1 | MODULE limthd_dh |
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2 | !!====================================================================== |
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3 | !! *** MODULE limthd_dh *** |
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4 | !! LIM-3 : thermodynamic growth and decay of the ice |
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5 | !!====================================================================== |
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6 | !! History : LIM ! 2003-05 (M. Vancoppenolle) Original code in 1D |
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7 | !! ! 2005-06 (M. Vancoppenolle) 3D version |
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8 | !! 3.2 ! 2009-07 (M. Vancoppenolle, Y. Aksenov, G. Madec) bug correction in rdmsnif & rdmicif |
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9 | !! 4.0 ! 2011-02 (G. Madec) dynamical allocation |
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10 | !!---------------------------------------------------------------------- |
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11 | #if defined key_lim3 |
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12 | !!---------------------------------------------------------------------- |
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13 | !! 'key_lim3' LIM3 sea-ice model |
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14 | !!---------------------------------------------------------------------- |
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15 | !! lim_thd_dh : vertical accr./abl. and lateral ablation of sea ice |
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16 | !!---------------------------------------------------------------------- |
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17 | USE par_oce ! ocean parameters |
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18 | USE phycst ! physical constants (OCE directory) |
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19 | USE sbc_oce ! Surface boundary condition: ocean fields |
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20 | USE ice ! LIM variables |
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21 | USE par_ice ! LIM parameters |
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22 | USE thd_ice ! LIM thermodynamics |
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23 | USE in_out_manager ! I/O manager |
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24 | USE lib_mpp ! MPP library |
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25 | USE wrk_nemo ! work arrays |
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26 | USE lib_fortran ! Fortran utilities (allows no signed zero when 'key_nosignedzero' defined) |
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27 | |
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28 | IMPLICIT NONE |
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29 | PRIVATE |
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30 | |
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31 | PUBLIC lim_thd_dh ! called by lim_thd |
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32 | |
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33 | REAL(wp) :: epsi20 = 1e-20 ! constant values |
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34 | REAL(wp) :: epsi13 = 1e-13 ! |
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35 | REAL(wp) :: epsi16 = 1e-16 ! |
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36 | REAL(wp) :: zzero = 0.e0 ! |
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37 | REAL(wp) :: zone = 1.e0 ! |
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38 | |
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39 | !!---------------------------------------------------------------------- |
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40 | !! NEMO/LIM3 3.4 , UCL - NEMO Consortium (2010) |
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41 | !! $Id$ |
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42 | !! Software governed by the CeCILL licence (NEMOGCM/NEMO_CeCILL.txt) |
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43 | !!---------------------------------------------------------------------- |
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44 | CONTAINS |
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45 | |
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46 | SUBROUTINE lim_thd_dh( kideb, kiut, jl ) |
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47 | !!------------------------------------------------------------------ |
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48 | !! *** ROUTINE lim_thd_dh *** |
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49 | !! |
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50 | !! ** Purpose : determines variations of ice and snow thicknesses. |
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51 | !! |
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52 | !! ** Method : Ice/Snow surface melting arises from imbalance in surface fluxes |
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53 | !! Bottom accretion/ablation arises from flux budget |
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54 | !! Snow thickness can increase by precipitation and decrease by sublimation |
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55 | !! If snow load excesses Archmiede limit, snow-ice is formed by |
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56 | !! the flooding of sea-water in the snow |
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57 | !! |
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58 | !! 1) Compute available flux of heat for surface ablation |
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59 | !! 2) Compute snow and sea ice enthalpies |
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60 | !! 3) Surface ablation and sublimation |
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61 | !! 4) Bottom accretion/ablation |
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62 | !! 5) Case of Total ablation |
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63 | !! 6) Snow ice formation |
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64 | !! |
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65 | !! References : Bitz and Lipscomb, 1999, J. Geophys. Res. |
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66 | !! Fichefet T. and M. Maqueda 1997, J. Geophys. Res., 102(C6), 12609-12646 |
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67 | !! Vancoppenolle, Fichefet and Bitz, 2005, Geophys. Res. Let. |
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68 | !! Vancoppenolle et al.,2009, Ocean Modelling |
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69 | !!------------------------------------------------------------------ |
