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East Asian rainy season

The East Asian rainy season (Chinese and Japanese: 梅雨; pinyin: méiyǔ; rōmaji: tsuyu/baiu; Korean: 장마; romaja: jangma), also called the plum rain, is caused by precipitation along a persistent stationary front known as the Meiyu front for nearly two months during the late spring and early summer in East Asia between mainland China, Taiwan, Korea and Japan. The wet season ends during the summer when the subtropical ridge becomes strong enough to push this front north of the region. These weather systems can produce heavy rainfall and flooding.

Plum rain falling on two clear umbrellas, looking up toward the Tokyo Metropolitan Government Building, in June 2009.
East Asian rainy season
Chinese name
Chinese梅雨
Literal meaningplum rain
Transcriptions
Standard Mandarin
Hanyu Pinyinméiyǔ
Bopomofoㄇㄟˊㄩˇ
IPAměiɥỳ
Hakka
Romanizationmòi-yí
Yue: Cantonese
Jyutpingmui4 jyu5
IPAmu̖ːy̯jy̗ː
Southern Min
Hokkien POJmûi-ú / bôe-í
Korean name
Hangul장마
Hanja長마
Transcriptions
Revised Romanizationjangma
Japanese name
Kanji梅雨
Kanaつゆ / ばいう
Hiraganaつゆ / ばいう
Katakanaツユ / バイウ
Transcriptions
Revised Hepburntsuyu / baiu
Kunrei-shikituyu / baiu
Russian name
RussianВосточно-азиатский сезон дождей

Etymology edit

In China, the term "plum rain" was used for the rain in the fourth and fifth lunar month.[1][2] It specifically refers to the historical belief that, when the plums turn yellow and fall at the south of the Yangtze in the fourth and fifth months, the moisture that evaporates from the plant turns into rain.[2]

The term appears in the following poem by Du Fu (fl. 8th century) of the Tang dynasty:

梅雨
南京犀浦道,四月熟黃梅。
湛湛長江去,冥冥細雨來。
茅茨疏易溼,雲霧密難開。
竟日蛟龍喜,盤渦與岸迴。

Plum rain
On the Xipu road from the Southern Capital [present-day Chengdu],
the fourth month ripens the yellow p[r]unus.
The long river goes off surging,
and, darkening, a fine rain comes.
Roof-thatch, loosely bound, is easily soaked,
clouds and fog are dense and will not lift.
All day long the dragons delight,
whirlpools turning with the bank.[1]

Japan later adapted and transliterated the Chinese term "plum rain" to call the rainy season tsuyu (梅雨).

The season is instead commonly called Jangma (장마) in Korea, which means "long rain". The term was originally spelled Dyangmah (댱맣) in 1500s, which was the mix of the hanja character 長 ("long") and the old native Korean word 맣 (mah, "rain"). The word Dyangmah eventually transformed from Jyangma (쟝마) in 1700s to the current form of Jangma after the 1900s.[3]

Formation edit

An east-west zone of disturbed weather during spring along this front stretches from the east China coast, initially across Taiwan and Okinawa, later, when it has shifted to the north, eastward into the southern peninsula of South Korea and Japan.[4] In Taiwan and Okinawa, the rainy season usually lasts from May to June.[5] In Russian Primorsky Krai, Japan, and Korea, it lasts from June to July (approximately 50 days). In eastern China (especially the Yangtze and Huai River regions), it lasts from July to August.[citation needed]

The weather front forms when the moist air over the Pacific meets the cooler continental air mass. The front and the formation of frontal depressions along it brings precipitation to Primorsky Krai, Japan, Korea, eastern China, and Taiwan. As the front moves back and forth depending on the strength of cool and warm air masses, there is often prolonged precipitation and sometimes flooding in eastern China. However, in the years that it does not rain as much as usual, a drought might result. The rainy season ends when the warm air mass associated with the subtropical ridge is strong enough to push the front north and away.[citation needed]

Effects edit

The high humidity in the air during this season encourages the formation of mold and rot not only on food but on fabrics as well. Environmentally, heavy rains encourage mudslides and flooding in all areas affected. The most rain in a one-hour period as recorded in Japan was in Nagasaki in 1982 with 153 millimetres (6.0 in). The highest overall recorded rainfall during the rainy season in Japan was in 2003 when Miyazaki Prefecture recorded rains of 8,670 millimetres (341 in).[citation needed]

