Typhoon

A typhoon is a tropical cyclone that develops between 180° and 100°E in the Northern Hemisphere.[1] This region is referred to as the Northwestern Pacific Basin,[2] accounting for almost one-third of the world's annual tropical cyclones. The term hurricane refers to a tropical cyclone in the northeast Pacific and northern Atlantic.[3] For organizational purposes, the northern Pacific Ocean is divided into three regions: the eastern (North America to 140°W), central (140°W to 180°), and western (180° to 100°E). The Regional Specialized Meteorological Center (RSMC) for tropical cyclone forecasts is in Japan, with other tropical cyclone warning centres for the northwest Pacific in Hawaii (the Joint Typhoon Warning Center), the Philippines, and Hong Kong. Although the RSMC names each system, the main name list itself is coordinated among 18 countries that have territories threatened by typhoons each year.[4]

This article is about Northwestern Pacific tropical cyclones. For other uses, see Typhoon (disambiguation). For other areas in which tropical cyclones occur, see Tropical cyclone basins.
Not to be confused with Typhoo or Typhon.
Satellite image of Typhoon Mangkhut
Three different tropical cyclones active over the Western Pacific Ocean on August 7, 2006 (Maria, Bopha, and Saomai). The cyclones on the lower and upper right are typhoons.

Within most of the northwestern Pacific, there are no official typhoon seasons as tropical cyclones form throughout the year. Like any tropical cyclone, there are several main requirements for typhoon formation and development. It must be in sufficiently warm sea surface temperatures, atmospheric instability, high humidity in the lower-to-middle levels of the troposphere, have enough Coriolis effect to develop a low pressure centre, a pre-existing low level focus or disturbance, and a low vertical wind shear. Although the majority of storms form between June and November, a few storms may occur between December and May (although tropical cyclone formation is at a minimum during that time). On average, the northwestern Pacific features the most numerous and intense tropical cyclones globally. Like other basins, they are steered by the subtropical ridge towards the west or northwest, with some systems recurving near and east of Japan. The Philippines receive the brunt of the landfalls, with China and Japan being less often impacted. However, some of the deadliest typhoons in history have struck China. Southern China has the longest record of typhoon impacts for the region, with a thousand-year sample via documents within their archives. Taiwan has received the wettest known typhoon on record for the northwest Pacific tropical cyclone basins. However, Vietnam recognises its typhoon season as lasting from the beginning of June through to the end of November, with an average of four to six typhoons hitting the country annually.[5][6]

According to the statistics of the Joint Typhoon Warning Center, from 1950 to 2022, the Northwest Pacific generated an average of 26.5 named tropical cyclones each year, of which an average of 16.6 reached typhoon standard or above as defined by the Joint Typhoon Warning Center.[7]

Nomenclature

Etymology

The etymology of typhoon is either Chinese or Arabic-Hindustani origin.

Typhoon may trace to 風癡 (meaning "winds which long last"), first attested in 1124 in China. It was pronounced as [hɔŋ tsʰi] in Min Chinese at the time, but later evolved to [hɔŋ tʰai]. New characters 風颱 were created to match the sound, no later than 1566.[8][9] The word was introduced to Mandarin Chinese in the inverted Mandarin order 颱風 [tʰaɪ fɤŋ], later picked up by foreign sailors to appear as typhoon.[8] The usage of 颱風 was not dominant until Chu Coching, the head of meteorology of the national academy from 1929 to 1936, declared it to be the standard term.[10][11] There were 29 alternative terms for typhoon recorded in a chronicle in 1762, now mostly wiped out by 颱風.[12] An exception was 風癡, survived in Min Chinese- and Wu Chinese- speaking areas from Chaozhou, Guangdong to Taizhou, Zhejiang.[8]

Some English linguists proposed the English word typhoon traced to the Cantonese pronunciation of 颱風 [tʰɔi fuŋ] (correspond to Mandarin [tʰaɪ fɤŋ]), in turn the Cantonese word traced to Arabic.[13] This claim contradicts the fact that the Cantonese term for typhoon was 風舊 [fuŋ kɐu] before the national promotion of 颱風.[8] 風舊 (meaning "winds which long last") was first attested in 280, being the oldest Chinese term for typhoon.[9] Not one Chinese historical record links 颱風 to an Arabic or foreign origin.[10][11] On the other hand, Chinese records consistently assert foreigners refer typhoon as "black wind".[10][11] "Black wind" eventually enters the vocabulary of Jin Chinese as 黑老風 [xəʔ lo fəŋ].[14]

