IOCAS-IR  > 海洋环流与波动重点实验室
Synergistic interdecadal effects of the North Pacific and North Atlantic SST on precipitation over eastern China as revealed in the ECHAM5 simulations
Wu, Minmin1; Zhang, Rong-Hua2,3; Zhi, Hai1; Hu, Junya3,4
2024-08-01
发表期刊CLIMATE DYNAMICS
ISSN0930-7575
页码23
通讯作者Zhang, Rong-Hua([email protected])
摘要In this investigation, we examine individual and synergistic effects of sea surface temperature (SST) in the North Pacific and North Atlantic on precipitation interdecadal variations over eastern China using the Multi-Taper Method-Singular Value Decomposition (MTM-SVD) method and the European Center Hamburg model version 5 (ECHAM5) simulations. Results reveal that the model adequately reproduces the quasi-periodic precipitation responses corresponding to interdecadal SST forcing in the North Pacific, North Atlantic and both regions. The Pacific Decadal Oscillation (PDO) is closely related to a meridional tri-polar precipitation pattern over eastern China, which is attributed to the western Pacific subtropical high and surface pressure anomalies over northern East Asia, influenced by the joint effects of a mid-latitude wave train and SST anomalies in the central-western North Pacific. The North Atlantic basin-scale SST (NABS) correlates positively with precipitation over North China and negatively with precipitation over Southwest China. This precipitation pattern is affected by the westward shift of the atmospheric activity center over East Asia associated with the mid-latitude wave train across Eurasia. The combined SST forcing from both the North Pacific and North Atlantic results in a meridional precipitation dipole pattern, and partially explains the precipitation interdecadal variation as observed. That is, as the PDO warm phase transitions to the NABS warm phase, rainbands experience an interdecadal northward shift from South China to North China. These results are pivotal for understanding how interdecadal SST forcing in the North Pacific and North Atlantic influences the precipitation distribution over China, thereby contributing to improvements in interdecadal climate prediction.
关键词Precipitation over eastern China MTM-SVD method Interdecadal variation Sea surface temperature (SST) ECHAM5 simulations
DOI10.1007/s00382-024-07334-8
收录类别SCI
语种英语
资助项目National Natural Science Foundation of China[42030410]; National Natural Science Foundation of China (NSFC)[XDB40000000]; Strategic Priority Research Program of the Chinese Academy of Sciences (CAS)[LSKJ202202403]; Strategic Priority Research Program of the Chinese Academy of Sciences (CAS)[LSKJ202202402]; Startup Foundation for Introducing Talent of NUIST, Laoshan Laboratory[202346]; Jiangsu Innovation Research Group[2024ZB391]; Jiangsu Funding Program for Excellent Postdoctoral Talent
WOS研究方向Meteorology & Atmospheric Sciences
WOS类目Meteorology & Atmospheric Sciences
WOS记录号WOS:001284569200003
出版者SPRINGER
WOS关键词ASIAN SUMMER MONSOON ; INDIAN-OCEAN DIPOLE ; PART I ; CLIMATE VARIABILITY ; ENSO ; TEMPERATURE ; OSCILLATION ; IMPACTS ; ROLES ; PDO
引用统计
文献类型期刊论文
条目标识符http://ir.qdio.ac.cn/handle/337002/186181
专题海洋环流与波动重点实验室
通讯作者Zhang, Rong-Hua
作者单位1.Nanjing Univ Informat Sci & Technol, Sch Atmospher Sci, Nanjing 210044, Peoples R China
2.Nanjing Univ Informat Sci & Technol, Sch Marine Sci, Nanjing 210044, Peoples R China
3.Laoshan Lab, Qingdao 266237, Peoples R China
4.Chinese Acad Sci, Inst Oceanol, Key Lab Ocean Circulat & Waves, Qingdao 266071, Peoples R China
推荐引用方式
GB/T 7714
Wu, Minmin,Zhang, Rong-Hua,Zhi, Hai,et al. Synergistic interdecadal effects of the North Pacific and North Atlantic SST on precipitation over eastern China as revealed in the ECHAM5 simulations[J]. CLIMATE DYNAMICS,2024:23.
APA Wu, Minmin,Zhang, Rong-Hua,Zhi, Hai,&Hu, Junya.(2024).Synergistic interdecadal effects of the North Pacific and North Atlantic SST on precipitation over eastern China as revealed in the ECHAM5 simulations.CLIMATE DYNAMICS,23.
MLA Wu, Minmin,et al."Synergistic interdecadal effects of the North Pacific and North Atlantic SST on precipitation over eastern China as revealed in the ECHAM5 simulations".CLIMATE DYNAMICS (2024):23.
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