1 | MODULE diffusion_u_mod |
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2 | |
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3 | !------------------------------------------------------------------------------! |
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4 | ! Current revisions: |
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5 | ! ----------------- |
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6 | ! |
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7 | ! |
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8 | ! Former revisions: |
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9 | ! ----------------- |
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10 | ! $Id: diffusion_u.f90 484 2010-02-05 07:36:54Z weinreis $ |
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11 | ! |
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12 | ! 366 2009-08-25 08:06:27Z raasch |
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13 | ! bc_ns replaced by bc_ns_cyc |
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14 | ! |
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15 | ! 106 2007-08-16 14:30:26Z raasch |
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16 | ! Momentumflux at top (uswst) included as boundary condition, |
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17 | ! i loop is starting from nxlu (needed for non-cyclic boundary conditions) |
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18 | ! |
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19 | ! 75 2007-03-22 09:54:05Z raasch |
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20 | ! Wall functions now include diabatic conditions, call of routine wall_fluxes, |
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21 | ! z0 removed from argument list, uxrp eliminated |
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22 | ! |
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23 | ! 20 2007-02-26 00:12:32Z raasch |
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24 | ! Bugfix: ddzw dimensioned 1:nzt"+1" |
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25 | ! |
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26 | ! RCS Log replace by Id keyword, revision history cleaned up |
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27 | ! |
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28 | ! Revision 1.15 2006/02/23 10:35:35 raasch |
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29 | ! nzb_2d replaced by nzb_u_outer in horizontal diffusion and by nzb_u_inner |
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30 | ! or nzb_diff_u, respectively, in vertical diffusion, |
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31 | ! wall functions added for north and south walls, +z0 in argument list, |
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32 | ! terms containing w(k-1,..) are removed from the Prandtl-layer equation |
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33 | ! because they cause errors at the edges of topography |
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34 | ! WARNING: loops containing the MAX function are still not properly vectorized! |
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35 | ! |
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36 | ! Revision 1.1 1997/09/12 06:23:51 raasch |
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37 | ! Initial revision |
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38 | ! |
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39 | ! |
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40 | ! Description: |
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41 | ! ------------ |
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42 | ! Diffusion term of the u-component |
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43 | ! To do: additional damping (needed for non-cyclic bc) causes bad vectorization |
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44 | ! and slows down the speed on NEC about 5-10% |
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45 | !------------------------------------------------------------------------------! |
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46 | |
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47 | USE wall_fluxes_mod |
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48 | |
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49 | PRIVATE |
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50 | PUBLIC diffusion_u |
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51 | |
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52 | INTERFACE diffusion_u |
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53 | MODULE PROCEDURE diffusion_u |
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54 | MODULE PROCEDURE diffusion_u_ij |
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55 | END INTERFACE diffusion_u |
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56 | |
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57 | CONTAINS |
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58 | |
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59 | |
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60 | !------------------------------------------------------------------------------! |
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61 | ! Call for all grid points |
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62 | !------------------------------------------------------------------------------! |
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63 | SUBROUTINE diffusion_u( ddzu, ddzw, km, km_damp_y, tend, u, usws, uswst, & |
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64 | v, w ) |
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65 | |
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66 | USE control_parameters |
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67 | USE grid_variables |
