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{{cn span|text=On July 26, JMA monitors a [[low-pressure area]] near [[Chuuk State|Chuuk]]. The system stalled for a few days and was upgraded into a tropical depression on July 28. Early on July 29, the depression showed signs of intensification and with that, JTWC upgraded it to Tropical Storm 11W. Later that day, JMA upgraded 11W to Tropical Storm Halong, |
{{cn span|text=On July 26, JMA monitors a [[low-pressure area]] near [[Chuuk State|Chuuk]]. The system stalled for a few days and was upgraded into a tropical depression on July 28. Early on July 29, the depression showed signs of intensification and with that, JTWC upgraded it to Tropical Storm 11W. Later that day, JMA upgraded 11W to Tropical Storm Halong.<ref>{{title=Tropical Storm Halong forms in Pacific, heading toward Japan|url=http://globalnews.ca/news/1484586/tropical-storm-halong-forms-in-pacific-heading-toward-japan/|accessdate=July 31, 2014}}</ref><ref>{{cite web|title=Okinawa and Possible Tropical Storm Nakri (Tuesday Update) |url=http://www.westernpacificweather.com/2014/07/28/okinawa-and-possible-tropical-storm-halong-tuesday-update/|accessdate=July 28, 2014|publisher=Robert Speta}}</ref> In the same time Halong started developing a small, unclear [[eye (cyclone)|eye]].<ref>{{cite web|title=Typhoon Warnings in Place as Halong Moves over Guam|url=http://www.westernpacificweather.com/2014/07/29/typhoon-warnings-in-place-as-halong-moves-over-guam/|accessdate=July 29, 2014|publisher=Robert Speta}}</ref> With this, gale and typhoon force winds were reported over [[Guam]].<ref>{{cite web|title=TS Watches in Guam , Tropical Storm Halong (Tuesday Update) |url=http://www.westernpacificweather.com/2014/07/29/ts-watches-in-guam-possible-tropical-storm-nakri-tuesday-update/|accessdate=July 29, 2014|publisher=Robert Speta}}</ref> |
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Revision as of 21:19, 1 August 2014
2014 Pacific typhoon season | |
---|---|
Seasonal boundaries | |
First system formed | January 10, 2014 |
Last system dissipated | Season currently active |
Strongest storm | |
Name | Neoguri |
• Maximum winds | 175 km/h (110 mph) (10-minute sustained) |
• Lowest pressure | 930 hPa (mbar) |
Seasonal statistics | |
Total depressions | 17 |
Total storms | 12 |
Typhoons | 5 |
Super typhoons | 2 (unofficial) |
Total fatalities | 339 total |
Total damage | $7.38 billion (2014 USD) |
Related article | |
The 2014 Pacific typhoon season is an ongoing event in the annual cycle of tropical cyclone formation, in which tropical cyclones form in the western Pacific Ocean. The season will run throughout 2014, 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.
