[825] | 1 | MODULE limthd_dh |
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[1572] | 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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[4688] | 8 | !! 3.2 ! 2009-07 (M. Vancoppenolle, Y. Aksenov, G. Madec) bug correction in wfx_snw & wfx_ice |
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[3625] | 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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[1572] | 11 | !!---------------------------------------------------------------------- |
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[825] | 12 | #if defined key_lim3 |
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[834] | 13 | !!---------------------------------------------------------------------- |
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| 14 | !! 'key_lim3' LIM3 sea-ice model |
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| 15 | !!---------------------------------------------------------------------- |
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[3625] | 16 | !! lim_thd_dh : vertical accr./abl. and lateral ablation of sea ice |
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[825] | 17 | !!---------------------------------------------------------------------- |
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[3625] | 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 thd_ice ! LIM thermodynamics |
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| 23 | USE in_out_manager ! I/O manager |
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| 24 | USE lib_mpp ! MPP library |
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| 25 | USE wrk_nemo ! work arrays |
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| 26 | USE lib_fortran ! Fortran utilities (allows no signed zero when 'key_nosignedzero' defined) |
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[4688] | 27 | |
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[825] | 28 | IMPLICIT NONE |
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| 29 | PRIVATE |
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| 30 | |
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[5407] | 31 | PUBLIC lim_thd_dh ! called by lim_thd |
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[5487] | 32 | PUBLIC lim_thd_snwblow ! called in sbcblk/sbcclio/sbccpl and here |
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[825] | 33 | |
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[5407] | 34 | INTERFACE lim_thd_snwblow |
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| 35 | MODULE PROCEDURE lim_thd_snwblow_1d, lim_thd_snwblow_2d |
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| 36 | END INTERFACE |
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| 37 | |
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[825] | 38 | !!---------------------------------------------------------------------- |
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[4161] | 39 | !! NEMO/LIM3 4.0 , UCL - NEMO Consortium (2010) |
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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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| 44 | |
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[4688] | 45 | SUBROUTINE lim_thd_dh( kideb, kiut ) |
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[921] | 46 | !!------------------------------------------------------------------ |
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| 47 | !! *** ROUTINE lim_thd_dh *** |
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| 48 | !! |
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[1572] | 49 | !! ** Purpose : determines variations of ice and snow thicknesses. |
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[921] | 50 | !! |
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[1572] | 51 | !! ** Method : Ice/Snow surface melting arises from imbalance in surface fluxes |
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| 52 | !! Bottom accretion/ablation arises from flux budget |
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| 53 | !! Snow thickness can increase by precipitation and decrease by sublimation |
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| 54 | !! If snow load excesses Archmiede limit, snow-ice is formed by |
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| 55 | !! the flooding of sea-water in the snow |
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[921] | 56 | !! |
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[1572] | 57 | !! 1) Compute available flux of heat for surface ablation |
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| 58 | !! 2) Compute snow and sea ice enthalpies |
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| 59 | !! 3) Surface ablation and sublimation |
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| 60 | !! 4) Bottom accretion/ablation |
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| 61 | !! 5) Case of Total ablation |
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| 62 | !! 6) Snow ice formation |
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[921] | 63 | !! |
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[1572] | 64 | !! References : Bitz and Lipscomb, 1999, J. Geophys. Res. |
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| 65 | !! Fichefet T. and M. Maqueda 1997, J. Geophys. Res., 102(C6), 12609-12646 |
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| 66 | !! Vancoppenolle, Fichefet and Bitz, 2005, Geophys. Res. Let. |
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| 67 | !! Vancoppenolle et al.,2009, Ocean Modelling |
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[921] | 68 | !!------------------------------------------------------------------ |
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[1572] | 69 | INTEGER , INTENT(in) :: kideb, kiut ! Start/End point on which the the computation is applied |
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| 70 | !! |
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| 71 | INTEGER :: ji , jk ! dummy loop indices |
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[4161] | 72 | INTEGER :: ii, ij ! 2D corresponding indices to ji |
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[1572] | 73 | INTEGER :: iter |
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[825] | 74 | |
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[4688] | 75 | REAL(wp) :: ztmelts ! local scalar |
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[6416] | 76 | REAL(wp) :: zdum |
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[1572] | 77 | REAL(wp) :: zfracs ! fractionation coefficient for bottom salt entrapment |
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| 78 | REAL(wp) :: zswi1 ! switch for computation of bottom salinity |
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| 79 | REAL(wp) :: zswi12 ! switch for computation of bottom salinity |
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| 80 | REAL(wp) :: zswi2 ! switch for computation of bottom salinity |
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| 81 | REAL(wp) :: zgrr ! bottom growth rate |
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[4688] | 82 | REAL(wp) :: zt_i_new ! bottom formation temperature |
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| 83 | |
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| 84 | REAL(wp) :: zQm ! enthalpy exchanged with the ocean (J/m2), >0 towards the ocean |
