[825] | 1 | MODULE limthd_lac |
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| 2 | !!====================================================================== |
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| 3 | !! *** MODULE limthd_lac *** |
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| 4 | !! lateral thermodynamic growth of the ice |
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| 5 | !!====================================================================== |
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[2715] | 6 | !! History : LIM ! 2005-12 (M. Vancoppenolle) Original code |
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| 7 | !! - ! 2006-01 (M. Vancoppenolle) add ITD |
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| 8 | !! 3.0 ! 2007-07 (M. Vancoppenolle) Mass and energy conservation tested |
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| 9 | !! 4.0 ! 2011-02 (G. Madec) dynamical allocation |
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| 10 | !!---------------------------------------------------------------------- |
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[888] | 11 | #if defined key_lim3 |
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[825] | 12 | !!---------------------------------------------------------------------- |
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[2528] | 13 | !! 'key_lim3' LIM3 sea-ice model |
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| 14 | !!---------------------------------------------------------------------- |
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[3625] | 15 | !! lim_lat_acr : lateral accretion of ice |
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[2528] | 16 | !!---------------------------------------------------------------------- |
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[3625] | 17 | USE par_oce ! ocean parameters |
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| 18 | USE dom_oce ! domain variables |
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| 19 | USE phycst ! physical constants |
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| 20 | USE sbc_oce ! Surface boundary condition: ocean fields |
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| 21 | USE sbc_ice ! Surface boundary condition: ice fields |
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| 22 | USE thd_ice ! LIM thermodynamics |
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| 23 | USE ice ! LIM variables |
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| 24 | USE limtab ! LIM 2D <==> 1D |
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| 25 | USE limcons ! LIM conservation |
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| 26 | USE in_out_manager ! I/O manager |
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| 27 | USE lib_mpp ! MPP library |
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[4833] | 28 | USE lbclnk ! ocean lateral boundary conditions (or mpp link) |
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[3625] | 29 | USE lib_fortran ! Fortran utilities (allows no signed zero when 'key_nosignedzero' defined) |
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[4688] | 30 | USE limthd_ent |
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[5167] | 31 | USE limvar |
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[921] | 32 | |
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[825] | 33 | IMPLICIT NONE |
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| 34 | PRIVATE |
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| 35 | |
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| 36 | PUBLIC lim_thd_lac ! called by lim_thd |
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| 37 | |
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| 38 | !!---------------------------------------------------------------------- |
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[4161] | 39 | !! NEMO/LIM3 4.0 , UCL - NEMO Consortium (2011) |
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[1156] | 40 | !! $Id$ |
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[2715] | 41 | !! Software governed by the CeCILL licence (NEMOGCM/NEMO_CeCILL.txt) |
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[825] | 42 | !!---------------------------------------------------------------------- |
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| 43 | CONTAINS |
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[921] | 44 | |
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[825] | 45 | SUBROUTINE lim_thd_lac |
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| 46 | !!------------------------------------------------------------------- |
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| 47 | !! *** ROUTINE lim_thd_lac *** |
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| 48 | !! |
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| 49 | !! ** Purpose : Computation of the evolution of the ice thickness and |
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| 50 | !! concentration as a function of the heat balance in the leads. |
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| 51 | !! It is only used for lateral accretion |
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| 52 | !! |
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| 53 | !! ** Method : Ice is formed in the open water when ocean lose heat |
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| 54 | !! (heat budget of open water Bl is negative) . |
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| 55 | !! Computation of the increase of 1-A (ice concentration) fol- |
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| 56 | !! lowing the law : |
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| 57 | !! (dA/dt)acc = F[ (1-A)/(1-a) ] * [ Bl / (Li*h0) ] |
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| 58 | !! where - h0 is the thickness of ice created in the lead |
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| 59 | !! - a is a minimum fraction for leads |
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| 60 | !! - F is a monotonic non-increasing function defined as: |
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| 61 | !! F(X)=( 1 - X**exld )**(1.0/exld) |
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| 62 | !! - exld is the exponent closure rate (=2 default val.) |
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| 63 | !! |
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| 64 | !! ** Action : - Adjustment of snow and ice thicknesses and heat |
