!copyright (C) 2001 MSC-RPN COMM %%%RPNPHY%%% *** S/P LACS #include "phy_macros_f.h"![]()
SUBROUTINE LACS (F, FSIZ, NI) 2 #include "impnone.cdk"
* integer fsiz, ni real f(fsiz) * *Author * Bernard Bilodeau (June 2001) - From lacs.cdk * *Revisions * 001 B. Dugas (Jul 03) - Introduce CRITLAC * *Object * define sea ice fraction and thickness over lakes * *Arguments * - Input/Output - * F permanent bus of the physics variables * * - Input - * FSIZ dimension of F * NI horizontal length * *Implicites * #include "surfacepar.cdk"
#include "phybus.cdk"
#include "consphy.cdk"
#include "leads.cdk"
* *** * integer i * *VDIR NODEP DO i=0,ni-1 * * Array ML is the fraction of lakes. * IF (f(ml+i).lt.critlac) then ! Not over lakes * * Leadfrac is the climatological value of % of leads in * MARINE ice. The ice-covered lakes remain untouched. * GLSEA0 contains the original value of the sea-ice * analysis (updated if needed with daily increments * if switch "CLIMAT" is true in subroutine CLIMPHS). * f(glsea +i ) = f(glsea +i) * + (1. - leadfrac) * * Set minimal ice depth if zero ice thickness in * analysis (or climatology) while ice fraction is non zero if (f(glsea+i).ge.0..and.f(icedp+i).le.0.) then f(icedp+i) = max(minicedp, 0.25 * f(glsea+i)) endif * ELSE ! Over lakes * * Water temperature of ice-covered lakes is 0 C. if (f(glsea+i) .gt. 10.*critmask) f(twater+i) = TRPL * * Over lakes, ice thickness is set to a minimum of 30 cm * if GL > 50%. GL is then changed to 100% since the lakes * are usually fully frozen. Otherwise, linear interpolation * of ice thickness (varying between 0 and 30 cm) is performed * when GL ranges from 0 to 50%. * IF (f(glsea+i).gt.0.50) then f(icedp +i ) = 0.30 f(glsea +i ) = 1.00 ELSE f(icedp +i ) = 0.60 * f(glsea+i) END IF * END IF * END DO * RETURN END