Mixing in the Salt Lake City is multi-scale in scope with drainage flows from the nearby mountains interacting with boundary layer motions whose scale is reduced due to the strong stratification in the nocturnal stable boundary layer. We are investigating four approaches for including the effects of this drainage flow on a boundary layer simulation: 1) use nudging and open boundary conditions to influence the boundary layer winds with a mesoscale mean wind and velocity gradient, 2) using periodic boundary conditions and nudging to influence the boundary layer winds with a mesoscale mean, 3) use approach 1 but with a random perturbation on inflow to simulate the effect of embedded turbulent motions in the mesoscale flow, 4) approach 1 but with perturbations derived from an LES model to better represent turbulent motions embedded in the mesoscale flow. Each approach will be evaluated on how it alters the dynamics of the boundary layer simulation and its effects on the dispersion patterns of advected tracers.
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