The Southwest China Flood of July 2018 and Its Causes

Excessive rainfall was observed over Southwest China in July 2018, leading to floods in several major tributaries of the Yangtze River and landslide and debris flow in the neighboring provinces. The rainfall during 7−11 July was unusually heavy and broke the record that can be traced back to 1961. T...
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Autor*in:	Lijuan Wang [verfasserIn] Lin Wang [verfasserIn] Yuyun Liu [verfasserIn] Wei Gu [verfasserIn] Peiqiang Xu [verfasserIn] Wen Chen [verfasserIn]

Format:	E-Artikel
Sprache:	Englisch

Erschienen:	2019

Schlagwörter:	El Niño-Southern Oscillation (ENSO) East Asian summer monsoon rainfall Pacific-Japan (PJ) pattern

Übergeordnetes Werk:	In: Atmosphere - MDPI AG, 2011, 10(2019), 5, p 247
Übergeordnetes Werk:	volume:10 ; year:2019 ; number:5, p 247

Links:	Link aufrufen Link aufrufen Link aufrufen Journal toc

DOI / URN:	10.3390/atmos10050247

Katalog-ID:	DOAJ031636543

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520			\|a Excessive rainfall was observed over Southwest China in July 2018, leading to floods in several major tributaries of the Yangtze River and landslide and debris flow in the neighboring provinces. The rainfall during 7−11 July was unusually heavy and broke the record that can be traced back to 1961. The occurrence of the excessive rain can be attributed to the anomalous convection over the western North Pacific and the presence of a mid-latitude Rossby wave train. On one hand, the convection over the western North Pacific was anomalously strong in July 2018, and it could have excited the negative phase of the Pacific−Japan pattern and led to a northwestward shift of the western Pacific subtropical high. Hence, the water vapor transport toward inland China including Southwest China was enhanced, providing a favorable moisture environment for precipitation. On the other hand, a mid-latitude Rossby wave train was observed to propagate from Northern Europe towards East Asia, which was conducive to anomalous ascending motion over Southwest China via warm advection and differential vorticity advection, creating a favorable dynamical condition for precipitation. As a result, the combination of the two effects mentioned above led to the occurrence of the flood over Southwest China in July 2018.
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spelling	10.3390/atmos10050247 doi (DE-627)DOAJ031636543 (DE-599)DOAJc8236f275d574382800e5065b2bf6517 DE-627 ger DE-627 rakwb eng QC851-999 Lijuan Wang verfasserin aut The Southwest China Flood of July 2018 and Its Causes 2019 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Excessive rainfall was observed over Southwest China in July 2018, leading to floods in several major tributaries of the Yangtze River and landslide and debris flow in the neighboring provinces. The rainfall during 7−11 July was unusually heavy and broke the record that can be traced back to 1961. The occurrence of the excessive rain can be attributed to the anomalous convection over the western North Pacific and the presence of a mid-latitude Rossby wave train. On one hand, the convection over the western North Pacific was anomalously strong in July 2018, and it could have excited the negative phase of the Pacific−Japan pattern and led to a northwestward shift of the western Pacific subtropical high. Hence, the water vapor transport toward inland China including Southwest China was enhanced, providing a favorable moisture environment for precipitation. On the other hand, a mid-latitude Rossby wave train was observed to propagate from Northern Europe towards East Asia, which was conducive to anomalous ascending motion over Southwest China via warm advection and differential vorticity advection, creating a favorable dynamical condition for precipitation. As a result, the combination of the two effects mentioned above led to the occurrence of the flood over Southwest China in July 2018. El Niño-Southern Oscillation (ENSO) East Asian summer monsoon rainfall Pacific-Japan (PJ) pattern Meteorology. Climatology Lin Wang verfasserin aut Yuyun Liu verfasserin aut Wei Gu verfasserin aut Peiqiang Xu verfasserin aut Wen Chen verfasserin aut In Atmosphere MDPI AG, 2011 10(2019), 5, p 247 (DE-627)657584010 (DE-600)2605928-9 20734433 nnns volume:10 year:2019 number:5, p 247 https://doi.org/10.3390/atmos10050247 kostenfrei https://doaj.org/article/c8236f275d574382800e5065b2bf6517 kostenfrei https://www.mdpi.com/2073-4433/10/5/247 kostenfrei https://doaj.org/toc/2073-4433 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2014 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 10 2019 5, p 247