Alternatively, some dictionaries propose that typhoon derived from(طوفان) ṭūfān, meaning storm in Arabic and Hindustani.[15][16] The root of (طوفان) ṭūfān ultimately traces to the Ancient Greek mythological creature Typhôn.[16] In French typhon was attested as storm in 1504.[17] Portuguese traveler Fernão Mendes Pinto referred to a tufão in his memoir published in 1614.[18] The earliest form in English was "touffon" (1588),[16] later as touffon, tuffon, tufon, tuffin, tuffoon, tayfun, tiffoon, typhawn.[10][11]

Intensity classifications
See also: Tropical cyclone scales
RSMC Tokyo's Tropical Cyclone Intensity Scale
Category Sustained winds
Violent typhoon ≥105 knots
≥194 km/h
Very strong typhoon 85–104 knots
157–193 km/h
Typhoon 64–84 knots
118–156 km/h
Severe tropical storm 48–63 knots
89–117 km/h
Tropical storm 34–47 knots
62–88 km/h
Tropical depression ≤33 knots
≤61 km/h

A tropical depression is the lowest category that the Japan Meteorological Agency uses and is the term used for a tropical system that has wind speeds not exceeding 33 knots (38 mph; 61 km/h).[19] A tropical depression is upgraded to a tropical storm should its sustained wind speeds exceed 34 knots (39 mph; 63 km/h). Tropical storms also receive official names from RSMC Tokyo.[19] Should the storm intensify further and reach sustained wind speeds of 48 knots (55 mph; 89 km/h) then it will be classified as a severe tropical storm.[19] Once the system's maximum sustained winds reach wind speeds of 64 knots (74 mph; 119 km/h), the JMA will designate the tropical cyclone as a typhoon—the highest category on its scale.[19]

Since 2009 the Hong Kong Observatory has divided typhoons into three different classifications: typhoon, severe typhoon and super typhoon.[20] A typhoon has wind speed of 64–79 knots (73–91 mph; 118–149 km/h), a severe typhoon has winds of at least 80 knots (92 mph; 150 km/h), and a super typhoon has winds of at least 100 knots (120 mph; 190 km/h).[20] The United States' Joint Typhoon Warning Center (JTWC) unofficially classifies typhoons with wind speeds of at least 130 knots (67 m/s; 150 mph; 241 km/h)—the equivalent of a strong Category 4 storm in the Saffir-Simpson scale—as super typhoons.[21] However, the maximum sustained wind speed measurements that the JTWC uses are based on a 1-minute averaging period, akin to the U.S.'s National Hurricane Center and Central Pacific Hurricane Center. As a result, the JTWC's wind reports are higher than JMA's measurements, as the latter is based on a 10-minute averaging interval.[22]

Genesis
Depth of 26 °C isotherm on October 1, 2006
See also: Tropical cyclogenesis

There are six main requirements for tropical cyclogenesis: sufficiently warm sea surface temperatures, atmospheric instability, high humidity in the lower to middle levels of the troposphere, enough Coriolis force to develop a low pressure center, a pre-existing low level focus or disturbance, and low vertical wind shear. While these conditions are necessary for tropical cyclone formation, they do not guarantee that a tropical cyclone will form. Normally, an ocean temperature of 26.5 °C (79.7 °F) spanning through a depth of at least 50 metres (160 ft) is considered the minimum to maintain the special mesocyclone that is the tropical cyclone. These warm waters are needed to maintain the warm core that fuels tropical systems. A minimum distance of 500 km (300 mi) from the equator is normally needed for tropical cyclogenesis.[23] Whether it be a depression in the Intertropical Convergence Zone (ITCZ) or monsoon trough, a broad surface front, or an outflow boundary, a low level feature with sufficient vorticity and convergence is required to begin tropical cyclogenesis. About 85 to 90 percent of Pacific typhoons form within the monsoon trough.[24] Even with perfect upper-level conditions and the required atmospheric instability, the lack of a surface focus will prevent the development of organized convection and a surface low. Vertical wind shear of less than 10 m/s (20 kn, 33 ft/s) between the ocean surface and the tropopause is required for tropical cyclone development.[23][25] Typically with Pacific typhoons, there are two outflow jets: one to the north ahead of an upper trough in the Westerlies, and a second towards the equator.[24]

