SUBROUTINE CIRA86(IDAY,SEC,GLAT,GLONG,STL,F107A,TINF,TLB,SIGMA) C******************************************************************* C Calculates neutral temperature parameters for IRI using the C MSIS-86/CIRA 1986 Neutral Thermosphere Model. The subroutines C GTS5, GLOBE5 and GLOBL5 developed by A.E. Hedin (2/26/87) were C modified for use in IRI --------- D. Bilitza -------- March 1991 C C INPUT: C IDAY - DAY OF YEAR C SEC - UT(SEC) C GLAT - GEODETIC LATITUDE(DEG) C GLONG - GEODETIC LONGITUDE(DEG) C STL - LOCAL APPARENT SOLAR TIME(HRS) C F107A - 3 MONTH AVERAGE OF F10.7 FLUX C C OUTPUT: C TINF - EXOSPHERIC TEMPERATURE (K) C TLB - TEMPERATURE AT LOWER BOUNDARY (K) C SIGMA - SHAPE PARAMETER FOR TEMPERATURE PROFILE C C ********************************************************************** DIMENSION PLG(9,4) DATA DR,DR2/1.72142E-2,0.0344284/,HR/.2618/,SR/7.2722E-5/, $ XL/1000./,TLL/1000./,DGTR/1.74533E-2/ C C CALCULATE LEGENDRE POLYNOMIALS C IF(XL.EQ.GLAT) GO TO 15 C = SIN(GLAT*DGTR) S = COS(GLAT*DGTR) C2 = C*C C4 = C2*C2 S2 = S*S PLG(2,1) = C PLG(3,1) = 0.5*(3.*C2 -1.) PLG(4,1) = 0.5*(5.*C*C2-3.*C) PLG(5,1) = (35.*C4 - 30.*C2 + 3.)/8. PLG(6,1) = (63.*C2*C2*C - 70.*C2*C + 15.*C)/8. PLG(2,2) = S PLG(3,2) = 3.*C*S PLG(4,2) = 1.5*(5.*C2-1.)*S PLG(5,2) = 2.5*(7.*C2*C-3.*C)*S PLG(6,2) = 1.875*(21.*C4 - 14.*C2 +1.)*S PLG(7,2) = (11.*C*PLG(6,2)-6.*PLG(5,2))/5. PLG(3,3) = 3.*S2 PLG(4,3) = 15.*S2*C PLG(5,3) = 7.5*(7.*C2 -1.)*S2 PLG(6,3) = 3.*C*PLG(5,3)-2.*PLG(4,3) PLG(4,4) = 15.*S2*S PLG(5,4) = 105.*S2*S*C PLG(6,4)=(9.*C*PLG(5,4)-7.*PLG(4,4))/2. PLG(7,4)=(11.*C*PLG(6,4)-8.*PLG(5,4))/3. XL=GLAT 15 CONTINUE IF(TLL.EQ.STL) GO TO 16 STLOC = SIN(HR*STL) CTLOC = COS(HR*STL) S2TLOC = SIN(2.*HR*STL) C2TLOC = COS(2.*HR*STL) S3TLOC = SIN(3.*HR*STL) C3TLOC = COS(3.*HR*STL) TLL = STL 16 CONTINUE C DFA=F107A-150. C C EXOSPHERIC TEMPERATURE C C F10.7 EFFECT T1 = ( 3.11701E-3 - 0.64111E-5 * DFA ) * DFA F1 = 1. + 0.426385E-2 * DFA F2 = 1. + 0.511819E-2 * DFA F3 = 1. + 0.292246E-2 * DFA C TIME INDEPENDENT T2 = 0.385528E-1 * PLG(3,1) + 0.303445E-2 * PLG(5,1) C SYMMETRICAL ANNUAL AND SEMIANNUAL CD14 = COS( DR * (IDAY+8.45398) ) CD18 = COS( DR2 * (IDAY-125.818) ) CD32 = COS( DR * (IDAY-30.0150) ) CD39 = COS( DR2 * (IDAY-2.75905) ) T3 = 0.805486E-2 * CD32 + 0.14237E-1 * CD18 C ASYMMETRICAL ANNUAL AND SEMIANNUAL T5 = F1 * (-0.127371 * PLG(2,1) - 0.302449E-1 * PLG(4,1) ) * CD14 & - 0.192645E-1 * PLG(2,1) * CD39 C DIURNAL T71 = 0.123512E-1 * PLG(3,2) * CD14 T72 = -0.526277E-2 * PLG(3,2) * CD14 T7 = ( -0.105531 *PLG(2,2) - 0.607134E-2 *PLG(4,2) + T71 ) *CTLOC 4 + ( -0.115622 *PLG(2,2) + 0.202240E-2 *PLG(4,2) + T72 ) *STLOC C SEMIDIURNAL T81 = 0.386578E-2 * PLG(4,3) * CD14 T82 = 0.389146E-2 * PLG(4,3) * CD14 T8= (-0.516278E-3 *PLG(3,3) - 0.117388E-2 *PLG(5,3) +T81)*C2TLOC 3 +( 0.990156E-2 *PLG(3,3) - 