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东亚季风近几十年来的主要变化特征

王会军 范可

大气科学2013,Vol.37Issue(2):313-318,6.
大气科学2013,Vol.37Issue(2):313-318,6.DOI:10.3878/j.issn.1006-9895.2012.12301

东亚季风近几十年来的主要变化特征

Recent Changes in the East Asian Monsoon

王会军 1范可2

作者信息

  • 1. 中国科学院大气物理研究所竺可桢—南森国际研究中心,北京100029
  • 2. 中国科学院气候变化研究中心,北京100029
  • 折叠

摘要

Abstract

Studies on the recent changes of the summer and winter monsoons, with priority on decadal-interdecadal scales, are reviewed briefly in this paper. The major changes in the East Asian summer monsoon (EASM) include a weakening of the EASM and a shift in precipitation patterns at the end of 1970s; an increase in South China precipitation after 1992-1993; a decrease in precipitation in the middle-and-lower reaches of the Yangtze River and an increase in precipitation in the Huaihe River valley after 1999; and instability in the relationship between the EASM and El Nino-Southern Oscillation (ENSO). The changes in the East Asian winter monsoon (EAWM) include a weakening of the EAWM and its interannual variability after the mid-1980s, an increase in winter snowfall in Northeast China after the mid-1980s, and a weakening of the EAWM-ENSO relationship after the mid-1970s. In addition, the impact of the autumn Arctic sea ice decline on the winter snow cover in the Northern Hemisphere is discussed. These changes in EASM and EAWM indicate that the extreme climate and phenology have been significantly altered.

关键词

东亚夏季风/东亚冬季风/年代际变化/ENSO/海冰

Key words

East Asian summer monsoon/ East Asian winter monsoon/ Interdecadal variability/ ENSO/ Sea ice

分类

天文与地球科学

引用本文复制引用

王会军,范可..东亚季风近几十年来的主要变化特征[J].大气科学,2013,37(2):313-318,6.

基金项目

国家自然科学基金项目41130103 ()

大气科学

OA北大核心CSCDCSTPCD

1006-9895

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