!-------------------------------------- LICENCE BEGIN ------------------------------------ !Environment Canada - Atmospheric Science and Technology License/Disclaimer, ! version 3; Last Modified: May 7, 2008. !This is free but copyrighted software; you can use/redistribute/modify it under the terms !of the Environment Canada - Atmospheric Science and Technology License/Disclaimer !version 3 or (at your option) any later version that should be found at: !http://collaboration.cmc.ec.gc.ca/science/rpn.comm/license.html ! !This software is distributed in the hope that it will be useful, but WITHOUT ANY WARRANTY; !without even the implied warranty of MERCHANTABILITY or FITNESS FOR A PARTICULAR PURPOSE. !See the above mentioned License/Disclaimer for more details. !You should have received a copy of the License/Disclaimer along with this software; !if not, you can write to: EC-RPN COMM Group, 2121 TransCanada, suite 500, Dorval (Quebec), !CANADA, H9P 1J3; or send e-mail to service.rpn@ec.gc.ca !-------------------------------------- LICENCE END -------------------------------------- ***S/P LIN_DIFF_VERT1 * #include "phy_macros_f.h"![]()
SUBROUTINE LIN_DIFF_VERTTQ1 (TU, U, KU, GU, ALFA, BETA, S, SK, 2,2 % TAU, F, A, B, C, D, N, NK) * #include "impnone.cdk"
INTEGER N, NK REAL TU(N, NK), U(N, NK), KU(N, NK), GU(N, NK) REAL ALFA(N), BETA(N), S(N,NK), SK(N,NK), TAU, F REAL A(N, NK), B(N, NK), C(N, NK), D(N, NK) * *Author * L. Spacek (Jun 2008) * *Object * to solve a TLM vertical diffusion equation by finite * differences on thermo levels * *Arguments * * - Output - * TU U tendency (D/DT U) due to the vertical diffusion and to * term R * * - Input - * U variable to diffuse (U,V,T,Q,E) * KU diffusion coefficient * GU optional countergradient term * ALFA inhomogeneous term for the surface flux * BETA homogeneous term for the surface flux * S sigma coordinates of full levels * SK sigma coordinates of diffusion coefficient levels * TAU length of timestep * F waiting factor for time 'N+1' * A work space (N,NK) * B work space (N,NK) * C work space (N,NK) * D work space (N,NK) * N number of columns to process * NK vertical dimension * *Notes * D/DT U = D(U) * D(U) = D/DS J(U) * J(U) = KU*(D/DS U + GU) * ** * INTEGER I, K REAL SC, SCTU, ST, SB, HM, HP, HD, KUM, KUP, SCK1 EXTERNAL LIN_DIFUVD1, LIN_DIFUVD2 * * ************************************************************************ * AUTOMATIC ARRAYS ************************************************************************ * AUTOMATIC (VHM ,REAL ,(N,NK) ) AUTOMATIC (VHP ,REAL ,(N,NK) ) AUTOMATIC (RHD ,REAL*8 ,(N,NK) ) AUTOMATIC (RHMD ,REAL*8 ,(N,NK) ) AUTOMATIC (RHPD ,REAL*8 ,(N,NK) ) * ST(i)=S(i,1)-0.5*(S(i,2)-S(i,1)) SB(i)=1. * SC = 1.0 SCTU = 0 SCK1 = 1 * * (1) CONSTRUIRE L'OPERATEUR TRIDIAGONAL DE DIFFUSION N=(A,B,C) * ET LE TERME CONTRE-GRADIENT (DANS D) * * K=1 * HM=0 DO I=1,N HM=SK(i,1)-ST(i) HP=SK(i,2)-SK(i,1) HD=S(i,2)-S(i,1) KUM=0 KUP=0.5*(KU(I,1)+KU(I,2)) A(I,1)=KUM/(HM*HD) C(I,1)=KUP/(HP*HD) B(I,1)=-A(I,1)-C(I,1) D(I,1)=(KUP*(GU(I,1)+GU(I,2))-KUM*GU(I,1))/(2*HD) ENDDO * * K=2...NK-1 * DO K=2,NK-1,1 DO I=1,N VHM(I,K)=SK(I,K)-SK(I,K-1) VHP(I,K)=SK(I,K+1)-SK(I,K) HD=S(I,K+1)-S(I,K) RHD(I,K)=HD RHMD(I,K)=VHM(I,K)*HD RHPD(I,K)=VHP(I,K)*HD ENDDO ENDDO CALL VREC( RHD(1,2), RHD(1,2),N*(NK-2)) CALL VREC(RHMD(1,2),RHMD(1,2),N*(NK-2)) CALL VREC(RHPD(1,2),RHPD(1,2),N*(NK-2)) DO K=2,NK-1,1 DO I=1,N KUM=0.5*(KU(I,K-1)+KU(I,K)) KUP=0.5*(KU(I,K+1)+KU(I,K)) A(I,K)=KUM*RHMD(I,K) C(I,K)=KUP*RHPD(I,K) B(I,K)=-A(I,K)-C(I,K) D(I,K)=.5*(KUP*(GU(I,K)+GU(I,K+1)) % -KUM*(GU(I,K-1)+GU(I,K)))*RHD(I,K) ENDDO ENDDO * * K=NK * HP=0 DO I=1,N HM=SK(i,NK)-SK(i,NK-1) HD=SB(i)-S(i,NK) KUM=0.5*(KU(I,NK)+KU(I,NK-1)) KUP=0 A(I,NK)=KUM/(HM*HD) C(I,NK)=0 B(I,NK)=-A(I,NK)-C(I,NK) D(I,NK)=(0-KUM*(GU(I,NK)+GU(I,NK-1)))/(2*HD) ENDDO * * * (2) CALCULER LE COTE DROIT D=TAU*(SC*N(U)+R+D/DS(KU*GU)) * CALL LIN_DIFUVD1
(D, SC, A, B, C, U, D, N, NK) DO K=1,NK DO I=1,N D(I,K) = TAU*D(I,K) ENDDO ENDDO * * (3) CALCULER OPERATEUR DU COTE GAUCHE * DO K=1,NK DO I=1,N A(I,K)= -SC*TAU*A(I,K) B(I,K)=1.-SC*TAU*B(I,K) C(I,K)= -SC*TAU*C(I,K) ENDDO ENDDO * * (4) AJOUTER TERME DE FLUX DE SURFACE POUR TYPE='U'/'UT' * DO I=1,N HD=SB(I)-S(I,NK) B(I,NK)=B(I,NK)-F*TAU*BETA(I)/HD D(I,NK)=D(I,NK)+(ALFA(I)+BETA(I)*U(I,NK))*TAU/HD ENDDO * * * (5) RESOUDRE SYSTEME TRIDIAGONAL [A,B,C] X = D. METTRE X DANS TU. * CALL LIN_DIFUVD2
(TU, A, B, C, D, D, N, NK) * * (6) OBTENIR TENDANCE * DO K=1,NK DO I=1,N TU(I,K) = TU(I,K)/TAU ENDDO ENDDO * RETURN END