Japan edit

In Japan, the rainy season is called tsuyu (梅雨), and lasts from early June to mid-July in most of the country (Honshu, Kyushu and Shikoku), approximately June 7 to July 20 in the Kansai and Kantō regions in Honshū.[6] The tsuyu season is roughly a month earlier (early May through mid-June) in Okinawa (the southernmost region of the country). There is no pronounced tsuyu season in Hokkaidō (the northernmost region of the country) because the tsuyu front usually attenuates before it reaches the region so that it cannot produce the abundant rainfall. Tsuyu is also known as Samidare (五月雨, literally "the fifth-month rain (in the Japanese traditional calendar)", roughly corresponding to June in the modern calendar). The pop artist Eiichi Ohtaki produced a popular song by this name, and a Second World War Japanese naval ship was also given this name.[citation needed]

The rains in the middle of November - early December are sometimes called the sazanka tsuyu, literally "rainy season of the camellia" on account of the timing with the blossoming of the seasonal flower.[citation needed]

This period is generally avoided for tourism, but some sights are considered particularly atmospheric in the rain and fog, particularly mountain forests, notably Sacred Sites and Pilgrimage Routes in the Kii Mountain Range (including Mount Kōya).[6] Vegetation, especially moss, is also rather lush at this time, and hence sights known for their moss, such as Saihō-ji (the moss temple) are also popular at this time of year.[citation needed]

Korea edit

The rainy season is between June and mid-July. It is caused by hot and humid high pressure forming in the Sea of Okhotsk due to the North Pacific anticyclone combining with Asiatic continental high pressure. When the two meteorological events meet they form a long jangmajeonseon (Korean: 장마전선, from 장마; lit. rainy season and 전선; 前線; lit. weather front). Beginning in late-May, the North Pacific high pressure forces the weaker continental anticyclone south of Okinawa Island. This fall to the south then reverses and gradually strengthens as it moves northwards back towards the Korean peninsula. On landfall, heavy monsoon rains lead to torrential downpours and flooding. By August the system has weakened as the southern systems retreat towards the Philippine archipelago.[citation needed]

By early autumn, the North Pacific high-pressure system is pushed away as Asiatic continental cold high pressure moves southwards. This produces inclement weather although not on the scale of the summer monsoons. Korea can, however, be struck by typhoons during this period.[citation needed]

Timing edit

In some years, the rainy season's actual beginning and end are under debate. For example, in 2005, the subtropical ridge moved quickly northward in late June/early July. The weather front skipped the Yangtze region and there was no rainy season there. Then, the ridge retreated southward and there was significant rainfall in the region. This gave rise to the question of whether this was the summer-type rainfall pattern that is common after the first rainy season or the second rainy season. Some meteorologists even argued that the rainy period in late June was not a true rainy season.[7][8][9][10][11]

See also edit

References edit

  1. ^ a b Owen, Stephen [translator & editor], Warner, Ding Xiang [editor], Kroll, Paul [editor] (2016). The Poetry of Du Fu 2019-05-20 at the Wayback Machine  , Volume 2. De Gruyter Mouton. Pages 298–299. ISBN 978-1-5015-0189-0
  2. ^ a b Lu Dian's Piya (published in the Song dynasty). Cited in Sargent, Stuart Howard (2007). The Poetry of He Zhu (1052-1125): Genres, Contexts, and Creativity. Brill. p. 18. ISBN 978-90-04-15711-8.
  3. ^ 내일 첫 장맛비…올 장마 짧지만 굵다 (in Korean). KBS News. 2019-06-25. Retrieved 2021-10-14.
  4. ^ [1] 2006-04-27 at the Wayback Machine
  5. ^ . Archived from the original on 2013-03-10. Retrieved 2011-05-13.
  6. ^ a b Rainy Season (Tsuyu), japan-guide.com
  7. ^ (in Chinese). Xinhuanet. 2005-07-14. Archived from the original on 2011-07-18. Retrieved 2008-05-07.
  8. ^ 倒黄梅?二度梅? 有关专家认为再下就要变成梅雨 (in Chinese). Sina. 2005-07-09. Retrieved 2008-05-07.
  9. ^ 是"倒黄梅"还是"二度梅"?接连阴雨让专家直挠头 (in Chinese). Sina. 2005-07-08. Retrieved 2008-05-07.
  10. ^ (in Chinese). CNHYC. 2005-07-17. Archived from the original on 2007-03-11. Retrieved 2008-05-07.
  11. ^ (in Chinese). 新华报业网. 2005-07-12. Archived from the original on 2008-05-25. Retrieved 2008-05-07.

