c ------------------------------------------------------------------ c --- matrix inversion subroutines for implicit solution of vertical c --- diffusion equation - tri-diagonal matrix c ------------------------------------------------------------------ c subroutine tridcof(diff,tri,nlayer,tcu,tcc,tcl) use mod_xc ! HYCOM communication interface use mod_cb_arrays ! HYCOM saved arrays implicit none c c --- compute coefficients for tridiagonal matrix (dimension=kdm). c --- Note: tcu(1) = 0. and tcl(kdm+1) = 0. are necessary conditions. c c --- input real diff(kdm+1) ! diffusivity profile on interfaces integer nlayer c c --- output real tcu(kdm), ! upper coeff. for (k-1) on k line of trid.matrix & tcc(kdm), ! central ... (k ) .. & tcl(kdm) ! lower ..... (k-1) .. c --- common tridiagonal factors real tri(kdm,0:1) ! dt/dz/dz factors in trid. matrix c c --- local integer k c c --- in the surface layer tcu(1)=0. tcc(1)=1.+tri(1,1)*diff(2) ! 1.+ delt1/h(1)/dzb(1)*diff(2) tcl(1)= -tri(1,1)*diff(2) ! - delt1/h(1)/dzb(1)*diff(2) c c --- inside the domain do 10 k=2,nlayer tcu(k)= -tri(k,0)*diff(k ) tcc(k)=1.+tri(k,1)*diff(k+1)+tri(k,0)*diff(k) tcl(k)= -tri(k,1)*diff(k+1) 10 continue c c --- in the bottom layer tcl(nlayer)= 0. return end *********************************************************************** subroutine tridrhs(h,yo,diff,ghat,ghatflux,tri,nlayer,rhs) use mod_xc ! HYCOM communication interface use mod_cb_arrays ! HYCOM saved arrays implicit none c c --- compute right hand side of tridiagonal matrix for scalar fields: c --- = yo (old field) c --- + flux-divergence of ghat c --- + flux-divergence of non-turbulant fluxes c c --- note: if surface and bottom fluxes are nonzero, the following must apply c --- sfc. lyr. needs +delt1/h(1)*surfaceflux c --- bot. lyr. needs +delt1/h(nlayer)*diff(nlayer+1)/ c --- dzb(nlayer)*yo(nlayer+1) c c --- input real h(kdm), ! layer thickness & yo(kdm+1), ! old profile & diff(kdm+1), ! diffusivity profile on interfaces & ghat(kdm+1), ! ghat turbulent flux & ghatflux ! surface flux for ghat: includes solar flux integer nlayer c c --- output real rhs(kdm) ! right hand side c real tri(kdm,0:1) ! dt/dz/dz factors in trid. matrix c c --- local integer k c c --- in the top layer rhs(1)=yo(1)+delt1/h(1)*(ghatflux*diff(2)*ghat(2)) c c --- inside the domain do 10 k=2,nlayer-1 rhs(k)=yo(k)+delt1/h(k)* & (ghatflux*(diff(k+1)*ghat(k+1)-diff(k)*ghat(k))) 10 continue c c --- in the bottom layer k=nlayer rhs(k)=yo(k)+delt1/h(k)* & (ghatflux*(diff(k+1)*ghat(k+1)-diff(k)*ghat(k))) c return end *********************************************************************** subroutine tridmat(tcu,tcc,tcl,nlayer,h,rhs,yo,yn,diff, i,j) use mod_xc ! HYCOM communication interface use mod_cb_arrays ! HYCOM saved arrays implicit none c c --- solve tridiagonal matrix for new vector yn, given right hand side c --- vector rhs. c c --- note: if surface and bottom fluxes are nonzero, the following must apply c --- surface layer needs +delt1*surfaceflux/(h(1)*bet) c --- bottom layer needs +tri(nlayer,1)*diff(nlayer+1)*yo(nlayer+1))/bet c c --- input real tcu (kdm), ! upper coeff. for (k-1) on k line of tridmatrix & tcc (kdm), ! central ... (k ) .. & tcl (kdm), ! lower ..... (k-1) .. & h (kdm), ! layer thickness & rhs(kdm), ! right hand side & yo(kdm+1), ! old field & diff(kdm+1), ! diffusivity profile & gam(kdm) ! temporary array for tridiagonal solver real bet ! ... integer nlayer, ! number of active layers <=kdm & i,j ! local grid point c c --- output real yn(kdm+1) ! new field c c --- local integer k c c --- solve tridiagonal matrix. bet=tcc(1) yn(1)=rhs(1)/bet ! surface do 21 k=2,nlayer gam(k)=tcl(k-1)/bet bet=tcc(k)-tcu(k)*gam(k) if(bet.eq.0.) then write(lp,*) write(lp,*) '** algorithm for solving tridiagonal matrix fails' write(lp,*) '** i,j=',i0+i,j0+j !global grid point write(lp,*) '** bet=',bet write(lp,*) '** k=',k,' tcc=',tcc(k),' tcu=',tcu(k), & ' gam=',gam(k) call flush(lp) call xchalt('(tridmat)') stop '(tridmat)' * bet=1.E-12 endif yn(k) = (rhs(k) - tcu(k) *yn(k-1) )/bet c to avoid "Underflow" at single precision on the sun c yni = (rhs(k) - tcu(k) *yn(k-1) )/bet c if(yni.lt.0.) then c yn(k) =min( (rhs(k) - tcu(k) *yn(k-1) )/bet ,-1.E-12 ) c else c yn(k) = max( (rhs(k) - tcu(k) *yn(k-1) )/bet , 1.E-12 ) c endif 21 continue c do 22 k=nlayer-1,1,-1 yn(k)=yn(k)-gam(k+1)*yn(k+1) 22 continue c yn(nlayer+1)=yo(nlayer+1) c return end