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 wfx_snw & wfx_ice |
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9 | !! 3.4 ! 2011-02 (G. Madec) dynamical allocation |
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10 | !! 3.5 ! 2012-10 (G. Madec & co) salt flux + bug fixes |
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11 | !!---------------------------------------------------------------------- |
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12 | #if defined key_lim3 |
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13 | !!---------------------------------------------------------------------- |
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14 | !! 'key_lim3' LIM3 sea-ice model |
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15 | !!---------------------------------------------------------------------- |
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16 | !! lim_thd_dh : vertical accr./abl. and lateral ablation of sea ice |
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17 | !!---------------------------------------------------------------------- |
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18 | USE par_oce ! ocean parameters |
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19 | USE phycst ! physical constants (OCE directory) |
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20 | USE sbc_oce ! Surface boundary condition: ocean fields |
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21 | USE ice ! LIM variables |
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22 | USE par_ice ! LIM parameters |
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23 | USE thd_ice ! LIM thermodynamics |
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24 | USE in_out_manager ! I/O manager |
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25 | USE lib_mpp ! MPP library |
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26 | USE wrk_nemo ! work arrays |
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27 | USE lib_fortran ! Fortran utilities (allows no signed zero when 'key_nosignedzero' defined) |
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28 | |
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29 | IMPLICIT NONE |
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30 | PRIVATE |
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31 | |
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32 | PUBLIC lim_thd_dh ! called by lim_thd |
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33 | |
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34 | !!---------------------------------------------------------------------- |
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35 | !! NEMO/LIM3 4.0 , UCL - NEMO Consortium (2010) |
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36 | !! $Id$ |
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37 | !! Software governed by the CeCILL licence (NEMOGCM/NEMO_CeCILL.txt) |
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38 | !!---------------------------------------------------------------------- |
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39 | CONTAINS |
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40 | |
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41 | SUBROUTINE lim_thd_dh( kideb, kiut ) |
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42 | !!------------------------------------------------------------------ |
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43 | !! *** ROUTINE lim_thd_dh *** |
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44 | !! |
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45 | !! ** Purpose : determines variations of ice and snow thicknesses. |
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46 | !! |
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47 | !! ** Method : Ice/Snow surface melting arises from imbalance in surface fluxes |
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48 | !! Bottom accretion/ablation arises from flux budget |
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49 | !! Snow thickness can increase by precipitation and decrease by sublimation |
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50 | !! If snow load excesses Archmiede limit, snow-ice is formed by |
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51 | !! the flooding of sea-water in the snow |
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52 | !! |
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53 | !! 1) Compute available flux of heat for surface ablation |
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54 | !! 2) Compute snow and sea ice enthalpies |
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55 | !! 3) Surface ablation and sublimation |
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56 | !! 4) Bottom accretion/ablation |
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57 | !! 5) Case of Total ablation |
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58 | !! 6) Snow ice formation |
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59 | !! |
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60 | !! References : Bitz and Lipscomb, 1999, J. Geophys. Res. |
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61 | !! Fichefet T. and M. Maqueda 1997, J. Geophys. Res., 102(C6), 12609-12646 |
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62 | !! Vancoppenolle, Fichefet and Bitz, 2005, Geophys. Res. Let. |
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63 | !! Vancoppenolle et al.,2009, Ocean Modelling |
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64 | !!------------------------------------------------------------------ |
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65 | INTEGER , INTENT(in) :: kideb, kiut ! Start/End point on which the the computation is applied |
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66 | !! |
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67 | INTEGER :: ji , jk ! dummy loop indices |
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68 | INTEGER :: ii, ij ! 2D corresponding indices to ji |
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69 | INTEGER :: iter |
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70 | |
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71 | REAL(wp) :: ztmelts ! local scalar |
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72 | REAL(wp) :: zdh, zfdum ! |
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73 | REAL(wp) :: zfracs ! fractionation coefficient for bottom salt entrapment |
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74 | REAL(wp) :: zcoeff ! dummy argument for snowfall partitioning over ice and leads |
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75 | REAL(wp) :: zs_snic ! snow-ice salinity |
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76 | REAL(wp) :: zswi1 ! switch for computation of bottom salinity |
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77 | REAL(wp) :: zswi12 ! switch for computation of bottom salinity |
