Anabatic Winds are upslope winds driven by warmer surface temperatures on a mountain slope than the surrounding air column. Katabatic. Katabatic wind · Local wind system. Anabatic wind, also called upslope wind, local air current that blows up a hill or mountain slope facing the Sun. During the . Katabatic wind (from the Greek: katabaino – to go down) is the generic term for downslope winds These winds are known as valley wind or anabatic wind.

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Katabatic wind may range over fairly large areas as in the case of the Santa Anna winds experienced throughout southern California during certain times of the year.

Because heating at the surface promotes deeper mixing than cooling does, the heated layer, often occurring as a convective or mixed layeris generally deeper than a cooled or katabatic layer.

Retrieved from ” http: Sometimes a bit fishy. Many strong katabatic winds are ajabatic triggered or are activated by large scale weather features such as a high pressure system over high elevations, as in Greenland, in California or, for example, the fjords of Norway.

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During the day, the Sun heats such a slope and the air over it faster than it does the adjacent atmosphere over a valley or a plain at the same altitude. What does it mean?

Katabatic winds

These winds are sometimes called Mountain Winds as they occur most frequently in mountainous areas, meteorologist call them Katabatic or Anabatic Winds. Anabatic winds vary in intensity and occurrance; in general anabatic winds are more pronounced in the summer season when the sun’s heating is more intense, and its velocity ranges from 10 to 30 knots.


Examples for these descending, adiabatically warmed katabatic winds are the Foehn winds. Once generated, however, there are many small scale surface structures that can modify the wind direction and speed and distort the accuracy of the observing instrumentation.

Speeds in the mountain—valley anabatic flow layer are often 3—5 m s This page has been accessed 7, times. From Wikipedia, the free encyclopedia.

Anabatic wind – AMS Glossary

Any text you add should be original, not copied from other sources. Warm, dry katabatic winds occur on the lee side of a mountain range situated in the path of a depression. However, katabatic winds might also reach gale force as an outblowing wind over ice-covered surfaces in Antarctica and Greenland, where the wind may be extremely strong and gusty near the coasts and less severe in mountain regions.

These types of winds can reach velocities of up to 4 meters per second. The air becomes relatively bouyant and rises up the orographic slope orographic liftresulting in the anabatic flow or wind. When the mountainside is heated by the Sun the mountain breeze will break down, reverse and blowing upslope. 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.

Katabatic and Anabatic Winds

In general usage, this term does not suffer from the multiplicity of meanings that katabatic wind does. We call these wind modifiers and will talk about them in future blogs. Clouds – sentry of the sky. You may find it helpful to search within the site to see how similar or related subjects are covered. Description Anabatic winds are mainly created by ultraviolet solar radiation heating up the lower regions of an orographic area i.


Anabatic wind Written Jatabatic Slopes occur on many scales, and consequently anabatic flows also occur on many scales. Wind Atmospheric science stubs. Glaze and Black Ice. As the air warms, its volume increases, and hence density and pressure decreases.

Retrieved from ” https: 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. Isobars on surface maps.

Our editors will review what you’ve submitted, and if it meets our criteria, wijds add it to the article. The horizontal pressure gradientmaximized at the slope surface, drives an acceleration directed toward the slope, or up the slope.

What Causes Surface Winds, Mountain Winds and Anabatic Winds – Belfort Instrument

North Atlantic Drift Gulf Stream. Help us improve this article! The gentler katabatic flows of hill slopes produce frost hollows. This page was last modified on 20 Februaryat Volcano, vent in the crust of the Earth or another planet or satellite, from which issue eruptions of….

This page was last edited on 5 Novemberat Discovery of the Jet Stream.