Blowing air is a system of cold air that is cooled by touching the ice, falling to the edge, and then dying within a short distance. Often light, the gentle breezes of the mountains may provide a breeze on the rough seas leading to the narrow river that has resulted in the cooling of many valleys. The nocturnal rays cool the slopes, causing cool, dense air to enter the valley (mountain air). Rising tides sometimes cause thunderstorms in the mountains. Similarly, the air flowing into the valley is produced by the rapid warming of the lower valley which causes the air to expand and flow up and down the slopes. Because of the high temperatures during the day, the sea breeze is strong sometimes it lowers temperatures by 8 ° C (15 ° F) or higher near the coastline and significantly changes the local climate.

As a result, cooler, cooler air usually flows from water to land (air flowing from the sea or lake) during the day, and from land to water (fresh air) at night.

The underground areas are warmer and cooler than the wetlands. They may be reinforced or blocked by the pressure of passing systems. These winds are very strong in warm, clear, dry weather, where daylight, or sunlight, is most intense. Breeze also refers to a variety of local winds (e.g., sea breeze, breeze, valley breeze, mountain breeze) produced by uneven diurnal temperatures and cooling of near-earth temperatures. Fresh air, air space on the Beaufort scale weaker than a storm.

Define valley breeze