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- MODULE icbthm
- !!======================================================================
- !! *** MODULE icbthm ***
- !! Icebergs: thermodynamics routines for icebergs
- !!======================================================================
- !! History : 3.3.1 ! 2010-01 (Martin&Adcroft) Original code
- !! - ! 2011-03 (Madec) Part conversion to NEMO form
- !! - ! Removal of mapping from another grid
- !! - ! 2011-04 (Alderson) Split into separate modules
- !! - ! 2011-05 (Alderson) Use tmask instead of tmask_i
- !!----------------------------------------------------------------------
- !!----------------------------------------------------------------------
- !! icb_thm : initialise
- !! reference for equations - M = Martin + Adcroft, OM 34, 2010
- !!----------------------------------------------------------------------
- USE par_oce ! NEMO parameters
- USE dom_oce ! NEMO domain
- USE in_out_manager ! NEMO IO routines, numout in particular
- USE lib_mpp ! NEMO MPI routines, ctl_stop in particular
- USE phycst ! NEMO physical constants
- USE sbc_oce
- USE eosbn2 ! equation of state
- USE lib_fortran, ONLY : DDPDD
- USE bdy_oce, ONLY : bdytmask,ln_bdy
- USE icb_oce ! define iceberg arrays
- USE icbutl ! iceberg utility routines
- USE icbdia ! iceberg budget routines
- IMPLICIT NONE
- PRIVATE
- PUBLIC icb_thm ! routine called in icbstp.F90 module
- !!----------------------------------------------------------------------
- !! NEMO/OCE 4.0 , NEMO Consortium (2018)
- !! $Id: icbthm.F90 15088 2021-07-06 13:03:34Z acc $
- !! Software governed by the CeCILL license (see ./LICENSE)
- !!----------------------------------------------------------------------
- CONTAINS
- SUBROUTINE icb_thm( kt )
- !!----------------------------------------------------------------------
- !! *** ROUTINE icb_thm ***
- !!
- !! ** Purpose : compute the iceberg thermodynamics.
- !!
- !! ** Method : - See Martin & Adcroft, Ocean Modelling 34, 2010
- !!----------------------------------------------------------------------
- INTEGER, INTENT(in) :: kt ! timestep number, just passed to icb_utl_print_berg
- !
- INTEGER :: ii, ij, jk, ikb
- REAL(wp) :: zM, zT, zW, zL, zSST, zVol, zLn, zWn, zTn, znVol, zIC, zDn, zD, zvb, zub, ztb
- REAL(wp) :: zMv, zMe, zMb, zmelt, zdvo, zdvob, zdva, zdM, zSs, zdMe, zdMb, zdMv
- REAL(wp) :: zSSS, zfzpt
- REAL(wp) :: zMnew, zMnew1, zMnew2, zheat_hcflux, zheat_latent, z1_12
- REAL(wp) :: zMbits, znMbits, zdMbitsE, zdMbitsM, zLbits, zAbits, zMbb
- REAL(wp) :: zxi, zyj, zff, z1_rday, z1_e1e2, zdt, z1_dt, z1_dt_e1e2, zdepw
- REAL(wp), DIMENSION(jpk) :: ztoce, zuoce, zvoce, ze3t, zzMv
- TYPE(iceberg), POINTER :: this, next
- TYPE(point) , POINTER :: pt
- !
- COMPLEX(dp), DIMENSION(jpi,jpj) :: cicb_melt, cicb_hflx
- !!----------------------------------------------------------------------
- !
- !! initialiaze cicb_melt and cicb_heat
- cicb_melt = CMPLX( 0.e0, 0.e0, dp )
- cicb_hflx = CMPLX( 0.e0, 0.e0, dp )
- !
- z1_rday = 1._wp / rday
- z1_12 = 1._wp / 12._wp
- zdt = berg_dt
- z1_dt = 1._wp / zdt
- !
- ! we're either going to ignore berg fresh water melt flux and associated heat
- ! or we pass it into the ocean, so at this point we set them both to zero,
- ! accumulate the contributions to them from each iceberg in the while loop following
- ! and then pass them (or not) to the ocean
- !
- berg_grid%floating_melt(:,:) = 0._wp
- ! calving_hflx re-used here as temporary workspace for the heat flux associated with melting
- berg_grid%calving_hflx(:,:) = 0._wp
- !
