Causes of high temperature weather in India

India is a monsoon country. Before the rainy season every year (from June to 10), it is often controlled by subtropical high for a long time, and high temperature weather occurs. At the same time, there is also the Qinghai-Tibet Plateau in northern India, and the special terrain is also one of the reasons for this climate.

The interaction of radiation intensity, topography and weather system makes the temperature in India higher than that in the same latitude area, sometimes reaching 45℃ to 48℃.

Extended data:

Climatic characteristics

The whole of India is hot, and most of it belongs to tropical monsoon climate, while thar desert in western India belongs to tropical desert climate. There is an obvious monsoon in summer and no obvious monsoon in winter. The climate in India is divided into rainy season (June ~ 65438+1October), dry season (March ~ May) and cool season (1 1 ~ February of the following year). In winter, due to the barrier of Himalayas, there is no cold current or cold high pressure going south to affect India.

India is the second most populous country in the world and one of the BRICS countries. Its economy and industry are diversified, including agriculture, handicrafts, textiles and even services.

Baidu Encyclopedia-India