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A low-pressure area developed into a tropical depression southeast of [[Taiwan]] early on August 31.<ref>{{cite web|title=Marine Weather Warning for GMDSS Metarea XI 2016-08-31T00:00:00Z|url=http://www.wis-jma.go.jp/cms/warning/2016/08/31/marine-weather-warning-for-gmdss-metarea-xi-2016-08-31t000000z/|website=WIS Portal – GISC Tokyo|publisher=Japan Meteorological Agency|accessdate=August 31, 2016|date=August 31, 2016}}</ref> {{cn span|On the next day, the system further developed into a tropical depression and was designated 15W. It later continued to intensify while over the Taiwan Strait and was assigned the name ''Namtheun'' upon reaching tropical storm intensity.|date=September 2016}} On the same day, PAGASA started to monitor the said weather disturbance and assigned it the local name ''Enteng''.<ref>{{cite web|title='Enteng' Now a tropical storm|url=http://www.gmanetwork.com/news/story/579746/scitech/weather/enteng-now-a-tropical-storm-pagasa|publisher=GMA Network.com|accessdate=September 2, 2016|date=September 1, 2016}}</ref>
A low-pressure area developed into a tropical depression southeast of [[Taiwan]] early on August 31.<ref>{{cite web|title=Marine Weather Warning for GMDSS Metarea XI 2016-08-31T00:00:00Z|url=http://www.wis-jma.go.jp/cms/warning/2016/08/31/marine-weather-warning-for-gmdss-metarea-xi-2016-08-31t000000z/|website=WIS Portal – GISC Tokyo|publisher=Japan Meteorological Agency|accessdate=August 31, 2016|date=August 31, 2016}}</ref> {{cn span|On the next day, the system further developed into a tropical depression and was designated 15W. It later continued to intensify while over the Taiwan Strait and was assigned the name ''Namtheun'' upon reaching tropical storm intensity.|date=September 2016}} On the same day, PAGASA started to monitor the said weather disturbance and assigned it the local name ''Enteng''.<ref>{{cite web|title='Enteng' Now a tropical storm|url=http://www.gmanetwork.com/news/story/579746/scitech/weather/enteng-now-a-tropical-storm-pagasa|publisher=GMA Network.com|accessdate=September 2, 2016|date=September 1, 2016}}</ref>
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Revision as of 23:01, 8 September 2016

2016 Pacific typhoon season
Season summary map
Seasonal boundaries
First system formedMay 26, 2016
Last system dissipatedSeason ongoing
Strongest storm
NameNepartak
 • Maximum winds205 km/h (125 mph)
(10-minute sustained)
 • Lowest pressure900 hPa (mbar)
Seasonal statistics
Total depressions31
Total storms13
Typhoons4
Super typhoons1 (unofficial)
Total fatalities187
Total damage$1.9 billion (2016 USD)
Pacific typhoon seasons
2014, 2015, 2016, 2017, 2018

The 2016 Pacific typhoon season is an event in the annual cycle of tropical cyclone formation, in which tropical cyclones form in the western Pacific Ocean. The season runs throughout 2016, though most tropical cyclones typically develop between May and October. The scope of this article is limited to the Pacific Ocean to the north of the equator between 100°E and 180th meridian. Within the northwestern Pacific Ocean, there are two separate agencies that assign names to tropical cyclones which can often result in a cyclone having two names. The Japan Meteorological Agency (JMA) will name a tropical cyclone should it be judged to have 10-minute sustained wind speeds of at least 65 km/h (40 mph) anywhere in the basin, whilst the Philippine Atmospheric, Geophysical and Astronomical Services Administration (PAGASA) assigns names to tropical cyclones which move into or form as a tropical depression in their area of responsibility located between 135°E and 115°E and between 5°N–25°N regardless of whether or not a tropical cyclone has already been given a name by the JMA. Tropical depressions that are monitored by the United States' Joint Typhoon Warning Center (JTWC) are given a number with a "W" suffix.