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78 | REAL(wp) :: zswi2 ! switch for computation of bottom salinity |
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79 | REAL(wp) :: zgrr ! bottom growth rate |
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80 | REAL(wp) :: zt_i_new ! bottom formation temperature |
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81 | |
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82 | REAL(wp) :: zQm ! enthalpy exchanged with the ocean (J/m2), >0 towards the ocean |
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83 | REAL(wp) :: zEi ! specific enthalpy of sea ice (J/kg) |
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84 | REAL(wp) :: zEw ! specific enthalpy of exchanged water (J/kg) |
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85 | REAL(wp) :: zdE ! specific enthalpy difference (J/kg) |
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86 | REAL(wp) :: zfmdt ! exchange mass flux x time step (J/m2), >0 towards the ocean |
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87 | REAL(wp) :: zsstK ! SST in Kelvin |
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88 | |
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89 | REAL(wp), POINTER, DIMENSION(:) :: zh_s ! snow layer thickness |
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90 | REAL(wp), POINTER, DIMENSION(:) :: zqprec ! energy of fallen snow (J.m-3) |
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91 | REAL(wp), POINTER, DIMENSION(:) :: zq_su ! heat for surface ablation (J.m-2) |
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92 | REAL(wp), POINTER, DIMENSION(:) :: zq_bo ! heat for bottom ablation (J.m-2) |
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93 | REAL(wp), POINTER, DIMENSION(:) :: zq_1cat ! corrected heat in case 1-cat and hmelt>15cm (J.m-2) |
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94 | REAL(wp), POINTER, DIMENSION(:) :: zq_rema ! remaining heat at the end of the routine (J.m-2) |
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95 | REAL(wp), POINTER, DIMENSION(:) :: zf_tt ! Heat budget to determine melting or freezing(W.m-2) |
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96 | INTEGER , POINTER, DIMENSION(:) :: icount ! number of layers vanished by melting |
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97 | |
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98 | REAL(wp), POINTER, DIMENSION(:) :: zdh_s_mel ! snow melt |
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99 | REAL(wp), POINTER, DIMENSION(:) :: zdh_s_pre ! snow precipitation |
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100 | REAL(wp), POINTER, DIMENSION(:) :: zdh_s_sub ! snow sublimation |
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101 | |
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102 | REAL(wp), POINTER, DIMENSION(:,:) :: zdeltah |
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103 | REAL(wp), POINTER, DIMENSION(:,:) :: zh_i ! ice layer thickness |
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104 | |
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105 | REAL(wp), POINTER, DIMENSION(:) :: zqh_i ! total ice heat content (J.m-2) |
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106 | REAL(wp), POINTER, DIMENSION(:) :: zqh_s ! total snow heat content (J.m-2) |
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107 | REAL(wp), POINTER, DIMENSION(:) :: zq_s ! total snow enthalpy (J.m-3) |
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108 | |
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109 | ! mass and salt flux (clem) |
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110 | REAL(wp) :: zdvres, zswitch_sal |
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111 | |
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112 | ! Heat conservation |
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113 | INTEGER :: num_iter_max |
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114 | |
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115 | !!------------------------------------------------------------------ |
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116 | |
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117 | ! Discriminate between varying salinity (num_sal=2) and prescribed cases (other values) |
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118 | SELECT CASE( num_sal ) ! varying salinity or not |
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119 | CASE( 1, 3, 4 ) ; zswitch_sal = 0 ! prescribed salinity profile |
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120 | CASE( 2 ) ; zswitch_sal = 1 ! varying salinity profile |
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121 | END SELECT |
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122 | |
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123 | CALL wrk_alloc( jpij, zh_s, zqprec, zq_su, zq_bo, zf_tt, zq_1cat, zq_rema ) |
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124 | CALL wrk_alloc( jpij, zdh_s_mel, zdh_s_pre, zdh_s_sub, zqh_i, zqh_s, zq_s ) |
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125 | CALL wrk_alloc( jpij, nlay_i+1, zdeltah, zh_i ) |
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126 | CALL wrk_alloc( jpij, icount ) |
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127 | |
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128 | dh_i_surf (:) = 0._wp ; dh_i_bott (:) = 0._wp ; dh_snowice(:) = 0._wp |
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129 | dsm_i_se_1d(:) = 0._wp ; dsm_i_si_1d(:) = 0._wp |
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130 | |
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131 | zqprec (:) = 0._wp ; zq_su (:) = 0._wp ; zq_bo (:) = 0._wp ; zf_tt (:) = 0._wp |
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132 | zq_1cat(:) = 0._wp ; zq_rema(:) = 0._wp |
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133 | |
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134 | zh_s (:) = 0._wp |
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135 | zdh_s_pre(:) = 0._wp |
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136 | zdh_s_mel(:) = 0._wp |
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137 | zdh_s_sub(:) = 0._wp |
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138 | zqh_s (:) = 0._wp |
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139 | zqh_i (:) = 0._wp |
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140 | |
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141 | zh_i (:,:) = 0._wp |
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142 | zdeltah (:,:) = 0._wp |
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143 | icount (:) = 0 |
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144 | |
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145 | ! initialize layer thicknesses and enthalpies |
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146 | h_i_old (:,0:nlay_i+1) = 0._wp |
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147 | qh_i_old(:,0:nlay_i+1) = 0._wp |
