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limthd_da.F90 in NEMO/branches/UKMO/r8395_restart_datestamp/NEMOGCM/NEMO/LIM_SRC_3 – NEMO

source: NEMO/branches/UKMO/r8395_restart_datestamp/NEMOGCM/NEMO/LIM_SRC_3/limthd_da.F90 @ 10758

Last change on this file since 10758 was 10758, checked in by jcastill, 5 years ago

Remove svn keywords

File size: 10.2 KB
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1MODULE limthd_da
2   !!======================================================================
3   !!                       ***  MODULE limthd_da ***
4   !! LIM-3 sea-ice :  computation of lateral melting in the ice
5   !!======================================================================
6   !! History :   4.0   ! 2016-03 (C. Rousset) original code
7   !!---------------------------------------------------------------------
8#if defined key_lim3
9   !!----------------------------------------------------------------------
10   !!   'key_lim3'                                      LIM-3 sea-ice model
11   !!----------------------------------------------------------------------
12   !!   lim_thd_da   : sea ice lateral melting
13   !!----------------------------------------------------------------------
14   USE par_oce                ! ocean parameters
15   USE phycst                 ! physical constants (ocean directory)
16   USE sbc_oce, ONLY: sst_m   ! Surface boundary condition: ocean fields
17   USE ice                    ! LIM variables
18   USE lib_mpp                ! MPP library
19   USE wrk_nemo               ! work arrays
20   USE lib_fortran            ! Fortran utilities (allows no signed zero when 'key_nosignedzero' defined) 
21
22   IMPLICIT NONE
23   PRIVATE
24
25   PUBLIC   lim_thd_da        ! called by limthd module
26
27   !!----------------------------------------------------------------------
28   !! NEMO/LIM3 4.0 , UCL - NEMO Consortium (2011)
29   !! $Id$
30   !! Software governed by the CeCILL licence     (NEMOGCM/NEMO_CeCILL.txt)
31   !!----------------------------------------------------------------------
32CONTAINS
33
34   SUBROUTINE lim_thd_da
35      !!-------------------------------------------------------------------
36      !!                ***  ROUTINE lim_thd_da  ***   
37      !!   
38      !! ** Purpose :   computes sea ice lateral melting
39      !!
40      !! ** Method  :   dA/dt = - P * W   [s-1]
41      !!                   W = melting velocity [m.s-1]
42      !!                   P = perimeter of ice-ocean lateral interface normalized by grid cell area [m.m-2]
43      !!
44      !!                   W = m1 * (Tw -Tf)**m2                    --- originally from Josberger 1979 ---
45      !!                      (Tw - Tf) = elevation of water temp above freezing
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
47      !!                      m1 and m2 = (3.0e-6 , 1.36) best fit from MIZEX 84 experiment (Maykut and Perovich 1987) => moving ice
48      !!
49      !!                   P = N * pi * D                           --- from Rothrock and Thorndike 1984 ---
50      !!                      D = mean floe caliper diameter
51      !!                      N = number of floes = ice area / floe area(average) = A / (Cs * D**2)
52      !!                         A = ice concentration
53      !!                         Cs = deviation from a square (square:Cs=1 ; circle:Cs=pi/4 ; floe:Cs=0.66)
54      !!
55      !!                   D = Dmin * ( Astar / (Astar-A) )**beta   --- from Lupkes et al., 2012 (eq. 26-27) ---
56      !!                                                             
57      !!                      Astar = 1 / ( 1 - (Dmin/Dmax)**(1/beta) )
58      !!                      Dmin = minimum floe diameter (recommended to be 8m +- 20%)
59      !!                      Dmax = maximum floe diameter (recommended to be 300m, but it does not impact melting much except for Dmax<100m)
60      !!                      beta = 1.0 +-20% (recommended value)
61      !!                           = 0.3 best fit for western Fram Strait and Antarctica
62      !!                           = 1.4 best fit for eastern Fram Strait
63      !!
64      !! ** Tunable parameters  :   We propose to tune the lateral melting via 2 parameters
65      !!                               Dmin [6-10m]   => 6  vs 8m = +40% melting at the peak (A~0.5)
66      !!                                                 10 vs 8m = -20% melting
67      !!                               beta [0.8-1.2] => decrease = more melt and melt peaks toward higher concentration
68      !!                                                                  (A~0.5 for beta=1 ; A~0.8 for beta=0.2)
69      !!                                                 0.3 = best fit for western Fram Strait and Antarctica
70      !!                                                 1.4 = best fit for eastern Fram Strait
71      !!
72      !! ** Note   :   Former and more simple formulations for floe diameters can be found in Mai (1995),
73      !!               Birnbaum and Lupkes (2002), Lupkes and Birnbaum (2005). They are reviewed in Lupkes et al 2012
74      !!               A simpler implementation for CICE can be found in Bitz et al (2001) and Tsamados et al (2015)
75      !!
76      !! ** References
77      !!    Bitz, C. M., Holland, M. M., Weaver, A. J., & Eby, M. (2001).
78      !!              Simulating the ice‐thickness distribution in a coupled climate model.
79      !!              Journal of Geophysical Research: Oceans, 106(C2), 2441-2463.
80      !!    Josberger, E. G. (1979).
