rain shadow]] of [[Steens Mountain]]) in eastern Oregon, get as little as {{convert|5|in|mm}}.{{sfn|Allan|Buckley|Meacham|2001|pp=154–55}}<ref name=WRCC>{{cite web|url=http://www.wrcc.dri.edu/narratives/OREGON.htm|title=Climate of Oregon|author=Western Regional Climate Center|publisher=[[Desert Research Institute]]|access-date=April 16, 2010|archive-date=December 21, 2016|archive-url=https://web.archive.org/web/20161221222524/http://www.wrcc.dri.edu/narratives/OREGON.htm|url-status=dead}}</ref> |
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The Pacific Ocean, the moisture-laden air above it, and the storms moving from it over the Oregon coast, are major factors in the state's precipitation patterns. As humid ocean air flows east from the ocean and encounters the [[Oregon Coast Range|Coast Range]], it rises steeply, cools, and loses moisture through [[condensation]], which produces heavy rain. The heaviest precipitation in the state occurs at {{convert|2000|to|4000|ft|m}} above sea level in these coastal mountains. At lower elevations along the coast, [[orographic precipitation]] is less intense but still produces {{convert|60|to|80|in|mm}} a year.{{sfn|Allan|Buckley|Meacham|2001|pp=154–55}} |
The Pacific Ocean, the moisture-laden air above it, and the storms moving from it over the Oregon coast, are major factors in the state's precipitation patterns. As humid ocean air flows east from the ocean and encounters the [[Oregon Coast Range|Coast Range]], it rises steeply, cools, and loses moisture through [[condensation]], which produces heavy rain. The heaviest precipitation in the state occurs at {{convert|2000|to|4000|ft|m}} above sea level in these coastal mountains. At lower elevations along the coast, [[orographic precipitation]] is less intense but still produces {{convert|60|to|80|in|mm}} a year.{{sfn|Allan|Buckley|Meacham|2001|pp=154–55}} |
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In addition to seasonal cycles in solar radiation (more in summer, less in winter), major factors affecting temperatures in Oregon include the moderating influence of the Pacific Ocean combined with variations in surface elevation, especially the Cascade Range. In general, temperatures on Earth drop by about 4 °F (2 °C) per each {{convert|1000|ft|m}} increase in elevation. Throughout the year, high elevations across the state tend to be cooler than low elevations. In addition, the Cascades, running north–south from border to border, generally retain relatively warm Pacific air masses on the western side of the state and relatively cool continental air masses on the eastern side. This prevailing pattern breaks down occasionally when dense cold air flows down the [[Columbia Gorge]] into the Willamette Valley and lowers temperatures more than usual from Portland to Eugene.{{sfn|Allan|Buckley|Meacham|2001|pp=158–59}} |
In addition to seasonal cycles in solar radiation (more in summer, less in winter), major factors affecting temperatures in Oregon include the moderating influence of the Pacific Ocean combined with variations in surface elevation, especially the Cascade Range. In general, temperatures on Earth drop by about 4 °F (2 °C) per each {{convert|1000|ft|m}} increase in elevation. Throughout the year, high elevations across the state tend to be cooler than low elevations. In addition, the Cascades, running north–south from border to border, generally retain relatively warm Pacific air masses on the western side of the state and relatively cool continental air masses on the eastern side. This prevailing pattern breaks down occasionally when dense cold air flows down the [[Columbia Gorge]] into the Willamette Valley and lowers temperatures more than usual from Portland to Eugene.{{sfn|Allan|Buckley|Meacham|2001|pp=158–59}} |
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Oregon has a wide range of temperatures, though the extremes are rare.<ref name=WRCC/> The highest was recorded on July 29, 1898, in [[ |
Oregon has a wide range of temperatures, though the extremes are rare.<ref name=WRCC/> The highest was recorded on July 29, 1898, in [[Hermiston, Oregon]], and again on August 10, 1898, in both [[Pendleton, Oregon]] and [[Redmond, Oregon]], and once more on [[2021 Western North America heat wave|June 29, 2021]], at [[Pelton Dam]]. All are east of the Cascades, when the temperature reached {{convert|119|F|C}}.{{sfn|Taylor|Hannan|1999|p=xii}} The lowest occurred on February 9, 1933, in [[Ukiah, Oregon|Ukiah]], and again on February 10, 1933, in [[Seneca, Oregon|Seneca]], also both east of the Cascades, when the temperature dropped to {{convert|-54|F|C}}.{{sfn|Taylor|Hannan|1999|p=xii}} The temperature in the [[Willamette Valley]] is mild compared to the desert regions of the state, with high temperatures at or above {{convert|90|F|C}} occurring only five to fifteen times per year, and low temperatures below {{convert|30|F|C}} similarly infrequent.<ref>{{cite web|url=http://www.ocs.orst.edu/county_climate/Multnomah_files/Multnomah.html|title=Climate of Multnomah County|author=Taylor, George, Cadee Hale and Sarah Joos|publisher=[[Oregon State University]]|access-date=2010-04-16|archive-url=https://web.archive.org/web/20100624153919/http://www.ocs.orst.edu/county_climate/Multnomah_files/Multnomah.html|archive-date=2010-06-24|url-status=dead}}</ref> The hottest area of the state is the southwest; [[Jackson County, Oregon|Jackson County]] is the warmest place in the state during summer.<ref>{{cite web|url=http://ocs.oregonstate.edu/county_climate/Jackson_files/Jackson.html|title=Climate of Jackson County|author=Taylor, George, Cadee Hale and Sarah Joos|publisher=[[Oregon State University]]|access-date=2010-04-16|archive-url=https://web.archive.org/web/20100304143656/http://www.ocs.oregonstate.edu/county_climate/Jackson_files/Jackson.html|archive-date=2010-03-04|url-status=dead}}</ref> |
