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  1. 防災科研関係論文

Decadal Shift in Summer Precipitation Variability over East Asia in the Mid-2000s and Wave Propagation toward North America

https://nied-repo.bosai.go.jp/records/6061
https://nied-repo.bosai.go.jp/records/6061
b71d626a-44fc-4c6e-9b84-0028eaefc344
Item type researchmap(1)
公開日 2023-04-27
タイトル
言語 en
タイトル Decadal Shift in Summer Precipitation Variability over East Asia in the Mid-2000s and Wave Propagation toward North America
言語
言語 eng
著者 Shinji Matsumura

× Shinji Matsumura

en Shinji Matsumura

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Takeshi Horinouchi

× Takeshi Horinouchi

en Takeshi Horinouchi

Search repository
抄録
内容記述タイプ Other
内容記述 Abstract

The East Asian summer climate displays a marked change after the late 1990s. This is principally due to a weakening of the Pacific–Japan (PJ) teleconnection pattern that was a dominant driver of precipitation variability over East Asia. Nevertheless, western Japan has frequently experienced heavy rainfall events over the past several years. Atmospheric reanalysis and observational datasets are used to investigate summer precipitation variability over East Asia in a view of interdecadal changes from 1979 to 2020. East Asian summer precipitation has increased the most in Japan, especially over and around the Southwest Islands in southern Japan, where cumulus convection has been more dominant for the characteristic of precipitation variability including mei-yu–baiu rainfall than frontal structure since the mid-2000s. Atmospheric analysis in vertical structures and convective instability indicates that moist instability is neutralized by cumulus convection over the southern East China Sea and off the Pacific coast of Japan, where recent warming in sea surface temperature (SST) along the Kuroshio exceeds the SST threshold for convection. This decadal shift in precipitation variability has a close relationship with the second precipitation mode over East Asia, which has taken the place of the PJ pattern as a leading driver of precipitation variability over western Japan in the past decade. The enhanced cumulus convection is enabled to act as a forcing mechanism for the Rossby wave train from East Asia toward North America along the westerly jet or for the eastward extension of the Silk Road pattern, which possibly favors a heatwave in the Pacific Northwest areas of North America.
言語 en
書誌情報 en : Journal of Climate

巻 36, 号 8, p. 2483-2496, 発行日 2023-03-14
出版者
言語 en
出版者 American Meteorological Society
ISSN
収録物識別子タイプ EISSN
収録物識別子 1520-0442
DOI
関連識別子 10.1175/jcli-d-22-0292.1
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