Katabatic winds develop at night when there are clear skies, a general slack Anabatic winds occur in the Alps in summer months when there is generally a. Anabatic wind. related topics. Katabatic wind · Local wind system. Anabatic wind, also called upslope wind, local air current that blows up a hill or mountain. Katabatic is a local wind caused (often at night) by the flow of air, cooled by radiation, down mountain slopes and valleys. It is also caused by.

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The impact mountains have on rainfall is one of the most significant.

If the air is sufficiently unstable, cumulonimbus clouds may be produced, resulting in orographic thunderstorms. Anabatic winds are mainly created by ultraviolet solar radiation heating up the katabaic regions of an orographic area i. Let’s start with the basic physics. Get updates Email alerts RSS. Average rainfall over England and Wales. We think of mountains as cold, often snow-covered, environments – but why are they like this and do we ever anabatoc exceptions? When the lower elevations are hot desert areas the temperature differences can be quite substantial on the order of 60 to 70 degrees F.

More air rises from below to replace it, producing a wind. We’ve brought you back to the current site. Conversely, Katabatic winds are down-slope winds, frequently produced at night by the opposite effect, the air near to the ground losing heat to it faster than air at a similar altitude over adjacent low-lying land.

It can also mean clouds form and are trapped at lower levels. The Editors of Encyclopaedia Britannica. Comments Membership info Katabqtic new Login. Related pages Met Office mountain widget Factsheets If you are interested in clouds or thunderstorms, UK climate or weather extremes, this series of factsheets clearly describes and illustrates the processes involved. kztabatic


Katabatic flows slumping down from uplands or mountains may be funneled and strengthened by the landscape and are then known as mountain gap wind such as the Santa Anamountain breeze or drainage wind. In general usage, this term does not suffer from the multiplicity of meanings that katabatic wind does.

We welcome suggested improvements to any of our articles. 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. Anabatic windalso called upslope windlocal air current that blows up a hill or mountain slope facing the Sun.

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What Causes Surface Winds, Mountain Winds and Anabatic Winds

Monsoon winds are similarly generated, but on a continental scale and seasonal cycle. Due to the interaction between gravity, pressure and temperature when the air is mixed in the vertical, you normally expect the atmosphere to get colder as you ascend – this is called the adiabatic lapse rate of temperature with height. As shown in figure 2. Temperature, wind and rainfall are all heavily influenced by these geographical wonders, to the extent that mountain ranges can impact the climate of vast areas.

These types of winds can reach velocities of up to 4 meters per second. Gravity sees that cold air accelerate down the mountain to the point where, in extreme places like Antarctica, these winds can reach hurricane force. Internet URLs are the best. Katabatic wind may range over fairly large areas as in the case of the Santa Anna winds experienced anabattic southern California during certain times of the year.

In mountain meteorology, an upslope wind driven by heating usually daytime insolation at the slope surface under fair-weather conditions. The warm surface heats a vertical column of the atmosphere starting at the slope surface and reaching up to a few hundred meters deep.

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The adiabatic lapse is easy to remember in dry air: There was a problem with your submission. Key to our weather symbols.

Weather Facts: Katabatic winds |

In North America, east of the Rockies, the Chinook wind is a powerful example of the Foehn phenomenon, known katabatkc its ability to “eat snow”.

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. At scales ranging from the slopes of individual hills and mountains to the slopes of anabxtic ranges and massifs, anabatic flows represent the daytime component of mountain—plains wind systems. Clearly this pleasant inversion scenario doesn’t happen all that often, so it’s safer to expect conditions to be colder up the mountain than down.

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When the mountainside is heated by the Sun the mountain breeze will katabayic down, reverse and blowing upslope. Banner Cloud – the peak’s flag. That said, you can expect that most of the time you will see a significant fall in temperature as you ascend – particularly when you include the impacts of more wind exposure increasing wind chill. Snow forms when tiny ice crystals in clouds stick together to become snowflakes. Polar low – the arctic hurricane. As the lowest layers of the air over the sunny slopes are warmed by the land, a current is set up which flows up the mountain.

As the same air crests a mountain peak, it descends potentially much drier because much of the moisture has already been rained or snowed out.