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  2. Climate of the Alps - Wikipedia

    en.wikipedia.org/wiki/Climate_of_the_Alps

    The climate of the Alps is the climate, or average weather conditions over a long period of time, of the exact middle Alpine region of Europe. [ 1 ] [ 2 ] As air rises from sea level to the upper regions of the atmosphere the temperature decreases .

  3. Alpine climate - Wikipedia

    en.wikipedia.org/wiki/Alpine_climate

    a) the alpine climate, which occurs when the mean biotemperature of a location is between 1.5 and 3 °C (34.7 and 37.4 °F). The alpine climate in Holdridge system is roughly equivalent to the warmest tundra climates (ET) in the Köppen system.

  4. Rocky Mountains - Wikipedia

    en.wikipedia.org/wiki/Rocky_Mountains

    The Rockies vary in width from 110 to 480 kilometres (70 to 300 miles). The Rocky Mountains contain the highest peaks in central North America. The range's highest peak is Mount Elbert in Colorado at 4,401 metres (14,440 feet) above sea level. Mount Robson in British Columbia, at 3,954 m (12,972 ft), is the highest peak in the Canadian Rockies.

  5. Köppen climate classification - Wikipedia

    en.wikipedia.org/wiki/Köppen_climate_classification

    No significant precipitation difference between seasons (neither the abovementioned set of conditions fulfilled). Dfb = Warm-summer humid continental climate ; coldest month averaging below 0 °C (32 °F) (or −3 °C (26.6 °F)), all months with average temperatures below 22 °C (71.6 °F), and at least four months averaging above 10 °C (50 °F).

  6. Mountain range - Wikipedia

    en.wikipedia.org/wiki/Mountain_range

    A mountain range or hill range is a series of mountains or hills arranged in a line and connected by high ground. A mountain system or mountain belt is a group of mountain ranges with similarity in form, structure, and alignment that have arisen from the same cause, usually an orogeny . [ 1 ]

  7. Foehn wind - Wikipedia

    en.wikipedia.org/wiki/Foehn_wind

    The causes of the Foehn effect in the lee of mountains (adapted from: [1]) Dissolving Föhn clouds over Cumbre Nueva, La Palma, at an elevation of 1,400 m (4,600 ft) A Foehn, or Föhn (UK: / f ɜː n /, US: / f eɪ n / fayn, [2] [3] US also / f ʌ n, f ɜːr n / fu(r)n [4] [5]), is a type of dry, relatively warm downslope wind in the lee of a mountain range.

  8. What is graupel? How it is different from sleet or hail? - AOL

    www.aol.com/weather/difference-between-freezing...

    Unlike hail or sleet, graupel is soft and can be crushed easily in your hand, and is sometimes called "soft hail." It is also usually smaller than hail, with a diameter of around 0.08-0.2 inches.

  9. Alpine tundra - Wikipedia

    en.wikipedia.org/wiki/Alpine_tundra

    Alpine tundra occurs at high enough altitude at any latitude.Portions of montane grasslands and shrublands ecoregions worldwide include alpine tundra. Large regions of alpine tundra occur in the North American Cordillera and parts of the northern Appalachian Mountains in North America, the Alps and Pyrenees of Europe, the Himalaya and Karakoram of Asia, the Andes of South America, the Eastern ...