| [1] | 1 | MODULE diffusion_v_mod |
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| 2 | |
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| 3 | !------------------------------------------------------------------------------! |
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| 4 | ! Actual revisions: |
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| 5 | ! ----------------- |
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| [106] | 6 | ! Momentumflux at top (vswst) included as boundary condition, |
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| 7 | ! j loop is starting from nysv (needed for non-cyclic boundary conditions) |
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| [1] | 8 | ! |
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| 9 | ! Former revisions: |
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| 10 | ! ----------------- |
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| [3] | 11 | ! $Id: diffusion_v.f90 106 2007-08-16 14:30:26Z raasch $ |
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| [39] | 12 | ! |
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| [77] | 13 | ! 75 2007-03-22 09:54:05Z raasch |
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| 14 | ! Wall functions now include diabatic conditions, call of routine wall_fluxes, |
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| 15 | ! z0 removed from argument list, vynp eliminated |
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| 16 | ! |
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| [39] | 17 | ! 20 2007-02-26 00:12:32Z raasch |
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| 18 | ! Bugfix: ddzw dimensioned 1:nzt"+1" |
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| 19 | ! |
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| [3] | 20 | ! RCS Log replace by Id keyword, revision history cleaned up |
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| 21 | ! |
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| [1] | 22 | ! Revision 1.15 2006/02/23 10:36:00 raasch |
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| 23 | ! nzb_2d replaced by nzb_v_outer in horizontal diffusion and by nzb_v_inner |
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| 24 | ! or nzb_diff_v, respectively, in vertical diffusion, |
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| 25 | ! wall functions added for north and south walls, +z0 in argument list, |
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| 26 | ! terms containing w(k-1,..) are removed from the Prandtl-layer equation |
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| 27 | ! because they cause errors at the edges of topography |
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| 28 | ! WARNING: loops containing the MAX function are still not properly vectorized! |
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| 29 | ! |
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| 30 | ! Revision 1.1 1997/09/12 06:24:01 raasch |
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| 31 | ! Initial revision |
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| 32 | ! |
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| 33 | ! |
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| 34 | ! Description: |
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| 35 | ! ------------ |
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| 36 | ! Diffusion term of the v-component |
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| 37 | !------------------------------------------------------------------------------! |
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| 38 | |
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| [56] | 39 | USE wall_fluxes_mod |
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| 40 | |
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| [1] | 41 | PRIVATE |
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| 42 | PUBLIC diffusion_v |
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| 43 | |
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| 44 | INTERFACE diffusion_v |
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| 45 | MODULE PROCEDURE diffusion_v |
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| 46 | MODULE PROCEDURE diffusion_v_ij |
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| 47 | END INTERFACE diffusion_v |
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| 48 | |
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| 49 | CONTAINS |
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| 50 | |
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| 51 | |
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| 52 | !------------------------------------------------------------------------------! |
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| 53 | ! Call for all grid points |
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| 54 | !------------------------------------------------------------------------------! |
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| [102] | 55 | SUBROUTINE diffusion_v( ddzu, ddzw, km, km_damp_x, tend, u, v, vsws, & |
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| 56 | vswst, w ) |
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| [1] | 57 | |
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| 58 | USE control_parameters |
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| 59 | USE grid_variables |
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| 60 | USE indices |
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| 61 | |
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| 62 | IMPLICIT NONE |
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| 63 | |
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| 64 | INTEGER :: i, j, k |
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| [51] | 65 | REAL :: kmxm_x, kmxm_y, kmxp_x, kmxp_y, kmzm, kmzp |
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| [20] | 66 | REAL :: ddzu(1:nzt+1), ddzw(1:nzt+1), km_damp_x(nxl-1:nxr+1) |