The first system formed on May 26, making it the fifth latest start for a Pacific typhoon season in the satellite era; only the 1973, 1983, 1984 and 1998 seasons started later. However, the first named tropical storm, Nepartak, did not develop until July 3, making it the second latest season for a named storm to develop. Nepartak's naming tied the record 199-day period (from December 17, 2015 to July 2, 2016) in which no named storm was active within the basin (1997–98).[1]

Seasonal forecasts

TSR forecasts
Date
Tropical
storms
Total
Typhoons
Intense
TCs
ACE Ref
Average (1965–2015) 26 16 9 298 [2]
May 7, 2016 22 13 6 217 [2]
July 6, 2016 22 13 7 239 [3]
August 8, 2016 22 13 7 231 [4]
Other forecasts
Date
Forecast
Center
Period Systems Ref
January 8, 2016 PAGASA January — March 1–2 tropical cyclones [5]
January 8, 2016 PAGASA April — June 1–3 tropical cyclones [5]
June 28, 2016 CWB January 1 — December 31 19–23 tropical storms [6]
July 15, 2016 PAGASA July — September 5–11 tropical cyclones [7]
July 15, 2016 PAGASA October — December 4–9 tropical cyclones [7]
Forecast
Center
Tropical
cyclones
Tropical
storms
Typhoons Ref
Actual activity: JMA 31 13 4
Actual activity: JTWC 16 12 4
Actual activity: PAGASA 5 4 2

During the year several national meteorological services and scientific agencies forecast how many tropical cyclones, tropical storms, and typhoons will form during a season and/or how many tropical cyclones will affect a particular country. These agencies included the Tropical Storm Risk (TSR) Consortium of the University College London, PAGASA and Taiwan's Central Weather Bureau. Some of the forecasts took into consideration what happened in previous seasons and the El Niño conditions that were observed during the previous year. The first forecast of the year was released by PAGASA during January 2016, within its seasonal climate outlook for the period January – June.[5] The outlook noted that one to two tropical cyclones were expected between January and March, while one to three were expected to develop or enter the Philippine Area of Responsibility between April and June.[5]

During March the Hong Kong Observatory predicted that the typhoon season in Hong Kong, would be near normal with four to seven tropical cyclones passing within 500 km (310 mi)* of the territory compared to an average of six.[8] On May 7, Tropical Storm Risk issued its first forecast for the season and predicted that it will be a quiet season, with 22 tropical storms, 13 typhoons, and 6 intense typhoons developing during the year, while an ACE Index of 217 was also forecast.[2] Ahead of the Thailand rainy season starting during May, the Thai Meteorological Department predicted that two tropical cyclones would move near Thailand during 2016.[9] They predicted that there was a high chance that the first tropical cyclone, would move past northern and north-eastern Thailand during August or September.[9] The second tropical cyclone was predicted to move past Southern Thailand during October and November.[9] On June 28, Taiwan's Central Weather Bureau predicted that between 19–23 tropical storms would develop over the basin, while two — four systems were expected to affect Taiwan itself.[6]

On July 6, TSR released their second forecast for the season. They predicted mostly the same numbers as the previous forecast, but raised the number of intense typhoons to 7.[3] PAGASA issued their second and final forecast for the year on July 15, within its seasonal climate outlook for the period July – December.[7] The outlook noted that 5–11 tropical cyclones were expected between July and September, while four to nine were expected to develop or enter the Philippine Area of Responsibility between October and December.[7] TSR issued their final forecast for the season on August 8, sustaining the tropical cyclone numbers, however its ACE was slightly lowered than the previous forecast.[4]

Season summary

The season had a late start, as the first tropical system developed on May 26 after six months of inactivity, making it the fifth latest season for a system to form. Four seasons started later - the 1973, 1983, 1984 and 1998 seasons. Tropical activity throughout the basin became marginally favorable for development, and two tropical depressions developed during June. On July 3, Nepartak became a tropical storm, making it the second-latest first named storm on record.[citation needed] Nepartak's naming tied the record 199-day period (from December 17, 2015 to July 2, 2016) in which a named storm was inactive within the basin (with 1997–98, from December 22, 1997 to July 8, 1998).[1] The season became significantly more active in July with seven depressions and four named storms in the month.[citation needed]

By the end of August, three storms had hit the Japanese island of Hokkaidō, the most since 1951.[10]

Storms

Tropical Depression 01W

Tropical depression (JMA)
Tropical depression (SSHWS)
 
DurationMay 26 – May 27
Peak intensity45 km/h (30 mph) (1-min);
998 hPa (mbar)

During May 26, Tropical Depression 01W developed over the northern South China Sea, about 600 km (375 mi)* to the south of Hong Kong, China.[11][12] The system subsequently moved north-westwards and slightly developed further, before it made landfall near Yangjiang in Guangdong, China during the next day.[12] The system subsequently quickly weakened and degenerated into an area of low pressure during May 27.[12]

