刘永明, 盛永昆. 楚雄州“2013.8.29”强降水天气过程分析[J]. 云南大学学报(自然科学版), 2014, 36(S1): 95-102. doi: 10.7540/j.ynu.20140014
引用本文: 刘永明, 盛永昆. 楚雄州“2013.8.29”强降水天气过程分析[J]. 云南大学学报(自然科学版), 2014, 36(S1): 95-102. doi: 10.7540/j.ynu.20140014
LIU Yongming, SHENG Yongkun. Chuxiong “2013.8.29” heavy precipitation process analysis[J]. Journal of Yunnan University: Natural Sciences Edition, 2014, 36(S1): 95-102. DOI: 10.7540/j.ynu.20140014
Citation: LIU Yongming, SHENG Yongkun. Chuxiong “2013.8.29” heavy precipitation process analysis[J]. Journal of Yunnan University: Natural Sciences Edition, 2014, 36(S1): 95-102. DOI: 10.7540/j.ynu.20140014

楚雄州“2013.8.29”强降水天气过程分析

Chuxiong “2013.8.29” heavy precipitation process analysis

  • 摘要: 应用micaps常规观测资料及FY-2E卫星云图,通过对环流形势场和物理量场的诊断分析研究了2013年8月29—30日发生在楚雄州地区的一次强降水天气过程.结果发现,这次天气过程发生在有利的环流背景形势下,由于川滇切变和辐合区的共同影响,以及孟加拉湾源源不断的水汽输送,卫星云图显示楚雄区域上的系统性对流云系旺盛,在冷暖空气的共同作用下,造成了这次楚雄州中到大雨局部暴雨的强降水天气过程.有利的热力环境、水汽条件和良好的动力条件是此次强降水产生和得以维持的机制.

     

    Abstract: Using micaps conventional observation data,FY-2E satellite image,through the circulation patterns and physical fields Field Diagnostic analyzes of the August 29,2013-August 30 occurred in Chuxiong region a heavy rainfall weather process.It was found that this process occurs in favorable weather circulation background situation,because Chuandian shear and high altitude combined effect of convergence zone,and the Bay of Bengal,a steady stream of water vapor transport,satellite images show systematic Chuxiong area strong convective clouds,and the interaction between cold and warm air,causing moderate to heavy rain this Chuxiong strong locally heavy rainfall weather process.Favorable thermodynamic environment,moisture conditions and good dynamic conditions is the heavy precipitation mechanisms for generating and maintained.

     

/

返回文章
返回