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| [1] | 67 | REAL :: tend(nzb:nzt+1,nys-1:nyn+1,nxl-1:nxr+1) |
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| [102] | 68 | REAL, DIMENSION(:,:), POINTER :: vsws, vswst |
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| [1] | 69 | REAL, DIMENSION(:,:,:), POINTER :: km, u, v, w |
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| [75] | 70 | REAL, DIMENSION(nzb:nzt+1,nys:nyn,nxl:nxr) :: vsus |
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| [1] | 71 | |
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| [56] | 72 | ! |
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| 73 | !-- First calculate horizontal momentum flux v'u' at vertical walls, |
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| 74 | !-- if neccessary |
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| 75 | IF ( topography /= 'flat' ) THEN |
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| [75] | 76 | CALL wall_fluxes( vsus, 0.0, 1.0, 0.0, 0.0, nzb_v_inner, & |
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| [56] | 77 | nzb_v_outer, wall_v ) |
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| 78 | ENDIF |
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| 79 | |
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| [1] | 80 | DO i = nxl, nxr |
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| [106] | 81 | DO j = nysv, nyn |
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| [1] | 82 | ! |
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| 83 | !-- Compute horizontal diffusion |
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| 84 | DO k = nzb_v_outer(j,i)+1, nzt |
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| 85 | ! |
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| 86 | !-- Interpolate eddy diffusivities on staggered gridpoints |
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| 87 | kmxp_x = 0.25 * & |
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| 88 | ( km(k,j,i)+km(k,j,i+1)+km(k,j-1,i)+km(k,j-1,i+1) ) |
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| 89 | kmxm_x = 0.25 * & |
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| 90 | ( km(k,j,i)+km(k,j,i-1)+km(k,j-1,i)+km(k,j-1,i-1) ) |
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| 91 | kmxp_y = kmxp_x |
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| 92 | kmxm_y = kmxm_x |
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| 93 | ! |
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| 94 | !-- Increase diffusion at the outflow boundary in case of |
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| 95 | !-- non-cyclic lateral boundaries. Damping is only needed for |
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| 96 | !-- velocity components parallel to the outflow boundary in |
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| 97 | !-- the direction normal to the outflow boundary. |
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| 98 | IF ( bc_lr /= 'cyclic' ) THEN |
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| 99 | kmxp_x = MAX( kmxp_x, km_damp_x(i) ) |
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| 100 | kmxm_x = MAX( kmxm_x, km_damp_x(i) ) |
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| 101 | ENDIF |
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| 102 | |
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| 103 | tend(k,j,i) = tend(k,j,i) & |
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| 104 | & + ( kmxp_x * ( v(k,j,i+1) - v(k,j,i) ) * ddx & |
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| 105 | & + kmxp_y * ( u(k,j,i+1) - u(k,j-1,i+1) ) * ddy & |
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| 106 | & - kmxm_x * ( v(k,j,i) - v(k,j,i-1) ) * ddx & |
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| 107 | & - kmxm_y * ( u(k,j,i) - u(k,j-1,i) ) * ddy & |
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| 108 | & ) * ddx & |
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| 109 | & + 2.0 * ( & |
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| 110 | & km(k,j,i) * ( v(k,j+1,i) - v(k,j,i) ) & |
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| 111 | & - km(k,j-1,i) * ( v(k,j,i) - v(k,j-1,i) ) & |
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| 112 | & ) * ddy2 |
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| 113 | ENDDO |
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| 114 | |
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| 115 | ! |
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| 116 | !-- Wall functions at the left and right walls, respectively |
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| 117 | IF ( wall_v(j,i) /= 0.0 ) THEN |
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| [51] | 118 | |
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| [1] | 119 | DO k = nzb_v_inner(j,i)+1, nzb_v_outer(j,i) |
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| 120 | kmxp_x = 0.25 * & |
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| 121 | ( km(k,j,i)+km(k,j,i+1)+km(k,j-1,i)+km(k,j-1,i+1) ) |
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| 122 | kmxm_x = 0.25 * & |
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| 123 | ( km(k,j,i)+km(k,j,i-1)+km(k,j-1,i)+km(k,j-1,i-1) ) |
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| 124 | kmxp_y = kmxp_x |
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| 125 | kmxm_y = kmxm_x |
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| 126 | ! |
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| 127 | !-- Increase diffusion at the outflow boundary in case of |
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| 128 | !-- non-cyclic lateral boundaries. Damping is only needed for |
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| 129 | !-- velocity components parallel to the outflow boundary in |
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| 130 | !-- the direction normal to the outflow boundary. |
