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  2. Orographic lift - Wikipedia

    en.wikipedia.org/wiki/Orographic_lift

    As air flows over mountain barriers, orographic lift can create a variety of cloud effects. Orographic fog is formed as the air rises up the slope and will often envelope the summit. When the air is humid, some of the moisture will fall on the windward slope and on the summit of the mountain.

  3. Precipitation types - Wikipedia

    en.wikipedia.org/wiki/Precipitation_types

    Orographic or relief rainfall is caused when masses of air are forced up the side of elevated land formations, such as large mountains or plateaus (often referred to as an upslope effect). The lift of the air up the side of the mountain results in adiabatic cooling with altitude, and ultimately condensation and precipitation.

  4. Orography - Wikipedia

    en.wikipedia.org/wiki/Orography

    An orographic map of Eastern Siberia from 1875 by Peter Kropotkin. Orography is the study of the topographic relief of mountains, [1] and can more broadly include hills, and any part of a region's elevated terrain. [2] Orography (also known as oreography, orology, or oreology) falls within the broader discipline of geomorphology. [3]

  5. Tectonic–climatic interaction - Wikipedia

    en.wikipedia.org/wiki/Tectonic–climatic...

    Tectonic–climatic interaction is the interrelationship between tectonic processes and the climate system. The tectonic processes in question include orogenesis, volcanism, and erosion, while relevant climatic processes include atmospheric circulation, orographic lift, monsoon circulation and the rain shadow effect.

  6. Precipitation - Wikipedia

    en.wikipedia.org/wiki/Precipitation

    Orographic effects. Orographic precipitation. Orographic precipitation ... All precipitation types are made up of hydrometeors by definition, ...

  7. Desert - Wikipedia

    en.wikipedia.org/wiki/Desert

    Orographic lift occurs as air masses rise to pass over high ground. In the process they cool and lose much of their moisture by precipitation on the windward slope of the mountain range . When they descend on the leeward side, they warm and their capacity to hold moisture increases so an area with relatively little precipitation occurs. [ 37 ]

  8. Rain shadow - Wikipedia

    en.wikipedia.org/wiki/Rain_shadow

    Effect of a rain shadow The Tibetan Plateau (center), perhaps the best example of a rain shadow. Rainfalls from the southern South Asian monsoon do not make it far past the Himalayas (seen by the snow line at the bottom), leading to an arid climate on the leeward (north) side of the mountain range and the desertification of the Tarim Basin (top).

  9. Land surface effects on climate - Wikipedia

    en.wikipedia.org/wiki/Land_surface_effects_on...

    Orographic lift occurs when an air mass is forced from a low elevation to a higher elevation as it moves over rising terrain. As the air mass gains altitude it quickly cools down adiabatically , which can raise the relative humidity to 100% and create clouds and, under the right conditions, precipitation .