1 | MODULE bdyice |
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2 | !!====================================================================== |
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3 | !! *** MODULE bdyice *** |
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4 | !! Unstructured Open Boundary Cond. : Flow Relaxation Scheme applied sea-ice |
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5 | !!====================================================================== |
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6 | !! History : 3.3 ! 2010-09 (D. Storkey) Original code |
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7 | !!---------------------------------------------------------------------- |
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8 | #if defined key_bdy && defined key_lim2 |
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9 | !!---------------------------------------------------------------------- |
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10 | !! 'key_bdy' and Unstructured Open Boundary Conditions |
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11 | !! 'key_lim2' LIM-2 sea ice model |
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12 | !!---------------------------------------------------------------------- |
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13 | !! bdy_ice : Relaxation of tracers on unstructured open boundaries |
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14 | !!---------------------------------------------------------------------- |
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15 | USE oce ! ocean dynamics and tracers variables |
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16 | USE ice_2 ! LIM_2 ice variables |
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17 | USE dom_oce ! ocean space and time domain variables |
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18 | USE bdy_oce ! ocean open boundary conditions |
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19 | USE lbclnk ! ocean lateral boundary conditions (or mpp link) |
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20 | USE in_out_manager ! write to numout file |
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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 bdy_ice ! routine called in sbcmod |
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26 | |
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27 | !!---------------------------------------------------------------------- |
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28 | !! NEMO/OPA 3.3 , NEMO Consortium (2010) |
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29 | !! Software governed by the CeCILL licence (modipsl/doc/NEMO_CeCILL.txt) |
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30 | !!---------------------------------------------------------------------- |
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31 | CONTAINS |
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32 | |
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33 | SUBROUTINE bdy_ice( kt ) |
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34 | !!------------------------------------------------------------------------------ |
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35 | !! *** SUBROUTINE bdy_ice *** |
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36 | !! |
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37 | !! ** Purpose : Apply the Flow Relaxation Scheme for sea-ice fields in the case |
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38 | !! of unstructured open boundaries. Currently only tested for LIM2. |
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39 | !! |
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40 | !! Reference : Engedahl H., 1995: Use of the flow relaxation scheme in a three- |
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41 | !! dimensional baroclinic ocean model with realistic topography. Tellus, 365-382. |
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42 | !!------------------------------------------------------------------------------ |
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43 | INTEGER, INTENT( in ) :: kt ! model time step index |
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44 | !! |
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45 | INTEGER :: jb, jk, jgrd ! dummy loop indices |
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46 | INTEGER :: ii, ij ! local scalar |
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47 | REAL(wp) :: zwgt, zwgt1 ! local scalar |
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48 | !!------------------------------------------------------------------------------ |
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49 | ! |
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50 | jgrd = 1 ! Everything is at T-points here |
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51 | ! |
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52 | IF( ln_bdy_ice_frs ) THEN ! update ice fields by relaxation at the boundary |
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53 | DO jb = 1, nblen(jgrd) |
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54 | DO jk = 1, jpkm1 |
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55 | ii = nbi(jb,jgrd) |
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56 | ij = nbj(jb,jgrd) |
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57 | zwgt = nbw(jb,jgrd) |
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58 | zwgt1 = 1.e0 - nbw(jb,jgrd) |
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59 | frld (ii,ij) = ( frld (ii,ij) * zwgt1 + frld_bdy (jb) * zwgt ) * tmask(ii,ij,1) ! Leads fraction |
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60 | hicif(ii,ij) = ( hicif(ii,ij) * zwgt1 + hicif_bdy(jb) * zwgt ) * tmask(ii,ij,1) ! Ice depth |
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61 | hsnif(ii,ij) = ( hsnif(ii,ij) * zwgt1 + hsnif_bdy(jb) * zwgt ) * tmask(ii,ij,1) ! Snow depth |
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62 | END DO |
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63 | END DO |
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64 | CALL lbc_lnk( frld, 'T', 1. ) ! lateral boundary conditions |
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65 | CALL lbc_lnk( hicif, 'T', 1. ) ; CALL lbc_lnk( hsnif, 'T', 1. ) |
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66 | ! |
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67 | ELSE ! we have called this routine without ln_bdy_ice_frs not set |
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68 | IF( kt == nit000 ) CALL ctl_warn( 'E R R O R (possible) called bdy_ice when ln_bdy_ice_frs is false?' ) |
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69 | ENDIF |
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70 | ! |
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71 | END SUBROUTINE bdy_ice |
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72 | #else |
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73 | !!--------------------------------------------------------------------------------- |
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74 | !! Default option Empty module |
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75 | !!--------------------------------------------------------------------------------- |
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76 | CONTAINS |
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77 | SUBROUTINE bdy_ice( kt ) ! Empty routine |
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78 | WRITE(*,*) 'bdy_ice: You should not have seen this print! error?', kt |
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79 | END SUBROUTINE bdy_ice |
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80 | #endif |
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81 | |
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82 | !!================================================================================= |
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83 | END MODULE bdyice |
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