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3 years ago

WILL MARK BRAINLIEST IF CORRECT

2 answers:

7 0

Answer: 1. During the day, the land surface heats up faster than the water surface. Therefore, the air above the land is warmer than the air above the ocean. Now, recall that warmer air is lighter than cooler air. As a result, warm air rises. When the Sun heats up the Earth, the air above warms, becomes less dense, expands and rises. ... Because of this horizontal air movement there is less air above the ground where the heating took place and this leads to an area of low pressure. As the air rises, it cools. As it cools, the air becomes more dense and sinks. 2. Therefore, the air above the land is warmer than the air above the ocean. Now, recall that warmer air is lighter than cooler air. As a result, warm air rises. Therefore, the warmer air over the land surface is rising. 3. : Land and water heat up at different rates. ... Then the cooler air on top of surrounding water rushes in to replace the hot air. This imbalance in heating creates strong monsoon winds, which blow across much of the Indian subcontinent.

Explanation:

erastova [34]3 years ago

3 0

Answer:

During the day, the land surface heats up faster than the water surface. Therefore, the air above the land is warmer than the air above the ocean. Now, recall that warmer air is lighter than cooler air. As a result, warm air rises. When the Sun heats up the Earth, the air above warms, becomes less dense, expands and rises. ... Because of this horizontal air movement there is less air above the ground where the heating took place and this leads to an area of low pressure. As the air rises, it cools. As it cools, the air becomes more dense and sinks. 2. Therefore, the air above the land is warmer than the air above the ocean. Now, recall that warmer air is lighter than cooler air. As a result, warm air rises. Therefore, the warmer air over the land surface is rising. 3. : Land and water heat up at different rates. ... Then the cooler air on top of surrounding water rushes in to replace the hot air. This imbalance in heating creates strong monsoon winds, which blow across much of the Indian subcontinent.

Explanation:

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