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precip_fall.f90
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precip_fall.f90
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subroutine precip_fall(qp, term_vel, hydro_type, omega, ind)
! positively definite monotonic advection with non-oscillatory option
! and gravitational sedimentation
use vars
use params
use microphysics, only: qtot_sed, qice_sed, prec_accum, prec_ice_accum
implicit none
real qp(dimx1_s:dimx2_s, dimy1_s:dimy2_s, nzm) ! falling hydrometeor
integer hydro_type ! 0 - all liquid, 1 - all ice, 2 - mixed
real omega(nx,ny,nzm) ! = 1: liquid, = 0: ice; = 0-1: mixed : used only when hydro_type=2
integer ind
! Terminal velocity fnction
real, external :: term_vel ! terminal velocity function
! Local:
real mx(nzm),mn(nzm), lfac(nz)
real www(nz),fz(nz)
real df(dimx1_s:dimx2_s, dimy1_s:dimy2_s, nzm)
real f0(nzm),df0(nzm)
real eps
integer i,j,k,kc,kb
logical nonos
real y,pp,pn
pp(y)= max(0.,y)
pn(y)=-min(0.,y)
real lat_heat, wmax
real wp(nzm), tmp_qp(nzm), irhoadz(nzm), iwmax(nzm), rhofac(nzm), prec_cfl
integer nprec, iprec
real flagstat
!bloss: used to compute individual tendency for ice sedimentation for energy budget terms.
real :: ice_frac(1:nz)
!--------------------------------------------------------
call t_startf ('precip_fall')
eps = 1.e-10
nonos = .true.
do k = 1,nzm
rhofac(k) = sqrt(1.29/rho(k))
irhoadz(k) = 1./(rho(k)*adz(k)) ! Useful factor
kb = max(1,k-1)
wmax = dz*adz(kb)/dtn ! Velocity equivalent to a cfl of 1.0.
iwmax(k) = 1./wmax
end do
! Add sedimentation of precipitation field to the vert. vel.
do j=1,ny
do i=1,nx
! Compute precipitation velocity and flux column-by-column
prec_cfl = 0.
do k=1,nzm
select case (hydro_type)
case(0)
lfac(k) = fac_cond
flagstat = 1.
case(1)
lfac(k) = fac_sub
flagstat = 1.
case(2)
lfac(k) = fac_cond + (1-omega(i,j,k))*fac_fus
flagstat = 1.
case(3)
lfac(k) = 0.
flagstat = 0.
case default
if(masterproc) then
print*, 'unknown hydro_type in precip_fall. exitting ...'
call task_abort
end if
end select
wp(k)=rhofac(k)*term_vel(i,j,k,ind)
prec_cfl = max(prec_cfl,wp(k)*iwmax(k)) ! Keep column maximum CFL
wp(k) = -wp(k)*rhow(k)*dtn/dz
end do ! k
fz(nz)=0.
www(nz)=0.
lfac(nz)=0
! If maximum CFL due to precipitation velocity is greater than 0.9,
! take more than one advection step to maintain stability.
if (prec_cfl.gt.0.9) then
nprec = CEILING(prec_cfl/0.9)
do k = 1,nzm
! wp already includes factor of dt, so reduce it by a
! factor equal to the number of precipitation steps.
wp(k) = wp(k)/float(nprec)
end do
else
nprec = 1
end if
do iprec = 1,nprec
do k = 1,nzm
tmp_qp(k) = qp(i,j,k) ! Temporary array for qp in this column
end do
!-----------------------------------------
if(nonos) then
do k=1,nzm
kc=min(nzm,k+1)
kb=max(1,k-1)
mx(k)=max(tmp_qp(kb),tmp_qp(kc),tmp_qp(k))
mn(k)=min(tmp_qp(kb),tmp_qp(kc),tmp_qp(k))
end do
end if ! nonos
! loop over iterations
do k=1,nzm
! Define upwind precipitation flux
fz(k)=tmp_qp(k)*wp(k)
end do
do k=1,nzm
kc=k+1
tmp_qp(k)=tmp_qp(k)-(fz(kc)-fz(k))*irhoadz(k) !Update temporary qp
end do
do k=1,nzm
! Also, compute anti-diffusive correction to previous
! (upwind) approximation to the flux
kb=max(1,k-1)
! The precipitation velocity is a cell-centered quantity,
! since it is computed from the cell-centered
! precipitation mass fraction. Therefore, a reformulated
! anti-diffusive flux is used here which accounts for
! this and results in reduced numerical diffusion.
