| The tropical Pacific-Indian Ocean temperature anomaly mode and its effect |
| |
| 作者姓名： | YANG Hui JIA Xiaolong LI Chongyin |
| |
| 作者单位： | [1]State Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China [2]Graduate University of Chinese Academy of Sciences, Beijing 100049, China [3]Meteorological College, PLA University of Science and Technology, Nanjing 211101, China |
| |
| 基金项目： | Acknowledgements This work was supported by the National Natural Science Foundation of China （Grant No. 40233033）, the National Key Basic Research and Development Project of China （Grant No. 2004CB18300）, and the Innovation Key Program of the Chinese Academy of Sciences （Grant No. ZKCX2-SW-226）. |
| |
| 摘 要： | Temperature anomaly in the Indian Ocean is closely related to that in the Pacific Ocean because of the Walker circulation and the Indonesian throughflow. So only the El Ni?o/Southern Oscillation (ENSO) in the Pacific cannot entirely explain the influence of sea surface temperature anomaly (SSTA) on climate variation. The tropical Pacific-Indian Ocean temperature anomaly mode (PIM) is presented based on the comprehensive research on the pattern and feature of SSTA in both Indian Ocean and Pacific Ocean. The features of PIM and ENSO mode and their influences on the climate in China and the rainfall in India are further compared. For proving the observation results, numerical experiments of the global atmospheric general circulation model are conducted. The results of observation and sensitivity experiments show that presenting PIM and studying its influence are very important for short-range climate prediction.
|
| 关 键 词： | 热带太平洋-印度洋温度异常 气候影响 合成模式 PIM |
| 收稿时间： | 2006-02-14 |
| 修稿时间： | 2006-02-142006-03-30 |
The tropical Pacific-Indian Ocean temperature anomaly mode and its effect |
| |
| YANG Hui JIA Xiaolong LI Chongyin.The tropical Pacific-Indian Ocean temperature anomaly mode and its effect[J].Chinese Science Bulletin,2006,51(23):2878-2884. |
| |
| Authors: | Hui Yang Xiaolong Jia Chongyin Li |
| |
| Institution: | (1) State Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing, 100029, China;(2) Graduate University of Chinese Academy of Sciences, Beijing, 100049, China;(3) Meteorological College, PLA University of Science and Technology, Nanjing, 211101, China |
| |
| Abstract: | Temperature anomaly in the Indian Ocean is closely related to that in the Pacific Ocean because of the Walker circulation and the Indonesian throughflow. So only the El Niño/Southern Oscillation (ENSO) in the Pacific cannot entirely explain the influence of sea surface temperature anomaly (SSTA) on climate variation. The tropical Pacific-Indian Ocean temperature anomaly mode (PIM) is presented based on the comprehensive research on the pattern and feature of SSTA in both Indian Ocean and Pacific Ocean. The features of PIM and ENSO mode and their influences on the climate in China and the rainfall in India are further compared. For proving the observation results, numerical experiments of the global atmospheric general circulation model are conducted. The results of observation and sensitivity experiments show that presenting PIM and studying its influence are very important for short-range climate prediction. |
| |
| Keywords: | tropical Pacific-Indian Ocean temperature anomaly composite mode influence on climate |
| 本文献已被 CNKI 维普 万方数据 SpringerLink 等数据库收录！ |
| 点击此处可从《中国科学通报(英文版)》浏览原始摘要信息 |
| 点击此处可从《中国科学通报(英文版)》下载免费的PDF全文 |