- ! virtual area set to 0
- virtual_area(:,:)= 0._wp
- virtual_area_e(:,:)= 0._wp
- !
- this => first_berg
- DO WHILE( ASSOCIATED(this) )
- !
- pt => this%current_point
- nknberg = this%number(1)
- CALL icb_utl_interp( pt%xi, pt%yj, & ! position
- & pssu=pt%ssu, pua=pt%ua, & ! oce/atm velocities
- & pssv=pt%ssv, pva=pt%va, & ! oce/atm velocities
- & psst=pt%sst, pcn=pt%cn, &
- & psss=pt%sss )
- IF ( nn_sample_rate > 0 .AND. MOD(kt-1,nn_sample_rate) == 0 ) THEN
- CALL icb_utl_interp( pt%xi, pt%yj, pe1=pt%e1, pe2=pt%e2, &
- & pui=pt%ui, pssh_i=pt%ssh_x, &
- & pvi=pt%vi, pssh_j=pt%ssh_y, &
- & phi=pt%hi, &
- & plat=pt%lat, plon=pt%lon )
- END IF
- !
- zSST = pt%sst
- zSSS = pt%sss
- CALL eos_fzp(zSSS,zfzpt) ! freezing point
- zIC = MIN( 1._wp, pt%cn + rn_sicn_shift ) ! Shift sea-ice concentration !!gm ???
- zM = pt%mass
- zT = pt%thickness ! total thickness
- zD = rho_berg_1_oce * zT ! draught (keel depth)
- zW = pt%width
- zL = pt%length
- zxi = pt%xi ! position in (i,j) referential
- zyj = pt%yj
- ii = INT( zxi + 0.5 ) ! T-cell of the berg
- ii = mi1( ii + (nn_hls-1) )
- ij = INT( zyj + 0.5 )
- ij = mj1( ij + (nn_hls-1) )
- zVol = zT * zW * zL
- ! Environment
- ! default sst, ssu and ssv
- ! ln_M2016: use temp, u and v profile
- IF ( ln_M2016 ) THEN
- ! load t, u, v and e3 profile at icb position
- CALL icb_utl_interp( pt%xi, pt%yj, ptoce=ztoce, puoce=zuoce, pvoce=zvoce, pe3t=ze3t )
-
- !compute bottom level
- CALL icb_utl_getkb( pt%kb, ze3t, zD )
- ikb = MIN(pt%kb,mbkt(ii,ij)) ! limit pt%kb by mbkt
- ! => bottom temperature used to fill ztoce(mbkt:jpk)
- ztb = ztoce(ikb) ! basal temperature
- zub = zuoce(ikb)
- zvb = zvoce(ikb)
- ELSE
- ztb = pt%sst
- zub = pt%ssu
- zvb = pt%ssv
- END IF
- zdvob = SQRT( (pt%uvel-zub)**2 + (pt%vvel-zvb)**2 ) ! relative basal velocity
- zdva = SQRT( (pt%ua -pt%ssu)**2 + (pt%va -pt%ssv)**2 ) ! relative wind
- zSs = 1.5_wp * SQRT( zdva ) + 0.1_wp * zdva ! Sea state (eqn M.A9)
- !
- ! Melt rates in m/s (i.e. division by rday)
- ! Buoyant convection at sides (eqn M.A10)
- IF ( ln_M2016 ) THEN
- ! averaging along all the iceberg draft
- zzMv(:) = MAX( 7.62d-3*ztoce(:)+1.29d-3*(ztoce(:)**2), 0._wp ) * z1_rday
- CALL icb_utl_zavg(zMv, zzMv, ze3t, zD, ikb )
- ELSE
- zMv = MAX( 7.62d-3*zSST+1.29d-3*(zSST**2), 0._wp ) * z1_rday
- END IF
- !
- ! Basal turbulent melting (eqn M.A7 )
- IF ( zSST > zfzpt ) THEN ! Calculate basal melting only if SST above freezing point
- zMb = MAX( 0.58_wp*(zdvob**0.8_wp)*(ztb+4.0_wp)/(zL**0.2_wp) , 0._wp ) * z1_rday
- ELSE
- zMb = 0._wp ! No basal melting if SST below freezing point
- ENDIF
- !
