Concept information
Preferred term
upward_eliassen_palm_flux_in_air
Definition
- "Eliassen Palm flux" is a widely used vector in the meridional plane, and the divergence of this flux appears as a forcing in the Transformed Eulerian mean formulation of the zonal mean zonal wind equation. "Upward" indicates a vector component which is positive when directed upward (negative downward).
Note
- Mapping to be determined
URI
https://vocab.met.no/CFSTDN/upward_eliassen_palm_flux_in_air
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