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| 65 | !! content in brine pockets |
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| 66 | !! - Updating ice internal temperature |
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| 67 | !! - Computation of variation of ice volume and mass |
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| 68 | !! - Computation of frldb after lateral accretion and |
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[4872] | 69 | !! update ht_s_1d, ht_i_1d and tbif_1d(:,:) |
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[825] | 70 | !!------------------------------------------------------------------------ |
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[7646] | 71 | INTEGER :: ji,jj,jk,jl ! dummy loop indices |
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| 72 | INTEGER :: nbpac ! local integers |
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| 73 | INTEGER :: ii, ij, iter ! - - |
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| 74 | REAL(wp) :: ztmelts, zdv, zfrazb, zweight, zde ! local scalars |
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[6416] | 75 | REAL(wp) :: zgamafr, zvfrx, zvgx, ztaux, ztwogp, zf ! - - |
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[2715] | 76 | REAL(wp) :: ztenagm, zvfry, zvgy, ztauy, zvrel2, zfp, zsqcd , zhicrit ! - - |
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| 77 | CHARACTER (len = 15) :: fieldid |
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[4688] | 78 | |
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| 79 | REAL(wp) :: zQm ! enthalpy exchanged with the ocean (J/m2, >0 towards ocean) |
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| 80 | REAL(wp) :: zEi ! sea ice specific enthalpy (J/kg) |
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| 81 | REAL(wp) :: zEw ! seawater specific enthalpy (J/kg) |
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| 82 | REAL(wp) :: zfmdt ! mass flux x time step (kg/m2, >0 towards ocean) |
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| 83 | |
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| 84 | REAL(wp) :: zv_newfra |
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| 85 | |
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[7910] | 86 | INTEGER , DIMENSION(jpij) :: jcat ! indexes of categories where new ice grows |
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| 87 | REAL(wp), DIMENSION(jpij) :: zswinew ! switch for new ice or not |
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[825] | 88 | |
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[7910] | 89 | REAL(wp), DIMENSION(jpij) :: zv_newice ! volume of accreted ice |
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| 90 | REAL(wp), DIMENSION(jpij) :: za_newice ! fractional area of accreted ice |
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| 91 | REAL(wp), DIMENSION(jpij) :: zh_newice ! thickness of accreted ice |
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| 92 | REAL(wp), DIMENSION(jpij) :: ze_newice ! heat content of accreted ice |
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| 93 | REAL(wp), DIMENSION(jpij) :: zs_newice ! salinity of accreted ice |
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| 94 | REAL(wp), DIMENSION(jpij) :: zo_newice ! age of accreted ice |
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| 95 | REAL(wp), DIMENSION(jpij) :: zdv_res ! residual volume in case of excessive heat budget |
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| 96 | REAL(wp), DIMENSION(jpij) :: zda_res ! residual area in case of excessive heat budget |
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| 97 | REAL(wp), DIMENSION(jpij) :: zat_i_1d ! total ice fraction |
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| 98 | REAL(wp), DIMENSION(jpij) :: zv_frazb ! accretion of frazil ice at the ice bottom |
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| 99 | REAL(wp), DIMENSION(jpij) :: zvrel_1d ! relative ice / frazil velocity (1D vector) |
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[825] | 100 | |
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[7910] | 101 | REAL(wp), DIMENSION(jpij,jpl) :: zv_b ! old volume of ice in category jl |
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| 102 | REAL(wp), DIMENSION(jpij,jpl) :: za_b ! old area of ice in category jl |
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| 103 | REAL(wp), DIMENSION(jpij,jpl) :: za_i_1d ! 1-D version of a_i |
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| 104 | REAL(wp), DIMENSION(jpij,jpl) :: zv_i_1d ! 1-D version of v_i |
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| 105 | REAL(wp), DIMENSION(jpij,jpl) :: zsmv_i_1d ! 1-D version of smv_i |
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[825] | 106 | |
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[7910] | 107 | REAL(wp), DIMENSION(jpij,nlay_i,jpl) :: ze_i_1d !: 1-D version of e_i |
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[825] | 108 | |
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[7910] | 109 | REAL(wp), DIMENSION(jpi,jpj) :: zvrel ! relative ice / frazil velocity |
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[5123] | 110 | |
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[6416] | 111 | REAL(wp) :: zcai = 1.4e-3_wp ! ice-air drag (clem: should be dependent on coupling/forcing used) |
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[3294] | 112 | !!-----------------------------------------------------------------------! |
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[825] | 113 | |
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[3294] | 114 | |
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[5167] | 115 | CALL lim_var_agg(1) |
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| 116 | CALL lim_var_glo2eqv |
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[921] | 117 | !------------------------------------------------------------------------------| |
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| 118 | ! 2) Convert units for ice internal energy |
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| 119 | !------------------------------------------------------------------------------| |
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[825] | 120 | DO jl = 1, jpl |
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[921] | 121 | DO jk = 1, nlay_i |
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| 122 | DO jj = 1, jpj |
