Foehn wind (Foehn wind) refers to the air flow through the mountains, along the windward slope of the cooling, in the water vapor before the saturation of the process by the dry adiabatic cooling, saturated, according to the wet insulation straight reduction rate, and due to precipitation While reducing moisture. After the mountain air down the leeward slope, according to the dry adiabatic straight rate of warming, so the air temperature after the mountain than the height of the mountain with the temperature is much higher, the humidity is also significantly reduced.
Land and sea wind is due to the ocean and the land is not uniform and formed in the vicinity of the coast of a change in the wind. When the base air is weak, the daytime wind blows from the sea to the land, and the night wind blows from the land to the ocean. The former known as the sea breeze, which is called land breeze, collectively known as sea and land wind.
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