The impact of Kunming quasi-stationary front on Zhenxiong County

Influence weather and climate. The Kunming quasi-stationary front is an atmospheric phenomenon in the Yunnan-Guizhou Plateau. It is mainly formed by the evolution of degenerated polar continental air masses and southwest airflow blocked by the terrain of the Yunnan-Guizhou Plateau. The clouds are low and thin, and it is easy to form continuous rainy weather. In winter, Kunming quasi-stationary fronts mostly appear in Zhenxiong County, which can cause changeable weather in Zhenxiong County, including rain, snowfall, rainfall and other weather phenomena.