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Mountain and valley breezes are other examples of local winds caused by an area's geography. Campers in mountainous areas may feel a warm afternoon quickly change into a cold night soon after the sun sets. During the day, the sun warms the air along the mountain slopes. This warm air rises up the mountain slopes, creating a valley breeze.
Mountain breeze may refer to: Mountain breeze and valley breeze, a localized pair of winds; Mountain Breeze, a generic store-brand citrus soda
Mountain Dew is a bit tangier than its Safeway SELECT counterpart, which focuses more on sweetness. [citation needed] The design of a Mountain Breeze soda can also bears a great resemblance to an older Mountain Dew can, more so than many of the generic citrus sodas. Safeway Select has replaced the brand name with Refreshe.
Examples of katabatic winds include the downslope valley and mountain breezes, the piteraq winds of Greenland, the moderate Bora in the Adriatic, [2] the Bohemian Wind or Böhmwind in the Ore Mountains, the Santa Ana in southern California, the oroshi in Japan, or "the Barber" in New Zealand [3].
In areas where winds tend to be light, the sea breeze/land breeze cycle is the most important cause of the prevailing wind; in areas which have variable terrain, mountain and valley breezes dominate the wind pattern. Highly elevated surfaces can induce a thermal low, which then augments the environmental wind flow.
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Thunderstorms and other atmospheric convection, squall lines, drylines, [9] sea and land breezes, mountain breeze and valley breezes, mountain waves, mesolows and mesohighs, wake lows, mesoscale convective vortices (MCVs), tropical cyclone and extratropical cyclone rainbands, macrobursts, gust fronts and outflow boundaries, heat bursts, urban heat islands (UHIs), and other mesoscale phenomena ...
Therefore, smaller scale wind patterns generated by local topography, such as diurnal mountain breeze [26] and katabatic wind, [25] [27] can be important in forcing circulation in alpine lakes. Wind patterns which vary spatially over the extent of the lake may create regions of upwelling and downwelling . [ 28 ]