The system brought squally and heavy rain to the Pearl River Delta, including parts of Hong Kong, Macau and Guangdong province, where a bridge was destroyed by flooding and two people were injured.[12][13] At the Macau Ferry Terminal, two passengers were injured as a vessel collided with the terminal, while there was no significant damage reported within Hong Kong.[12]

Tropical Depression Ambo

Tropical depression (JMA)
 
DurationJune 26 – June 28
Peak intensity55 km/h (35 mph) (10-min);
1002 hPa (mbar)

Early on June 26, the JMA and PAGASA reported that Tropical Depression Ambo had developed over the Philippine Sea, about 555 km (345 mi)* to the east of Manila on the island of Luzon in the Philippines.[14][15] The system was located within an environment that was thought to be favourable for further development, with low vertical wind shear and a fair outflow.[16] However, the depression's broad low level circulation centre was moving north-westwards quickly, which meant that the circulation's southern edge could not close off and was exposed.[16] The system subsequently made landfall on Luzon in Philippines later that day, where according to PAGASA it quickly weakened into a low pressure area.[17] However, the JMA continued to monitor the system as a tropical depression throughout June 27, as it emerged into an unfavourable environment for further development in the South China Sea.[18][19] The depression subsequently made landfall on China's Guangdong Province, before it was last noted during June 28, as it dissipated over land.[18] Several sea-trips in the Philippine island province of Catanduanes were cancelled with a total of seven passengers, three rolling cargoes and a sea vessel stranded at the port of Virac.[20]

Typhoon Nepartak (Butchoy)

Violent typhoon (JMA)
Category 5 super typhoon (SSHWS)
 
DurationJuly 2 – July 10
Peak intensity205 km/h (125 mph) (10-min);
900 hPa (mbar)

During the evening of June 30 the JMA began monitoring an area of low pressure over the eastern Caroline Islands.[21] Over the next few days the area of disturbed weather became further organised, and by July 1 it had developed a closed circulation.[22] The JMA upgraded the low pressure area into a tropical depression early on July 2.[23] Under the influence of weak steering currents and warm waters the system moved slowly northwestward. By July 3 the JMA analyzed the depression as a tropical storm and gave it the name Nepartak.[24] During July 3 a tropical upper tropospheric trough (TUTT) to the north of the system moved towards the west, allowing conditions in the immediate area of Nepartak to become more favourable, facilitating steady intensification.[25] Microwave imagery revealed an eye had developed within deep convection late on July 4, leading the JMA and JTWC to upgrade Nepartak to a typhoon soon thereafter on July 5.[26][27] On the same day, PAGASA reported that Nepartak had entered its area of responsibility and assigned it the local name Butchoy.[28][29]

Two people drowned on July 7 after being washed out to sea by strong winds in Taiwan.[30]

Tropical Depression 03W

Tropical depression (JMA)
Tropical depression (SSHWS)
 
DurationJuly 15 – July 20
Peak intensity45 km/h (30 mph) (1-min);
1006 hPa (mbar)

During July 14, a tropical disturbance developed about 400 km (250 mi)* to the west-northwest of Guam.[31] At this time atmospheric convection surrounding the system was flaring, over the system's weak but developing low level circulation center.[31] However, as a subtropical ridge of high pressure extended a significant amount of dry air over the disturbance, conditions were assessed to be marginally favorable for further development of the system.[31] Over the next couple of days the system gradually developed further as it moved north-westwards and was classified as a tropical depression by the JMA during July 15.[32][33] After the system had consolidated further, it was classified as Tropical Depression 03W by the JTWC during July 17.[34] However, the system weakened during that day as it moved polewards, along the western edge of the subtropical ridge of high pressure, into an area of increasing vertical windshear.[34] As a result, the JTWC expected the system to quickly dissipate and issued their final advisory later that day.[35] However, over the next couple of days the system continued to move northwards and impacted the Ryukyu Islands, before it was last noted by the JMA during July 20.[36][37]

Tropical Storm Lupit

Tropical storm (JMA)
Tropical storm (SSHWS)
 
DurationJuly 22 – July 24
Peak intensity75 km/h (45 mph) (10-min);
1000 hPa (mbar)

