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《Plateau Meteorology》 2006-03
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Mesoscale Numerical Simulation of a Heavy Snowfall Process in Northern China

JIANG Xue-gong~(1,2),LI Zhang-jun~(3), KANG Ling~(2), SHI Shao-hong~(2)(1.Inner Mongolia Ecological and Agricaltural Meteorological Center,Huhhot 010051,China;2.Inner Mongolia Meteorological Observatory,Huhhot,010051 China;3.Inner Mongolia Meteorological Bureau,Huhhot 010051,China)  
Using the mesoscale modle MM5,a snowstorm process in the middle and southern part of Inner Mongolia from 14 to 16 March,2003 is simulated.The results shown that the strength,position and time change of heavy snowfall center are successfully simulated.The main effect system of causing snowstorm process is surface inverse trough and 700 hPa meso-α-scale low vortex,and its impact time is relative to the lasting.The couple of divergence in upper troposphere and convergence in lower troposphere producted the short wave trough in upper level induced the heavy snowfall to occur,but it induced two peak values in the snowfall process.Meanwhile,the forming and strengthening of meso-α-scale low vortex and its fitting collocation with warm and wet jet flows in low level are another factor of heavy snowfall occurring.The Yinshan mountain has a great impact on the strength and position of the snowfall process.It made the snowfall strenthened at the south of mountain and minimized at the north of mountain.The lifting of topographic forcing is direction reason of the heavy snowfall.The impact of the topography on the divergence was complex and in this condition the associationbetween the lower level divergence and the ascendingmotion became faintness.
【Fund】: 国家社会公益专项资金项目“我国牧区暴风雪灾害监测预警系统研究”资助
【CateGory Index】: P426.63
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3 YE Du zheng 1, CHOU Ji fan 2, LIU Ji yuan 3, ZHANG Zeng xiang 4, WANG Yi mou 5, ZHOU Zi jiang 6, JU Hong bo 7, HUANG Hong qian 8 (1 Institute of Atmospheric Physics, CAS, Beijing 100029, China; 2 Beijing Institute of Meteorology, Beij;Causes of Sand-stormy Weather in Northern China and Contral Measures[J];ACTA GEOGRAPHICA SINICA;2000-05
4 Zeng Qing-cun Li Rong-feng(Institute of Atmospheric Physics, Academia Sinica);ON THE COMPUTATIONAL CHAOS IN THE FINITE DIFFERENCE SCHEMES WITH NON-UNIFORM GRIDS[J];Chinese Journal of Atmospheric Sciences;1982-04
5 Hu Yinqiao ( Lanzhou Institute of Plateau Atmospheric Physics, Chinese Academy of Sciences, Lanzhou 730000) Y Mitsuta ( Disaster Prevention Research Institute, Kyoto University, Uji, Kyoto 611, Japan );Micrometeorological Characteristics and Local Triggering Mechanism of Strong Dust Storm[J];SCIENTIA ATMOSPHERICA SINICA;1997-05
6 Huang Meiyuan and Wang Zifa (State Key Laboratory of Atmospheric Boundary Physics and Atmospheric Chemistry, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029);A Model for Long-range Transport of Yellow-sand in East Asia[J];SCIENTIA ATMOSPHERICA SINICA;1998-04
7 Zhou Zijiang (National Meteorological Center, Beijing 100081);BLOWING-SAND AND SANDSTORM IN CHINA IN RECENT 45 YEARS[J];Quaternary Sciences;2001-01
8 ;The causes of sand dust transport in the deserts of China and in North Africa[J];Quaternary Sciences;2001-02
9 FAN Yi da 1, SHI Pei jun 1,WANG Xiushan 2, PAN Yao zhong 1 (1. Institute of Resources Science, Beijing Normal University, China Center of Desert Research at Beijing Normal University, Key Laboratory of Environmental Change and Natural Disaster,;THE ANALYSIS OF TYPICAL DUST STORM IN NORTHERN CHINA BY REMOTE SENSING[J];Advance In Earth Sciences;2002-02
10 QIAN Yun, FU Congbin, WANG Shuyu (START Regional Center for TEA, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029,China);MINERAL DUST AND CLIMATE CHANGE[J];ADVANCE IN EARTH SCIENCES;1999-04
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