source: LMDZ6/branches/Amaury_dev/libf/dyn3d/top_bound.F90 @ 5325

! $Id: top_bound.F90 5159 2024-08-02 19:58:25Z abarral $

SUBROUTINE top_bound(vcov, ucov, teta, masse, dt)

  USE comconst_mod, ONLY: iflag_top_bound, mode_top_bound, &
          tau_top_bound
  USE comvert_mod, ONLY: presnivs, preff, scaleheight
  USE lmdz_iniprint, ONLY: lunout, prt_level
  USE lmdz_comdissipn, ONLY: tetaudiv, tetaurot, tetah, cdivu, crot, cdivh
  USE lmdz_comgeom2

USE lmdz_dimensions, ONLY: iim, jjm, llm, ndm
  USE lmdz_paramet
  IMPLICIT NONE
  !




  ! ..  DISSIPATION LINEAIRE A HAUT NIVEAU, RUN MESO,
  ! F. LOTT DEC. 2006
  !                             (  10/12/06  )

  !=======================================================================

  !   Auteur:  F. LOTT
  !   -------

  !   Objet:
  !   ------

  !   Dissipation linéaire (ex top_bound de la physique)

  !=======================================================================

  ! top_bound sponge layer model:
  ! Quenching is modeled as: A(t)=Am+A0*exp(-lambda*t)
  ! where Am is the zonal average of the field (or zero), and lambda the inverse
  ! of the characteristic quenching/relaxation time scale
  ! Thus, assuming Am to be time-independent, field at time t+dt is given by:
  ! A(t+dt)=A(t)-(A(t)-Am)*(1-exp(-lambda*t))
  ! Moreover lambda can be a function of model level (see below), and relaxation
  ! can be toward the average zonal field or just zero (see below).

  ! NB: top_bound sponge is only called from leapfrog if ok_strato=.TRUE.

  ! sponge parameters: (loaded/set in conf_gcm.F ; stored in comconst_mod)
  !    iflag_top_bound=0 for no sponge
  !    iflag_top_bound=1 for sponge over 4 topmost layers
  !    iflag_top_bound=2 for sponge from top to ~1% of top layer pressure
  !    mode_top_bound=0: no relaxation
  !    mode_top_bound=1: u and v relax towards 0
  !    mode_top_bound=2: u and v relax towards their zonal mean
  !    mode_top_bound=3: u,v and pot. temp. relax towards their zonal mean
  !    tau_top_bound : inverse of charactericstic relaxation time scale at
  !                   the topmost layer (Hz)

  !   Arguments:
  !   ----------

  REAL, INTENT(INOUT) :: ucov(iip1, jjp1, llm) ! covariant zonal wind
  REAL, INTENT(INOUT) :: vcov(iip1, jjm, llm) ! covariant meridional wind
  REAL, INTENT(INOUT) :: teta(iip1, jjp1, llm) ! potential temperature
  REAL, INTENT(IN) :: masse(iip1, jjp1, llm) ! mass of atmosphere
  REAL, INTENT(IN) :: dt ! time step (s) of sponge model

  !   Local:
  !   ------

  REAL :: massebx(iip1, jjp1, llm), masseby(iip1, jjm, llm), zm
  REAL :: uzon(jjp1, llm), vzon(jjm, llm), tzon(jjp1, llm)

  INTEGER :: i
  REAL, SAVE :: rdamp(llm) ! quenching coefficient
  REAL, save :: lambda(llm) ! inverse or quenching time scale (Hz)

  LOGICAL, SAVE :: first = .TRUE.

