[1442] | 1 | SUBROUTINE SW_venus_dc_1Dglobave(PRMU0, PFRAC, |
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| 2 | S PPB, pt, |
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| 3 | S PHEAT, |
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| 4 | S PTOPSW,PSOLSW,ZFSNET) |
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| 5 | |
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| 6 | use dimphy |
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[1621] | 7 | use cpdet_phy_mod, only: cpdet |
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[1442] | 8 | IMPLICIT none |
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| 9 | |
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| 10 | #include "YOMCST.h" |
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| 11 | C |
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| 12 | C ------------------------------------------------------------------ |
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| 13 | C |
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| 14 | C PURPOSE. |
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| 15 | C -------- |
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| 16 | C |
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| 17 | c this routine loads and interpolates the shortwave radiation |
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| 18 | c fluxes taken from Dave Crisp calculations for Venus. |
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| 19 | c Ref: Crisp 1986. |
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| 20 | C |
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| 21 | C AUTHOR. |
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| 22 | C ------- |
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| 23 | C Sebastien Lebonnois |
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| 24 | C |
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| 25 | C MODIFICATIONS. |
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| 26 | C -------------- |
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| 27 | C ORIGINAL : 27/07/2005 |
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| 28 | c L.Salmi : june 2013 astuce to reduce the excess of NIR |
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| 29 | c in the transition region LTE/LTE |
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| 30 | c |
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| 31 | c G.Gilli : feb 2014 |
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| 32 | C ------------------------------------------------------------------ |
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| 33 | C |
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| 34 | C* ARGUMENTS: |
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| 35 | C |
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| 36 | c inputs |
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| 37 | |
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| 38 | REAL PRMU0 ! COSINE OF ZENITHAL ANGLE |
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| 39 | REAL PFRAC ! fraction de la journee |
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| 40 | REAL PPB(klev+1) ! inter-couches PRESSURE (bar) |
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| 41 | REAL pt(klev) ! mid-layer temperature |
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| 42 | C |
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| 43 | c output |
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| 44 | |
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| 45 | REAL PHEAT(klev) ! SHORTWAVE HEATING (K/s) within each layer |
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| 46 | REAL PTOPSW ! SHORTWAVE FLUX AT T.O.A. (net) |
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| 47 | REAL PSOLSW ! SHORTWAVE FLUX AT SURFACE (net) |
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| 48 | REAL ZFSNET(klev+1) ! net solar flux at ppb levels |
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| 49 | |
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| 50 | C |
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| 51 | C* LOCAL VARIABLES: |
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| 52 | C |
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| 53 | integer nldc,nszadc |
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| 54 | parameter (nldc=49) ! fichiers Crisp |
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| 55 | parameter (nszadc=8) ! fichiers Crisp |
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| 56 | |
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| 57 | integer i,j,nsza,nsza0,nl0 |
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| 58 | real solarrate ! solar heating rate (K/earthday) |
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| 59 | real zsnet(nldc+1,nszadc) ! net solar flux (W/m**2) (+ vers bas) |
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| 60 | real zsdn,zsup ! downward/upward solar flux (W/m**2) |
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| 61 | real solza(nszadc) ! solar zenith angles in table |
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| 62 | real presdc(nldc+1) ! pressure levels in table (bar) |
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| 63 | real tempdc(nldc+1) ! temperature in table (K) |
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| 64 | real altdc(nldc+1) ! altitude in table (km) |
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| 65 | real coolrate ! IR heating rate (K/earthday) ? |
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| 66 | real totalrate ! total rate (K/earthday) |
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| 67 | real zldn ! downward IR flux (W/m**2) ? |
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| 68 | real zlup ! upward IR flux (W/m**2) ? |
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| 69 | real zsolnet(nldc+1) ! for testing mean net solar flux in DC |
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| 70 | character*22 nullchar |
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| 71 | real deltasza |
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| 72 | real sza0,factflux |
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| 73 | logical firstcall |
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| 74 | data firstcall/.true./ |
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| 75 | save solza,zsnet,presdc,tempdc,altdc,zsolnet |
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| 76 | save firstcall |
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| 77 | |
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| 78 | c ------------------------ |
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| 79 | c Loading the file |
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| 80 | c ------------------------ |
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| 81 | |
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| 82 | if (firstcall) then |
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| 83 | |
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| 84 | open(11,file='dataDCrisp.dat') |
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| 85 | read(11,*) nullchar |
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| 86 | |
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| 87 | do nsza=1,nszadc |
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| 88 | read(11,*) nullchar |
