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Climatology and Interannual Variation of the East Asian Winter Monsoon: Results from the 1979--95 NCEP/NCAR Reanalysis.

Authors :
Yi Zhang
Sperber, Kenneth R.
Boyle, James S.
Source :
Monthly Weather Review; Oct97, Vol. 125 Issue 10, p2605, 15p
Publication Year :
1997

Abstract

This paper presents the climatology and interannual variation of the East Asian winter monsoon based on the 1979--95 National Centers for Environmental Prediction/National Center for Atmospheric Research reanalysis. In addition to documenting the frequency, intensity, and preferred propagation tracks of cold surges and the evolution patterns of related fields, the authors discuss the temporal distribution of the Siberian high and cold surges. Further, the interannual variation of the cold surges and winter monsoon circulation and its relationship with ENSO were examined. There are on average 13 cold surges in each winter season (October--April), of which two are strong cases. The average intensity of cold surges, measured by maximum sea level pressure, is 1053 hPa. The cold surges originate from two source regions: 1) northwest of Lake Baikal, and 2) north of Lake Balkhash. The typical evolution of a cold surge occurs over a period of 5--14 days. Trajectory and correlation analyses indicate that, during this time, high pressure centers propagate southeastward around the edge of the Tibetan Plateau from the mentioned source regions. Some of these high pressure centers then move eastward and diminish over the oceans, while others proceed southward. The signatures of the associated temperature, wind, and pressure fields propagate farther southward and eastward. The affected area encompasses the bulk of the maritime continent. Although the intensity of the Siberian high peaks during December and January, the frequency of cold surges reaches a maximum in November and in March. This result suggests that November through March should be considered as the East Asian winter monsoon season. Two stratifications of cold surges are used to examine the relationship between ENSO and the interannual variation of the winter monsoon. The first one, described as conventional cold surges, indicates that the surge frequency reaches a minimum a year... [ABSTRACT FROM AUTHOR]

Subjects

Subjects :
CLIMATOLOGY
WINTER
MONSOONS

Details

Language :
English
ISSN :
00270644
Volume :
125
Issue :
10
Database :
Complementary Index
Journal :
Monthly Weather Review
Publication Type :
Academic Journal
Accession number :
5656073
Full Text :
https://doi.org/10.1175/1520-0493(1997)125<2605:CAIVOT>2.0.CO;2