In general, the westerly wind increases associated with the Madden–Julian oscillation lead to increased tropical cyclogenesis in all tropical cyclone basins. As the oscillation propagates from west to east, it leads to an eastward march in tropical cyclogenesis with time during that hemisphere's summer season.[26] On average, twice per year twin tropical cyclones will form in the western Pacific Ocean, near the 5th parallel north and the 5th parallel south, along the same meridian, or line of longitude.[27] There is an inverse relationship between tropical cyclone activity in the western Pacific basin and the North Atlantic basin, however. When one basin is active, the other is normally quiet, and vice versa. The main reason for this appears to be the phase of the Madden–Julian oscillation, or MJO, which is normally in opposite modes between the two basins at any given time.[28]

Frequency
Storm Frequency
Tropical storms and Typhoons by month,
for the period 1959–2015 (Northwest Pacific)
Month Count Average
Jan280.5
Feb140.2
Mar260.5
Apr370.6
May661.2
Jun1001.8
Jul2213.9
Aug3105.4
Sep2804.9
Oct2284.0
Nov1392.4
Dec691.2
Annual151826.6
Source: JTWC[29]

Nearly one-third of the world's tropical cyclones form within the western Pacific. This makes this basin the most active on Earth.[30] Pacific typhoons have formed year-round, with peak months from August to October. The peak months correspond to that of the Atlantic hurricane seasons. Along with a high storm frequency, this basin also features the most globally intense storms on record. One of the most recent busy seasons was 2013. Tropical cyclones form in any month of the year across the northwest Pacific Ocean and concentrate around June and November in the northern Indian Ocean. The area just northeast of the Philippines is the most active place on Earth for tropical cyclones to exist.

Across the Philippines themselves, activity reaches a minimum in February, before increasing steadily through June and spiking from July through October, with September being the most active month for tropical cyclones across the archipelago. Activity falls off significantly in November, although Typhoon Haiyan, the strongest Philippine typhoon on record, was a November typhoon.[31] The most frequently impacted areas of the Philippines by tropical cyclones are northern and central Luzon and eastern Visayas.[32] A ten-year average of satellite determined precipitation showed that at least 30 percent of the annual rainfall in the northern Philippines could be traced to tropical cyclones, while the southern islands receive less than 10 percent of their annual rainfall from tropical cyclones.[33] The genesis and intensity of typhoons are also modulated by slow variation of the sea surface temperature and circulation features following a near-10-year frequency.[34]

Paths
See also: Hurricane Alley
Tracks of all tropical cyclones in the northernwestern Pacific Ocean between 1980 and 2005. The vertical line to the right is the International Date Line.

Most tropical cyclones form on the side of the subtropical ridge closer to the equator, then move poleward past the ridge axis before recurving north and northeast into the main belt of the Westerlies.[35] Most typhoons form in a region in the northwest Pacific known as typhoon alley, where the planet's most powerful tropical cyclones most frequently develop.[36] When the subtropical ridge shifts due to El Niño, so will the preferred tropical cyclone tracks. Areas west of Japan and Korea tend to experience many fewer September–November tropical cyclone impacts during El Niño and neutral years. During El Niño years, the break in the subtropical ridge tends to lie near 130°E, which would favor the Japanese archipelago.[37] During La Niña years, the formation of tropical cyclones, and the subtropical ridge position, shift westward across the western Pacific Ocean, which increases the landfall threat to China and greater intensity to Philippines.[37] Those that form near the Marshall Islands find their way to Jeju Island, Korea.[38] Typhoon paths follow three general directions.[30]

  • Straight track (or straight runner). A general westward path affects the Philippines, southern China, Taiwan, and Vietnam.
  • A parabolic recurving track. Storms recurving affect the eastern Philippines, eastern China, Taiwan, Korea, Japan, and the Russian Far East.
  • Northward track. From point of origin, the storm follows a northerly direction, only affecting small islands.

