Decadal warming of coastal China Seas and coupling with winter monsoon and currents

L. Y. Oey, M. C. Chang, Yu-Lin Chang, Y. C. Lin, F. H. Xu

研究成果: 雜誌貢獻文章

33 引文 (Scopus)

摘要

In recent decades, wintertime sea surface temperatures off the eastern coast of China have steadily increased. The warming is accompanied by on-coast wind convergence across East China Sea and by stronger northeasterly wind which is spatially inhomogeneous being greatest in the Taiwan Strait. Strong winds favor more frequent cross-shelf currents and vigorous spreading of heat from the Kuroshio, which warms the coastal sea in a positive feedback loop. The process also weakens the East Asian winter monsoon over eastern China, contributing to its decoupling from the recent rebound of the Siberian High. Key Points Recent warming off coastal China is accompanied by stronger northeasterly wind Stronger winter monsoon spreads heat from Kuroshio producing air-sea response The increased wind is detached from the recent rebound of the Siberian High

原文英語
頁(從 - 到)6288-6292
頁數5
期刊Geophysical Research Letters
40
發行號23
DOIs
出版狀態已發佈 - 2013 十二月 16

指紋

monsoons
winter
China
monsoon
warming
heating
coasts
heat
positive feedback
straits
coast
sea surface temperature
Taiwan
shelves
decoupling
strait
sea
air

ASJC Scopus subject areas

  • Geophysics
  • Earth and Planetary Sciences(all)

引用此文

Decadal warming of coastal China Seas and coupling with winter monsoon and currents. / Oey, L. Y.; Chang, M. C.; Chang, Yu-Lin; Lin, Y. C.; Xu, F. H.

於: Geophysical Research Letters, 卷 40, 編號 23, 16.12.2013, p. 6288-6292.

研究成果: 雜誌貢獻文章

Oey, L. Y. ; Chang, M. C. ; Chang, Yu-Lin ; Lin, Y. C. ; Xu, F. H. / Decadal warming of coastal China Seas and coupling with winter monsoon and currents. 於: Geophysical Research Letters. 2013 ; 卷 40, 編號 23. 頁 6288-6292.
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abstract = "In recent decades, wintertime sea surface temperatures off the eastern coast of China have steadily increased. The warming is accompanied by on-coast wind convergence across East China Sea and by stronger northeasterly wind which is spatially inhomogeneous being greatest in the Taiwan Strait. Strong winds favor more frequent cross-shelf currents and vigorous spreading of heat from the Kuroshio, which warms the coastal sea in a positive feedback loop. The process also weakens the East Asian winter monsoon over eastern China, contributing to its decoupling from the recent rebound of the Siberian High. Key Points Recent warming off coastal China is accompanied by stronger northeasterly wind Stronger winter monsoon spreads heat from Kuroshio producing air-sea response The increased wind is detached from the recent rebound of the Siberian High",
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AU - Chang, M. C.

AU - Chang, Yu-Lin

AU - Lin, Y. C.

AU - Xu, F. H.

PY - 2013/12/16

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AB - In recent decades, wintertime sea surface temperatures off the eastern coast of China have steadily increased. The warming is accompanied by on-coast wind convergence across East China Sea and by stronger northeasterly wind which is spatially inhomogeneous being greatest in the Taiwan Strait. Strong winds favor more frequent cross-shelf currents and vigorous spreading of heat from the Kuroshio, which warms the coastal sea in a positive feedback loop. The process also weakens the East Asian winter monsoon over eastern China, contributing to its decoupling from the recent rebound of the Siberian High. Key Points Recent warming off coastal China is accompanied by stronger northeasterly wind Stronger winter monsoon spreads heat from Kuroshio producing air-sea response The increased wind is detached from the recent rebound of the Siberian High

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KW - Taiwan Strait currents

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KW - coastal warming

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