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| 131 | IF ( bc_lr /= 'cyclic' ) THEN |
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| 132 | kmxp_x = MAX( kmxp_x, km_damp_x(i) ) |
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| 133 | kmxm_x = MAX( kmxm_x, km_damp_x(i) ) |
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| 134 | ENDIF |
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| 135 | |
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| 136 | tend(k,j,i) = tend(k,j,i) & |
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| 137 | + 2.0 * ( & |
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| 138 | km(k,j,i) * ( v(k,j+1,i) - v(k,j,i) ) & |
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| 139 | - km(k,j-1,i) * ( v(k,j,i) - v(k,j-1,i) ) & |
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| 140 | ) * ddy2 & |
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| 141 | + ( fxp(j,i) * ( & |
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| 142 | kmxp_x * ( v(k,j,i+1) - v(k,j,i) ) * ddx & |
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| 143 | + kmxp_y * ( u(k,j,i+1) - u(k,j-1,i+1) ) * ddy & |
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| 144 | ) & |
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| 145 | - fxm(j,i) * ( & |
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| 146 | kmxm_x * ( v(k,j,i) - v(k,j,i-1) ) * ddx & |
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| 147 | + kmxm_y * ( u(k,j,i) - u(k,j-1,i) ) * ddy & |
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| 148 | ) & |
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| [56] | 149 | + wall_v(j,i) * vsus(k,j,i) & |
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| [1] | 150 | ) * ddx |
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| 151 | ENDDO |
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| 152 | ENDIF |
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| 153 | |
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| 154 | ! |
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| 155 | !-- Compute vertical diffusion. In case of simulating a Prandtl |
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| 156 | !-- layer, index k starts at nzb_v_inner+2. |
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| [102] | 157 | DO k = nzb_diff_v(j,i), nzt_diff |
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| [1] | 158 | ! |
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| 159 | !-- Interpolate eddy diffusivities on staggered gridpoints |
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| 160 | kmzp = 0.25 * & |
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| 161 | ( km(k,j,i)+km(k+1,j,i)+km(k,j-1,i)+km(k+1,j-1,i) ) |
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| 162 | kmzm = 0.25 * & |
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| 163 | ( km(k,j,i)+km(k-1,j,i)+km(k,j-1,i)+km(k-1,j-1,i) ) |
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| 164 | |
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| 165 | tend(k,j,i) = tend(k,j,i) & |
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| 166 | & + ( kmzp * ( ( v(k+1,j,i) - v(k,j,i) ) * ddzu(k+1) & |
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| 167 | & + ( w(k,j,i) - w(k,j-1,i) ) * ddy & |
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| 168 | & ) & |
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| 169 | & - kmzm * ( ( v(k,j,i) - v(k-1,j,i) ) * ddzu(k) & |
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| 170 | & + ( w(k-1,j,i) - w(k-1,j-1,i) ) * ddy & |
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| 171 | & ) & |
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| 172 | & ) * ddzw(k) |
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| 173 | ENDDO |
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| 174 | |
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| 175 | ! |
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| 176 | !-- Vertical diffusion at the first grid point above the surface, |
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| 177 | !-- if the momentum flux at the bottom is given by the Prandtl law |
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| 178 | !-- or if it is prescribed by the user. |
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| 179 | !-- Difference quotient of the momentum flux is not formed over |
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| 180 | !-- half of the grid spacing (2.0*ddzw(k)) any more, since the |
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| 181 | !-- comparison with other (LES) modell showed that the values of |
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| 182 | !-- the momentum flux becomes too large in this case. |
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| 183 | !-- The term containing w(k-1,..) (see above equation) is removed here |
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| 184 | !-- because the vertical velocity is assumed to be zero at the surface. |
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| 185 | IF ( use_surface_fluxes ) THEN |
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| 186 | k = nzb_v_inner(j,i)+1 |
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| 187 | ! |
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| 188 | !-- Interpolate eddy diffusivities on staggered gridpoints |
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| 189 | kmzp = 0.25 * & |
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| 190 | ( km(k,j,i)+km(k+1,j,i)+km(k,j-1,i)+km(k+1,j-1,i) ) |
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| 191 | kmzm = 0.25 * & |
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| 192 | ( km(k,j,i)+km(k-1,j,i)+km(k,j-1,i)+km(k-1,j-1,i) ) |
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| 193 | |
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| 194 | tend(k,j,i) = tend(k,j,i) & |
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| 195 | & + ( kmzp * ( w(k,j,i) - w(k,j-1,i) ) * ddy & |