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68 | USE indices |
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69 | |
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70 | IMPLICIT NONE |
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71 | |
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72 | INTEGER :: i, j, k |
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73 | REAL :: kmym_x, kmym_y, kmyp_x, kmyp_y, kmzm, kmzp |
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74 | REAL :: ddzu(1:nzt+1), ddzw(1:nzt+1), km_damp_y(nys-1:nyn+1) |
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75 | REAL :: tend(nzb:nzt+1,nys-1:nyn+1,nxl-1:nxr+1) |
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76 | REAL, DIMENSION(:,:), POINTER :: usws, uswst |
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77 | REAL, DIMENSION(:,:,:), POINTER :: km, u, v, w |
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78 | REAL, DIMENSION(nzb:nzt+1,nys:nyn,nxl:nxr) :: usvs |
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79 | |
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80 | ! |
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81 | !-- First calculate horizontal momentum flux u'v' at vertical walls, |
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82 | !-- if neccessary |
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83 | IF ( topography /= 'flat' ) THEN |
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84 | CALL wall_fluxes( usvs, 1.0, 0.0, 0.0, 0.0, nzb_u_inner, & |
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85 | nzb_u_outer, wall_u ) |
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86 | ENDIF |
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87 | |
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88 | DO i = nxlu, nxr |
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89 | DO j = nys,nyn |
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90 | ! |
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91 | !-- Compute horizontal diffusion |
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92 | DO k = nzb_u_outer(j,i)+1, nzt |
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93 | ! |
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94 | !-- Interpolate eddy diffusivities on staggered gridpoints |
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95 | kmyp_x = 0.25 * & |
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96 | ( km(k,j,i)+km(k,j+1,i)+km(k,j,i-1)+km(k,j+1,i-1) ) |
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97 | kmym_x = 0.25 * & |
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98 | ( km(k,j,i)+km(k,j-1,i)+km(k,j,i-1)+km(k,j-1,i-1) ) |
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99 | kmyp_y = kmyp_x |
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100 | kmym_y = kmym_x |
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101 | ! |
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102 | !-- Increase diffusion at the outflow boundary in case of |
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103 | !-- non-cyclic lateral boundaries. Damping is only needed for |
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104 | !-- velocity components parallel to the outflow boundary in |
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105 | !-- the direction normal to the outflow boundary. |
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106 | IF ( .NOT. bc_ns_cyc ) THEN |
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107 | kmyp_y = MAX( kmyp_y, km_damp_y(j) ) |
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108 | kmym_y = MAX( kmym_y, km_damp_y(j) ) |
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109 | ENDIF |
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110 | |
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111 | tend(k,j,i) = tend(k,j,i) & |
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112 | & + 2.0 * ( & |
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113 | & km(k,j,i) * ( u(k,j,i+1) - u(k,j,i) ) & |
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114 | & - km(k,j,i-1) * ( u(k,j,i) - u(k,j,i-1) ) & |
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115 | & ) * ddx2 & |
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116 | & + ( kmyp_y * ( u(k,j+1,i) - u(k,j,i) ) * ddy & |
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117 | & + kmyp_x * ( v(k,j+1,i) - v(k,j+1,i-1) ) * ddx & |
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118 | & - kmym_y * ( u(k,j,i) - u(k,j-1,i) ) * ddy & |
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119 | & - kmym_x * ( v(k,j,i) - v(k,j,i-1) ) * ddx & |
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120 | & ) * ddy |
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121 | ENDDO |
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122 | |
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123 | ! |
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124 | !-- Wall functions at the north and south walls, respectively |
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125 | IF ( wall_u(j,i) /= 0.0 ) THEN |
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126 | |
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127 | DO k = nzb_u_inner(j,i)+1, nzb_u_outer(j,i) |
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128 | kmyp_x = 0.25 * & |
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129 | ( km(k,j,i)+km(k,j+1,i)+km(k,j,i-1)+km(k,j+1,i-1) ) |
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130 | kmym_x = 0.25 * & |
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131 | ( km(k,j,i)+km(k,j-1,i)+km(k,j,i-1)+km(k,j-1,i-1) ) |
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132 | kmyp_y = kmyp_x |
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133 | kmym_y = kmym_x |
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134 | ! |
