katabatic wind - Axtarish в Google
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Катабатический ветер Катабатический ветер
Катабатический ветер, также падающий — плотный и холодный воздушный поток, направленный вниз по склонам земной поверхности, а также нисходящие струи холодного воздуха в кучево-дождевых облаках. Не все ветры, дующие вниз по склону, являются... Википедия
A katabatic wind carries high-density air from a higher elevation down a slope under the force of gravity. Such winds are sometimes also called fall winds; ... Foehn wind · Bora (wind) · Anabatic wind · Makhtesh Ramon
10 окт. 2024 г. · Katabatic wind, wind that blows down a slope because of gravity. It occurs at night, when the highlands radiate heat and are cooled.
As air cools it becomes denser and therefore heavier. The cold air then flows down the side of the mountain, resulting in a katabatic flow (or wind). Fig. 1 is ...
9 нояб. 2015 г. · Also known as fall winds, katabatic winds are usually caused by gravity pulling higher density air downslope to lower density air.
The air flow gets stronger, turning into fast-flowing winds called katabatic winds. These katabatic winds roar toward the coast of Antarctica. Fairly quiet ...
A katabatic wind is a dense and cold air current directed downward from mountain peaks, as well as downdrafts of cold air in.
26 мар. 2024 г. · A downslope flow driven by cooling at the slope surface during periods of light larger-scale winds; the nocturnal component of the along-slope wind systems.
29 мая 2024 г. · A katabatic wind is created by the same rush of colder, heavier air but this time the cold air is tumbling off something high, like a mountain ...
Katabatic wind (from the Greek: katabaino - to go down) is the generic term for downslope winds flowing from high elevations of mountains, plateaus, and.
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