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148 | DO jk = 1, nlay_i |
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149 | DO ji = kideb, kiut |
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150 | h_i_old (ji,jk) = ht_i_1d(ji) / REAL( nlay_i ) |
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151 | qh_i_old(ji,jk) = q_i_1d(ji,jk) * h_i_old(ji,jk) |
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152 | ENDDO |
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153 | ENDDO |
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154 | ! |
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155 | !------------------------------------------------------------------------------! |
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156 | ! 1) Calculate available heat for surface and bottom ablation ! |
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157 | !------------------------------------------------------------------------------! |
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158 | ! |
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159 | DO ji = kideb, kiut |
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160 | rswitch = 1._wp - MAX( 0._wp , SIGN( 1._wp , - ht_s_1d(ji) ) ) |
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161 | ztmelts = rswitch * rtt + ( 1._wp - rswitch ) * rtt |
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162 | |
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163 | zfdum = qns_ice_1d(ji) + ( 1._wp - i0(ji) ) * qsr_ice_1d(ji) - fc_su(ji) |
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164 | zf_tt(ji) = fc_bo_i(ji) + fhtur_1d(ji) + fhld_1d(ji) |
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165 | |
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166 | zq_su (ji) = MAX( 0._wp, zfdum * rdt_ice ) * MAX( 0._wp , SIGN( 1._wp, t_su_1d(ji) - ztmelts ) ) |
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167 | zq_bo (ji) = MAX( 0._wp, zf_tt(ji) * rdt_ice ) |
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168 | END DO |
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169 | |
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170 | ! |
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171 | !------------------------------------------------------------------------------! |
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172 | ! If snow temperature is above freezing point, then snow melts |
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173 | ! (should not happen but sometimes it does) |
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174 | !------------------------------------------------------------------------------! |
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175 | DO ji = kideb, kiut |
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176 | IF( t_s_1d(ji,1) > rtt ) THEN !!! Internal melting |
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177 | ! Contribution to heat flux to the ocean [W.m-2], < 0 |
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178 | hfx_res_1d(ji) = hfx_res_1d(ji) + q_s_1d(ji,1) * ht_s_1d(ji) * a_i_1d(ji) * r1_rdtice |
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179 | ! Contribution to mass flux |
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180 | wfx_snw_1d(ji) = wfx_snw_1d(ji) + rhosn * ht_s_1d(ji) * a_i_1d(ji) * r1_rdtice |
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181 | ! updates |
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182 | ht_s_1d(ji) = 0._wp |
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183 | q_s_1d (ji,1) = 0._wp |
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184 | t_s_1d (ji,1) = rtt |
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185 | END IF |
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186 | END DO |
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187 | |
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188 | !------------------------------------------------------------! |
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189 | ! 2) Computing layer thicknesses and enthalpies. ! |
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190 | !------------------------------------------------------------! |
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191 | ! |
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192 | DO ji = kideb, kiut |
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193 | zh_s(ji) = ht_s_1d(ji) / REAL( nlay_s ) |
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194 | END DO |
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195 | ! |
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196 | DO jk = 1, nlay_s |
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197 | DO ji = kideb, kiut |
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198 | zqh_s(ji) = zqh_s(ji) + q_s_1d(ji,jk) * zh_s(ji) |
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199 | END DO |
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200 | END DO |
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201 | ! |
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202 | DO jk = 1, nlay_i |
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203 | DO ji = kideb, kiut |
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204 | zh_i(ji,jk) = ht_i_1d(ji) / REAL( nlay_i ) |
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205 | zqh_i(ji) = zqh_i(ji) + q_i_1d(ji,jk) * zh_i(ji,jk) |
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206 | END DO |
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207 | END DO |
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208 | ! |
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209 | !------------------------------------------------------------------------------| |
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210 | ! 3) Surface ablation and sublimation | |
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211 | !------------------------------------------------------------------------------| |
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212 | ! |
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213 | !------------------------- |
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214 | ! 3.1 Snow precips / melt |
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215 | !------------------------- |
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216 | ! Snow accumulation in one thermodynamic time step |
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217 | ! snowfall is partitionned between leads and ice |
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218 | ! if snow fall was uniform, a fraction (1-at_i) would fall into leads |
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219 | ! but because of the winds, more snow falls on leads than on sea ice |
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220 | ! and a greater fraction (1-at_i)^beta of the total mass of snow |
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221 | ! (beta < 1) falls in leads. |
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222 | ! In reality, beta depends on wind speed, |
