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Types of Wind

Three groups of winds may be described. First are the planetary winds, which include the Trade winds and middle latitude westerlies. Second are the secondary winds, sea breezes, Monsoon winds, and cyclonic winds. The last group includes the regional anabatic and Katabatic winds, as described below:

Planetary winds. In planetary winds, which are a major component of the general circulation, a rising motion occurs in the low latitudes where low pressure is created by maximum solar heating. A compensating inflow occurs at low levels in each hemisphere, producing the northeast trade winds of the Northern Hemisphere. The outflow of air from the tropics in the upper troposphere is diverted by the Coriolis force to produce strong westerlies.

The westerlies may become unstable and produce such mid-latitude disturbances as jet streams, cyclones, and anticyclones as well as  associated secondary wind systems. They remain essentially westerly, however, if stable. The westerlies penetrate the atmosphere to the Earth's surface, where they are dissipated by friction.

Secondary winds.  Secondary winds develop to minimize local imbalances. Monsoons, for example, minimize the temperature gradient between warm landmasses and the adjacent cooler by the Coriolis force, the summer monsoon winds approach Asia from the southwest. In winter, air flows off the extremely cold Asian landmasses toward the warmer oceans as the northeast monsoons.

An example of middle-latitude secondary wind are the winds associated with transient WEATHER systems. Besides possessing specific directions relative to the pressure centers, the winds associated with these systems are characterized by gales. A more benign system is the sea breeze, which is  usually  confined to within 20 kilometer (12.5 mi) of a coastline and to a vertical column of a few kilometers. If daytime heating is strong enough, as in the tropics, the moist onshore flow, which is forced to rise by surface heating, may form large convective clouds that yield brief, heavy showers. The cooling of the land at night reverses the sea-breeze circulation, resulting in a weak offshore surface low.

Regional winds.  Regional winds are usually the effects of such geographic features as mountain ranges. A moist wind upon a  mountain is forced to rise and may produce significant climatological effects. Cooling adiabatically, the rising air may produce rainfall on the windward side of mountains. As the air descends on the lee side, the adiabatic heating, plus the heat added to the system from condensation on the windward side, causes a very warm wind. Such MOUNTAIN and VALLEY WINDS may be very turbulent and can inflict severe damage. Ascending winds are called katabatic. A potentially destructive katabatic wind called a microburst - an intense localized downdraft that spreads along the ground - causes the condition known as wind shear. Often associated with THUNDERSTORMS and rain showers, wind shears are characterized by sudden shifts in wind speed and direction.

[Causes of Wind] [Types of Winds] [Hail Storm] [Hurricane] [Tornado] [Typhoon] [Wind Erosion]



 

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