How do you breezes now from the different ocean to land during the day?

During the day, breezes typically flow from the ocean to the land due to differential heating. The land heats up faster than the water, causing the air above it to warm and rise, creating a low-pressure area. Meanwhile, the cooler, denser air over the ocean moves in to replace the rising warm air, resulting in a sea breeze. This process is driven by the temperature difference between the land and the ocean.