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2007—2012年夏季中国青藏高原以东地区MCC的分布特征
引用本文:常春辉,丁治英.2007—2012年夏季中国青藏高原以东地区MCC的分布特征[J].气象科学,2015,35(4):445-453.
作者姓名:常春辉  丁治英
作者单位:南京信息工程大学 气象灾害省部共建教育部重点实验室, 南京 210044,南京信息工程大学 气象灾害省部共建教育部重点实验室, 南京 210044
基金项目:国家重点基础研究发展计划(973计划)项目(2009CB421503;2013CB430103);国家自然科学基金资助项目(41375058);江苏省优秀科技创新团队基金;江苏高校优势学科建设工程资助项目(PAPD)
摘    要:用FY-2D和FY-2E地球静止卫星相当黑体温度资料,对2007—2012年夏季(6—8月)中国青藏高原以东地区的中尺度对流复合体(MCC)进行普查分析,并分为MCC和类MCC(偏心率在0.5~0.6之间),共计190个MCC和62个类MCC。西南和华南地区的MCC和类MCC占总数的60%,华东和华中地区占总数的27%,东北、华北和西北地区最少。两类MCC的生成源地和消散地的海陆性质相同。东北和华北地区MCC主要向东北移动,华中和华东地区MCC向东南移动。华南和西南地区的MCC移动方向具有多样性,大多为不移动类型。从月际变化来看,MCC在6月份最多,类MCC在7月份最多。MCC的日变化具有区域性特征,西南地区的MCC在22:00—23:00是形成高峰,03:00—04:00达到成熟,06:00—08:00开始消散。东北、华北、华中和华东地区的MCC形成高峰在16:00—18:00,19:00—23:00和02:00—03:00是成熟高峰,21:00—01:00消散。华南地区的MCC主要形成在23:00—03:00,11:00—14:00成熟,14:00—15:00消散。

关 键 词:中尺度对流复合体  地理分布  移动路径  青藏高原
收稿时间:2013/11/28 0:00:00
修稿时间:2014/1/11 0:00:00

Distribution characteristics of MCCs in eastern Tibetan Plateau in summer from 2007 to 2012
CHANG Chunhui and DING Zhiying.Distribution characteristics of MCCs in eastern Tibetan Plateau in summer from 2007 to 2012[J].Scientia Meteorologica Sinica,2015,35(4):445-453.
Authors:CHANG Chunhui and DING Zhiying
Institution:Key Laboratory of Meteorological Disaster of Ministry of Education, Nanjing University of Information Science & Technology, Nanjing 210044, China and Key Laboratory of Meteorological Disaster of Ministry of Education, Nanjing University of Information Science & Technology, Nanjing 210044, China
Abstract:Based on the FY-2D and FY-2E geostationary satellite black body temperature(TBB) data in summer (June to August) from 2007 to 2012, the mesoscale convective complexes(MCC) in the eastern Tibetan Plateau of China were investigated and were classified into MCC and similar MCC(0.5-0.6 eccentricity).Results reveal that there were 190 MCCs and 62 similar MCCs in summer during 6 years. 60% MCCs and similar MCCs occurred in southwest China and south China, 27% in central-eastern China, but in northeast China, northwest China and north China they occurred the least. The land and sea properties of formation and dissipation regions of the two types of MCCs were similar. MCCs in northeast China and north China moved towards northeast; while in central-eastern China, mainly to southeast. Most of the MCCs in south China and southwest China moved in various directions, and most of them were almost stagnant. MCCs happened most in June while similar MCCs in July. The diurnal variation of MCC differed one from another: in southwest China, it formed at 22:00-23:00, matured in the early morning of 03:00-04:00 then dissipated in the morning of 06:00-08:00; in northeast China, north China, central and eastern China, it generated in the afternoon of 16:00-18:00, matured at night of 19:00-23:00 and in the early morning of 02:00-03:00, finally dissipated at night of 21:00-01:00; in south China, it formed around midnight of 23:00-03:00,matured around midday of 11:00-14:00 and disappeared at 14:00-15:00.
Keywords:MCC  Geographical distribution  Shift path  Tibetan Plateau
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