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• W1998880455 endingPage "074006" @default.
• W1998880455 startingPage "074006" @default.
• W1998880455 abstract "This study demonstrates a robust relationship between the Indo-Pacific warm pool (IPWP) and North Pacific Ocean dipole (IPOD) and the East Asian summer monsoon (EASM) using observational datasets and sensitivity tests from the Community Atmosphere Model version 3.1 of the National Center for Atmospheric Research. The IPOD, which is a significant pattern of boreal summer SSTA in the Indian and Pacific oceans characterized by positive (negative) sea-surface temperature anomalies (SSTA) in the North Pacific and negative (positive) SSTA in the IPWP, appears around May, intensifies in the following months, and weakens in September. In summers with a positive IPOD phase, the western Pacific subtropical high (WPSH) weakens and shrinks with the axis of the WPSH ridge moving northwards, which favours an intensified EASM and a decrease in summer rainfall in the Yangtze River valley, and vice versa." @default.
• W1998880455 created "2016-06-24" @default.
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• W1998880455 date "2014-07-01" @default.
• W1998880455 modified "2023-10-18" @default.
• W1998880455 title "A dipole pattern in the Indian and Pacific oceans and its relationship with the East Asian summer monsoon" @default.
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• W1998880455 doi "https://doi.org/10.1088/1748-9326/9/7/074006" @default.
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