The monsoon climate in eastern China is very remarkable.

The main reason is the difference of thermal properties between land and sea. China is adjacent to the world's largest ocean in the east and the world's largest continent in the west. The thermal properties of land and sea are quite different. There is a great difference in air pressure between the two seasons in Xia Dong, resulting in a remarkable monsoon climate. The secondary reason is the difference in latitude and geographical location.

The cause of the remarkable monsoon climate.

China is located in the southeast of Asia-Europe continent, the largest continent on earth, and is adjacent to the Pacific Ocean, the largest ocean on earth in the east. Due to the great difference between land and sea, the northern part of the Asian continent becomes a gathering place of cold air in winter, with high air pressure, and cold air diverges from the central area of high pressure to the surrounding areas; In summer, the land temperature rises rapidly and the air pressure is low, while the ocean air pressure is relatively high, and the warm and humid airflow blows from the ocean to the mainland.

The climate of China.

Influenced by latitude position and land and sea position, the prevailing wind direction in most parts of China changes significantly with the seasons within one year, forming a typical monsoon climate. The cold wind and dry cooling in winter is one of the main reasons for the large temperature difference between north and south in winter in China. The summer monsoon is warm and humid, forming the rainy season in China. In addition to the Qinghai-Tibet Plateau, China is customarily divided into monsoon region and non-monsoon region with Daxinganling-Yinshan-Helan Mountain as the boundary. The climate types in China mainly include tropical monsoon climate, subtropical monsoon climate, temperate monsoon climate, temperate continental climate and plateau mountain climate.