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70 | INTEGER , INTENT(in) :: kideb, kiut ! Start/End point on which the the computation is applied |
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71 | INTEGER , INTENT(in) :: jl ! Thickness cateogry number |
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72 | !! |
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73 | INTEGER :: ji , jk ! dummy loop indices |
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74 | INTEGER :: zji, zjj ! 2D corresponding indices to ji |
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75 | INTEGER :: isnow ! switch for presence (1) or absence (0) of snow |
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76 | INTEGER :: isnowic ! snow ice formation not |
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77 | INTEGER :: i_ice_switch ! ice thickness above a certain treshold or not |
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78 | INTEGER :: iter |
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79 | |
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80 | REAL(wp) :: zzfmass_i, zihgnew ! local scalar |
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81 | REAL(wp) :: zzfmass_s, zhsnew, ztmelts ! local scalar |
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82 | REAL(wp) :: zhn, zdhcf, zdhbf, zhni, zhnfi, zihg ! |
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83 | REAL(wp) :: zdhnm, zhnnew, zhisn, zihic, zzc ! |
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84 | REAL(wp) :: zfracs ! fractionation coefficient for bottom salt entrapment |
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85 | REAL(wp) :: zds ! increment of bottom ice salinity |
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86 | REAL(wp) :: zcoeff ! dummy argument for snowfall partitioning over ice and leads |
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87 | REAL(wp) :: zsm_snowice ! snow-ice salinity |
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88 | REAL(wp) :: zswi1 ! switch for computation of bottom salinity |
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89 | REAL(wp) :: zswi12 ! switch for computation of bottom salinity |
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90 | REAL(wp) :: zswi2 ! switch for computation of bottom salinity |
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91 | REAL(wp) :: zgrr ! bottom growth rate |
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92 | REAL(wp) :: ztform ! bottom formation temperature |
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93 | ! |
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94 | REAL(wp), POINTER, DIMENSION(:) :: zh_i ! ice layer thickness |
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95 | REAL(wp), POINTER, DIMENSION(:) :: zh_s ! snow layer thickness |
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96 | REAL(wp), POINTER, DIMENSION(:) :: ztfs ! melting point |
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97 | REAL(wp), POINTER, DIMENSION(:) :: zhsold ! old snow thickness |
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98 | REAL(wp), POINTER, DIMENSION(:) :: zqprec ! energy of fallen snow |
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99 | REAL(wp), POINTER, DIMENSION(:) :: zqfont_su ! incoming, remaining surface energy |
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100 | REAL(wp), POINTER, DIMENSION(:) :: zqfont_bo ! incoming, bottom energy |
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101 | REAL(wp), POINTER, DIMENSION(:) :: z_f_surf ! surface heat for ablation |
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102 | REAL(wp), POINTER, DIMENSION(:) :: zhgnew ! new ice thickness |
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103 | REAL(wp), POINTER, DIMENSION(:) :: zfmass_i ! |
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104 | |
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105 | REAL(wp), POINTER, DIMENSION(:) :: zdh_s_mel ! snow melt |
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106 | REAL(wp), POINTER, DIMENSION(:) :: zdh_s_pre ! snow precipitation |
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107 | REAL(wp), POINTER, DIMENSION(:) :: zdh_s_sub ! snow sublimation |
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108 | REAL(wp), POINTER, DIMENSION(:) :: zfsalt_melt ! salt flux due to ice melt |
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109 | |
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110 | REAL(wp), POINTER, DIMENSION(:,:) :: zdeltah |
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111 | |
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112 | ! Pathological cases |
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113 | REAL(wp), POINTER, DIMENSION(:) :: zfdt_init ! total incoming heat for ice melt |
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114 | REAL(wp), POINTER, DIMENSION(:) :: zfdt_final ! total remaing heat for ice melt |
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115 | REAL(wp), POINTER, DIMENSION(:) :: zqt_i ! total ice heat content |
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116 | REAL(wp), POINTER, DIMENSION(:) :: zqt_s ! total snow heat content |
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117 | REAL(wp), POINTER, DIMENSION(:) :: zqt_dummy ! dummy heat content |
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118 | |
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119 | REAL(wp), POINTER, DIMENSION(:,:) :: zqt_i_lay ! total ice heat content |
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120 | |
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121 | ! Heat conservation |
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122 | INTEGER :: num_iter_max, numce_dh |
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123 | REAL(wp) :: meance_dh |
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124 | REAL(wp), POINTER, DIMENSION(:) :: zinnermelt |
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125 | REAL(wp), POINTER, DIMENSION(:) :: zfbase, zdq_i |
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126 | !!------------------------------------------------------------------ |
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127 | |
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128 | CALL wrk_alloc( jpij, zh_i, zh_s, ztfs, zhsold, zqprec, zqfont_su, zqfont_bo, z_f_surf, zhgnew, zfmass_i ) |
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129 | CALL wrk_alloc( jpij, zdh_s_mel, zdh_s_pre, zdh_s_sub, zfsalt_melt, zfdt_init, zfdt_final, zqt_i, zqt_s, zqt_dummy ) |
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130 | CALL wrk_alloc( jpij, zinnermelt, zfbase, zdq_i ) |
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131 | CALL wrk_alloc( jpij, jkmax, zdeltah, zqt_i_lay ) |
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132 | |
