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出 处:《黑龙江气象》2017年第3期1-3,共3页Heilongjiang Meteorology
摘 要:本文利用常规观测资料,对2014年11月30日和2016年11月4日牡丹江出现的两场暴雪天气过程进行初步对比分析,结果表明:过程1是高空阶梯槽的形成和维持,为暴雪提供了有利的环流背景,配合地面低压倒槽结构产生的暴雪过程;过程2是鄂霍次克海上空的冷涡系统配合西北高空急流,将西伯利亚附近的冷空气输送到黑龙江省,与低层的暖湿空气交汇而产生的,地面受蒙古低压影响。物理量场上,过程2水汽条件和动力条件均好于过程1,充足的水汽条件是降水过程产生和维持的重要条件,而低层辐合高层辐散的抽吸作用,为降水的产生提供了有利动力条件。Analyze the two snowstorm weather events of Mudanjiang happened on November 30, 2014 and November 4, 2016 with the conventional observation data, the results show that, Process 1: the formation and maintenance of the high-altitude ladder provides a favorable circulation background and with the ground low-pressure inverted structure which yield the Blizzard;process2: Okhotsk sea cold vortex system with the northwest high-altitude jet bring the cold air near Siberia to Heilongjiang province, which join in the low-level warm and humid air and Blizzard happened, the ground is affected by low pressure in Mongolia. Physical field, water vapor conditions and dynamic conditions of the process of 2 are better than that of the process 1, the sufficient water vapor condition is an important condition for the generation and maintenance of the precipitation process, while the low-level convergence of the high-level divergence of the suction effect provide a favorable power conditions to the precipitation.
分 类 号:P458[天文地球—大气科学及气象学]
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