Seasonal forecasts
TSR forecasts | |||||
---|---|---|---|---|---|
Date | Tropical storms |
Total Typhoons |
Intense TCs |
ACE Index |
Ref |
Average (1965–2013) | 26 | 16 | 8 | 295 | |
May 6, 2014 | 27 | 17 | 11 | 375 | [1] |
July 3, 2014 | 26 | 16 | 9 | 335 | [2] |
Date | Forecast Center |
Tropical storms |
Total Typhoons |
Ref | |
May 5, 2014 | CMA-STI | 26–28 | – | [1] | |
June 30, 2013 | CWB | 29–32 | – | [3] | |
Actual activity | JMA | 12 | 5 | ||
Actual activity | JTWC | 10 | 6 |
During each season, 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.[1] These agencies include the Tropical Storm Risk (TSR) Consortium of the University College London, Philippine Atmospheric, Geophysical and Astronomical Services Administration (PAGASA) and the Taiwan's Central Weather Bureau.[1][3][4]
During October 2013, the VNCHMF predicted that one to two tropical cyclones would develop and possibly affect Vietnam between November 2013 and April 2014.[5] Within its January–June seasonal climate outlook, PAGASA predicted that one to two tropical cyclones were likely to develop and/or enter the Philippine area of responsibility between January and March, three to six for April to June, eight to ten during July to September, and five to seven were predicted for the October–December period.[4][6]
Season summary
Storms
Tropical Storm Lingling (Agaton)
Tropical storm (JMA) | |
Tropical storm (SSHWS) | |
Duration | January 15 – January 20 |
---|---|
Peak intensity | 65 km/h (40 mph) (10-min); 1002 hPa (mbar) |
On January 15, the JMA started to monitor a tropical depression that had developed, within an area of high vertical wind shear about 730 km (455 mi)* to the southeast of Manila in the Philippines.[7][8] PAGASA then named the system Agaton early on January 17.[9] The next day, its circulation became a bit exposed as it intensifies into a tropical storm by the JMA, naming it Lingling.[10] The JTWC upgraded it to a tropical depression, giving the designation 01W later that day.[11] The storm reached its peak intensity at noon of January 18, before the JTWC issued its final advisory late on January 19.[12][13] Early on January 20, Lingling was rapidly downgraded to a tropical disturbance, before its remnants were absorbed by a cold front early on January 23.[14][15]
Floods and landslides killed 70 people in the Philippines. A total of nearly $13 million are damage loss from Lingling, due to heavy rainfall for three days.[16]
Tropical Storm Kajiki (Basyang)
Tropical storm (JMA) | |
Tropical storm (SSHWS) | |
Duration | January 29 – February 1 |
---|---|
Peak intensity | 65 km/h (40 mph) (10-min); 1000 hPa (mbar) |
One week after the first storm of 2014 dissipated, the JMA reported that another tropical depression had formed east of Yap on January 29.[17][18] Due to warm waters, the system organized and strengthened into Tropical Depression 02W by the JTWC on January 30. The next day, both the JMA and PAGASA upgraded it to a tropical storm, naming it Kajiki by the JMA and Basyang by PAGASA. The JTWC upgraded this storm to a tropical storm later that day, as it slowly intensified with convection.[19][20] According to PAGASA the storm made landfall over Siargao Island on January 31.[21] Due to the unfavorable conditions in the South China Sea, Kajiki dissipated late on February 1.[22][23]
During its lifecycle, Kajiki killed 6 people in the Philippines.[24]
Typhoon Faxai
Typhoon (JMA) | |
Category 1 typhoon (SSHWS) | |
Duration | February 27 – March 5 |
---|---|
Peak intensity | 120 km/h (75 mph) (10-min); 975 hPa (mbar) |
Late on February 15, a tropical disturbance was spotted near Chuuk, near the equator and was later designated as Invest 93W, in which is moving slowly in an area of high vertical wind shear.[25] Upon moving in an area of lower vertical wind shear, the storm was able to consolidate and organize. On February 27, the disturbance was upgraded to tropical depression status by the Japan Meteorological Agency and was given a Tropical Cyclone Formation Alert by the Joint Typhoon Warning Center. The following day, it was upgraded by the JTWC to a tropical depression and designated as 03W.[26] Several hours later, the JMA upgraded the system to a tropical storm and named it Faxai.[27] Faxai started rapidly intensifying into a severe tropical storm, then a typhoon for a short period of time on March 4.[28] The system became extratropical on March 6,[29] before it fully dissipated several thousands of kilometers southeast of Japan, late on March 8.[citation needed]