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133 | zfsalt_melt(:) = 0._wp |
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134 | ftotal_fin(:) = 0._wp |
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135 | zfdt_init(:) = 0._wp |
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136 | zfdt_final(:) = 0._wp |
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137 | |
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138 | DO ji = kideb, kiut |
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139 | old_ht_i_b(ji) = ht_i_b(ji) |
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140 | old_ht_s_b(ji) = ht_s_b(ji) |
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141 | END DO |
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142 | ! |
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143 | !------------------------------------------------------------------------------! |
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144 | ! 1) Calculate available heat for surface ablation ! |
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145 | !------------------------------------------------------------------------------! |
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146 | ! |
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147 | DO ji = kideb, kiut |
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148 | isnow = INT( 1.0 - MAX ( 0.0 , SIGN ( 1.0 , - ht_s_b(ji) ) ) ) |
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149 | ztfs(ji) = isnow * rtt + ( 1.0 - isnow ) * rtt |
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150 | z_f_surf(ji) = qnsr_ice_1d(ji) + ( 1.0 - i0(ji) ) * qsr_ice_1d(ji) - fc_su(ji) |
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151 | z_f_surf(ji) = MAX( zzero , z_f_surf(ji) ) * MAX( zzero , SIGN( zone , t_su_b(ji) - ztfs(ji) ) ) |
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152 | zfdt_init(ji) = ( z_f_surf(ji) + MAX( fbif_1d(ji) + qlbbq_1d(ji) + fc_bo_i(ji),0.0 ) ) * rdt_ice |
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153 | END DO ! ji |
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154 | |
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155 | zqfont_su (:) = 0._wp |
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156 | zqfont_bo (:) = 0._wp |
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157 | dsm_i_se_1d(:) = 0._wp |
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158 | dsm_i_si_1d(:) = 0._wp |
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159 | ! |
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160 | !------------------------------------------------------------------------------! |
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161 | ! 2) Computing layer thicknesses and snow and sea-ice enthalpies. ! |
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162 | !------------------------------------------------------------------------------! |
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163 | ! |
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164 | DO ji = kideb, kiut ! Layer thickness |
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165 | zh_i(ji) = ht_i_b(ji) / nlay_i |
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166 | zh_s(ji) = ht_s_b(ji) / nlay_s |
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167 | END DO |
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168 | ! |
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169 | zqt_s(:) = 0._wp ! Total enthalpy of the snow |
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170 | DO jk = 1, nlay_s |
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171 | DO ji = kideb, kiut |
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172 | zqt_s(ji) = zqt_s(ji) + q_s_b(ji,jk) * ht_s_b(ji) / nlay_s |
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173 | END DO |
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174 | END DO |
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175 | ! |
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176 | zqt_i(:) = 0._wp ! Total enthalpy of the ice |
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177 | DO jk = 1, nlay_i |
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178 | DO ji = kideb, kiut |
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179 | zzc = q_i_b(ji,jk) * ht_i_b(ji) / nlay_i |
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180 | zqt_i(ji) = zqt_i(ji) + zzc |
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181 | zqt_i_lay(ji,jk) = zzc |
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182 | END DO |
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183 | END DO |
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184 | ! |
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185 | !------------------------------------------------------------------------------| |
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186 | ! 3) Surface ablation and sublimation | |
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187 | !------------------------------------------------------------------------------| |
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188 | ! |
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189 | !------------------------- |
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190 | ! 3.1 Snow precips / melt |
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191 | !------------------------- |
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192 | ! Snow accumulation in one thermodynamic time step |
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193 | ! snowfall is partitionned between leads and ice |
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194 | ! if snow fall was uniform, a fraction (1-at_i) would fall into leads |
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195 | ! but because of the winds, more snow falls on leads than on sea ice |
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196 | ! and a greater fraction (1-at_i)^beta of the total mass of snow |
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197 | ! (beta < 1) falls in leads. |
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198 | ! In reality, beta depends on wind speed, |
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199 | ! and should decrease with increasing wind speed but here, it is |
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200 | ! considered as a constant. an average value is 0.66 |
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201 | ! Martin Vancoppenolle, December 2006 |
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202 | |
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203 | ! Snow fall |
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204 | DO ji = kideb, kiut |
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205 | zcoeff = ( 1.0 - ( 1.0 - at_i_b(ji) )**betas ) / at_i_b(ji) |
