Upper-level cyclone: Difference between revisions
From Glossary of Meteorology
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<div class="definition"><div class="short_definition">(''Also called'' upper-level low, upper cyclone, upper low, high-level cyclone, low aloft.) A [[cyclonic circulation]] existing in the [[upper air]]; specifically as seen on an upper-level [[constant-pressure chart]].</div><br/> <div class="paragraph">This term is often restricted to such [[cyclones]] associated with relatively little cyclonic circulation in the [[lower atmosphere]].</div><br/> </div> | <div class="definition"><div class="short_definition">(''Also called'' upper-level low, upper cyclone, upper low, high-level cyclone, low aloft.) A [[cyclonic circulation]] existing in the [[upper-air|upper air]]; specifically as seen on an upper-level [[constant-pressure chart]].</div><br/> <div class="paragraph">This term is often restricted to such [[cyclones]] associated with relatively little cyclonic circulation in the [[lower atmosphere]].</div><br/> </div> | ||
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Latest revision as of 17:10, 25 April 2012
upper-level cyclone
(Also called upper-level low, upper cyclone, upper low, high-level cyclone, low aloft.) A cyclonic circulation existing in the upper air; specifically as seen on an upper-level constant-pressure chart.
This term is often restricted to such cyclones associated with relatively little cyclonic circulation in the lower atmosphere.
