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atmospheric layer, and Δ q is the change in q a due to the surface turbulent fluxes and boundary layer mixing processes. The total kinematic evaporation flux E in the Noah LSM has five components representing the contributions from the direct evaporation flux from the ground surface: evaporation fluxes via roots from the three below-surface soil layers and evaporation fluxes from the precipitation intercepted by vegetation as well as dew formed on the canopy. These five evaporation fluxes are
atmospheric layer, and Δ q is the change in q a due to the surface turbulent fluxes and boundary layer mixing processes. The total kinematic evaporation flux E in the Noah LSM has five components representing the contributions from the direct evaporation flux from the ground surface: evaporation fluxes via roots from the three below-surface soil layers and evaporation fluxes from the precipitation intercepted by vegetation as well as dew formed on the canopy. These five evaporation fluxes are
