4.7 Article

Intermodel Uncertainty in the Change of ENSO's Amplitude under Global Warming: Role of the Response of Atmospheric Circulation to SST Anomalies

期刊

JOURNAL OF CLIMATE
卷 32, 期 2, 页码 369-383

出版社

AMER METEOROLOGICAL SOC
DOI: 10.1175/JCLI-D-18-0456.1

关键词

Atmosphere-ocean interaction; ENSO; Greenhouse gases; Tropical variability

资金

  1. National Natural Science Foundation of China [41706024, 41690121, 41690120, 41621064, 41575088, 41722504]
  2. Youth Innovation Promotion Association of CAS
  3. Fundamental Research Funds for the Central Universities

向作者/读者索取更多资源

This study investigates the mechanism of the large intermodel uncertainty in the change of ENSO's amplitude under global warming based on 31 CMIP5 models. We find that the uncertainty in ENSO's amplitude is significantly correlated to that of the change in the response of atmospheric circulation to SST anomalies (SSTAs) in the eastern equatorial Pacific Nino-3 region. This effect of the atmospheric response to SSTAs mainly influences the uncertainty in ENSO's amplitude during El Nino (EN) phases, but not during La Nina (LN) phases, showing pronounced nonlinearity. The effect of the relative SST warming and the present-day response of atmospheric circulation to SSTAs are the two major contributors to the intermodel spread of the change in the atmospheric response to SSTAs, of which the latter is more important. On the one hand, models with a stronger (weaker) mean-state SST warming in the eastern equatorial Pacific, relative to the tropical-mean warming, favor a larger (smaller) increase in the change in the response of atmospheric circulation to SSTAs in the eastern equatorial Pacific during EN. On the other hand, models with a weaker (stronger) present-day response of atmospheric circulation to SSTAs during EN tend to exhibit a larger (smaller) increase in the change under global warming. The result implies that an improved simulation of the present-day response of atmospheric circulation to SSTAs could be effective in lowering the uncertainty in ENSO's amplitude change under global warming.

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