A rare few storms, like Hurricane John, were redesignated as typhoons as they originated in the Eastern/Central Pacific and moved into the western Pacific.

Basin monitoring

Within the Western Pacific, RSMC Tokyo-Typhoon Center, part of the Japan Meteorological Agency, has had the official warning responsibility for the whole of the Western Pacific since 1989,[39] and the naming responsibility for systems of tropical storm strength or greater since 2000.[20] However each National Meteorological and Hydrological Service within the western Pacific has the responsibility for issuing warnings for land areas about tropical cyclones affecting their country, such as the Joint Typhoon Warning Center for United States agencies,[40] the Philippine Atmospheric, Geophysical and Astronomical Services Administration (PAGASA) for interests in the island archipelago nation,[41] and the Hong Kong Observatory for storms that come close enough to cause the issuance of warning signals.[42]

Name sources and name list

The list of names consists of entries from 14 southeast and east Asian nations and regions and the United States who have territories directly affected by typhoons. The submitted names are arranged into a list, the names on the list will be used from up to down, from left to right. When all names on the list are used, it will start again from the left-top corner. When a typhoon causes damage in a region, the affected region can request for retiring the name in the next session of the ESCAP/WMO Typhoon Committee. A new name will be decided by the region whose name was retired.

Unlike tropical cyclones in other parts of the world, typhoons are not named after people. Instead, they generally refer to animals, flowers, astrological signs, and a few personal names. However, Philippines (PAGASA) retains its own naming list, which consists of both human names and other things.[43] Japan and some other East Asian countries also assign numbers to typhoons.[44]

Storms that cross the date line from the central Pacific retain their original name, but the designation of hurricane becomes typhoon.

List of Western Pacific tropical cyclone names (as of 2023)
List Contributing nations/regions
 Cambodia  China  North Korea  Hong Kong, China  Japan  Laos  Macau, China  Malaysia  Federated States of Micronesia  Philippines  South Korea  Thailand  United States  Vietnam
1 DamreyHaikuiKirogiYun-yeungKoinuBolavenSanbaJelawatEwiniarMaliksiGaemiPrapiroonMariaSon-Tinh
AmpilWukongJongdariShanshanYagiLeepiBebincaPulasanSoulikCimaronJebiKrathonBarijatTrami
2 Kong-reyYinxingTorajiMan-yiUsagiPabukWutipSepatMunDanasNariWiphaFranciscoCo-may
KrosaBailuPodulLinglingKajikiNongfaPeipahTapahMitagRagasaNeoguriBualoiMatmoHalong
3 NakriFengshenKalmaegiFung-wongKotoNokaenPenhaNuriSinlakuHagupitJangmiMekkhalaHigosBavi
MaysakHaishenNoulDolphinKujiraChan-homPeilouNangkaSaudelNarraGaenariAtsaniEtauBang-Lang
4 KrovanhDujuanSurigaeChoi-wanKogumaChampiIn-faCempakaNepartakLupitMirinaeNidaOmaisConson
ChanthuDianmuMindulleLionrockKompasuNamtheunMalouNyatohRaiMalakasMegiChabaAereSongda
5 TrasesMulanMeariMa-onTokageHinnamnorMuifaMerbokNanmadolTalasNoruKulapRokeSonca
NesatHaitangNalgaeBanyanYamanekoPakharSanvuMawarGucholTalimDoksuriKhanunLanSaola
References:[45]

Records
Total
storms		 Year Tropical
storms		 Typhoons Super
typhoons
39196413197
351965
1967
1971		14
15
11		10
16
16		11
4
4
34199414146
33199612156
32197416160
311989
1992
2013		10
13
18		15
17
8		6
5
5
301962
1966
1972
1990
2004		7
10
8
9
10
17
17
20
17
13		6
3
2
4
7

