What Causes A Mountain Breeze

A mountain cakewalk and a valley breeze are two related, localized winds that occur 1 after the other on a daily cycle. They are an example of anabatic and katabatic winds occurring at local scales.^[i] These winds are opposite from each other. Mount winds blow from mount towards valley afterward sunset, when mountain cools down and valley zone is insufficiently warmer. While valley breezes occur when the warm air rises up the sides of the valley,^[2] warm air in a mountain breeze will rise upward the middle.^[3]

Cause [edit]

Diurnal wind system variation in the Appalachian mountain range.

Mountain and valley breezes form through a process similar to body of water and land breezes. During the twenty-four hours, the sun heats up mountain air rapidly while the valley remains relatively cooler. Convection causes information technology to ascent, causing a valley cakewalk. At night, the process is reversed. During the night the slopes go cooled and the dumbo air descends into the valley as the mountain air current.^[four] These breezes occur more often than not during at-home and articulate weather. Mount and valley breezes are other examples of local winds caused by an surface area's geography. Campers in mountainous areas may feel a warm afternoon quickly change into a cold dark soon afterward the sun sets. During the day, the sun warms the air forth the mount slopes. This warm air rises upward the mountain slopes, creating a valley cakewalk. At nightfall, the air along the mountain slopes cools. This absurd air moves downward the slopes into the valley, producing a mountain breeze.

References [edit]

^ "katabatic wind, on AMS Glossary of Meteorology". American Meteorological Society.
^ "Valley breeze". Glossary. American Meteorological Society.
^ "Mountain cakewalk". Glossary. American Meteorological Gild.
^ Christopherson, Robert West. (1992). Geosystems: An Introduction to Physical Geography. Macmillan Publishing Company. p. 155. ISBN0-02-322443-six.