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

From Pathfinder Wiki
< AY Honors‎ | Weather - AdvancedAY Honors/Weather - Advanced/Answer Key
(18 intermediate revisions by the same user not shown)
Line 1: Line 1:
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]].
+
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 pressure area|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.
  
{{stub}}
+
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.
  
 +
[[Anticyclonic tornado]]s often occur; while tornados' [[vortex|vortices]] are low-pressure regions, this occurs because tornados occur on a small enough scale such that the Coriolis effect is negligible.
  
[[Category:Meteorology]]
+
==References==
 +
{{unreferenced|date=October 2006}}
 +
 
 +
[[Category:Storms]]
 +
[[Category:Anticyclones]]
 +
Colin is a boob
 +
 
 +
{{climate-stub}}

Revision as of 13:33, 19 May 2007

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 small enough scale such that the Coriolis effect is negligible.

References

Template:Unreferenced Colin is a boob

Template:Climate-stub