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  2. Alpine climate - Wikipedia

    en.wikipedia.org/wiki/Alpine_climate

    Alpine climate is the typical climate for elevations above the tree line, where trees fail to grow due to cold. This climate is also referred to as a mountain climate or highland climate . Definition

  3. Köppen climate classification - Wikipedia

    en.wikipedia.org/wiki/Köppen_climate_classification

    Polar and alpine climates has every month of the year with an average temperature below 10 °C (50 °F). [9] [11] ET = Tundra climate; average temperature of warmest month between 0 °C (32 °F) and 10 °C (50 °F). [9] [11] EF = Ice cap climate; eternal winter, with all 12 months of the year with average temperatures below 0 °C (32 °F). [9] [11]

  4. List of alpine climate locations - Wikipedia

    en.wikipedia.org/wiki/List_of_alpine_climate...

    A number of locations around the Earth have alpine climate. The climate of some of these locations is described, below. The climate of some of these locations is described, below. For tropical oceanic locations, such as the summit of Mauna Loa , elev. 13,679 ft (4,169 m), the temperature is roughly constant throughout the year:

  5. Sol-air temperature - Wikipedia

    en.wikipedia.org/wiki/Sol-air_temperature

    Sol-air temperature (T sol-air) is a variable used to calculate cooling load of a building and determine the total heat gain through exterior surfaces. It is an improvement over: It is an improvement over:

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  7. Air changes per hour - Wikipedia

    en.wikipedia.org/wiki/Air_changes_per_hour

    Air changes per hour, abbreviated ACPH or ACH, or air change rate is the number of times that the total air volume in a room or space is completely removed and replaced in an hour. If the air in the space is either uniform or perfectly mixed, air changes per hour is a measure of how many times the air within a defined space is replaced each hour.

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  9. Tree line - Wikipedia

    en.wikipedia.org/wiki/Tree_line

    The decrease in air temperature with increasing elevation creates the alpine climate. The rate of decrease can vary in different mountain chains, from 3.5 °F (1.9 °C) per 1,000 feet (300 m) of elevation gain in the dry mountains of the western United States, [ 17 ] to 1.4 °F (0.78 °C) per 1,000 feet (300 m) in the moister mountains of the ...

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