81      !!              Laminar and turbulent boundary layers adjacent to melting vertical ice walls in salt water
82      !!              (No. SCIENTIFIC-16). WASHINGTON UNIV SEATTLE DEPT OF ATMOSPHERIC SCIENCES.
83      !!    Lüpkes, C., Gryanik, V. M., Hartmann, J., & Andreas, E. L. (2012).
84      !!              A parametrization, based on sea ice morphology, of the neutral atmospheric drag coefficients
85      !!              for weather prediction and climate models.
86      !!              Journal of Geophysical Research: Atmospheres, 117(D13).
87      !!    Maykut, G. A., & Perovich, D. K. (1987).
88      !!              The role of shortwave radiation in the summer decay of a sea ice cover.
89      !!              Journal of Geophysical Research: Oceans, 92(C7), 7032-7044.
90      !!    Perovich, D. K. (1983).
91      !!              On the summer decay of a sea ice cover. (Doctoral dissertation, University of Washington).
92      !!    Rothrock, D. A., & Thorndike, A. S. (1984).
93      !!              Measuring the sea ice floe size distribution.
94      !!              Journal of Geophysical Research: Oceans, 89(C4), 6477-6486.
95      !!    Tsamados, M., Feltham, D., Petty, A., Schroeder, D., & Flocco, D. (2015).
96      !!              Processes controlling surface, bottom and lateral melt of Arctic sea ice in a state of the art sea ice model.
97      !!              Phil. Trans. R. Soc. A, 373(2052), 20140167.
98      !!---------------------------------------------------------------------
99      INTEGER             ::   ji, jj, jl      ! dummy loop indices
100      REAL(wp)            ::   zastar, zdfloe, zperi, zwlat, zda
101      REAL(wp), PARAMETER ::   zdmax = 300._wp
102      REAL(wp), PARAMETER ::   zcs   = 0.66_wp
103      REAL(wp), PARAMETER ::   zm1   = 3.e-6_wp
104      REAL(wp), PARAMETER ::   zm2   = 1.36_wp
105      !
106      REAL(wp), POINTER, DIMENSION(:,:) ::   zda_tot
107      !!---------------------------------------------------------------------
108      CALL wrk_alloc( jpi,jpj, zda_tot )
109
110      !------------------------------------------------------------!
111      ! --- Calculate reduction of total sea ice concentration --- !
112      !------------------------------------------------------------!
113      zastar = 1._wp / ( 1._wp - (rn_dmin / zdmax)**(1._wp/rn_beta) )
114     
115      DO jj = 1, jpj
116         DO ji = 1, jpi
117           
118            ! Mean floe caliper diameter [m]
119            zdfloe = rn_dmin * ( zastar / ( zastar - at_i(ji,jj) ) )**rn_beta
120           
121            ! Mean perimeter of the floe = N*pi*D = (A/cs*D^2)*pi*D [m.m-2]
122            zperi = at_i(ji,jj) * rpi / ( zcs * zdfloe )
123           
124            ! Melt speed rate [m/s]
125            zwlat = zm1 * ( MAX( 0._wp, sst_m(ji,jj) - ( t_bo(ji,jj) - rt0 ) ) )**zm2
126           
127            ! sea ice concentration decrease
128            zda_tot(ji,jj) = - MIN( zwlat * zperi * rdt_ice, at_i(ji,jj) )
129           
130         END DO
131      END DO
132     
133      !---------------------------------------------------------------------------------------------!
134      ! --- Distribute reduction among ice categories and calculate associated ice-ocean fluxes --- !
135      !---------------------------------------------------------------------------------------------!
136      DO jl = jpl, 1, -1
137         DO jj = 1, jpj
138            DO ji = 1, jpi
139               
140               ! decrease of concentration for the category jl
141               !    1st option: each category contributes to melting in proportion to its concentration
142               rswitch = MAX( 0._wp , SIGN( 1._wp, at_i(ji,jj) - epsi10 ) )
143               zda     = rswitch * zda_tot(ji,jj) * a_i(ji,jj,jl) / MAX( at_i(ji,jj), epsi10 )
144               !    2d option: melting of the upper cat first
145               !!zda = MAX( zda_tot(ji,jj), - a_i(ji,jj,jl) )
146               !!zda_tot(ji,jj) = zda_tot(ji,jj) + zda
147               
148               ! Contribution to salt flux
149               sfx_lam(ji,jj) = sfx_lam(ji,jj) - rhoic *  ht_i(ji,jj,jl) * zda * sm_i(ji,jj,jl) * r1_rdtice
150               
151               ! Contribution to heat flux into the ocean [W.m-2], <0 
152               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  &
153                  &                                                + ht_s(ji,jj,jl) *      e_s(ji,jj,1,jl)   * r1_nlay_s )
154               
155               ! Contribution to mass flux
156               wfx_lam(ji,jj) =  wfx_lam(ji,jj) - zda * r1_rdtice * ( rhoic * ht_i(ji,jj,jl) + rhosn * ht_s(ji,jj,jl) )
157               
158               ! new concentration
159               a_i(ji,jj,jl) = a_i(ji,jj,jl) + zda
160            END DO
161         END DO
162      END DO
163     
164      ! total concentration
165      at_i(:,:) = SUM( a_i(:,:,:), dim=3 )
166     
167      ! --- ensure that ht_i = 0 where a_i = 0 ---
168      WHERE( a_i == 0._wp ) ht_i = 0._wp
169      !
170      CALL wrk_dealloc( jpi,jpj, zda_tot )
171      !
172   END SUBROUTINE lim_thd_da
173   
174#else
175   !!----------------------------------------------------------------------
176   !!   Default option         Dummy Module          No LIM-3 sea-ice model
177   !!----------------------------------------------------------------------
178CONTAINS
179   SUBROUTINE lim_thd_da          ! Empty routine
180   END SUBROUTINE lim_thd_da
181#endif
182   !!======================================================================
183END MODULE limthd_da
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