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《Meteorological Monthly》 2011-09
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The Role of Sea Breeze Front in Local Storm of Bohai Coast

DONG Gaohong~1 HE Qunying~1 LIU Yiwei~1 XIE Yiyang~2 DAI Yunwei~3 1 Tianjin Meteorological Observatory,Tianjin 300074 2 Tianjin Institute of Meteorological Science,Tianjin 300074 3 China Meteorological Huayun Company,Beijing 100081  
Using the data obtained by conventional observations,ground densified automatic weather stations, Doppler radar observations and mesoscale TJ-WRF model,we analyze the heavy rain occurring on 6 July 2009 at Ninghe District of Tianjin and highlight the trigger mechanism of coastal local storm caused by sea breeze front of the Bohai Gulf.The results show that the heavy rain occurred in the favorable weather conditions,and there were local instability and adequate vapor conditions.Sea breeze front itself has a convergent uplift area where weak convection exists;when sea breeze front moves to the unstable and adequate vapor areas,it will strengthen the convergence positive movement of convergent uplift area and lead to the new storm development.The meeting of the sea breeze front and thunderstorm will play a strengthened role in its development.By analyzing the data obtained by mesoscale WRF model,we can see that at the warm and dry ground in front area near the north end of the wet air interchange,the intersection of the two convergence lines is easy to stimulate strong thunderstorms,and thunderstorm accrues at the intersection of the north of the subaerial warm and dry front zone and humid air.Sea breeze front plays an important role in the development of the thunderstorm.
【Fund】: 公益性行业(气象)科研专项(GYHY200906011);; 北京城市所基金课题(UMRF201008);; 国家科技支撑计划重点项目(2008BAC37B05) (2008BAC37B01)共同资助
【CateGory Index】: P458.121.1
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【Citations】
Chinese Journal Full-text Database 10 Hits
1 Jin Hao and Wang Yanchang(Department of Atmospheric Sciences, Nanjing University);NUMERICAL SIMULATION OF THREE DIMENSIONAL SEA LAND BREEZE[J];Chinese Journal of Atmospheric Sciences;1991-05
2 Liu Liping 1), Shao Aimei 2), Ge Rensheng 1), and Liang Haihe 1)1) (Chinese Academy of Meteorological Sciences,Beijing 100081) 2) (Department of Atmospheric Sciences, Lanzhou University,Lanzhou 730000);A Study of Mesoscale Wind Structures in Heavy Rainfall System of Merging Cloud with Dual-Doppler Radar[J];Chinese Journal of Atmospheric Sciences;2004-02
3 Chang Zhiqing Wu Zengmao Gao Shanhong(Institute of Physical Oceanography, Ocean University of China, Qingdao 266003, China);Numerical simulation Three Dimensional Structure of Sea and Land Breezes over Qingdao[J];Journal of Ocean University of Qingdao;2002-06
4 Yu Enhong Chen Bin Bai Yurong(Meteorogical Research Institute in Tianjin);LAND AND SEA BREEZES IN THE WESTERN BOHAI WAN[J];Acta Meteorologica Sinica;1987-03
5 Shan Yichang Liu Guicai Zhang Xiuzhen Gao Xiaomei (Weifang Meteorological Office, Shandong Province 261011);Analysis and Nowcasting of Frequent and Severe Convections in Coastal North of Shandong Province[J];Meteorological Monthly;2003-11
6 Wang Yan Li Shengshan Quo Li Feng Jinhu Wang Qingyuan Dong Gaohong Tianjin Meteorological Observatory,300742;Chinese Academy of Meteorology Sciences,Beijingi Binhai Meteorological Office,Tianjin;Doppler Radar Echo Features of Sea Breeze Front in Bohai Bay[J];Meteorological;2006-12
7 Lu Huanzhen1 Zhao Yujie1 Yu Xiaoding2 Feng Jinhu1(1.Binhai Meteorological Office,Tianjin 300457;2.China MeteorologicalAdministration Training Center);Comparative Analysis of Sea-land Breeze Convergence Line along Bohai Gulf with Radar CINRAD-SA and Automatic Meteorological Station Data[J];Meteorological Monthly;2008-09
