Sea breeze absorbs heat faster during the daytime because the land heats up more quickly than the ocean due to differences in specific heat capacity. As a result, the air above the land rises and cooler air from the sea moves in to replace it, creating a sea breeze.
The usual cause of sea breeze is the difference in specific heat capacity between land and water Land heats and cools more quickly than water.
A sea breeze is a wind that blows from the sea towards the land.
When a sea breeze moving north meets a sea breeze moving south, they converge to form a squall line. This can result in thunderstorms and heavy rainfall along the boundary where the two air masses meet.
a sea breeze
Sea breeze absorbs heat faster during the daytime because the land heats up more quickly than the ocean due to differences in specific heat capacity. As a result, the air above the land rises and cooler air from the sea moves in to replace it, creating a sea breeze.
The usual cause of sea breeze is the difference in specific heat capacity between land and water Land heats and cools more quickly than water.
Two forms of heat transfer help create a sea breeze are conduction and convection. Another form of heat transfer help create a sea breeze is radiation.
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The two forms of heat transfer that help create a sea breeze are convection and radiation. During the day, the land heats up more quickly than the sea due to differences in specific heat capacities. This causes the air above the land to rise, creating a low-pressure area. The cooler air from the sea moves in to replace it, creating the sea breeze.
convection
Sea breeze is a type of convection, which involves the transfer of heat through the movement of air. During the day, the land heats up more quickly than the sea, causing the air above the land to rise and cooler air from over the sea to move in, creating the sea breeze.
The high latent heat of water.
A sea breeze blows from sea to land, typically during the day when the land heats up more quickly than the sea. This creates a pressure difference that causes the cool air over the sea to move towards the warmer land.
convection and conduction only
The forms of heat transfer that help create a sea breeze are conduction and convection. During the day, the land heats up faster than the sea, causing air to rise over the land (convection) and cooler air from the sea to move in (conduction) to replace it, resulting in a sea breeze.
The usual cause of sea breeze is the difference in specific heat capacity between land and water Land heats and cools more quickly than water.