Storm track: Difference between revisions
From Glossary of Meteorology
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#<div class="definition"><div class="short_definition">A region in which the [[synoptic]] eddy activity is statistically and locally most prevalent and intense.</div><br/> <div class="paragraph">It also roughly corresponds to the mean trajectory of the [[cyclones]] in winter. In winter, there are two [[storm]] tracks in the Northern Hemisphere centered at about 45& | #<div class="definition"><div class="short_definition">A region in which the [[synoptic]] eddy activity is statistically and locally most prevalent and intense.</div><br/> <div class="paragraph">It also roughly corresponds to the mean trajectory of the [[cyclones]] in winter. In winter, there are two [[storm]] tracks in the Northern Hemisphere centered at about 45°N, one over the Pacific Ocean and the other over the Atlantic Ocean. There is one storm track in the Southern Hemisphere over the South Indian Ocean region at about 50°S prevalent throughout most of the year.</div><br/> </div> | ||
#<div class="definition"><div class="short_definition">The path followed by a meteorological phenomenon, for example, a center of low atmospheric [[pressure]], a severe [[thunderstorm]], a [[tornado]].</div><br/> </div> | #<div class="definition"><div class="short_definition">The path followed by a meteorological phenomenon, for example, a center of low atmospheric [[pressure]], a severe [[thunderstorm]], a [[tornado]].</div><br/> </div> | ||
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Latest revision as of 15:13, 20 February 2012
storm track
- A region in which the synoptic eddy activity is statistically and locally most prevalent and intense.
It also roughly corresponds to the mean trajectory of the cyclones in winter. In winter, there are two storm tracks in the Northern Hemisphere centered at about 45°N, one over the Pacific Ocean and the other over the Atlantic Ocean. There is one storm track in the Southern Hemisphere over the South Indian Ocean region at about 50°S prevalent throughout most of the year.
- The path followed by a meteorological phenomenon, for example, a center of low atmospheric pressure, a severe thunderstorm, a tornado.