What are the frontal weather in China? And a brief analysis

There are mainly three kinds of frontal weather in China, namely, quasi-static front, warm front and cold front, which are determined by the strength of the converging cold and warm air masses.

The northwest monsoon prevailing in winter in China is dominated by the cold front, and the southeast monsoon prevailing in summer is mainly covered by warm wind. At the same time, there is a quasi-static front in the middle and lower reaches of the Yangtze River in summer, that is, Meiyu in the middle and lower reaches of the Yangtze River.

In winter, there is also a quasi-static front in China, that is, the quasi-static front in Kunming, because the terrain of Yunnan-Guizhou Plateau is too undulating. The cold air cannot rise, which leads to the formation of Kunming quasi-static front in Yunnan-Guizhou Plateau.