Reexamining the Indian Summer Monsoon Rainfall-ENSO Relationship From Its Recovery in the 21st Century: Role of the Indian Ocean SST Anomaly Associated With Types of ENSO Evolution

被引:34
作者
Yu, Shi-Yun [1 ,2 ]
Fan, Lei [1 ,2 ]
Zhang, Yu [1 ,3 ,4 ]
Zheng, Xiao-Tong [1 ,2 ,3 ,4 ]
Li, Ziguang [1 ,2 ,3 ,4 ]
机构
[1] Ocean Univ China, Collaborat Innovat Ctr Marine Sci & Technol, Phys Oceanog Lab, Qingdao, Peoples R China
[2] Ocean Univ China, Coll Ocean & Atmospher Sci, Qingdao, Peoples R China
[3] Ocean Univ China, Frontiers Sci Ctr Deep Ocean Multispheres & Earth, Qingdao, Peoples R China
[4] Qingdao Natl Lab Marine Sci & Technol, Qingdao, Peoples R China
基金
国家重点研发计划;
关键词
Indian summer monsoon rainfall; ENSO; Indian Ocean basin-wide SST anomaly; recovery; SEA-SURFACE TEMPERATURE; INDO-WESTERN PACIFIC; EL-NINO; CLIMATE; VARIABILITY; ATLANTIC; DIPOLE; IMPACT;
D O I
10.1029/2021GL092873
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
This study found that the relationship between the Indian Summer Monsoon Rainfall (ISMR) and El Nino-Southern Oscillation (ENSO) has recovered since 2001, and the relationship strength is closely related to the summer tropical Indian Ocean (TIO) sea surface temperature (SST) anomaly, with the TIO warming (cooling) indicating a stronger (weaker) relationship. Under the same El Nino/La Nina scenario, different signs of the TIO anomaly indicate distinct atmospheric circulation anomalies over the Indian Ocean, thus affecting the ISMR-ENSO relationship. The TIO anomaly is principally associated with different types of ENSO temporal evolution. Strong El Nino events with an early onset, and the transition of El Nino to La Nina, tend to have a warmer TIO and a stronger ISMR-ENSO relationship, in contrast to most of the cases of a decaying La Nina or a La Nina that persists throughout the year. The result brings a prospect for improving the ISMR prediction.
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页数:8
相关论文
共 41 条
[1]   Impact of Indian Ocean sea surface temperature on developing El Nino [J].
Annamalai, H ;
Xie, SP ;
McCreary, JP ;
Murtugudde, R .
JOURNAL OF CLIMATE, 2005, 18 (02) :302-319
[2]   Impact of the Indian Ocean Dipole on the relationship between the Indian monsoon rainfall and ENSO [J].
Ashok, K ;
Guan, ZY ;
Yamagata, T .
GEOPHYSICAL RESEARCH LETTERS, 2001, 28 (23) :4499-4502
[3]   Possible shift in the ENSO-Indian monsoon rainfall relationship under future global warming [J].
Azad, Sarita ;
Rajeevan, M. .
SCIENTIFIC REPORTS, 2016, 6
[4]   Sampling variability and the changing ENSO-monsoon relationship [J].
Cash, Benjamin A. ;
Barimalala, Rondrotiana ;
Kinter, James L., III ;
Altshuler, Eric L. ;
Fennessy, Michael J. ;
Manganello, Julia V. ;
Molteni, Franco ;
Towers, Peter ;
Vitart, Frederic .
CLIMATE DYNAMICS, 2017, 48 (11) :4071-4079
[5]  
Chang CP, 2001, J CLIMATE, V14, P2376, DOI 10.1175/1520-0442(2001)014<2376:PROACO>2.0.CO
[6]  
2
[7]   Indian Ocean warming during 1958-2004 simulated by a climate system model and its mechanism [J].
Dong, Lu ;
Zhou, Tianjun ;
Wu, Bo .
CLIMATE DYNAMICS, 2014, 42 (1-2) :203-217
[8]   Role of atmospheric adjustments in the tropical Indian Ocean warming during the 20th century in climate models [J].
Du, Yan ;
Xie, Shang-Ping .
GEOPHYSICAL RESEARCH LETTERS, 2008, 35 (08)
[9]   Role of Air-Sea Interaction in the Long Persistence of El Nino-Induced North Indian Ocean Warming [J].
Du, Yan ;
Xie, Shang-Ping ;
Huang, Gang ;
Hu, Kaiming .
JOURNAL OF CLIMATE, 2009, 22 (08) :2023-2038
[10]   Revisiting the relationship between the South Asian summer monsoon drought and El Nino warming pattern [J].
Fan, Fangxing ;
Dong, Xiao ;
Fang, Xianghui ;
Xue, Feng ;
Zheng, Fei ;
Zhu, Jiang .
ATMOSPHERIC SCIENCE LETTERS, 2017, 18 (04) :175-182