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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This effect is enhanced during winter over snow covered surfaces and after dry, clear nights. As the air sinds, its volume increases, and hence density and pressure decreases. These winds typically occur during the daytime in calm sunny weather.

Internet URLs are the best. Help us improve this article! These can then produce rain or even thunderstorms. If the air is cooled sufficiently to reach the air’s dewpoint temperature, the saturated air may condense its water vapour content, resulting in mainly convective clouds.

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.

The air becomes relatively bouyant and rises up the orographic slope orographic liftresulting in the anabatic flow or wind. Sometimes a bit fishy.


From Wikipedia, the free encyclopedia. This warming decreases the density of the air, causing it to rise.

What Causes Surface Winds, Mountain Winds and Anabatic Winds

Although the pressure-gradient forcing is at its maximum at the slope, surface friction causes the kahabatic in the anabatic wind speeds to occur above the surface, often by several tens of meters; if the surface heating is strong, however, the momentum will tend to be vertically mixed. Keep Exploring Britannica Volcano.

North Atlantic Drift Gulf Stream. Winds can be derived from a number of different meteorological phenomena that are either caused by large scale synoptic pressure and temperature differences or by local temperature and pressure differences.

Local Surface winds are sometimes more a function of Temperature Differences between mountain tops and lower anavatic than overriding Synoptic winds.

Wind Atmospheric science stubs. When the mountainside is heated by the Sun the mountain breeze will break down, reverse and blowing upslope. Aurorae – Northern Lights.

Anabatic Wind – SKYbrary Aviation Safety

Your contribution may be further edited by our staff, and its publication is subject to our final approval. This column is warmer than the column at the same levels over the valley or plain, resulting in hydrostatic low pressure over the slope relative to over the valley or plain. Due to its limited heat capacity, the surface heats the air immediately above it by conduction. 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.


Retrieved from ” https: Discovery of the Jet Stream. As shown in figure 2. If you prefer to suggest your katabatc revision of the article, you can go to edit mode requires login.

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

In mountain meteorology, an upslope wind driven by heating usually daytime insolation at the slope surface under fair-weather conditions. At local scales anabatic winds are an along-slope component of mountain—valley wind systems. You may find it helpful to search within the site to see how similar or related subjects are covered. You can katabatc it easier for us to review and, hopefully, publish your contribution by keeping a few points in mind. An anabatic wind often attains a velocity of 3—5 metres per second 7—11 miles per hour.

Weather Facts A is for Air. We call these wind modifiers and will talk about them in future blogs.

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