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一次阻塞型华北对流性暴雨过程的诊断分析和数值模拟
  • ISSN号:1000-0534
  • 期刊名称:高原气象
  • 时间:0
  • 页码:1283-1293
  • 分类:P426.62[天文地球—大气科学及气象学]
  • 作者机构:[1]内蒙古自治区气象台,内蒙古呼和浩特010051, [2]内蒙古气象科学研究所,内蒙古呼和浩特010051, [3]内蒙古自治区气象局,内蒙古呼和浩特010051
  • 相关基金:公益性行业(气象)科研专项(GYHY200706042); 国家自然科学基金项目(40965005)共同资助
  • 相关项目:东亚沙尘气溶胶的对流层-平流层输送
中文摘要:

利用常规和地面加密气象观测资料、卫星云图、NCEP再分析资料及中尺度模式MM5,对2006年7月23日一次阻塞型华北暴雨过程进行了诊断分析和数值模拟。结果表明,此次暴雨过程发生在以东西伯利亚阻塞高压为典型特征的大尺度鞍型场的背景下,宽广的低压区及高、低空急流次级环流为中尺度对流系统(MCS)的发生、发展提供了适宜的环境和动力强迫;700hPa和850hPa天气尺度的偏西水汽输送和低涡北侧的偏东水汽输送改善了环北京地区的水汽条件,暴雨发生前850hPa中尺度西南水汽输送对北京暴雨的发生有直接影响;MM5模式再现了导致MCS的形成及演变过程;中-β尺度MCS是这次暴雨的直接触发系统,其水平尺度约为0.5个经距,垂直方向由地面伸展到300hPa左右,具有典型的暖心结构,辐合、辐散中心分别位于900hPa和400hPa;MCS北侧强垂直次级环流为强对流的产生创造了有利条件。同时,MCS南侧相当位温的强梯度高能区及该区域的不稳定能量输送也是暴雨发生的重要条件。

英文摘要:

Using the routine and intensive observational data,the NCEP reanalysis data,the satellite images and the high resolution simulation result by MM5,a diagnosis and numerical simulation of a block type convective rainstorm process occurred in North China on July 23,2006 were conducted.The result showed that the process happened in the low pressure circulation,in which the East Siberia Block was the main feature.The broad low pressure area and the vertical secondary circulation induced by the jet stream provided the valuable environmental condition and dynamic forcing for the rainstorm.The water vapor transportation of synoptic scale on 700 hPa and 850 hPa,which was westerly direction to the south of 40°N and easterly direction on the north side of the low,improved the environmental moisture conditions around Beijing.Just before the occurrence of rainstorm,the mesoscale moisture transportation with south-westerly direction on 850 hPa is a key of forming rainstorm.MM5 model successfully reproduced the formation and evolution processes of the mesoscale convective systems(MCS),which was the directly weather system causing the rainstorm.The horizontally scale of MCS crossed 0.5 longitudes and from surface to 300 hPa vertically with a typical warm heart construction.The strong vertical secondary circulation,which was consistent with strong divergence on 400 hPa and convergence on 900 hPa,produced a favorable condition for the exploding of strong convection.Meanwhile,the instable energy transportation on the south side of the MCS,in which the intensive potential equivalent temperature gradient appeared,contributed to the rainstorm evidently.

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期刊信息
  • 《高原气象》
  • 北大核心期刊(2011版)
  • 主管单位:中国科学院
  • 主办单位:中国科学院 寒区旱区环境与工程研究所
  • 主编:文军
  • 地址:甘肃省兰州市天水中路8号
  • 邮编:730000
  • 邮箱:gybjb@lzb.ac.cn gyqx@lzb.ac.cn
  • 电话:0931-82600935
  • 国际标准刊号:ISSN:1000-0534
  • 国内统一刊号:ISSN:62-1061/P
  • 邮发代号:54-43
  • 获奖情况:
  • 中国自然科学核心期刊,1995年获甘肃省编校质量达标优秀期刊,中国期刊方阵“双效”期刊
  • 国内外数据库收录:
  • 美国剑桥科学文摘,日本日本科学技术振兴机构数据库,中国中国科技核心期刊,中国北大核心期刊(2004版),中国北大核心期刊(2008版),中国北大核心期刊(2011版),中国北大核心期刊(2014版),中国北大核心期刊(2000版)
  • 被引量:19859