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135 | !-- Increase diffusion at the outflow boundary in case of |
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136 | !-- non-cyclic lateral boundaries. Damping is only needed for |
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137 | !-- velocity components parallel to the outflow boundary in |
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138 | !-- the direction normal to the outflow boundary. |
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139 | IF ( .NOT. bc_ns_cyc ) THEN |
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140 | kmyp_y = MAX( kmyp_y, km_damp_y(j) ) |
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141 | kmym_y = MAX( kmym_y, km_damp_y(j) ) |
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142 | ENDIF |
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143 | |
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144 | tend(k,j,i) = tend(k,j,i) & |
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145 | + 2.0 * ( & |
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146 | km(k,j,i) * ( u(k,j,i+1) - u(k,j,i) ) & |
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147 | - km(k,j,i-1) * ( u(k,j,i) - u(k,j,i-1) ) & |
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148 | ) * ddx2 & |
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149 | + ( fyp(j,i) * ( & |
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150 | kmyp_y * ( u(k,j+1,i) - u(k,j,i) ) * ddy & |
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151 | + kmyp_x * ( v(k,j+1,i) - v(k,j+1,i-1) ) * ddx & |
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152 | ) & |
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153 | - fym(j,i) * ( & |
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154 | kmym_y * ( u(k,j,i) - u(k,j-1,i) ) * ddy & |
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155 | + kmym_x * ( v(k,j,i) - v(k,j,i-1) ) * ddx & |
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156 | ) & |
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157 | + wall_u(j,i) * usvs(k,j,i) & |
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158 | ) * ddy |
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159 | ENDDO |
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160 | ENDIF |
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161 | |
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162 | ! |
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163 | !-- Compute vertical diffusion. In case of simulating a Prandtl layer, |
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164 | !-- index k starts at nzb_u_inner+2. |
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165 | DO k = nzb_diff_u(j,i), nzt_diff |
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166 | ! |
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167 | !-- Interpolate eddy diffusivities on staggered gridpoints |
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168 | kmzp = 0.25 * & |
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169 | ( km(k,j,i)+km(k+1,j,i)+km(k,j,i-1)+km(k+1,j,i-1) ) |
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170 | kmzm = 0.25 * & |
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171 | ( km(k,j,i)+km(k-1,j,i)+km(k,j,i-1)+km(k-1,j,i-1) ) |
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172 | |
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173 | tend(k,j,i) = tend(k,j,i) & |
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174 | & + ( kmzp * ( ( u(k+1,j,i) - u(k,j,i) ) * ddzu(k+1) & |
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175 | & + ( w(k,j,i) - w(k,j,i-1) ) * ddx & |
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176 | & ) & |
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177 | & - kmzm * ( ( u(k,j,i) - u(k-1,j,i) ) * ddzu(k) & |
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178 | & + ( w(k-1,j,i) - w(k-1,j,i-1) ) * ddx & |
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179 | & ) & |
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180 | & ) * ddzw(k) |
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181 | ENDDO |
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182 | |
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183 | ! |
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184 | !-- Vertical diffusion at the first grid point above the surface, |
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185 | !-- if the momentum flux at the bottom is given by the Prandtl law or |
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186 | !-- if it is prescribed by the user. |
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187 | !-- Difference quotient of the momentum flux is not formed over half |
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188 | !-- of the grid spacing (2.0*ddzw(k)) any more, since the comparison |
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189 | !-- with other (LES) modell showed that the values of the momentum |
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190 | !-- flux becomes too large in this case. |
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191 | !-- The term containing w(k-1,..) (see above equation) is removed here |
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192 | !-- because the vertical velocity is assumed to be zero at the surface. |
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193 | IF ( use_surface_fluxes ) THEN |
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194 | k = nzb_u_inner(j,i)+1 |
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195 | ! |
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196 | !-- Interpolate eddy diffusivities on staggered gridpoints |
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197 | kmzp = 0.25 * & |
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198 | ( km(k,j,i)+km(k+1,j,i)+km(k,j,i-1)+km(k+1,j,i-1) ) |
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199 | kmzm = 0.25 * & |
