| 1 | MODULE limthd_da |
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| 2 | !!====================================================================== |
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| 3 | !! *** MODULE limthd_da *** |
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| 4 | !! LIM-3 sea-ice : computation of lateral melting in the ice |
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| 5 | !!====================================================================== |
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| 6 | !! History : 4.0 ! 2016-03 (C. Rousset) original code |
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| 7 | !!--------------------------------------------------------------------- |
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| 8 | #if defined key_lim3 |
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| 9 | !!---------------------------------------------------------------------- |
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| 10 | !! 'key_lim3' LIM-3 sea-ice model |
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| 11 | !!---------------------------------------------------------------------- |
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| 12 | !! lim_thd_da : sea ice lateral melting |
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| 13 | !!---------------------------------------------------------------------- |
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| 14 | USE par_oce ! ocean parameters |
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| 15 | USE phycst ! physical constants (ocean directory) |
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| 16 | USE sbc_oce, ONLY: sst_m ! Surface boundary condition: ocean fields |
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| 17 | USE ice ! LIM variables |
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| 18 | USE lib_mpp ! MPP library |
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| 19 | USE wrk_nemo ! work arrays |
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| 20 | USE lib_fortran ! Fortran utilities (allows no signed zero when 'key_nosignedzero' defined) |
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| 21 | |
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| 22 | IMPLICIT NONE |
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| 23 | PRIVATE |
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| 24 | |
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| 25 | PUBLIC lim_thd_da ! called by limthd module |
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| 26 | |
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| 27 | !!---------------------------------------------------------------------- |
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| 28 | !! NEMO/LIM3 4.0 , UCL - NEMO Consortium (2011) |
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| 29 | !! $Id: limthd_da.F90 5123 2015-03-04 16:06:03Z clem $ |
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| 30 | !! Software governed by the CeCILL licence (NEMOGCM/NEMO_CeCILL.txt) |
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| 31 | !!---------------------------------------------------------------------- |
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| 32 | CONTAINS |
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| 33 | |
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| 34 | SUBROUTINE lim_thd_da |
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| 35 | !!------------------------------------------------------------------- |
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| 36 | !! *** ROUTINE lim_thd_da *** |
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| 37 | !! |
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| 38 | !! ** Purpose : computes sea ice lateral melting |
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| 39 | !! |
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| 40 | !! ** Method : dA/dt = - P * W [s-1] |
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| 41 | !! W = melting velocity [m.s-1] |
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| 42 | !! P = perimeter of ice-ocean lateral interface normalized by grid cell area [m.m-2] |
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| 43 | !! |
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| 44 | !! W = m1 * (Tw -Tf)**m2 --- originally from Josberger 1979 --- |
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| 45 | !! (Tw - Tf) = elevation of water temp above freezing |
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| 46 | !! m1 and m2 = (1.6e-6 , 1.36) best fit from field experiment near the coast of Prince Patrick Island (Perovich 1983) => static ice |
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| 47 | !! m1 and m2 = (3.0e-6 , 1.36) best fit from MIZEX 84 experiment (Maykut and Perovich 1987) => moving ice |
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| 48 | !! |
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| 49 | !! P = N * pi * D --- from Rothrock and Thorndike 1984 --- |
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| 50 | !! D = mean floe caliper diameter |
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| 51 | !! N = number of floes = ice area / floe area(average) = A / (Cs * D**2) |
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| 52 | !! A = ice concentration |
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| 53 | !! Cs = deviation from a square (square:Cs=1 ; circle:Cs=pi/4 ; floe:Cs=0.66) |
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| 54 | !! |
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| 55 | !! D = Dmin * ( Astar / (Astar-A) )**beta --- from Lupkes et al., 2012 (eq. 26-27) --- |
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| 56 | !! |
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| 57 | !! Astar = 1 / ( 1 - (Dmin/Dmax)**(1/beta) ) |
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| 58 | !! Dmin = minimum floe diameter (recommended to be 8m +- 20%) |
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| 59 | !! Dmax = maximum floe diameter (recommended to be 300m, but it does not impact melting much except for Dmax<100m) |
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| 60 | !! beta = 1.0 +-20% (recommended value) |
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| 61 | !! = 0.3 best fit for western Fram Strait and Antarctica |
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| 62 | !! = 1.4 best fit for eastern Fram Strait |