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223 | ! and should decrease with increasing wind speed but here, it is |
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224 | ! considered as a constant. an average value is 0.66 |
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225 | ! Martin Vancoppenolle, December 2006 |
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226 | |
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227 | DO ji = kideb, kiut |
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228 | !----------- |
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229 | ! Snow fall |
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230 | !----------- |
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231 | ! thickness change |
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232 | zcoeff = ( 1._wp - ( 1._wp - at_i_1d(ji) )**betas ) / at_i_1d(ji) |
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233 | zdh_s_pre(ji) = zcoeff * sprecip_1d(ji) * rdt_ice / rhosn |
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234 | ! enthalpy of the precip (>0, J.m-3) (tatm_ice is now in K) |
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235 | zqprec (ji) = rhosn * ( cpic * ( rtt - MIN( tatm_ice_1d(ji), rt0_snow) ) + lfus ) |
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236 | IF( sprecip_1d(ji) == 0._wp ) zqprec(ji) = 0._wp |
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237 | ! heat flux from snow precip (>0, W.m-2) |
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238 | hfx_spr_1d(ji) = hfx_spr_1d(ji) + zdh_s_pre(ji) * a_i_1d(ji) * zqprec(ji) * r1_rdtice |
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239 | ! mass flux, <0 |
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240 | wfx_spr_1d(ji) = wfx_spr_1d(ji) - rhosn * a_i_1d(ji) * zdh_s_pre(ji) * r1_rdtice |
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241 | ! update thickness |
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242 | ht_s_1d (ji) = MAX( 0._wp , ht_s_1d(ji) + zdh_s_pre(ji) ) |
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243 | |
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244 | !--------------------- |
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245 | ! Melt of falling snow |
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246 | !--------------------- |
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247 | ! thickness change |
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248 | IF( zdh_s_pre(ji) > 0._wp ) THEN |
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249 | rswitch = 1._wp - MAX( 0._wp , SIGN( 1._wp , - zqprec(ji) + epsi20 ) ) |
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250 | zdh_s_mel (ji) = - rswitch * zq_su(ji) / MAX( zqprec(ji) , epsi20 ) |
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251 | zdh_s_mel (ji) = MAX( - zdh_s_pre(ji), zdh_s_mel(ji) ) ! bound melting |
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252 | ! heat used to melt snow (W.m-2, >0) |
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253 | hfx_snw_1d(ji) = hfx_snw_1d(ji) - zdh_s_mel(ji) * a_i_1d(ji) * zqprec(ji) * r1_rdtice |
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254 | ! snow melting only = water into the ocean (then without snow precip), >0 |
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255 | wfx_snw_1d(ji) = wfx_snw_1d(ji) - rhosn * a_i_1d(ji) * zdh_s_mel(ji) * r1_rdtice |
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256 | |
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257 | ! updates available heat + thickness |
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258 | zq_su (ji) = MAX( 0._wp , zq_su (ji) + zdh_s_mel(ji) * zqprec(ji) ) |
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259 | ht_s_1d(ji) = MAX( 0._wp , ht_s_1d(ji) + zdh_s_mel(ji) ) |
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260 | zh_s (ji) = ht_s_1d(ji) / REAL( nlay_s ) |
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261 | |
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262 | ENDIF |
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263 | END DO |
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264 | |
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265 | ! If heat still available, then melt more snow |
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266 | zdeltah(:,:) = 0._wp ! important |
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267 | DO jk = 1, nlay_s |
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268 | DO ji = kideb, kiut |
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269 | ! thickness change |
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270 | rswitch = 1._wp - MAX( 0._wp, SIGN( 1._wp, - ht_s_1d(ji) ) ) |
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271 | rswitch = rswitch * ( 1._wp - MAX( 0._wp, SIGN( 1._wp, - q_s_1d(ji,jk) + epsi20 ) ) ) |
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272 | zdeltah (ji,jk) = - rswitch * zq_su(ji) / MAX( q_s_1d(ji,jk), epsi20 ) |
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273 | zdeltah (ji,jk) = MAX( zdeltah(ji,jk) , - zh_s(ji) ) ! bound melting |
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274 | zdh_s_mel(ji) = zdh_s_mel(ji) + zdeltah(ji,jk) |
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275 | ! heat used to melt snow(W.m-2, >0) |
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276 | hfx_snw_1d(ji) = hfx_snw_1d(ji) - zdeltah(ji,jk) * a_i_1d(ji) * q_s_1d(ji,jk) * r1_rdtice |
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277 | ! snow melting only = water into the ocean (then without snow precip) |
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278 | wfx_snw_1d(ji) = wfx_snw_1d(ji) - rhosn * a_i_1d(ji) * zdeltah(ji,jk) * r1_rdtice |
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279 | |
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280 | ! updates available heat + thickness |
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281 | zq_su (ji) = MAX( 0._wp , zq_su (ji) + zdeltah(ji,jk) * q_s_1d(ji,jk) ) |
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282 | ht_s_1d(ji) = MAX( 0._wp , ht_s_1d(ji) + zdeltah(ji,jk) ) |
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283 | |
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284 | END DO |
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285 | END DO |
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286 | |
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287 | !---------------------- |
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288 | ! 3.2 Snow sublimation |
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289 | !---------------------- |
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290 | ! qla_ice is always >=0 (upwards), heat goes to the atmosphere, therefore snow sublimates |
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291 | ! clem comment: not counted in mass exchange in limsbc since this is an exchange with atm. (not ocean) |