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| 123 | DO ji = 1, jpi |
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| 124 | !Energy of melting q(S,T) [J.m-3] |
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[5134] | 125 | rswitch = MAX( 0._wp , SIGN( 1._wp , v_i(ji,jj,jl) - epsi20 ) ) !0 if no ice |
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[5123] | 126 | e_i(ji,jj,jk,jl) = rswitch * e_i(ji,jj,jk,jl) / MAX( v_i(ji,jj,jl), epsi20 ) * REAL( nlay_i, wp ) |
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[921] | 127 | END DO |
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[825] | 128 | END DO |
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[921] | 129 | END DO |
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[825] | 130 | END DO |
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| 131 | |
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[921] | 132 | !------------------------------------------------------------------------------! |
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| 133 | ! 3) Collection thickness of ice formed in leads and polynyas |
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| 134 | !------------------------------------------------------------------------------! |
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[865] | 135 | ! hicol is the thickness of new ice formed in open water |
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[6416] | 136 | ! hicol can be either prescribed (frazswi = 0) or computed (frazswi = 1) |
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[825] | 137 | ! Frazil ice forms in open water, is transported by wind |
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| 138 | ! accumulates at the edge of the consolidated ice edge |
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| 139 | ! where it forms aggregates of a specific thickness called |
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| 140 | ! collection thickness. |
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| 141 | |
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[865] | 142 | ! Note : the following algorithm currently breaks vectorization |
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| 143 | ! |
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| 144 | |
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[7753] | 145 | zvrel(:,:) = 0._wp |
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[825] | 146 | |
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[7753] | 147 | ! Default new ice thickness |
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| 148 | WHERE( qlead(:,:) < 0._wp ) ; hicol(:,:) = rn_hnewice |
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| 149 | ELSEWHERE ; hicol(:,:) = 0._wp |
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| 150 | END WHERE |
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[825] | 151 | |
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[5123] | 152 | IF( ln_frazil ) THEN |
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[825] | 153 | |
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[921] | 154 | !-------------------- |
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| 155 | ! Physical constants |
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| 156 | !-------------------- |
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[7753] | 157 | hicol(:,:) = 0._wp |
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[825] | 158 | |
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[921] | 159 | zhicrit = 0.04 ! frazil ice thickness |
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| 160 | ztwogp = 2. * rau0 / ( grav * 0.3 * ( rau0 - rhoic ) ) ! reduced grav |
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[5123] | 161 | zsqcd = 1.0 / SQRT( 1.3 * zcai ) ! 1/SQRT(airdensity*drag) |
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[921] | 162 | zgamafr = 0.03 |
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[825] | 163 | |
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[7646] | 164 | DO jj = 2, jpjm1 |
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| 165 | DO ji = 2, jpim1 |
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| 166 | IF ( qlead(ji,jj) < 0._wp .AND. tau_icebfr(ji,jj) == 0._wp ) THEN ! activated if cooling and no landfast |
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[921] | 167 | !------------- |
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| 168 | ! Wind stress |
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| 169 | !------------- |
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| 170 | ! C-grid wind stress components |
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[5123] | 171 | ztaux = ( utau_ice(ji-1,jj ) * umask(ji-1,jj ,1) & |
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| 172 | & + utau_ice(ji ,jj ) * umask(ji ,jj ,1) ) * 0.5_wp |
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| 173 | ztauy = ( vtau_ice(ji ,jj-1) * vmask(ji ,jj-1,1) & |
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| 174 | & + vtau_ice(ji ,jj ) * vmask(ji ,jj ,1) ) * 0.5_wp |
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[921] | 175 | ! Square root of wind stress |
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[6416] | 176 | ztenagm = SQRT( SQRT( ztaux * ztaux + ztauy * ztauy ) ) |
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[825] | 177 | |
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[921] | 178 | !--------------------- |
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| 179 | ! Frazil ice velocity |
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| 180 | !--------------------- |
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[4990] | 181 | rswitch = MAX( 0._wp, SIGN( 1._wp , ztenagm - epsi10 ) ) |
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| 182 | zvfrx = rswitch * zgamafr * zsqcd * ztaux / MAX( ztenagm, epsi10 ) |
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| 183 | zvfry = rswitch * zgamafr * zsqcd * ztauy / MAX( ztenagm, epsi10 ) |
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[825] | 184 | |
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[921] | 185 | !------------------- |
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| 186 | ! Pack ice velocity |
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| 187 | !------------------- |
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| 188 | ! C-grid ice velocity |
