Why the Western Pacific Subtropical High Has Extended Westward since the Late 1970s

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Why the Western Pacific Subtropical High Has Extended Westward since the Late 1970s

The western Pacific subtropical high (WPSH) is closely related to Asian climate. Previous examination of changes in the WPSH found a westward extension since the late 1970s, which has contributed to the interdecadal transition of East Asian climate. The reason for the westward extension is unknown, however. The present study suggests that this significant change of WPSH is partly due to the atm...

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ژورنال

عنوان ژورنال: Journal of Climate

سال: 2009

ISSN: 1520-0442,0894-8755

DOI: 10.1175/2008jcli2527.1