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1 1. Membership Eligibility ......................................................................................................................1 2. Individual Accounts..........................................................................................................................1 3. Joint Accounts .................................................................................................................................1 4. POD/Trust Beneficiaries.
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150th FAQ
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A depression that forms at the site of a wave-like buckle on a front. As the wave moves along the front, the latter splits into distinct warm and cold fronts. See also polar-air depression; secondary depression.
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If the upper levels are favorable for cyclone development, then there is a region of divergence aloft above the developing Low-pressure center. This will help pull the air that is converging at the surface upward and continue to develop the surface cyclone.
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Extratropical cyclones, sometimes called mid-latitude cyclones or wave cyclones, are low-pressure areas which, along with the anticyclones of high-pressure areas, drive the weather over much of the Earth.
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Cyclones are caused by atmospheric disturbances around a low-pressure area distinguished by swift and often destructive air circulation. Cyclones are usually accompanied by violent storms and bad weather.
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(Also called wave depression.) A cyclone that forms and moves along a front. The circulation about the cyclone center tends to produce a wavelike deformation of the front. The wave cyclone is the most frequent form of extratropical cyclone (or low).
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[ weyv-sahy-klohn ] show ipa. nounMeteorology. a cyclone that forms on a front and, in maturing, produces an increasingly sharp, wavelike deformation of the front.
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