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《Chinese Journal of Atmospheric Sciences》 2001-04
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The Dipole in the Equatorial Indian Ocean and Its Impacts on Climate

Li Chongyin and Mu Mingquan (Stale Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029)  
The analyses in observational data of near 100 years showed that the variation of SST in the equatorial Indian Ocean has a feature of the diople oscillation: It mainly shows a positive phase pattern (higher SST in the west and lower SST in the east) and a negative phase pattern (higher SST in the east and lower SST in the west), the amplitude of the positive phase is larger than that of the negative phase. The dipole is stronger in September- November and weaker in January- April. It also has interannual variation (4- 5 year period) and interdecadal variation (25-30 year period). Although the Indian Ocean dipole in the individual year seems to be independent of the ENSO in the equatorial Pacific, in general, the Indian Ocean dipole has obviously negative correlation with the Pacific Ocean dipole (similar to ENSO). The atmospheric zonal (Walker) circulation is fundamental to relate the two dipoles. The data analyses still showed that the lower tropospheric wind fields over the southern Asia, the Tibetan high in the upper troposphere and the subtropical high over the northwestern Pacific are all related to the Indian Ocean dipole, which shows the important impact of the Indian Ocean dipole on the Asian monsoon activities.
【Fund】: 国家重点基础研究发展规划项目G1998040903;; 国家自然科学基金资助项目49823002共同资助
【CateGory Index】: P731
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5 DAO SHIH-YEN, HSU SHU-YING, KUO CHI-YUNN (Institute of Geophysics and Meteorology, Academia Sinica);THE CHARACTERISTICS OF THE ZONAL AND MERIDIONAL CIRCULATION OVER TROPICAL AND SUBTROPICAL REGIONS IN EASTERN ASIA IN SUMMER[J];Acta Meteorologica Sinica;1962-02
6 S. S. HWANG, T. H. YUE(Department of Meteorology, Nanking University);ON THE STRUCTURE OF THE SUB-TROPICAL HIGHS AND SOME ASSOCIATED ASPECTS OF THE GENERAL CIRCULATION OF ATMOSPHERE[J];Acta Meteorologica Sinica;1962-S1
7 HOU YI-RU CHEN CHIAN (Meteorological Observatory of Lanchow);THE LONG WAVE OF SUBTROPICAL JET OVER ASIA IN SUMMER[J];Acta Meteorologica Sinica;1963-03
8 ZOU HAO, QIAN ZI-QIANG, ZHU CUI-YING, QIANG PAN-QING(Meteorological Observatory of Shanghai);AN ANALYSIS ON THE 500 MB CIRCULATION DURING MAI-Y PERIOD IN THE LOWER AND MIDDLE YANTZE[J];Acta Meteorologica Sinica;1964-02
9 DAO SHIH-YEN (Institute of Geophysics and Meteorology)CHU FU-KANG (Research Institute of Meteorology, Central Meteorology Senice);THE 100-MB FLOW PATTERNS IN SOUTHERN ASIA IN SUMMER AND ITS RELATION TO THE ADVANCE AND RETREAT OF THE WEST-PACIFIC SUBTROPICAL ANTICYCLONE OVERTHE FAR EAST[J];Acta Meteorologica Sinica;1964-04
10 Yi LanTao Shiyan(National Climate Center, Beijing 100081)(Institute of Atmospheric Physics, CAS, Beijing, 100080);Construction and Analysis of a Precipitation Recycling Model[J];ADVANCES IN WATER SCIENCE;1997-03
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