Journal of Tropical Oceanography ›› 2023, Vol. 42 ›› Issue (2): 21-33.doi: 10.11978/2022067CSTR: 32234.14.2022067

Special Issue: 全球变化专题

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Assessment of El Niño diversity simulations using CMIP6 and CMIP5 models*

WANG Weiqiang1,2(), ZHANG Xiya1,3, XU Kang1,2, LI Junling1,3, MIAO Haoyu1,3   

  1. 1. State Key Laboratory of Tropical Oceanography (South China Sea Institute of Oceanology, Chinese Academy of Sciences), Guangzhou 510301, China
    2. Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou), Guangzhou 511458, China
    3. University of Chinese Academy of Sciences, Beijing 100049, China
  • Received:2022-04-07 Revised:2022-05-24 Online:2023-03-10 Published:2022-05-24
  • Contact: WANG Weiqiang. email: weiqiang.wang@scsio.ac.cn
  • Supported by:
    National Natural Science Foundation of China(42076020); Open Fund of Key Laboratory of Marine Science and Numerical Modeling, Ministry of Natural Resources(2020-ZD-04); Youth Innovation Promotion Association CAS(2020340); Hainan Province Science and Technology Special Fund(ZDYF2020174); Rising Star Foundation of the South China Sea Institute of Oceanology(NHXX2018WL0201); Key Special Project for Introduced Talents Team of Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou)(GML2019ZD0306); Independent Research Project Program of State Key Laboratory of Tropical Oceanography(LTOZZ2101)

Abstract:

Based on the observations and the global climate model simulation outputs of historical run and future warming scenarios from phase 5 and phase 6 of the coupled model intercomparison project (CMIP), we assessed the performance of 23 CMIP6 and 32 CMIP5 models in reproducing El Niño diversity, and then projected the responses of the eastern Pacific (EP) and central Pacific (CP) type of El Niño to global warming. The results show that most CMIP5/6 models can reasonably simulate the characteristics of El Niño diversity, and the simulation performance of CMIP6 models is significantly improved compared with CMIP5 models. Not only do the CMIP6 models weaken the discreteness of the simulated EP El Niño-related spatial patterns, but also significantly improve the simulation ability of the CP El Niño-associated spatial patterns. The CMIP5/6 models can basically simulate the seasonal phase-locking characteristics of the EP and CP El Niño events, however, compared to the observation, the decay time of the simulated CP El Niño is obviously delayed by 3 months. The intensity of EP El Niño simulated by CMIP5/6 is close to the observation, but the counterpart of CP El Niño is stronger than the observation. Under global warming, the frequency of CP El Niño will tend to decrease relative to EP El Niño. The amplitudes of EP and CP El Niño will be enhanced along with the intensification of global warming, and the enhanced amplitude of EP El Niño is greatly stronger than that of CP El Niño.

Key words: CMIP5/6 climate models, Eastern Pacific El Niño, Central Pacific El Niño, global warming, Future projection