During July 21, a subtropical disturbance developed at the tailend of a mid-latitude trough of low pressure, about 775 km (480 mi)* to the east of Iwo-To.[38] Over the next day, deep atmospheric convection developed over the system's elongated low level circulation, before it was classified as a tropical depression by the JMA during July 22.[38][39] Over the next day, as the storm moved north-northeastwards around a subtropical ridge of high pressure, its structure improved as it developed a warm core and consolidated.[40] The hybrid system was subsequently classified as Tropical Storm 04W by the JTWC during July 23, before the JMA named it Lupit later that day.[39][40] Over the next day, Lupit peaked with sustained winds of 75 km/h (47 mph), as it went through an extratropical transition and took on frontal characteristics.[39][41] Lupit subsequently became extratropical during July 24, before it dissipated during July 26, as it moved into the Sea of Okhotsk.[39]

Severe Tropical Storm Mirinae

Severe tropical storm (JMA)
Tropical storm (SSHWS)
 
DurationJuly 25 – July 29
Peak intensity100 km/h (65 mph) (10-min);
980 hPa (mbar)

Mirinae was first noted as a tropical depression during July 25, as it moved off the west coast of Luzon into the South China Sea, about 300 km (185 mi)* to the east of the Paracel Islands.[42][43] The system's well defined low level circulation centre was located in a very favourable environment for further development, with low vertical windshear and very warm sea surface temperatures.[43][44] Later that day the JTWC initiated advisories on the system and classified it as Tropical Depression 05W, as it moved north-westwards along the periphery of a subtropical ridge of high pressure.[44] During the next day, as the system moved west-northwestwards, it continued to intensify was named Mirinae by the JMA after it had become a tropical storm.[42][45] Mirinae subsequently weakened slightly as it made landfall later that day, near Wanning and crossed Hainan Island, before it re-intensified as it had moved into the Gulf of Tonkin.[42][46] The system was classified as a severe tropical storm by the JMA during July 27, as it was estimated that Mirinae had peaked with sustained wind-speeds of 95 km/h (59 mph).[37][47] The system subsequently made landfall about 110 km (70 mi)* to the south of Hanoi in northern Vietnam later that day.[42][48] Mirinae subsequently weakened gradually over northern Vietnam, before it was last noted during July 28, as it dissipated to the north of Hanoi.[37][42]

By July 29, the storm had left five people dead and five others missing. Severe damage to infrastructure was reported in Northern Vietnam, with damage to power lines causing blackouts and power cuts in some areas. Mirinae also sank 12 boats, destroyed the roofs of 1,425 houses and uprooted about 5,000 trees.[49]

Severe Tropical Storm Nida (Carina)

Severe tropical storm (JMA)
Category 1 typhoon (SSHWS)
 
DurationJuly 29 – August 3
Peak intensity110 km/h (70 mph) (10-min);
975 hPa (mbar)

By July 28, the JMA had upgraded a low-pressure area east of the Philippines to a tropical depression.[50] During the next day, PAGASA started to track the system and named it Carina. Late on July 29, the Joint Typhoon Warning Center upgraded the system into a tropical storm, with the JMA following suit, naming it Nida.[citation needed]

Severe Tropical Storm Omais

Severe tropical storm (JMA)
Tropical storm (SSHWS)
 
DurationAugust 3 – August 9
Peak intensity110 km/h (70 mph) (10-min);
975 hPa (mbar)

During August 3, the JMA reported that a tropical depression had developed about 675 km (420 mi)* to the north-northeast of Guam. Over the next day, the system moved towards the northwest within a favorable environment for further development, before the JTWC issued a tropical cyclone formation alert on the system during August 4. At the same time, they classified the system as a monsoon depression, with bands of atmospheric convection to the south and southeast of the system's ill-defined and broad center. During that day, the JMA named the depression Omais as the system transitioned from being monsoon depression into a tropical storm. As a result of this transition, the JTWC initiated advisories on the system and classified it as Tropical Storm 07W.[citation needed]

Severe Tropical Storm Conson

Severe tropical storm (JMA)
Tropical storm (SSHWS)
 
DurationAugust 7 – August 15
Peak intensity95 km/h (60 mph) (10-min);
985 hPa (mbar)

On August 7, the JMA started to monitor a tropical depression west of Wake Island.[51] During the next day, the JTWC followed suit, and gave the identifier 08W.[52] Satellite imagery showed that 08W was located in a region of warm sea surface temperatures, causing the formation of a deep formative banding to its LLCC.[53] Later that day, the JMA upgraded 08W to a tropical storm, naming it Conson.[54] Despite some moderate wind shear, Conson slowly intensified and later reached severe tropical storm strength on August 10.[55][56] The JTWC later stated that deep convection was forming near the center of Conson,[57] however shortly thereafter, convection became disorganized.[58]

