convection
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 land breeze is a type of wind that blows from the land to the ocean.A sen breeze blowing toward the land from the sea, esp. during the day owing to the relative warmth of the land.
A sea breeze blows from the ocean to the land. Land heats more rapidly than water, resulting in lower pressure and rising air over land, which causes air to move from the ocean to land.
Land breezes occur during the night when the land looses heat and the ocean or body of water is warmer. The warm water air becomes less dense and rises (low pressure) while the air above land is cold so it sinks (high pressure) since air travels from high pressure to low pressure, the high pressure from land goes to the water mass. Winds are named for the origin, so it is called a land breeze.
convection
Convection & Conduction
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.
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 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.
At night, the land looses heat faster than water does. Cooler air from the land moves toward the water, causing a land breeze.
The only difference - is the direction of flow. A sea breeze blows from the sea onto the land. A land breeze flows in the opposite direction.
The sun
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.
The land breeze causes the air to move counterclockwise
The beach lies at the interface of the ocean and the land. These two bodies heat and cool at very different rates, and this unequal heating/cooling of the air causes the local coastal winds. As distinct from the meteorological winds, which are caused by upper atmosphere conditions. This is called the transmission of heat (Convection currents produced by sea breeze and land breeze). Sea and land breezes On a hot day, the land heats up faster than the sea. Hot air over the land rises. This hot air is replaced by cold, denser air from the sea. This produces a breeze from the sea to the land. The breeze is called a sea breeze. At night, the land cools quicker than the sea. The hot air over the sea rises. Cold air from the land replaces the hot air. This produces a land 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.