The asymmetric response of Yangtze river basin summer rainfall to El Niño/La Niña

The Yangtze river basin, in South East China, experiences anomalously high precipitation in summers following El Niño. This can lead to extensive flooding and loss of life. However, the response following La Niña has not been well documented. In this study, the response of Yangtze summer rainfall to...

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Main Authors: Steven C Hardiman, Nick J Dunstone, Adam A Scaife, Philip E Bett, Chaofan Li, Bo Lu, Hong-Li Ren, Doug M Smith, Claudia C Stephan
Format: Article
Language:English
Published: IOP Publishing 2018-01-01
Series:Environmental Research Letters
Subjects:
Online Access:https://doi.org/10.1088/1748-9326/aaa172
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author Steven C Hardiman
Nick J Dunstone
Adam A Scaife
Philip E Bett
Chaofan Li
Bo Lu
Hong-Li Ren
Doug M Smith
Claudia C Stephan
author_facet Steven C Hardiman
Nick J Dunstone
Adam A Scaife
Philip E Bett
Chaofan Li
Bo Lu
Hong-Li Ren
Doug M Smith
Claudia C Stephan
author_sort Steven C Hardiman
collection DOAJ
description The Yangtze river basin, in South East China, experiences anomalously high precipitation in summers following El Niño. This can lead to extensive flooding and loss of life. However, the response following La Niña has not been well documented. In this study, the response of Yangtze summer rainfall to El Niño/La Niña is found to be asymmetric, with no significant response following La Niña. The nature of this asymmetric response is found to be in good agreement with that simulated by the Met Office seasonal forecast system. Yangtze summer rainfall correlates positively with spring sea surface temperatures in the Indian Ocean and northwest Pacific. Indian Ocean sea surface temperatures are found to respond linearly to El Niño/La Niña, and to have a linear impact on Yangtze summer rainfall. However, northwest Pacific sea surface temperatures respond much more strongly following El Niño and, further, correlate more strongly with positive rainfall years. It is concluded that, whilst delayed Indian Ocean signals may influence summer Yangtze rainfall, it is likely that they do not lead to the asymmetric nature of the rainfall response to El Niño/La Niña.
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spelling doaj.art-4893c1d62f1e4459856c468c3bd858d92023-08-09T14:37:52ZengIOP PublishingEnvironmental Research Letters1748-93262018-01-0113202401510.1088/1748-9326/aaa172The asymmetric response of Yangtze river basin summer rainfall to El Niño/La NiñaSteven C Hardiman0https://orcid.org/0000-0001-9813-1209Nick J Dunstone1Adam A Scaife2Philip E Bett3https://orcid.org/0000-0002-4508-7192Chaofan Li4Bo Lu5Hong-Li Ren6Doug M Smith7Claudia C Stephan8Met Office , FitzRoy Road, Exeter, Devon, United Kingdom; Author to whom any correspondence should be addressed.Met Office , FitzRoy Road, Exeter, Devon, United KingdomMet Office , FitzRoy Road, Exeter, Devon, United Kingdom; College of Engineering, Mathematics and Physical Sciences, University of Exeter , Exeter, Devon, United KingdomMet Office , FitzRoy Road, Exeter, Devon, United KingdomCenter for Monsoon System Research, Institute of Atmospheric Physics, Chinese Academy of Sciences , Beijing, People’s Republic of ChinaLaboratory for Climate Studies, National Climate Center, China Meteorological Administration , Beijing, People’s Republic of ChinaLaboratory for Climate Studies, National Climate Center, China Meteorological Administration , Beijing, People’s Republic of ChinaMet Office , FitzRoy Road, Exeter, Devon, United KingdomDepartment of Meteorology, University of Reading , Reading, United KingdomThe Yangtze river basin, in South East China, experiences anomalously high precipitation in summers following El Niño. This can lead to extensive flooding and loss of life. However, the response following La Niña has not been well documented. In this study, the response of Yangtze summer rainfall to El Niño/La Niña is found to be asymmetric, with no significant response following La Niña. The nature of this asymmetric response is found to be in good agreement with that simulated by the Met Office seasonal forecast system. Yangtze summer rainfall correlates positively with spring sea surface temperatures in the Indian Ocean and northwest Pacific. Indian Ocean sea surface temperatures are found to respond linearly to El Niño/La Niña, and to have a linear impact on Yangtze summer rainfall. However, northwest Pacific sea surface temperatures respond much more strongly following El Niño and, further, correlate more strongly with positive rainfall years. It is concluded that, whilst delayed Indian Ocean signals may influence summer Yangtze rainfall, it is likely that they do not lead to the asymmetric nature of the rainfall response to El Niño/La Niña.https://doi.org/10.1088/1748-9326/aaa172seasonal forecastingYangtze basin rainfallENSOasymmetric rainfall responseIndian Ocean
spellingShingle Steven C Hardiman
Nick J Dunstone
Adam A Scaife
Philip E Bett
Chaofan Li
Bo Lu
Hong-Li Ren
Doug M Smith
Claudia C Stephan
The asymmetric response of Yangtze river basin summer rainfall to El Niño/La Niña
Environmental Research Letters
seasonal forecasting
Yangtze basin rainfall
ENSO
asymmetric rainfall response
Indian Ocean
title The asymmetric response of Yangtze river basin summer rainfall to El Niño/La Niña
title_full The asymmetric response of Yangtze river basin summer rainfall to El Niño/La Niña
title_fullStr The asymmetric response of Yangtze river basin summer rainfall to El Niño/La Niña
title_full_unstemmed The asymmetric response of Yangtze river basin summer rainfall to El Niño/La Niña
title_short The asymmetric response of Yangtze river basin summer rainfall to El Niño/La Niña
title_sort asymmetric response of yangtze river basin summer rainfall to el nino la nina
topic seasonal forecasting
Yangtze basin rainfall
ENSO
asymmetric rainfall response
Indian Ocean
url https://doi.org/10.1088/1748-9326/aaa172
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