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200 | ( km(k,j,i)+km(k-1,j,i)+km(k,j,i-1)+km(k-1,j,i-1) ) |
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201 | |
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202 | tend(k,j,i) = tend(k,j,i) & |
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203 | & + ( kmzp * ( w(k,j,i) - w(k,j,i-1) ) * ddx & |
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204 | & ) * ddzw(k) & |
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205 | & + ( kmzp * ( u(k+1,j,i) - u(k,j,i) ) * ddzu(k+1) & |
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206 | & + usws(j,i) & |
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207 | & ) * ddzw(k) |
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208 | ENDIF |
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209 | |
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210 | ! |
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211 | !-- Vertical diffusion at the first gridpoint below the top boundary, |
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212 | !-- if the momentum flux at the top is prescribed by the user |
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213 | IF ( use_top_fluxes .AND. constant_top_momentumflux ) THEN |
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214 | k = nzt |
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215 | ! |
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216 | !-- Interpolate eddy diffusivities on staggered gridpoints |
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217 | kmzp = 0.25 * & |
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218 | ( km(k,j,i)+km(k+1,j,i)+km(k,j,i-1)+km(k+1,j,i-1) ) |
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219 | kmzm = 0.25 * & |
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220 | ( km(k,j,i)+km(k-1,j,i)+km(k,j,i-1)+km(k-1,j,i-1) ) |
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221 | |
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222 | tend(k,j,i) = tend(k,j,i) & |
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223 | & - ( kmzm * ( w(k-1,j,i) - w(k-1,j,i-1) ) * ddx & |
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224 | & ) * ddzw(k) & |
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225 | & + ( -uswst(j,i) & |
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226 | & - kmzm * ( u(k,j,i) - u(k-1,j,i) ) * ddzu(k) & |
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227 | & ) * ddzw(k) |
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228 | ENDIF |
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229 | |
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230 | ENDDO |
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231 | ENDDO |
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232 | |
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233 | END SUBROUTINE diffusion_u |
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234 | |
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235 | |
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236 | !------------------------------------------------------------------------------! |
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237 | ! Call for grid point i,j |
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238 | !------------------------------------------------------------------------------! |
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239 | SUBROUTINE diffusion_u_ij( i, j, ddzu, ddzw, km, km_damp_y, tend, u, usws, & |
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240 | uswst, v, w ) |
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241 | |
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242 | USE control_parameters |
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243 | USE grid_variables |
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244 | USE indices |
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245 | |
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246 | IMPLICIT NONE |
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247 | |
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248 | INTEGER :: i, j, k |
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249 | REAL :: kmym_x, kmym_y, kmyp_x, kmyp_y, kmzm, kmzp |
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250 | REAL :: ddzu(1:nzt+1), ddzw(1:nzt+1), km_damp_y(nys-1:nyn+1) |
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251 | REAL :: tend(nzb:nzt+1,nys-1:nyn+1,nxl-1:nxr+1) |
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252 | REAL, DIMENSION(nzb:nzt+1) :: usvs |
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253 | REAL, DIMENSION(:,:), POINTER :: usws, uswst |
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254 | REAL, DIMENSION(:,:,:), POINTER :: km, u, v, w |
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255 | |
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256 | ! |
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257 | !-- Compute horizontal diffusion |
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258 | DO k = nzb_u_outer(j,i)+1, nzt |
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259 | ! |
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260 | !-- Interpolate eddy diffusivities on staggered gridpoints |
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261 | kmyp_x = 0.25 * ( km(k,j,i)+km(k,j+1,i)+km(k,j,i-1)+km(k,j+1,i-1) ) |
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262 | kmym_x = 0.25 * ( km(k,j,i)+km(k,j-1,i)+km(k,j,i-1)+km(k,j-1,i-1) ) |
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263 | kmyp_y = kmyp_x |
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264 | kmym_y = kmym_x |
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265 | |
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266 | ! |
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267 | !-- Increase diffusion at the outflow boundary in case of non-cyclic |
