Influence of Kunming quasi-static front on Zhenxiong County

Affect weather and climate. The quasi-static front in Kunming is an atmospheric phenomenon in Yunnan-Guizhou Plateau, which is mainly formed by metamorphic polar continental air mass and southwest airflow blocked by Yunnan-Guizhou Plateau topography. Clouds are low and thin, and it is easy to form continuous rainy weather. In winter, quasi-static fronts in Kunming mostly appear in Zhenxiong County, which will lead to changeable weather in Zhenxiong County, including rainy weather, snowfall, rainfall and other weather phenomena.