! source file: /raid23/csomes/UVic/2.9/c_n_isotopes/last_glacial_experiments/dlgsd6p15/updates/vmixc.F subroutine vmixc (joff, js, je, is, ie) !======================================================================= ! 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, k1 real zn2, hab, zkappa, qk1, qo1, edr, q2 include "size.h" include "param.h" include "pconst.h" include "stdunits.h" include "coord.h" include "mw.h" include "switch.h" include "vmixc.h" include "isopyc.h" include "tidal_kv.h" include "diag.h" include "grdvar.h" include "levind.h" include "timeavgs.h" !----------------------------------------------------------------------- ! 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 !----------------------------------------------------------------------- ! constant vertical mixing coefficients !----------------------------------------------------------------------- do j=jstrt,jend jrow = j + joff do i=istrt,iend if (abs(tlat(i,jrow)) .lt. 30.) then qk1 = 0.33 qo1 = 0.33 else qk1 = 1. qo1 = 1. endif if (abs(tlat(i,jrow)) .lt. 70.) then q2 = 0.33 else q2 = 1. endif c q2=0.5 do k=1,kmt(i,jrow)-1 visc_cbu(i,k,j) = kappa_m ! 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 = max(-gravrho0r*drodzb(i,k,j,0),1e-8) ! subgrid-scale scheme: sum over all levels below k edr = 0. do k1=k+1,kmt(i,jrow) ! height above bottom hab = zw(k) - zw(k1) edr = edr + (q2*(edrm2(i,k1,jrow)+edrs2(i,k1,jrow)) & + qk1*edrk1(i,k1,jrow) + qo1*edro1(i,k1,jrow)) & *exp(hab*zetar)/(1-exp(-zetar*zw(k1))) enddo zkappa = ogamma*edr/ZN2 ! Andreas: high mixing in Southern Ocean below 500 m as in observations zkappa = max(zkappa, & (1-tanh((tlat(i,j+joff)+20)/3))/13.4) zkappa = max(zkappa,tanh((zw(k)-50000.)/10000)* & (1-tanh((tlat(i,j+joff)-20)/3))/13.4) zkappa = max(zkappa, & (1-(1-tanh((tlat(i,j+joff)-20)/3))/2)/6.7) zkappa = max(zkappa, tanh((zw(k)-50000.)/10000)* & (1-(1-tanh((tlat(i,j+joff)+20)/3))/2)/6.7) ! limit diff_cbt diff_cbt(i,k,j) = max(kappa_h, min(100., zkappa + kappa_h)) if (k .le. 2) then diff_cbt(i,k,j) = max(kappa_h*2. & , min(100., zkappa + kappa_h)) else diff_cbt(i,k,j) = max(kappa_h, min(100. & , zkappa + kappa_h)) endif c & .and.(tlat(i,j).le.25)) then c diff_cbt(i,k,j) = max(kappa_h/2. c &, min(100., zkappa + kappa_h/2.)) c else c diff_cbt(i,k,j) = max(kappa_h, min(100. c &, zkappa + kappa_h)) c endif enddo enddo enddo !----------------------------------------------------------------------- ! 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 !----------------------------------------------------------------------- ! 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 return end