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[7646] | 189 | zvgx = ( u_ice(ji-1,jj ) * umask(ji-1,jj ,1) + u_ice(ji,jj) * umask(ji,jj,1) ) * 0.5_wp |
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| 190 | zvgy = ( v_ice(ji ,jj-1) * vmask(ji ,jj-1,1) + v_ice(ji,jj) * vmask(ji,jj,1) ) * 0.5_wp |
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[825] | 191 | |
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[921] | 192 | !----------------------------------- |
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| 193 | ! Relative frazil/pack ice velocity |
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| 194 | !----------------------------------- |
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| 195 | ! absolute relative velocity |
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[7646] | 196 | rswitch = MAX( 0._wp, SIGN( 1._wp , at_i(ji,jj) - epsi10 ) ) |
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| 197 | zvrel2 = MAX( ( zvfrx - zvgx ) * ( zvfrx - zvgx ) & |
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| 198 | & + ( zvfry - zvgy ) * ( zvfry - zvgy ) , 0.15 * 0.15 ) * rswitch |
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[6416] | 199 | zvrel(ji,jj) = SQRT( zvrel2 ) |
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[825] | 200 | |
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[921] | 201 | !--------------------- |
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| 202 | ! Iterative procedure |
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| 203 | !--------------------- |
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[6416] | 204 | hicol(ji,jj) = zhicrit + ( zhicrit + 0.1 ) & |
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| 205 | & / ( ( zhicrit + 0.1 ) * ( zhicrit + 0.1 ) - zhicrit * zhicrit ) * ztwogp * zvrel2 |
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[825] | 206 | |
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[921] | 207 | iter = 1 |
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[6416] | 208 | DO WHILE ( iter < 20 ) |
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| 209 | zf = ( hicol(ji,jj) - zhicrit ) * ( hicol(ji,jj) * hicol(ji,jj) - zhicrit * zhicrit ) - & |
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| 210 | & hicol(ji,jj) * zhicrit * ztwogp * zvrel2 |
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| 211 | zfp = ( hicol(ji,jj) - zhicrit ) * ( 3.0 * hicol(ji,jj) + zhicrit ) - zhicrit * ztwogp * zvrel2 |
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[825] | 212 | |
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[7646] | 213 | hicol(ji,jj) = hicol(ji,jj) - zf / MAX( zfp, epsi20 ) |
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[921] | 214 | iter = iter + 1 |
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[6416] | 215 | END DO |
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[825] | 216 | |
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[921] | 217 | ENDIF ! end of selection of pixels where ice forms |
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[825] | 218 | |
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[6416] | 219 | END DO |
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| 220 | END DO |
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| 221 | ! |
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[7646] | 222 | CALL lbc_lnk( zvrel, 'T', 1. ) |
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| 223 | CALL lbc_lnk( hicol, 'T', 1. ) |
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[825] | 224 | |
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| 225 | ENDIF ! End of computation of frazil ice collection thickness |
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| 226 | |
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[921] | 227 | !------------------------------------------------------------------------------! |
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| 228 | ! 4) Identify grid points where new ice forms |
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| 229 | !------------------------------------------------------------------------------! |
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[825] | 230 | |
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| 231 | !------------------------------------- |
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| 232 | ! Select points for new ice formation |
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| 233 | !------------------------------------- |
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[7646] | 234 | ! This occurs if open water energy budget is negative (cooling) and there is no landfast ice |
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[825] | 235 | nbpac = 0 |
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[4833] | 236 | npac(:) = 0 |
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| 237 | ! |
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[825] | 238 | DO jj = 1, jpj |
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| 239 | DO ji = 1, jpi |
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[7646] | 240 | IF ( qlead(ji,jj) < 0._wp .AND. tau_icebfr(ji,jj) == 0._wp ) THEN |
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[825] | 241 | nbpac = nbpac + 1 |
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| 242 | npac( nbpac ) = (jj - 1) * jpi + ji |
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| 243 | ENDIF |
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| 244 | END DO |
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| 245 | END DO |
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| 246 | |
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[4333] | 247 | ! debug point to follow |
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| 248 | jiindex_1d = 0 |
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[7646] | 249 | IF( ln_limctl ) THEN |
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[5128] | 250 | DO ji = mi0(iiceprt), mi1(iiceprt) |
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| 251 | DO jj = mj0(jiceprt), mj1(jiceprt) |
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[4688] | 252 | IF ( qlead(ji,jj) < 0._wp ) THEN |
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[4333] | 253 | jiindex_1d = (jj - 1) * jpi + ji |
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| 254 | ENDIF |
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| 255 | END DO |
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| 256 | END DO |
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| 257 | ENDIF |
