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See also:TORNADO (Span., tornada, a turning about, cf. " turn ") , a See also:local whirlwind of extreme violence, usually formed within a thunderstorm . In See also:appearance it consists of a See also:funnel-shaped See also:cloud, depending from the See also:mass of See also:storm-cloud above, and when fully See also:developed tapering downwards to the See also:earth . Besides its whirling See also:motion, a See also:tornado has an advancing See also:movement of from 20 to 40 M. an See also:hour—and along its own narrow path it carries destruction . Its duration is usually from See also:half an hour to an hour . Tornadoes are most See also:common in See also:America, especially in the See also:Mississippi Valley and the See also:Southern states; in See also:Europe and elsewhere they are comparatively rare . Owing to their association with thunderstorms they generally occur in warm See also:weather . A tornado is the result of a See also:condition of local in-stability in the See also:atmosphere, originating high above the earth . A current of See also:air is induced to ascend with a rapid See also:spiral motion See also:round a central core of See also:low pressure . The moisture in the ascending air is condensed by cooling both as it ascends and as it expands into the low-pressure core . The cloud-funnel appears to grow downwards because the moisture in the air is condensed more rapidly than the air itself, following a spiral course, ascends . |
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