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206 | zdh_s_pre(ji) = zcoeff * sprecip_1d(ji) * rdt_ice / rhosn |
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207 | END DO |
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208 | zdh_s_mel(:) = 0._wp |
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209 | |
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210 | ! Melt of fallen snow |
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211 | DO ji = kideb, kiut |
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212 | ! tatm_ice is now in K |
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213 | zqprec (ji) = rhosn * ( cpic * ( rtt - tatm_ice_1d(ji) ) + lfus ) |
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214 | zqfont_su(ji) = z_f_surf(ji) * rdt_ice |
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215 | zdeltah (ji,1) = MIN( 0.e0 , - zqfont_su(ji) / MAX( zqprec(ji) , epsi13 ) ) |
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216 | zqfont_su(ji) = MAX( 0.e0 , - zdh_s_pre(ji) - zdeltah(ji,1) ) * zqprec(ji) |
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217 | zdeltah (ji,1) = MAX( - zdh_s_pre(ji) , zdeltah(ji,1) ) |
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218 | zdh_s_mel(ji) = zdh_s_mel(ji) + zdeltah(ji,1) |
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219 | ! heat conservation |
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220 | qt_s_in(ji,jl) = qt_s_in(ji,jl) + zqprec(ji) * zdh_s_pre(ji) |
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221 | zqt_s (ji) = zqt_s (ji) + zqprec(ji) * zdh_s_pre(ji) |
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222 | zqt_s (ji) = MAX( zqt_s(ji) - zqfont_su(ji) , 0.e0 ) |
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223 | END DO |
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224 | |
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225 | |
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226 | ! Snow melt due to surface heat imbalance |
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227 | DO jk = 1, nlay_s |
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228 | DO ji = kideb, kiut |
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229 | zdeltah (ji,jk) = - zqfont_su(ji) / q_s_b(ji,jk) |
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230 | zqfont_su(ji) = MAX( 0.0 , - zh_s(ji) - zdeltah(ji,jk) ) * q_s_b(ji,jk) |
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231 | zdeltah (ji,jk) = MAX( zdeltah(ji,jk) , - zh_s(ji) ) |
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232 | zdh_s_mel(ji) = zdh_s_mel(ji) + zdeltah(ji,jk) ! resulting melt of snow |
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233 | END DO |
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234 | END DO |
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235 | |
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236 | ! Apply snow melt to snow depth |
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237 | DO ji = kideb, kiut |
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238 | dh_s_tot(ji) = zdh_s_mel(ji) + zdh_s_pre(ji) |
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239 | ! Old and new snow depths |
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240 | zhsold(ji) = ht_s_b(ji) |
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241 | zhsnew = ht_s_b(ji) + dh_s_tot(ji) |
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242 | ! If snow is still present zhn = 1, else zhn = 0 |
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243 | zhn = 1.0 - MAX( zzero , SIGN( zone , - zhsnew ) ) |
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244 | ht_s_b(ji) = MAX( zzero , zhsnew ) |
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245 | ! Volume and mass variations of snow |
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246 | dvsbq_1d (ji) = a_i_b(ji) * ( ht_s_b(ji) - zhsold(ji) - zdh_s_pre(ji) ) |
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247 | dvsbq_1d (ji) = MIN( zzero, dvsbq_1d(ji) ) |
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248 | rdmsnif_1d(ji) = rdmsnif_1d(ji) + rhosn * dvsbq_1d(ji) |
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249 | END DO ! ji |
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250 | |
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251 | !-------------------------- |
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252 | ! 3.2 Surface ice ablation |
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253 | !-------------------------- |
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254 | DO ji = kideb, kiut |
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255 | dh_i_surf(ji) = 0._wp |
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256 | z_f_surf (ji) = zqfont_su(ji) / rdt_ice ! heat conservation test |
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257 | zdq_i (ji) = 0._wp |
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258 | END DO ! ji |
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259 | |
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260 | DO jk = 1, nlay_i |
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261 | DO ji = kideb, kiut |
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262 | ! ! melt of layer jk |
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263 | zdeltah (ji,jk) = - zqfont_su(ji) / q_i_b(ji,jk) |
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264 | ! ! recompute heat available |
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265 | zqfont_su(ji) = MAX( 0.0 , - zh_i(ji) - zdeltah(ji,jk) ) * q_i_b(ji,jk) |
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266 | ! ! melt of layer jk cannot be higher than its thickness |
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267 | zdeltah (ji,jk) = MAX( zdeltah(ji,jk) , - zh_i(ji) ) |
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268 | ! ! update surface melt |
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269 | dh_i_surf(ji) = dh_i_surf(ji) + zdeltah(ji,jk) |
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270 | ! ! for energy conservation |
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271 | zdq_i (ji) = zdq_i(ji) + zdeltah(ji,jk) * q_i_b(ji,jk) / rdt_ice |
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272 | ! |
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273 | ! contribution to ice-ocean salt flux |
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274 | zji = MOD( npb(ji) - 1 , jpi ) + 1 |
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275 | zjj = ( npb(ji) - 1 ) / jpi + 1 |
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276 | zfsalt_melt(ji) = zfsalt_melt(ji) + ( sss_m(zji,zjj) - sm_i_b(ji) ) * a_i_b(ji) & |
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277 | & * MIN( zdeltah(ji,jk) , 0.e0 ) * rhoic / rdt_ice |
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278 | END DO |
