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影响江南春雨年际变化的前期海洋信号及可能机理

胡雅君 刘屹岷 吴琼 王晓春

大气科学2017,Vol.41Issue(2):395-408,14.
大气科学2017,Vol.41Issue(2):395-408,14.DOI:10.3878/j.issn.1006-9895.1605.16133

影响江南春雨年际变化的前期海洋信号及可能机理

Preceding Oceanic Influences on the Inter-annual Variation of Spring Persistent Rain in Jiangnan of China and the Possible Mechanism

胡雅君 1刘屹岷 2吴琼 1王晓春3

作者信息

  • 1. 中国科学院大气物理研究所大气科学与地球流体力学数值模拟国家重点实验室,北京100029
  • 2. 中国科学院大学,北京100049
  • 3. 南京信息工程大学海洋科学学院,南京210044
  • 折叠

摘要

Abstract

Based on analysis of observations,we defined the starting and ending time and the total rainfall of the spring persistent rainfall in Jiangnan of China (SPRJ) from 1982 to 2014,and investigated the climatic characters of the SPRJ as well as its interannual variation.The relationship between the SST anomaly of Nino3.4 region in the preceding winter and the SPRJ and its physical mechanism were further studied,Results show that there is a significant positive correlation between the preceding winter Nino3.4 index and total SPRJ.The warm water can trigger an anomalous Walker circulation that leads to significant abnormal descending motions and corresponding low-level anticyclonic circulation near 120°E at the equator.The strengthened southwesterly winds of the anticyclone in the low level of the South China Sea facilitate more water vapor transport from the South China Sea to Jiangnan of China.On the other hand,the Indian Ocean SST anomaly associated with El Ni(n)o events can induce abnormal low level easterly winds in tropical Indian Ocean and anticyclone in the north of the Bay of Bengal,which also promotes the water vapor transportation.Meanwhile,the westerly anomalies in the upper troposphere above South Asia enhances divergence and pumping above Jiangnan of China,and thus are favorable for ascending motions and more SPRJ.In contrast,there is less SPRJ following a La Ni(n)a event.Moreover,the influence of El Ni(n)o on the SPRJ changes with its original intensity.With a strong El Ni(n)o in the preceding winter,the SSTA in the Pacific can persist to the following spring and there will be more SPRJ rainfall;with a weak El Ni(n)o in the preceding winter,however,the SSTA in the Pacific cannot persist to the following spring and the SPRJ total rainfall will decrease.Besides,when considering the combined effects of Nino3.4 index and Antarctic Oscillation Index and Indian Ocean Basin Mode of the preceding winter,the seasonal prediction is improved.Thus the multiple linear regression of the three predictors is useful for the prediction of the SPRJ.

关键词

江南春雨/年际变化/Nino3.4指数/E1 Ni(n)o强度/季节预测

Key words

Spring persistent rainfall in Jiangnan of China/Interannual variation/Nino3.4 index/El Ni(n)o intensity/Seasonal prediction

分类

天文与地球科学

引用本文复制引用

胡雅君,刘屹岷,吴琼,王晓春..影响江南春雨年际变化的前期海洋信号及可能机理[J].大气科学,2017,41(2):395-408,14.

基金项目

国家自然科学基金项目41328006,海洋专项XDA11010402,南京信息工程大学启动经费项目S8113046001,2015江苏双创团队,江苏高校优势学科建设工程资助项目(PAPD) National Natural Science Foundation of China (NSFC) (Grant 41328006),Marine Special Project (Grant XDA11010402),Start-up Project Foundation of NUIST (Grant S8113046001),Jiangsu Innovative and Entrepreneurial Team,Advanced Subjects Foundation of Jiangsu Colleges and Universities (PAPD) (PAPD)

大气科学

OA北大核心CSCDCSTPCD

1006-9895

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