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| 85 | REAL(wp) :: zEi ! specific enthalpy of sea ice (J/kg) |
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| 86 | REAL(wp) :: zEw ! specific enthalpy of exchanged water (J/kg) |
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| 87 | REAL(wp) :: zdE ! specific enthalpy difference (J/kg) |
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| 88 | REAL(wp) :: zfmdt ! exchange mass flux x time step (J/m2), >0 towards the ocean |
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| 89 | REAL(wp) :: zsstK ! SST in Kelvin |
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| 90 | |
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| 91 | REAL(wp), POINTER, DIMENSION(:) :: zqprec ! energy of fallen snow (J.m-3) |
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| 92 | REAL(wp), POINTER, DIMENSION(:) :: zq_su ! heat for surface ablation (J.m-2) |
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| 93 | REAL(wp), POINTER, DIMENSION(:) :: zq_bo ! heat for bottom ablation (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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[5123] | 95 | REAL(wp), POINTER, DIMENSION(:) :: zf_tt ! Heat budget to determine melting or freezing(W.m-2) |
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[6416] | 96 | REAL(wp), POINTER, DIMENSION(:) :: zevap_rema ! remaining mass flux from sublimation (kg.m-2) |
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[3294] | 97 | |
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[3625] | 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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[3294] | 101 | |
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| 102 | REAL(wp), POINTER, DIMENSION(:,:) :: zdeltah |
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[4688] | 103 | REAL(wp), POINTER, DIMENSION(:,:) :: zh_i ! ice layer thickness |
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[5202] | 104 | INTEGER , POINTER, DIMENSION(:,:) :: icount ! number of layers vanished by melting |
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[3294] | 105 | |
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[4688] | 106 | REAL(wp), POINTER, DIMENSION(:) :: zqh_i ! total ice heat content (J.m-2) |
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[5407] | 107 | REAL(wp), POINTER, DIMENSION(:) :: zsnw ! distribution of snow after wind blowing |
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[3294] | 108 | |
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[5123] | 109 | REAL(wp) :: zswitch_sal |
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[4161] | 110 | |
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[3294] | 111 | ! Heat conservation |
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[4688] | 112 | INTEGER :: num_iter_max |
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| 113 | |
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[1572] | 114 | !!------------------------------------------------------------------ |
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[825] | 115 | |
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[5123] | 116 | ! Discriminate between varying salinity (nn_icesal=2) and prescribed cases (other values) |
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[7646] | 117 | SELECT CASE( nn_icesal ) ! varying salinity or not |
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[6470] | 118 | CASE( 1, 3 ) ; zswitch_sal = 0 ! prescribed salinity profile |
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| 119 | CASE( 2 ) ; zswitch_sal = 1 ! varying salinity profile |
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[4688] | 120 | END SELECT |
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[825] | 121 | |
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[6416] | 122 | CALL wrk_alloc( jpij, zqprec, zq_su, zq_bo, zf_tt, zq_rema, zsnw, zevap_rema ) |
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| 123 | CALL wrk_alloc( jpij, zdh_s_mel, zdh_s_pre, zdh_s_sub, zqh_i ) |
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[5202] | 124 | CALL wrk_alloc( jpij, nlay_i, zdeltah, zh_i ) |
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| 125 | CALL wrk_alloc( jpij, nlay_i, icount ) |
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[5487] | 126 | |
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| 127 | zqprec (:) = 0._wp ; zq_su (:) = 0._wp ; zq_bo (:) = 0._wp ; zf_tt(:) = 0._wp |
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[6416] | 128 | zq_rema (:) = 0._wp ; zsnw (:) = 0._wp ; zevap_rema(:) = 0._wp ; |
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[5487] | 129 | zdh_s_mel(:) = 0._wp ; zdh_s_pre(:) = 0._wp ; zdh_s_sub(:) = 0._wp ; zqh_i(:) = 0._wp |
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[4161] | 130 | |
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[5487] | 131 | zdeltah(:,:) = 0._wp ; zh_i(:,:) = 0._wp |
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| 132 | icount (:,:) = 0 |
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[4688] | 133 | |
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[5167] | 134 | ! Initialize enthalpy at nlay_i+1 |
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| 135 | DO ji = kideb, kiut |
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| 136 | q_i_1d(ji,nlay_i+1) = 0._wp |
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| 137 | END DO |
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| 138 | |
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[4688] | 139 | ! initialize layer thicknesses and enthalpies |
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| 140 | h_i_old (:,0:nlay_i+1) = 0._wp |
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| 141 | qh_i_old(:,0:nlay_i+1) = 0._wp |
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| 142 | DO jk = 1, nlay_i |
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| 143 | DO ji = kideb, kiut |
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[5123] | 144 | h_i_old (ji,jk) = ht_i_1d(ji) * r1_nlay_i |
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[4872] | 145 | qh_i_old(ji,jk) = q_i_1d(ji,jk) * h_i_old(ji,jk) |
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[4688] | 146 | ENDDO |
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| 147 | ENDDO |
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[921] | 148 | ! |
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| 149 | !------------------------------------------------------------------------------! |
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[4688] | 150 | ! 1) Calculate available heat for surface and bottom ablation ! |
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[921] | 151 | !------------------------------------------------------------------------------! |
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| 152 | ! |
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[2715] | 153 | DO ji = kideb, kiut |
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[6416] | 154 | zdum = qns_ice_1d(ji) + ( 1._wp - i0(ji) ) * qsr_ice_1d(ji) - fc_su(ji) |
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[4990] | 155 | zf_tt(ji) = fc_bo_i(ji) + fhtur_1d(ji) + fhld_1d(ji) |
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[4688] | 156 | |
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[6416] | 157 | zq_su (ji) = MAX( 0._wp, zdum * rdt_ice ) * MAX( 0._wp , SIGN( 1._wp, t_su_1d(ji) - rt0 ) ) |
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[4688] | 158 | zq_bo (ji) = MAX( 0._wp, zf_tt(ji) * rdt_ice ) |
