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Events of decadal thermocline variations in the South Pacific Ocean

中国海洋湖沼学报(英文版)2006,Vol.24Issue(2):111-117,7.
中国海洋湖沼学报(英文版)2006,Vol.24Issue(2):111-117,7.

Events of decadal thermocline variations in the South Pacific Ocean

Events of decadal thermocline variations in the South Pacific Ocean

1

作者信息

  • 1. Institute of Climate System, Chinese Academy of Meteorological Sciences, Beijing, 100081, China;Institute of Physical Oceanography, Ocean University of China, Qingdao 266003, China;Institute of Physical Oceanography, Ocean University of China, Qingdao 266003, China
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摘要

Abstract

The SODA data generated from a numerical model with data assimilation are used to study the decadal thermal anomalies in the therrnocline of the South Pacific. Three notable events of decadal thermocline variations are found. First, two major warm subduction events originated from outcrop regions centered at 30°S,150°W in the South Pacific Ocean occurred between 1960s and 1980s propagating toward the western Tropics and at 30°S, 90°W in the late 1970s propagating directly toward the eastern Tropics. Second, a special westward warm event originating from the eastern boundary around 15°S occurred in the early 1980s. Thirdly, a distinct zonal location transition of the positive temperature anomalies near 10°S took place in the late 1970s. The results suggest that the warm events in the subtropical South Pacific region are important to the decadal variability of the western tropical Pacific before the late 1970s and to the eastern tropical Pacific after the late 1970s.

关键词

decadal variability/the South Pacific Ocean

Key words

decadal variability/the South Pacific Ocean

分类

海洋科学

引用本文复制引用

..Events of decadal thermocline variations in the South Pacific Ocean[J].中国海洋湖沼学报(英文版),2006,24(2):111-117,7.

基金项目

Supported by The National Natural Science Foundation of China (Nos.40406004, 40490263 and 40306002) and by the University Doctorate Foundation (No.20030423004). (Nos.40406004, 40490263 and 40306002)

中国海洋湖沼学报(英文版)

OACSCDCSTPCD

2096-5508

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