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5th-order upwind advection (Wicker & Skamarock 2002) for horizontal fluxes in 2D and 3D, configurable via advection_scheme: "upwind5" — provides implicit numerical dissipation, eliminating the need for explicit horizontal diffusion
Beljaars (1994) convective velocity scale in MOST surface layer — prevents flux collapse in free-convective (low wind) conditions
Bug Fixes
Fix MOST surface flux collapse when mean wind is weak by incorporating M_eff = sqrt(M² + (1.2·w*)²)
Fix TKE over-initialization: use tke_min cold-start instead of convective scaling profile that caused excessive initial dissipation
Increase theta perturbation amplitude to 0.1 K (standard LES practice)
Set theta_surface to 307 K for consistency with target heat flux (~0.24 K m/s)
Other
Add minimal 2D config (cbl_2d_minimal.yaml) for isolated physics testing