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Roles of Tropical Indian-Pacific Oceans SSTs in the Interdecadal Variability of East Asian Summer Monsoon: A Modeling Study

机译:热带印度太平洋太平洋海表温度在东亚夏季风年代际年代际变化中的作用:一个模型研究

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This study investigates the roles of tropical Indian-Pacific oceans SSTs in the interdecadal variability of East Asian Summer Monsoon (EASM) during the second half of the twentieth century based on simulations from an atmospheric general circulation model, NCAR CAM3 (Community Atmospheric Model). These simulations are conducted by the observed 1950-2000 monthly SSTs in the tropical Indian-Pacific oceans, tropical Indian Ocean and tropical Pacific, independently. Results show that CAM3 is able to simulate the observed interdecadal weakening of EASM occurred in the mid-late 1970s when SSTs in tropical Indian-Pacific Oceans and tropical Pacific SSTs are determined, but to simulate the interdecadal strengthening of EASM when SSTs in the tropical Indian Ocean are determined. These results indicate that SST anomaly in the tropical Pacific plays a central role in the interdecadal weakening of EASM occurred in the mid-late of 1970s, while SST anomaly in the tropical Indian Ocean plays a converse role in it. As a background, the interdecadal variation of tropical Pacific SSTs has an important effect upon the interdecadal weakening of EASM.
机译:这项研究基于20世纪下半叶东亚夏季风(EASM)年代际变率中热带印度洋-太平洋SST的作用,该研究基于大气总循环模型NCAR CAM3(社区大气模型)的模拟。这些模拟是通过分别在热带印度洋-太平洋,热带印度洋和热带太平洋观测到的1950-2000每月SST进行的。结果表明,CAM3能够模拟观测到的1970年代中期EASM年代际减弱,当确定热带印度太平洋和热带太平洋SSTs时,EASM年代际减弱,但是模拟EASM年代际增强的情况。海洋确定了。这些结果表明,热带太平洋海表温度异常在1970年代中后期发生的EASM年代际减弱中起着重要作用,而热带印度洋海表温度异常在其中起相反的作用。作为背景,热带太平洋海表温度的年代际变化对东亚夏季风的年代际减弱具有重要影响。

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