The most active Western Pacific typhoon season was in 1964, when 39 storms of tropical storm strength formed. Only 15 seasons had 30 or more storms developing since reliable records began. The least activity seen in the northwest Pacific Ocean was during the 2010 Pacific typhoon season, when only 14 tropical storms and seven typhoons formed. In the Philippines, the most active season, since 1945, for tropical cyclone strikes was 1993 when nineteen tropical cyclones moved through the country.[46] There was only one tropical cyclone that moved through the Philippines in 1958. The 2004 Pacific typhoon season was the busiest for Okinawa since 1957.[47] Within Guangdong in southern China, during the past thousand years, the most active decades for typhoon strikes were the 1660s and 1670s.[48]

The highest reliably-estimated maximum sustained winds on record for a typhoon was that of Typhoon Haiyan at 314 km/h (195 mph) shortly before its landfall in the central Philippines on November 8, 2013.[49] The most intense storm based on minimum pressure was Typhoon Tip in the northwestern Pacific Ocean in 1979, which reached a minimum pressure of 870 hectopascals (26 inHg) and maximum sustained wind speeds of 165 knots (85 m/s, 190 mph, 310 km/h).[50] The deadliest typhoon of the 20th century was Typhoon Nina, which killed nearly 100,000 in China in 1975 due to a flood that caused 12 reservoirs to fail.[51] After Typhoon Morakot landed in Taiwan at midnight on August 8, 2009, almost the entire southern region of Taiwan (Chiayi County/Chiayi City, Tainan County/Tainan City (now merged as Tainan), Kaohsiung County/Kaohsiung City (now merged as Kaohsiung), and Pingtung County) and parts of Taitung County and Nantou County were flooded by record-breaking heavy rain. The rainfall in Pingtung County reached 2,327 millimeters (91.6 in),[52] breaking all rainfall records of any single place in Taiwan induced by a single typhoon,[53] and making the cyclone the wettest known typhoon.

See also

For storms that have affected countries in this basin:

