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Winds occur on a range of scales, from thunderstorm flows lasting tens of minutes, to local breezes generated by heating of land surfaces and lasting a few hours, to global winds resulting from the difference in absorption of solar energy between the climate zones on earth. It is the hypothetical vertical wind shear that would exist if the winds obey geostrophic balance in the horizontal, while pressure obeys hydrostatic balance in the vertical. Diurnal wind change in local coastal area, also applies on the continental scale

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While the hadley, ferrel, and polar cells (whose axes are oriented along parallels or latitudes) are the major features of global heat transport, they do not act alone. In atmospheric science, the thermal wind is the vector difference between the geostrophic wind at upper altitudes minus that at lower altitudes in the atmosphere 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. The acronym gcm originally stood for general circulation model Recently, a second meaning came into use, namely global climate model

While these do not refer to the same thing, general circulation models are typically the tools used for modeling climate, and hence the two terms are sometimes used interchangeably However, the term global climate model is ambiguous and may refer to an. List of local winds this is a list of names given to winds local to specific regions. The trade winds blow mainly from the northeast in the northern hemisphere and from the southeast in the southern hemisphere, strengthening during the winter and when the arctic oscillation is in its warm phase.