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Convection causes it to rise, causing a valley breeze. At night, the process is reversed. During the night the slopes get cooled and the dense air descends into the valley as the mountain wind. [4] These breezes occur mostly during calm and clear weather. Mountain and valley breezes are other examples of local winds caused by an area's geography.
Mountain breeze may refer to: Mountain breeze and valley breeze, a localized pair of winds; Mountain Breeze, a generic store-brand citrus soda
Examples of katabatic winds include the downslope valley and mountain breezes, the piteraq winds of Greenland, the Bora in the Adriatic, [2] the Bohemian Wind or Böhmwind in the Ore Mountains, the Santa Ana winds in southern California, the oroshi in Japan, or "the Barber" in New Zealand [3]. Not all downslope winds are katabatic.
The area boasts three winter resorts: Jackson Hole Mountain Resort, Snow King Mountain Resort and Grand Targhee Resort. Downtown has adorable shops, Western-inspired bars and wonderful restaurants.
Bayswater Point State Park is a 17-acre (0.069 km 2) state park located on Jamaica Bay in Queens, New York.The park is located at the western end of Mott Avenue in Bayswater near Far Rockaway and is built on land that once housed the mansion and estate of banker Louis A. Heinsheimer.
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An anabatic wind, from the Greek anabatos, verbal of anabainein meaning "moving upward", is a warm wind which blows up a steep slope or mountain side, driven by heating of the slope through insolation. [1] [2] It is also known as upslope flow. These winds typically occur during the daytime in calm sunny weather.