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279 | END DO |
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280 | |
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281 | ! !------------------- |
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282 | IF( con_i ) THEN ! Conservation test |
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283 | ! !------------------- |
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284 | numce_dh = 0 |
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285 | meance_dh = 0._wp |
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286 | DO ji = kideb, kiut |
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287 | IF ( ( z_f_surf(ji) + zdq_i(ji) ) .GE. 1.0e-3 ) THEN |
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288 | numce_dh = numce_dh + 1 |
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289 | meance_dh = meance_dh + z_f_surf(ji) + zdq_i(ji) |
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290 | ENDIF |
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291 | IF( z_f_surf(ji) + zdq_i(ji) .GE. 1.0e-3 ) THEN! |
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292 | WRITE(numout,*) ' ALERTE heat loss for surface melt ' |
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293 | WRITE(numout,*) ' zji, zjj, jl :', zji, zjj, jl |
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294 | WRITE(numout,*) ' ht_i_b : ', ht_i_b(ji) |
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295 | WRITE(numout,*) ' z_f_surf : ', z_f_surf(ji) |
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296 | WRITE(numout,*) ' zdq_i : ', zdq_i(ji) |
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297 | WRITE(numout,*) ' ht_i_b : ', ht_i_b(ji) |
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298 | WRITE(numout,*) ' fc_bo_i : ', fc_bo_i(ji) |
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299 | WRITE(numout,*) ' fbif_1d : ', fbif_1d(ji) |
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300 | WRITE(numout,*) ' qlbbq_1d : ', qlbbq_1d(ji) |
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301 | WRITE(numout,*) ' s_i_new : ', s_i_new(ji) |
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302 | WRITE(numout,*) ' sss_m : ', sss_m(zji,zjj) |
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303 | ENDIF |
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304 | END DO |
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305 | ! |
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306 | IF( numce_dh > 0 ) meance_dh = meance_dh / numce_dh |
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307 | WRITE(numout,*) ' Error report - Category : ', jl |
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308 | WRITE(numout,*) ' ~~~~~~~~~~~~ ' |
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309 | WRITE(numout,*) ' Number of points where there is sur. me. error : ', numce_dh |
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310 | WRITE(numout,*) ' Mean basal growth error on error points : ', meance_dh |
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311 | ! |
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312 | ENDIF |
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313 | |
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314 | !---------------------- |
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315 | ! 3.3 Snow sublimation |
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316 | !---------------------- |
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317 | |
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318 | DO ji = kideb, kiut |
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319 | ! qla_ice is always >=0 (upwards), heat goes to the atmosphere, therefore snow sublimates |
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320 | #if defined key_coupled |
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321 | zdh_s_sub(ji) = 0._wp ! coupled mode: sublimation already included in emp_ice (to do in limsbc_ice) |
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322 | #else |
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323 | ! ! forced mode: snow thickness change due to sublimation |
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324 | zdh_s_sub(ji) = - parsub * qla_ice_1d(ji) / ( rhosn * lsub ) * rdt_ice |
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325 | #endif |
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326 | dh_s_tot (ji) = dh_s_tot(ji) + zdh_s_sub(ji) |
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327 | zdhcf = ht_s_b(ji) + zdh_s_sub(ji) |
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328 | ht_s_b (ji) = MAX( zzero , zdhcf ) |
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329 | ! we recompute dh_s_tot |
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330 | dh_s_tot (ji) = ht_s_b(ji) - zhsold(ji) |
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331 | qt_s_in (ji,jl) = qt_s_in(ji,jl) + zdh_s_sub(ji)*q_s_b(ji,1) |
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332 | END DO |
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333 | |
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334 | zqt_dummy(:) = 0.e0 |
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335 | DO jk = 1, nlay_s |
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336 | DO ji = kideb,kiut |
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337 | q_s_b (ji,jk) = rhosn * ( cpic * ( rtt - t_s_b(ji,jk) ) + lfus ) |
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338 | zqt_dummy(ji) = zqt_dummy(ji) + q_s_b(ji,jk) * ht_s_b(ji) / nlay_s ! heat conservation |
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339 | END DO |
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340 | END DO |
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341 | |
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342 | DO jk = 1, nlay_s |
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343 | DO ji = kideb, kiut |
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344 | ! In case of disparition of the snow, we have to update the snow temperatures |
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345 | zhisn = MAX( zzero , SIGN( zone, - ht_s_b(ji) ) ) |
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346 | t_s_b(ji,jk) = ( 1.0 - zhisn ) * t_s_b(ji,jk) + zhisn * rtt |
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347 | q_s_b(ji,jk) = ( 1.0 - zhisn ) * q_s_b(ji,jk) |
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348 | END DO |
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349 | END DO |
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350 | |
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351 | ! |
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352 | !------------------------------------------------------------------------------! |
