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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What does it mean?
We call these wind modifiers and will talk about them in future blogs. The greater the temperature difference the stronger the wind.
The air becomes relatively bouyant and rises up the orographic slope orographic liftresulting iatabatic the anabatic flow or wind. Retrieved from ” https: You can make it easier for us to review and, hopefully, publish your contribution by keeping a few points in mind. Please note that our editors may make some formatting changes or correct spelling or grammatical errors, and may also contact you if any clarifications are needed.
From Wikipedia, the free encyclopedia. Local Surface winds are sometimes more a function of Temperature Differences between mountain tops and lower elevations than overriding Synoptic adn. 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. An anabatic windfrom the Greek anabatosverbal of anabainein meaning winrs upward, is a warm wind which blows up a steep slope or mountain side, driven by heating of the slope through insolation.
Key to our weather symbols. Weather Facts A anabaic for Air. The rush of wnd air down the slopes rapidly decreases the surrounding air temperature as it speeds down the topography to the valleys and planes below it. As the air warms, its volume increases, and hence density and pressure decreases.
Drifting snow – blowing snow. Katabatic winds are downslope winds created when the mountain surface is colder than the surrounding air and creates a down slope wind.
Webarchive template wayback links All stub articles. Slopes occur on many scales, and consequently anabatic flows also occur on many scales. Winds can be derived nad 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. You may find it helpful to search within the site to see how similar or related subjects are covered.
Anabatic wind – AMS Glossary
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Speeds in the mountain—valley anabatic flow layer are often 3—5 m s The mechanism of the anabatic wind can be described as follows. The warm surface heats a vertical column of the atmosphere starting at the slope surface and reaching up to a few hundred meters deep. 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.
Weather Facts: Katabatic winds |
Isobars on surface maps. At the bottom of the article, feel free to list any sources that support your changes, so that we can fully understand their context. If you prefer to suggest your own revision of the article, you can go to edit mode requires login. Air masses and their sources.
Thank you for your feedback. Retrieved from ” https: Views Read Edit View history. North Atlantic Drift Gulf Stream. In mountain meteorology, an upslope wind driven by heating usually daytime insolation at the slope surface under fair-weather conditions.
Warm, dry katabatic winds occur on the lee side of a mountain range situated in the path of a depression.