期刊
INTERNATIONAL JOURNAL OF CLIMATOLOGY
卷 28, 期 14, 页码 1849-1859出版社
WILEY-BLACKWELL
DOI: 10.1002/joc.1678
关键词
Indian Ocean dipole; South China sea summer monsoon; Asian summer monsoon; positive phase; negative phase
资金
- China national 973 Program [2006CB403600]
- National Key Basic Research and Development Project of China [2004CB18300]
By exploring the spatiotemporal features of the Indian Ocean Dipole (IOD) both oil the sea Surface and in the subsurface ocean, the present article reveals that the subsurface dipole mode, with larger amplitude than the Surface one, is likely to prolong the dipole signal for a long time. Using the wind and geopotential height data from NCEP/NCAR, this article further investigates TOD impacts on the Asian summer monsoon activities in the following year. A normal (late) South China Sea summer monsoon onset is associated with the previous positive (negative) TOD. In the summer after an TOD year, a positive (negative) TOD tends to induce a stronger (weaker) 100-hPa South Asian High, with a more (less) eastward-extending high ridge, and also an enhanced (a weakened) 500-hPa western Pacific subtropical high, with a westward-advancing (an eastward-retreating) high ridge. Influenced by the anomalous 850-hPa Asian monsoon circulations and the longitudinal position of the 500-hPa subtropical high ridge, Summer rainfall in China also exhibits different patterns corresponding to different phases of the TOD in the previous year. Copyright (C) 2008 Royal Meteorological Society
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