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Characteristics of Soliton with Dynamic Constraints on its Existence/Propagation in Tropical Easterly Wave
引用本文:Zhang Ren. Characteristics of Soliton with Dynamic Constraints on its Existence/Propagation in Tropical Easterly Wave[J]. 大气科学进展, 1996, 13(3): 325-339. DOI: 10.1007/BF02656850
作者姓名:Zhang Ren
作者单位:Air Force
摘    要:The study concerns the propagation of easterly wave (EW) at tropics as west-moving soliton more steady both in ionn and velocity as evidenced in the dynamic framework.Under the impact of different circulation patterns over the regions of western Pacific trade wind,South-Asia monsoon and their transition,such a soliton becomes tapering off during its westward movement and degrading to a common dispersive wave on the whole,followed by dismtegra-non when striking the South-China Sea monsoon segment,thereby indicating that the sea sector is inaccessible to the soliton When no monsoon trough is present over the South Asian monsoon area around 30癗 or the monsoon depression ]S shallow,it is likely to have west-travelling soliton,which suggests the incursion of the EW into the South-Asian monsoon region.

收稿时间:1995-03-11

Characteristics of soliton with dynamic constraints on its existence / propagation in tropical easterly wave
Zhang Ren. Characteristics of soliton with dynamic constraints on its existence / propagation in tropical easterly wave[J]. Advances in Atmospheric Sciences, 1996, 13(3): 325-339. DOI: 10.1007/BF02656850
Authors:Zhang Ren
Affiliation:Air Force Institute of Meteorology, Nanjing 211101
Abstract:The study concerns the propagation of easterly wave (EW) at tropics as west-moving soliton more steady both in form and velocity as evidenced in the dynamic framework. Under the impact of different circulation patterns over the regions of western Pacific trade wind, South-Asia monsoon and their transition, such a soliton becomes tapering off during its westward movement and degrading to a common dispersive wave on the whole, followed by disintegra-tion when striking the South-China Sea monsoon segment, thereby indicating that the sea sector is inaccessible to the soliton. When no monsoon trough is present over the South Asian monsoon area around 30oN or the monsoon de-pression is shallow, it is likely to have west-travelling soliton, which suggests the incursion of the EW into the South-Asian monsoon region.
Keywords:Easterly wave (EW)   Soliton
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