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268 | !-- lateral boundaries. Damping is only needed for velocity components |
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269 | !-- parallel to the outflow boundary in the direction normal to the |
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270 | !-- outflow boundary. |
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271 | IF ( .NOT. bc_ns_cyc ) THEN |
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272 | kmyp_y = MAX( kmyp_y, km_damp_y(j) ) |
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273 | kmym_y = MAX( kmym_y, km_damp_y(j) ) |
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274 | ENDIF |
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275 | |
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276 | tend(k,j,i) = tend(k,j,i) & |
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277 | & + 2.0 * ( & |
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278 | & km(k,j,i) * ( u(k,j,i+1) - u(k,j,i) ) & |
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279 | & - km(k,j,i-1) * ( u(k,j,i) - u(k,j,i-1) ) & |
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280 | & ) * ddx2 & |
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281 | & + ( kmyp_y * ( u(k,j+1,i) - u(k,j,i) ) * ddy & |
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282 | & + kmyp_x * ( v(k,j+1,i) - v(k,j+1,i-1) ) * ddx & |
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283 | & - kmym_y * ( u(k,j,i) - u(k,j-1,i) ) * ddy & |
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284 | & - kmym_x * ( v(k,j,i) - v(k,j,i-1) ) * ddx & |
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285 | & ) * ddy |
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286 | ENDDO |
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287 | |
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288 | ! |
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289 | !-- Wall functions at the north and south walls, respectively |
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290 | IF ( wall_u(j,i) .NE. 0.0 ) THEN |
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291 | |
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292 | ! |
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293 | !-- Calculate the horizontal momentum flux u'v' |
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294 | CALL wall_fluxes( i, j, nzb_u_inner(j,i)+1, nzb_u_outer(j,i), & |
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295 | usvs, 1.0, 0.0, 0.0, 0.0 ) |
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296 | |
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297 | DO k = nzb_u_inner(j,i)+1, nzb_u_outer(j,i) |
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298 | kmyp_x = 0.25 * ( km(k,j,i)+km(k,j+1,i)+km(k,j,i-1)+km(k,j+1,i-1) ) |
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299 | kmym_x = 0.25 * ( km(k,j,i)+km(k,j-1,i)+km(k,j,i-1)+km(k,j-1,i-1) ) |
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300 | kmyp_y = kmyp_x |
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301 | kmym_y = kmym_x |
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302 | ! |
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303 | !-- Increase diffusion at the outflow boundary in case of |
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304 | !-- non-cyclic lateral boundaries. Damping is only needed for |
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305 | !-- velocity components parallel to the outflow boundary in |
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306 | !-- the direction normal to the outflow boundary. |
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307 | IF ( .NOT. bc_ns_cyc ) THEN |
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308 | kmyp_y = MAX( kmyp_y, km_damp_y(j) ) |
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309 | kmym_y = MAX( kmym_y, km_damp_y(j) ) |
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310 | ENDIF |
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311 | |
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312 | tend(k,j,i) = tend(k,j,i) & |
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313 | + 2.0 * ( & |
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314 | km(k,j,i) * ( u(k,j,i+1) - u(k,j,i) ) & |
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315 | - km(k,j,i-1) * ( u(k,j,i) - u(k,j,i-1) ) & |
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316 | ) * ddx2 & |
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317 | + ( fyp(j,i) * ( & |
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318 | kmyp_y * ( u(k,j+1,i) - u(k,j,i) ) * ddy & |
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319 | + kmyp_x * ( v(k,j+1,i) - v(k,j+1,i-1) ) * ddx & |
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320 | ) & |
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321 | - fym(j,i) * ( & |
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322 | kmym_y * ( u(k,j,i) - u(k,j-1,i) ) * ddy & |
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323 | + kmym_x * ( v(k,j,i) - v(k,j,i-1) ) * ddx & |
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324 | ) & |
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325 | + wall_u(j,i) * usvs(k) & |
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326 | ) * ddy |
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327 | ENDDO |
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328 | ENDIF |
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329 | |
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330 | ! |
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331 | !-- Compute vertical diffusion. In case of simulating a Prandtl layer, |
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332 | !-- index k starts at nzb_u_inner+2. |
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333 | DO k = nzb_diff_u(j,i), nzt_diff |
