Concept information
Preferred term
upward_heat_flux_in_air
Definition
- 'Upward' indicates a vector component which is positive when directed upward (negative downward). The vertical heat flux in air is the sum of all heat fluxes i.e. radiative, latent and sensible. In accordance with common usage in geophysical disciplines, 'flux' implies per unit area, called 'flux density' in physics.
Note
- Mapping to be determined
URI
https://vocab.met.no/CFSTDN/upward_heat_flux_in_air
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