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353 | ! 4) Basal growth / melt ! |
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354 | !------------------------------------------------------------------------------! |
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355 | ! |
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356 | ! Ice basal growth / melt is given by the ratio of heat budget over basal |
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357 | ! ice heat content. Basal heat budget is given by the difference between |
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358 | ! the inner conductive flux (fc_bo_i), from the open water heat flux |
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359 | ! (qlbbqb) and the turbulent ocean flux (fbif). |
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360 | ! fc_bo_i is positive downwards. fbif and qlbbq are positive to the ice |
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361 | |
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362 | !----------------------------------------------------- |
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363 | ! 4.1 Basal growth - (a) salinity not varying in time |
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364 | !----------------------------------------------------- |
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365 | IF( num_sal /= 2 .AND. num_sal /= 4 ) THEN |
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366 | DO ji = kideb, kiut |
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367 | IF( ( fc_bo_i(ji) + fbif_1d(ji) + qlbbq_1d(ji) ) < 0.0 ) THEN |
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368 | s_i_new(ji) = sm_i_b(ji) |
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369 | ! Melting point in K |
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370 | ztmelts = - tmut * s_i_new(ji) + rtt |
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371 | ! New ice heat content (Bitz and Lipscomb, 1999) |
---|
372 | ztform = t_i_b(ji,nlay_i) ! t_bo_b crashes in the |
---|
373 | ! Baltic |
---|
374 | q_i_b(ji,nlay_i+1) = rhoic * ( cpic * ( ztmelts - ztform ) & |
---|
375 | & + lfus * ( 1.0 - ( ztmelts - rtt ) / ( ztform - rtt ) ) & |
---|
376 | & - rcp * ( ztmelts - rtt ) ) |
---|
377 | ! Basal growth rate = - F*dt / q |
---|
378 | dh_i_bott(ji) = - rdt_ice*( fc_bo_i(ji) + fbif_1d(ji) + qlbbq_1d(ji) ) / q_i_b(ji,nlay_i+1) |
---|
379 | ENDIF |
---|
380 | END DO |
---|
381 | ENDIF |
---|
382 | |
---|
383 | !------------------------------------------------- |
---|
384 | ! 4.1 Basal growth - (b) salinity varying in time |
---|
385 | !------------------------------------------------- |
---|
386 | IF( num_sal == 2 .OR. num_sal == 4 ) THEN |
---|
387 | ! the growth rate (dh_i_bott) is function of the new ice |
---|
388 | ! heat content (q_i_b(nlay_i+1)). q_i_b depends on the new ice |
---|
389 | ! salinity (snewice). snewice depends on dh_i_bott |
---|
390 | ! it converges quickly, so, no problem |
---|
391 | ! See Vancoppenolle et al., OM08 for more info on this |
---|
392 | |
---|
393 | ! Initial value (tested 1D, can be anything between 1 and 20) |
---|
394 | num_iter_max = 4 |
---|
395 | s_i_new(:) = 4.0 |
---|
396 | |
---|
397 | ! Iterative procedure |
---|
398 | DO iter = 1, num_iter_max |
---|
399 | DO ji = kideb, kiut |
---|
400 | IF( fc_bo_i(ji) + fbif_1d(ji) + qlbbq_1d(ji) < 0.e0 ) THEN |
---|
401 | zji = MOD( npb(ji) - 1, jpi ) + 1 |
---|
402 | zjj = ( npb(ji) - 1 ) / jpi + 1 |
---|
403 | ! Melting point in K |
---|
404 | ztmelts = - tmut * s_i_new(ji) + rtt |
---|
405 | ! New ice heat content (Bitz and Lipscomb, 1999) |
---|
406 | q_i_b(ji,nlay_i+1) = rhoic * ( cpic * ( ztmelts - t_bo_b(ji) ) & |
---|
407 | & + lfus * ( 1.0 - ( ztmelts - rtt ) / ( t_bo_b(ji) - rtt ) ) & |
---|
408 | & - rcp * ( ztmelts-rtt ) ) |
---|
409 | ! Bottom growth rate = - F*dt / q |
---|
410 | dh_i_bott(ji) = - rdt_ice * ( fc_bo_i(ji) + fbif_1d(ji) + qlbbq_1d(ji) ) / q_i_b(ji,nlay_i+1) |
---|
411 | ! New ice salinity ( Cox and Weeks, JGR, 1988 ) |
---|
412 | ! zswi2 (1) if dh_i_bott/rdt .GT. 3.6e-7 |
---|
413 | ! zswi12 (1) if dh_i_bott/rdt .LT. 3.6e-7 and .GT. 2.0e-8 |
---|
414 | ! zswi1 (1) if dh_i_bott/rdt .LT. 2.0e-8 |
---|
415 | zgrr = MIN( 1.0e-3, MAX ( dh_i_bott(ji) / rdt_ice , epsi13 ) ) |
---|
416 | zswi2 = MAX( zzero , SIGN( zone , zgrr - 3.6e-7 ) ) |
---|
417 | zswi12 = MAX( zzero , SIGN( zone , zgrr - 2.0e-8 ) ) * ( 1.0 - zswi2 ) |
---|
418 | zswi1 = 1. - zswi2 * zswi12 |
---|
419 | zfracs = zswi1 * 0.12 + zswi12 * ( 0.8925 + 0.0568 * LOG( 100.0 * zgrr ) ) & |
---|
420 | & + zswi2 * 0.26 / ( 0.26 + 0.74 * EXP ( - 724300.0 * zgrr ) ) |
---|
421 | zds = zfracs * sss_m(zji,zjj) - s_i_new(ji) |
---|
422 | s_i_new(ji) = zfracs * sss_m(zji,zjj) |
---|
423 | ENDIF ! fc_bo_i |
---|
424 | END DO ! ji |
---|
425 | END DO ! iter |
---|
426 | |
---|
427 | ! Final values |
---|
428 | DO ji = kideb, kiut |
---|
429 | IF( ( fc_bo_i(ji) + fbif_1d(ji) + qlbbq_1d(ji) ) .LT. 0.0 ) THEN |
---|
430 | ! New ice salinity must not exceed 15 psu |
---|
431 | s_i_new(ji) = MIN( s_i_new(ji), s_i_max ) |
---|
432 | ! Metling point in K |
---|
433 | ztmelts = - tmut * s_i_new(ji) + rtt |
---|
434 | ! New ice heat content (Bitz and Lipscomb, 1999) |
---|
435 | q_i_b(ji,nlay_i+1) = rhoic * ( cpic * ( ztmelts - t_bo_b(ji) ) & |
---|
436 | & + lfus * ( 1.0 - ( ztmelts - rtt ) / ( t_bo_b(ji) - rtt ) ) & |
---|
437 | & - rcp * ( ztmelts - rtt ) ) |
---|
438 | ! Basal growth rate = - F*dt / q |
---|
439 | dh_i_bott(ji) = - rdt_ice*( fc_bo_i(ji) + fbif_1d(ji) + qlbbq_1d(ji) ) / q_i_b(ji,nlay_i+1) |
---|
440 | ! Salinity update |
---|
441 | ! entrapment during bottom growth |
---|
442 | dsm_i_se_1d(ji) = ( s_i_new(ji) * dh_i_bott(ji) + sm_i_b(ji) * ht_i_b(ji) ) & |
---|
443 | & / MAX( ht_i_b(ji) + dh_i_bott(ji) ,epsi13 ) - sm_i_b(ji) |
---|
444 | ENDIF ! heat budget |
---|
445 | END DO |
---|
446 | ENDIF |
---|
447 | |
---|
448 | !---------------- |
---|
449 | ! 4.2 Basal melt |
---|
450 | !---------------- |
---|
451 | meance_dh = 0._wp |
---|
452 | numce_dh = 0 |
---|
453 | zinnermelt(:) = 0._wp |
---|
454 | |
---|
455 | DO ji = kideb, kiut |
---|
456 | ! heat convergence at the surface > 0 |
---|
457 | IF( ( fc_bo_i(ji) + fbif_1d(ji) + qlbbq_1d(ji) ) >= 0._wp ) THEN |
---|
458 | s_i_new(ji) = s_i_b(ji,nlay_i) |
---|
459 | zqfont_bo(ji) = rdt_ice * ( fc_bo_i(ji) + fbif_1d(ji) + qlbbq_1d(ji) ) |
---|
460 | zfbase(ji) = zqfont_bo(ji) / rdt_ice ! heat conservation test |
---|
461 | zdq_i(ji) = 0._wp |
---|
462 | dh_i_bott(ji) = 0._wp |
---|
463 | ENDIF |
---|
464 | END DO |
---|
465 | |
---|
466 | DO jk = nlay_i, 1, -1 |
---|
467 | DO ji = kideb, kiut |
---|
468 | IF ( ( fc_bo_i(ji) + fbif_1d(ji) + qlbbq_1d(ji) ) .GE. 0.0 ) THEN |
---|
469 | ztmelts = - tmut * s_i_b(ji,jk) + rtt |
---|
470 | IF( t_i_b(ji,jk) >= ztmelts ) THEN |
---|
471 | zdeltah(ji,jk) = - zh_i(ji) |
---|
472 | dh_i_bott(ji) = dh_i_bott(ji) + zdeltah(ji,jk) |