east, asian, rainy, season, chinese, japanese, 梅雨, pinyin, méiyǔ, rōmaji, tsuyu, baiu, korean, 장마, romaja, jangma, also, called, plum, rain, caused, precipitation, along, persistent, stationary, front, known, meiyu, front, nearly, months, during, late, spring,. The East Asian rainy season Chinese and Japanese 梅雨 pinyin meiyǔ rōmaji tsuyu baiu Korean 장마 romaja jangma also called the plum rain is caused by precipitation along a persistent stationary front known as the Meiyu front for nearly two months during the late spring and early summer in East Asia between mainland China Taiwan Korea and Japan The wet season ends during the summer when the subtropical ridge becomes strong enough to push this front north of the region These weather systems can produce heavy rainfall and flooding Plum rain falling on two clear umbrellas looking up toward the Tokyo Metropolitan Government Building in June 2009 East Asian rainy seasonChinese nameChinese梅雨Literal meaningplum rainTranscriptionsStandard MandarinHanyu PinyinmeiyǔBopomofoㄇㄟˊㄩˇIPAmeiɥỳHakkaRomanizationmoi yiYue CantoneseJyutpingmui4 jyu5IPAmu ːy jy ːSouthern MinHokkien POJmui u boe iKorean nameHangul장마Hanja長마TranscriptionsRevised RomanizationjangmaJapanese nameKanji梅雨Kanaつゆ ばいうHiraganaつゆ ばいうKatakanaツユ バイウTranscriptionsRevised Hepburntsuyu baiuKunrei shikituyu baiuRussian nameRussianVostochno aziatskij sezon dozhdej Contents 1 Etymology 2 Formation 3 Effects 3 1 Japan 3 2 Korea 4 Timing 5 See also 6 ReferencesEtymology editIn China the term plum rain was used for the rain in the fourth and fifth lunar month 1 2 It specifically refers to the historical belief that when the plums turn yellow and fall at the south of the Yangtze in the fourth and fifth months the moisture that evaporates from the plant turns into rain 2 The term appears in the following poem by Du Fu fl 8th century of the Tang dynasty 梅雨 南京犀浦道 四月熟黃梅 湛湛長江去 冥冥細雨來 茅茨疏易溼 雲霧密難開 竟日蛟龍喜 盤渦與岸迴 Plum rain On the Xipu road from the Southern Capital present day Chengdu the fourth month ripens the yellow p r unus The long river goes off surging and darkening a fine rain comes Roof thatch loosely bound is easily soaked clouds and fog are dense and will not lift All day long the dragons delight whirlpools turning with the bank 1 Japan later adapted and transliterated the Chinese term plum rain to call the rainy season tsuyu 梅雨 The season is instead commonly called Jangma 장마 in Korea which means long rain The term was originally spelled Dyangmah 댱맣 in 1500s which was the mix of the hanja character 長 long and the old native Korean word 맣 mah rain The word Dyangmah eventually transformed from Jyangma 쟝마 in 1700s to the current form of Jangma after the 1900s 3 Formation editAn east west zone of disturbed weather during spring along this front stretches from the east China coast initially across Taiwan and Okinawa later when it has shifted to the north eastward into the southern peninsula of South Korea and Japan 4 In Taiwan and Okinawa the rainy season usually lasts from May to June 5 In Russian Primorsky Krai Japan and Korea it lasts from June to July approximately 50 days In eastern China especially the Yangtze and Huai River regions it lasts from July to August citation needed The weather front forms when the moist air over the Pacific meets the cooler continental air mass The front and the formation of frontal depressions along it brings precipitation to Primorsky Krai Japan Korea eastern China and Taiwan As the front moves back and forth depending on the strength of cool and warm air masses there is often prolonged precipitation and sometimes flooding in eastern China However in the years that it does not rain as much as usual a drought might result The rainy season ends when the warm air mass associated with the subtropical ridge is strong enough to push the front north and away citation needed Effects editThe high humidity in the air during this season encourages the formation of mold and rot not only on food but on fabrics as well Environmentally heavy rains encourage mudslides and flooding in all areas affected The most rain in a one hour period as recorded in Japan was in Nagasaki in 1982 with 153 millimetres 6 0 in The highest overall recorded rainfall during the rainy season in Japan was in 2003 when Miyazaki Prefecture recorded rains of 8 670 millimetres 341 in citation needed Japan edit In Japan the rainy season is called tsuyu 梅雨 and lasts from early June to mid July in most of the country Honshu Kyushu and Shikoku approximately June 