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| 63 | !! |
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| 64 | !! ** Tunable parameters : We propose to tune the lateral melting via 2 parameters |
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| 65 | !! Dmin [6-10m] => 6 vs 8m = +40% melting at the peak (A~0.5) |
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| 66 | !! 10 vs 8m = -20% melting |
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| 67 | !! beta [0.8-1.2] => decrease = more melt and melt peaks toward higher concentration |
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| 68 | !! (A~0.5 for beta=1 ; A~0.8 for beta=0.2) |
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| 69 | !! 0.3 = best fit for western Fram Strait and Antarctica |
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| 70 | !! 1.4 = best fit for eastern Fram Strait |
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| 71 | !! |
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| 72 | !! ** Note : Former and more simple formulations for floe diameters can be found in Mai (1995), |
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| 73 | !! Birnbaum and Lupkes (2002), Lupkes and Birnbaum (2005). They are reviewed in Lupkes et al 2012 |
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| 74 | !! A simpler implementation for CICE can be found in Bitz et al (2001) and Tsamados et al (2015) |
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| 75 | !! |
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| 76 | !! ** References |
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| 77 | !! Bitz, C. M., Holland, M. M., Weaver, A. J., & Eby, M. (2001). |
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| 78 | !! Simulating the ice‐thickness distribution in a coupled climate model. |
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| 79 | !! Journal of Geophysical Research: Oceans, 106(C2), 2441-2463. |
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| 80 | !! Josberger, E. G. (1979). |
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| 81 | !! Laminar and turbulent boundary layers adjacent to melting vertical ice walls in salt water |
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| 82 | !! (No. SCIENTIFIC-16). WASHINGTON UNIV SEATTLE DEPT OF ATMOSPHERIC SCIENCES. |
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| 83 | !! Lüpkes, C., Gryanik, V. M., Hartmann, J., & Andreas, E. L. (2012). |
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| 84 | !! A parametrization, based on sea ice morphology, of the neutral atmospheric drag coefficients |
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| 85 | !! for weather prediction and climate models. |
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| 86 | !! Journal of Geophysical Research: Atmospheres, 117(D13). |
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| 87 | !! Maykut, G. A., & Perovich, D. K. (1987). |
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| 88 | !! The role of shortwave radiation in the summer decay of a sea ice cover. |
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| 89 | !! Journal of Geophysical Research: Oceans, 92(C7), 7032-7044. |
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| 90 | !! Perovich, D. K. (1983). |
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| 91 | !! On the summer decay of a sea ice cover. (Doctoral dissertation, University of Washington). |
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| 92 | !! Rothrock, D. A., & Thorndike, A. S. (1984). |
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| 93 | !! Measuring the sea ice floe size distribution. |
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| 94 | !! Journal of Geophysical Research: Oceans, 89(C4), 6477-6486. |
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| 95 | !! Tsamados, M., Feltham, D., Petty, A., Schroeder, D., & Flocco, D. (2015). |
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| 96 | !! Processes controlling surface, bottom and lateral melt of Arctic sea ice in a state of the art sea ice model. |
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| 97 | !! Phil. Trans. R. Soc. A, 373(2052), 20140167. |
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| 98 | !!--------------------------------------------------------------------- |
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| 99 | INTEGER :: ji, jj, jl ! dummy loop indices |
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| 100 | REAL(wp) :: zastar, zdfloe, zperi, zwlat, zda |
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| 101 | REAL(wp), PARAMETER :: zdmax = 300._wp |
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| 102 | REAL(wp), PARAMETER :: zcs = 0.66_wp |
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| 103 | REAL(wp), PARAMETER :: zm1 = 3.e-6_wp |
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| 104 | REAL(wp), PARAMETER :: zm2 = 1.36_wp |
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| 105 | ! |
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| 106 | REAL(wp), POINTER, DIMENSION(:,:) :: zda_tot |
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| 107 | !!--------------------------------------------------------------------- |
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| 108 | CALL wrk_alloc( jpi,jpj, zda_tot ) |
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| 109 | |
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| 110 | !------------------------------------------------------------! |
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| 111 | ! --- Calculate reduction of total sea ice concentration --- ! |
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| 112 | !------------------------------------------------------------! |
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| 113 | zastar = 1._wp / ( 1._wp - (rn_dmin / zdmax)**(1._wp/rn_beta) ) |
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| 114 | |
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| 115 | DO jj = 1, jpj |
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| 116 | DO ji = 1, jpi |
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| 117 | |
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| 118 | ! Mean floe caliper diameter [m] |
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| 119 | zdfloe = rn_dmin * ( zastar / ( zastar - at_i(ji,jj) ) )**rn_beta |
