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These can then produce rain or even thunderstorms.[2]. References[edit]. It is common for the air rising from the tops of large mountains to reach a height where it cools adiabatically to below its dew point and forms cumulus clouds. Air at a similar altitude over an adjacent valley or plain does not get warmed so much because of the greater distance to the ground below it. You can help Wikipedia by expanding it. Cookies We use cookies to improve your experience with our site. More information Accept . Over 10 million scientific documents at your fingertips Home Impressum Legal Information Contact Us 2016 Springer International Publishing. Search .

If the problem continues, please let us know. .. An anabatic wind, from the Greek anabatos, verbal of anabainein meaning moving upward, is a warm wind which blows up a steep slope or mountain side, driven by heating of the slope through insolation.[1][2] It is also known as an upslope flow. Mountain breeze and valley breeze . Anabatic winds can be detrimental to the maximum downhill speed of cyclists. Part of Springer Nature.. ^ Marine Meteorological Glossary ^ a b American Meteorology Society Glossary . Anabatic winds are particularly useful to soaring glider pilots who can use them to increase the aircraft's altitude.

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