Intraseasonal Oscillation in the Tropical Indian Ocean

被引:0
作者
李崇银
胡瑞金
杨辉
机构
[1] State Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics (LASG)
[2] Institute of Atmospheric Physics
[3] Chinese Academy of Sciences
[4] Physical Oceanography Laboratory & Ocean-Atmosphere Interaction and Climate Laboratory
[5] Ocean University of China
[6] Chinese Academy of Sciences Beijing
[7] Institute of Meteorology
[8] PLA University of Science and Technology
[9] Nanjing
[10] Qingdao
[11] Beijing
关键词
intraseasonal oscillation; tyopical Indian ocean; atmospheric ISO; oceanic ISO;
D O I
暂无
中图分类号
P732.3 [海洋热带气象];
学科分类号
0706 ; 070601 ;
摘要
The features of the intraseasonal oscillation (ISO) of the tropical Indian Ocean are studied using several sources of observational data. It is shown that there are intraseasonal oscillations in the tropical Indian Ocean, but their periods vary with latitude: the major period is about 20-30 days in the equatorial region, about 30-50 days at 10°N/10°S latitude and 60-90 days at 20°N/20°S latitude. The intensity of the ISO increases with latitude but the speed of the westward propagation of the ISO decreases with latitude. The intensity and propagation speed of the ISO have clear interannual variation features. The atmospheric intraseasonal oscillation over the tropical Indian Ocean is also analyzed and compared with the oceanic intraseasonal oscillation. It is shown that the major period is in the range 30-60 days and the intensity and period of the atmospheric ISO decrease with latitude slightly. The zonal propagation of the atmospheric ISO also has some differences with the oceanic ISO. It is necessary to study the relationship between the atmospheric ISO and oceanic ISO in the tropical Indian Ocean deeply.
引用
收藏
页码:617 / 624
页数:8
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