Author(s)

Ruiqi Li

School of Atmospheric Sciences, Nanjing University of Information Science and Technology, Nanjing, China.

The China National Climate Center and National Centers for Environmental Prediction data were used in this work. Using the knowledge of synoptic principles and synoptic analysis, the rain and snow weather process in the middle and east of China from December 28 to 30, 2020 was analyzed. The results show that: 1) This weather process was a large-scale precipitation process. Affected by the cold wave, the temperature drops sharply, and the temperature in many places dropped below the extreme value, accompanied by strong winds. 2) This process is mainly caused by the eastward movement of the upper-level trough leading the cold air southward to intersect with the warm and wet air, and the shear thread in the lower layer cooperates. 3) The cold air is from the ocean east of Novaya Zemlya. 4) From the evolution trend of 500 hPa geopotential height field and ground pressure field, the cold surge process belongs to the type of transverse trough to vertical.

Precipitation, Cold Surge, Style, Cold Front, Atmospheric Circulation

Li, R. (2023) Analysis of Rain and Snow Weather Process in the Middle and East of China from December 28 to 30, 2020. Journal of Geoscience and Environment Protection, 11, 181-191. doi: 10.4236/gep.2023.117012.