Notes

    References
    1. "Typhoon". Glossary of Meteorology. American Meteorological Society. 2012. Archived from the original on 2015-04-12. Retrieved 2015-04-05.
    2. Chris Landsea (2010-06-01). "Subject: F1) What regions around the globe have tropical cyclones and who is responsible for forecasting there?". Journal of Geophysical Research: Atmospheres: D06108. Archived from the original on 2012-07-31. Retrieved 2011-03-30.
    3. "Hurricane". Glossary of Meteorology. American Meteorological Society. 2012. Archived from the original on 2015-04-05. Retrieved 2015-04-05.
    4. "What is the difference between a hurricane, a cyclone, and a typhoon?". OCEAN FACTS. National Ocean Service. Archived from the original on 2016-12-25. Retrieved 2016-12-24.
    5. "Typhoon and Tropical Cyclone Seasons in Vietnam". U.S. Embassy & Consulate in Vietnam. 2019-10-29. Archived from the original on 2022-01-07. Retrieved 2022-01-07.
    6. Briefing, Vietnam (2021-09-15). "Typhoon Season in Vietnam: How to Prepare Your Business". Vietnam Briefing News. Archived from the original on 2021-12-16. Retrieved 2022-01-07.
    7. "Northwest Pacific Ocean Historical Tropical Cyclone Statistics". Colorado State University.
    8. 李荣 (1990). "台风的本字(上)". 方言 (4).; 李荣 (1991). "台风的本字(中)". 方言 (1).; 李荣 (1991). "台风的本字(下)". 方言 (2).; 李荣 (2006). 冯爱珍 (ed.). "台风的本字 [Selected reprint]". 科技术语研究(季刊). 8 (4).
    9. Chen, Shou, ed. (280). "陸凱傳". 三國志·吳書 [Records of the Three Kingdoms - Book of Wu]. 蒼梧、南海，歲有舊風瘴氣之害，風則折木，飛沙轉石; 徐兢 (1124). 宣和奉使高麗圖經 [The trip of the Imperial envoy to Korea, with illustrations]. 海道之難甚矣...又惡三種險：曰癡風，曰黑風，曰海動。癡風之作，連日怒號不止，四方莫辨; 荔鏡記 [Tale of the Lychee Mirror]. 1566. 風台過了，今即會[sic, 回]南. As cited in 李荣 (1990). "台风的本字(上)". 方言 (4).; 李荣 (1991). "台风的本字(中)". 方言 (1).; 李荣 (1991). "台风的本字(下)". 方言 (2).
    10. Fu; et al. (2023). "Historic and Future Perspectives of Storm and Cyclone" (PDF). Advances in Atmospheric Sciences. 40 (3): 450–451. Bibcode:2023AdAtS..40..447F. doi:10.1007/s00376-022-2184-1. ISSN 0256-1530. S2CID 253918708.
    11. Wu, Liguang (2020). "台风一词的历史沿革" [Historical evolution of the word 'Typhoon']. 气象学报 (Acta Meteorologica Sinica). 78 (6): 1065–1075. doi:10.11676/qxxb2020.072. ISSN 0577-6619.
    12. The Chaozhou Chronicle 潮州府志 (1762) recorded 29 expressions for typhoon, including 回南風, 落西風, 蕩西風, 奔龍 and 鐵風篩. As cited in 李荣 (1990). "台风的本字(上)". 方言 (4).; 李荣 (1991). "台风的本字(中)". 方言 (1).; 李荣 (1991). "台风的本字(下)". 方言 (2).
    13. Garland Hampton Cannon; Alan S. Kaye (1994). The Arabic Contributions to the English Language: An Historical Dictionary. Otto Harrassowitz Verlag. p. 74. ISBN 978-3-447-03491-3. Archived from the original on 2022-05-02. Retrieved 2021-12-05. Typhoon [...] is a special case, transmitted by Cantonese, from Arabic, but ultimately deriving from Greek.
    14. 贺雪梅 (2020). "吴堡县篇". In 王建领 (ed.). 陕西方言集成:榆林卷. 商务印书馆. pp. 692–726.
    15. Onions, C. T., ed. (1966). "Typhoon". The Oxford Dictionary of English Etymology. Oxford University Press. p. 965. typhoon. cyclonic storm in the China seas. XVI [century]. Adoption of Chinese tai fung, dialect variant of ta big, feng wind; confer German taifun, teifun, French typhon. Earlier † tuffoon (XVII), identified in form with † touffon (XVI), † tuffon (XVII) violent storm in India, adoption of Portuguese tufão, adoption of Hindustani (in turn, adoption of Arabic) ṭūfān hurricane, tornado, beside which there was a contemporary † typhon (XVI), adoption of Latin tȳphōn, adoption of Greek tuphôn, related to tūphein (see TYPHUS).
    16. "typhoon | Origin and meaning of typhoon by Online Etymology Dictionary". Online Etymology Dictionary. Archived from the original on 2014-01-25. Retrieved 2008-10-26.
    17. "TYPHON : Définition de TYPHON" (in French). Archived from the original on 2020-08-09. Retrieved 2019-08-19.
    18. Pinto, Fernão Mendes (2013) [1614]. Peregrinação: volume I (PDF). Rio de Janeiro: Fundação Darcy Ribeiro. pp. 181, 295.