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allfieldsGer	10.3390/atmos10050247 doi (DE-627)DOAJ031636543 (DE-599)DOAJc8236f275d574382800e5065b2bf6517 DE-627 ger DE-627 rakwb eng QC851-999 Lijuan Wang verfasserin aut The Southwest China Flood of July 2018 and Its Causes 2019 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Excessive rainfall was observed over Southwest China in July 2018, leading to floods in several major tributaries of the Yangtze River and landslide and debris flow in the neighboring provinces. The rainfall during 7−11 July was unusually heavy and broke the record that can be traced back to 1961. The occurrence of the excessive rain can be attributed to the anomalous convection over the western North Pacific and the presence of a mid-latitude Rossby wave train. On one hand, the convection over the western North Pacific was anomalously strong in July 2018, and it could have excited the negative phase of the Pacific−Japan pattern and led to a northwestward shift of the western Pacific subtropical high. Hence, the water vapor transport toward inland China including Southwest China was enhanced, providing a favorable moisture environment for precipitation. On the other hand, a mid-latitude Rossby wave train was observed to propagate from Northern Europe towards East Asia, which was conducive to anomalous ascending motion over Southwest China via warm advection and differential vorticity advection, creating a favorable dynamical condition for precipitation. As a result, the combination of the two effects mentioned above led to the occurrence of the flood over Southwest China in July 2018. El Niño-Southern Oscillation (ENSO) East Asian summer monsoon rainfall Pacific-Japan (PJ) pattern Meteorology. Climatology Lin Wang verfasserin aut Yuyun Liu verfasserin aut Wei Gu verfasserin aut Peiqiang Xu verfasserin aut Wen Chen verfasserin aut In Atmosphere MDPI AG, 2011 10(2019), 5, p 247 (DE-627)657584010 (DE-600)2605928-9 20734433 nnns volume:10 year:2019 number:5, p 247 https://doi.org/10.3390/atmos10050247 kostenfrei https://doaj.org/article/c8236f275d574382800e5065b2bf6517 kostenfrei https://www.mdpi.com/2073-4433/10/5/247 kostenfrei https://doaj.org/toc/2073-4433 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2014 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 10 2019 5, p 247
allfieldsSound	10.3390/atmos10050247 doi (DE-627)DOAJ031636543 (DE-599)DOAJc8236f275d574382800e5065b2bf6517 DE-627 ger DE-627 rakwb eng QC851-999 Lijuan Wang verfasserin aut The Southwest China Flood of July 2018 and Its Causes 2019 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Excessive rainfall was observed over Southwest China in July 2018, leading to floods in several major tributaries of the Yangtze River and landslide and debris flow in the neighboring provinces. The rainfall during 7−11 July was unusually heavy and broke the record that can be traced back to 1961. The occurrence of the excessive rain can be attributed to the anomalous convection over the western North Pacific and the presence of a mid-latitude Rossby wave train. On one hand, the convection over the western North Pacific was anomalously strong in July 2018, and it could have excited the negative phase of the Pacific−Japan pattern and led to a northwestward shift of the western Pacific subtropical high. Hence, the water vapor transport toward inland China including Southwest China was enhanced, providing a favorable moisture environment for precipitation. On the other hand, a mid-latitude Rossby wave train was observed to propagate from Northern Europe towards East Asia, which was conducive to anomalous ascending motion over Southwest China via warm advection and differential vorticity advection, creating a favorable dynamical condition for precipitation. As a result, the combination of the two effects mentioned above led to the occurrence of the flood over Southwest China in July 2018. El Niño-Southern Oscillation (ENSO) East Asian summer monsoon rainfall Pacific-Japan (PJ) pattern Meteorology. Climatology Lin Wang verfasserin aut Yuyun Liu verfasserin aut Wei Gu verfasserin aut Peiqiang Xu verfasserin aut Wen Chen verfasserin aut In Atmosphere MDPI AG, 2011 10(2019), 5, p 247 (DE-627)657584010 (DE-600)2605928-9 20734433 nnns volume:10 year:2019 number:5, p 247 https://doi.org/10.3390/atmos10050247 kostenfrei https://doaj.org/article/c8236f275d574382800e5065b2bf6517 kostenfrei https://www.mdpi.com/2073-4433/10/5/247 kostenfrei https://doaj.org/toc/2073-4433 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2014 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 10 2019 5, p 247
language	English
source	In Atmosphere 10(2019), 5, p 247 volume:10 year:2019 number:5, p 247
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authorswithroles_txt_mv	Lijuan Wang @@aut@@ Lin Wang @@aut@@ Yuyun Liu @@aut@@ Wei Gu @@aut@@ Peiqiang Xu @@aut@@ Wen Chen @@aut@@
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callnumber-first	Q - Science
author	Lijuan Wang
spellingShingle	Lijuan Wang misc QC851-999 misc El Niño-Southern Oscillation (ENSO) misc East Asian summer monsoon misc rainfall misc Pacific-Japan (PJ) pattern misc Meteorology. Climatology The Southwest China Flood of July 2018 and Its Causes
