CMIP6 模型中印度夏季季风对厄尔尼诺/南方涛动的不同影响及其可能原因

Shuheng Lin, Buwen Dong, Song Yang, Tuantuan Zhang
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引用次数: 0

摘要

本研究考察了耦合模式相互比较项目(CMIP6)第 6 阶段 52 个模式在捕捉印度夏季季风(ISM)对厄尔尼诺-南方涛动(ENSO)演变的影响方面的表现。印度夏季季候风对厄尔尼诺-南方涛动的影响在各种模式中表现出很大的差异。一些模式模拟的影响强度与观测结果相当,而另一些模式模拟的影响则要弱得多。结果表明,这种多样性与模式间 ISM 降水年际变率的差异有很大关系。ISM 降水变率较大的模式模拟了季风季节北太平洋西部降水和大气环流中 ISM 诱导的较强异常。因此,这些模式在西太平洋异常环流的南侧表现出更大的季风诱导的风异常,从而通过在热带太平洋上空造成更强的海气耦合过程,对随后的厄尔尼诺/南方涛动演变产生更显著的影响。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Diverse impacts of the Indian summer monsoon on ENSO among CMIP6 models and its possible causes
This study examines the performance of 52 models from phase 6 of the Coupled Model Intercomparison Project (CMIP6) in capturing the effects of the Indian summer monsoon (ISM) on the evolution of El Niño–Southern Oscillation (ENSO). The ISM’s impacts on ENSO show a substantial diversity among the models. While some models simulate the strength of the impacts comparable to observations, others represent much weaker influences. Results indicate that the diversity is highly related to inter-model spread in interannual variability of ISM rainfall among the models. Models with a larger ISM rainfall variability simulate stronger ISM-induced anomalies in precipitation and atmospheric circulation over the western North Pacific during the monsoon season. As a result, these models exhibit larger wind anomalies induced by monsoon on the south flank of the anomalous circulation in the western Pacific, thereby influencing subsequent ENSO evolution more significantly by causing stronger air-sea coupling processes over the tropical Pacific.
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