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