Influence of Asian low pressure on climate

In summer, a thermal low pressure center appeared in the Asian continent, which cut off the subtropical high pressure zone, and the subtropical high pressure zone remained in the ocean, and changed from a zonal distribution to a high pressure center.

due to the influence of the Asian depression (also known as the Indian depression), the wind blows from the ocean to the land, and the southeast monsoon prevails in summer in China, resulting in typhoons, strong winds and heavy rains along the southeast coast.

The humid air flow brought by the southeast monsoon from the sea began to land in China at the end of April, reached the middle and lower reaches of the Yangtze River in May and June, reached North China in July and August, and reached Northeast China in September. In October, the Asian high began to appear, and the rain belt quickly withdrew southward. Where the moist airflow (or rain belt) brought by the southeast monsoon from the sea stops, there will be heavy rain, but once it leaves this place, it will be dry after a long time. This has caused the instability of monsoon in China, and the change of precipitation season has led to the flood disaster in China.

there is no Asian low in winter, only the Asian high (also known as the Mongolian high). As a result, the northwest monsoon prevails in China. Because the wind blows from land to sea and the airflow is dry, there is a general lack of precipitation in China, and most areas are dry and have little precipitation.

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