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南海热带气旋极端快速加强标准研究

龚月婷 程正泉 杨诗琪

热带气象学报2024,Vol.40Issue(4):650-658,9.
热带气象学报2024,Vol.40Issue(4):650-658,9.DOI:10.16032/j.issn.1004-4965.2024.057

南海热带气旋极端快速加强标准研究

Definition of Extremely Rapid Intensification of Tropical Cyclones over the South China Sea for Operational Forecasting

龚月婷 1程正泉 1杨诗琪1

作者信息

  • 1. 广东省气象台,广东 广州 510641
  • 折叠

摘要

Abstract

The definition of extremely rapid intensification(ERI)of tropical cyclones(TCs)and the statistical characteristics of TCs that experienced ERI(ERI TCs)over the South China Sea(SCS)were studied using the best track dataset from the Shanghai Typhoon Institute of China Meteorological Administration for TCs during 1981-2022.ERI was defined as intensity increases of at least 10 m·s-1·(6 h)-1,13 m·s-1·(12 h)-1,and 20 m·s-1·(24 h)-1 over the SCS and 10 m·s-1·(6 h)-1,20 m·s-1·(12 h)-1,and 30 m·s-1·(24 h)-1 over the western North Pacific(WNP),which corresponds to the 98th percentile of maximum intensity change for all TCs.Compared with conventional methods,the proposed ERI definition better describes the extremity of rapidly intensifying TCs and the intensity development difference between TCs over the WNP and the SCS.This makes it more useful for TC operational forecasting.Only 12%of TCs over the WNP and 4%of TCs over the SCS underwent ERI,and they were mainly located over the region bounded by 135~145 (°E),15~20 (°N) and the northern SCS near 20 (°N).72%of ERI TCs over the SCS made landfall in China,mostly in Hainan and Guangdong provinces,and 69%of these landing TCs occurred after 2000.ERI TCs over the SCS exhibited characteristics of being close to land,with short landing time and strong landing intensity,which significantly increased the difficulty of TC forecasting and disaster mitigation.

关键词

热带气旋/极端快速加强/标准/南海

Key words

tropical cyclone/extremely rapid intensification/definition/South China Sea

分类

天文与地球科学

引用本文复制引用

龚月婷,程正泉,杨诗琪..南海热带气旋极端快速加强标准研究[J].热带气象学报,2024,40(4):650-658,9.

基金项目

中国气象局重点创新团队(CMA2023ZD07) (CMA2023ZD07)

广东省气象局科技创新团队(GRMCTD202102) (GRMCTD202102)

广东省气象局科研基金(GRMC2022LM01)共同资助 (GRMC2022LM01)

热带气象学报

OA北大核心CSTPCD

1004-4965

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