Causes of the formation of Asian low and Pacific high in the northern hemisphere in summer

Difference of thermal characteristics between land and sea

Seasonal movement of pressure zone and wind zone.

Asian low: This is just the opposite of the formation of Asian high. Due to the high land temperature in summer, the airflow rises, forming a low pressure center, that is, the Asian low pressure.

Asian high: generally formed in winter, because the temperature drops in winter, and the specific heat capacity of ocean and land is different, which leads to the low temperature of land, thus forming a high pressure center. Asian high school.