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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Anabatic wind

Anabatic winds can be detrimental to the maximum downhill speed of cyclists. Katabatic winds are downslope qnabatic created when the mountain surface is colder than the surrounding air and creates a down slope wind. Isobars on surface maps.

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.

Although the pressure-gradient forcing is at its maximum at the slope, surface friction causes the peak 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.

These winds are sometimes called Mountain Winds as they occur most frequently in mountainous areas, meteorologist call them Katabatic or Anabatic 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.

The air over the hill top is now warmer than the air at a similar altitude around it and will rise through convection.

Anabatic wind – AMS Glossary

As the air warms, its volume increases, and hence density and pressure decreases. Predominantly a day time phenomenon, anabatic wind may flow further than the orographic tops, cooling as it rises vertically convectiondry-adiabatically.

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Weather Facts: Katabatic winds |

Internet URLs are the best. Wind Atmospheric science stubs. When the mountainside is heated by the Sun the mountain breeze will break down, reverse and blowing upslope. This website uses cookies. At scales ranging from the slopes of individual hills and mountains to the slopes of mountain ranges and massifs, anabatic flows represent the daytime component of aktabatic wind systems.

This page was last edited on 5 Novemberat Local Surface winds are sometimes more a function of Temperature Differences between mountain tops and lower elevations than overriding Synoptic winds. Anabatic katabahicalso called upslope windlocal air current that blows up a hill or mountain slope facing the Sun. Glaze and Black Ice. Anabatic Winds are upslope winds driven by warmer katahatic temperatures jatabatic a mountain slope than the surrounding air column.

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. Retrieved from ” https: These winds typically occur during the daytime in calm sunny weather.

The rush of cold air down the slopes rapidly decreases the surrounding air temperature as it speeds down the topography to the valleys and planes below it. Banner Cloud – the peak’s flag. This page has been accessed 7, times. Mountain breezes are part of a local wind system.

The effect may be enhanced if the lower lying ground is shaded by the mountain and so receives less heat. Katabatic wind from the Greek: Volcano, vent in the crust of the Earth or another planet or satellite, from which katqbatic eruptions of…. Quantum mechanics, science dealing with the behaviour of matter and light on the atomic and subatomic…. Cold and usually dry katabatic winds, like the Boraresult from the downslope gravity flow of cold, dense air.


Examples for these descending, adiabatically warmed katabatic winds are the Foehn winds. More air rises from below to replace it, producing a wind. If you prefer to suggest your own revision of the article, you katabaitc go to edit mode requires login.

Keep Exploring Britannica Volcano. If the air is sufficiently unstable, cumulonimbus clouds may be produced, resulting in orographic thunderstorms. Why Skies are Ad. When the lower elevations are hot desert areas the temperature differences can be quite substantial on the order of 60 to 70 degrees F.

This column is warmer than the column at the wjnds levels over the valley or plain, resulting in hydrostatic low pressure over the slope relative to over the valley or plain.

Katabatic and Anabatic Winds

Most katabatic winds except the Foehn are more or less the result of air in contact with upper level ground is cooled by radiation, increases in density, and flows downhill and along the valley bottom. The mechanism of the anabatic wind can be described as follows. These winds are known as valley wind or anabatic wind. Jan 28, Wind Measurement. Thank you for your feedback. These can then produce rain or even thunderstorms. There was a problem with your submission.

A hill or mountain top will be radiatively warmed by the Sun which in turn heats the air just above ,atabatic. Unfortunately, our editorial approach may not be able to accommodate all contributions.

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