subroutine vmixc (joff, js, je, is, ie) #if defined O_mom !======================================================================= ! set viscosity coefficient on bottom face of "u" cells ! set diffusion coefficient on bottom face of "t" cells ! input: ! joff = offset relating "j" in the MW to latitude "jrow" ! js = starting row in the MW ! je = ending row in the MW ! is = starting longitude index in the MW ! ie = ending longitude index in the MW !======================================================================= implicit none integer i, k, j, ip, kr, jq, js, je, istrt, is, iend, ie, jstrt integer jend, jrow, joff, ks real zn2, hab, zkappa include "size.h" include "param.h" include "pconst.h" include "stdunits.h" include "coord.h" include "mw.h" include "switch.h" include "vmixc.h" # if defined O_isopycmix || defined O_redi_diffusion include "isopyc.h" # if defined O_tidal_kv include "tidal_kv.h" include "diag.h" include "grdvar.h" include "levind.h" # endif # if defined O_save_kv include "timeavgs.h" # endif # endif # if defined O_constvmix && defined O_implicitvmix real temp(imt,km,jsmw:jmw) # endif !----------------------------------------------------------------------- ! bail out if starting row exceeds ending row !----------------------------------------------------------------------- if (js .gt. je) return !----------------------------------------------------------------------- ! limit the longitude and latitude indices !----------------------------------------------------------------------- istrt = max(2,is) iend = min(imt-1,ie) jstrt = max(2,js-1) jend = je-1 # if defined O_constvmix !----------------------------------------------------------------------- ! constant vertical mixing coefficients !----------------------------------------------------------------------- do j=jstrt,jend jrow = j + joff do i=istrt,iend do k=1,km visc_cbu(i,k,j) = kappa_m # if defined O_tidal_kv && defined O_isopycmix ! calculate N^2 = -g/rho drhodz on bottom of cell face ! (where K33 and diff_cbt = kappa_h are defined). Note that ! N2 is not guaranteed to be positive. If instability occurs, ! convective adjustment will eliminate it. ! drodzb is defined in isopyc.h ! ZN2 is defined on T-cell bottom (zw pt) ZN2 = -gravrho0r*drodzb(i,k,j,0) ! height above bottom if (kmt(i,jrow) .ne. 0.0) then hab = zw(k) - zw(kmt(i,jrow) - 1) else hab = 0.0 endif if (Zn2 .ne. 0.0) then zkappa = 0.33*ogamma*edr(i,jrow)*exp(hab*zetar)/ & (ZN2*(1-exp(-zetar*zw(kmt(i,jrow))))) else zkappa = 0.0 endif # if defined O_highmix_Southern_Ocean & !defined O_highmix_Southern_Ocean_tuned ! The following is A. Oschlies UVic 2.8 code if (tlat(i,j+joff) .lt. -40.) zkappa = max(zkappa,1.00) cao below is the old code used in "my" standard version and in Schmittner et al. (2009). a.o., 27.12.10 ! if (tlat(i,j+joff) .lt. -40. .and. ! & zw(kmt(i,j+joff)).gt.50000.) zkappa = max(zkappa,1.00) ! print*, "zkappa = ", zkappa # elseif defined O_highmix_Southern_Ocean_tuned & defined O_highmix_Southern_Ocean ! Below is an updated version of this from A. Schmittner that smooths this mixing below 500m if (tlat(i,j+joff) .lt. -40.) zkappa = max(zkappa,tanh & ((zw(k)-50000.)/10000)* & (1-tanh((tlat(i,j+joff)+40)/8))/2) # endif ! limit diff_cbt # if defined O_bryan_lewis_vertical diff_cbt(i,k,j) = max(Ahv(k), min(10., zkappa + Ahv(k))) # else diff_cbt(i,k,j) = max(kappa_h, min(10., zkappa + kappa_h)) # endif # elif defined O_bryan_lewis_vertical diff_cbt(i,k,j) = Ahv(k) # else diff_cbt(i,k,j) = kappa_h # endif enddo enddo enddo # if defined O_implicitvmix do ks=1,2 ! find density call statec (t(1,1,1,1,taum1), t(1,1,1,2,taum1), temp(1,1,jsmw) &, jstrt, jend, istrt, iend, ks) ! set large diffusion coefficient between unstable layers ! (note: viscosity coefficient is not limited but could be here) do j=jstrt,jend do k=ks,kmm1,2 do i=istrt,iend if (temp(i,k,j) .gt. temp(i,k+1,j)) then diff_cbt(i,k,j) = diff_cbt_limit*tmask(i,k+1,j) endif enddo enddo enddo enddo # endif # endif # if defined O_ppvmix !----------------------------------------------------------------------- ! for momentum and tracers based on the pacanowski & philander ! richardson mixing scheme (JPO vol 11, # 11, 1981). !----------------------------------------------------------------------- call ppmix (joff, js, je, istrt, iend) # endif # if defined O_isopycmix || defined O_redi_diffusion # if defined O_save_kv !----------------------------------------------------------------------- ! accumulate time average diapycnal (without K33) diffusivity !----------------------------------------------------------------------- if (timavgperts .and. .not. euler2) then do j=jstrt,jend jrow = j + joff do k=1,km do i=istrt,iend ta_diff_cbt(i,k,jrow) = ta_diff_cbt(i,k,jrow) & + diff_cbt(i,k,j) enddo enddo enddo endif # endif !----------------------------------------------------------------------- ! Add K33 component to vertical diffusion coefficient !----------------------------------------------------------------------- do j=jstrt,jend do i=istrt,iend do k=1,km diff_cbt(i,k,j) = diff_cbt(i,k,j) + K33(i,k,j) enddo enddo enddo # endif #endif return end