what is the relationship of the sea and land breeze to the temperature of an area?
Answers
the relationship of the sea and land breeze to the temperature of an area.
- A land breeze is a breeze that moves from land to sea.It is generally warmer.
- A sea breeze is a breeze that moves from sea to land they are generally cool.
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Answer:
The sea breeze is known as Virajon. Due to the difference in day and night temperatures, the surface heats up and cools cyclically. This causes the Earth's surface, when it is warmer than normal and does so before the ocean surface, to generate warm, rising air currents.
When warm air escapes because it is warmer than the ocean surface, it leaves a low pressure difference. The air rises higher and higher as it warms and the cooler air close to the surface of the ocean leaves a space with high pressure, which seeks to occupy the space left by the air. Therefore, the air mass with the highest pressure over the ocean moves over the low pressure area located near the land.
This causes air from the surface of the sea to enter the coast and is generally more pleasant in summer, but colder in winter, due to the cooling.
The movement of the sea happens at any time. It is only necessary for the surface temperature of the Sun to be warmer than the air around the surface of the ocean. On a day with less wind in general, there may be more sea breeze, because the Earth's surface is warmer.
The most pleasant winds to feel are created in spring and summer thanks to the fact that the sun warms the surface of the land more and the water is still cooler than in winter. Unless there is an increase in sea temperature due to the acceleration effect, ocean movement will be more continuous.
The air temperature generated by the sea breeze depends on the temperature contrast. The greater the difference between the temperatures of the two surfaces, the greater the wind speed, because there is more air that seeks to replace the lower pressure gap by the rise of warmer air.
The sea breeze blows vertically towards the coast and is capable of reaching 20 miles to the sea. Since a strong temperature contrast is required between the land and sea surfaces, the maximum strength of sea breeze is attained after noon, when the sun is most powerfully warm. Wind speed also depends on the orography of the terrain. Although they are generally mild and pleasant winds, if the orography is stable, the wind can reach up to 25 knots.
Sometimes, the convection that occurs above Earth's temperature and the strong moisture that the surrounding air brings from the ocean, create vertically growing clouds (called cumolnimbus) that can lead to conditions of atmospheric instability. There are great rainfall and strong lightning storms in short periods of time. This is the origin of some famous summer storms: those that, in just 20 minutes, leave behind a waterfall that can cause serious damage.