Tropical Depression 04W (Caloy)
Tropical depression (JMA) | |
Tropical depression (SSHWS) | |
Duration | March 18 – March 24 |
---|---|
Peak intensity | <55 km/h (35 mph) (10-min); 1004 hPa (mbar) |
On March 12, a tropical disturbance formed southeast of Guam.[30] Early on March 18, the JMA reported that it had intensified to a tropical depression, which had developed about 395 km (245 mi) east-northeast of Koror, Palau.[31] Over the next few days, the system became more organised and it was named Caloy by PAGASA on March 21. Late on March 22, the system was designated as 04W by the JTWC. Due to less convection and land reaction on March 24, the system was downgraded to a disturbance and dissipated later that day. The remnants continued to move westward towards the South China Sea, before dissipating completely to the southwest of Vietnam on March 27.[citation needed]
Tropical Storm Peipah (Domeng)
Tropical storm (JMA) | |
Tropical storm (SSHWS) | |
Duration | April 2 – April 8 |
---|---|
Peak intensity | 65 km/h (40 mph) (10-min); 998 hPa (mbar) |
On March 30, a cluster of thunderstorms formed near the equator and Papua New Guinea. The large cluster separated into 2 systems, with the other strengthening into Cyclone Ita. It intensified into a tropical depression on April 2[32][33] and strengthened into 05W by the JTWC the next day.[34] The next day, convection built up and the system intensified into a tropical storm, prompting the JMA to name it Peipah.[35] Early on April 9, Peipah weakened to a tropical depression.[36] Later on April 10, the JMA declared that Peipah had dissipated as the JTWC classifies that it is still a tropical depression. The JTWC made its final warning on Peipah later that day, as the storm's remnants continued to move northwest slowly towards the eastern Philippines.[citation needed]
Severe Tropical Storm Tapah
Severe tropical storm (JMA) | |
Category 1 typhoon (SSHWS) | |
Duration | April 27 – May 2 |
---|---|
Peak intensity | 95 km/h (60 mph) (10-min); 985 hPa (mbar) |
Early on April 27, the JMA reported that a tropical depression had formed about 515 km (320 mi) south-southeast of Hagåtña, Guam.[37][38] Later that day, the JTWC upgraded it to Tropical Depression 06W as it moved north.[39] Due to warm waters, the system rapidly intensified into a tropical storm with the JMA naming it Tapah on April 28.[40] Later that day, convection occurred and the system was upgraded to a severe tropical storm.[41] Early on April 29, the JTWC upgraded Tapah into a minimal typhoon, but the JMA upgraded it to a typhoon.[42] It weakened back to a tropical storm late on April 30.[43] On May 2, the JMA downgraded Tapah to a depression due to a very exposed circulation. Later on the same day, the remnants of Tapah were absorbed by a developing extratropical system.[44]
Tropical Storm Mitag (Ester)
Tropical storm (JMA) | |
Subtropical storm (SSHWS) | |
Duration | June 9 – June 12 |
---|---|
Peak intensity | 75 km/h (45 mph) (10-min); 994 hPa (mbar) |
Late on June 6, a low-pressure area formed near the island of Guandong, China, embedded from the monsoon trough. The next day, the system slowly moved in an eastward direction.[citation needed] Early on June 9, the JMA reported that it intensified into a tropical depression which had developed about 115 km (71 mi) to the south-southeast of Hengchun, Taiwan.[45] On June 10, PAGASA named the system Ester, as it brought flooding to the Philippines.[46][47] On the night of the next day, convection increased to the system as the JMA upgraded to Tropical Storm Mitag.[48] In the same time, the JTWC classified it as subtropical.[49] Very early on June 12, the JMA issued its final advisory on Mitag, as the system was absorbed by a developing extratropical cyclone located north of Japan.[citation needed]
Due to the southwest monsoon enhanced by Tropical Storm Mitag bringing rains to the Philippines, PAGASA reported that the official rainy season started on June 10.[50][51]
Tropical Storm Hagibis
Tropical storm (JMA) | |
Tropical storm (SSHWS) | |
Duration | June 13 – June 17 |
---|---|
Peak intensity | 75 km/h (45 mph) (10-min); 996 hPa (mbar) |