7 to July 20 in the Kansai and Kantō regions in Honshu 6 The tsuyu season is roughly a month earlier early May through mid June in Okinawa the southernmost region of the country There is no pronounced tsuyu season in Hokkaidō the northernmost region of the country because the tsuyu front usually attenuates before it reaches the region so that it cannot produce the abundant rainfall Tsuyu is also known as Samidare 五月雨 literally the fifth month rain in the Japanese traditional calendar roughly corresponding to June in the modern calendar The pop artist Eiichi Ohtaki produced a popular song by this name and a Second World War Japanese naval ship was also given this name citation needed The rains in the middle of November early December are sometimes called the sazanka tsuyu literally rainy season of the camellia on account of the timing with the blossoming of the seasonal flower citation needed This period is generally avoided for tourism but some sights are considered particularly atmospheric in the rain and fog particularly mountain forests notably Sacred Sites and Pilgrimage Routes in the Kii Mountain Range including Mount Kōya 6 Vegetation especially moss is also rather lush at this time and hence sights known for their moss such as Saihō ji the moss temple are also popular at this time of year citation needed Korea edit The rainy season is between June and mid July It is caused by hot and humid high pressure forming in the Sea of Okhotsk due to the North Pacific anticyclone combining with Asiatic continental high pressure When the two meteorological events meet they form a long jangmajeonseon Korean 장마전선 from 장마 lit rainy season and 전선 前線 lit weather front Beginning in late May the North Pacific high pressure forces the weaker continental anticyclone south of Okinawa Island This fall to the south then reverses and gradually strengthens as it moves northwards back towards the Korean peninsula On landfall heavy monsoon rains lead to torrential downpours and flooding By August the system has weakened as the southern systems retreat towards the Philippine archipelago citation needed By early autumn the North Pacific high pressure system is pushed away as Asiatic continental cold high pressure moves southwards This produces inclement weather although not on the scale of the summer monsoons Korea can however be struck by typhoons during this period citation needed Timing editIn some years the rainy season s actual beginning and end are under debate For example in 2005 the subtropical ridge moved quickly northward in late June early July The weather front skipped the Yangtze region and there was no rainy season there Then the ridge retreated southward and there was significant rainfall in the region This gave rise to the question of whether this was the summer type rainfall pattern that is common after the first rainy season or the second rainy season Some meteorologists even argued that the rainy period in late June was not a true rainy season 7 8 9 10 11 See also editEast Asian Monsoon Meiyu front List of China related topics List of Japan related topics List of Taiwan related topicsReferences edit a b Owen Stephen translator amp editor Warner Ding Xiang editor Kroll Paul editor 2016 The Poetry of Du Fu Archived 2019 05 20 at the Wayback Machine nbsp Volume 2 De Gruyter Mouton Pages 298 299 ISBN 978 1 5015 0189 0 a b Lu Dian s Piya published in the Song dynasty Cited in Sargent Stuart Howard 2007 The Poetry of He Zhu 1052 1125 Genres Contexts and Creativity Brill p 18 ISBN 978 90 04 15711 8 내일 첫 장맛비 올 장마 짧지만 굵다 in Korean KBS News 2019 06 25 Retrieved 2021 10 14 1 Archived 2006 04 27 at the Wayback Machine Okinawa Travel Information Archived from the original on 2013 03 10 Retrieved 2011 05 13 a b Rainy Season Tsuyu japan guide com 入梅不像梅出梅梅更浓 梅雨 变味 真假难辨 in Chinese Xinhuanet 2005 07 14 Archived from the original on 2011 07 18 Retrieved 2008 05 07 倒黄梅 二度梅 有关专家认为再下就要变成梅雨 in Chinese Sina 2005 07 09 Retrieved 2008 05 07 是 倒黄梅 还是 二度梅 接连阴雨让专家直挠头 in Chinese Sina 2005 07 08 Retrieved 2008 05 07 上海是否出现了 倒黄梅 为啥视而不见 in Chinese CNHYC 2005 07 17 Archived from the original on 2007 03 11 Retrieved 2008 05 07 是倒黄梅还是二度梅 in Chinese 新华报业网 2005 07 12 Archived from the original on 2008 05 25 Retrieved 2008 05 07 nbsp Look up plum rain in Wiktionary the free dictionary Retrieved from https en wikipedia org w index php title East Asian rainy season amp oldid 1211957306, wikipedia, wiki, book, books, library,

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