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Knowing the wind sampling average is important, as the value of a one-minute sustained wind is typically 14% greater than a ten-minute sustained wind. [16] A short burst of high speed wind is termed a wind gust ; one technical definition of a wind gust is: the maxima that exceed the lowest wind speed measured during a ten-minute time interval ...
WW2D uses images from WorldWind's servers. WW2D Plus One - an update to WW2D providing a 3D view. Punt was a fork of the .NET NASA WorldWind project, and was started by two members of the free software community who had made contributions to WorldWind.
Buran (a wind which blows across eastern Asia. It is also known as Purga when over the tundra); Karakaze (strong cold mountain wind from Gunma Prefecture in Japan); East Asian Monsoon, known in China and Taiwan as meiyu (梅雨), in Korea as jangma (), and in Japan as tsuyu (梅雨) when advancing northwards in the spring and shurin (秋霖) when retreating southwards in autumn.
Peak wind speeds are forecast to reach 50 to 70 mph along the coasts and valleys, according to the weather service office in Los Angeles. Gusts of 60 to 80 mph will race across the mountains and ...
The Hindu wind god, Vayu. A wind god is a god who controls the wind(s). Air deities may also be considered here as wind is nothing more than moving air. Many polytheistic religions have one or more wind gods. They may also have a separate air god or a wind god may double as an air god. Many wind gods are also linked with one of the four seasons.
Mistral wind blowing near Marseille.In the centre is the Château d'If.. The mistral (Catalan: mestral, Corsican: maestrale, Croatian: maestral, Greek: μαΐστρος, Italian: maestrale, Maltese: majjistral) is a strong, cold, northwesterly wind that blows from southern France into the Gulf of Lion in the northern Mediterranean. [1]
The interior Chinook is a föhn wind, a rain shadow wind which results from the subsequent adiabatic warming of air which has dropped most of its moisture on windward slopes (orographic lift). As a consequence of the different adiabatic rates of moist and dry air, the air on the leeward slopes becomes warmer than equivalent elevations on the ...
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