The cool air current and the upper air current are drawn correctly
What is the land breeze?
The land breeze emerges as the land cools faster than the surrounding water, generating a distinct wind pattern. This phenomenon arises from temperature discrepancies that drive the convection process, prompting air movement.
In daylight hours, the land's rapid heating surpasses that of the nearby water. Consequently, warmer air ascends above the land, creating a vacuum filled by cooler air from the water—an airflow known as the sea breeze.