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台湾地形对海棠台风影响的数值模拟研究

程婧 倪允琪

气象科学2009,Vol.29Issue(5):575-583,9.
气象科学2009,Vol.29Issue(5):575-583,9.

台湾地形对海棠台风影响的数值模拟研究

Numerical simulation of typhoon Haitang(2005) and the topographic effect of Taiwan island

程婧 1倪允琪2

作者信息

  • 1. 南京大学,大气科学学院,南京,210093
  • 2. 中国气象局,气象科学研究院,北京,100081
  • 折叠

摘要

Abstract

The Weather Research and Forecasting (WRF) model is used to study the evolution of typhoon Haitang and the topographic effect of Tainwan island. Although the variable track could not be reflected exactly, the model can capture Haitang's evolution of intensity and structure, especially its weakening during landfall, as well as precipitation distribution in Taiwan. Analysis of mesoscale system shows that the sub-vertical circulation which is inspired by the interaction of typhoon Haitang circulation with CMR terrain generates strong upward motion in precipitation area. And horizontal wind transports warm and moist air to this area and provides plenty of vapor for supporting convection development. The special correlation between typhoon Haitang circulation and CMR terrain plays an important part in typhoon Haitang precipitation.

关键词

台风降水/结构强度变化/地形强迫作用/数值模拟

Key words

Typhoon rainfall/Evolution of typhoon's structure and intensity/Terrain force/Numerical simulation

分类

天文与地球科学

引用本文复制引用

程婧,倪允琪..台湾地形对海棠台风影响的数值模拟研究[J].气象科学,2009,29(5):575-583,9.

基金项目

国家重点基础研究发展规划973项目"我国南方致洪暴雨监测与预测的理论和方法研究"(2004 CB418300) (2004 CB418300)

气象科学

OA北大核心CSCDCSTPCD

1009-0827

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