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| 159 | END DO |
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| 160 | |
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[921] | 161 | ! |
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| 162 | !------------------------------------------------------------------------------! |
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[4688] | 163 | ! If snow temperature is above freezing point, then snow melts |
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| 164 | ! (should not happen but sometimes it does) |
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[921] | 165 | !------------------------------------------------------------------------------! |
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[4688] | 166 | DO ji = kideb, kiut |
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[5123] | 167 | IF( t_s_1d(ji,1) > rt0 ) THEN !!! Internal melting |
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[4688] | 168 | ! Contribution to heat flux to the ocean [W.m-2], < 0 |
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[4872] | 169 | 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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[4688] | 170 | ! Contribution to mass flux |
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[4872] | 171 | wfx_snw_1d(ji) = wfx_snw_1d(ji) + rhosn * ht_s_1d(ji) * a_i_1d(ji) * r1_rdtice |
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[4688] | 172 | ! updates |
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[4872] | 173 | ht_s_1d(ji) = 0._wp |
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| 174 | q_s_1d (ji,1) = 0._wp |
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[5123] | 175 | t_s_1d (ji,1) = rt0 |
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[4688] | 176 | END IF |
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| 177 | END DO |
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| 178 | |
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| 179 | !------------------------------------------------------------! |
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| 180 | ! 2) Computing layer thicknesses and enthalpies. ! |
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| 181 | !------------------------------------------------------------! |
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[921] | 182 | ! |
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[825] | 183 | DO jk = 1, nlay_i |
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[2715] | 184 | DO ji = kideb, kiut |
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[5123] | 185 | zh_i(ji,jk) = ht_i_1d(ji) * r1_nlay_i |
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[4872] | 186 | zqh_i(ji) = zqh_i(ji) + q_i_1d(ji,jk) * zh_i(ji,jk) |
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[825] | 187 | END DO |
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| 188 | END DO |
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[921] | 189 | ! |
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| 190 | !------------------------------------------------------------------------------| |
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| 191 | ! 3) Surface ablation and sublimation | |
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| 192 | !------------------------------------------------------------------------------| |
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| 193 | ! |
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[834] | 194 | !------------------------- |
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| 195 | ! 3.1 Snow precips / melt |
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| 196 | !------------------------- |
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[825] | 197 | ! Snow accumulation in one thermodynamic time step |
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| 198 | ! snowfall is partitionned between leads and ice |
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| 199 | ! if snow fall was uniform, a fraction (1-at_i) would fall into leads |
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| 200 | ! but because of the winds, more snow falls on leads than on sea ice |
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| 201 | ! and a greater fraction (1-at_i)^beta of the total mass of snow |
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[834] | 202 | ! (beta < 1) falls in leads. |
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[825] | 203 | ! In reality, beta depends on wind speed, |
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| 204 | ! and should decrease with increasing wind speed but here, it is |
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[834] | 205 | ! considered as a constant. an average value is 0.66 |
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[825] | 206 | ! Martin Vancoppenolle, December 2006 |
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| 207 | |
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[5487] | 208 | CALL lim_thd_snwblow( 1. - at_i_1d(kideb:kiut), zsnw(kideb:kiut) ) ! snow distribution over ice after wind blowing |
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| 209 | |
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[5167] | 210 | zdeltah(:,:) = 0._wp |
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[825] | 211 | DO ji = kideb, kiut |
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[4688] | 212 | !----------- |
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| 213 | ! Snow fall |
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| 214 | !----------- |
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| 215 | ! thickness change |
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[5407] | 216 | zdh_s_pre(ji) = zsnw(ji) * sprecip_1d(ji) * rdt_ice * r1_rhosn / at_i_1d(ji) |
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| 217 | ! enthalpy of the precip (>0, J.m-3) |
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| 218 | zqprec (ji) = - qprec_ice_1d(ji) |
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[4688] | 219 | IF( sprecip_1d(ji) == 0._wp ) zqprec(ji) = 0._wp |
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| 220 | ! heat flux from snow precip (>0, W.m-2) |
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[4872] | 221 | hfx_spr_1d(ji) = hfx_spr_1d(ji) + zdh_s_pre(ji) * a_i_1d(ji) * zqprec(ji) * r1_rdtice |
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[4688] | 222 | ! mass flux, <0 |
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[4872] | 223 | wfx_spr_1d(ji) = wfx_spr_1d(ji) - rhosn * a_i_1d(ji) * zdh_s_pre(ji) * r1_rdtice |
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[825] | 224 | |
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[4688] | 225 | !--------------------- |
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| 226 | ! Melt of falling snow |
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| 227 | !--------------------- |
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| 228 | ! thickness change |
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[5134] | 229 | rswitch = MAX( 0._wp , SIGN( 1._wp , zqprec(ji) - epsi20 ) ) |
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[5167] | 230 | zdeltah (ji,1) = - rswitch * zq_su(ji) / MAX( zqprec(ji) , epsi20 ) |
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| 231 | zdeltah (ji,1) = MAX( - zdh_s_pre(ji), zdeltah(ji,1) ) ! bound melting |