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{{Weatherbox |
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| single line = Y |
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| location = Oregon |
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| Jan record high F = 82 |
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| Feb record high F = 89 |
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| Mar record high F = 99 |
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| Apr record high F = 102 |
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| May record high F = 108 |
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| Jun record high F = 119 |
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| Jul record high F = 119 |
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| Aug record high F = 119 |
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| Sep record high F = 111 |
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| Oct record high F = 104 |
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| Nov record high F = 89 |
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| Dec record high F = 81 |
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| year record high F = 119 |
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| Jan record low F = -52 |
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| Feb record low F = -54 |
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| Mar record low F = -30 |
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| Apr record low F = -23 |
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| May record low F = 0 |
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| Jun record low F = 11 |
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| Jul record low F = 14 |
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| Aug record low F = 13 |
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| Sep record low F = 2 |
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| Oct record low F = -11 |
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| Nov record low F = -32 |
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| Dec record low F = -53 |
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| year record low F = -54 |
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| source = https://www.factmonster.com/math-science/weather/oregon-temperature-extremes |
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}} |
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==Selected climate charts== |
==Selected climate charts== |
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{{Location map~ |
{{Location map~ |
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|Oregon |
|Oregon |
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| label = [[Medford |
| label = [[Medford Oregon|Medford]] |
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| label_size = 75 |
| label_size = 75 |
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| mark = purple pog.svg |
| mark = purple pog.svg |
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{{nowrap| |
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{{climate chart|[[Astoria, Oregon|Astoria]] |
{{climate chart|[[Astoria, Oregon|Astoria]] |
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|37.7|49.8|10.20 |
|37.7|49.8|10.20 |
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{{ |
{{Clear}} |
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{{climate chart|[[Medford, Oregon|Medford]] |
{{climate chart|[[Medford, Oregon|Medford]] |
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|32|48|2.42 |
|32|48|2.42 |
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{{Clear}} |
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==See also== |
==See also== |
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*[[Climate of the United States]] |
*[[Climate of the United States]] |
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*[[Climate change in Oregon]] |
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==References== |
==References== |
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===Works cited=== |
===Works cited=== |
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*{{cite book|editor=Loy, William G.|last=Allan|first=Stuart|last2=Buckley|first2=Aileen R.|last3=Meacham|first3=James E.|title=Atlas of Oregon|edition=2nd|publisher=University of Oregon Press|location=Eugene|year=2001|isbn=0-87114-101-9 |
*{{cite book|editor=Loy, William G.|last=Allan|first=Stuart|last2=Buckley|first2=Aileen R.|last3=Meacham|first3=James E.|title=Atlas of Oregon|edition=2nd|publisher=University of Oregon Press|location=Eugene|year=2001|isbn=0-87114-101-9}} |
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* {{cite book|last=Taylor|first=George H.|last2=Hannan|first2=Chris|year=1999|title=The Climate of Oregon: From Rain Forest to Desert|location=Corvallis|publisher=Oregon State University Press|isbn=978-0-87071-468-9 |
* {{cite book|last=Taylor|first=George H.|last2=Hannan|first2=Chris|year=1999|title=The Climate of Oregon: From Rain Forest to Desert|location=Corvallis|publisher=Oregon State University Press|isbn=978-0-87071-468-9}} |
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{{Oregon}} |
{{Oregon}} |
Latest revision as of 01:50, 5 August 2024
According to the Köppen climate classification, most of Western Oregon has a warm-summer Mediterranean climate (or Csb type), which features warm, dry summers, and wet winters with frequent overcast and cloudy skies. Eastern Oregon falls into the cold semi-arid climate (or BSk type), which features drier weather.
