An aftereffect of global warming on tropical Pacific decadal variability

郑建; 刘秦玉; 王传阳

doi:10.1007/s00343-017-6267-2

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An aftereffect of global warming on tropical Pacific decadal variability

Physics | Updated：2023-05-19

- An aftereffect of global warming on tropical Pacific decadal variability
- An aftereffect of global warming on tropical Pacific decadal variability
- 海洋湖沼学报（英文） 2018年36卷第2期页码：193-204
- Affiliations：
  
  1.Key Laboratory of Ocean Circulation and Wave, Institute of Oceanology, Chinese Academy of Sciences, Qingdao, China, and Laboratory for Ocean and Climate Dynamics, Qingdao National Laboratory for Marine Science and Technology, Qingdao 266071, China
  2.Physical Oceanography Laboratory/Qingdao Collaborative Innovation Center of Marine Science and Technology, Key Laboratory of Ocean-Atmosphere Interaction and Climate in Universities of Shandong, Ocean University of China, Qingdao 266000, China
- Author bio：
  
  ZHENG Jian, zhengjian@qdio.ac.cn
- Funds：
  
  the Strategic Priority Project of CAS(XDA11010102);the National Natural Science Foundation of China(41490643);the National Natural Science Foundation of China(41606018);the National Natural Science Foundation of China(41421005);the NSFC-Shandong Joint Fund for Marine Science Research Centers(U1406401)
- DOI：10.1007/s00343-017-6267-2
  中图分类号：
- 收稿：2016-10-08，
  
  录用：2016-11-21，
  
  网络首发：2018-01-04，
  
  纸质出版：2018-03
- Accepted：
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郑建, 刘秦玉, 王传阳. An aftereffect of global warming on tropical Pacific decadal variability[J]. 海洋湖沼学报（英文）, 2018,36(2):193-204.

Jian ZHENG, Qinyu LIU, Chuanyang WANG. An aftereffect of global warming on tropical Pacific decadal variability[J]. Chinese Journal of Oceanology and Limnology, 2018, 36(2): 193-204.
郑建, 刘秦玉, 王传阳. An aftereffect of global warming on tropical Pacific decadal variability[J]. 海洋湖沼学报（英文）, 2018,36(2):193-204. DOI： 10.1007/s00343-017-6267-2.

Jian ZHENG, Qinyu LIU, Chuanyang WANG. An aftereffect of global warming on tropical Pacific decadal variability[J]. Chinese Journal of Oceanology and Limnology, 2018, 36(2): 193-204. DOI： 10.1007/s00343-017-6267-2.

摘要

Abstract

Studies have shown that global warming over the past six decades can weaken the tropical Pacific Walker circulation and maintain the positive phase of the Interdecadal Pacific Oscillation (IPO). Based on observations and model simulations

another aftereffect of global warming on IPO is found. After removing linear trends (global warming signals) from observations

however

the tropical Pacific climate still exhibited some obvious differences between two IPO negative phases. The boreal winter (DJF) equatorial central-eastern Pacific sea surface temperature (SST) was colder during the 1999-2014 period (P2) than that during 1961-1976 (P1). This difference may have been a result of global warming nonlinear modulation of precipitation; i.e.

in the climatological rainy region

the core area of the tropical Indo-western Pacific warm pool receives more precipitation through the "wet-get-wetter" mechanism. Positive precipitation anomalies in the warm pool during P2 are much stronger than those during P1

even after subtracting the linear trend. Corresponding to the differences of precipitation

the Pacific Walker circulation is stronger in P2 than in P1. Consequent easterly winds over the equatorial Pacific led to a colder equatorial eastern-central Pacific during P2. Therefore

tropical Pacific climate differences between the two negative IPO phases are aftereffects of global warming. These aftereffects are supported by the results of coupled climate model experiments

with and without global warming.

关键词

Keywords

references

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