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334 | ! |
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335 | !-- Interpolate eddy diffusivities on staggered gridpoints |
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336 | kmzp = 0.25 * ( km(k,j,i)+km(k+1,j,i)+km(k,j,i-1)+km(k+1,j,i-1) ) |
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337 | kmzm = 0.25 * ( km(k,j,i)+km(k-1,j,i)+km(k,j,i-1)+km(k-1,j,i-1) ) |
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338 | |
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339 | tend(k,j,i) = tend(k,j,i) & |
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340 | & + ( kmzp * ( ( u(k+1,j,i) - u(k,j,i) ) * ddzu(k+1) & |
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341 | & + ( w(k,j,i) - w(k,j,i-1) ) * ddx & |
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342 | & ) & |
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343 | & - kmzm * ( ( u(k,j,i) - u(k-1,j,i) ) * ddzu(k) & |
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344 | & + ( w(k-1,j,i) - w(k-1,j,i-1) ) * ddx & |
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345 | & ) & |
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346 | & ) * ddzw(k) |
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347 | ENDDO |
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348 | |
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349 | ! |
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350 | !-- Vertical diffusion at the first grid point above the surface, if the |
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351 | !-- momentum flux at the bottom is given by the Prandtl law or if it is |
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352 | !-- prescribed by the user. |
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353 | !-- Difference quotient of the momentum flux is not formed over half of |
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354 | !-- the grid spacing (2.0*ddzw(k)) any more, since the comparison with |
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355 | !-- other (LES) modell showed that the values of the momentum flux becomes |
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356 | !-- too large in this case. |
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357 | !-- The term containing w(k-1,..) (see above equation) is removed here |
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358 | !-- because the vertical velocity is assumed to be zero at the surface. |
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359 | IF ( use_surface_fluxes ) THEN |
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360 | k = nzb_u_inner(j,i)+1 |
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361 | ! |
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362 | !-- Interpolate eddy diffusivities on staggered gridpoints |
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363 | kmzp = 0.25 * ( km(k,j,i)+km(k+1,j,i)+km(k,j,i-1)+km(k+1,j,i-1) ) |
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364 | kmzm = 0.25 * ( km(k,j,i)+km(k-1,j,i)+km(k,j,i-1)+km(k-1,j,i-1) ) |
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365 | |
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366 | tend(k,j,i) = tend(k,j,i) & |
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367 | & + ( kmzp * ( w(k,j,i) - w(k,j,i-1) ) * ddx & |
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368 | & ) * ddzw(k) & |
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369 | & + ( kmzp * ( u(k+1,j,i) - u(k,j,i) ) * ddzu(k+1) & |
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370 | & + usws(j,i) & |
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371 | & ) * ddzw(k) |
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372 | ENDIF |
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373 | |
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374 | ! |
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375 | !-- Vertical diffusion at the first gridpoint below the top boundary, |
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376 | !-- if the momentum flux at the top is prescribed by the user |
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377 | IF ( use_top_fluxes .AND. constant_top_momentumflux ) THEN |
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378 | k = nzt |
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379 | ! |
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380 | !-- Interpolate eddy diffusivities on staggered gridpoints |
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381 | kmzp = 0.25 * & |
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382 | ( km(k,j,i)+km(k+1,j,i)+km(k,j,i-1)+km(k+1,j,i-1) ) |
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383 | kmzm = 0.25 * & |
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384 | ( km(k,j,i)+km(k-1,j,i)+km(k,j,i-1)+km(k-1,j,i-1) ) |
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385 | |
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386 | tend(k,j,i) = tend(k,j,i) & |
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387 | & - ( kmzm * ( w(k-1,j,i) - w(k-1,j,i-1) ) * ddx & |
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388 | & ) * ddzw(k) & |
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389 | & + ( -uswst(j,i) & |
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390 | & - kmzm * ( u(k,j,i) - u(k-1,j,i) ) * ddzu(k) & |
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391 | & ) * ddzw(k) |
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392 | ENDIF |
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393 | |
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394 | END SUBROUTINE diffusion_u_ij |
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395 | |
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396 | END MODULE diffusion_u_mod |
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