Difference between revisions of "AY Honors/Weather - Advanced/Answer Key"

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A '''[[squall]] line''' is a line of severe [[thunderstorms]] that can form ahead of a [[cold front]] and can contain heavy [[precipitation (meteorology)|precipitation]], [[hail]], frequent [[lightning]], dangerous straight line winds, and possibly [[tornadoes]] and [[waterspouts]].
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An '''anticyclonic storm''' is a weather [[storm]] where winds around the storm flow contrary to the direction dictated by the [[Coriolis effect]] about a [[low (atmospheric) | region of low pressure]]. In the northern hemisphere, anticyclonic storms involve clockwise wind flow; in the southern hemisphere, they involve anticlockwise (also called ''counterclockwise'') wind flow.
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Anticyclonic storms usually form around [[pressure system | high-pressure systems]]. These do not "contradict" the [[Coriolis effect]]; it predicts such anticyclonic flow about high-pressure regions. Anticyclonic storms, as high-pressure systems, usually accompany cold weather and are frequently a factor in large [[snowstorm]]s.
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Anticyclonic [[tornado]]s often occur; while tornados' [[vortex|vortices]] are low-pressure regions, this occurs because tornados occur on a scale small enough that the Coriolis effect is negligible.
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[[Category:Weather]]

Revision as of 00:22, 14 March 2005

An anticyclonic storm is a weather storm where winds around the storm flow contrary to the direction dictated by the Coriolis effect about a region of low pressure. In the northern hemisphere, anticyclonic storms involve clockwise wind flow; in the southern hemisphere, they involve anticlockwise (also called counterclockwise) wind flow.

Anticyclonic storms usually form around high-pressure systems. These do not "contradict" the Coriolis effect; it predicts such anticyclonic flow about high-pressure regions. Anticyclonic storms, as high-pressure systems, usually accompany cold weather and are frequently a factor in large snowstorms.

Anticyclonic tornados often occur; while tornados' vortices are low-pressure regions, this occurs because tornados occur on a scale small enough that the Coriolis effect is negligible.