By August 11, convection once re-intensified again, however its LLCC became exposed, causing the JTWC to lower its intensity to lower-end of tropical storm strength.[59] The JMA also downgraded Conson to a tropical storm.[60] During the next day, satellite image showed that the convective structure of Conson was beginning to deteriorate as it started to interact with drier air, suppressing convection.[61] The center of Conson became much broader and exposed early on August 13.[62] While moving northwestward, Conson became better defined than before, however its convection was more shallow as it started to interact will cooler sea-surface temperatures and drier air.[63] By August 14, the JTWC issued their final warning on Conson as it started to undergo its extratropical transition with a result of a strong wind shear and the interaction of the mid-latitude baroclinic zone.[64][65] The JMA tracked Conson until it fully transitioned into an extratropical cyclone on August 15 and made landfall near Nemuro Peninsula.[66]

Severe Tropical Storm Chanthu

Severe tropical storm (JMA)
Tropical storm (SSHWS)
 
DurationAugust 11 – August 17
Peak intensity100 km/h (65 mph) (10-min);
980 hPa (mbar)

During August 11, the JMA started to track a tropical depression, whereas the JTWC issued a Tropical Cyclone Formation Alert, as it was located about 695 km (432 mi) west-northwest of Guam.[67][68] After meandering eastwards, the JTWC designates the system as 09W, while the JMA immediately upgraded 09W to a tropical storm, with the naming of Chanthu on August 13.[69][70] The JTWC followed suit early on August 14.[71] With an improving LLCC, Chanthu rapidly developed into a severe tropical storm from the JMA,[72][73] as it was later located over in an area of favorable environments of strengthening.[74] Despite a high chance of strengthening and a well-defined LLCC, Chanthu stopped generating convection as the JMA downgraded it to a tropical storm.[75][76]

Later that day, flaring convection was associated with its LLCC as it was beginning its extratropical transition while interacting with mid-latitude flow.[77] Therefore, early on August 17, Chanthu once again reached severe tropical strom strength as it attained its peak intensity with a minimal pressure of 980 millibars (28.94 inHg), while east of the Japanese archipelago of Honshu.[78] Shortly thereafter, the JTWC issued its final warning on Chanthu.[79] The JMA issued its final warning a few hours later as it made landfall over Cape Erimo of Hokkaido, Japan, at peak intensity.[80]

Tropical Storm Dianmu

Tropical storm (JMA)
Tropical storm (SSHWS)
 
DurationAugust 15 – August 19
Peak intensity75 km/h (45 mph) (10-min);
985 hPa (mbar)

During August 15, the JMA reported that a tropical depression, had developed about 205 km (125 mi)* to the southeast of Hong Kong.[81] The system meandered slowly westward until the JTWC issued a Tropical Cyclone Formation Alert (TCFA) on August 17.[82] By August 18, the JMA upgraded the depression to a tropical storm, prompting to name it as Dianmu.[83] Shortly thereafter, the JTWC began issuing advisories, classifying it as a tropical depression with the identifier of 11W.[84] During the course of the day, enhanced satellite imagery showed that Dianmu was rapidly organizing with deep flaring convection surrounding its LLCC.[85] Due to warm sea-surface temperatures with a compact microwave eye feature seen from satellite imagery, the JTWC upgraded Dianmu to a tropical storm.[86] However the JTWC issued its final warning on Dianmu as it made landfall over in Haiphong and Thái Bình Province in northern Vietnam.[87][88] The JMA stopped issuing warnings on Dianmu on midday of August 19 as it was located inland.[89]

In the province of Hainan, China, Dianmu's heavy rains brought the water level at the Longtang Dam on the Nandu River to a ten-year high of 13.35 metres. Hainan's capital, Haikou, experienced flooding in some areas. Over in Quang Ninh, a total of 11 houses were collapsed and total damages in the city amounted to 3.5 billion VND (US$157 thousand).[90]

Typhoon Lionrock (Dindo)

Very strong typhoon (JMA)
Category 4 typhoon (SSHWS)
 
DurationAugust 16 – August 30
Peak intensity165 km/h (105 mph) (10-min);
940 hPa (mbar)

