Question

explain land breeze and sea breeze with diagram

Answer 1

Answer:

• The procedure is repeated throughout the day. The sun heats both the sea and the land's surface. Because the sea has a far higher heat capacity than the land, it heats up more slowly. As a result, the temperature above the ground surface rises, warming the surrounding air. Expansion happens in the less dense warm air, resulting in the formation of a low-pressure zone over the continent. A high-pressure area forms on the sea's surface at the same moment. The air flows from the high pressure over the sea to the low pressure over the land because to the pressure difference. This flow of air from the sea to the land is termed as the sea breeze.
  
  
• This process continues throughout the night, and then the above-mentioned process is reversed. When the sun sets, both the land and the sea begin to cool. Because the land has a lower heat capacity than the water, it cools off faster. As a result of the higher temperature above the water compared to the land, a low-pressure condition develops over the sea. As a result, air rushes from the land to the sea, resulting in the land breeze.
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Answer 2

Answer:

• A breeze is a cool, gentle wind that feels pleasant.
• There are two kinds of breezes. One is referred to as a sea breeze, while the other is referred to as a land breeze.
• Both land wind and sea breeze occur around huge bodies of water.
• The sun is responsible for both the land and the water's heating.
• The heating is not consistent, and neither the land nor the water heats or cools in the same way.
• Breezes are created when the land and the sea are heated and cooled differently.

Land Breeze

• The movement of wind from land to water represents the land breeze.
•  During the night and early morning, when the temperature of the land falls below that of nearby water bodies, a land breeze occurs.
• During the last few weeks of summer, the warmth of the water raises the daily temperature of the land. This prolongs the duration of land breezes.
• Due to the lack of sunlight, the terrain swiftly cools off at night.
• Water bodies have a significant heat-retention capability when compared to land.
• As a result, the air above the water has a low density and rises over it, resulting in low pressure over the water.
• On the other hand, high pressure is created on the land.
• The denser air from the ground rises to the space above the water.
• Wind moves from high-pressure to low-pressure zones.

Sea Breeze

• The flow of wind from the sea to the land is referred to as sea breeze.
• During the spring and summer, these winds may be felt.
• This is because the temperature difference between land and ocean is greater.
• Sea breeze happens when the land achieves its maximum heat level in the afternoon.
• During the winter, sea breezes are more reliable due to the large temperature differential between the sea and the land.
• Thunderstorms form, as a result, bringing rain.
• During the day, the ground quickly heats up, and the air above it warms up faster than the air over the ocean.
• Warmer air rises and becomes less dense as it passes over land. Over land, a low-pressure region has developed.
• The denser air from the water rises into the atmosphere above the ground. As a result, there is a sea breeze.

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