Similar to the formation of Mitag, a small circulation started to develop in the South China Sea, late on June 8. Early on June 11, the system was upgraded to a tropical disturbance. On June 13, the JMA classified the storm as a tropical depression, as it started to move slowly towards the northeast. Early on June 14, the JTWC issued a TCFA alert on the tropical depression. Later that day, the JTWC upgraded the storm to Tropical Depression 07W, and at the same time, the JMA upgraded it to a tropical storm, naming it Hagibis.[citation needed] Early on June 15, Hagibis made landfall over southern China.[52] During the next day, both agencies stopped issuing warnings on the system, as it rapidly weakened to a tropical depression over land. Its remnants still continued to move northward, by on June 17, the remnants of Hagibis curved eastwards, as it re-generated into a tropical storm. As a result, the JMA reinitiated advisories on Hagibis.[citation needed] Late on June 17, Hagibis transitioned into an extratropical cyclone. On June 21, the remnants of the storm were absorbed by another developing extratropical cyclone to the north. The system moved out of the basin on June 23.[53]
About 13,000 people were affected by the storm.[54][55] Economic losses from Hagibis reached a total of 577 million yuan ($93 million USD). Two days later, it was topped to 675 million yuan ($103.3 million USD),[56] and reached a total of $131 million as of June 20.[57][58] As of June 19, the Chinese Government had reported that there were 11 casualties in regions affected by Hagibis.[59]
Typhoon Neoguri (Florita)
Very strong typhoon (JMA) | |
Category 4 super typhoon (SSHWS) | |
Duration | July 2 – July 11 |
---|---|
Peak intensity | 175 km/h (110 mph) (10-min); 930 hPa (mbar) |
A weak tropical disturbance formed near Guam on June 30.[60] On July 1, it further intensified due to warm sea-surface temperatures and convection, and it was upgraded to a tropical depression late on July 2. The next day, it was classified as Tropical Depression 08W by JTWC.[61] Early on July 4, it was upgraded to a tropical storm by the both agencies, with the latter naming it as Neoguri.[62] Later that day, Neoguri rapidly intensified into a minimal typhoon. Early on July 5, it once again rapidly intensified and was upgraded to Category 4 status by the JTWC as the eye developed clearly. In the same time, the storm entered the PAR, with PAGASA giving it the name Florita. Late the next day, Neoguri entered an area of very warm sea temperatures as it intensified into a super typhoon by the JTWC and reached peak intensity early on July 7,[63] with the JTWC refusing to upgrade it to Category 5 status. Early on July 8, Neoguri weakened to a Category 3 typhoon.[64] and PAGASA stated that the storm had exited their area later that day.[65] Late the next day, Neoguri further weakened to a severe tropical storm by the JMA. Due to the strong jet stream, Neoguri moved in an eastward direction instead of moving towards Korea. On July 10, JMA downgraded the system to a tropical storm as the JTWC made their final warning and stopped issuing advisories. At the same time, Neoguri's circulation became totally exposed as it was affecting southern Japan. JMA made their final warning early on July 11, as Neoguri started to become extratropical. The extratropical remnants of Neoguri collided with another weak, developing system north of it on July 14.[citation needed]
Typhoon Rammasun (Glenda)
Very strong typhoon (JMA) | |
Category 4 super typhoon (SSHWS) | |
Duration | July 10 – July 20 |
---|---|
Peak intensity | 165 km/h (105 mph) (10-min); 940 hPa (mbar) |
During July 10, the JMA and JTWC reported that a tropical depression had developed to the southeast of the Mariana Islands, with the latter assigning it the designation 09W.[66][67] On the night of the same day, JTWC downgraded 09W to a tropical depression as it passed through Guam, entering an area of favorable conditions and low vertical wind shear on July 12.[68] Later that day, the JMA had upgraded it to Tropical Storm Rammasun.[69] Tracking westward at over 15 knots (28 km/h; 17 mph), the system's convective banding became more persistent.[70] Rammasun held that intensity as it entered the PAR, with PAGASA assigning the name Glenda on July 13.