一次豫北春季持续性大风天气的分析

An Analysis of Persistent Spring Gale in the Northern Henan Province

  • 摘要: 利用常规观测资料和NCEP再分析资料,分析了2015年3月31日到4月1日豫北大风过程持续的原因。结果表明,中高纬度冷空气的持续补充减缓了冷高压变性速度,中低纬度的西南气流使暖低压不断发展,形成对峙,使豫北长时间处于变压梯度和气压梯度大值区中,有利于豫北大风发展和维持。热力强迫的维持,有利于高低纬的气压中心和变压中心的维持,即有利于大风的维持。散度分布作用下产生的次级环流也有利于此次豫北大风的形成和维持。

     

    Abstract: Based on the conventional observation data and NCEP reanalysis data, this article analyzes the reasons of a persistent gale happened in the northern Henan Province on 31 March and 1 April 2015. Results show that the cold high pressure was persisting in the cold air flow from high latitudes, while warm low pressure was developing quickly the southwest air flow from low latitudes, it keeps a strong pressure gradient in the northern Henan for a long time, and benefits of the development and persistence of a gale. The persistence of thermal force is conducive to the persistence of the pressure gradient and then to the persistence of high winds. The secondary circulation generated by the distribution of divergence is also conducive to the formation and persistence of the gale.

     

/

返回文章
返回