2021年11月5-9日东北地区暴雪过程分析

Ruizhi Hu
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摘要

2021年11月东北地区降水较同期偏多。其中,同期降水最多的是东北地区的黑龙江和吉林。我研究了11月5日至9日的一次降雪天气过程,主要包括动态情况、天气背景和形势。结果表明:在欧亚大陆中高纬度地区,环流由纬向向经向调整,波动较大;槽后的北风不断将极地冷空气输送到南方。低压槽后的西北气流引导冷空气向东南爆发。在向南移动的过程中,冷空气与槽前的暖湿空气相遇,造成东北地区降雪。低气压东侧偏南气流和东南气流持续输送来自黄海和日本海的暖湿气流,增强了降雪。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Analysis of Snowstorm Process in Northeast China during 5-9 November, 2021
In November 2021, Northeast China had more precipitation than in the same period. Among them, Heilongjiang and Jilin provinces in the Northeast China were the highest precipitation in the same period. I study a snowfall weather process from November 5 to 9, which mainly includes dynamic situation, synoptic background and situation. The results show that: In the middle and high latitudes of Eurasia, circulation is adjusted from zonal to meridional with large fluctuations. The northerly wind behind the trough continuously transports the polar cold air to the south. The northwest airflow behind the trough led the cold air to erupt to the southeast. In the process of moving southward, the cold air meets the warm and humid air in front of the trough, causing snowfall in the northeast. The southerly airflow and southeasterly airflow on the east side of the vortex continued to transport warm and humid airflow from the Yellow Sea and the Sea of Japan, which enhanced the snowfall.
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