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Recent and future changes in the Asian monsoon-ENSO relationship: Natural or forced?

机译:亚洲季风与ENSO关系的近期和未来变化:自然还是强迫?

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摘要

The Asian monsoon-ENSO (El Nino-Southern Oscillation) relationship in the 20th and 21st centuries is examined using observations and Coupled Model Intercomparison Project Phase 5 (CMIP5) model simulations. CMIP5 models can simulate the ENSO-monsoon spatial structure reasonably well when using the multimodel mean. Running correlations show prominent decadal variability of the ENSO-monsoon relationship in observations. The modeled ENSO-monsoon relation shows large intermodel spread, indicating large variations across the model ensemble. The anthropogenically forced component of ENSO-monsoon relationship is separated from the naturally varying component based on a signal-to-noise maximizing empirical orthogonal function analysis using global sea surface temperature (SST). Results show that natural variability plays a dominant role in the varied ENSO-monsoon relationship during the 20th century. In the 21st century, the forced component is dominated by enhanced monsoon rainfall associated with SST warming, which may contribute to a slightly weakened ENSO-monsoon relation in the future.
机译:使用观测和耦合模型比较项目阶段5(CMIP5)模型模拟​​研究了20世纪和21世纪亚洲季风与ENSO(厄尔尼诺-南方涛动)的关系。使用多模型均值时,CMIP5模型可以很好地模拟ENSO季风空间结构。运行相关性在观测中显示出ENSO-季风关系的显着年代际变化。建模的ENSO-季风关系显示出较大的模型间分布,表明整个模型集合之间存在较大差异。基于信噪比最大化的经验正交函数分析,使用全球海表温度(SST),将ENSO季风关系的人为强迫分量与自然变化分量分离。结果表明,自然可变性在20世纪ENSO-季风关系的变化中起着主导作用。在21世纪,强迫分量主要由与SST变暖相关的季风降雨增加所主导,这可能会导致将来ENSO与季风的关系略微减弱。

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