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| 120 | |
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| 121 | ! Mean perimeter of the floe = N*pi*D = (A/cs*D^2)*pi*D [m.m-2] |
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| 122 | zperi = at_i(ji,jj) * rpi / ( zcs * zdfloe ) |
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| 123 | |
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| 124 | ! Melt speed rate [m/s] |
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| 125 | zwlat = zm1 * ( MAX( 0._wp, sst_m(ji,jj) - ( t_bo(ji,jj) - rt0 ) ) )**zm2 |
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| 126 | |
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| 127 | ! sea ice concentration decrease |
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| 128 | zda_tot(ji,jj) = - MIN( zwlat * zperi * rdt_ice, at_i(ji,jj) ) |
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| 129 | |
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| 130 | END DO |
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| 131 | END DO |
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| 132 | |
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| 133 | !---------------------------------------------------------------------------------------------! |
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| 134 | ! --- Distribute reduction among ice categories and calculate associated ice-ocean fluxes --- ! |
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| 135 | !---------------------------------------------------------------------------------------------! |
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| 136 | DO jl = jpl, 1, -1 |
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| 137 | DO jj = 1, jpj |
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| 138 | DO ji = 1, jpi |
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| 139 | |
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| 140 | ! decrease of concentration for the category jl |
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| 141 | ! 1st option: each category contributes to melting in proportion to its concentration |
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| 142 | rswitch = MAX( 0._wp , SIGN( 1._wp, at_i(ji,jj) - epsi10 ) ) |
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| 143 | zda = rswitch * zda_tot(ji,jj) * a_i(ji,jj,jl) / MAX( at_i(ji,jj), epsi10 ) |
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| 144 | ! 2d option: melting of the upper cat first |
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| 145 | !!zda = MAX( zda_tot(ji,jj), - a_i(ji,jj,jl) ) |
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| 146 | !!zda_tot(ji,jj) = zda_tot(ji,jj) + zda |
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| 147 | |
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| 148 | ! Contribution to salt flux |
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| 149 | sfx_lam(ji,jj) = sfx_lam(ji,jj) - rhoic * ht_i(ji,jj,jl) * zda * sm_i(ji,jj,jl) * r1_rdtice |
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| 150 | |
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| 151 | ! Contribution to heat flux into the ocean [W.m-2], <0 |
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| 152 | !clemX hfx_thd(ji,jj) = hfx_thd(ji,jj) + zda * r1_rdtice * ( ht_i(ji,jj,jl) * SUM( e_i(ji,jj,:,jl) ) * r1_nlay_i & |
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| 153 | ! & + ht_s(ji,jj,jl) * e_s(ji,jj,1,jl) * r1_nlay_s ) |
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| 154 | hfx_thd(ji,jj) = hfx_thd(ji,jj) + rswitch * zda_tot(ji,jj) / MAX( at_i(ji,jj), epsi10 ) & |
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| 155 | & * r1_rdtice * ( SUM( e_i(ji,jj,:,jl) ) + e_s(ji,jj,1,jl) ) |
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| 156 | |
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| 157 | ! Contribution to mass flux |
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| 158 | wfx_lam(ji,jj) = wfx_lam(ji,jj) - zda * r1_rdtice * ( rhoic * ht_i(ji,jj,jl) + rhosn * ht_s(ji,jj,jl) ) |
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| 159 | |
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| 160 | ! new concentration |
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| 161 | a_i(ji,jj,jl) = a_i(ji,jj,jl) + zda |
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| 162 | END DO |
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| 163 | END DO |
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| 164 | END DO |
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| 165 | |
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| 166 | ! total concentration |
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| 167 | at_i(:,:) = SUM( a_i(:,:,:), dim=3 ) |
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| 168 | |
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| 169 | ! --- ensure that ht_i = 0 where a_i = 0 --- |
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| 170 | WHERE( a_i == 0._wp ) ht_i = 0._wp |
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| 171 | ! |
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| 172 | CALL wrk_dealloc( jpi,jpj, zda_tot ) |
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| 173 | ! |
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| 174 | END SUBROUTINE lim_thd_da |
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| 175 | |
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| 176 | #else |
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| 177 | !!---------------------------------------------------------------------- |
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| 178 | !! Default option Dummy Module No LIM-3 sea-ice model |
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| 179 | !!---------------------------------------------------------------------- |
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| 180 | CONTAINS |
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| 181 | SUBROUTINE lim_thd_da ! Empty routine |
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| 182 | END SUBROUTINE lim_thd_da |
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| 183 | #endif |
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| 184 | !!====================================================================== |
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| 185 | END MODULE limthd_da |
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