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[4688] | 232 | ! heat used to melt snow (W.m-2, >0) |
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[5167] | 233 | hfx_snw_1d(ji) = hfx_snw_1d(ji) - zdeltah(ji,1) * a_i_1d(ji) * zqprec(ji) * r1_rdtice |
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[4688] | 234 | ! snow melting only = water into the ocean (then without snow precip), >0 |
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[5167] | 235 | wfx_snw_1d(ji) = wfx_snw_1d(ji) - rhosn * a_i_1d(ji) * zdeltah(ji,1) * r1_rdtice |
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| 236 | ! updates available heat + precipitations after melting |
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| 237 | zq_su (ji) = MAX( 0._wp , zq_su (ji) + zdeltah(ji,1) * zqprec(ji) ) |
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| 238 | zdh_s_pre (ji) = zdh_s_pre(ji) + zdeltah(ji,1) |
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[4688] | 239 | |
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[5167] | 240 | ! update thickness |
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| 241 | ht_s_1d(ji) = MAX( 0._wp , ht_s_1d(ji) + zdh_s_pre(ji) ) |
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[825] | 242 | END DO |
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| 243 | |
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[5167] | 244 | ! If heat still available (zq_su > 0), then melt more snow |
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| 245 | zdeltah(:,:) = 0._wp |
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[825] | 246 | DO jk = 1, nlay_s |
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| 247 | DO ji = kideb, kiut |
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[4688] | 248 | ! thickness change |
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[4990] | 249 | rswitch = 1._wp - MAX( 0._wp, SIGN( 1._wp, - ht_s_1d(ji) ) ) |
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[5134] | 250 | rswitch = rswitch * ( MAX( 0._wp, SIGN( 1._wp, q_s_1d(ji,jk) - epsi20 ) ) ) |
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[4990] | 251 | zdeltah (ji,jk) = - rswitch * zq_su(ji) / MAX( q_s_1d(ji,jk), epsi20 ) |
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[5167] | 252 | zdeltah (ji,jk) = MAX( zdeltah(ji,jk) , - ht_s_1d(ji) ) ! bound melting |
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[4688] | 253 | zdh_s_mel(ji) = zdh_s_mel(ji) + zdeltah(ji,jk) |
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| 254 | ! heat used to melt snow(W.m-2, >0) |
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[4872] | 255 | 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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[4688] | 256 | ! snow melting only = water into the ocean (then without snow precip) |
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[4872] | 257 | wfx_snw_1d(ji) = wfx_snw_1d(ji) - rhosn * a_i_1d(ji) * zdeltah(ji,jk) * r1_rdtice |
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[4688] | 258 | ! updates available heat + thickness |
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[5123] | 259 | zq_su (ji) = MAX( 0._wp , zq_su (ji) + zdeltah(ji,jk) * q_s_1d(ji,jk) ) |
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[4872] | 260 | ht_s_1d(ji) = MAX( 0._wp , ht_s_1d(ji) + zdeltah(ji,jk) ) |
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[1572] | 261 | END DO |
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| 262 | END DO |
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[825] | 263 | |
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[6416] | 264 | !------------------------------ |
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| 265 | ! 3.2 Sublimation (part1: snow) |
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| 266 | !------------------------------ |
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[4688] | 267 | ! qla_ice is always >=0 (upwards), heat goes to the atmosphere, therefore snow sublimates |
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[5167] | 268 | ! clem comment: not counted in mass/heat exchange in limsbc since this is an exchange with atm. (not ocean) |
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| 269 | zdeltah(:,:) = 0._wp |
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[5407] | 270 | DO ji = kideb, kiut |
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[6416] | 271 | zdh_s_sub(ji) = MAX( - ht_s_1d(ji) , - evap_ice_1d(ji) * r1_rhosn * rdt_ice ) |
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| 272 | ! remaining evap in kg.m-2 (used for ice melting later on) |
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| 273 | zevap_rema(ji) = evap_ice_1d(ji) * rdt_ice + zdh_s_sub(ji) * rhosn |
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| 274 | ! Heat flux by sublimation [W.m-2], < 0 (sublimate first snow that had fallen, then pre-existing snow) |
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[5407] | 275 | zdeltah(ji,1) = MAX( zdh_s_sub(ji), - zdh_s_pre(ji) ) |
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| 276 | hfx_sub_1d(ji) = hfx_sub_1d(ji) + ( zdeltah(ji,1) * zqprec(ji) + ( zdh_s_sub(ji) - zdeltah(ji,1) ) * q_s_1d(ji,1) & |
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| 277 | & ) * a_i_1d(ji) * r1_rdtice |
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| 278 | ! Mass flux by sublimation |
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| 279 | wfx_sub_1d(ji) = wfx_sub_1d(ji) - rhosn * a_i_1d(ji) * zdh_s_sub(ji) * r1_rdtice |
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| 280 | ! new snow thickness |
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| 281 | ht_s_1d(ji) = MAX( 0._wp , ht_s_1d(ji) + zdh_s_sub(ji) ) |
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| 282 | ! update precipitations after sublimation and correct sublimation |
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| 283 | zdh_s_pre(ji) = zdh_s_pre(ji) + zdeltah(ji,1) |
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| 284 | zdh_s_sub(ji) = zdh_s_sub(ji) - zdeltah(ji,1) |
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| 285 | END DO |
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| 286 | |
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[4688] | 287 | ! --- Update snow diags --- ! |
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[825] | 288 | DO ji = kideb, kiut |
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[5167] | 289 | dh_s_tot(ji) = zdh_s_mel(ji) + zdh_s_pre(ji) + zdh_s_sub(ji) |
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| 290 | END DO |
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[825] | 291 | |
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[4688] | 292 | !------------------------------------------- |
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| 293 | ! 3.3 Update temperature, energy |
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| 294 | !------------------------------------------- |
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| 295 | ! new temp and enthalpy of the snow (remaining snow precip + remaining pre-existing snow) |
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[825] | 296 | DO jk = 1, nlay_s |
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| 297 | DO ji = kideb,kiut |
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[6416] | 298 | rswitch = MAX( 0._wp , SIGN( 1._wp, ht_s_1d(ji) - epsi20 ) ) |
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| 299 | q_s_1d(ji,jk) = rswitch / MAX( ht_s_1d(ji), epsi20 ) * & |
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| 300 | & ( ( zdh_s_pre(ji) ) * zqprec(ji) + & |