The JMA upgraded a low-pressure area to a tropical depression about 690 km (430 mi) northwest of Wake Island on August 16.[91]

Typhoon Mindulle

Typhoon (JMA)
Tropical storm (SSHWS)
 
DurationAugust 17 – August 23
Peak intensity120 km/h (75 mph) (10-min);
975 hPa (mbar)

A tropical depression formed northwest of Guam on August 17.[92]

Tropical Storm Kompasu

Tropical storm (JMA)
Tropical storm (SSHWS)
 
DurationAugust 18 – August 21
Peak intensity65 km/h (40 mph) (10-min);
994 hPa (mbar)

Although the JMA stopped monitoring on a separate previous system, the agency started to monitor the same tropical depression again in the afternoon of August 18.[93] The JTWC started issuing advisories by the next day as it was immediately classified as a tropical storm and the identifier of 13W.[94] The JMA followed suit early on August 20, and was named Kompasu.[95] Despite wind shear and an exposed LLCC, tightly curved banding was reported embedded within the northern extent of a very broad "monsoon gyre" circulation.[96] Both agencies reported that Kompasu had reached its peak strength as a minimal tropical storm with a minimum barometric pressure of about 994 mbar.[97] Later that day, deep convection of Kompasu had rapidly decreased as it was located in marginally favorable environments with low wind shear and sea-surface temperatures of about 26 degrees Celsius.[98] On August 21, the JTWC downgraded Kompasu to a tropical depression and issued their final bulletin on the system.[99] The JMA did the same and issued its final advisory on Kompasu as it transitioned into an extratropical system.[100]

Floods in Hokkaidō killed one person when a driver was stranded in his flooded car.[101]

Tropical Depression 14W

Tropical depression (JMA)
Tropical depression (SSHWS)
 
DurationAugust 23 – August 24
Peak intensity55 km/h (35 mph) (10-min);
1000 hPa (mbar)

Typhoon Namtheun (Enteng)

Typhoon (JMA)
Category 3 typhoon (SSHWS)
 
DurationAugust 31 – September 5
Peak intensity140 km/h (85 mph) (10-min);
955 hPa (mbar)

A low-pressure area developed into a tropical depression southeast of Taiwan early on August 31.[102] On the next day, the system further developed into a tropical depression and was designated 15W. It later continued to intensify while over the Taiwan Strait and was assigned the name Namtheun upon reaching tropical storm intensity.[citation needed] On the same day, PAGASA started to monitor the said weather disturbance and assigned it the local name Enteng.[103]

Tropical Storm Malou

Tropical storm (JMA)
 
DurationSeptember 5 – September 7
Peak intensity75 km/h (45 mph) (10-min);
1000 hPa (mbar)

The JMA upgraded a low-pressure area to a tropical depression over Okinawa on September 5.[104]

Tropical Depression 16W

Tropical depression (JMA)
Tropical depression (SSHWS)
 
DurationSeptember 8 – Present
Peak intensity45 km/h (30 mph) (1-min);
1006 hPa (mbar)

Other storms

On June 23, the JMA started to monitor a tropical depression about 650 km west-southwest of Manila, Philippines. The depression briefly continued moving in a slow westward direction until it became stationary over in the South China Sea. Due to unfavorable environments, the JMA stopped tracking the depression on June 25.[citation needed] However, its remnants caused heavy rainfall in Central and Southern Vietnam.[105] Late on July 27, the JMA very briefly monitored a weak tropical depression south of Japan.[106] The JMA also indicated that a tropical depression had formed southeast of Japan in the afternoon on July 28, however it was downgraded to a low-pressure area early on the next day.[50][107] The JMA upgraded a low-pressure area east of Taiwan to a tropical depression on August 6.[108] The system made landfall over eastern China on August 9. On August 10, the JMA reported that a tropical depression had developed, about 300 km (185 mi)* to the southeast of Ishigaki Island.[109][110] Over the next day the system moved north-westwards, within a marginal environment for further development, before it passed over northern Taiwan and moved into the East China Sea.[110][111][112] The system subsequently continued moved westwards, before it was last noted as it made landfall on southern China later that day.[113]

