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南海土台风和非局地台风的对比研究
引用本文:程 撼,梁楚进,董昌明,刘正礼.南海土台风和非局地台风的对比研究[J].海洋学研究,2014,32(1):19-30.
作者姓名:程 撼  梁楚进  董昌明  刘正礼
作者单位:1.卫星海洋环境动力学国家重点实验室,浙江 杭州 310012;2.国家海洋局 第二海洋研究所,浙江 杭州 310012;3.地球与行星物理研究所,美国加州大学洛杉矶分校,美国加利福尼亚州 洛杉矶 90095;4.中海石油(中国)有限公司 深圳分公司 钻井部,广东 深圳 518067
基金项目:国家重点基础研究发展计划项目资助(2012CB417303);全球变化与海气相互作用专项资助
摘    要:利用1951—2012年日本气象厅(JMA)热带气旋(TC)最佳路径资料,分析了影响南海的土台风和非局地台风62 a间的时空分布特征,比较了二者在时空分布上的差异性,得到以下主要结果:土台风源地位置与热带季风性气候有关,夏季风时主要在15°N以北,冬季风时向15°N以南移动;土台风与非局地台风相比,活动范围更广,但强度比后者弱;土台风在南海的强度发展过程呈对称曲线形式,非局地台风则是一条递减曲线;土台风和非局地台风的登陆位置都具有季风期规律,夏季风时登陆的TC比冬季风时登陆的多得多,同纬度的非局地台风比土台风移动速度大。

关 键 词:南海  热带气旋  土台风  非局地台风  登陆  季风  
收稿时间:2013-06-25

Temporal and spatial distribution of local typhoon and non-local typhoon in the South China Sea
CHENG Han,LIANG Chu-jin,DONG Chang-ming,LIU Zheng-li.Temporal and spatial distribution of local typhoon and non-local typhoon in the South China Sea[J].Journal of Marine Sciences,2014,32(1):19-30.
Authors:CHENG Han  LIANG Chu-jin  DONG Chang-ming  LIU Zheng-li
Institution:1. State Key Laboratory of Satellite Ocean Environment Dynamics, Hangzhou 310012,China;2. The Second Institute of Oceanography, SOA,Hangzhou 310012, China;3. Institute of Geophysics and Planetary Physics, University of California, Los Angeles CA 90095, USA;4. Drilling Department, Shenzhen Branch of CNOOC Ltd. , Shenzhen 518067, China
Abstract:The best track data of tropical cyclones (TC) for 62 years (1951-2012) obtained from Japan Meteorological Agency (JMA) were used to make an analysis on the temporal and spatial distribution of two kinds of tropical cyclones, i. e. entitled local typhoon and non-local typhoon which have impact on the South China Sea (SCS). The result suggests that local typhoon’s sources are associated with the monsoon period. In summer monsoon, the sources mainly located on the north of 15°N, and in winter monsoon, it moved to the south of 15°N. Compared with non-local typhoon, local typhoon’s activity is broader in space, but weaker in intensity in commonly. In the intensity development process, the time-intensisy curve of local typhoon is almost symmetrical, but that of non-local typhoon is a decline curve. The two kinds of TC’s landing positions are also associated with the monsoon. In summer monsoon, local typhoon and non-local typhoon make landfall more frequently than those in winter monsoon. And in the same latitude, non-local typhoon moves faster than local typhoon.
Keywords:SCS  tropical cyclone  local typhoon  non-local typhoon  landfall  monsoon  
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