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出 处:《Advances in Atmospheric Sciences》2002年第6期1069-1078,共10页大气科学进展(英文版)
基 金:This paper is supported by " 973" heavy rainfall program and the National Natural Science Foundation of China under Grant Nos. 49775263 and 40175019.
摘 要:With a quasi-geostrophic barotropic model on the β-plane with a topography term, 16 experiments were performed with an integration period of 6 days. The interaction between tropical cyclone tracks and 500 km-scale vortices originating from the western part of a large-scale topography is investigated. It is suggested that this kind of interaction may have a significant impact on the moving speed and direction of tropical cyclones. Under certain conditions, this interaction may be a factor in causing an abnormal tropical cyclone track. Furthermore, the effect of large-scale topography plays an important role in the formation of unusual tropical cyclone tracks.With a quasi-geostrophic barotropic model on the β-plane with a topography term, 16 experiments were performed with an integration period of 6 days. The interaction between tropical cyclone tracks and 500 km-scale vortices originating from the western part of a large-scale topography is investigated. It is suggested that this kind of interaction may have a significant impact on the moving speed and direction of tropical cyclones. Under certain conditions, this interaction may be a factor in causing an abnormal tropical cyclone track. Furthermore, the effect of large-scale topography plays an important role in the formation of unusual tropical cyclone tracks.
关 键 词:Tibetan Plateau DIPOLE interaction tropical cyclone abnormal track topographic effect
分 类 号:P444[天文地球—大气科学及气象学]
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