Question

Бриз днём дует с моря на сушу, потому что атмосферное давление над сушей ...

Answer 1

Воздушные массы движутся из области высокого давления в область низкого давления, чем больше разница, тем сильнее ветер. Днем высокое давление над морем, а над сушей низкое и ветер дует с моря, ночью наоборот. Давление над сушей поднимается и ветер дует с суши.

Answer 2

Why does the sea breeze blow towards the land during the day?

The sea breeze is a phenomenon where wind blows from the sea towards the land during the day. This occurs due to the difference in temperature between the land and the sea. Here's a detailed explanation:

During the day, the land heats up faster than the sea because land has a lower heat capacity than water. As a result, the air above the land becomes warmer than the air above the sea. Warmer air is less dense and tends to rise, creating a region of low pressure over the land. At the same time, the air above the sea remains relatively cooler and denser, creating a region of high pressure over the sea.

Air flows from areas of high pressure to areas of low pressure, so the air from the sea moves towards the land to equalize the pressure difference. This movement of air from the sea towards the land is known as the sea breeze. The sea breeze is typically strongest during the afternoon when the temperature difference between the land and the sea is greatest.

It's important to note that the sea breeze is a local wind pattern and is influenced by various factors such as the geography of the area, the temperature difference between the land and the sea, and the prevailing weather conditions. These factors can affect the strength and timing of the sea breeze.

Conclusion

The sea breeze blows towards the land during the day because of the temperature difference between the land and the sea. The land heats up faster, creating a region of low pressure over the land, while the sea remains relatively cooler, creating a region of high pressure over the sea. Air flows from the high-pressure area over the sea to the low-pressure area over the land, resulting in the sea breeze phenomenon.