| 20 | | Here, ''i'', ''j'', ''k'' ∈ {1, 2, 3}. ''u'',,i,, are the velocity components (''u,,1,, = u, u,,2,, = v, u,,3,, = w'') with location ''x'',,i,, (''x,,1,, = x, x,,2,, = y, x,,3,, = z''), ''t'' is time, ''f,,i,, = (0, 2 Ω cos(φ), 2 Ω |
| 21 | | sin(φ))'' is the Coriolis parameter with ''Ω'' being the Earth's angular velocity and ''φ'' being the geographical latitude. ''u'',,g,k,, are the geostrophic wind speed components, ''ρ'',,0,, is the density of dry air, ''π^∗^ = p^∗^ + 2/3 ρ,,0,, e '' is the modified perturbation pressure with ''p^∗^'' being the perturbation pressure and the SGS-TKE |
| | 20 | Here, ''i'', ''j'', ''k'' ∈ {1, 2, 3}. ''u'',,i,, are the velocity components (''u,,1,, = u, u,,2,, = v, u,,3,, = w'') with location ''x'',,i,, (''x,,1,, = x, x,,2,, = y, x,,3,, = z''), ''t'' is time, ''f,,i,, = (-2 Ω cos(φ) sin(α), 2 Ω cos(φ) cos(α), 2 Ω |
| | 21 | sin(φ))'' is the Coriolis parameter with ''Ω'' being the Earth's angular velocity, ''φ'' being the geographical latitude, and ''α'' being the (clockwise) rotation angle of the model domain. ''u'',,g,k,, are the geostrophic wind speed components, ''ρ'',,0,, is the density of dry air, ''π^∗^ = p^∗^ + 2/3 ρ,,0,, e '' is the modified perturbation pressure with ''p^∗^'' being the perturbation pressure and the SGS-TKE |
