ERF_AddTKESources.H File Reference

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Functions
	if (l_use_keqn &&(start_comp<=RhoKE_comp) &&(end_comp >=RhoKE_comp))

Function Documentation

if()

if

(

l_use_keqn &&

start_comp<=RhoKE_comp) &&(end_comp >=RhoKE_comp

)

                                                                              {
        int qty_index = RhoKE_comp;
        ParallelFor(bx,[=] AMREX_GPU_DEVICE (int i, int j, int k) noexcept
        {
            // Add Buoyancy Source
            // where the SGS buoyancy flux tau_{theta,i} = -KH * dtheta/dx_i,
            // such that for dtheta/dz < 0, there is a positive (upward) heat
            // flux; the TKE buoyancy production is then
            //   B = g/theta_0 * tau_{theta,w}
            // for a dry atmosphere.
            // TODO: To account for moisture, the Brunt-Vaisala frequency,
            //   N^2 = g[1/theta * dtheta/dz + ...]
            // **should** be a function of the water vapor and total water
            // mixing ratios, depending on whether conditions are saturated or
            // not (see the WRF model description, Skamarock et al 2019).
            cell_rhs(i,j,k,qty_index) += l_abs_g * l_inv_theta0 * hfx_z(i,j,k);
            if (!use_ref_theta) {
                // l_inv_theta0 == 1, divide by actual theta
                cell_rhs(i,j,k,qty_index) /= cell_prim(i,j,k,PrimTheta_comp);
            }
 
            // TKE shear production
            //   P = -tau_ij * S_ij = 2 * mu_turb * S_ij * S_ij
            // Note: This assumes that the horizontal and vertical diffusivities
            // of momentum are equal
            cell_rhs(i,j,k,qty_index) += 2.0*mu_turb(i,j,k,EddyDiff::Mom_v) * SmnSmn_a(i,j,k);
 
            // TKE dissipation
            cell_rhs(i,j,k,qty_index) -= diss(i,j,k);
        });
    }

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