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| 258 | |
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[7646] | 259 | IF( ln_limctl ) WRITE(numout,*) 'lim_thd_lac : nbpac = ', nbpac |
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[825] | 260 | |
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| 261 | !------------------------------ |
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| 262 | ! Move from 2-D to 1-D vectors |
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| 263 | !------------------------------ |
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[6416] | 264 | ! If ocean gains heat do nothing. Otherwise compute new ice formation |
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[825] | 265 | |
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| 266 | IF ( nbpac > 0 ) THEN |
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| 267 | |
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[4688] | 268 | CALL tab_2d_1d( nbpac, zat_i_1d (1:nbpac) , at_i , jpi, jpj, npac(1:nbpac) ) |
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[921] | 269 | DO jl = 1, jpl |
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[4688] | 270 | CALL tab_2d_1d( nbpac, za_i_1d (1:nbpac,jl), a_i (:,:,jl), jpi, jpj, npac(1:nbpac) ) |
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| 271 | CALL tab_2d_1d( nbpac, zv_i_1d (1:nbpac,jl), v_i (:,:,jl), jpi, jpj, npac(1:nbpac) ) |
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| 272 | CALL tab_2d_1d( nbpac, zsmv_i_1d(1:nbpac,jl), smv_i(:,:,jl), jpi, jpj, npac(1:nbpac) ) |
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[921] | 273 | DO jk = 1, nlay_i |
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[4688] | 274 | CALL tab_2d_1d( nbpac, ze_i_1d(1:nbpac,jk,jl), e_i(:,:,jk,jl) , jpi, jpj, npac(1:nbpac) ) |
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[5202] | 275 | END DO |
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| 276 | END DO |
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[825] | 277 | |
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[6403] | 278 | CALL tab_2d_1d( nbpac, qlead_1d (1:nbpac) , qlead , jpi, jpj, npac(1:nbpac) ) |
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| 279 | CALL tab_2d_1d( nbpac, t_bo_1d (1:nbpac) , t_bo , jpi, jpj, npac(1:nbpac) ) |
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| 280 | CALL tab_2d_1d( nbpac, sfx_opw_1d(1:nbpac) , sfx_opw , jpi, jpj, npac(1:nbpac) ) |
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| 281 | CALL tab_2d_1d( nbpac, wfx_opw_1d(1:nbpac) , wfx_opw , jpi, jpj, npac(1:nbpac) ) |
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| 282 | CALL tab_2d_1d( nbpac, hicol_1d (1:nbpac) , hicol , jpi, jpj, npac(1:nbpac) ) |
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| 283 | CALL tab_2d_1d( nbpac, zvrel_1d (1:nbpac) , zvrel , jpi, jpj, npac(1:nbpac) ) |
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[834] | 284 | |
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[6403] | 285 | CALL tab_2d_1d( nbpac, hfx_thd_1d(1:nbpac) , hfx_thd , jpi, jpj, npac(1:nbpac) ) |
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| 286 | CALL tab_2d_1d( nbpac, hfx_opw_1d(1:nbpac) , hfx_opw , jpi, jpj, npac(1:nbpac) ) |
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| 287 | CALL tab_2d_1d( nbpac, rn_amax_1d(1:nbpac) , rn_amax_2d, jpi, jpj, npac(1:nbpac) ) |
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[4688] | 288 | |
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[921] | 289 | !------------------------------------------------------------------------------! |
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| 290 | ! 5) Compute thickness, salinity, enthalpy, age, area and volume of new ice |
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| 291 | !------------------------------------------------------------------------------! |
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[825] | 292 | |
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[4688] | 293 | !----------------------------------------- |
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| 294 | ! Keep old ice areas and volume in memory |
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| 295 | !----------------------------------------- |
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[4872] | 296 | zv_b(1:nbpac,:) = zv_i_1d(1:nbpac,:) |
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| 297 | za_b(1:nbpac,:) = za_i_1d(1:nbpac,:) |
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[6416] | 298 | |
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[921] | 299 | !---------------------- |
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| 300 | ! Thickness of new ice |
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| 301 | !---------------------- |
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[6416] | 302 | zh_newice(1:nbpac) = hicol_1d(1:nbpac) |
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[825] | 303 | |
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[921] | 304 | !---------------------- |
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| 305 | ! Salinity of new ice |
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| 306 | !---------------------- |
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[5123] | 307 | SELECT CASE ( nn_icesal ) |
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[3625] | 308 | CASE ( 1 ) ! Sice = constant |
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[5123] | 309 | zs_newice(1:nbpac) = rn_icesal |
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[3625] | 310 | CASE ( 2 ) ! Sice = F(z,t) [Vancoppenolle et al (2005)] |
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[921] | 311 | DO ji = 1, nbpac |
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[4161] | 312 | ii = MOD( npac(ji) - 1 , jpi ) + 1 |
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| 313 | ij = ( npac(ji) - 1 ) / jpi + 1 |
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[5123] | 314 | zs_newice(ji) = MIN( 4.606 + 0.91 / zh_newice(ji) , rn_simax , 0.5 * sss_m(ii,ij) ) |
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[3625] | 315 | END DO |
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| 316 | CASE ( 3 ) ! Sice = F(z) [multiyear ice] |
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[4833] | 317 | zs_newice(1:nbpac) = 2.3 |
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[3625] | 318 | END SELECT |
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[825] | 319 | |
