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“0814”号强台风发展维持的环境场分析

赵大军 于玉斌 李莹

气象科学2011,Vol.31Issue(5):591-597,7.
气象科学2011,Vol.31Issue(5):591-597,7.

“0814”号强台风发展维持的环境场分析

A diagnostic analysis of the intensity change of strong typhoon Hagupit

赵大军 1于玉斌 2李莹3

作者信息

  • 1. 解放军93762部队,北京102105
  • 2. 中国气象局,北京100081
  • 3. 中国气象局国家气候中心,北京100081
  • 折叠

摘要

Abstract

Based on NCAR/NCEP reanalysis data, the intensity change of 0814 strong typhoon Hagupit is diagnosed. The results showed that the high SST of the Western Pacific is conducive to the generation of Haqupit, the offshore high SST of Zhejang, Fujian and Hainan contributes to the development and maintenance of Hagupit. At the TC genesis stage, the subtropical high stretches northward and westward, strengthens and maintains its intensity steadily. When the typhoon moves towards the subtropical high, the pressure gradient between them increases, the south easterly wind enables Hagupit to move northwest quickly and strengthen. When the TC entered the South China Sea, the subtropical high maintains and further strengthens westward, but the westerly trough moves eastward so that the typhoon moves northwestward and develops into a strong typhoon. The intensity change of Hagupit is affected by following factors. In the upper troposphere, the strong northeast wind on the eastern side of South Asia high transports high potential vorticity to the typhoon area, and makes Hagupit develop. In the lower troposphere , strong southwest monsoon provides adequate water sources and transports cyclonic relative vorticity to the typhoon zone, and then enables Haqupit to rapidly develop and maintain its strength.

关键词

强台风/南亚高压/西南季风

Key words

Strong typhoon/South Asian high/Southwest monsoon

分类

天文与地球科学

引用本文复制引用

赵大军,于玉斌,李莹..“0814”号强台风发展维持的环境场分析[J].气象科学,2011,31(5):591-597,7.

基金项目

国家自然科学基金资助项目(40875030,40730948,40575018) (40875030,40730948,40575018)

上海台风研究基金(2008ST04). (2008ST04)

气象科学

OA北大核心CSCDCSTPCD

1009-0827

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