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Orographic lift - Wikipedia, the free encyclopedia
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 expands and cools adiabatically, which ...
en.wikipedia.org/wiki/Orographic_lift
Martian orographic clouds exhibit similar characteristics. Orographic clouds form when the Martian atmosphere rises while flowing up the slopes and over mountains to begin the condensation process.
alpo-astronomy.org/mars/discrete.htm
Typical for such clouds is the elongated, smooth form. The Orographic clouds are often called almond clouds or lenticular clouds, and they move very little, in spite of a often very strong wind. In the upper picture we can see clouds formed on top of a air wave just over the top of Beerenberg.
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When air is confronted by a mountain, it is lifted up and over the mountain, cooling as it rises. If the air cools to its saturation point, the water vapor condenses and a cloud forms. ... These types of clouds are called "orographic clouds", which develop in response to lifting forced by the topography the earth.
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These types of clouds are called "orographic clouds", which develop in response to lifting forced by the topography the earth. ... [Image: lee mountain wave clouds (78K)]; Photograph by: Holle ... clouds, precipitation...
ww2010.atmos.uiuc.edu/(Gl)/guides/mtr/cld/dvlp/org.rxml
Parmenter-Holt could well be correct in some cases, for wave-like orographic clouds often form in the lee of mountain ranges, such as the Rockies. Some of the plumes, however, extend for 175 kilometers, as described above.
www.science-frontiers.com/sf053/sf053g13.htm
All articles related to How Clouds Form written by Suite101 experts - enter curious ... One of the reasons for mountain rainfall is orographic lift, or the orographic effect on precipitation. why it rains in mountains • orographic effect precipitation • orographic lift • how clouds form • mountains and cloud formation...
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[1991]) showed that the storm above the barrier was dominated by barrier level orographic clouds or propagating mesoscale cloud systems. The orographic cloud component consisted of weakly supercooled liquid water (-3 to -7 C) in the form of an extended barrier wide cap cloud.
www.agu.org/revgeophys/rasmus00/node20.html
We are comfortable with the idea that -- what we observe, as bright patches on Mars are in fact atmospheric clouds, fogs, and/or hazes. In the Earth's atmosphere clouds often form on the windward side of mountains and are classified as Orographic Clouds.
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