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[921] | 320 | !------------------------- |
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| 321 | ! Heat content of new ice |
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| 322 | !------------------------- |
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| 323 | ! We assume that new ice is formed at the seawater freezing point |
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| 324 | DO ji = 1, nbpac |
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[5123] | 325 | ztmelts = - tmut * zs_newice(ji) + rt0 ! Melting point (K) |
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[6416] | 326 | ze_newice(ji) = rhoic * ( cpic * ( ztmelts - t_bo_1d(ji) ) & |
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[5123] | 327 | & + lfus * ( 1.0 - ( ztmelts - rt0 ) / MIN( t_bo_1d(ji) - rt0, -epsi10 ) ) & |
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| 328 | & - rcp * ( ztmelts - rt0 ) ) |
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| 329 | END DO |
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[4688] | 330 | |
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[921] | 331 | !---------------- |
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| 332 | ! Age of new ice |
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| 333 | !---------------- |
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| 334 | DO ji = 1, nbpac |
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[3625] | 335 | zo_newice(ji) = 0._wp |
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[5202] | 336 | END DO |
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[825] | 337 | |
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[921] | 338 | !------------------- |
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| 339 | ! Volume of new ice |
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| 340 | !------------------- |
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| 341 | DO ji = 1, nbpac |
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[825] | 342 | |
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[5123] | 343 | zEi = - ze_newice(ji) * r1_rhoic ! specific enthalpy of forming ice [J/kg] |
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[4688] | 344 | |
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[5123] | 345 | zEw = rcp * ( t_bo_1d(ji) - rt0 ) ! specific enthalpy of seawater at t_bo_1d [J/kg] |
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[4688] | 346 | ! clem: we suppose we are already at the freezing point (condition qlead<0 is satisfyied) |
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| 347 | |
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| 348 | zdE = zEi - zEw ! specific enthalpy difference [J/kg] |
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| 349 | |
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| 350 | zfmdt = - qlead_1d(ji) / zdE ! Fm.dt [kg/m2] (<0) |
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| 351 | ! clem: we use qlead instead of zqld (limthd) because we suppose we are at the freezing point |
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[5123] | 352 | zv_newice(ji) = - zfmdt * r1_rhoic |
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[4688] | 353 | |
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| 354 | zQm = zfmdt * zEw ! heat to the ocean >0 associated with mass flux |
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| 355 | |
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| 356 | ! Contribution to heat flux to the ocean [W.m-2], >0 |
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| 357 | hfx_thd_1d(ji) = hfx_thd_1d(ji) + zfmdt * zEw * r1_rdtice |
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| 358 | ! Total heat flux used in this process [W.m-2] |
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| 359 | hfx_opw_1d(ji) = hfx_opw_1d(ji) - zfmdt * zdE * r1_rdtice |
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| 360 | ! mass flux |
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| 361 | wfx_opw_1d(ji) = wfx_opw_1d(ji) - zv_newice(ji) * rhoic * r1_rdtice |
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| 362 | ! salt flux |
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| 363 | sfx_opw_1d(ji) = sfx_opw_1d(ji) - zv_newice(ji) * rhoic * zs_newice(ji) * r1_rdtice |
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[6416] | 364 | END DO |
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| 365 | |
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| 366 | zv_frazb(:) = 0._wp |
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| 367 | IF( ln_frazil ) THEN |
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[921] | 368 | ! A fraction zfrazb of frazil ice is accreted at the ice bottom |
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[6416] | 369 | DO ji = 1, nbpac |
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| 370 | rswitch = 1._wp - MAX( 0._wp, SIGN( 1._wp , - zat_i_1d(ji) ) ) |
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| 371 | zfrazb = rswitch * ( TANH( rn_Cfrazb * ( zvrel_1d(ji) - rn_vfrazb ) ) + 1.0 ) * 0.5 * rn_maxfrazb |
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| 372 | zv_frazb(ji) = zfrazb * zv_newice(ji) |
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| 373 | zv_newice(ji) = ( 1.0 - zfrazb ) * zv_newice(ji) |
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| 374 | END DO |
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| 375 | END IF |
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| 376 | |
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[921] | 377 | !----------------- |
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| 378 | ! Area of new ice |
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| 379 | !----------------- |
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| 380 | DO ji = 1, nbpac |
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[3625] | 381 | za_newice(ji) = zv_newice(ji) / zh_newice(ji) |
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[4688] | 382 | END DO |
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[825] | 383 | |
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[921] | 384 | !------------------------------------------------------------------------------! |
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| 385 | ! 6) Redistribute new ice area and volume into ice categories ! |
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| 386 | !------------------------------------------------------------------------------! |