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| 301 | & ( ht_s_1d(ji) - zdh_s_pre(ji) ) * rhosn * ( cpic * ( rt0 - t_s_1d(ji,jk) ) + lfus ) ) |
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[825] | 302 | END DO |
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| 303 | END DO |
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| 304 | |
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[4688] | 305 | !-------------------------- |
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| 306 | ! 3.4 Surface ice ablation |
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| 307 | !-------------------------- |
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| 308 | zdeltah(:,:) = 0._wp ! important |
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| 309 | DO jk = 1, nlay_i |
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[5167] | 310 | DO ji = kideb, kiut |
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[5202] | 311 | ztmelts = - tmut * s_i_1d(ji,jk) + rt0 ! Melting point of layer k [K] |
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| 312 | |
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| 313 | IF( t_i_1d(ji,jk) >= ztmelts ) THEN !!! Internal melting |
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[4688] | 314 | |
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[5202] | 315 | zEi = - q_i_1d(ji,jk) * r1_rhoic ! Specific enthalpy of layer k [J/kg, <0] |
---|
| 316 | zdE = 0._wp ! Specific enthalpy difference (J/kg, <0) |
---|
| 317 | ! set up at 0 since no energy is needed to melt water...(it is already melted) |
---|
| 318 | zdeltah(ji,jk) = MIN( 0._wp , - zh_i(ji,jk) ) ! internal melting occurs when the internal temperature is above freezing |
---|
| 319 | ! this should normally not happen, but sometimes, heat diffusion leads to this |
---|
| 320 | zfmdt = - zdeltah(ji,jk) * rhoic ! Mass flux x time step > 0 |
---|
| 321 | |
---|
| 322 | dh_i_surf(ji) = dh_i_surf(ji) + zdeltah(ji,jk) ! Cumulate surface melt |
---|
| 323 | |
---|
| 324 | zfmdt = - rhoic * zdeltah(ji,jk) ! Recompute mass flux [kg/m2, >0] |
---|
[4688] | 325 | |
---|
[5202] | 326 | ! Contribution to heat flux to the ocean [W.m-2], <0 (ice enthalpy zEi is "sent" to the ocean) |
---|
| 327 | hfx_res_1d(ji) = hfx_res_1d(ji) + zfmdt * a_i_1d(ji) * zEi * r1_rdtice |
---|
| 328 | |
---|
| 329 | ! Contribution to salt flux (clem: using sm_i_1d and not s_i_1d(jk) is ok) |
---|
| 330 | sfx_res_1d(ji) = sfx_res_1d(ji) - rhoic * a_i_1d(ji) * zdeltah(ji,jk) * sm_i_1d(ji) * r1_rdtice |
---|
| 331 | |
---|
| 332 | ! Contribution to mass flux |
---|
| 333 | wfx_res_1d(ji) = wfx_res_1d(ji) - rhoic * a_i_1d(ji) * zdeltah(ji,jk) * r1_rdtice |
---|
[4688] | 334 | |
---|
[5202] | 335 | ELSE !!! Surface melting |
---|
| 336 | |
---|
| 337 | zEi = - q_i_1d(ji,jk) * r1_rhoic ! Specific enthalpy of layer k [J/kg, <0] |
---|
| 338 | zEw = rcp * ( ztmelts - rt0 ) ! Specific enthalpy of resulting meltwater [J/kg, <0] |
---|
| 339 | zdE = zEi - zEw ! Specific enthalpy difference < 0 |
---|
| 340 | |
---|
| 341 | zfmdt = - zq_su(ji) / zdE ! Mass flux to the ocean [kg/m2, >0] |
---|
| 342 | |
---|
| 343 | zdeltah(ji,jk) = - zfmdt * r1_rhoic ! Melt of layer jk [m, <0] |
---|
| 344 | |
---|
| 345 | 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] |
---|
| 346 | |
---|
| 347 | zq_su(ji) = MAX( 0._wp , zq_su(ji) - zdeltah(ji,jk) * rhoic * zdE ) ! update available heat |
---|
| 348 | |
---|
| 349 | dh_i_surf(ji) = dh_i_surf(ji) + zdeltah(ji,jk) ! Cumulate surface melt |
---|
| 350 | |
---|
| 351 | zfmdt = - rhoic * zdeltah(ji,jk) ! Recompute mass flux [kg/m2, >0] |
---|
| 352 | |
---|
| 353 | zQm = zfmdt * zEw ! Energy of the melt water sent to the ocean [J/m2, <0] |
---|
| 354 | |
---|
[6416] | 355 | ! Contribution to salt flux >0 (clem: using sm_i_1d and not s_i_1d(jk) is ok) |
---|
[5202] | 356 | sfx_sum_1d(ji) = sfx_sum_1d(ji) - rhoic * a_i_1d(ji) * zdeltah(ji,jk) * sm_i_1d(ji) * r1_rdtice |
---|
| 357 | |
---|
| 358 | ! Contribution to heat flux [W.m-2], < 0 |
---|
| 359 | hfx_thd_1d(ji) = hfx_thd_1d(ji) + zfmdt * a_i_1d(ji) * zEw * r1_rdtice |
---|
| 360 | |
---|
| 361 | ! Total heat flux used in this process [W.m-2], > 0 |
---|
| 362 | hfx_sum_1d(ji) = hfx_sum_1d(ji) - zfmdt * a_i_1d(ji) * zdE * r1_rdtice |
---|
| 363 | |
---|
| 364 | ! Contribution to mass flux |
---|
| 365 | wfx_sum_1d(ji) = wfx_sum_1d(ji) - rhoic * a_i_1d(ji) * zdeltah(ji,jk) * r1_rdtice |
---|
| 366 | |
---|
[5167] | 367 | END IF |
---|
[6416] | 368 | ! ---------------------- |
---|
| 369 | ! Sublimation part2: ice |
---|
| 370 | ! ---------------------- |
---|
| 371 | zdum = MAX( - ( zh_i(ji,jk) + zdeltah(ji,jk) ) , - zevap_rema(ji) * r1_rhoic ) |
---|
| 372 | zdeltah(ji,jk) = zdeltah(ji,jk) + zdum |
---|
| 373 | dh_i_sub(ji) = dh_i_sub(ji) + zdum |
---|
| 374 | ! Salt flux > 0 (clem2016: flux is sent to the ocean for simplicity but salt should remain in the ice except if all ice is melted. |
---|
| 375 | ! It must be corrected at some point) |
---|
| 376 | sfx_sub_1d(ji) = sfx_sub_1d(ji) - rhoic * a_i_1d(ji) * zdum * sm_i_1d(ji) * r1_rdtice |
---|
| 377 | ! Heat flux [W.m-2], < 0 |
---|
| 378 | hfx_sub_1d(ji) = hfx_sub_1d(ji) + zdum * q_i_1d(ji,jk) * a_i_1d(ji) * r1_rdtice |
---|
| 379 | ! Mass flux > 0 |
---|
| 380 | wfx_sub_1d(ji) = wfx_sub_1d(ji) - rhoic * a_i_1d(ji) * zdum * r1_rdtice |
---|
| 381 | ! update remaining mass flux |
---|
| 382 | zevap_rema(ji) = zevap_rema(ji) + zdum * rhoic |
---|
| 383 | |
---|
[4688] | 384 | ! record which layers have disappeared (for bottom melting) |
---|
| 385 | ! => icount=0 : no layer has vanished |
---|
| 386 | ! => icount=5 : 5 layers have vanished |
---|
[5202] | 387 | rswitch = MAX( 0._wp , SIGN( 1._wp , - ( zh_i(ji,jk) + zdeltah(ji,jk) ) ) ) |
---|
| 388 | icount(ji,jk) = NINT( rswitch ) |
---|
| 389 | zh_i(ji,jk) = MAX( 0._wp , zh_i(ji,jk) + zdeltah(ji,jk) ) |
---|
[6416] | 390 | |
---|
[4688] | 391 | ! update heat content (J.m-2) and layer thickness |
---|
[4872] | 392 | qh_i_old(ji,jk) = qh_i_old(ji,jk) + zdeltah(ji,jk) * q_i_1d(ji,jk) |
---|
[4688] | 393 | h_i_old (ji,jk) = h_i_old (ji,jk) + zdeltah(ji,jk) |
---|
[825] | 394 | END DO |
---|
[921] | 395 | END DO |
---|
[4688] | 396 | ! update ice thickness |
---|
| 397 | DO ji = kideb, kiut |
---|
[6416] | 398 | ht_i_1d(ji) = MAX( 0._wp , ht_i_1d(ji) + dh_i_surf(ji) + dh_i_sub(ji) ) |
---|
[4688] | 399 | END DO |
---|
[825] | 400 | |
---|
[6416] | 401 | ! remaining "potential" evap is sent to ocean |
---|
| 402 | DO ji = kideb, kiut |
---|
| 403 | ii = MOD( npb(ji) - 1, jpi ) + 1 ; ij = ( npb(ji) - 1 ) / jpi + 1 |
---|
| 404 | wfx_err_sub(ii,ij) = wfx_err_sub(ii,ij) - zevap_rema(ji) * a_i_1d(ji) * r1_rdtice ! <=0 (net evap for the ocean in kg.m-2.s-1) |
---|
| 405 | END DO |
---|
| 406 | |
---|
[921] | 407 | ! |
---|
| 408 | !------------------------------------------------------------------------------! |
---|
| 409 | ! 4) Basal growth / melt ! |
---|
| 410 | !------------------------------------------------------------------------------! |
---|
| 411 | ! |
---|
[4688] | 412 | !------------------ |
---|
| 413 | ! 4.1 Basal growth |
---|
| 414 | !------------------ |
---|
| 415 | ! Basal growth is driven by heat imbalance at the ice-ocean interface, |
---|
| 416 | ! between the inner conductive flux (fc_bo_i), from the open water heat flux |
---|
| 417 | ! (fhld) and the turbulent ocean flux (fhtur). |
---|
| 418 | ! fc_bo_i is positive downwards. fhtur and fhld are positive to the ice |
---|
[825] | 419 | |
---|
