Land and sea breezes on a continental scale are called

The phenomenon where there is a regular pattern of wind blowing from the sea towards the land during the day, and from the land towards the sea during the night on a large scale (continent-scale) is known as "monsoons". During the day, the land heats up faster than the sea, causing the air above the land to rise and cooler air from the sea to move in, resulting in a sea breeze. At night, the land cools down faster than the sea, causing the air above the sea to rise and cooler air from the land to move in, resulting in a land breeze. This phenomenon is particularly prominent in the Indian subcontinent and Southeast Asia, where it causes significant seasonal changes in temperature, humidity, and precipitation. In the summer, the warm, moist air from the Indian Ocean is drawn towards the land, resulting in heavy rainfall and flooding in some regions. In the winter, the cooler, drier air from the land moves towards the Indian Ocean, resulting in dry and clear weather. In conclusion, the phenomenon of regular land and sea breezes on a continental scale is known as "monsoons". Typhoons, fohn, and chinook are different weather-related phenomena that are not related to monsoons.