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- MODULE dynldf_lap
- !!======================================================================
- !! *** MODULE dynldf_lap ***
- !! Ocean dynamics: lateral viscosity trend
- !!======================================================================
- !! History : OPA ! 1990-09 (G. Madec) Original code
- !! 4.0 ! 1991-11 (G. Madec)
- !! 6.0 ! 1996-01 (G. Madec) statement function for e3 and ahm
- !! NEMO 1.0 ! 2002-06 (G. Madec) F90: Free form and module
- !! - ! 2004-08 (C. Talandier) New trends organization
- !!----------------------------------------------------------------------
- !!----------------------------------------------------------------------
- !! dyn_ldf_lap : update the momentum trend with the lateral diffusion
- !! using an iso-level harmonic operator
- !!----------------------------------------------------------------------
- USE oce ! ocean dynamics and tracers
- USE dom_oce ! ocean space and time domain
- USE phycst ! physical constants
- USE ldfdyn_oce ! ocean dynamics: lateral physics
- USE zdf_oce ! ocean vertical physics
- !
- USE in_out_manager ! I/O manager
- USE iom ! I/O library
- USE timing ! Timing
- IMPLICIT NONE
- PRIVATE
- PUBLIC dyn_ldf_lap ! called by step.F90
- !! * Substitutions
- # include "domzgr_substitute.h90"
- # include "ldfdyn_substitute.h90"
- # include "vectopt_loop_substitute.h90"
- !!----------------------------------------------------------------------
- !! NEMO/OPA 3.3 , NEMO Consortium (2010)
- !! $Id: dynldf_lap.F90 4990 2014-12-15 16:42:49Z timgraham $
- !! Software governed by the CeCILL licence (NEMOGCM/NEMO_CeCILL.txt)
- !!----------------------------------------------------------------------
- CONTAINS
- SUBROUTINE dyn_ldf_lap( kt )
- !!----------------------------------------------------------------------
- !! *** ROUTINE dyn_ldf_lap ***
- !!
- !! ** Purpose : Compute the before horizontal tracer (t & s) diffusive
- !! trend and add it to the general trend of tracer equation.
- !!
- !! ** Method : The before horizontal momentum diffusion trend is an
- !! harmonic operator (laplacian type) which separates the divergent
- !! and rotational parts of the flow.
- !! Its horizontal components are computed as follow:
- !! difu = 1/e1u di[ahmt hdivb] - 1/(e2u*e3u) dj-1[e3f ahmf rotb]
- !! difv = 1/e2v dj[ahmt hdivb] + 1/(e1v*e3v) di-1[e3f ahmf rotb]
- !! in the rotational part of the diffusion.
- !! Add this before trend to the general trend (ua,va):
- !! (ua,va) = (ua,va) + (diffu,diffv)
- !!
- !! ** Action : - Update (ua,va) with the iso-level harmonic mixing trend
- !!----------------------------------------------------------------------
- INTEGER, INTENT( in ) :: kt ! ocean time-step index
- !
- INTEGER :: ji, jj, jk ! dummy loop indices
- REAL(wp) :: zua, zva, ze2u, ze1v ! local scalars
- REAL(wp), ALLOCATABLE, DIMENSION(:,:) :: z2d ! 2D workspace
- !!----------------------------------------------------------------------
- !
- IF( nn_timing == 1 ) CALL timing_start('dyn_ldf_lap')
- !
- IF( kt == nit000 ) THEN
- IF(lwp) WRITE(numout,*)
- IF(lwp) WRITE(numout,*) 'dyn_ldf : iso-level harmonic (laplacian) operator'
- IF(lwp) WRITE(numout,*) '~~~~~~~ '
- ENDIF
- ! ! ===============
- DO jk = 1, jpkm1 ! Horizontal slab
- ! ! ===============
- DO jj = 2, jpjm1
- DO ji = fs_2, fs_jpim1 ! vector opt.
- ze2u = rotb (ji,jj,jk) * fsahmf(ji,jj,jk) * fse3f(ji,jj,jk)
- ze1v = hdivb(ji,jj,jk) * fsahmt(ji,jj,jk)
- ! horizontal diffusive trends
- zua = - ( ze2u - rotb (ji,jj-1,jk)*fsahmf(ji,jj-1,jk)*fse3f(ji,jj-1,jk) ) / ( e2u(ji,jj) * fse3u(ji,jj,jk) ) &
- + ( hdivb(ji+1,jj,jk)*fsahmt(ji+1,jj,jk) - ze1v ) / e1u(ji,jj)
- zva = + ( ze2u - rotb (ji-1,jj,jk)*fsahmf(ji-1,jj,jk)*fse3f(ji-1,jj,jk) ) / ( e1v(ji,jj) * fse3v(ji,jj,jk) ) &
- + ( hdivb(ji,jj+1,jk)*fsahmt(ji,jj+1,jk) - ze1v ) / e2v(ji,jj)
- ! add it to the general momentum trends
- ua(ji,jj,jk) = ua(ji,jj,jk) + zua
- va(ji,jj,jk) = va(ji,jj,jk) + zva
- END DO
- END DO
- ! ! ===============
- END DO ! End of slab
- ! ! ===============
-
- IF( iom_use('dispkexyfo') ) THEN ! ocean Kinetic Energy dissipation per unit area
- ! ! due to lateral friction (xy=lateral)
- ! see NEMO_book appendix C, §C.7.2 (N.B. here averaged at t-points)
- ! local dissipation of KE at t-point due to laplacian operator is given by :
- ! - ahmt hdivb**2 - mi( mj(ahmf rotb**2 e1f*e2f*e3t) ) / (e1e2t*e3t)
- !
- ALLOCATE( z2d(jpi,jpj) )
- z2d(:,:) = 0._wp
- DO jk = 1, jpkm1
- DO jj = 2, jpjm1
- DO ji = 2, jpim1
- z2d(ji,jj) = z2d(ji,jj) - ( &
- & hdivb(ji,jj,jk)**2 * fsahmt(ji,jj,jk) * fse3t_n(ji,jj,jk) &
- & + 0.25_wp * ( &
- & rotb (ji ,jj ,jk)**2 * fsahmf(ji ,jj ,jk) * e12f(ji ,jj ) * fse3f(ji ,jj ,jk) &
- & + rotb (ji-1,jj ,jk)**2 * fsahmf(ji-1,jj ,jk) * e12f(ji-1,jj ) * fse3f(ji-1,jj ,jk) &
- & + rotb (ji ,jj-1,jk)**2 * fsahmf(ji ,jj-1,jk) * e12f(ji ,jj-1) * fse3f(ji ,jj-1,jk) &
- & + rotb (ji-1,jj-1,jk)**2 * fsahmf(ji-1,jj-1,jk) * e12f(ji-1,jj-1) * fse3f(ji-1,jj-1,jk) &
- & ) * r1_e12t(ji,jj) ) * tmask(ji,jj,jk)
- END DO
- END DO
- END DO
- z2d(:,:) = rau0 * z2d(:,:)
- CALL lbc_lnk( z2d,'T', 1. )
- CALL iom_put( 'dispkexyfo', z2d )
- DEALLOCATE( z2d )
- ENDIF
- IF( nn_timing == 1 ) CALL timing_stop('dyn_ldf_lap')
- !
- END SUBROUTINE dyn_ldf_lap
- !!======================================================================
- END MODULE dynldf_lap
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