[4688] | 420 | ! If salinity varies in time, an iterative procedure is required, because |
---|
| 421 | ! the involved quantities are inter-dependent. |
---|
| 422 | ! Basal growth (dh_i_bott) depends upon new ice specific enthalpy (zEi), |
---|
| 423 | ! which depends on forming ice salinity (s_i_new), which depends on dh/dt (dh_i_bott) |
---|
| 424 | ! -> need for an iterative procedure, which converges quickly |
---|
| 425 | |
---|
[5167] | 426 | num_iter_max = 1 |
---|
| 427 | IF( nn_icesal == 2 ) num_iter_max = 5 |
---|
[825] | 428 | |
---|
[4688] | 429 | ! Iterative procedure |
---|
| 430 | DO iter = 1, num_iter_max |
---|
| 431 | DO ji = kideb, kiut |
---|
| 432 | IF( zf_tt(ji) < 0._wp ) THEN |
---|
[825] | 433 | |
---|
[4688] | 434 | ! New bottom ice salinity (Cox & Weeks, JGR88 ) |
---|
| 435 | !--- zswi1 if dh/dt < 2.0e-8 |
---|
| 436 | !--- zswi12 if 2.0e-8 < dh/dt < 3.6e-7 |
---|
| 437 | !--- zswi2 if dh/dt > 3.6e-7 |
---|
| 438 | zgrr = MIN( 1.0e-3, MAX ( dh_i_bott(ji) * r1_rdtice , epsi10 ) ) |
---|
| 439 | zswi2 = MAX( 0._wp , SIGN( 1._wp , zgrr - 3.6e-7 ) ) |
---|
| 440 | zswi12 = MAX( 0._wp , SIGN( 1._wp , zgrr - 2.0e-8 ) ) * ( 1.0 - zswi2 ) |
---|
| 441 | zswi1 = 1. - zswi2 * zswi12 |
---|
| 442 | zfracs = MIN ( zswi1 * 0.12 + zswi12 * ( 0.8925 + 0.0568 * LOG( 100.0 * zgrr ) ) & |
---|
| 443 | & + zswi2 * 0.26 / ( 0.26 + 0.74 * EXP ( - 724300.0 * zgrr ) ) , 0.5 ) |
---|
[825] | 444 | |
---|
[4688] | 445 | ii = MOD( npb(ji) - 1, jpi ) + 1 ; ij = ( npb(ji) - 1 ) / jpi + 1 |
---|
[825] | 446 | |
---|
[4688] | 447 | s_i_new(ji) = zswitch_sal * zfracs * sss_m(ii,ij) & ! New ice salinity |
---|
[4872] | 448 | + ( 1. - zswitch_sal ) * sm_i_1d(ji) |
---|
[4688] | 449 | ! New ice growth |
---|
[5123] | 450 | ztmelts = - tmut * s_i_new(ji) + rt0 ! New ice melting point (K) |
---|
[825] | 451 | |
---|
[4872] | 452 | zt_i_new = zswitch_sal * t_bo_1d(ji) + ( 1. - zswitch_sal) * t_i_1d(ji, nlay_i) |
---|
[4688] | 453 | |
---|
| 454 | zEi = cpic * ( zt_i_new - ztmelts ) & ! Specific enthalpy of forming ice (J/kg, <0) |
---|
[5123] | 455 | & - lfus * ( 1.0 - ( ztmelts - rt0 ) / ( zt_i_new - rt0 ) ) & |
---|
| 456 | & + rcp * ( ztmelts-rt0 ) |
---|
[4688] | 457 | |
---|
[4872] | 458 | zEw = rcp * ( t_bo_1d(ji) - rt0 ) ! Specific enthalpy of seawater (J/kg, < 0) |
---|
[4688] | 459 | |
---|
| 460 | zdE = zEi - zEw ! Specific enthalpy difference (J/kg, <0) |
---|
| 461 | |
---|
| 462 | dh_i_bott(ji) = rdt_ice * MAX( 0._wp , zf_tt(ji) / ( zdE * rhoic ) ) |
---|
| 463 | |
---|
[4872] | 464 | q_i_1d(ji,nlay_i+1) = -zEi * rhoic ! New ice energy of melting (J/m3, >0) |
---|
[4688] | 465 | |
---|
[5134] | 466 | ENDIF |
---|
| 467 | END DO |
---|
| 468 | END DO |
---|
[4688] | 469 | |
---|
| 470 | ! Contribution to Energy and Salt Fluxes |
---|
[825] | 471 | DO ji = kideb, kiut |
---|
[4688] | 472 | IF( zf_tt(ji) < 0._wp ) THEN |
---|
| 473 | ! New ice growth |
---|
| 474 | |
---|
| 475 | zfmdt = - rhoic * dh_i_bott(ji) ! Mass flux x time step (kg/m2, < 0) |
---|
| 476 | |
---|
[5123] | 477 | ztmelts = - tmut * s_i_new(ji) + rt0 ! New ice melting point (K) |
---|
[4688] | 478 | |
---|
[4872] | 479 | zt_i_new = zswitch_sal * t_bo_1d(ji) + ( 1. - zswitch_sal) * t_i_1d(ji, nlay_i) |
---|
[4688] | 480 | |
---|
| 481 | zEi = cpic * ( zt_i_new - ztmelts ) & ! Specific enthalpy of forming ice (J/kg, <0) |
---|
[5123] | 482 | & - lfus * ( 1.0 - ( ztmelts - rt0 ) / ( zt_i_new - rt0 ) ) & |
---|
| 483 | & + rcp * ( ztmelts-rt0 ) |
---|
[4688] | 484 | |
---|
[4872] | 485 | zEw = rcp * ( t_bo_1d(ji) - rt0 ) ! Specific enthalpy of seawater (J/kg, < 0) |
---|
[4688] | 486 | |
---|
| 487 | zdE = zEi - zEw ! Specific enthalpy difference (J/kg, <0) |
---|
| 488 | |
---|
| 489 | ! Contribution to heat flux to the ocean [W.m-2], >0 |
---|
[4872] | 490 | hfx_thd_1d(ji) = hfx_thd_1d(ji) + zfmdt * a_i_1d(ji) * zEw * r1_rdtice |
---|
[4688] | 491 | |
---|
| 492 | ! Total heat flux used in this process [W.m-2], <0 |
---|
[4872] | 493 | hfx_bog_1d(ji) = hfx_bog_1d(ji) - zfmdt * a_i_1d(ji) * zdE * r1_rdtice |
---|
[4688] | 494 | |
---|
| 495 | ! Contribution to salt flux, <0 |
---|
[5167] | 496 | sfx_bog_1d(ji) = sfx_bog_1d(ji) - rhoic * a_i_1d(ji) * dh_i_bott(ji) * s_i_new(ji) * r1_rdtice |
---|
[4688] | 497 | |
---|
| 498 | ! Contribution to mass flux, <0 |
---|
[4872] | 499 | wfx_bog_1d(ji) = wfx_bog_1d(ji) - rhoic * a_i_1d(ji) * dh_i_bott(ji) * r1_rdtice |
---|
[4688] | 500 | |
---|
| 501 | ! update heat content (J.m-2) and layer thickness |
---|
[4872] | 502 | 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) |
---|
[4688] | 503 | h_i_old (ji,nlay_i+1) = h_i_old (ji,nlay_i+1) + dh_i_bott(ji) |
---|
[825] | 504 | ENDIF |
---|
| 505 | END DO |
---|
| 506 | |
---|
[4688] | 507 | !---------------- |
---|
| 508 | ! 4.2 Basal melt |
---|
| 509 | !---------------- |
---|
| 510 | zdeltah(:,:) = 0._wp ! important |
---|
[825] | 511 | DO jk = nlay_i, 1, -1 |
---|
| 512 | DO ji = kideb, kiut |
---|
[5202] | 513 | IF( zf_tt(ji) > 0._wp .AND. jk > icount(ji,jk) ) THEN ! do not calculate where layer has already disappeared by surface melting |
---|
[825] | 514 | |
---|
[5123] | 515 | ztmelts = - tmut * s_i_1d(ji,jk) + rt0 ! Melting point of layer jk (K) |
---|
[825] | 516 | |
---|
[4872] | 517 | IF( t_i_1d(ji,jk) >= ztmelts ) THEN !!! Internal melting |
---|
[825] | 518 | |
---|
[5123] | 519 | zEi = - q_i_1d(ji,jk) * r1_rhoic ! Specific enthalpy of melting ice (J/kg, <0) |
---|
[4688] | 520 | zdE = 0._wp ! Specific enthalpy difference (J/kg, <0) |
---|
| 521 | ! set up at 0 since no energy is needed to melt water...(it is already melted) |
---|
[5202] | 522 | zdeltah (ji,jk) = MIN( 0._wp , - zh_i(ji,jk) ) ! internal melting occurs when the internal temperature is above freezing |
---|
| 523 | ! this should normally not happen, but sometimes, heat diffusion leads to this |
---|
[4161] | 524 | |
---|
[4688] | 525 | dh_i_bott (ji) = dh_i_bott(ji) + zdeltah(ji,jk) |
---|
[825] | 526 | |
---|
[5202] | 527 | zfmdt = - zdeltah(ji,jk) * rhoic ! Mass flux x time step > 0 |
---|
[825] | 528 | |
---|
[4688] | 529 | ! Contribution to heat flux to the ocean [W.m-2], <0 (ice enthalpy zEi is "sent" to the ocean) |
---|
[4872] | 530 | hfx_res_1d(ji) = hfx_res_1d(ji) + zfmdt * a_i_1d(ji) * zEi * r1_rdtice |
---|
[825] | 531 | |
---|
[4872] | 532 | ! Contribution to salt flux (clem: using sm_i_1d and not s_i_1d(jk) is ok) |
---|
[5167] | 533 | sfx_res_1d(ji) = sfx_res_1d(ji) - rhoic * a_i_1d(ji) * zdeltah(ji,jk) * sm_i_1d(ji) * r1_rdtice |
---|
[4688] | 534 | |
---|
| 535 | ! Contribution to mass flux |
---|
[4872] | 536 | wfx_res_1d(ji) = wfx_res_1d(ji) - rhoic * a_i_1d(ji) * zdeltah(ji,jk) * r1_rdtice |
---|
[825] | 537 | |
---|
[4688] | 538 | ! update heat content (J.m-2) and layer thickness |
---|
[4872] | 539 | qh_i_old(ji,jk) = qh_i_old(ji,jk) + zdeltah(ji,jk) * q_i_1d(ji,jk) |
---|
[4688] | 540 | h_i_old (ji,jk) = h_i_old (ji,jk) + zdeltah(ji,jk) |
---|
[825] | 541 | |
---|
[4688] | 542 | ELSE !!! Basal melting |
---|
[825] | 543 | |
---|
[5202] | 544 | zEi = - q_i_1d(ji,jk) * r1_rhoic ! Specific enthalpy of melting ice (J/kg, <0) |
---|
| 545 | zEw = rcp * ( ztmelts - rt0 ) ! Specific enthalpy of meltwater (J/kg, <0) |
---|
| 546 | zdE = zEi - zEw ! Specific enthalpy difference (J/kg, <0) |
---|
[825] | 547 | |
---|
[5202] | 548 | zfmdt = - zq_bo(ji) / zdE ! Mass flux x time step (kg/m2, >0) |
---|
[825] | 549 | |
---|
[5202] | 550 | zdeltah(ji,jk) = - zfmdt * r1_rhoic ! Gross thickness change |
---|
[4688] | 551 | |
---|
[5202] | 552 | zdeltah(ji,jk) = MIN( 0._wp , MAX( zdeltah(ji,jk), - zh_i(ji,jk) ) ) ! bound thickness change |
---|
[4688] | 553 | |
---|