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292 | ! clem comment: ice should also sublimate |
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293 | IF( lk_cpl ) THEN |
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294 | ! coupled mode: sublimation already included in emp_ice (to do in limsbc_ice) |
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295 | zdh_s_sub(:) = 0._wp |
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296 | ELSE |
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297 | ! forced mode: snow thickness change due to sublimation |
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298 | DO ji = kideb, kiut |
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299 | zdh_s_sub(ji) = MAX( - ht_s_1d(ji) , - parsub * qla_ice_1d(ji) / ( rhosn * lsub ) * rdt_ice ) |
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300 | ! Heat flux by sublimation [W.m-2], < 0 |
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301 | ! sublimate first snow that had fallen, then pre-existing snow |
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302 | zcoeff = ( MAX( zdh_s_sub(ji), - MAX( 0._wp, zdh_s_pre(ji) + zdh_s_mel(ji) ) ) * zqprec(ji) + & |
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303 | & ( zdh_s_sub(ji) - MAX( zdh_s_sub(ji), - MAX( 0._wp, zdh_s_pre(ji) + zdh_s_mel(ji) ) ) ) * q_s_1d(ji,1) ) & |
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304 | & * a_i_1d(ji) * r1_rdtice |
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305 | hfx_sub_1d(ji) = hfx_sub_1d(ji) + zcoeff |
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306 | ! Mass flux by sublimation |
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307 | wfx_sub_1d(ji) = wfx_sub_1d(ji) - rhosn * a_i_1d(ji) * zdh_s_sub(ji) * r1_rdtice |
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308 | ! new snow thickness |
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309 | ht_s_1d(ji) = MAX( 0._wp , ht_s_1d(ji) + zdh_s_sub(ji) ) |
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310 | END DO |
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311 | ENDIF |
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312 | |
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313 | ! --- Update snow diags --- ! |
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314 | DO ji = kideb, kiut |
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315 | dh_s_tot(ji) = zdh_s_mel(ji) + zdh_s_pre(ji) + zdh_s_sub(ji) |
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316 | zh_s(ji) = ht_s_1d(ji) / REAL( nlay_s ) |
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317 | END DO ! ji |
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318 | |
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319 | !------------------------------------------- |
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320 | ! 3.3 Update temperature, energy |
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321 | !------------------------------------------- |
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322 | ! new temp and enthalpy of the snow (remaining snow precip + remaining pre-existing snow) |
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323 | zq_s(:) = 0._wp |
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324 | DO jk = 1, nlay_s |
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325 | DO ji = kideb,kiut |
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326 | rswitch = MAX( 0._wp , SIGN( 1._wp, - ht_s_1d(ji) + epsi20 ) ) |
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327 | q_s_1d(ji,jk) = ( 1._wp - rswitch ) / MAX( ht_s_1d(ji), epsi20 ) * & |
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328 | & ( ( MAX( 0._wp, dh_s_tot(ji) ) ) * zqprec(ji) + & |
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329 | & ( - MAX( 0._wp, dh_s_tot(ji) ) + ht_s_1d(ji) ) * rhosn * ( cpic * ( rtt - t_s_1d(ji,jk) ) + lfus ) ) |
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330 | zq_s(ji) = zq_s(ji) + q_s_1d(ji,jk) |
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331 | END DO |
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332 | END DO |
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333 | |
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334 | !-------------------------- |
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335 | ! 3.4 Surface ice ablation |
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336 | !-------------------------- |
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337 | zdeltah(:,:) = 0._wp ! important |
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338 | DO jk = 1, nlay_i |
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339 | DO ji = kideb, kiut |
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340 | zEi = - q_i_1d(ji,jk) / rhoic ! Specific enthalpy of layer k [J/kg, <0] |
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341 | |
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342 | ztmelts = - tmut * s_i_1d(ji,jk) + rtt ! Melting point of layer k [K] |
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343 | |
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344 | zEw = rcp * ( ztmelts - rt0 ) ! Specific enthalpy of resulting meltwater [J/kg, <0] |
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345 | |
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346 | zdE = zEi - zEw ! Specific enthalpy difference < 0 |
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347 | |
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348 | zfmdt = - zq_su(ji) / zdE ! Mass flux to the ocean [kg/m2, >0] |
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349 | |
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350 | zdeltah(ji,jk) = - zfmdt / rhoic ! Melt of layer jk [m, <0] |
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351 | |
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352 | zdeltah(ji,jk) = MIN( 0._wp , MAX( zdeltah(ji,jk) , - zh_i(ji,jk) ) ) ! Melt of layer jk cannot exceed the layer thickness [m, <0] |
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353 | |
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354 | zq_su(ji) = MAX( 0._wp , zq_su(ji) - zdeltah(ji,jk) * rhoic * zdE ) ! update available heat |
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355 | |
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356 | dh_i_surf(ji) = dh_i_surf(ji) + zdeltah(ji,jk) ! Cumulate surface melt |
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357 | |
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358 | zfmdt = - rhoic * zdeltah(ji,jk) ! Recompute mass flux [kg/m2, >0] |
---|
359 | |
---|
360 | zQm = zfmdt * zEw ! Energy of the melt water sent to the ocean [J/m2, <0] |
---|
361 | |
---|
362 | ! Contribution to salt flux (clem: using sm_i_1d and not s_i_1d(jk) is ok) |
---|
363 | sfx_sum_1d(ji) = sfx_sum_1d(ji) - sm_i_1d(ji) * a_i_1d(ji) * zdeltah(ji,jk) * rhoic * r1_rdtice |
---|
364 | |
---|
365 | ! Contribution to heat flux [W.m-2], < 0 |
---|
366 | hfx_thd_1d(ji) = hfx_thd_1d(ji) + zfmdt * a_i_1d(ji) * zEw * r1_rdtice |
---|
367 | |
---|
