Influences of tropical Pacific and North Atlantic SST anomalies on summer drought over Asia

Present study investigates the characteristics and factors of summer drought variations over Asia during 1950–2020 using 3-month Standardized Precipitation Evapotranspiration Index (SPEI03) in July. The leading mode of Asian summer drought variations exhibits a roughly north–south contrasting distri...

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Vydáno v:	Climate dynamics Ročník 61; číslo 11-12; s. 5827 - 5844
Hlavní autoři:	Zhang, Jianmin, Wu, Renguang, Gu, Qinlu, Chen, Xinhai, Jia, Xiaojing, Zhang, Yanting
Médium:	Journal Article
Jazyk:	angličtina
Vydáno:	Berlin/Heidelberg Springer Berlin Heidelberg 01.12.2023 Springer Springer Nature B.V
Témata:	Agricultural production Anomalies Asia Climatology Drought Droughts Earth and Environmental Science Earth Sciences East Asia Environmental aspects evaporation evapotranspiration Geophysics/Geodesy Investigations latitude Ocean temperature Oceanography Precipitation Precipitation (Meteorology) Radiation Regions Sea surface Sea surface temperature anomalies sensible heat flux Soil moisture soil water spring summer surface water temperature terrestrial radiation Water shortages wind winter Asia East Asia Asian summer drought SST anomalies Atmospheric wave train Soil moisture Precipitation and temperature
ISSN:	0930-7575, 1432-0894
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Abstract	Present study investigates the characteristics and factors of summer drought variations over Asia during 1950–2020 using 3-month Standardized Precipitation Evapotranspiration Index (SPEI03) in July. The leading mode of Asian summer drought variations exhibits a roughly north–south contrasting distribution across 30° N with dominant interannual variability. The interannual variation of the leading mode is associated with both precipitation and temperature. In comparison, the contribution of precipitation is larger in the eastern part of the mid-latitude Asia. The Asian summer drought variations subject to both individual and combined impacts of preceding winter equatorial central-eastern Pacific (ECEP) sea surface temperature (SST) anomalies and concurrent North Atlantic (NA) tripole SST anomalies. Preceding ECEP SST anomalies induce anomalous vertical motion and precipitation over the mid-latitude Asia through large-scale divergence and convergence in previous winter and spring. The resulted soil moisture anomalies persist to summer and are conducive to anomalous summer precipitation through evaporation. The accompanying changes in cloud-radiation, surface longwave radiation and sensible heat flux induce temperature and evapotranspiration anomalies. The NA tripole SST anomalies induce anomalous vorticity forcing over the western mid-latitude NA. This contributes to a wave train that propagates from the NA to East Asia and affects wind and vertical motion over the mid-latitude Asia.
AbstractList	Present study investigates the characteristics and factors of summer drought variations over Asia during 1950-2020 using 3-month Standardized Precipitation Evapotranspiration Index (SPEI03) in July. The leading mode of Asian summer drought variations exhibits a roughly north-south contrasting distribution across 30° N with dominant interannual variability. The interannual variation of the leading mode is associated with both precipitation and temperature. In comparison, the contribution of precipitation is larger in the eastern part of the mid-latitude Asia. The Asian summer drought variations subject to both individual and combined impacts of preceding winter equatorial central-eastern Pacific (ECEP) sea surface temperature (SST) anomalies and concurrent North Atlantic (NA) tripole SST anomalies. Preceding ECEP SST anomalies induce anomalous vertical motion and precipitation over the mid-latitude Asia through large-scale divergence and convergence in previous winter and spring. The resulted soil moisture anomalies persist to summer and are conducive to anomalous summer precipitation through evaporation. The accompanying changes in cloud-radiation, surface longwave radiation and sensible heat flux induce temperature and evapotranspiration anomalies. The NA tripole SST anomalies induce anomalous vorticity forcing over the western mid-latitude NA. This contributes to a wave train that propagates from the NA to East Asia and affects wind and vertical motion over the mid-latitude Asia. Present study investigates the characteristics and factors of summer drought variations over Asia during 1950–2020 using 3-month Standardized Precipitation Evapotranspiration Index (SPEI03) in July. The leading mode of Asian summer drought variations exhibits a roughly north–south contrasting distribution across 30° N with dominant interannual variability. The interannual variation of the leading mode is associated with both precipitation and temperature. In comparison, the contribution of precipitation is larger in the eastern part of the mid-latitude Asia. The Asian summer drought variations subject to both individual and combined impacts of preceding winter equatorial central-eastern Pacific (ECEP) sea surface temperature (SST) anomalies and concurrent North Atlantic (NA) tripole SST anomalies. Preceding ECEP SST anomalies induce anomalous vertical motion and precipitation over the mid-latitude Asia through large-scale divergence and convergence in previous winter and spring. The resulted soil moisture anomalies persist to summer and are conducive to anomalous summer precipitation through evaporation. The accompanying changes in cloud-radiation, surface longwave radiation and sensible heat flux induce temperature and evapotranspiration anomalies. The NA tripole SST anomalies induce anomalous vorticity forcing over the western mid-latitude NA. This contributes to a wave train that propagates from the NA to East Asia and affects wind and vertical motion over the mid-latitude Asia.
Audience	Academic
Author	Wu, Renguang Chen, Xinhai Gu, Qinlu Jia, Xiaojing Zhang, Yanting Zhang, Jianmin
Author_xml	– sequence: 1 givenname: Jianmin surname: Zhang fullname: Zhang, Jianmin organization: School of Earth Sciences, Zhejiang University – sequence: 2 givenname: Renguang orcidid: 0000-0003-4712-2251 surname: Wu fullname: Wu, Renguang email: renguang@zju.edu.cn organization: School of Earth Sciences, Zhejiang University, Southern Marine Science and Engineering Guangdong Laboratory (Zhuhai) – sequence: 3 givenname: Qinlu surname: Gu fullname: Gu, Qinlu organization: School of Earth Sciences, Zhejiang University – sequence: 4 givenname: Xinhai surname: Chen fullname: Chen, Xinhai organization: School of Earth Sciences, Zhejiang University – sequence: 5 givenname: Xiaojing surname: Jia fullname: Jia, Xiaojing organization: School of Earth Sciences, Zhejiang University – sequence: 6 givenname: Yanting surname: Zhang fullname: Zhang, Yanting organization: College of Oceanic and Atmospheric Sciences, Ocean University of China, Key Laboratory of Physical Oceanography, Ocean University of China
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Snippet	Present study investigates the characteristics and factors of summer drought variations over Asia during 1950–2020 using 3-month Standardized Precipitation... Present study investigates the characteristics and factors of summer drought variations over Asia during 1950-2020 using 3-month Standardized Precipitation...
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SubjectTerms	Agricultural production Anomalies Asia Climatology Drought Droughts Earth and Environmental Science Earth Sciences East Asia Environmental aspects evaporation evapotranspiration Geophysics/Geodesy Investigations latitude Ocean temperature Oceanography Precipitation Precipitation (Meteorology) Radiation Regions Sea surface Sea surface temperature anomalies sensible heat flux Soil moisture soil water spring summer surface water temperature terrestrial radiation Water shortages wind winter
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Title	Influences of tropical Pacific and North Atlantic SST anomalies on summer drought over Asia
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