摘要
The rainfall over the Yangtze River val- ley during flood seasons (June to July) shows both interannual and decadal variations. The rainfall has been increasing since 1990, showing a decadal sig- nal. The variations of rainfall are influenced by the multi-scale interactions in the atmosphere-ocean coupled climate system. The rainfall, SST, and cir- culation are analyzed with the Chinese 160 station data, and other observational/reanalysis data, re- spectively. The separation between the interannual and decadal variations is carried out. The key areas affecting the Yangtze rainfall are the western Pacific warm pool on the interannual time scale and the EINO3 area on the decadal time scale, respectively. The circulation anomaly associated with the interan- nual variation occurs in the upper troposphere whereas that associated with the decadal variation appears in the lower troposphere.
The rainfall over the Yangtze River valley during flood seasons （June to July） shows both interannual and decadal variations. The rainfall has been increasing since 1990, showing a decadal signal. The variations of rainfall are influenced by the multi-scale interactions in the atmosphere-ocean coupled climate system. The rainfall, SST, and circulation are analyzed with the Chinese 160 station data, and other observational/reanalysis data, respectively. The separation between the interannual and decadal variations is carried out. The key areas affecting the Yangtze rainfall are the western Pacific warm pool on the interannual time scale and the EINO3 area on the decadal time scale, respectively. The circulation anomaly associated with the interannual variation occurs in the upper troposphere whereas that associated with the decadal variation appears in the lower troposphere.
基金
supported by the National Natural Science Foundation of China(Grant Nos.40333028 and 40305010)
the National Key Basic Research Project(Grant No.2004CB418302).
关键词
长江流域
降雨量
动力学因素
比较分析
rainfall in Yangtze River valley, annual and decadal variations, factors.
