Interdecadal Change of the Relationship Between the Tropical Indian Ocean Dipole Mode and the Summer Climate Anomaly in China

• Published in: Acta meteorologica Sinica Vol. 25; no. 2; pp. 129 - 141
• Main Author: 赵珊珊 周天军 杨修群 朱益民 谭言科 孙旭光
• Format: Journal Article
• Language: English
• Published: Heidelberg The Chinese Meteorological Society 01.04.2011; Division of Climate Impact Assessment, National Climate Center, Beijing 100081%State Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029%School of Atmospheric Sciences, Nanjing University, Nanjing 210093%Institute of Meteorology, PLA University of Science and Technology, Nanjing 211101
• Subjects: Atmospheric Protection/Air Quality Control/Air Pollution; Atmospheric Sciences; Earth and Environmental Science; Earth Sciences; Geophysics and Environmental Physics; Marine; Meteorology; 东亚夏季风; 中国南方; 偶极子; 年代际变化; 月降水量; 气候异常; 温度记录; 热带印度洋; China, People's Rep., Changjiang R; China, People's Rep., Huang He R; ISW, Tropical Indian Ocean; interdecadal change; interannual variability; summer climate anomaly in China; tropical Indian Ocean dipole (IOD); interannual variability,interdecadal change
• ISSN: 0894-0525; 2191-4788
• DOI: 10.1007/s13351-011-0021-z

The interdecadal change of the relationship between the tropical Indian Ocean dipole（IOD） mode and the summer climate anomaly in China is investigated by using monthly precipitation and temperature records at 210 stations in China and the NCEP/NCAR reanalysis data for 1957-2005.The results indicate that along with the interdecadal shift in the large-scale general circulation around the late 1970s,the relationship between the IOD mode and the summer climate anomaly in some regions of China has significantly changed.Before the late 1970s,a developing IOD event is associated with an enhanced East Asian summer monsoon,which tends to decrease summer precipitation and increase summer temperature in South China;while after the late 1970s,it is associated with a weakened East Asian summer monsoon,which tends to increase（decrease） precipitation and decrease（increase） temperature in the south（north） of the Yangtze River.During the next summer,following a positive IOD event,precipitation is increased in most of China before the late 1970s,while it is decreased（increased） south（north） of the Yangtze River after the late 1970s.There is no significant correlation between the IOD and surface air temperature anomaly in most of China in the next summer before the late 1970s;however,the IOD tends to increase the next summer temperature south of the Yellow River after the late 1970s.