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[825] | 387 | |
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[4688] | 388 | !------------------------ |
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| 389 | ! 6.1) lateral ice growth |
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| 390 | !------------------------ |
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[921] | 391 | ! If lateral ice growth gives an ice concentration gt 1, then |
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[3625] | 392 | ! we keep the excessive volume in memory and attribute it later to bottom accretion |
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[921] | 393 | DO ji = 1, nbpac |
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[6403] | 394 | IF ( za_newice(ji) > ( rn_amax_1d(ji) - zat_i_1d(ji) ) ) THEN |
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| 395 | zda_res(ji) = za_newice(ji) - ( rn_amax_1d(ji) - zat_i_1d(ji) ) |
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[3625] | 396 | zdv_res(ji) = zda_res (ji) * zh_newice(ji) |
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| 397 | za_newice(ji) = za_newice(ji) - zda_res (ji) |
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| 398 | zv_newice(ji) = zv_newice(ji) - zdv_res (ji) |
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[921] | 399 | ELSE |
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[3625] | 400 | zda_res(ji) = 0._wp |
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| 401 | zdv_res(ji) = 0._wp |
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[921] | 402 | ENDIF |
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[4688] | 403 | END DO |
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[825] | 404 | |
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[4688] | 405 | ! find which category to fill |
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| 406 | zat_i_1d(:) = 0._wp |
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[921] | 407 | DO jl = 1, jpl |
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| 408 | DO ji = 1, nbpac |
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[4688] | 409 | IF( zh_newice(ji) > hi_max(jl-1) .AND. zh_newice(ji) <= hi_max(jl) ) THEN |
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| 410 | za_i_1d (ji,jl) = za_i_1d (ji,jl) + za_newice(ji) |
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| 411 | zv_i_1d (ji,jl) = zv_i_1d (ji,jl) + zv_newice(ji) |
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| 412 | jcat (ji) = jl |
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[921] | 413 | ENDIF |
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[4688] | 414 | zat_i_1d(ji) = zat_i_1d(ji) + za_i_1d (ji,jl) |
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[3625] | 415 | END DO |
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| 416 | END DO |
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[825] | 417 | |
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[4688] | 418 | ! Heat content |
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[921] | 419 | DO ji = 1, nbpac |
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[4688] | 420 | jl = jcat(ji) ! categroy in which new ice is put |
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[4872] | 421 | zswinew (ji) = MAX( 0._wp , SIGN( 1._wp , - za_b(ji,jl) ) ) ! 0 if old ice |
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[921] | 422 | END DO |
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[825] | 423 | |
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[921] | 424 | DO jk = 1, nlay_i |
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| 425 | DO ji = 1, nbpac |
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[4688] | 426 | jl = jcat(ji) |
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[4990] | 427 | rswitch = MAX( 0._wp, SIGN( 1._wp , zv_i_1d(ji,jl) - epsi20 ) ) |
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[6416] | 428 | ze_i_1d(ji,jk,jl) = zswinew(ji) * ze_newice(ji) + & |
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[4872] | 429 | & ( 1.0 - zswinew(ji) ) * ( ze_newice(ji) * zv_newice(ji) + ze_i_1d(ji,jk,jl) * zv_b(ji,jl) ) & |
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[4990] | 430 | & * rswitch / MAX( zv_i_1d(ji,jl), epsi20 ) |
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[2715] | 431 | END DO |
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| 432 | END DO |
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[825] | 433 | |
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[4688] | 434 | !------------------------------------------------ |
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| 435 | ! 6.2) bottom ice growth + ice enthalpy remapping |
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| 436 | !------------------------------------------------ |
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| 437 | DO jl = 1, jpl |
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[825] | 438 | |
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[4688] | 439 | ! for remapping |
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| 440 | h_i_old (1:nbpac,0:nlay_i+1) = 0._wp |
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| 441 | qh_i_old(1:nbpac,0:nlay_i+1) = 0._wp |
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[921] | 442 | DO jk = 1, nlay_i |
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| 443 | DO ji = 1, nbpac |
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[5123] | 444 | h_i_old (ji,jk) = zv_i_1d(ji,jl) * r1_nlay_i |
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[4688] | 445 | qh_i_old(ji,jk) = ze_i_1d(ji,jk,jl) * h_i_old(ji,jk) |
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[2715] | 446 | END DO |
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| 447 | END DO |
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[4688] | 448 | |
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| 449 | ! new volumes including lateral/bottom accretion + residual |
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[921] | 450 | DO ji = 1, nbpac |
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[4990] | 451 | rswitch = MAX( 0._wp, SIGN( 1._wp , zat_i_1d(ji) - epsi20 ) ) |
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| 452 | zv_newfra = rswitch * ( zdv_res(ji) + zv_frazb(ji) ) * za_i_1d(ji,jl) / MAX( zat_i_1d(ji) , epsi20 ) |
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| 453 | za_i_1d(ji,jl) = rswitch * za_i_1d(ji,jl) |