During August 12 a tropical depression developed near the coast of Taiwan, about 160 km (100 mi)* to the southeast of Taipei.[114] The system subsequently made landfall on the island nation, before it was last noted during the next day as it dissipated over Taiwan.[115] A tropical depression briefly appeared over the Gulf of Tonkin early on August 16.[116] A tropical depression persisted east of the Northern Mariana Islands in the afternoon of August 17.[92] The system was last noted early on the next day and led to the formation of Tropical Storm Kompasu.[117] During August 24, two tropical depressions briefly developed; one in the South China Sea, and one over to the northeast of the Mariana Islands.[118] However, the system over the South China Sea briefly developed into a tropical depression twice on August 25 and 27.[citation needed] A tropical depression formed north of Wake Island early on August 30, and it became extratropical on the next day.[119][120]

Storm names

Within the Northwest Pacific Ocean, both the Japan Meteorological Agency (JMA) and the Philippine Atmospheric, Geophysical and Astronomical Services Administration (PAGASA) assign names to tropical cyclones that develop in the Western Pacific, which can result in a tropical cyclone having two names.[121] The Japan Meteorological Agency's RSMC Tokyo — Typhoon Center assigns international names to tropical cyclones on behalf of the World Meteorological Organization's Typhoon Committee, should they be judged to have 10-minute sustained windspeeds of 65 km/h (40 mph)*.[122] PAGASA names to tropical cyclones which move into or form as a tropical depression in their area of responsibility located between 135°E and 115°E and between 5°N and 25°N even if the cyclone has had an international name assigned to it.[121] The names of significant tropical cyclones are retired, by both PAGASA and the Typhoon Committee.[122] Should the list of names for the Philippine region be exhausted then names will be taken from an auxiliary list of which the first ten are published each season. Unused names are marked in gray.

International names

A tropical cyclone is named when it is judged to have 10-minute sustained windspeeds of 65 km/h (40 mph)*.[123] The JMA selected the names from a list of 140 names, that had been developed by the 14 members nations and territories of the ESCAP/WMO Typhoon Committee.[124] The next 24 names on the naming list are listed here along with their international numeric designation, if they are used.

  • Nepartak (1601)
  • Lupit (1602)
  • Mirinae (1603)
  • Nida (1604)
  • Omais (1605)
  • Conson (1606)
  • Chanthu (1607)
  • Dianmu (1608)
  • Mindulle (1609)
  • Lionrock (1610)
  • Kompasu (1611)
  • Namtheun (1612)
  • Malou (1613)
  • Meranti (unused)
  • Rai (unused)
  • Malakas (unused)
  • Megi (unused)
  • Chaba (unused)
  • Aere (unused)
  • Songda (unused)
  • Sarika (unused)
  • Haima (unused)
  • Meari (unused)
  • Ma-on (unused)

Philippines

This season, PAGASA will use its own naming scheme, that will either develop within or move into their self-defined area of responsibility.[125][126] The names were taken from a list of names, that was last used during 2012 and are scheduled to be used again during 2020.[125] All of the names are the same except for Pepito, which replaced the name Pablo after it was retired.[125] The name Gardo was replaced by Gomer after Gardo was added to PAGASA's main list replacing Glenda, which was retired after the 2014 season.

  • Ambo
  • Butchoy (1601)
  • Carina (1604)
  • Dindo (1610)
  • Enteng (1612)
  • Ferdie (unused)
  • Gener (unused)
  • Helen (unused)
  • Igme (unused)
  • Julian (unused)
  • Karen (unused)
  • Lawin (unused)
  • Marce (unused)
  • Nina (unused)
  • Ofel (unused)
  • Pepito (unused)
  • Quinta (unused)
  • Rolly (unused)
  • Siony (unused)
  • Tonyo (unused)
  • Ulysses (unused)
  • Vicky (unused)
  • Warren (unused)
  • Yoyong (unused)
  • Zosimo (unused)

Auxiliary list

  • Alakdan (unused)
  • Baldo (unused)
  • Clara (unused)
  • Dencio (unused)
  • Estong (unused)
  • Felipe (unused)
  • Gomer (unused)
  • Heling (unused)
  • Ismael (unused)
  • Julio (unused)

Season effects

This table will list all the storms that developed in the northwestern Pacific Ocean west of the International Date Line and north of the equator during 2016. It will include their intensity, duration, name, areas affected, deaths, and damage totals. Classification and intensity values will be based on estimations conducted by the JMA. All damage figures will be in 2016 USD. Damages and deaths from a storm will include when the storm was a precursor wave or an extratropical cyclone.

