摘要
利用Vaisala RS-92型GPS探空仪加密探测和飞机云物理探测资料,对2009年春季张家口地区一次层积云降水过程进行了研究。从准饱和区、位势不稳定区以及风场的演变等方面探讨了降水的宏观天气学特征;从水汽输送、水汽总含量变化,各高度水汽分布等方面分析了降水的水汽变化特征。同时,对GPS探空和飞机探测结果进行了对比分析。
Data from Vaisala RS-92 GPS raalosonue, and observed by aircraft are analyzed to research the feature of one spring stratiform cloud precipitation of 2009 at Zhangjiakou. Analyses of quasi-saturation areas, potential instability districts and the evolution of the wind field show the weather characteristics of this event. The result shows the reason of the water vapor variation through its transportation, total content variation and uneven distribution along the altitude. Furthermore, comparison between the Vaisala RS-92 GPS radiosonde data and the aircraft observed cloud physics data shows they can complement each other.
出处
《北京大学学报(自然科学版)》
EI
CAS
CSCD
北大核心
2011年第4期619-626,共8页
Acta Scientiarum Naturalium Universitatis Pekinensis
基金
国家科技支撑项目(2006BAC12B001)
灾害天气国家重点实验室开放课题(2010LASW-A09)资助
关键词
GPS探空
飞机探测
层积云降水
张家口
GPS radiosonde
aircraft detection
stratiform cloud precipitation
Zhangjiakou