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| 196 | & ) * ddzw(k) & |
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| [102] | 197 | & + ( kmzp * ( v(k+1,j,i) - v(k,j,i) ) * ddzu(k+1) & |
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| [1] | 198 | & + vsws(j,i) & |
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| 199 | & ) * ddzw(k) |
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| 200 | ENDIF |
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| 201 | |
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| [102] | 202 | ! |
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| 203 | !-- Vertical diffusion at the first gridpoint below the top boundary, |
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| 204 | !-- if the momentum flux at the top is prescribed by the user |
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| [103] | 205 | IF ( use_top_fluxes .AND. constant_top_momentumflux ) THEN |
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| [102] | 206 | k = nzt |
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| 207 | ! |
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| 208 | !-- Interpolate eddy diffusivities on staggered gridpoints |
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| 209 | kmzp = 0.25 * & |
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| 210 | ( km(k,j,i)+km(k+1,j,i)+km(k,j-1,i)+km(k+1,j-1,i) ) |
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| 211 | kmzm = 0.25 * & |
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| 212 | ( km(k,j,i)+km(k-1,j,i)+km(k,j-1,i)+km(k-1,j-1,i) ) |
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| 213 | |
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| 214 | tend(k,j,i) = tend(k,j,i) & |
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| 215 | & - ( kmzm * ( w(k-1,j,i) - w(k-1,j-1,i) ) * ddy & |
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| 216 | & ) * ddzw(k) & |
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| 217 | & + ( -vswst(j,i) & |
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| 218 | & - kmzm * ( v(k,j,i) - v(k-1,j,i) ) * ddzu(k) & |
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| 219 | & ) * ddzw(k) |
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| 220 | ENDIF |
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| 221 | |
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| [1] | 222 | ENDDO |
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| 223 | ENDDO |
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| 224 | |
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| 225 | END SUBROUTINE diffusion_v |
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| 226 | |
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| 227 | |
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| 228 | !------------------------------------------------------------------------------! |
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| 229 | ! Call for grid point i,j |
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| 230 | !------------------------------------------------------------------------------! |
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| 231 | SUBROUTINE diffusion_v_ij( i, j, ddzu, ddzw, km, km_damp_x, tend, u, v, & |
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| [102] | 232 | vsws, vswst, w ) |
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| [1] | 233 | |
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| 234 | USE control_parameters |
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| 235 | USE grid_variables |
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| 236 | USE indices |
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| 237 | |
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| 238 | IMPLICIT NONE |
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| 239 | |
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| 240 | INTEGER :: i, j, k |
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| [51] | 241 | REAL :: kmxm_x, kmxm_y, kmxp_x, kmxp_y, kmzm, kmzp |
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| [20] | 242 | REAL :: ddzu(1:nzt+1), ddzw(1:nzt+1), km_damp_x(nxl-1:nxr+1) |
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| [1] | 243 | REAL :: tend(nzb:nzt+1,nys-1:nyn+1,nxl-1:nxr+1) |
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| [51] | 244 | REAL, DIMENSION(nzb:nzt+1) :: vsus |
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| [102] | 245 | REAL, DIMENSION(:,:), POINTER :: vsws, vswst |
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| [1] | 246 | REAL, DIMENSION(:,:,:), POINTER :: km, u, v, w |
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| 247 | |
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| 248 | ! |
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| 249 | !-- Compute horizontal diffusion |
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| 250 | DO k = nzb_v_outer(j,i)+1, nzt |
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| 251 | ! |
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| 252 | !-- Interpolate eddy diffusivities on staggered gridpoints |
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| 253 | kmxp_x = 0.25 * ( km(k,j,i)+km(k,j,i+1)+km(k,j-1,i)+km(k,j-1,i+1) ) |
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| 254 | kmxm_x = 0.25 * ( km(k,j,i)+km(k,j,i-1)+km(k,j-1,i)+km(k,j-1,i-1) ) |
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| 255 | kmxp_y = kmxp_x |
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| 256 | kmxm_y = kmxm_x |
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| 257 | ! |
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| 258 | !-- Increase diffusion at the outflow boundary in case of non-cyclic |
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| 259 | !-- lateral boundaries. Damping is only needed for velocity components |
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| 260 | !-- parallel to the outflow boundary in the direction normal to the |
