| 注册
首页|期刊导航|热带气象学报|热带印度洋海表面温度偶极子模态的气候演变特征

热带印度洋海表面温度偶极子模态的气候演变特征

杨梦兮 胡瑞金 刘梅

热带气象学报2017,Vol.33Issue(2):177-186,10.
热带气象学报2017,Vol.33Issue(2):177-186,10.DOI:10.16032/j.issn.1004-4965.2017.02.004

热带印度洋海表面温度偶极子模态的气候演变特征

CLIMATIC EVOLUTION CHARACTERISTICS OF THE DIPOLE MODE OF SEA SURFACE TEMPERATURE IN THE TROPICAL INDIAN OCEAN

杨梦兮 1胡瑞金 2刘梅3

作者信息

  • 1. 泰州市气象局,江苏泰州225300
  • 2. 中国海洋大学物理海洋实验室和山东省高校海洋-大气相互作用与气候重点实验室,山东青岛266100
  • 3. 江苏省气象台,江苏南京210008
  • 折叠

摘要

Abstract

Based on a total of 49a SODA data from January 1960 to December 2008,the climatic evolution characteristics of the tropical Indian Ocean dipole mode (IODM) of sea surface temperature are studied.The main results are as follows:(1) The IODM spatial patterns derived from the moving EOF (empirical orthogonal function) with 1a interval and 10a length do not always show the well-known distribution of the east-west dipole,but has an evolution from a south-north dipole to an east-west one;(2) In the case of the south-north dipole,the SST north (south) of 10 °S shows overall warming (cooling).For the east-west dipole,meanwhile,the SST in the tropical eastern (western) IO shows alternate variations of warming (cooling) and cooling (warming) on quasi-decadal timescales;(3) There are also four quasi-decadal variations in IODM,occurring in 1976,1987,1994 and 2005 respectively;(4) There is a reverse trend between the variance rate of the second mode (the IODM) and that of the first mode,in moving EOF.

关键词

热带印度洋/SSTA/滑动EOF/IODM/时空演变

Key words

tropical Indian Ocean/SSTA/moving EOF/IODM/spatial-temporal evolution

分类

天文与地球科学

引用本文复制引用

杨梦兮,胡瑞金,刘梅..热带印度洋海表面温度偶极子模态的气候演变特征[J].热带气象学报,2017,33(2):177-186,10.

基金项目

国家自然科学基金(41405092)资助 (41405092)

热带气象学报

OA北大核心CSCDCSTPCD

1004-4965

访问量0
|
下载量0
段落导航相关论文