    19. Typhoon Committee (2008). "Typhoon Committee Operational Manual" (PDF) (report). World Meteorological Organization. Archived from the original (PDF) on 2012-07-17. Retrieved 2008-12-23.
    20. "Classifications of Tropical cyclones" (PDF). Hong Kong Observatory. 2009-03-18. Archived from the original (PDF) on 2012-03-30. Retrieved 2009-04-27.
    21. Joint Typhoon Warning Center (2008-03-31). "What are the description labels used with tropical cyclones by JTWC?". Joint Typhoon Warning Center – Frequently Asked Questions (FAQ). Archived from the original on 2012-07-15. Retrieved 2008-12-22.
    22. "How are JTWC forecasts different than forecasts issued by tropical cyclone warning centres (TCWCs) of other countries?". Joint Typhoon Warning Center. 2008-03-31. Archived from the original on 2012-07-15. Retrieved 2008-12-26.
    23. Chris Landsea (1 June 2010). "Subject: A15) How do tropical cyclones form ?". NOAA's Atlantic Oceanographic and Meteorological Laboratory. National Hurricane Center. Archived from the original on 2009-08-27. Retrieved 2011-03-24.
    24. Roger Graham Barry; Andrew Mark Carleto (2001). Synoptic and dynamic climatology. Psychology Press. pp. 520–521. ISBN 978-0-415-03115-8. Archived from the original on 2022-05-02. Retrieved 2011-03-06.
    25. "Hurricane FAQ". NOAA's Atlantic Oceanographic and Meteorological Laboratory.
    26. John Molinari; David Vollaro (September 2000). "Planetary- and Synoptic-Scale Influences on Eastern Pacific Tropical Cyclogenesis". Monthly Weather Review. 128 (9): 3296–307. Bibcode:2000MWRv..128.3296M. doi:10.1175/1520-0493(2000)128<3296:PASSIO>2.0.CO;2. ISSN 0027-0644. S2CID 9278279.
    27. Roger Graham Barry; Richard J. Chorley (2003). Atmosphere, weather, and climate. Psychology Press. p. 271. ISBN 978-0-415-27170-7. Archived from the original on 2022-05-02. Retrieved 2011-03-06.
    28. E. D. Maloney; D. L. Hartmann (September 2001). "The Madden–Julian Oscillation, Barotropic Dynamics, and North Pacific Tropical Cyclone Formation. Part I: Observations". Journal of the Atmospheric Sciences. 58 (17): 2545–2558. Bibcode:2001JAtS...58.2545M. CiteSeerX 10.1.1.583.3789. doi:10.1175/1520-0469(2001)058<2545:TMJOBD>2.0.CO;2. ISSN 0022-4928. S2CID 35852730.
    29. Joint Typhoon Warning Center (2015). 2015 Annual Tropical Cyclone Report: Western Pacific (PDF) (Report). United States Navy, United States Air Force. Retrieved 2016-07-11.
    30. James B. Elsner; Kam-Biu Liu (2003-10-08). "Examining the ENSO-Typhoon Hypothesis" (PDF). Climate Research. 25: 43. Bibcode:2003ClRes..25...43E. doi:10.3354/cr025043. ISSN 0936-577X. Archived (PDF) from the original on 2008-04-09. Retrieved 2007-08-18.
    31. Ricardo García-Herrera, Pedro Ribera, Emiliano Hernández and Luis Gimeno (2006). "Typhoons in the Philippine Islands, 1566–1900" (PDF). Journal of Geophysical Research. 112 (D6): 40. Bibcode:2007JGRD..112.6108G. doi:10.1029/2006JD007370. ISSN 0148-0227. Archived (PDF) from the original on 2009-10-07. Retrieved 2010-04-13.{{cite journal}}: CS1 maint: multiple names: authors list (link)
    32. Colleen A. Sexton (2006). Philippines in Pictures. Twenty-First Century Books. p. 16. ISBN 978-0-8225-2677-3. Retrieved 2008-11-01. most active typhoon season for the Philippines.
    33. Edward B. Rodgers; Robert F. Adler; Harold F. Pierce (October 2000). "Contribution of Tropical Cyclones to the North Pacific Climatological Rainfall as Observed from Satellites". Journal of Applied Meteorology. 39 (10): 1662. Bibcode:2000JApMe..39.1658R. doi:10.1175/1520-0450(2000)039<1658:COTCTT>2.0.CO;2. hdl:2060/19990109670. ISSN 1558-8424.
    34. Wang, Shih-Yu; Clark, Adam J. (2011). "Quasi-decadal spectral peaks of tropical western Pacific SSTs as a precursor for tropical cyclone threat". Geophysical Research Letters. 37 (21): n/a. Bibcode:2010GeoRL..3721810W. doi:10.1029/2010GL044709. ISSN 0094-8276. S2CID 39433860. Archived from the original on 2017-06-30.
    35. Joint Typhoon Warning Center (2006). "3.3 JTWC Forecasting Philosophies" (PDF). United States Navy. Archived (PDF) from the original on 2012-07-05. Retrieved 2007-02-11.