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| 261 | !-- outflow boundary. |
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| 262 | IF ( bc_lr /= 'cyclic' ) THEN |
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| 263 | kmxp_x = MAX( kmxp_x, km_damp_x(i) ) |
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| 264 | kmxm_x = MAX( kmxm_x, km_damp_x(i) ) |
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| 265 | ENDIF |
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| 266 | |
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| 267 | tend(k,j,i) = tend(k,j,i) & |
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| 268 | & + ( kmxp_x * ( v(k,j,i+1) - v(k,j,i) ) * ddx & |
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| 269 | & + kmxp_y * ( u(k,j,i+1) - u(k,j-1,i+1) ) * ddy & |
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| 270 | & - kmxm_x * ( v(k,j,i) - v(k,j,i-1) ) * ddx & |
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| 271 | & - kmxm_y * ( u(k,j,i) - u(k,j-1,i) ) * ddy & |
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| 272 | & ) * ddx & |
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| 273 | & + 2.0 * ( & |
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| 274 | & km(k,j,i) * ( v(k,j+1,i) - v(k,j,i) ) & |
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| 275 | & - km(k,j-1,i) * ( v(k,j,i) - v(k,j-1,i) ) & |
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| 276 | & ) * ddy2 |
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| 277 | ENDDO |
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| 278 | |
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| 279 | ! |
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| 280 | !-- Wall functions at the left and right walls, respectively |
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| 281 | IF ( wall_v(j,i) /= 0.0 ) THEN |
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| [51] | 282 | |
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| 283 | ! |
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| 284 | !-- Calculate the horizontal momentum flux v'u' |
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| 285 | CALL wall_fluxes( i, j, nzb_v_inner(j,i)+1, nzb_v_outer(j,i), & |
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| 286 | vsus, 0.0, 1.0, 0.0, 0.0 ) |
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| 287 | |
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| [1] | 288 | DO k = nzb_v_inner(j,i)+1, nzb_v_outer(j,i) |
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| 289 | kmxp_x = 0.25 * & |
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| 290 | ( km(k,j,i)+km(k,j,i+1)+km(k,j-1,i)+km(k,j-1,i+1) ) |
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| 291 | kmxm_x = 0.25 * & |
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| 292 | ( km(k,j,i)+km(k,j,i-1)+km(k,j-1,i)+km(k,j-1,i-1) ) |
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| 293 | kmxp_y = kmxp_x |
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| 294 | kmxm_y = kmxm_x |
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| 295 | ! |
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| 296 | !-- Increase diffusion at the outflow boundary in case of |
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| 297 | !-- non-cyclic lateral boundaries. Damping is only needed for |
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| 298 | !-- velocity components parallel to the outflow boundary in |
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| 299 | !-- the direction normal to the outflow boundary. |
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| 300 | IF ( bc_lr /= 'cyclic' ) THEN |
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| 301 | kmxp_x = MAX( kmxp_x, km_damp_x(i) ) |
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| 302 | kmxm_x = MAX( kmxm_x, km_damp_x(i) ) |
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| 303 | ENDIF |
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| 304 | |
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| 305 | tend(k,j,i) = tend(k,j,i) & |
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| 306 | + 2.0 * ( & |
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| 307 | km(k,j,i) * ( v(k,j+1,i) - v(k,j,i) ) & |
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| 308 | - km(k,j-1,i) * ( v(k,j,i) - v(k,j-1,i) ) & |
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| 309 | ) * ddy2 & |
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| 310 | + ( fxp(j,i) * ( & |
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| 311 | kmxp_x * ( v(k,j,i+1) - v(k,j,i) ) * ddx & |
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| 312 | + kmxp_y * ( u(k,j,i+1) - u(k,j-1,i+1) ) * ddy & |
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| 313 | ) & |
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| 314 | - fxm(j,i) * ( & |
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| 315 | kmxm_x * ( v(k,j,i) - v(k,j,i-1) ) * ddx & |
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| 316 | + kmxm_y * ( u(k,j,i) - u(k,j-1,i) ) * ddy & |
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| 317 | ) & |
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| [51] | 318 | + wall_v(j,i) * vsus(k) & |
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| [1] | 319 | ) * ddx |
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| 320 | ENDDO |
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| 321 | ENDIF |
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| 322 | |
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| 323 | ! |
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| 324 | !-- Compute vertical diffusion. In case of simulating a Prandtl layer, |
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| 325 | !-- index k starts at nzb_v_inner+2. |
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| [102] | 326 | DO k = nzb_diff_v(j,i), nzt_diff |
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| [1] | 327 | ! |