- ! Wave erosion (eqn M.A8 )
- zMe = MAX( z1_12*(zSST+2.)*zSs*(1._wp+COS(rpi*(zIC**3))) , 0._wp ) * z1_rday
- IF( ln_operator_splitting ) THEN ! Operator split update of volume/mass
- zTn = MAX( zT - zMb*zdt , 0._wp ) ! new total thickness (m)
- znVol = zTn * zW * zL ! new volume (m^3)
- zMnew1 = ( znVol / zVol ) * zM ! new mass (kg)
- zdMb = zM - zMnew1 ! mass lost to basal melting (>0) (kg)
- !
- zLn = MAX( zL - zMv*zdt , 0._wp ) ! new length (m)
- zWn = MAX( zW - zMv*zdt , 0._wp ) ! new width (m)
- znVol = zTn * zWn * zLn ! new volume (m^3)
- zMnew2 = ( znVol / zVol ) * zM ! new mass (kg)
- zdMv = zMnew1 - zMnew2 ! mass lost to buoyant convection (>0) (kg)
- !
- zLn = MAX( zLn - zMe*zdt , 0._wp ) ! new length (m)
- zWn = MAX( zWn - zMe*zdt , 0._wp ) ! new width (m)
- znVol = zTn * zWn * zLn ! new volume (m^3)
- zMnew = ( znVol / zVol ) * zM ! new mass (kg)
- zdMe = zMnew2 - zMnew ! mass lost to erosion (>0) (kg)
- zdM = zM - zMnew ! mass lost to all erosion and melting (>0) (kg)
- !
- ELSE ! Update dimensions of berg
- zLn = MAX( zL -(zMv+zMe)*zdt ,0._wp ) ! (m)
- zWn = MAX( zW -(zMv+zMe)*zdt ,0._wp ) ! (m)
- zTn = MAX( zT - zMb *zdt ,0._wp ) ! (m)
- ! Update volume and mass of berg
- znVol = zTn*zWn*zLn ! (m^3)
- zMnew = (znVol/zVol)*zM ! (kg)
- zdM = zM - zMnew ! (kg)
- zdMb = (zM/zVol) * (zW* zL ) *zMb*zdt ! approx. mass loss to basal melting (kg)
- zdMe = (zM/zVol) * (zT*(zW+zL)) *zMe*zdt ! approx. mass lost to erosion (kg)
- zdMv = (zM/zVol) * (zT*(zW+zL)) *zMv*zdt ! approx. mass loss to buoyant convection (kg)
- ENDIF
- IF( rn_bits_erosion_fraction > 0._wp ) THEN ! Bergy bits
- !
- zMbits = pt%mass_of_bits ! mass of bergy bits (kg)
- zdMbitsE = rn_bits_erosion_fraction * zdMe ! change in mass of bits (kg)
- znMbits = zMbits + zdMbitsE ! add new bergy bits to mass (kg)
- zLbits = MIN( zL, zW, zT, 40._wp ) ! assume bergy bits are smallest dimension or 40 meters
- zAbits = ( zMbits / rn_rho_bergs ) / zLbits ! Effective bottom area (assuming T=Lbits)
- zMbb = MAX( 0.58_wp*(zdvob**0.8_wp)*(zSST+2._wp) / &
- & ( zLbits**0.2_wp ) , 0._wp ) * z1_rday ! Basal turbulent melting (for bits)
- zMbb = rn_rho_bergs * zAbits * zMbb ! in kg/s
- zdMbitsM = MIN( zMbb*zdt , znMbits ) ! bergy bits mass lost to melting (kg)
- znMbits = znMbits-zdMbitsM ! remove mass lost to bergy bits melt
- IF( zMnew == 0._wp ) THEN ! if parent berg has completely melted then
- zdMbitsM = zdMbitsM + znMbits ! instantly melt all the bergy bits
- znMbits = 0._wp
- ENDIF
- ELSE ! No bergy bits
- zAbits = 0._wp
- zdMbitsE = 0._wp
- zdMbitsM = 0._wp
- znMbits = pt%mass_of_bits ! retain previous value incase non-zero
- ENDIF
- ! use tmask rather than tmask_i when dealing with icebergs
- IF( tmask(ii,ij,1) /= 0._wp ) THEN ! Add melting to the grid and field diagnostics
- z1_e1e2 = r1_e1e2t(ii,ij) * this%mass_scaling
- z1_dt_e1e2 = z1_dt * z1_e1e2
- !
