#define WRF_PORT
#define MODAL_AERO
! Updated to CESM1.0.3 (CAM5.1.01) by Balwinder.Singh@pnnl.gov
module trb_mtn_stress 2,2
use shr_kind_mod
, only : r8 => shr_kind_r8
#ifndef WRF_PORT
use cam_logfile, only : iulog
#else
use module_cam_support, only: iulog
#endif
implicit none
private
save
public init_tms ! Initialization
public compute_tms ! Full routine
! ------------ !
! Private data !
! ------------ !
real(r8), parameter :: horomin= 1._r8 ! Minimum value of subgrid orographic height for mountain stress [ m ]
real(r8), parameter :: z0max = 100._r8 ! Maximum value of z_0 for orography [ m ]
real(r8), parameter :: dv2min = 0.01_r8 ! Minimum shear squared [ m2/s2 ]
real(r8) :: orocnst ! Converts from standard deviation to height [ no unit ]
real(r8) :: z0fac ! Factor determining z_0 from orographic standard deviation [ no unit ]
real(r8) :: karman ! von Karman constant
real(r8) :: gravit ! Acceleration due to gravity
real(r8) :: rair ! Gas constant for dry air
contains
!============================================================================ !
! !
!============================================================================ !
subroutine init_tms( kind, oro_in, z0fac_in, karman_in, gravit_in, rair_in ) 1
integer, intent(in) :: kind
real(r8), intent(in) :: oro_in, z0fac_in, karman_in, gravit_in, rair_in
if( kind .ne. r8 ) then
write(iulog,*) 'KIND of reals passed to init_tms -- exiting.'
stop 'compute_tms'
endif
orocnst = oro_in
z0fac = z0fac_in
karman = karman_in
gravit = gravit_in
rair = rair_in
return
end subroutine init_tms
!============================================================================ !
! !
!============================================================================ !
subroutine compute_tms( pcols , pver , ncol , & 1
u , v , t , pmid , exner , &
zm , sgh , ksrf , taux , tauy , &
landfrac )
!------------------------------------------------------------------------------ !
! Turbulent mountain stress parameterization !
! !
! Returns surface drag coefficient and stress associated with subgrid mountains !
! For points where the orographic variance is small ( including ocean ), !
! the returned surface drag coefficient and stress is zero. !
! !
! Lastly arranged : Sungsu Park. Jan. 2010. !
!------------------------------------------------------------------------------ !
! ---------------------- !
! Input-Output Arguments !
! ---------------------- !
integer, intent(in) :: pcols ! Number of columns dimensioned
integer, intent(in) :: pver ! Number of model layers
integer, intent(in) :: ncol ! Number of columns actually used
real(r8), intent(in) :: u(pcols,pver) ! Layer mid-point zonal wind [ m/s ]
real(r8), intent(in) :: v(pcols,pver) ! Layer mid-point meridional wind [ m/s ]
real(r8), intent(in) :: t(pcols,pver) ! Layer mid-point temperature [ K ]
real(r8), intent(in) :: pmid(pcols,pver) ! Layer mid-point pressure [ Pa ]
real(r8), intent(in) :: exner(pcols,pver) ! Layer mid-point exner function [ no unit ]
real(r8), intent(in) :: zm(pcols,pver) ! Layer mid-point height [ m ]
real(r8), intent(in) :: sgh(pcols) ! Standard deviation of orography [ m ]
real(r8), intent(in) :: landfrac(pcols) ! Land fraction [ fraction ]
real(r8), intent(out) :: ksrf(pcols) ! Surface drag coefficient [ kg/s/m2 ]
real(r8), intent(out) :: taux(pcols) ! Surface zonal wind stress [ N/m2 ]
real(r8), intent(out) :: tauy(pcols) ! Surface meridional wind stress [ N/m2 ]
! --------------- !
! Local Variables !
! --------------- !
integer :: i ! Loop index
integer :: kb, kt ! Bottom and top of source region
real(r8) :: horo ! Orographic height [ m ]
real(r8) :: z0oro ! Orographic z0 for momentum [ m ]
real(r8) :: dv2 ! (delta v)**2 [ m2/s2 ]
real(r8) :: ri ! Richardson number [ no unit ]
real(r8) :: stabfri ! Instability function of Richardson number [ no unit ]
real(r8) :: rho ! Density [ kg/m3 ]
real(r8) :: cd ! Drag coefficient [ no unit ]
real(r8) :: vmag ! Velocity magnitude [ m /s ]
! ----------------------- !
! Main Computation Begins !
! ----------------------- !
do i = 1, ncol
! determine subgrid orgraphic height ( mean to peak )
horo = orocnst * sgh(i)
! No mountain stress if horo is too small
if( horo < horomin ) then
ksrf(i) = 0._r8
taux(i) = 0._r8
tauy(i) = 0._r8
else
! Determine z0m for orography
z0oro = min( z0fac * horo, z0max )
! Calculate neutral drag coefficient
cd = ( karman / log( ( zm(i,pver) + z0oro ) / z0oro) )**2
! Calculate the Richardson number over the lowest 2 layers
kt = pver - 1
kb = pver
dv2 = max( ( u(i,kt) - u(i,kb) )**2 + ( v(i,kt) - v(i,kb) )**2, dv2min )
! Modification : Below computation of Ri is wrong. Note that 'Exner' function here is
! inverse exner function. Here, exner function is not multiplied in
! the denominator. Also, we should use moist Ri not dry Ri.
! Also, this approach using the two lowest model layers can be potentially
! sensitive to the vertical resolution.
! OK. I only modified the part associated with exner function.
ri = 2._r8 * gravit * ( t(i,kt) * exner(i,kt) - t(i,kb) * exner(i,kb) ) * ( zm(i,kt) - zm(i,kb) ) &
/ ( ( t(i,kt) * exner(i,kt) + t(i,kb) * exner(i,kb) ) * dv2 )
! ri = 2._r8 * gravit * ( t(i,kt) * exner(i,kt) - t(i,kb) * exner(i,kb) ) * ( zm(i,kt) - zm(i,kb) ) &
! / ( ( t(i,kt) + t(i,kb) ) * dv2 )
! Calculate the instability function and modify the neutral drag cofficient.
! We should probably follow more elegant approach like Louis et al (1982) or Bretherton and Park (2009)
! but for now we use very crude approach : just 1 for ri < 0, 0 for ri > 1, and linear ramping.
stabfri = max( 0._r8, min( 1._r8, 1._r8 - ri ) )
cd = cd * stabfri
! Compute density, velocity magnitude and stress using bottom level properties
rho = pmid(i,pver) / ( rair * t(i,pver) )
vmag = sqrt( u(i,pver)**2 + v(i,pver)**2 )
ksrf(i) = rho * cd * vmag * landfrac(i)
taux(i) = -ksrf(i) * u(i,pver)
tauy(i) = -ksrf(i) * v(i,pver)
end if
end do
return
end subroutine compute_tms
end module trb_mtn_stress