8 HE Qunying~1 XIE Yiyang~2 DONG Gaohong~1 LIU Yiwei~3 SUN Yixin~4 1 Tianjin Meteorological Observatory,Tianjin 300074 2 Tianjin Research Institute of Meteorological Science,Tianjin 300074 3 Nanjing University of Information Science and Technology,Nanjing 210044 4 Nanjing University,Nanjing 210093;The Role of Sea-Land Breeze Circulation in Local Convective Torrential Rain Happening in Tianjin on 26 September 2009[J];Meteorological Monthly;2011-03
9 Fu Xiuhua (Institute of Atmospheric Physics,Academia Sinica)Li Xingsheng (Academy of Meteorological Science,SMA)Lü Naiping (National Environmental Forecasting Center,SOA)Shi Luhuai (Environmental Protect Institute for Electrical Power,MER);THREE DIMENTIONAL NUMERICAL MODEL OF THE SEA AND LAND BREEZE WITH COMPLEX TERRAIN[J];Quarterly Journal of Applied Meteorology;1991-02
10 Liu Yunce Zhuang Xudong Li Xianzhou (Guangzhou Central Meteorological Observatory, Guangzhou 510080);SEVREE LOCAL STORMS INITIATED BY THE SEA BREEZE FRONT IN THE PEARL RIVER DELTA DURING THE LATE SPRING AND SUMMER[J];Quarterly Journal of Applied Meteorlolgy;2001-04
【Secondary Citations】
Chinese Journal Full-text Database 10 Hits
1 Jin Hao and Wang Yanchang(Department of Atmospheric Sciences, Nanjing University);NUMERICAL SIMULATION OF THREE DIMENSIONAL SEA LAND BREEZE[J];Chinese Journal of Atmospheric Sciences;1991-05
2 Bei Naifang and Zhao Sixiong(Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029);Mesoscale Analysis of Severe Local Heavy Rainfall during the Second Stage of the 1998 Meiyu Season[J];Chinese Journal of Atmospheric Sciences;2002-04
3 Sun Jianhua and Zhao Sixiong(Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029);A Study of Mesoscale Convective Systems and Its Environmental Fields during the June 1994 Record Heavy Rainfall in South China Part Ⅱ: Effect of Physical Processes, Initial Environmental Fields and Topography on Meso-β Convective System[J];Chinese Journal of Atmospheric Sciences;2002-05
4 Lei Hengchi, Wang Hong, Hu Zhaoxia, Xiao Hui and Huang Meiyuan(Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029);A Numerical Research on Rain Storm Kinetic Process of the Wuhan Area on July 21,1998[J];Chinese Journal of Atmospheric Sciences;2002-05
5 Liu Liping 1), Shao Aimei 2), Ge Rensheng 1), and Liang Haihe 1)1) (Chinese Academy of Meteorological Sciences,Beijing 100081) 2) (Department of Atmospheric Sciences, Lanzhou University,Lanzhou 730000);A Study of Mesoscale Wind Structures in Heavy Rainfall System of Merging Cloud with Dual-Doppler Radar[J];Chinese Journal of Atmospheric Sciences;2004-02
6 SUN Ji-Song~(1,2),WANG Hua~1,WANG Ling~1,LIANG Feng~1,KANG Yu-Xia~(1),and JIANG Xiao-Yan~(3)1 Beijing Meteorological Observatory,Beijing 1000892 State Key Laboratory of Severe Weather,Chinese Academy of Meteorological Sciences,Beijing 100081 3 Beijing Urban Meteorological Institute,China Meteorological Administration,Beijing 100089;The Role of Urban Boundary Layer in Local Convective Torrential Rain Happening in Beijing on 10 July 2004[J];Chinese Journal of Atmospheric Sciences;2006-02
7 Wang Weiguo and Jiang Weimei(Department Of Atmospheric Sciences,Naming University, Naming 210093);Numerical Simulation on the Structure of the Atmospheric Boundary Layer in Qingdao Regions[J];SCIENTIA ATMOSPHERICA SINICA;1996-02
8 LIAN Zhi-luan1,GAO Lian-shan1,LI Guo-cui1,ZHAO Rui-jin2,ZHAO Yan-chang1(1.Shijiazhuang Meteorological Bureau,Shijiazhuang 050081,China;2.Hebei Meteorological Observatory,Shijiazhuang 050021,China);Analayese on CG Lightning Characteristics in Hailstorm process in Center-South Parts of Hebei Caused East Mongolia Cold Vortex[J];Plateau Meteorology;2009-01
9 LI Jie, WU Zeng mao, HE Min, GUO Jing tian, YUE Shu hong, GUAN Qin le (Ocean University of China, Qingdao 266003, China );BASIC CHARACTERISTIC ANALYSIS OF WEATHER UNFAVOURABLE TO QINGDAO OLYMPIC GAMES SAIL BOAT RACING[J];Coastal Engineering;2002-04
10 Lin Li,Li Rong,Zhang Xia,Feng Huimin,Wang Hongxing (Zhengzhou Meteorological Bureau,Zhengzhou 450005,China);Analysis of the Stability and Energy Parameters in a Short-time Rainstorm[J];Meteorological and Environmental Sciences;2007-04
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