368 | ! Total heat flux used in this process [W.m-2], > 0 |
---|
369 | hfx_sum_1d(ji) = hfx_sum_1d(ji) - zfmdt * a_i_1d(ji) * zdE * r1_rdtice |
---|
370 | |
---|
371 | ! Contribution to mass flux |
---|
372 | wfx_sum_1d(ji) = wfx_sum_1d(ji) - rhoic * a_i_1d(ji) * zdeltah(ji,jk) * r1_rdtice |
---|
373 | |
---|
374 | ! record which layers have disappeared (for bottom melting) |
---|
375 | ! => icount=0 : no layer has vanished |
---|
376 | ! => icount=5 : 5 layers have vanished |
---|
377 | rswitch = MAX( 0._wp , SIGN( 1._wp , - ( zh_i(ji,jk) + zdeltah(ji,jk) ) ) ) |
---|
378 | icount(ji) = icount(ji) + NINT( rswitch ) |
---|
379 | zh_i(ji,jk) = MAX( 0._wp , zh_i(ji,jk) + zdeltah(ji,jk) ) |
---|
380 | |
---|
381 | ! update heat content (J.m-2) and layer thickness |
---|
382 | qh_i_old(ji,jk) = qh_i_old(ji,jk) + zdeltah(ji,jk) * q_i_1d(ji,jk) |
---|
383 | h_i_old (ji,jk) = h_i_old (ji,jk) + zdeltah(ji,jk) |
---|
384 | END DO |
---|
385 | END DO |
---|
386 | ! update ice thickness |
---|
387 | DO ji = kideb, kiut |
---|
388 | ht_i_1d(ji) = MAX( 0._wp , ht_i_1d(ji) + dh_i_surf(ji) ) |
---|
389 | END DO |
---|
390 | |
---|
391 | ! |
---|
392 | !------------------------------------------------------------------------------! |
---|
393 | ! 4) Basal growth / melt ! |
---|
394 | !------------------------------------------------------------------------------! |
---|
395 | ! |
---|
396 | !------------------ |
---|
397 | ! 4.1 Basal growth |
---|
398 | !------------------ |
---|
399 | ! Basal growth is driven by heat imbalance at the ice-ocean interface, |
---|
400 | ! between the inner conductive flux (fc_bo_i), from the open water heat flux |
---|
401 | ! (fhld) and the turbulent ocean flux (fhtur). |
---|
402 | ! fc_bo_i is positive downwards. fhtur and fhld are positive to the ice |
---|
403 | |
---|
404 | ! If salinity varies in time, an iterative procedure is required, because |
---|
405 | ! the involved quantities are inter-dependent. |
---|
406 | ! Basal growth (dh_i_bott) depends upon new ice specific enthalpy (zEi), |
---|
407 | ! which depends on forming ice salinity (s_i_new), which depends on dh/dt (dh_i_bott) |
---|
408 | ! -> need for an iterative procedure, which converges quickly |
---|
409 | |
---|
410 | IF ( num_sal == 2 ) THEN |
---|
411 | num_iter_max = 5 |
---|
412 | ELSE |
---|
413 | num_iter_max = 1 |
---|
414 | ENDIF |
---|
415 | |
---|
416 | !clem debug. Just to be sure that enthalpy at nlay_i+1 is null |
---|
417 | DO ji = kideb, kiut |
---|
418 | q_i_1d(ji,nlay_i+1) = 0._wp |
---|
419 | END DO |
---|
420 | |
---|
421 | ! Iterative procedure |
---|
422 | DO iter = 1, num_iter_max |
---|
423 | DO ji = kideb, kiut |
---|
424 | IF( zf_tt(ji) < 0._wp ) THEN |
---|
425 | |
---|
426 | ! New bottom ice salinity (Cox & Weeks, JGR88 ) |
---|
427 | !--- zswi1 if dh/dt < 2.0e-8 |
---|
428 | !--- zswi12 if 2.0e-8 < dh/dt < 3.6e-7 |
---|
429 | !--- zswi2 if dh/dt > 3.6e-7 |
---|
430 | zgrr = MIN( 1.0e-3, MAX ( dh_i_bott(ji) * r1_rdtice , epsi10 ) ) |
---|
431 | zswi2 = MAX( 0._wp , SIGN( 1._wp , zgrr - 3.6e-7 ) ) |
---|
432 | zswi12 = MAX( 0._wp , SIGN( 1._wp , zgrr - 2.0e-8 ) ) * ( 1.0 - zswi2 ) |
---|
433 | zswi1 = 1. - zswi2 * zswi12 |
---|
434 | zfracs = MIN ( zswi1 * 0.12 + zswi12 * ( 0.8925 + 0.0568 * LOG( 100.0 * zgrr ) ) & |
---|
435 | & + zswi2 * 0.26 / ( 0.26 + 0.74 * EXP ( - 724300.0 * zgrr ) ) , 0.5 ) |
---|
436 | |
---|
437 | ii = MOD( npb(ji) - 1, jpi ) + 1 ; ij = ( npb(ji) - 1 ) / jpi + 1 |
---|
438 | |
---|
439 | s_i_new(ji) = zswitch_sal * zfracs * sss_m(ii,ij) & ! New ice salinity |
---|
440 | + ( 1. - zswitch_sal ) * sm_i_1d(ji) |
---|
441 | ! New ice growth |
---|
442 | ztmelts = - tmut * s_i_new(ji) + rtt ! New ice melting point (K) |
---|
443 | |
---|
444 | zt_i_new = zswitch_sal * t_bo_1d(ji) + ( 1. - zswitch_sal) * t_i_1d(ji, nlay_i) |
---|
445 | |
---|
446 | zEi = cpic * ( zt_i_new - ztmelts ) & ! Specific enthalpy of forming ice (J/kg, <0) |
---|
447 | & - lfus * ( 1.0 - ( ztmelts - rtt ) / ( zt_i_new - rtt ) ) & |
---|
448 | & + rcp * ( ztmelts-rtt ) |
---|
449 | |
---|
450 | zEw = rcp * ( t_bo_1d(ji) - rt0 ) ! Specific enthalpy of seawater (J/kg, < 0) |
---|
451 | |
---|
452 | zdE = zEi - zEw ! Specific enthalpy difference (J/kg, <0) |
---|
453 | |
---|
454 | dh_i_bott(ji) = rdt_ice * MAX( 0._wp , zf_tt(ji) / ( zdE * rhoic ) ) |
---|
455 | |
---|
456 | q_i_1d(ji,nlay_i+1) = -zEi * rhoic ! New ice energy of melting (J/m3, >0) |
---|
457 | |
---|
458 | ENDIF ! fc_bo_i |
---|
459 | END DO ! ji |
---|
460 | END DO ! iter |
---|
461 | |
---|
462 | ! Contribution to Energy and Salt Fluxes |
---|
463 | DO ji = kideb, kiut |
---|
464 | IF( zf_tt(ji) < 0._wp ) THEN |
---|
465 | ! New ice growth |
---|
466 | |
---|
467 | zfmdt = - rhoic * dh_i_bott(ji) ! Mass flux x time step (kg/m2, < 0) |
---|
468 | |
---|
469 | ztmelts = - tmut * s_i_new(ji) + rtt ! New ice melting point (K) |
---|
470 | |
---|
471 | zt_i_new = zswitch_sal * t_bo_1d(ji) + ( 1. - zswitch_sal) * t_i_1d(ji, nlay_i) |
---|
472 | |
---|
473 | zEi = cpic * ( zt_i_new - ztmelts ) & ! Specific enthalpy of forming ice (J/kg, <0) |
---|
474 | & - lfus * ( 1.0 - ( ztmelts - rtt ) / ( zt_i_new - rtt ) ) & |
---|
475 | & + rcp * ( ztmelts-rtt ) |
---|
476 | |
---|
477 | zEw = rcp * ( t_bo_1d(ji) - rt0 ) ! Specific enthalpy of seawater (J/kg, < 0) |
---|
478 | |
---|
479 | zdE = zEi - zEw ! Specific enthalpy difference (J/kg, <0) |
---|
480 | |
---|
481 | ! Contribution to heat flux to the ocean [W.m-2], >0 |
---|
482 | hfx_thd_1d(ji) = hfx_thd_1d(ji) + zfmdt * a_i_1d(ji) * zEw * r1_rdtice |
---|
483 | |
---|
484 | ! Total heat flux used in this process [W.m-2], <0 |
---|
485 | hfx_bog_1d(ji) = hfx_bog_1d(ji) - zfmdt * a_i_1d(ji) * zdE * r1_rdtice |
---|
486 | |
---|
487 | ! Contribution to salt flux, <0 |
---|
488 | sfx_bog_1d(ji) = sfx_bog_1d(ji) + s_i_new(ji) * a_i_1d(ji) * zfmdt * r1_rdtice |
---|
489 | |
---|
490 | ! Contribution to mass flux, <0 |
---|
491 | wfx_bog_1d(ji) = wfx_bog_1d(ji) - rhoic * a_i_1d(ji) * dh_i_bott(ji) * r1_rdtice |
---|
492 | |
---|
493 | ! update heat content (J.m-2) and layer thickness |
---|
494 | qh_i_old(ji,nlay_i+1) = qh_i_old(ji,nlay_i+1) + dh_i_bott(ji) * q_i_1d(ji,nlay_i+1) |
---|
495 | h_i_old (ji,nlay_i+1) = h_i_old (ji,nlay_i+1) + dh_i_bott(ji) |
---|
496 | ENDIF |
---|
497 | END DO |
---|
498 | |
---|
499 | !---------------- |
---|
500 | ! 4.2 Basal melt |
---|
501 | !---------------- |
---|
502 | zdeltah(:,:) = 0._wp ! important |
---|
503 | DO jk = nlay_i, 1, -1 |
---|
504 | DO ji = kideb, kiut |
---|
505 | IF( zf_tt(ji) >= 0._wp .AND. jk > icount(ji) ) THEN ! do not calculate where layer has already disappeared from surface melting |
---|
506 | |
---|
507 | ztmelts = - tmut * s_i_1d(ji,jk) + rtt ! Melting point of layer jk (K) |
---|
508 | |
---|
509 | IF( t_i_1d(ji,jk) >= ztmelts ) THEN !!! Internal melting |
---|
510 | |
---|
511 | zEi = - q_i_1d(ji,jk) / rhoic ! Specific enthalpy of melting ice (J/kg, <0) |
---|
512 | |
---|
513 | !!zEw = rcp * ( t_i_1d(ji,jk) - rtt ) ! Specific enthalpy of meltwater at T = t_i_1d (J/kg, <0) |
---|
514 | |
---|
515 | zdE = 0._wp ! Specific enthalpy difference (J/kg, <0) |
