In a sea breeze scenario, what occurs to thermal energy at higher altitudes?

In a sea breeze scenario, the correct answer highlights the process of thermal energy transfer. When the sun heats the land during the day, the air above it also warms up. This warm air is less dense and tends to rise. As it ascends, it creates a low-pressure area over the land. To balance this low pressure, cooler air from over the sea moves in, creating the sea breeze. The transfer of thermal energy occurs as this warm air moves upwards and creates convective currents, while the cooler air flows in to replace it.

This process exemplifies convection, as warm air rises and cooler air descends, causing thermal energy to be redistributed in the atmosphere. Understanding this convection cycle is crucial because it illustrates the fundamental principles of how temperature differences drive wind patterns and weather phenomena, including the formation of sea breezes. The other choices do not accurately capture the dynamics occurring in this scenario.