Characteristics of heat distribution in Asia

Affected by the subtropical high, the weather in West Asia is sunny and hot with little rain and high temperature. East Asia has a monsoon climate, among which Southeast Asia has a tropical monsoon climate, with high temperature, rainy weather and humid heat. The subtropical monsoon climate in the central part of China is similar to that in Shanghai. There are four distinct seasons throughout the year. From mid-June to early July every year, there is continuous rainfall (plum rain) affected by quasi-static front, and the temperature is low. Then, affected by the subtropical high in the northwest Pacific, there was a summer drought. Winter in the Asian continent is hot, sunny and cold. Further north is the temperate monsoon climate, which is cold in winter, mostly between 0~- 15℃, with little rain and snow and high temperature and rainy in summer. Generally speaking, rain and heat are the same, similar to Beijing. Finally, northern Asia, such as eastern Russia (although Russia belongs to Europe, many places can actually be regarded as Asia), belongs to the sub-cold zone coniferous forest climate, and the weather is cold all year round.