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[4688] | 454 | zv_i_1d(ji,jl) = zv_i_1d(ji,jl) + zv_newfra |
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| 455 | ! for remapping |
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| 456 | h_i_old (ji,nlay_i+1) = zv_newfra |
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| 457 | qh_i_old(ji,nlay_i+1) = ze_newice(ji) * zv_newfra |
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| 458 | ENDDO |
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| 459 | ! --- Ice enthalpy remapping --- ! |
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[4833] | 460 | CALL lim_thd_ent( 1, nbpac, ze_i_1d(1:nbpac,:,jl) ) |
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[4688] | 461 | ENDDO |
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| 462 | |
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[921] | 463 | !----------------- |
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| 464 | ! Update salinity |
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| 465 | !----------------- |
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[4161] | 466 | DO jl = 1, jpl |
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| 467 | DO ji = 1, nbpac |
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[4872] | 468 | zdv = zv_i_1d(ji,jl) - zv_b(ji,jl) |
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[4688] | 469 | zsmv_i_1d(ji,jl) = zsmv_i_1d(ji,jl) + zdv * zs_newice(ji) |
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| 470 | END DO |
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[4161] | 471 | END DO |
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| 472 | |
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[921] | 473 | !------------------------------------------------------------------------------! |
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[4688] | 474 | ! 7) Change 2D vectors to 1D vectors |
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[921] | 475 | !------------------------------------------------------------------------------! |
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| 476 | DO jl = 1, jpl |
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[4688] | 477 | CALL tab_1d_2d( nbpac, a_i (:,:,jl), npac(1:nbpac), za_i_1d (1:nbpac,jl), jpi, jpj ) |
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| 478 | CALL tab_1d_2d( nbpac, v_i (:,:,jl), npac(1:nbpac), zv_i_1d (1:nbpac,jl), jpi, jpj ) |
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| 479 | CALL tab_1d_2d( nbpac, smv_i (:,:,jl), npac(1:nbpac), zsmv_i_1d(1:nbpac,jl) , jpi, jpj ) |
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[921] | 480 | DO jk = 1, nlay_i |
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[4688] | 481 | CALL tab_1d_2d( nbpac, e_i(:,:,jk,jl), npac(1:nbpac), ze_i_1d(1:nbpac,jk,jl), jpi, jpj ) |
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[2715] | 482 | END DO |
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| 483 | END DO |
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[4688] | 484 | CALL tab_1d_2d( nbpac, sfx_opw, npac(1:nbpac), sfx_opw_1d(1:nbpac), jpi, jpj ) |
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| 485 | CALL tab_1d_2d( nbpac, wfx_opw, npac(1:nbpac), wfx_opw_1d(1:nbpac), jpi, jpj ) |
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| 486 | |
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| 487 | CALL tab_1d_2d( nbpac, hfx_thd, npac(1:nbpac), hfx_thd_1d(1:nbpac), jpi, jpj ) |
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| 488 | CALL tab_1d_2d( nbpac, hfx_opw, npac(1:nbpac), hfx_opw_1d(1:nbpac), jpi, jpj ) |
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[2715] | 489 | ! |
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[921] | 490 | ENDIF ! nbpac > 0 |
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[825] | 491 | |
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[921] | 492 | !------------------------------------------------------------------------------! |
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[4688] | 493 | ! 8) Change units for e_i |
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[921] | 494 | !------------------------------------------------------------------------------! |
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[825] | 495 | DO jl = 1, jpl |
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[4688] | 496 | DO jk = 1, nlay_i |
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| 497 | DO jj = 1, jpj |
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| 498 | DO ji = 1, jpi |
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[5123] | 499 | ! heat content in J/m2 |
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| 500 | e_i(ji,jj,jk,jl) = e_i(ji,jj,jk,jl) * v_i(ji,jj,jl) * r1_nlay_i |
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[4688] | 501 | END DO |
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| 502 | END DO |
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[825] | 503 | END DO |
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| 504 | END DO |
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| 505 | |
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[2715] | 506 | ! |
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| 507 | ! |
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[825] | 508 | END SUBROUTINE lim_thd_lac |
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| 509 | |
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| 510 | #else |
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[2715] | 511 | !!---------------------------------------------------------------------- |
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| 512 | !! Default option NO LIM3 sea-ice model |
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| 513 | !!---------------------------------------------------------------------- |
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[825] | 514 | CONTAINS |
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| 515 | SUBROUTINE lim_thd_lac ! Empty routine |
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| 516 | END SUBROUTINE lim_thd_lac |
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| 517 | #endif |
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[2715] | 518 | |
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| 519 | !!====================================================================== |
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[825] | 520 | END MODULE limthd_lac |
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