---|
473 | zinnermelt(ji) = 1._wp |
---|
474 | ELSE ! normal ablation |
---|
475 | zdeltah(ji,jk) = - zqfont_bo(ji) / q_i_b(ji,jk) |
---|
476 | zqfont_bo(ji) = MAX( 0.0 , - zh_i(ji) - zdeltah(ji,jk) ) * q_i_b(ji,jk) |
---|
477 | zdeltah(ji,jk) = MAX(zdeltah(ji,jk), - zh_i(ji) ) |
---|
478 | dh_i_bott(ji) = dh_i_bott(ji) + zdeltah(ji,jk) |
---|
479 | zdq_i(ji) = zdq_i(ji) + zdeltah(ji,jk) * q_i_b(ji,jk) / rdt_ice |
---|
480 | ! contribution to salt flux |
---|
481 | zji = MOD( npb(ji) - 1, jpi ) + 1 |
---|
482 | zjj = ( npb(ji) - 1 ) / jpi + 1 |
---|
483 | zfsalt_melt(ji) = zfsalt_melt(ji) + ( sss_m(zji,zjj) - sm_i_b(ji) ) * a_i_b(ji) & |
---|
484 | & * MIN( zdeltah(ji,jk) , 0.0 ) * rhoic / rdt_ice |
---|
485 | ENDIF |
---|
486 | ENDIF |
---|
487 | END DO ! ji |
---|
488 | END DO ! jk |
---|
489 | |
---|
490 | ! !------------------- |
---|
491 | IF( con_i ) THEN ! Conservation test |
---|
492 | ! !------------------- |
---|
493 | DO ji = kideb, kiut |
---|
494 | IF( ( fc_bo_i(ji) + fbif_1d(ji) + qlbbq_1d(ji) ) >= 0.e0 ) THEN |
---|
495 | IF( ( zfbase(ji) + zdq_i(ji) ) >= 1.e-3 ) THEN |
---|
496 | numce_dh = numce_dh + 1 |
---|
497 | meance_dh = meance_dh + zfbase(ji) + zdq_i(ji) |
---|
498 | ENDIF |
---|
499 | IF ( zfbase(ji) + zdq_i(ji) .GE. 1.0e-3 ) THEN |
---|
500 | WRITE(numout,*) ' ALERTE heat loss for basal melt : zji, zjj, jl :', zji, zjj, jl |
---|
501 | WRITE(numout,*) ' ht_i_b : ', ht_i_b(ji) |
---|
502 | WRITE(numout,*) ' zfbase : ', zfbase(ji) |
---|
503 | WRITE(numout,*) ' zdq_i : ', zdq_i(ji) |
---|
504 | WRITE(numout,*) ' ht_i_b : ', ht_i_b(ji) |
---|
505 | WRITE(numout,*) ' fc_bo_i : ', fc_bo_i(ji) |
---|
506 | WRITE(numout,*) ' fbif_1d : ', fbif_1d(ji) |
---|
507 | WRITE(numout,*) ' qlbbq_1d : ', qlbbq_1d(ji) |
---|
508 | WRITE(numout,*) ' s_i_new : ', s_i_new(ji) |
---|
509 | WRITE(numout,*) ' sss_m : ', sss_m(zji,zjj) |
---|
510 | WRITE(numout,*) ' dh_i_bott : ', dh_i_bott(ji) |
---|
511 | WRITE(numout,*) ' innermelt : ', INT( zinnermelt(ji) ) |
---|
512 | ENDIF |
---|
513 | ENDIF |
---|
514 | END DO |
---|
515 | IF( numce_dh > 0 ) meance_dh = meance_dh / numce_dh |
---|
516 | WRITE(numout,*) ' Number of points where there is bas. me. error : ', numce_dh |
---|
517 | WRITE(numout,*) ' Mean basal melt error on error points : ', meance_dh |
---|
518 | WRITE(numout,*) ' Remaining bottom heat : ', zqfont_bo(jiindex_1d) |
---|
519 | ! |
---|
520 | ENDIF |
---|
521 | |
---|
522 | ! |
---|
523 | !------------------------------------------------------------------------------! |
---|
524 | ! 5) Pathological cases ! |
---|
525 | !------------------------------------------------------------------------------! |
---|
526 | ! |
---|
527 | !---------------------------------------------- |
---|
528 | ! 5.1 Excessive ablation in a 1-category model |
---|
529 | !---------------------------------------------- |
---|
530 | |
---|
531 | DO ji = kideb, kiut |
---|
532 | ! ! in a 1-category sea ice model, bottom ablation must not exceed hmelt (-0.15) |
---|
533 | IF( jpl == 1 ) THEN ; zdhbf = MAX( hmelt , dh_i_bott(ji) ) |
---|
534 | ELSE ; zdhbf = dh_i_bott(ji) |
---|
535 | ENDIF |
---|
536 | ! ! excessive energy is sent to lateral ablation |
---|
537 | fsup (ji) = rhoic * lfus * at_i_b(ji) / MAX( 1.0 - at_i_b(ji) , epsi13 ) & |
---|
538 | & * ( zdhbf - dh_i_bott(ji) ) / rdt_ice |
---|
539 | dh_i_bott(ji) = zdhbf |
---|
540 | ! !since ice volume is only used for outputs, we keep it global for all categories |
---|
541 | dvbbq_1d (ji) = a_i_b(ji) * dh_i_bott(ji) |
---|
542 | ! !new ice thickness |
---|
543 | zhgnew (ji) = ht_i_b(ji) + dh_i_surf(ji) + dh_i_bott(ji) |
---|
544 | ! ! diagnostic ( bottom ice growth ) |
---|
545 | zji = MOD( npb(ji) - 1, jpi ) + 1 |
---|
546 | zjj = ( npb(ji) - 1 ) / jpi + 1 |
---|
547 | diag_bot_gr(zji,zjj) = diag_bot_gr(zji,zjj) + MAX(dh_i_bott(ji),0.0)*a_i_b(ji) / rdt_ice |
---|
548 | diag_sur_me(zji,zjj) = diag_sur_me(zji,zjj) + MIN(dh_i_surf(ji),0.0)*a_i_b(ji) / rdt_ice |
---|
549 | diag_bot_me(zji,zjj) = diag_bot_me(zji,zjj) + MIN(dh_i_bott(ji),0.0)*a_i_b(ji) / rdt_ice |
---|
550 | END DO |
---|
551 | |
---|
552 | !----------------------------------- |
---|
553 | ! 5.2 More than available ice melts |
---|
554 | !----------------------------------- |
---|
555 | ! then heat applied minus heat content at previous time step |
---|
556 | ! should equal heat remaining |
---|
557 | ! |
---|
558 | DO ji = kideb, kiut |
---|
559 | ! Adapt the remaining energy if too much ice melts |
---|
560 | !-------------------------------------------------- |
---|
561 | zihgnew = 1.0 - MAX( zzero , SIGN( zone , - zhgnew(ji) ) ) !1 if ice |
---|
562 | ! 0 if no more ice |
---|
563 | zhgnew (ji) = zihgnew * zhgnew(ji) ! ice thickness is put to 0 |
---|
564 | ! remaining heat |
---|
565 | zfdt_final(ji) = ( 1.0 - zihgnew ) * ( zqfont_su(ji) + zqfont_bo(ji) ) |
---|
566 | |
---|
567 | ! If snow remains, energy is used to melt snow |
---|
568 | zhni = ht_s_b(ji) ! snow depth at previous time step |
---|
569 | zihg = MAX( zzero , SIGN ( zone , - ht_s_b(ji) ) ) ! 0 if snow |
---|
570 | |
---|
571 | ! energy of melting of remaining snow |
---|
572 | zqt_s(ji) = ( 1. - zihg ) * zqt_s(ji) / MAX( zhni, epsi13 ) |
---|
573 | zdhnm = - ( 1. - zihg ) * ( 1. - zihgnew ) * zfdt_final(ji) / MAX( zqt_s(ji) , epsi13 ) |
---|
574 | zhnfi = zhni + zdhnm |
---|
575 | zfdt_final(ji) = MAX( zfdt_final(ji) + zqt_s(ji) * zdhnm , 0.0 ) |
---|
576 | ht_s_b(ji) = MAX( zzero , zhnfi ) |
---|
577 | zqt_s(ji) = zqt_s(ji) * ht_s_b(ji) |
---|
578 | |
---|
579 | ! Mass variations of ice and snow |
---|
580 | !--------------------------------- |
---|
581 | ! ! mass variation of the jl category |
---|
582 | zzfmass_s = - a_i_b(ji) * ( zhni - ht_s_b(ji) ) * rhosn ! snow |
---|
583 | zzfmass_i = a_i_b(ji) * ( zhgnew(ji) - ht_i_b(ji) ) * rhoic ! ice |
---|
584 | ! |
---|
585 | zfmass_i(ji) = zzfmass_i ! ice variation saved to compute salt flux (see below) |
---|
586 | ! |
---|
587 | ! ! mass variation cumulated over category |
---|
588 | rdmsnif_1d(ji) = rdmsnif_1d(ji) + zzfmass_s ! snow |
---|
589 | rdmicif_1d(ji) = rdmicif_1d(ji) + zzfmass_i ! ice |
---|
590 | |
---|
591 | ! Remaining heat to the ocean |
---|
592 | !--------------------------------- |
---|
593 | focea(ji) = - zfdt_final(ji) / rdt_ice ! focea is in W.m-2 * dt |
---|
594 | |
---|
595 | END DO |
---|
596 | |
---|
597 | ftotal_fin (:) = zfdt_final(:) / rdt_ice |
---|
598 | |
---|
599 | !--------------------------- |
---|
600 | ! Salt flux and heat fluxes |
---|
601 | !--------------------------- |
---|
602 | DO ji = kideb, kiut |
---|
603 | zihgnew = 1.0 - MAX( zzero , SIGN( zone , - zhgnew(ji) ) ) !1 if ice |
---|
604 | |
---|
605 | ! Salt flux |
---|
606 | zji = MOD( npb(ji) - 1, jpi ) + 1 |
---|
607 | zjj = ( npb(ji) - 1 ) / jpi + 1 |
---|
608 | ! new lines |
---|
609 | IF( num_sal == 4 ) THEN |
---|
610 | fseqv_1d(ji) = fseqv_1d(ji) + zihgnew * zfsalt_melt(ji) & |
---|