---|
516 | ! set up at 0 since no energy is needed to melt water...(it is already melted) |
---|
517 | |
---|
518 | zdeltah (ji,jk) = MIN( 0._wp , - zh_i(ji,jk) ) ! internal melting occurs when the internal temperature is above freezing |
---|
519 | ! this should normally not happen, but sometimes, heat diffusion leads to this |
---|
520 | |
---|
521 | dh_i_bott (ji) = dh_i_bott(ji) + zdeltah(ji,jk) |
---|
522 | |
---|
523 | zfmdt = - zdeltah(ji,jk) * rhoic ! Mass flux x time step > 0 |
---|
524 | |
---|
525 | ! Contribution to heat flux to the ocean [W.m-2], <0 (ice enthalpy zEi is "sent" to the ocean) |
---|
526 | hfx_res_1d(ji) = hfx_res_1d(ji) + zfmdt * a_i_1d(ji) * zEi * r1_rdtice |
---|
527 | |
---|
528 | ! Contribution to salt flux (clem: using sm_i_1d and not s_i_1d(jk) is ok) |
---|
529 | sfx_res_1d(ji) = sfx_res_1d(ji) - sm_i_1d(ji) * a_i_1d(ji) * zdeltah(ji,jk) * rhoic * r1_rdtice |
---|
530 | |
---|
531 | ! Contribution to mass flux |
---|
532 | wfx_res_1d(ji) = wfx_res_1d(ji) - rhoic * a_i_1d(ji) * zdeltah(ji,jk) * r1_rdtice |
---|
533 | |
---|
534 | ! update heat content (J.m-2) and layer thickness |
---|
535 | qh_i_old(ji,jk) = qh_i_old(ji,jk) + zdeltah(ji,jk) * q_i_1d(ji,jk) |
---|
536 | h_i_old (ji,jk) = h_i_old (ji,jk) + zdeltah(ji,jk) |
---|
537 | |
---|
538 | ELSE !!! Basal melting |
---|
539 | |
---|
540 | zEi = - q_i_1d(ji,jk) / rhoic ! Specific enthalpy of melting ice (J/kg, <0) |
---|
541 | |
---|
542 | zEw = rcp * ( ztmelts - rtt )! Specific enthalpy of meltwater (J/kg, <0) |
---|
543 | |
---|
544 | zdE = zEi - zEw ! Specific enthalpy difference (J/kg, <0) |
---|
545 | |
---|
546 | zfmdt = - zq_bo(ji) / zdE ! Mass flux x time step (kg/m2, >0) |
---|
547 | |
---|
548 | zdeltah(ji,jk) = - zfmdt / rhoic ! Gross thickness change |
---|
549 | |
---|
550 | zdeltah(ji,jk) = MIN( 0._wp , MAX( zdeltah(ji,jk), - zh_i(ji,jk) ) ) ! bound thickness change |
---|
551 | |
---|
552 | zq_bo(ji) = MAX( 0._wp , zq_bo(ji) - zdeltah(ji,jk) * rhoic * zdE ) ! update available heat. MAX is necessary for roundup errors |
---|
553 | |
---|
554 | dh_i_bott(ji) = dh_i_bott(ji) + zdeltah(ji,jk) ! Update basal melt |
---|
555 | |
---|
556 | zfmdt = - zdeltah(ji,jk) * rhoic ! Mass flux x time step > 0 |
---|
557 | |
---|
558 | zQm = zfmdt * zEw ! Heat exchanged with ocean |
---|
559 | |
---|
560 | ! Contribution to heat flux to the ocean [W.m-2], <0 |
---|
561 | hfx_thd_1d(ji) = hfx_thd_1d(ji) + zfmdt * a_i_1d(ji) * zEw * r1_rdtice |
---|
562 | |
---|
563 | ! Contribution to salt flux (clem: using sm_i_1d and not s_i_1d(jk) is ok) |
---|
564 | sfx_bom_1d(ji) = sfx_bom_1d(ji) - sm_i_1d(ji) * a_i_1d(ji) * zdeltah(ji,jk) * rhoic * r1_rdtice |
---|
565 | |
---|
566 | ! Total heat flux used in this process [W.m-2], >0 |
---|
567 | hfx_bom_1d(ji) = hfx_bom_1d(ji) - zfmdt * a_i_1d(ji) * zdE * r1_rdtice |
---|
568 | |
---|
569 | ! Contribution to mass flux |
---|
570 | wfx_bom_1d(ji) = wfx_bom_1d(ji) - rhoic * a_i_1d(ji) * zdeltah(ji,jk) * r1_rdtice |
---|
571 | |
---|
572 | ! update heat content (J.m-2) and layer thickness |
---|
573 | qh_i_old(ji,jk) = qh_i_old(ji,jk) + zdeltah(ji,jk) * q_i_1d(ji,jk) |
---|
574 | h_i_old (ji,jk) = h_i_old (ji,jk) + zdeltah(ji,jk) |
---|
575 | ENDIF |
---|
576 | |
---|
577 | ENDIF |
---|
578 | END DO ! ji |
---|
579 | END DO ! jk |
---|
580 | |
---|
581 | !------------------------------------------------------------------------------! |
---|
582 | ! Excessive ablation in a 1-category model |
---|
583 | ! in a 1-category sea ice model, bottom ablation must not exceed hmelt (-0.15) |
---|
584 | !------------------------------------------------------------------------------! |
---|
585 | ! ??? keep ??? |
---|
586 | ! clem bug: I think this should be included above, so we would not have to |
---|
587 | ! track heat/salt/mass fluxes backwards |
---|
588 | ! IF( jpl == 1 ) THEN |
---|
589 | ! DO ji = kideb, kiut |
---|
590 | ! IF( zf_tt(ji) >= 0._wp ) THEN |
---|
591 | ! zdh = MAX( hmelt , dh_i_bott(ji) ) |
---|
592 | ! zdvres = zdh - dh_i_bott(ji) ! >=0 |
---|
593 | ! dh_i_bott(ji) = zdh |
---|
594 | ! |
---|
595 | ! ! excessive energy is sent to lateral ablation |
---|
596 | ! rswitch = MAX( 0._wp, SIGN( 1._wp , 1._wp - at_i_1d(ji) - epsi20 ) ) |
---|
597 | ! zq_1cat(ji) = rswitch * rhoic * lfus * at_i_1d(ji) / MAX( 1._wp - at_i_1d(ji) , epsi20 ) * zdvres ! J.m-2 >=0 |
---|
598 | ! |
---|
599 | ! ! correct salt and mass fluxes |
---|
600 | ! sfx_bom_1d(ji) = sfx_bom_1d(ji) - sm_i_1d(ji) * a_i_1d(ji) * zdvres * rhoic * r1_rdtice ! this is only a raw approximation |
---|
601 | ! wfx_bom_1d(ji) = wfx_bom_1d(ji) - rhoic * a_i_1d(ji) * zdvres * r1_rdtice |
---|
602 | ! ENDIF |
---|
603 | ! END DO |
---|
604 | ! ENDIF |
---|
605 | |
---|
606 | !------------------------------------------- |
---|
607 | ! Update temperature, energy |
---|
608 | !------------------------------------------- |
---|
609 | DO ji = kideb, kiut |
---|
610 | ht_i_1d(ji) = MAX( 0._wp , ht_i_1d(ji) + dh_i_bott(ji) ) |
---|
611 | END DO |
---|
612 | |
---|
613 | !------------------------------------------- |
---|
614 | ! 5. What to do with remaining energy |
---|
615 | !------------------------------------------- |
---|
616 | ! If heat still available for melting and snow remains, then melt more snow |
---|
617 | !------------------------------------------- |
---|
618 | zdeltah(:,:) = 0._wp ! important |
---|
619 | DO ji = kideb, kiut |
---|
620 | zq_rema(ji) = zq_su(ji) + zq_bo(ji) |
---|
621 | ! zindh = 1._wp - MAX( 0._wp, SIGN( 1._wp, - ht_s_1d(ji) ) ) ! =1 if snow |
---|
622 | ! zindq = 1._wp - MAX( 0._wp, SIGN( 1._wp, - zq_s(ji) + epsi20 ) ) |
---|
623 | ! zdeltah (ji,1) = - zindh * zindq * zq_rema(ji) / MAX( zq_s(ji), epsi20 ) |
---|
624 | ! zdeltah (ji,1) = MIN( 0._wp , MAX( zdeltah(ji,1) , - ht_s_1d(ji) ) ) ! bound melting |
---|
625 | ! zdh_s_mel(ji) = zdh_s_mel(ji) + zdeltah(ji,1) |
---|
626 | ! dh_s_tot (ji) = dh_s_tot(ji) + zdeltah(ji,1) |
---|
627 | ! ht_s_1d (ji) = ht_s_1d(ji) + zdeltah(ji,1) |
---|
628 | ! |
---|
629 | ! zq_rema(ji) = zq_rema(ji) + zdeltah(ji,1) * zq_s(ji) ! update available heat (J.m-2) |
---|
630 | ! ! heat used to melt snow |
---|
631 | ! hfx_snw_1d(ji) = hfx_snw_1d(ji) - zdeltah(ji,1) * a_i_1d(ji) * zq_s(ji) * r1_rdtice ! W.m-2 (>0) |
---|
632 | ! ! Contribution to mass flux |
---|
633 | ! wfx_snw_1d(ji) = wfx_snw_1d(ji) - rhosn * a_i_1d(ji) * zdeltah(ji,1) * r1_rdtice |
---|
634 | ! |
---|
635 | ii = MOD( npb(ji) - 1, jpi ) + 1 ; ij = ( npb(ji) - 1 ) / jpi + 1 |
---|
636 | ! Remaining heat flux (W.m-2) is sent to the ocean heat budget |
---|
637 | hfx_out(ii,ij) = hfx_out(ii,ij) + ( zq_1cat(ji) + zq_rema(ji) * a_i_1d(ji) ) * r1_rdtice |
---|
638 | |
---|
639 | IF( ln_nicep .AND. zq_rema(ji) < 0. .AND. lwp ) WRITE(numout,*) 'ALERTE zq_rema <0 = ', zq_rema(ji) |
---|
640 | END DO |
---|
641 | |
---|
642 | ! |
---|
643 | !------------------------------------------------------------------------------| |
---|
644 | ! 6) Snow-Ice formation | |
---|
645 | !------------------------------------------------------------------------------| |
---|
