Storm-relative environmental helicity: Difference between revisions
From Glossary of Meteorology
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|Display title=storm-relative environmental helicity | |||
|Definitions={{Definition | |||
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|Meaning=(Abbreviated SREH.) A measure of the [[streamwise vorticity]] within the [[inflow]] environment of a [[convective storm]]. | |||
|Explanation=It is calculated by multiplying the storm-relative inflow velocity [[vector]] by the [[streamwise vorticity|streamwise vorticity]] and integrating this quantity over the inflow depth. Geometrically, the storm-relative environmental helicity is represented by the area on a [[hodograph]] swept out by the storm-relative [[wind]] vectors between specified levels (typically the surface and 3 km to represent the primary [[storm]] inflow). It is thought to be a measure of the tendency of a [[supercell]] to rotate. | |||
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Latest revision as of 07:30, 30 March 2024
(Abbreviated SREH.) A measure of the streamwise vorticity within the inflow environment of a convective storm.
It is calculated by multiplying the storm-relative inflow velocity vector by the streamwise vorticity and integrating this quantity over the inflow depth. Geometrically, the storm-relative environmental helicity is represented by the area on a hodograph swept out by the storm-relative wind vectors between specified levels (typically the surface and 3 km to represent the primary storm inflow). It is thought to be a measure of the tendency of a supercell to rotate.