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topic_title	QC851-999 The Southwest China Flood of July 2018 and Its Causes El Niño-Southern Oscillation (ENSO) East Asian summer monsoon rainfall Pacific-Japan (PJ) pattern
topic	misc QC851-999 misc El Niño-Southern Oscillation (ENSO) misc East Asian summer monsoon misc rainfall misc Pacific-Japan (PJ) pattern misc Meteorology. Climatology
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title	The Southwest China Flood of July 2018 and Its Causes
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title_full	The Southwest China Flood of July 2018 and Its Causes
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title_sort	southwest china flood of july 2018 and its causes
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title_auth	The Southwest China Flood of July 2018 and Its Causes
abstract	Excessive rainfall was observed over Southwest China in July 2018, leading to floods in several major tributaries of the Yangtze River and landslide and debris flow in the neighboring provinces. The rainfall during 7−11 July was unusually heavy and broke the record that can be traced back to 1961. The occurrence of the excessive rain can be attributed to the anomalous convection over the western North Pacific and the presence of a mid-latitude Rossby wave train. On one hand, the convection over the western North Pacific was anomalously strong in July 2018, and it could have excited the negative phase of the Pacific−Japan pattern and led to a northwestward shift of the western Pacific subtropical high. Hence, the water vapor transport toward inland China including Southwest China was enhanced, providing a favorable moisture environment for precipitation. On the other hand, a mid-latitude Rossby wave train was observed to propagate from Northern Europe towards East Asia, which was conducive to anomalous ascending motion over Southwest China via warm advection and differential vorticity advection, creating a favorable dynamical condition for precipitation. As a result, the combination of the two effects mentioned above led to the occurrence of the flood over Southwest China in July 2018.
abstractGer	Excessive rainfall was observed over Southwest China in July 2018, leading to floods in several major tributaries of the Yangtze River and landslide and debris flow in the neighboring provinces. The rainfall during 7−11 July was unusually heavy and broke the record that can be traced back to 1961. The occurrence of the excessive rain can be attributed to the anomalous convection over the western North Pacific and the presence of a mid-latitude Rossby wave train. On one hand, the convection over the western North Pacific was anomalously strong in July 2018, and it could have excited the negative phase of the Pacific−Japan pattern and led to a northwestward shift of the western Pacific subtropical high. Hence, the water vapor transport toward inland China including Southwest China was enhanced, providing a favorable moisture environment for precipitation. On the other hand, a mid-latitude Rossby wave train was observed to propagate from Northern Europe towards East Asia, which was conducive to anomalous ascending motion over Southwest China via warm advection and differential vorticity advection, creating a favorable dynamical condition for precipitation. As a result, the combination of the two effects mentioned above led to the occurrence of the flood over Southwest China in July 2018.
abstract_unstemmed	Excessive rainfall was observed over Southwest China in July 2018, leading to floods in several major tributaries of the Yangtze River and landslide and debris flow in the neighboring provinces. The rainfall during 7−11 July was unusually heavy and broke the record that can be traced back to 1961. The occurrence of the excessive rain can be attributed to the anomalous convection over the western North Pacific and the presence of a mid-latitude Rossby wave train. On one hand, the convection over the western North Pacific was anomalously strong in July 2018, and it could have excited the negative phase of the Pacific−Japan pattern and led to a northwestward shift of the western Pacific subtropical high. Hence, the water vapor transport toward inland China including Southwest China was enhanced, providing a favorable moisture environment for precipitation. On the other hand, a mid-latitude Rossby wave train was observed to propagate from Northern Europe towards East Asia, which was conducive to anomalous ascending motion over Southwest China via warm advection and differential vorticity advection, creating a favorable dynamical condition for precipitation. As a result, the combination of the two effects mentioned above led to the occurrence of the flood over Southwest China in July 2018.
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title_short	The Southwest China Flood of July 2018 and Its Causes
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The Southwest China Flood of July 2018 and Its Causes

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