646 | ! When snow load excesses Archimede's limit, snow-ice interface goes down under sea-level, |
---|
647 | ! flooding of seawater transforms snow into ice dh_snowice is positive for the ice |
---|
648 | DO ji = kideb, kiut |
---|
649 | ! |
---|
650 | dh_snowice(ji) = MAX( 0._wp , ( rhosn * ht_s_1d(ji) + (rhoic-rau0) * ht_i_1d(ji) ) / ( rhosn+rau0-rhoic ) ) |
---|
651 | |
---|
652 | ht_i_1d(ji) = ht_i_1d(ji) + dh_snowice(ji) |
---|
653 | ht_s_1d(ji) = ht_s_1d(ji) - dh_snowice(ji) |
---|
654 | |
---|
655 | ! Salinity of snow ice |
---|
656 | ii = MOD( npb(ji) - 1, jpi ) + 1 ; ij = ( npb(ji) - 1 ) / jpi + 1 |
---|
657 | zs_snic = zswitch_sal * sss_m(ii,ij) * ( rhoic - rhosn ) / rhoic + ( 1. - zswitch_sal ) * sm_i_1d(ji) |
---|
658 | |
---|
659 | ! entrapment during snow ice formation |
---|
660 | ! new salinity difference stored (to be used in limthd_ent.F90) |
---|
661 | IF ( num_sal == 2 ) THEN |
---|
662 | rswitch = MAX( 0._wp , SIGN( 1._wp , ht_i_1d(ji) - epsi10 ) ) |
---|
663 | ! salinity dif due to snow-ice formation |
---|
664 | dsm_i_si_1d(ji) = ( zs_snic - sm_i_1d(ji) ) * dh_snowice(ji) / MAX( ht_i_1d(ji), epsi10 ) * rswitch |
---|
665 | ! salinity dif due to bottom growth |
---|
666 | IF ( zf_tt(ji) < 0._wp ) THEN |
---|
667 | dsm_i_se_1d(ji) = ( s_i_new(ji) - sm_i_1d(ji) ) * dh_i_bott(ji) / MAX( ht_i_1d(ji), epsi10 ) * rswitch |
---|
668 | ENDIF |
---|
669 | ENDIF |
---|
670 | |
---|
671 | ! Contribution to energy flux to the ocean [J/m2], >0 (if sst<0) |
---|
672 | ii = MOD( npb(ji) - 1, jpi ) + 1 ; ij = ( npb(ji) - 1 ) / jpi + 1 |
---|
673 | zfmdt = ( rhosn - rhoic ) * MAX( dh_snowice(ji), 0._wp ) ! <0 |
---|
674 | zsstK = sst_m(ii,ij) + rt0 |
---|
675 | zEw = rcp * ( zsstK - rt0 ) |
---|
676 | zQm = zfmdt * zEw |
---|
677 | |
---|
678 | ! Contribution to heat flux |
---|
679 | hfx_thd_1d(ji) = hfx_thd_1d(ji) + zfmdt * a_i_1d(ji) * zEw * r1_rdtice |
---|
680 | |
---|
681 | ! Contribution to salt flux |
---|
682 | sfx_sni_1d(ji) = sfx_sni_1d(ji) + sss_m(ii,ij) * a_i_1d(ji) * zfmdt * r1_rdtice |
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683 | |
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684 | ! Contribution to mass flux |
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685 | ! All snow is thrown in the ocean, and seawater is taken to replace the volume |
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686 | wfx_sni_1d(ji) = wfx_sni_1d(ji) - a_i_1d(ji) * dh_snowice(ji) * rhoic * r1_rdtice |
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687 | wfx_snw_1d(ji) = wfx_snw_1d(ji) + a_i_1d(ji) * dh_snowice(ji) * rhosn * r1_rdtice |
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688 | |
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689 | ! update heat content (J.m-2) and layer thickness |
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690 | qh_i_old(ji,0) = qh_i_old(ji,0) + dh_snowice(ji) * q_s_1d(ji,1) + zfmdt * zEw |
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691 | h_i_old (ji,0) = h_i_old (ji,0) + dh_snowice(ji) |
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692 | |
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693 | ! Total ablation (to debug) |
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694 | IF( ht_i_1d(ji) <= 0._wp ) a_i_1d(ji) = 0._wp |
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695 | |
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696 | END DO !ji |
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697 | |
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698 | ! |
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699 | !------------------------------------------- |
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700 | ! Update temperature, energy |
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701 | !------------------------------------------- |
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702 | !clem bug: we should take snow into account here |
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703 | DO ji = kideb, kiut |
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704 | rswitch = 1.0 - MAX( 0._wp , SIGN( 1._wp , - ht_i_1d(ji) ) ) |
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705 | t_su_1d(ji) = rswitch * t_su_1d(ji) + ( 1.0 - rswitch ) * rtt |
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706 | END DO ! ji |
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707 | |
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708 | DO jk = 1, nlay_s |
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709 | DO ji = kideb,kiut |
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710 | ! mask enthalpy |
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711 | rswitch = MAX( 0._wp , SIGN( 1._wp, - ht_s_1d(ji) ) ) |
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712 | q_s_1d(ji,jk) = ( 1.0 - rswitch ) * q_s_1d(ji,jk) |
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713 | ! recalculate t_s_1d from q_s_1d |
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714 | t_s_1d(ji,jk) = rtt + ( 1._wp - rswitch ) * ( - q_s_1d(ji,jk) / ( rhosn * cpic ) + lfus / cpic ) |
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715 | END DO |
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716 | END DO |
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717 | |
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718 | CALL wrk_dealloc( jpij, zh_s, zqprec, zq_su, zq_bo, zf_tt, zq_1cat, zq_rema ) |
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719 | CALL wrk_dealloc( jpij, zdh_s_mel, zdh_s_pre, zdh_s_sub, zqh_i, zqh_s, zq_s ) |
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720 | CALL wrk_dealloc( jpij, nlay_i+1, zdeltah, zh_i ) |
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721 | CALL wrk_dealloc( jpij, icount ) |
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722 | ! |
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723 | ! |
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724 | END SUBROUTINE lim_thd_dh |
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725 | |
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726 | #else |
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727 | !!---------------------------------------------------------------------- |
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728 | !! Default option NO LIM3 sea-ice model |
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729 | !!---------------------------------------------------------------------- |
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730 | CONTAINS |
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731 | SUBROUTINE lim_thd_dh ! Empty routine |
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732 | END SUBROUTINE lim_thd_dh |
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733 | #endif |
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734 | |
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735 | !!====================================================================== |
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736 | END MODULE limthd_dh |
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