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Term: wind guards
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wind guards!
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wind guards
Comprehensive Analysis
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1) "Wind" -- As to wind guards 1wind Pronunciation: 'wind, archaic or poetic 'wInd Function: noun Usage: often attributive Etymology: Middle English, from Old English; akin to Old High German wint wind, Latin ventus, Greek aEnai to blow, Sanskrit vAti it blows 1 a : a natural movement of air of any velocity; especially : the earth's air or the gas surrounding a planet in natural motion horizontally b : an artificially produced movement of air c : SOLAR WIND, STELLAR WIND 2 a : a destructive force or influence b : a force or agency that carries along or influences : TENDENCY, TREND <withstood the winds of popular opinion -- Felix Frankfurter> 3 a : BREATH 4a b : BREATH 2a c : the pit of the stomach : SOLAR PLEXUS 4 : gas generated in the stomach or the intestines <pass wind> 5 a : compressed air or gas b archaic : AIR 6 : something that is insubstantial: as a : mere talk : idle words b : NOTHING, NOTHINGNESS c : vain self-satisfaction 7 a : air carrying a scent (as of a hunter or game) b : slight information especially about something secret : INTIMATION <got wind of the plan> 8 a : musical wind instruments especially as distinguished from strings and percussion b plural : players of wind instruments 9 a : a direction from which the wind may blow : a point of the compass; especially : one of the cardinal points b : the direction from which the wind is blowing - wind·less /-l&s/ adjective Wind, tacuinum sanitatis casanatensis (XIV century) Wind is the rough horizontal movement of air (as opposed to an air current) caused by uneven heating of the Earth's surface. It occurs at all scales, from local breezes generated by heating of land surfaces and lasting tens of minutes to global winds resulting from solar heating of the Earth. The two major influences on the atmospheric circulation are the differential heating between the equator and the poles, and the rotation of the planet (Coriolis effect). Given a difference in barometric pressure between two air masses, a wind will arise between the two which tends to flow from the area of high pressure to the area of low pressure until the two air masses are at the same pressure, although these flows will be modified by the Coriolis effect in the extratropics. Winds can be classified either by their scale, the kinds of forces which cause them (according to the atmospheric equations of motion), or the geographic regions in which they exist. There are global winds, such as the wind belts which exist between the atmospheric circulation cells. There are upper-level winds, such as the jet streams. There are synoptic-scale winds that result from pressure differences in surface air masses in the middle latitudes, and there are winds that come about as a consequence of geographic features such as the sea breeze. Mesoscale winds are those which act on a local scale, such as gust fronts. At the smallest scale are the microscale winds which blow on a scale of only tens to hundreds of meters and are essentially unpredictable, such as dust devils and microbursts. Winds can also shape landforms, via a variety of eolian processes.
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