摘要
利用江淮地区常规观测资料、FY2C卫星资料以及NCEP/NCAR提供再分析资料计算的多种物理量场,分析了2007年6月27—30日发生在湖北地区的一次强降水天气过程,结果表明:①此次强降水过程是一次典型的梅雨锋降水,降水强度大,持续时间长;②在对流层中层高纬度地区存在阻塞高压,中纬度地区表现为稳定的高空槽,而低纬度的东部沿海地区处于副高西侧控制,属于梅雨期的典型流场分布;高低空急流配置,对流层中低层的不稳定能量以及丰沛水汽输送等因素,共同触发了此次灾害性强降水过程的发生.③卫星TBB资料较好地描述了此次强降水过程表现出雨量分布不均,强度大的特征,黑体温度低值区与强降水区域一致.
In order to study mechanism of heavy rainfall in plum rain period,the paper use the data of global from 27 June to 30 June in 2007 of NCEP / NCAR and the same time of the data of general observations,FY2C in China's Jianghuai region to analysis a heavy precipitation in plum rain period.The results show that:①The heavy precipitation is a typical precipitation in plum rain period.The intensity of rainfall is strong,and it last a long time.②There is blocking high in the middle troposphere in high latitudes,and mid-latitudes showed stable upper trough,while the eastern coastal areas in the control of the subtropical high in the low latitudes.It is belong to a typical plum rain season flow field.The high or low jet,unstable energy in low level troposphere,and abundant moisture transportation are the important factors for the catastrophic heavy rainfall.③The data of satellite describe the characteristic of the heavy precipitation process,including the distribution uneven and the large intensity.The low value area of blackbody temperature corresponds to heavy precipitation area.
出处
《云南大学学报(自然科学版)》
CAS
CSCD
北大核心
2013年第S2期243-253,共11页
Journal of Yunnan University(Natural Sciences Edition)
基金
国家自然科学基金(U0933603)
高原大气与环境四川省重点实验室开放课题(PAEKL-2013-K3)
关键词
梅雨
诊断分析
环流分析
动力过程
热力过程
meiyu
diagnostic analysis
circulation analysis
physical process
energy process