  INTEGER :: j, l

  IF (iflag_top_bound==0) return

  IF (first) THEN
    IF (iflag_top_bound==1) THEN
      ! sponge quenching over the topmost 4 atmospheric layers
      lambda(:) = 0.
      lambda(llm) = tau_top_bound
      lambda(llm - 1) = tau_top_bound / 2.
      lambda(llm - 2) = tau_top_bound / 4.
      lambda(llm - 3) = tau_top_bound / 8.
    ELSE IF (iflag_top_bound==2) THEN
      ! sponge quenching over topmost layers down to pressures which are
      ! higher than 100 times the topmost layer pressure
      lambda(:) = tau_top_bound &
              * max(presnivs(llm) / presnivs(:) - 0.01, 0.)
    endif

    ! quenching coefficient rdamp(:)
    ! rdamp(:)=dt*lambda(:) ! Explicit Euler approx.
    rdamp(:) = 1. - exp(-lambda(:) * dt)

    WRITE(lunout, *)'TOP_BOUND mode', mode_top_bound
    WRITE(lunout, *)'Sponge layer coefficients'
    WRITE(lunout, *)'p (Pa)  z(km)  tau(s)   1./tau (Hz)'
    DO l = 1, llm
      IF (rdamp(l)/=0.) THEN
        WRITE(lunout, '(6(1pe12.4,1x))') &
                presnivs(l), log(preff / presnivs(l)) * scaleheight, &
                1. / lambda(l), lambda(l)
      endif
    enddo
    first = .FALSE.
  ENDIF ! of if (first)

  CALL massbar(masse, massebx, masseby)

  ! compute zonal average of vcov and u
  IF (mode_top_bound>=2) THEN
    DO l = 1, llm
      DO j = 1, jjm
        vzon(j, l) = 0.
        zm = 0.
        DO i = 1, iim
          ! NB: we can work using vcov zonal mean rather than v since the
          ! cv coefficient (which relates the two) only varies with latitudes
          vzon(j, l) = vzon(j, l) + vcov(i, j, l) * masseby(i, j, l)
          zm = zm + masseby(i, j, l)
        enddo
        vzon(j, l) = vzon(j, l) / zm
      enddo
    enddo

    DO l = 1, llm
      DO j = 2, jjm ! excluding poles
        uzon(j, l) = 0.
        zm = 0.
        DO i = 1, iim
          uzon(j, l) = uzon(j, l) + massebx(i, j, l) * ucov(i, j, l) / cu(i, j)
          zm = zm + massebx(i, j, l)
        enddo
        uzon(j, l) = uzon(j, l) / zm
      enddo
    enddo
  else ! ucov and vcov will relax towards 0
    vzon(:, :) = 0.
    uzon(:, :) = 0.
  ENDIF ! of if (mode_top_bound.ge.2)

  ! compute zonal average of potential temperature, if necessary
  IF (mode_top_bound>=3) THEN
    DO l = 1, llm
      DO j = 2, jjm ! excluding poles
        zm = 0.
        tzon(j, l) = 0.
        DO i = 1, iim
          tzon(j, l) = tzon(j, l) + teta(i, j, l) * masse(i, j, l)
          zm = zm + masse(i, j, l)
        enddo
        tzon(j, l) = tzon(j, l) / zm
      enddo
    enddo
  ENDIF ! of if (mode_top_bound.ge.3)

  IF (mode_top_bound>=1) THEN
    ! Apply sponge quenching on vcov:
    DO l = 1, llm
      DO i = 1, iip1
        DO j = 1, jjm
          vcov(i, j, l) = vcov(i, j, l) &
                  - rdamp(l) * (vcov(i, j, l) - vzon(j, l))
        enddo
      enddo
    enddo

    ! Apply sponge quenching on ucov:
    DO l = 1, llm
      DO i = 1, iip1
        DO j = 2, jjm ! excluding poles
          ucov(i, j, l) = ucov(i, j, l) &
                  - rdamp(l) * (ucov(i, j, l) - cu(i, j) * uzon(j, l))
        enddo
      enddo
    enddo
  ENDIF ! of if (mode_top_bound.ge.1)

  IF (mode_top_bound>=3) THEN
    ! Apply sponge quenching on teta:
    DO l = 1, llm
      DO i = 1, iip1
        DO j = 2, jjm ! excluding poles
          teta(i, j, l) = teta(i, j, l) &
                  - rdamp(l) * (teta(i, j, l) - tzon(j, l))
        enddo
      enddo
    enddo
  ENDIF ! of if (mode_top_bound.ge.3)

END SUBROUTINE top_bound