Name Dates Peak intensity Areas affected Damage
(USD)
Deaths Refs
Category Wind speed Pressure
01W May 26 – 27 Tropical depression Not specified 998 hPa (29.47 inHg) South China Unknown None
TD June 23 – 25 Tropical depression 55 km/h (35 mph) 1006 hPa (29.71 inHg) Philippines, Vietnam None None
Ambo June 26 – 28 Tropical depression 55 km/h (35 mph) 1004 hPa (29.65 inHg) Philippines, South China None None
Nepartak
(Butchoy)
July 2 – 10 Typhoon 205 km/h (125 mph) 900 hPa (26.58 inHg) Philippines, Ryukyu Islands
Taiwan, East China
$1.52 billion 86 [127][128][129]
03W July 15 – 20 Tropical depression Not specified 1006 hPa (29.71 inHg) Ryukyu Islands None None
Lupit July 22 – 24 Tropical storm 75 km/h (45 mph) 1000 hPa (29.53 inHg) None None None
Mirinae July 25 – 29 Severe tropical storm 100 km/h (65 mph) 980 hPa (28.94 inHg) South China, Vietnam $289 million 5 [130]
TD July 27 Tropical depression Not specified 1006 hPa (29.71 inHg) None None None
Nida (Carina) July 29 – August 3 Severe tropical storm 110 km/h (70 mph) 975 hPa (28.79 inHg) Philippines, Taiwan
South China, Vietnam
$89 million 4 [130]
TD July 28 – 29 Tropical depression Not specified 1008 hPa (29.76 inHg) None None None
Omais August 3 – 9 Severe tropical storm 110 km/h (70 mph) 975 hPa (28.79 inHg) Mariana Islands, Japan
Russian Far East
None None
TD August 6 – 9 Tropical depression 55 km/h (35 mph) 998 hPa (29.47 inHg) Ryukyu Islands, East China None None
Conson August 7 – 15 Severe tropical storm 95 km/h (60 mph) 985 hPa (29.09 inHg) Japan, Russian Far East None None
TD August 10 – 12 Tropical depression 55 km/h (35 mph) 1000 hPa (29.53 inHg) Ryukyu Islands, Taiwan
East China
None None
Chanthu August 11 – 17 Severe tropical storm 100 km/h (65 mph) 980 hPa (28.94 inHg) Japan, Russian Far East None None
TD August 12 – 13 Tropical depression 55 km/h (35 mph) 1002 hPa (29.59 inHg) Taiwan None None
Dianmu August 15 – 19 Tropical storm 75 km/h (45 mph) 985 hPa (29.09 inHg) South China, Vietnam, Laos
Myanmar, Bangladesh
$6.9 million 9 [131]
TD August 16 Tropical depression Not specified 996 hPa (29.41 inHg) South China, Vietnam None None
Lionrock (Dindo) August 16 – 30 Typhoon 165 km/h (105 mph) 940 hPa (27.76 inHg) Japan Unknown 80 [132][133]
Mindulle August 17 – 23 Typhoon 120 km/h (75 mph) 975 hPa (28.79 inHg) Mariana Islands, Japan Unknown 2 [134]
TD August 17 – 18 Tropical depression Not specified 1000 hPa (29.53 inHg) None None None
Kompasu August 18 – 21 Tropical storm 65 km/h (40 mph) 994 hPa (29.35 inHg) Japan, Russian Far East None 1
14W August 23 – 24 Tropical depression 55 km/h (35 mph) 1000 hPa (29.53 inHg) Mariana Islands None None
TD August 24 Tropical depression Not specified 1002 hPa (29.59 inHg) None None None
TD August 24 Tropical depression Not specified 1000 hPa (29.53 inHg) None None None
TD August 25 Tropical depression Not specified 1002 hPa (29.59 inHg) None None None
TD August 27 Tropical depression Not specified 1006 hPa (29.71 inHg) None None None
TD August 30 – 31 Tropical depression Not specified 1004 hPa (29.65 inHg) None None None
Namtheun (Enteng) August 31 – September 5 Typhoon 140 km/h (85 mph) 955 hPa (28.20 inHg) Japan None None
Malou September 5 – 7 Tropical storm 75 km/h (45 mph) 1000 hPa (29.53 inHg) Ryukyu Islands None None
16W September 8 – Present Tropical depression Not specified 1006 hPa (29.71 inHg) None None None
Season aggregates
31 systems May 26 –
Season ongoing
205 km/h (125 mph)* 900 hPa (26.58 inHg) $1.9 billion 187

See also

References

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