What's the climate like in most parts of South Asia?

Most parts of South Asia belong to tropical monsoon climate, characterized by high temperature and rainy summer, warm and dry winter, divided into obvious dry and wet seasons, and high temperature throughout the year.

Most of South Asia has a tropical monsoon climate, which is divided into hot season (March-May), rainy season (6-65438+1October) and cool season (165438+1October to February of the following year). The temperature is high throughout the year and the precipitation changes greatly. The rainfall on the windward slope of the southwest monsoon is extremely rich, which is one of the highest rainfall areas in the world (such as Kira Bangqi, India). There is less precipitation in northwest China.

Most of South Asia lies north of the equator and south of 30 north latitude. Except for the tropical desert climate in northwestern India and southern Pakistan, most other areas have tropical monsoon climate. The formation of South Asian monsoon climate is closely related to the difference of thermal properties between land and sea, the seasonal movement of wind belt in pressure zone and the topography of Qinghai-Tibet Plateau.