SUBROUTINE SETWIN C ================= C C Initialisation of an extended radial structure C (spherical symmetry is assumed) C with a continuous connection between the lower quasi-hydrostatic C layers and the upper, supersonic layers. The velocity structure C in the upper layers is a beta-type law (v=vinf*(1-r0/r)^beta). C C Additional input are read at the end of Unit 8: C RCORE : Core radius (deepest layer, in solar radii or in cm) C NDRAD : Number of layers C NRCORE: Number of core rays C INRV : Switch indicating the data to be read: C = 0 : Read an hydrostatic, plane-parallel model only; the C routine builds the radial points, density and C velocity structure; C < 0 : Read also an hydrostatic, plane-parallel model, but C an empirical velocity law V(r) is read at each C radial point (r(id) is read); C > 0 : Input from an extended model atmosphere; the velocity C law is read; the density structure is recomputed for C a possibly different mass-loss rate. C XMDOT : Mass loss rate (in solar mass/yr) C BETAV, VINF : Parameters of the velocity law (VINF in km/s) C RD, VEL: Radial points, expansion velocity C C Synspec version C INCLUDE 'PARAMS.FOR' INCLUDE 'MODELP.FOR' INCLUDE 'WINCOM.FOR' PARAMETER (RSUN=6.96D10) common/velaux/velmax,iemoff,nltoff,itrad C C Read data for spherical atmosphere and velocity law C READ(8,*,END=9,ERR=9) RCORE,NDRAD,NRCORE,INRV,NFIRY,NDF IF(RCORE.LT.1.E5) RCORE=RCORE*RSUN IF(NDRAD.GT.MDEPTH) CALL quit('NDRAD too large') READ(8,*) XMDOT,BETAV,VINF XMDOT=6.30289D25*XMDOT VINF=1.D5*VINF ND=NDRAD DO ID=1,ND READ(8,*) RD(ID),VEL(ID),VTURB(ID),DENSCON(ID) if(denscon(id).eq.0.) denscon(id)=1. vturb(id)=vturb(id)*vturb(id) END DO C C Apply density contrast for clumping C DO ID=1,ND ELEC(ID) = ELEC(ID) * DENSCON(ID) DENS(ID) = DENS(ID) * DENSCON(ID) DO I=1,NLEVEL POPUL(I,ID) = POPUL(I,ID) * DENSCON(ID) END DO END DO C C Set up rays and weights C itrad=1 call radtem CALL SETRAY CALL WGTJH1 C 9 continue RETURN END