0.354589E-3 *PLG(5,3) +T82)*S2TLOC C TERDIURNAL Z1 = PLG(5,4) * CD14 Z2 = PLG(7,4) * CD14 T14=(0.147284E-2*PLG(4,4)-0.173933E-3*Z1+0.365016E-4*Z2)*S3TLOC 2 +(0.341345E-3*PLG(4,4)-0.153218E-3*Z1+0.115102E-3*Z2)*C3TLOC T7814 = F2 * ( T7 + T8 + T14 ) C LONGITUDINAL T11= F3 * (( 0.562606E-2 * PLG(3,2) + 0.594053E-2 * PLG(5,2) + $ 0.109358E-2 * PLG(7,2) - 0.301801E-2 * PLG(2,2) - $ 0.423564E-2 * PLG(4,2) - 0.248289E-2 * PLG(6,2) + $ (0.189689E-2 * PLG(2,2) + 0.415654E-2 * PLG(4,2)) * CD14 $ ) * COS(DGTR*GLONG) + $ ( -0.11654E-1 * PLG(3,2) - 0.449173E-2 * PLG(5,2) - $ 0.353189E-3 * PLG(7,2) + 0.919286E-3 * PLG(2,2) + $ 0.216372E-2 * PLG(4,2) + 0.863968E-3 * PLG(6,2) + $ (0.118068E-1 * PLG(2,2) + 0.331190E-2 * PLG(4,2)) * CD14 $ ) * SIN(DGTR*GLONG) ) C UT AND MIXED UT,LONGITUDE T12 = ( 1. - 0.565411 * PLG(2,1) ) * COS( SR*(SEC-31137.0) ) * $ (-0.13341E-1*PLG(2,1)-0.243409E-1*PLG(4,1)-0.135688E-1*PLG(6,1)) $ + ( 0.845583E-3 * PLG(4,3) + 0.538706E-3 * PLG(6,3) ) * $ COS( SR * (SEC-247.956) + 2.*DGTR*GLONG ) C Exospheric temperature TINF/K [Eq. A7] TINF = 1041.3 * ( 1. + T1+T2+T3+T5+T7814+T11+T12 ) * 0.99604 C C TEMPERATURE DERIVATIVE AT LOWER BOUNDARY C C F10.7 EFFECT T1 = 0.252317E-2 * DFA C TIME INDEPENDENT T2 = -0.467542E-1 * PLG(3,1) + 0.12026 * PLG(5,1) C ASYMMETRICAL ANNUAL CD14 = COS( DR * (IDAY+8.45398) ) T5 = -0.13324 * PLG(2,1) * CD14 C SEMIDIURNAL ZZ = PLG(4,3) * CD14 T81 = -0.973404E-2 * ZZ T82 = -0.718482E-3 * ZZ T8 =(0.191357E-1 *PLG(3,3) + 0.787683E-2 *PLG(5,3) + T81) *C2TLOC 3 + (0.125429E-2 *PLG(3,3) - 0.233698E-2 *PLG(5,3) + T82) *S2TLOC C dTn/dh at lower boundary [Eq. A6] G0 = 0.166728E2 * ( 1. + T1+T2+T5+T8 ) * 0.951363 C C NEUTRAL TEMPERATURE AT LOWER BOUNDARY 120KM C CD9 = COS( DR2 * (IDAY-89.3820) ) CD11 = COS( DR * (IDAY+8.45398) ) T1 = 0.568478E-3 * DFA T4 = 0.107674E-1 * CD9 T5 =-0.192414E-1 * PLG(2,1) * CD11 T7 = -0.2002E-1 *PLG(2,2) *CTLOC - 0.195833E-2 *PLG(2,2) *STLOC T8 = (-0.938391E-2 * PLG(3,3) - 0.260147E-2 * PLG(5,3) $ + 0.511651E-4 * PLG(6,3) * CD11 ) * C2TLOC $ + ( 0.131480E-1 * PLG(3,3) - 0.808556E-3 * PLG(5,3) $ + 0.255717E-2 * PLG(6,3) * CD11 ) * S2TLOC C Tn at lower boundary 120km [Eq. A8] TLB = 386.0 * ( 1. + T1+T4+T5+T7+T8 ) * 0.976619 C Sigma [Eq. A5] SIGMA = G0 / ( TINF - TLB ) RETURN END C C FUNCTION TN(H,TINF,TLBD,S) C-------------------------------------------------------------------- C Calculate Temperature for MSIS/CIRA-86 model C-------------------------------------------------------------------- ZG2 = ( H - 120. ) * 6476.77 / ( 6356.77 + H ) TN = TINF - TLBD * EXP ( - S * ZG2 ) RETURN END C C FUNCTION DTNDH(H,TINF,TLBD,S) C--------------------------------------------------------------------- ZG1 = 6356.77 + H ZG2 = 6476.77 / ZG1 ZG3 = ( H - 120. ) * ZG2 DTNDH = - TLBD * EXP ( - S * ZG3 ) * ( S / ZG1 * ( ZG3 - ZG2 ) ) RETURN END