[5202] | 554 | zq_bo(ji) = MAX( 0._wp , zq_bo(ji) - zdeltah(ji,jk) * rhoic * zdE ) ! update available heat. MAX is necessary for roundup errors |
---|
[4688] | 555 | |
---|
[5202] | 556 | dh_i_bott(ji) = dh_i_bott(ji) + zdeltah(ji,jk) ! Update basal melt |
---|
[4688] | 557 | |
---|
[5202] | 558 | zfmdt = - zdeltah(ji,jk) * rhoic ! Mass flux x time step > 0 |
---|
[4688] | 559 | |
---|
[5202] | 560 | zQm = zfmdt * zEw ! Heat exchanged with ocean |
---|
[4688] | 561 | |
---|
| 562 | ! Contribution to heat flux to the ocean [W.m-2], <0 |
---|
[5202] | 563 | hfx_thd_1d(ji) = hfx_thd_1d(ji) + zfmdt * a_i_1d(ji) * zEw * r1_rdtice |
---|
[4688] | 564 | |
---|
[4872] | 565 | ! Contribution to salt flux (clem: using sm_i_1d and not s_i_1d(jk) is ok) |
---|
[5202] | 566 | sfx_bom_1d(ji) = sfx_bom_1d(ji) - rhoic * a_i_1d(ji) * zdeltah(ji,jk) * sm_i_1d(ji) * r1_rdtice |
---|
[4688] | 567 | |
---|
| 568 | ! Total heat flux used in this process [W.m-2], >0 |
---|
[5202] | 569 | hfx_bom_1d(ji) = hfx_bom_1d(ji) - zfmdt * a_i_1d(ji) * zdE * r1_rdtice |
---|
[4688] | 570 | |
---|
| 571 | ! Contribution to mass flux |
---|
[5202] | 572 | wfx_bom_1d(ji) = wfx_bom_1d(ji) - rhoic * a_i_1d(ji) * zdeltah(ji,jk) * r1_rdtice |
---|
[4688] | 573 | |
---|
| 574 | ! update heat content (J.m-2) and layer thickness |
---|
[4872] | 575 | qh_i_old(ji,jk) = qh_i_old(ji,jk) + zdeltah(ji,jk) * q_i_1d(ji,jk) |
---|
[4688] | 576 | h_i_old (ji,jk) = h_i_old (ji,jk) + zdeltah(ji,jk) |
---|
| 577 | ENDIF |
---|
| 578 | |
---|
| 579 | ENDIF |
---|
[5123] | 580 | END DO |
---|
| 581 | END DO |
---|
[4688] | 582 | |
---|
[825] | 583 | !------------------------------------------- |
---|
[4688] | 584 | ! Update temperature, energy |
---|
[825] | 585 | !------------------------------------------- |
---|
| 586 | DO ji = kideb, kiut |
---|
[4872] | 587 | ht_i_1d(ji) = MAX( 0._wp , ht_i_1d(ji) + dh_i_bott(ji) ) |
---|
[4688] | 588 | END DO |
---|
[825] | 589 | |
---|
[4688] | 590 | !------------------------------------------- |
---|
| 591 | ! 5. What to do with remaining energy |
---|
| 592 | !------------------------------------------- |
---|
| 593 | ! If heat still available for melting and snow remains, then melt more snow |
---|
| 594 | !------------------------------------------- |
---|
| 595 | zdeltah(:,:) = 0._wp ! important |
---|
| 596 | DO ji = kideb, kiut |
---|
| 597 | zq_rema(ji) = zq_su(ji) + zq_bo(ji) |
---|
[5128] | 598 | rswitch = 1._wp - MAX( 0._wp, SIGN( 1._wp, - ht_s_1d(ji) ) ) ! =1 if snow |
---|
[5134] | 599 | rswitch = rswitch * MAX( 0._wp, SIGN( 1._wp, q_s_1d(ji,1) - epsi20 ) ) |
---|
| 600 | zdeltah (ji,1) = - rswitch * zq_rema(ji) / MAX( q_s_1d(ji,1), epsi20 ) |
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[5128] | 601 | zdeltah (ji,1) = MIN( 0._wp , MAX( zdeltah(ji,1) , - ht_s_1d(ji) ) ) ! bound melting |
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| 602 | dh_s_tot (ji) = dh_s_tot(ji) + zdeltah(ji,1) |
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| 603 | ht_s_1d (ji) = ht_s_1d(ji) + zdeltah(ji,1) |
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| 604 | |
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[5134] | 605 | zq_rema(ji) = zq_rema(ji) + zdeltah(ji,1) * q_s_1d(ji,1) ! update available heat (J.m-2) |
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[5128] | 606 | ! heat used to melt snow |
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[5134] | 607 | hfx_snw_1d(ji) = hfx_snw_1d(ji) - zdeltah(ji,1) * a_i_1d(ji) * q_s_1d(ji,1) * r1_rdtice ! W.m-2 (>0) |
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[5128] | 608 | ! Contribution to mass flux |
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| 609 | wfx_snw_1d(ji) = wfx_snw_1d(ji) - rhosn * a_i_1d(ji) * zdeltah(ji,1) * r1_rdtice |
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| 610 | ! |
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[4688] | 611 | ii = MOD( npb(ji) - 1, jpi ) + 1 ; ij = ( npb(ji) - 1 ) / jpi + 1 |
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| 612 | ! Remaining heat flux (W.m-2) is sent to the ocean heat budget |
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[5123] | 613 | hfx_out(ii,ij) = hfx_out(ii,ij) + ( zq_rema(ji) * a_i_1d(ji) ) * r1_rdtice |
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[825] | 614 | |
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[7646] | 615 | IF( ln_limctl .AND. zq_rema(ji) < 0. .AND. lwp ) WRITE(numout,*) 'ALERTE zq_rema <0 = ', zq_rema(ji) |
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[4688] | 616 | END DO |
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| 617 | |
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[921] | 618 | ! |
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| 619 | !------------------------------------------------------------------------------| |
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| 620 | ! 6) Snow-Ice formation | |
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| 621 | !------------------------------------------------------------------------------| |
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[1572] | 622 | ! When snow load excesses Archimede's limit, snow-ice interface goes down under sea-level, |
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| 623 | ! flooding of seawater transforms snow into ice dh_snowice is positive for the ice |
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[825] | 624 | DO ji = kideb, kiut |
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[1572] | 625 | ! |
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[4872] | 626 | dh_snowice(ji) = MAX( 0._wp , ( rhosn * ht_s_1d(ji) + (rhoic-rau0) * ht_i_1d(ji) ) / ( rhosn+rau0-rhoic ) ) |
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[825] | 627 | |
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[5167] | 628 | ht_i_1d(ji) = ht_i_1d(ji) + dh_snowice(ji) |
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| 629 | ht_s_1d(ji) = ht_s_1d(ji) - dh_snowice(ji) |
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[825] | 630 | |
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[4688] | 631 | ! Contribution to energy flux to the ocean [J/m2], >0 (if sst<0) |
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| 632 | ii = MOD( npb(ji) - 1, jpi ) + 1 ; ij = ( npb(ji) - 1 ) / jpi + 1 |
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[7646] | 633 | zfmdt = ( rhosn - rhoic ) * dh_snowice(ji) ! <0 |
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[4688] | 634 | zsstK = sst_m(ii,ij) + rt0 |
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| 635 | zEw = rcp * ( zsstK - rt0 ) |
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| 636 | zQm = zfmdt * zEw |
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| 637 | |
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| 638 | ! Contribution to heat flux |
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[4872] | 639 | hfx_thd_1d(ji) = hfx_thd_1d(ji) + zfmdt * a_i_1d(ji) * zEw * r1_rdtice |
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[825] | 640 | |
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[4688] | 641 | ! Contribution to salt flux |
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[4872] | 642 | sfx_sni_1d(ji) = sfx_sni_1d(ji) + sss_m(ii,ij) * a_i_1d(ji) * zfmdt * r1_rdtice |
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[7646] | 643 | |
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[6470] | 644 | ! virtual salt flux to keep salinity constant |
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| 645 | IF( nn_icesal == 1 .OR. nn_icesal == 3 ) THEN |
