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The coupling instability of Rossby and topographic Rossby waves in the equatorial area
作者姓名:CHAO Jiping    LIU Lin  & YU Weidong . Laboratory of Marine Science and Numerical Modeling  State Oceanic Administration  Qingdao  China  . National Research Center for Marine Environmental Forecasts  State Oceanic Administration  Beijing  China  . Ocean University of China  Qingdao  China
作者单位:CHAO Jiping1,2,LIU Lin1,3 & YU Weidong1 1. Laboratory of Marine Science and Numerical Modeling,State Oceanic Administration,Qingdao 266061,China; 2. National Research Center for Marine Environmental Forecasts,State Oceanic Administration,Beijing 100081,China; 3. Ocean University of China,Qingdao 266003,China
基金项目:国家自然科学基金,科技部资助项目
摘    要:Before the 1980s, El Ni?o was believed as the sea surface warming along the coast of Peru in South America. As the positive anomaly strengths, the warm water expands westward along the equator to form large area of anomalous high sea surface temperature. Rasmusson and Carpenter (1982) summarized the de-velopment process of the sea surface warm water and the corresponding wind field1] during ENSO cylce. However, this canonical El Ni?o was questioned by 1982-1983 warm episode and later dat…


The coupling instability of Rossby and topographic Rossby waves in the equatorial area
CHAO Jiping,,LIU Lin, & YU Weidong . Laboratory of Marine Science and Numerical Modeling,State Oceanic Administration,Qingdao ,China, . National Research Center for Marine Environmental Forecasts,State Oceanic Administration,Beijing ,China, . Ocean University of China,Qingdao ,China.The coupling instability of Rossby and topographic Rossby waves in the equatorial area[J].Science in China(Earth Sciences),2005,48(10).
Authors:CHAO Jiping  LIU Lin  YU Weidong
Institution:1. Laboratory of Marine Science and Numerical Modeling, State Oceanic Administration, Qingdao 266061, China;National Research Center for Marine Environmental Forecasts, State Oceanic Administration, Beijing 100081, China
2. Laboratory of Marine Science and Numerical Modeling, State Oceanic Administration, Qingdao 266061, China;Ocean University of China, Qingdao 266003, China
3. Laboratory of Marine Science and Numerical Modeling, State Oceanic Administration, Qingdao 266061, China
Abstract:In case of considering the fact that the tropical ocean thermocline or the lower at-mosphere height field has the meridional variation, the topographic Rossby wave will be excited. Also the background geostrophic current emerges. Under such conditions, the topographic Rossby wave can interact with the classical Rossby wave at some parameter band and thus brings a new kind of instability, which may be of potential application in understanding some phenomena of the ENSO cycle.
Keywords:thermocline variation  equatorial jet  Rossby wave  topographic Rossby wave  coupling instability
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