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Evaporation of Damp Air on Mountain Ridges (Stock Footage)

Evaporation of Damp Air on Mountain Ridges (Stock Footage)

Alpine weather is referred to as a mountain highland climate. The temperature profile of the atmosphere is a result of an interaction between radiation and convection. Sunlight in the visible spectrum hits the ground and heats it. Vapor contains latent heat of vaporization. As air rises and cools, it eventually becomes saturated and cannot hold its quantity. Fog is a aerosol consisting of tiny water droplets or ice crystals suspended the Earth’s surface. Collision of damp and dry mass. Foggy can be considered a type of low-lying cloud, usually resembling stratus, and is heavily influenced by nearby bodies topography and wind conditions. Haze mist mistiness mountainous hot cold heavy evaporation breeze wind flow mix mixed peak summit sweating light weight high altitude. Air masses on two different slopes of the mountain ridge. Condensation. 4K 3840×2160.

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