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[7646] | 646 | sfx_bri_1d(ji) = sfx_bri_1d(ji) - sss_m(ii,ij) * a_i_1d(ji) * zfmdt * r1_rdtice & ! put back sss_m into the ocean |
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| 647 | & - sm_i_1d(ji) * a_i_1d(ji) * dh_snowice(ji) * rhoic * r1_rdtice ! and get rn_icesal from the ocean |
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[6470] | 648 | ENDIF |
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| 649 | |
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[4688] | 650 | ! Contribution to mass flux |
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| 651 | ! All snow is thrown in the ocean, and seawater is taken to replace the volume |
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[4872] | 652 | wfx_sni_1d(ji) = wfx_sni_1d(ji) - a_i_1d(ji) * dh_snowice(ji) * rhoic * r1_rdtice |
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| 653 | wfx_snw_1d(ji) = wfx_snw_1d(ji) + a_i_1d(ji) * dh_snowice(ji) * rhosn * r1_rdtice |
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[4688] | 654 | |
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| 655 | ! update heat content (J.m-2) and layer thickness |
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[4872] | 656 | qh_i_old(ji,0) = qh_i_old(ji,0) + dh_snowice(ji) * q_s_1d(ji,1) + zfmdt * zEw |
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[4688] | 657 | h_i_old (ji,0) = h_i_old (ji,0) + dh_snowice(ji) |
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| 658 | |
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[5134] | 659 | END DO |
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[825] | 660 | |
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[2715] | 661 | ! |
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[4688] | 662 | !------------------------------------------- |
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| 663 | ! Update temperature, energy |
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| 664 | !------------------------------------------- |
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| 665 | DO ji = kideb, kiut |
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[4990] | 666 | rswitch = 1.0 - MAX( 0._wp , SIGN( 1._wp , - ht_i_1d(ji) ) ) |
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[5123] | 667 | t_su_1d(ji) = rswitch * t_su_1d(ji) + ( 1.0 - rswitch ) * rt0 |
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[5134] | 668 | END DO |
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[4688] | 669 | |
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| 670 | DO jk = 1, nlay_s |
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| 671 | DO ji = kideb,kiut |
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| 672 | ! mask enthalpy |
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[5134] | 673 | rswitch = 1._wp - MAX( 0._wp , SIGN( 1._wp, - ht_s_1d(ji) ) ) |
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| 674 | q_s_1d(ji,jk) = rswitch * q_s_1d(ji,jk) |
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[4872] | 675 | ! recalculate t_s_1d from q_s_1d |
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[5134] | 676 | t_s_1d(ji,jk) = rt0 + rswitch * ( - q_s_1d(ji,jk) / ( rhosn * cpic ) + lfus / cpic ) |
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[4688] | 677 | END DO |
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| 678 | END DO |
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[5134] | 679 | |
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| 680 | ! --- ensure that a_i = 0 where ht_i = 0 --- |
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| 681 | WHERE( ht_i_1d == 0._wp ) a_i_1d = 0._wp |
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[5123] | 682 | |
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[6416] | 683 | CALL wrk_dealloc( jpij, zqprec, zq_su, zq_bo, zf_tt, zq_rema, zsnw, zevap_rema ) |
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| 684 | CALL wrk_dealloc( jpij, zdh_s_mel, zdh_s_pre, zdh_s_sub, zqh_i ) |
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[5202] | 685 | CALL wrk_dealloc( jpij, nlay_i, zdeltah, zh_i ) |
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| 686 | CALL wrk_dealloc( jpij, nlay_i, icount ) |
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[2715] | 687 | ! |
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[4161] | 688 | ! |
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[921] | 689 | END SUBROUTINE lim_thd_dh |
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[5407] | 690 | |
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| 691 | |
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| 692 | !!-------------------------------------------------------------------------- |
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| 693 | !! INTERFACE lim_thd_snwblow |
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| 694 | !! ** Purpose : Compute distribution of precip over the ice |
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| 695 | !!-------------------------------------------------------------------------- |
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| 696 | SUBROUTINE lim_thd_snwblow_2d( pin, pout ) |
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[5487] | 697 | REAL(wp), DIMENSION(:,:), INTENT(in ) :: pin ! previous fraction lead ( pfrld or (1. - a_i_b) ) |
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| 698 | REAL(wp), DIMENSION(:,:), INTENT(inout) :: pout |
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[5407] | 699 | pout = ( 1._wp - ( pin )**rn_betas ) |
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| 700 | END SUBROUTINE lim_thd_snwblow_2d |
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| 701 | |
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| 702 | SUBROUTINE lim_thd_snwblow_1d( pin, pout ) |
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[5487] | 703 | REAL(wp), DIMENSION(:), INTENT(in ) :: pin |
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| 704 | REAL(wp), DIMENSION(:), INTENT(inout) :: pout |
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[5407] | 705 | pout = ( 1._wp - ( pin )**rn_betas ) |
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| 706 | END SUBROUTINE lim_thd_snwblow_1d |
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| 707 | |
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[1572] | 708 | |
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[825] | 709 | #else |
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[1572] | 710 | !!---------------------------------------------------------------------- |
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| 711 | !! Default option NO LIM3 sea-ice model |
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| 712 | !!---------------------------------------------------------------------- |
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[825] | 713 | CONTAINS |
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| 714 | SUBROUTINE lim_thd_dh ! Empty routine |
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| 715 | END SUBROUTINE lim_thd_dh |
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| 716 | #endif |
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[1572] | 717 | |
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| 718 | !!====================================================================== |
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[921] | 719 | END MODULE limthd_dh |
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