www(k) = 0.5*(1.+wp(k)*irhoadz(k)) &
*(tmp_qp(kb)*wp(kb) - tmp_qp(k)*wp(k)) ! works for wp(k)<0
end do
!---------- non-osscilatory option ---------------
if(nonos) then
do k=1,nzm
kc=min(nzm,k+1)
kb=max(1,k-1)
mx(k)=max(tmp_qp(kb),tmp_qp(kc),tmp_qp(k),mx(k))
mn(k)=min(tmp_qp(kb),tmp_qp(kc),tmp_qp(k),mn(k))
end do
do k=1,nzm
kc=min(nzm,k+1)
mx(k)=rho(k)*adz(k)*(mx(k)-tmp_qp(k))/(pn(www(kc)) + pp(www(k))+eps)
mn(k)=rho(k)*adz(k)*(tmp_qp(k)-mn(k))/(pp(www(kc)) + pn(www(k))+eps)
end do
do k=1,nzm
kb=max(1,k-1)
! Add limited flux correction to fz(k).
fz(k) = fz(k) & ! Upwind flux
+ pp(www(k))*min(1.,mx(k), mn(kb)) &
- pn(www(k))*min(1.,mx(kb),mn(k)) ! Anti-diffusive flux
end do
endif ! nonos
! Update precipitation mass fraction and liquid-ice static
! energy using precipitation fluxes computed in this column.
do k=1,nzm
kc=k+1
! Update precipitation mass fraction.
! Note that fz is the total flux, including both the
! upwind flux and the anti-diffusive correction.
qp(i,j,k)=qp(i,j,k)-(fz(kc)-fz(k))*irhoadz(k)
qpfall(k)=qpfall(k)-(fz(kc)-fz(k))*irhoadz(k)*flagstat ! For qp budget
lat_heat = -(lfac(kc)*fz(kc)-lfac(k)*fz(k))*irhoadz(k)
t(i,j,k)=t(i,j,k)-lat_heat
tlat(k)=tlat(k)-lat_heat ! For energy budget
precflux(k) = precflux(k) - fz(k)*flagstat ! For statistics
end do
precsfc(i,j) = precsfc(i,j) - fz(1)*flagstat ! For statistics
prec_xy(i,j) = prec_xy(i,j) - fz(1)*flagstat ! For 2D output
if(do_chunked_energy_budgets.AND.(flagstat.gt.0)) then
!bloss: accumulate sedimentation tendencies for total water and for ice
! so that they can be included in energy budgets
qtot_sed(i,j,:) = qtot_sed(i,j,:) - irhoadz(1:nzm)*( fz(2:nz)-fz(1:nzm) )
ice_frac(1:nz) = MAX(0., MIN(1., (lfac(1:nz) - fac_cond)/fac_fus ) )
qice_sed(i,j,:) = qice_sed(i,j,:) &
- irhoadz(1:nzm)*( ice_frac(2:nz)*fz(2:nz) - ice_frac(1:nzm)*fz(1:nzm) )
prec_accum(i,j) = prec_accum(i,j) - fz(1)
prec_ice_accum(i,j) = prec_ice_accum(i,j) - ice_frac(1)*fz(1)
end if
if (iprec.lt.nprec) then
! Re-compute precipitation velocity using new value of qp.
do k=1,nzm
wp(k) = rhofac(k)*term_vel(i,j,k,ind)
! Decrease precipitation velocity by factor of nprec
wp(k) = -wp(k)*rhow(k)*dtn/dz/float(nprec)
! Note: Don't bother checking CFL condition at each
! substep since it's unlikely that the CFL will
! increase very much between substeps when using
! monotonic advection schemes.
end do
fz(nz)=0.
www(nz)=0.
lfac(nz)=0.
end if
end do !iprec
end do
end do
call t_stopf ('precip_fall')
end subroutine precip_fall