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机构地区:[1]College of Atmospheric Sciences of Lanzhou University Lanzhou 730000 China,DalianMeteorological Observatory, Dalian 116001 China [2]Chinese Academy of Meteorological Sciences Beijing100081 China [3]College of Atmospheric Sciences of Lanzhou University Lanzhou 730000 China
出 处:《Journal of Tropical Meteorology》2006年第1期99-100,共2页热带气象学报(英文版)
基 金:Project 973 from the Ministry of Science and Technology of China (2004CB418301);a projectof Natural Science Foundation of China (40175019)
摘 要:1 INTRODUCTION Tropical cyclones (TCs) moving north and getting to the Liaodong Peninsula and waters of the Yellow and Bohai Seas are in their late phase of life cycle. While weakening rapidly, TCs carry a large amount of warm and humid air that forms heavy rainfall by itself on the one hand and interact with westerlies in the middle latitudes on the other. With their warm-core structure destroyed by intruded cooler air, TCs absorb baroclinic energy while it weakens and experiences extratropical transition (ET). With right conditions and complicated topographic features of the peninsula, the transformed extratropical cyclone evolves to intensify heavy rainfall in most cases and even results in secondary disasters like storm surges. Therefore, the extratropical transition of TCs is usually responsible for more serious damage in mid-latitude areas. For the forecast of heavy rain associated with north-going TCs experiencing extratropical transition, it not only involves their own intensity and structure but also the distribution of the surrounding field and its interactions with TCs. Most of the present studies discuss TCs-inflicted heavy rains or those taking place south of the Shandong Peninsula. Focusing on intense precipitation resulted from TCs over the Liaodong Peninsula, this work analyzes the distribution of the ambient field and physical quantities hoping to help forecast TCs-related heavy rains accurately.
关 键 词:Tropical cyclone Liaodong peninsula comparative analysis severe precipitation
分 类 号:P444[天文地球—大气科学及气象学]
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