    36. Jonathan Belles (July 6, 2016). "Typhoon Alley: Where the Planet's Most Intense Tropical Cyclones Most Frequently Happen". The Weather Company. Archived from the original on April 12, 2019. Retrieved April 12, 2019.
    37. M. C. Wu; W. L. Chang; W. M. Leung (2003). "Impacts of El Nino-Southern Oscillation Events on Tropical Cyclone Landfalling Activity in the Western North Pacific". Journal of Climate. 17 (6): 1419–1428. Bibcode:2004JCli...17.1419W. CiteSeerX 10.1.1.461.2391. doi:10.1175/1520-0442(2004)017<1419:IOENOE>2.0.CO;2. ISSN 0894-8755.
    38. David J. Nemeth (1987). The architecture of ideology: neo-Confucian imprinting on Cheju Island, Korea. University of California Press. p. 51. ISBN 978-0-520-09713-1. Archived from the original on 2022-05-02. Retrieved 2011-03-06.
    39. Japan Meteorological Agency (2001-05-25). "Annual Report on Activities of the RSMC Tokyo – Typhoon Center: 2000" (PDF). pp. iii, 11. Archived (PDF) from the original on 2013-12-12. Retrieved 2011-03-11.
    40. Naval Meteorology and Oceanography Command (2011). "Products and Service Notice". United States Navy. Archived from the original on 2017-06-09. Retrieved 2011-03-11.
    41. Philippine Atmospheric, Geophysical & Astronomical Services Administration (2004). "Mission/Vision". Archived from the original on 2004-04-22. Retrieved 2011-03-11.
    42. Hong Kong Observatory (September 2010). "Tropical Cyclones in 2009" (PDF). pp. 18–19. Archived from the original (PDF) on 2017-06-29. Retrieved 2011-03-11.
    43. "How typhoons are named". USA Today. 2007-11-01. Archived from the original on 2008-09-30. Retrieved 2008-08-18.
    44. "Digital Typhoon: Typhoon Names (Asian Names)". agora.ex.nii.ac.jp. Retrieved 2023-07-31.
    45. RSMC Tokyo-Typhoon Center. "List of names for tropical cyclones adopted by the ESCAP/WMO Typhoon Committee for the western North Pacific and the South China Sea (valid as of 2019)". Japan Meteorological Agency: RSMC Tokyo - Typhoon Center. Japan Meteorological Agency. Archived from the original on January 5, 2021. Retrieved October 25, 2019.
    46. Joint Typhoon Warning Center (2009). "Member Report Republic of the Philippines" (PDF). Philippine Atmospheric, Geophysical and Astronomical Services Administration. World Meteorological Organization. Archived (PDF) from the original on 2019-09-12. Retrieved 2010-04-14.
    47. Erik Slavin (2005-05-30). "Preparation critical for Japan's coming typhoon season". Stars and Stripes. Archived from the original on 2011-06-28. Retrieved 2011-03-06.
    48. Kam-Biu Liu; Caiming Shen; Kin-Sheun Louie (2001). "A 1,000-Year History of Typhoon Landfalls in Guangdong, Southern China, Reconstructed from Chinese Historical Documentary Records". Annals of the Association of American Geographers. 91 (3): 453–464. doi:10.1111/0004-5608.00253. ISSN 0004-5608. S2CID 53066209.
    49. Samenow, Jason; McNoldy Brian (2013-11-08). "Among Strongest Storms Ever". The Washington Post. Archived from the original on 2013-11-08. Retrieved 2013-11-08.
    50. George M. Dunnavan; John W. Diercks (1980). "An Analysis of Super Typhoon Tip (October 1979)". Monthly Weather Review. 108 (11): 1915–1923. Bibcode:1980MWRv..108.1915D. doi:10.1175/1520-0493(1980)108<1915:AAOSTT>2.0.CO;2. ISSN 1520-0493.
    51. Anderson-Berry, Linda J.; Weyman James C. (2008-02-26). "Fifth International Workshop on Tropycal Cyclones: Topic 5.1: Societal Impacts of Tropical Cyclones". World Meteorological Organization. National Oceanic and Atmospheric Administration. Archived from the original on 2012-11-14. Retrieved 2011-03-31.
    52. Arizona State University (2009-08-12). "Taiwan Rainfall Record Investigation". Archived from the original on 2011-01-02. Retrieved 2011-03-06.
    53. "Record rains in south". The China Post. 2009-08-09. Archived from the original on 2009-08-12. Retrieved 2009-08-09.

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