West of the Cascade Range, winters are chilly with frequent rain and occasional snow. Temperatures can get very cold, but only occasionally, as the result of Arctic cold waves. The high desert region of the state is much drier, with less rain, more snow, colder winters, and hotter summers.[1]
Precipitation
[edit]Precipitation in the state varies widely: some western coastal slopes approach 200 inches (5,100 mm) annually, while the driest places, such as the Alvord Desert (in the rain shadow of Steens Mountain) in eastern Oregon, get as little as 5 inches (130 mm).[2][3]
The Pacific Ocean, the moisture-laden air above it, and the storms moving from it over the Oregon coast, are major factors in the state's precipitation patterns. As humid ocean air flows east from the ocean and encounters the Coast Range, it rises steeply, cools, and loses moisture through condensation, which produces heavy rain. The heaviest precipitation in the state occurs at 2,000 to 4,000 feet (610 to 1,220 m) above sea level in these coastal mountains. At lower elevations along the coast, orographic precipitation is less intense but still produces 60 to 80 inches (1,500 to 2,000 mm) a year.[2]
In the Willamette Valley east of the Coast Range, storms "blowing" from the Pacific retain enough moisture to drop from 35 to 45 inches (890 to 1,140 mm) annually in the most heavily populated part of the state. East of the valley, the storm air rises again as it meets the Cascade Range, cooling once more and forming condensate at elevations often as low as 3,000 feet (910 m).[2] Since volcanic peaks in the range are quite high—more than 11,000 feet (3,400 m) in the case of Mount Hood[4]—most of the remaining Pacific moisture falls here in the form of rain or snow.[2]
The remaining two-thirds of the state is relatively dry, classified as semi-arid, with large areas receiving no more than 12 inches (300 mm) a year. Exceptions occur at higher elevations in the Blue Mountains and the Wallowa Mountains to the northeast, which get 50 to 80 inches (1,300 to 2,000 mm) a year.[2]
Across Oregon, the wet season runs from November through March, when the jet stream is strongest in the Northern Hemisphere. Precipitation is less in the months between winter and summer: April through June in the spring and September and October in the fall. Statewide, the dry months are July and August, when moisture arrives during afternoon thunderstorms, mainly in the mountains, and less often from storms that reach the north coast and adjacent counties.[5]
Snow
[edit]Snowfall in Oregon is greatest in the Cascade Range. Based on data from ski resorts and a few official weather stations, average annual snowfall in the Cascades can range from 300 to 550 inches (760 to 1,400 cm).[3] The state's largest annual snowfall on record, 903 inches (2,290 cm), occurred at Crater Lake in the Cascades in 1950.[6] In the Blue Mountains of eastern Oregon, snowfall totals can also be large, between 150 and 300 inches (380 and 760 cm). On the other hand, most winter precipitation in the Coast Range falls as rain, though heavy snow sometimes occurs.[3]
In most mountain areas in Oregon, the ground above 4,500 feet (1,400 m) is covered with snow from December through April. Snow depths, which vary with elevation and time of year, average an estimated 50 to 100 inches (130 to 250 cm) in the Cascades and 25 to 65 inches (64 to 165 cm) in the Blue Mountains at the end of January; by the end of April, they diminish to 40 to 120 inches (100 to 300 cm) in the Cascades and 5 to 45 inches (13 to 114 cm) in the Blues. Glaciers remain year-round on some Cascade peaks higher than 7,000 feet (2,100 m) above sea level.[3]
Annual snowfall along the coastal plain averages 1 to 3 inches (2.5 to 7.6 cm) a year, including years with none. Further inland, between the Coast Range and the Cascades, snowfall generally averages from 5 to 10 inches (13 to 25 cm) a year. East of the Cascades, in non-mountain settings, the annual totals range from 15 to 75 inches (38 to 191 cm), depending on location; they are smallest in the north-central region and the Snake River basin in the southeast and largest in the northeastern valleys and in the high plateaus of the south-central part of the state.[3]