[71] The system finally gradually developed further to a severe tropical storm as it entered an area of favorable environmental conditions, warm waters and low vertical wind shear.[72][73] Both the JMA and the JTWC upgraded Rammasun to a typhoon, as an eye developed. In the morning hours of July 15, Rammasun further intensified into a Category 3 typhoon with a minimum pressure of 945 millibars. With JTWC's best track data, they upgraded it to Category 4 status, as it made landfall over Albay.[74][75] Due to land interaction, Rammasun rapidly weakened to a minimal typhoon and its eye collapsed late on July 16.[76] Later that day, the storm entered the South China Sea and re-intensified to a Category 3 typhoon. On July 18, Rammasun entered another area of very warm sea-surface temperatures, as it strengthened to Category 4 super typhoon status again by the JTWC,[77] but this time it reached its peak intensity.[78] Later that day, the center of Rammasun made landfall over Hainan.[79] The next day, the storm started to weaken and it weakened to Category 2 strength. Later that day, both agencies downgraded Rammasun to a tropical storm as it moved to the province of Guangxi and made its third landfall.[80][81] JTWC made its final warning on the system on the night of the same day. Early on July 20, the JMA reported that Rammasun had weakened to a tropical depression before it was last noted later that day over the Chinese Province of Yunnan.[82][83][84]
As of July 17, it is reported from NDRRMC that the death toll has reached 40 and the total amount of damages were amounted to 1 billion ($27 million USD).[85] In China, 18 persons were killed due to the storm.[86]
Typhoon Matmo (Henry)
Typhoon (JMA) | |
Category 2 typhoon (SSHWS) | |
Duration | July 16 – July 25 |
---|---|
Peak intensity | 140 km/h (85 mph) (10-min); 960 hPa (mbar) |
Late on July 13, the Intertropical Convergence Zone formed another tropical disturbance.[87][88] But due to Typhoon Rammasun being nearby, the disturbance started to weaken. The next day, it gathered warm waters and favorable conditions.[citation needed] Very early on July 16, JMA upgraded the system to a weak tropical depression, as it started to show signs of intensification. At the same time, JTWC made a TCFA alert on the system.[89][90] The next day, JTWC upgraded the system to Tropical Storm 10W, whilst the JMA named the system Matmo after it strengthened to a tropical storm.[citation needed] Early on July 18, Matmo entered the PAR, with PAGASA giving it the name Henry.[91] On July 19, JMA upgraded the system to a severe tropical storm. Matmo started to slowly intensify to a typhoon the next day. JTWC in the other hand, still classified it as a tropical storm. Later that day, JTWC upgraded it to a category 1 typhoon. In the same time, Matmo curved towards the northwest.[92] JMA downgraded Matmo to a severe tropical storm again late on July 22. Early the next day, JTWC instead upgraded Matmo to a category 2. With that, a small unclear eye developed in Matmo's center.[93]
One person was reported dead and there were some damages reported.[94] At least 48 people died in a plane crash in the Taiwan strait, the crash may have been caused by the typhoon.[95] As of July 24, according to the Yilan County Government, the agricultural damage in the county was estimated at about NT$44 million ($1.5 million USD).[96]
Severe Tropical Storm Nakri (Inday)
Severe tropical storm (JMA scale) | |
---|---|
Current storm status As of: 18:00 UTC, August 1 | |
Location | 31°18′N 125°06′E / 31.3°N 125.1°E |
Movement | NNW at 12 kn (22 km/h; 14 mph) |
Winds | 10-minute sustained: 100 km/h (65 mph) Gusts: 150 km/h (90 mph) |
Pressure | 980 hPa (mbar); 28.94 inHg |
On July 19, a tropical depression formed to the southeast of Guam. It slowly moved in a northwest direction over the next few days. Early on July 22, JTWC classified it as a TCFA Alert.[citation needed] A low-pressure area re-formed east of Palau early on July 24.[97] JMA upgraded the system to a tropical depression early on July 26,[98] as it started to move in a northward direction. The depression continued to intensify but it didn't reach tropical storm strength. Due to weakening convection east of the tropical depression, it started to weaken on July 28.[citation needed] Later that day, more convection increased in the western side of the storm, as it continued to intensify. On July 29, JMA upgraded it to Tropical Storm Nakri, but JTWC still calls this a disturbance. Deep convection occurred in Nakri, as JTWC classifies it as a monsoonal depression.[99]
