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2009年秋季河南一次连阴雨天气成因分析
引用本文:孔海江,吴胜安,王蕊,赵培娟,乔春贵,吕晓娜. 2009年秋季河南一次连阴雨天气成因分析[J]. 气象与环境学报, 2011, 27(2): 39-44
作者姓名:孔海江  吴胜安  王蕊  赵培娟  乔春贵  吕晓娜
作者单位:1.中国科学院大气物理研究所,北京 100029;2.中国科学院研究生院,北京 100049;3.河南省气象台,河南 郑州 450003;4.中国气象局农业气象保障与应用技术重点开放实验室,河南 郑州 450003
基金项目:中国气象局农业气象保障与应用技术重点开放实验室项目“河南省关键农事季节连阴雨中期预报方法研究”(Z201003)、“河南省持续性暴雨中期预报方法研究”(Z200903); 公益性行业(气象)科研专项“夏玉米高产稳产气象保障关键技术研究”(CYHY201006041)第7子专题(气象灾害监测、预报预警)共同资助
摘    要:采用合成分析和动力诊断分析及统计方法,利用NCEP资料和常规气象观测资料对造成2009年9月6-20日河南省北中部地区15 d连阴雨天气成因进行分析.结果表明:200 hPa高空急流的出现并且维持,南亚高压的偏东偏北,副热带高压的偏西略偏北,以及边界层的东北风(或偏东风),是造成此次长连阴雨天气的主要影响因素;200 ...

关 键 词:连阴雨  副热带高压  高空急流  边界层
收稿时间:2010-12-16

Study on forming reasons of a continuous autumn rain event in 2009 in He'nan province
KONG Hai-jiang,WU Sheng-an,WANG Rui,ZHAO Pei-juan,QIAO Chun-gui,LV Xiao-na. Study on forming reasons of a continuous autumn rain event in 2009 in He'nan province[J]. Journal of Meteorology and Environment, 2011, 27(2): 39-44
Authors:KONG Hai-jiang  WU Sheng-an  WANG Rui  ZHAO Pei-juan  QIAO Chun-gui  LV Xiao-na
Affiliation:1. Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China; 2. Graduate University of Chinese Academy of Sciences, Beijing 100049, China; 3. He’nan Meteorological Observatory, Zhengzhou 450003, China; 4. Key Laboratory of Agrometeorological Safeguard and Applied Technique, China Meteorological Administration, Zhengzhou 450003, China
Abstract:Based on NCEP data and the conventional observation data, forming reasons of a continuous autumn rain event on September 6 to 20 in 2009 were analyzed in the mid-north region of He’nan province. The results indicate that the main reasons causing this process are the occurrence and maintenance of upper level jet in 200 hPa, the leaning eastern and northern South Asia high, the northwestern subtropical high pressure and the northeastern wind in boundary layer (or the easterly wind). The positive anomaly in East Asia westerly jet of 200 hPa and warm anomaly in the middle and upper layers of troposphere (300 hPa) match each other on dynamic relation. The shallow wet layer, insufficient water vapor conditions and the lower level influenced by cold air could make the accumulative total precipitation of the continuous autumn rain lower. Temperature anomaly increases with height and makes high cloud cover increasing, which is the possible reason for few sunshine and lower air temperature.
Keywords:A continuous rain  Subtropical high pressure  Upper level jet  Boundary layer  
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