Temperature
[edit]In addition to seasonal cycles in solar radiation (more in summer, less in winter), major factors affecting temperatures in Oregon include the moderating influence of the Pacific Ocean combined with variations in surface elevation, especially the Cascade Range. In general, temperatures on Earth drop by about 4 °F (2 °C) per each 1,000 feet (300 m) increase in elevation. Throughout the year, high elevations across the state tend to be cooler than low elevations. In addition, the Cascades, running north–south from border to border, generally retain relatively warm Pacific air masses on the western side of the state and relatively cool continental air masses on the eastern side. This prevailing pattern breaks down occasionally when dense cold air flows down the Columbia Gorge into the Willamette Valley and lowers temperatures more than usual from Portland to Eugene.[7]
Oregon has a wide range of temperatures, though the extremes are rare.[3] The highest was recorded on July 29, 1898, in Hermiston, Oregon, and again on August 10, 1898, in both Pendleton, Oregon and Redmond, Oregon, and once more on June 29, 2021, at Pelton Dam. All are east of the Cascades, when the temperature reached 119 °F (48 °C).[6] The lowest occurred on February 9, 1933, in Ukiah, and again on February 10, 1933, in Seneca, also both east of the Cascades, when the temperature dropped to −54 °F (−48 °C).[6] The temperature in the Willamette Valley is mild compared to the desert regions of the state, with high temperatures at or above 90 °F (32 °C) occurring only five to fifteen times per year, and low temperatures below 30 °F (−1 °C) similarly infrequent.[8] The hottest area of the state is the southwest; Jackson County is the warmest place in the state during summer.[9]
Climate data for Oregon | |||||||||||||
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Month | Jan | Feb | Mar | Apr | May | Jun | Jul | Aug | Sep | Oct | Nov | Dec | Year |
Record high °F (°C) | 82 (28) |
89 (32) |
99 (37) |
102 (39) |
108 (42) |
119 (48) |
119 (48) |
119 (48) |
111 (44) |
104 (40) |
89 (32) |
81 (27) |
119 (48) |
Record low °F (°C) | −52 (−47) |
−54 (−48) |
−30 (−34) |
−23 (−31) |
0 (−18) |
11 (−12) |
14 (−10) |
13 (−11) |
2 (−17) |
−11 (−24) |
−32 (−36) |
−53 (−47) |
−54 (−48) |
Source: https://www.factmonster.com/math-science/weather/oregon-temperature-extremes |
Selected climate charts
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Ontario | ||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
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See also
[edit]References
[edit]- ^ Lew, Allen A. (2004). "The Pacific Coast". Northern Arizona University. Archived from the original on May 31, 2009. Retrieved April 16, 2010.
- ^ a b c d e Allan, Buckley & Meacham 2001, pp. 154–55.
- ^ a b c d e f Western Regional Climate Center. "Climate of Oregon". Desert Research Institute. Archived from the original on December 21, 2016. Retrieved April 16, 2010.
- ^ Allan, Buckley & Meacham 2001, pp. 130–31.
- ^ Allan, Buckley & Meacham 2001, pp. 156–57.
- ^ a b c Taylor & Hannan 1999, p. xii.
- ^ Allan, Buckley & Meacham 2001, pp. 158–59.
- ^ Taylor, George, Cadee Hale and Sarah Joos. "Climate of Multnomah County". Oregon State University. Archived from the original on 2010-06-24. Retrieved 2010-04-16.
{{cite web}}
: CS1 maint: multiple names: authors list (link) - ^ Taylor, George, Cadee Hale and Sarah Joos. "Climate of Jackson County". Oregon State University. Archived from the original on 2010-03-04. Retrieved 2010-04-16.
{{cite web}}
: CS1 maint: multiple names: authors list (link)
Works cited
[edit]- Allan, Stuart; Buckley, Aileen R.; Meacham, James E. (2001). Loy, William G. (ed.). Atlas of Oregon (2nd ed.). Eugene: University of Oregon Press. ISBN 0-87114-101-9.
- Taylor, George H.; Hannan, Chris (1999). The Climate of Oregon: From Rain Forest to Desert. Corvallis: Oregon State University Press. ISBN 978-0-87071-468-9.