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| 328 | !-- Interpolate eddy diffusivities on staggered gridpoints |
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| 329 | kmzp = 0.25 * ( km(k,j,i)+km(k+1,j,i)+km(k,j-1,i)+km(k+1,j-1,i) ) |
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| 330 | kmzm = 0.25 * ( km(k,j,i)+km(k-1,j,i)+km(k,j-1,i)+km(k-1,j-1,i) ) |
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| 331 | |
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| 332 | tend(k,j,i) = tend(k,j,i) & |
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| 333 | & + ( kmzp * ( ( v(k+1,j,i) - v(k,j,i) ) * ddzu(k+1) & |
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| 334 | & + ( w(k,j,i) - w(k,j-1,i) ) * ddy & |
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| 335 | & ) & |
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| 336 | & - kmzm * ( ( v(k,j,i) - v(k-1,j,i) ) * ddzu(k) & |
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| 337 | & + ( w(k-1,j,i) - w(k-1,j-1,i) ) * ddy & |
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| 338 | & ) & |
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| 339 | & ) * ddzw(k) |
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| 340 | ENDDO |
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| 341 | |
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| 342 | ! |
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| 343 | !-- Vertical diffusion at the first grid point above the surface, if the |
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| 344 | !-- momentum flux at the bottom is given by the Prandtl law or if it is |
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| 345 | !-- prescribed by the user. |
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| 346 | !-- Difference quotient of the momentum flux is not formed over half of |
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| 347 | !-- the grid spacing (2.0*ddzw(k)) any more, since the comparison with |
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| 348 | !-- other (LES) modell showed that the values of the momentum flux becomes |
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| 349 | !-- too large in this case. |
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| 350 | !-- The term containing w(k-1,..) (see above equation) is removed here |
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| 351 | !-- because the vertical velocity is assumed to be zero at the surface. |
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| 352 | IF ( use_surface_fluxes ) THEN |
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| 353 | k = nzb_v_inner(j,i)+1 |
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| 354 | ! |
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| 355 | !-- Interpolate eddy diffusivities on staggered gridpoints |
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| 356 | kmzp = 0.25 * ( km(k,j,i)+km(k+1,j,i)+km(k,j-1,i)+km(k+1,j-1,i) ) |
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| 357 | kmzm = 0.25 * ( km(k,j,i)+km(k-1,j,i)+km(k,j-1,i)+km(k-1,j-1,i) ) |
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| 358 | |
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| 359 | tend(k,j,i) = tend(k,j,i) & |
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| 360 | & + ( kmzp * ( w(k,j,i) - w(k,j-1,i) ) * ddy & |
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| 361 | & ) * ddzw(k) & |
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| [102] | 362 | & + ( kmzp * ( v(k+1,j,i) - v(k,j,i) ) * ddzu(k+1) & |
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| [1] | 363 | & + vsws(j,i) & |
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| 364 | & ) * ddzw(k) |
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| 365 | ENDIF |
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| 366 | |
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| [102] | 367 | ! |
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| 368 | !-- Vertical diffusion at the first gridpoint below the top boundary, |
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| 369 | !-- if the momentum flux at the top is prescribed by the user |
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| [103] | 370 | IF ( use_top_fluxes .AND. constant_top_momentumflux ) THEN |
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| [102] | 371 | k = nzt |
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| 372 | ! |
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| 373 | !-- Interpolate eddy diffusivities on staggered gridpoints |
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| 374 | kmzp = 0.25 * & |
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| 375 | ( km(k,j,i)+km(k+1,j,i)+km(k,j-1,i)+km(k+1,j-1,i) ) |
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| 376 | kmzm = 0.25 * & |
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| 377 | ( km(k,j,i)+km(k-1,j,i)+km(k,j-1,i)+km(k-1,j-1,i) ) |
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| 378 | |
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| 379 | tend(k,j,i) = tend(k,j,i) & |
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| 380 | & - ( kmzm * ( w(k-1,j,i) - w(k-1,j-1,i) ) * ddy & |
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| 381 | & ) * ddzw(k) & |
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| 382 | & + ( -vswst(j,i) & |
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| 383 | & - kmzm * ( v(k,j,i) - v(k-1,j,i) ) * ddzu(k) & |
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| 384 | & ) * ddzw(k) |
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| 385 | ENDIF |
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| 386 | |
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| [1] | 387 | END SUBROUTINE diffusion_v_ij |
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| 388 | |
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| 389 | END MODULE diffusion_v_mod |
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