Upper-level cyclone: Difference between revisions
From Glossary of Meteorology
No edit summary |
m (Rewrite with Template:Term and clean up) |
||
(One intermediate revision by the same user not shown) | |||
Line 1: | Line 1: | ||
{{Term | |||
|Display title=upper-level cyclone | |||
{{ | |Definitions={{Definition | ||
|Num=1 | |||
|Meaning= | |||
(''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]].<br/> This term is often restricted to such [[cyclones]] associated with relatively little cyclonic circulation in the [[lower atmosphere]]. | |||
}} | |||
}} | |||
Latest revision as of 03:40, 27 March 2024
(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.