611 | & + (1.0 - zihgnew) * zfmass_i(ji) * ( sss_m(zji,zjj) - bulk_sal ) / rdt_ice |
---|
612 | ELSE |
---|
613 | fseqv_1d(ji) = fseqv_1d(ji) + zihgnew * zfsalt_melt(ji) & |
---|
614 | & + (1.0 - zihgnew) * zfmass_i(ji) * ( sss_m(zji,zjj) - sm_i_b(ji) ) / rdt_ice |
---|
615 | ENDIF |
---|
616 | ! Heat flux |
---|
617 | ! excessive bottom ablation energy (fsup) - 0 except if jpl = 1 |
---|
618 | ! excessive total ablation energy (focea) sent to the ocean |
---|
619 | qfvbq_1d(ji) = qfvbq_1d(ji) + fsup(ji) + ( 1.0 - zihgnew ) * focea(ji) * a_i_b(ji) * rdt_ice |
---|
620 | |
---|
621 | zihic = 1.0 - MAX( zzero , SIGN( zone , -ht_i_b(ji) ) ) |
---|
622 | ! equals 0 if ht_i = 0, 1 if ht_i gt 0 |
---|
623 | fscbq_1d(ji) = a_i_b(ji) * fstbif_1d(ji) |
---|
624 | qldif_1d(ji) = qldif_1d(ji) + fsup(ji) + ( 1.0 - zihgnew ) * focea(ji) * a_i_b(ji) * rdt_ice & |
---|
625 | & + ( 1.0 - zihic ) * fscbq_1d(ji) * rdt_ice |
---|
626 | END DO ! ji |
---|
627 | |
---|
628 | !------------------------------------------- |
---|
629 | ! Correct temperature, energy and thickness |
---|
630 | !------------------------------------------- |
---|
631 | DO ji = kideb, kiut |
---|
632 | zihgnew = 1.0 - MAX( zzero , SIGN( zone , - zhgnew(ji) ) ) |
---|
633 | t_su_b(ji) = zihgnew * t_su_b(ji) + ( 1.0 - zihgnew ) * rtt |
---|
634 | END DO ! ji |
---|
635 | |
---|
636 | DO jk = 1, nlay_i |
---|
637 | DO ji = kideb, kiut |
---|
638 | zihgnew = 1.0 - MAX( zzero , SIGN( zone , - zhgnew(ji) ) ) |
---|
639 | t_i_b(ji,jk) = zihgnew * t_i_b(ji,jk) + ( 1.0 - zihgnew ) * rtt |
---|
640 | q_i_b(ji,jk) = zihgnew * q_i_b(ji,jk) |
---|
641 | END DO |
---|
642 | END DO ! ji |
---|
643 | |
---|
644 | DO ji = kideb, kiut |
---|
645 | ht_i_b(ji) = zhgnew(ji) |
---|
646 | END DO ! ji |
---|
647 | ! |
---|
648 | !------------------------------------------------------------------------------| |
---|
649 | ! 6) Snow-Ice formation | |
---|
650 | !------------------------------------------------------------------------------| |
---|
651 | ! When snow load excesses Archimede's limit, snow-ice interface goes down under sea-level, |
---|
652 | ! flooding of seawater transforms snow into ice dh_snowice is positive for the ice |
---|
653 | DO ji = kideb, kiut |
---|
654 | ! |
---|
655 | dh_snowice(ji) = MAX( zzero , ( rhosn * ht_s_b(ji) + (rhoic-rau0) * ht_i_b(ji) ) / ( rhosn+rau0-rhoic ) ) |
---|
656 | zhgnew(ji) = MAX( zhgnew(ji) , zhgnew(ji) + dh_snowice(ji) ) |
---|
657 | zhnnew = MIN( ht_s_b(ji) , ht_s_b(ji) - dh_snowice(ji) ) |
---|
658 | |
---|
659 | ! Changes in ice volume and ice mass. |
---|
660 | dvnbq_1d (ji) = a_i_b(ji) * ( zhgnew(ji)-ht_i_b(ji) ) |
---|
661 | dmgwi_1d (ji) = dmgwi_1d(ji) + a_i_b(ji) * ( ht_s_b(ji) - zhnnew ) * rhosn |
---|
662 | |
---|
663 | rdmicif_1d(ji) = rdmicif_1d(ji) + a_i_b(ji) * ( zhgnew(ji) - ht_i_b(ji) ) * rhoic |
---|
664 | rdmsnif_1d(ji) = rdmsnif_1d(ji) + a_i_b(ji) * ( zhnnew - ht_s_b(ji) ) * rhosn |
---|
665 | |
---|
666 | ! Equivalent salt flux (1) Snow-ice formation component |
---|
667 | ! ----------------------------------------------------- |
---|
668 | zji = MOD( npb(ji) - 1, jpi ) + 1 |
---|
669 | zjj = ( npb(ji) - 1 ) / jpi + 1 |
---|
670 | |
---|
671 | IF( num_sal /= 2 ) THEN ; zsm_snowice = sm_i_b(ji) |
---|
672 | ELSE ; zsm_snowice = ( rhoic - rhosn ) / rhoic * sss_m(zji,zjj) |
---|
673 | ENDIF |
---|
674 | IF( num_sal == 4 ) THEN |
---|
675 | fseqv_1d(ji) = fseqv_1d(ji) + ( sss_m(zji,zjj) - bulk_sal ) * a_i_b(ji) & |
---|
676 | & * ( zhgnew(ji) - ht_i_b(ji) ) * rhoic / rdt_ice |
---|
677 | ELSE |
---|
678 | fseqv_1d(ji) = fseqv_1d(ji) + ( sss_m(zji,zjj) - zsm_snowice ) * a_i_b(ji) & |
---|
679 | & * ( zhgnew(ji) - ht_i_b(ji) ) * rhoic / rdt_ice |
---|
680 | ENDIF |
---|
681 | ! entrapment during snow ice formation |
---|
682 | i_ice_switch = 1.0 - MAX( 0.e0 , SIGN( 1.0 , - ht_i_b(ji) + 1.0e-6 ) ) |
---|
683 | isnowic = 1.0 - MAX( 0.e0 , SIGN( 1.0 , - dh_snowice(ji) ) ) * i_ice_switch |
---|
684 | IF( num_sal == 2 .OR. num_sal == 4 ) & |
---|
685 | dsm_i_si_1d(ji) = ( zsm_snowice*dh_snowice(ji) & |
---|
686 | & + sm_i_b(ji) * ht_i_b(ji) / MAX( ht_i_b(ji) + dh_snowice(ji), epsi13) & |
---|
687 | & - sm_i_b(ji) ) * isnowic |
---|
688 | |
---|
689 | ! Actualize new snow and ice thickness. |
---|
690 | ht_s_b(ji) = zhnnew |
---|
691 | ht_i_b(ji) = zhgnew(ji) |
---|
692 | |
---|
693 | ! Total ablation ! new lines added to debug |
---|
694 | IF( ht_i_b(ji) <= 0._wp ) a_i_b(ji) = 0._wp |
---|
695 | |
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696 | ! diagnostic ( snow ice growth ) |
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697 | zji = MOD( npb(ji) - 1, jpi ) + 1 |
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698 | zjj = ( npb(ji) - 1 ) / jpi + 1 |
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699 | diag_sni_gr(zji,zjj) = diag_sni_gr(zji,zjj) + dh_snowice(ji)*a_i_b(ji) / rdt_ice |
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700 | ! |
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701 | END DO !ji |
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702 | ! |
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703 | CALL wrk_dealloc( jpij, zh_i, zh_s, ztfs, zhsold, zqprec, zqfont_su, zqfont_bo, z_f_surf, zhgnew, zfmass_i ) |
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704 | CALL wrk_dealloc( jpij, zdh_s_mel, zdh_s_pre, zdh_s_sub, zfsalt_melt, zfdt_init, zfdt_final, zqt_i, zqt_s, zqt_dummy ) |
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705 | CALL wrk_dealloc( jpij, zinnermelt, zfbase, zdq_i ) |
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706 | CALL wrk_dealloc( jpij, jkmax, zdeltah, zqt_i_lay ) |
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707 | ! |
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708 | END SUBROUTINE lim_thd_dh |
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709 | |
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710 | #else |
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711 | !!---------------------------------------------------------------------- |
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712 | !! Default option NO LIM3 sea-ice model |
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713 | !!---------------------------------------------------------------------- |
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714 | CONTAINS |
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715 | SUBROUTINE lim_thd_dh ! Empty routine |
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716 | END SUBROUTINE lim_thd_dh |
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717 | #endif |
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718 | |
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719 | !!====================================================================== |
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720 | END MODULE limthd_dh |
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