- ! iceberg melt
- !! the use of DDPDD function for the cumulative sum is needed for reproducibility
- zmelt = ( zdM - ( zdMbitsE - zdMbitsM ) ) * z1_dt ! kg/s
- CALL DDPDD( CMPLX( zmelt * z1_e1e2, 0.e0, dp ), cicb_melt(ii,ij) )
- !
- ! iceberg heat flux
- !! the use of DDPDD function for the cumulative sum is needed for reproducibility
- !! NB. The src_calving_hflx field is currently hardwired to zero in icb_stp, which means that the
- !! heat density of the icebergs is zero and the heat content flux to the ocean from iceberg
- !! melting is always zero. Leaving the term in the code until such a time as this is fixed. DS.
- zheat_hcflux = zmelt * pt%heat_density ! heat content flux : kg/s x J/kg = J/s
- zheat_latent = - zmelt * rLfus ! latent heat flux: kg/s x J/kg = J/s
- CALL DDPDD( CMPLX( ( zheat_hcflux + zheat_latent ) * z1_e1e2, 0.e0, dp ), cicb_hflx(ii,ij) )
- !
- ! diagnostics
- CALL icb_dia_melt( ii, ij, zMnew, zheat_hcflux, zheat_latent, this%mass_scaling, &
- & zdM, zdMbitsE, zdMbitsM, zdMb, zdMe, &
- & zdMv, z1_dt_e1e2, z1_e1e2 )
- ELSE
- WRITE(numout,*) 'icb_thm: berg ',this%number(:),' appears to have grounded at ',narea,ii,ij
- CALL icb_utl_print_berg( this, kt )
- WRITE(numout,*) 'msk=',tmask(ii,ij,1), e1e2t(ii,ij)
- CALL ctl_stop('icb_thm', 'berg appears to have grounded!')
- ENDIF
- ! Rolling
- zDn = rho_berg_1_oce * zTn ! draught (keel depth)
- IF( zDn > 0._wp .AND. MAX(zWn,zLn) < SQRT( 0.92*(zDn**2) + 58.32*zDn ) ) THEN
- zT = zTn
- zTn = zWn
- zWn = zT
- ENDIF
- ! Store the new state of iceberg (with L>W)
- pt%mass = zMnew
- pt%mass_of_bits = znMbits
- pt%thickness = zTn
- pt%width = MIN( zWn , zLn )
- pt%length = MAX( zWn , zLn )
- next=>this%next
- !!gm add a test to avoid over melting ?
- !!pm I agree, over melting could break conservation (more melt than calving)
- IF( zMnew <= 0._wp ) THEN ! Delete the berg if completely melted
- CALL icb_utl_delete( first_berg, this )
- !
- ELSE IF (ln_bdy .AND. bdytmask(ii,ij)==0.) THEN !!pm + CK remove icb if at bdy
-
- CALL icb_utl_delete( first_berg, this )
-
- ELSE ! Diagnose mass distribution on grid
- z1_e1e2 = r1_e1e2t(ii,ij) * this%mass_scaling
- CALL icb_dia_size( ii, ij, zWn, zLn, zAbits, &
- & this%mass_scaling, zMnew, znMbits, z1_e1e2 )
- !
- ! ! diagnose virtual area on grid (ln_icb_area_mask or ln_icb_diag)
- virtual_area(ii,ij) = virtual_area(ii,ij) + ( zWn * zLn + zAbits ) * this%mass_scaling ! m^2
- !
- ENDIF
- !
-
-
- this=>next
- !
- END DO
- !
- berg_grid%floating_melt = REAL(cicb_melt,dp) ! kg/m2/s
- berg_grid%calving_hflx = REAL(cicb_hflx,dp)
- !
- ! now use melt and associated heat flux in ocean (or not)
- !
- IF(.NOT. ln_passive_mode ) THEN
- emp (:,:) = emp (:,:) - berg_grid%floating_melt(:,:)
- qns (:,:) = qns (:,:) + berg_grid%calving_hflx (:,:)
- ENDIF
- !
- END SUBROUTINE icb_thm
- !!======================================================================
- END MODULE icbthm
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