This is the first time that JMA only classified it except JTWC, since Severe Tropical Storm Phanfone in 2008.[100]
Typhoon Halong
Typhoon (JMA scale) | |
---|---|
Category 1 typhoon (SSHWS) | |
Current storm status As of: 18:00 UTC, August 1 | |
Location | 14°54′N 137°06′E / 14.9°N 137.1°E About 324 nmi (600 km; 373 mi) N of Yap |
Movement | WNW at 7 kn (13 km/h; 8.1 mph) |
Winds | 10-minute sustained: 120 km/h (75 mph) 1-minute sustained: 140 km/h (85 mph) Gusts: 175 km/h (110 mph) |
Pressure | 975 hPa (mbar); 28.79 inHg |
{{cn span|text=On July 26, JMA monitors a low-pressure area near Chuuk. The system stalled for a few days and was upgraded into a tropical depression on July 28. Early on July 29, the depression showed signs of intensification and with that, JTWC upgraded it to Tropical Storm 11W. Later that day, JMA upgraded 11W to Tropical Storm Halong.[101][102] In the same time Halong started developing a small, unclear eye.[103] With this, gale and typhoon force winds were reported over Guam.[104]
Other storms
On January 10, the JMA started to monitor a tropical depression, that had developed about 370 km (230 mi)* to the southwest of Palau.[105][106] Over the next two days the system became disorganized as it moved towards the north-northwest, before it was last noted during January 12, as it affected Mindanao.[107][108][109] During March 11, the JMA monitored a tropical depression that had developed about 195 km (120 mi)* to the east of Mati City, Philippines.[110] Over the next day the system moved westwards, before it was last noted within the Celebes Sea on March 12.[110] Late on April 13, the remnants of Peipah regenerated into a tropical depression to the east of the Philippines, while slowly continuing to approach the island nation. On April 15, the depression became disorganized and the system's convection was displaced from its center of circulation, prompting the JTWC to issue its final advisory on the system.[111] During the next several hours, the remnants of the depression turned towards the southwest, until it dissipated late on April 15, just off the northeastern coast of the island of Mindanao. On April 17, PAGASA downgraded it to a low-pressure area and issued their final advisory. On April 19, the JMA reported that a tropical depression had developed about 490 km (300 mi) southwest of Hagåtña, Guam.[112] Due to less convection and cool waters on April 21, the depression weakened to a disturbance while still moving west. The remnants of the depression affected the northern Philippines and dissipated on April 23, due to land interaction.[113][114]
Names
International names
Tropical cyclones are named from a set of five naming lists set by the JMA's Regional Specialized Meteorological Centre in Tokyo, Japan, once they reach tropical storm strength.[115] Names are contributed by members of the ESCAP/WMO Typhoon Committee. Each of the 14 nations and territories submitted ten names, which are used in alphabetical order, by the official English name of the country.[116] The next 25 names on the naming list are listed here along with their international numeric designation, if they are used.
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Philippines
PAGASA uses its own naming scheme for tropical cyclones in their area of responsibility. PAGASA assigns names to tropical depressions that form within their area of responsibility and any tropical cyclone that might move into their area of responsibility. Should the list of names for a given year be exhausted, names will be taken from an auxiliary list, the first ten of which are published each year before the season starts. Names not retired from this list will be used again in the 2018 season. This is the same list used in the 2010 season, with the exception of Jose and Kanor which replaced Juan and Katring.[117]
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Auxiliary list
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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 2014. 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 2014 USD. Damages and deaths from a storm will include when the storm was a precursor wave or an extratropical low.
Name | Dates | Peak intensity | Areas affected | Damage (USD) |
Deaths | Refs | ||
---|---|---|---|---|---|---|---|---|
Category | Wind speed | Pressure | ||||||
Tropical depression | January 10 – 12 | Tropical depression | 55 km/h (35 mph) | 1004 hPa (29.65 inHg) | Palau, Philippines | None | None | |
Lingling (Agaton) | January 15 – 20 | Tropical storm | 65 km/h (40 mph) | 1002 hPa (29.59 inHg) | Philippines | $12.9 million | 70 | [16] |
Kajiki (Basyang) | January 29 – February 1 | Tropical storm | 65 km/h (40 mph) | 1000 hPa (29.53 inHg) | Caroline Islands, Philippines | Minor | 6 | [24] |
Faxai | February 27 – March 5 | Typhoon | 120 km/h (75 mph) | 975 hPa (28.79 inHg) | Caroline Islands, Mariana Islands | None | None | |
Tropical depression | March 11 – 12 | Tropical depression | Not specified | 1008 hPa (29.77 inHg) | Philippines, Indonesia | None | None | |
04W (Caloy) | March 18 – 24 | Tropical depression | Not specified | 1004 hPa (29.65 inHg) | Caroline Islands, Philippines | None | None | |
Peipah (Domeng) | April 2 – 8 | Tropical storm | 65 km/h (40 mph) | 998 hPa (29.47 inHg) | Caroline Islands | None | None | |
Tropical depression | April 13 – 15 | Tropical depression | Not specified | 1004 hPa (29.65 inHg) | Philippines | None | None | |
Tropical depression | April 19 – 21 | Tropical depression | Not specified | 1004 hPa (29.65 inHg) | Guam, Palau | None | None | |
Tapah | April 27 – May 2 | Severe tropical storm | 95 km/h (60 mph) | 985 hPa (29.09 inHg) | Mariana Islands | None | None | |
Mitag (Ester) | June 9 – 12 | Tropical storm | 75 km/h (45 mph) | 994 hPa (29.35 inHg) | Philippines, Taiwan, Japan | None | None | |
Hagibis | June 13 – 17 | Tropical storm | 75 km/h (45 mph) | 996 hPa (29.41 inHg) | Philippines, China, Taiwan, Japan | $131 million | 11 | |
Neoguri (Florita) | July 2 – 11 | Typhoon | 175 km/h (110 mph) | 930 hPa (27.46 inHg) | Caroline Islands, Guam, Japan | $156 million | 3 | [118] |
Rammasun (Glenda) | July 10 – 20 | Typhoon | 165 km/h (105 mph) | 940 hPa (27.76 inHg) | Caroline Islands, Guam, Philippines, China, Vietnam | $6.51 billion | 187 | [119][120][121] |
Matmo (Henry) | July 16 – 25 | Typhoon | 140 km/h (85 mph) | 960 hPa (28.35 inHg) | Palau, Philippines, Taiwan, China, Korea | $567 million | 62 | [95][122][123][124] |
Nakri (Inday) | July 19 – Currently active | Severe tropical storm | 100 km/h (65 mph) | 980 hPa (28.94 inHg) | Caroline Islands, Mariana Islands, Palau, Philippines, Japan, Korea | Minor | None | |
Halong | July 28 – Currently active | Typhoon | 120 km/h (75 mph) | 975 hPa (28.79 inHg) | Caroline Islands, Mariana Islands | Minimal | None | |
Season aggregates | ||||||||
17 systems | January 10 – Currently active | 175 km/h (110 mph) | 930 hPa (27.46 inHg) | $7.38 billion | 339 |
See also
- List of Pacific typhoon seasons
- 2014 Pacific hurricane season
- 2014 Atlantic hurricane season
- 2014 North Indian Ocean cyclone season
- South-West Indian Ocean cyclone seasons: 2013–14, 2014–15
- Australian region cyclone seasons: 2013–14, 2014–15
- South Pacific cyclone seasons: 2013–14, 2014–15
References
- ^ a b c d Saunders, Mark; Lea, Adam (May 6, 2014). Extended Range Forecast for Northwest Pacific Typhoon Activity in 2014 (Report). Tropical Storm Risk Consortium. Archived from the original (PDF) on May 7, 2014. Retrieved May 7, 2014.
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: Unknown parameter|deadurl=
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ignored (|url-status=
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External links
- China Meteorological Agency
- Digital Typhoon
- Hong Kong Observatory
- Japan Meteorological Agency
- Joint Typhoon Warning Center
- Korea Meteorological Administration
- Malaysian Meteorological Department
- National Weather Service Guam
- Philippine Atmospheric, Geophysical and Astronomical Services Administration
- Taiwan Central Weather Bureau
- TCWC Jakarta
- Thai Meteorological Department
- Typhoon2000
- Vietnam's National Hydro-Meteorological Service