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| 89 | read(11,*) nullchar |
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| 90 | read(11,*) nullchar |
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| 91 | read(11,'(22x,F11.5)') solza(nsza) |
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| 92 | read(11,*) nullchar |
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| 93 | read(11,*) nullchar |
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| 94 | read(11,*) nullchar |
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| 95 | read(11,'(3(2x,F10.4),36x,4(2x,F11.5))') |
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| 96 | . presdc(nldc+1),tempdc(nldc+1), altdc(nldc+1), |
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| 97 | . zsdn,zsup,zldn,zlup |
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| 98 | zsnet(nldc+1,nsza)=zsdn-zsup |
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| 99 | do i=1,nldc |
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| 100 | j = nldc+1-i ! changing: vectors from surface to top |
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| 101 | read(11,'(6(2x,F10.4),4(2x,F11.5))') |
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| 102 | . presdc(j),tempdc(j),altdc(j), |
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| 103 | . solarrate,coolrate,totalrate, |
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| 104 | . zsdn,zsup,zldn,zlup |
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| 105 | zsnet(j,nsza)=zsdn-zsup |
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| 106 | enddo |
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| 107 | enddo |
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| 108 | |
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| 109 | close(11) |
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| 110 | |
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| 111 | c ----------- TEST ------------ |
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| 112 | c Moyenne planetaire |
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| 113 | c ----------------------------- |
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| 114 | |
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| 115 | deltasza=(solza(2)-solza(1))*RPI/180. |
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| 116 | |
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| 117 | do j=1,nldc+1 |
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| 118 | zsolnet(j) = zsnet(j,1)*deltasza*deltasza/16. |
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| 119 | do nsza=2,nszadc |
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| 120 | zsolnet(j) = zsolnet(j)+zsnet(j,nsza)*0.5*deltasza* |
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| 121 | . sin(solza(nsza)*RPI/180.) |
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| 122 | enddo |
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| 123 | c overestimation: |
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| 124 | zsolnet(j) = zsolnet(j)*0.84 |
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| 125 | c print*,j,altdc(j),zsolnet(j) |
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| 126 | enddo |
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| 127 | c stop |
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| 128 | c ----------------------------- |
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| 129 | c -------- FIN TEST ---------- |
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| 130 | |
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| 131 | firstcall=.false. |
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| 132 | endif |
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| 133 | |
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| 134 | c -------------------------------------- |
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| 135 | c Interpolation in the GCM vertical grid |
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| 136 | c -------------------------------------- |
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| 137 | |
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| 138 | c Pressure levels |
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| 139 | c --------------- |
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| 140 | |
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| 141 | do j=1,klev+1 |
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| 142 | nl0 = 2 |
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| 143 | do i=1,nldc |
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| 144 | if (presdc(i).ge.PPB(j)) then |
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| 145 | nl0 = i+1 |
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| 146 | endif |
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| 147 | enddo |
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| 148 | |
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| 149 | factflux = (log10(max(PPB(j),presdc(nldc+1))) |
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| 150 | . -log10(presdc(nl0-1))) |
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| 151 | . /(log10(presdc(nl0))-log10(presdc(nl0-1))) |
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| 152 | ZFSNET(j) = factflux *zsolnet(nl0) |
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| 153 | . + (1.-factflux)*zsolnet(nl0-1) |
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| 154 | |
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| 155 | enddo |
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| 156 | |
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| 157 | PTOPSW = ZFSNET(klev+1) |
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| 158 | PSOLSW = ZFSNET(1) |
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| 159 | |
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| 160 | c Heating rates |
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| 161 | c ------------- |
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| 162 | c On utilise le gradient du flux pour calculer le taux de chauffage: |
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| 163 | c heat(K/s) = d(fluxnet) (W/m2) |
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| 164 | c *g (m/s2) |
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| 165 | c /(-dp) (epaisseur couche, en Pa=kg/m/s2) |
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| 166 | c /cp (J/kg/K) |
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| 167 | |
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| 168 | do j=1,klev |
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| 169 | ! ADAPTATION GCM POUR CP(T) |
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| 170 | PHEAT(j) = (ZFSNET(j+1)-ZFSNET(j)) |
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| 171 | . *RG/cpdet(pt(j)) / ((PPB(j)-PPB(j+1))*1.e5) |
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| 172 | c-------------- |
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| 173 | c BIDOUILLE POUR AJUSTEMENT ET TEST |
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| 174 | c if (PPB(j).lt.1.e-2) then |
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| 175 | c PHEAT(j) = PHEAT(j)*0.3 |
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| 176 | c endif |
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| 177 | c if ((PPB(j).gt.1.e-2).and.(PPB(j).lt.2.e-1)) then |
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| 178 | c PHEAT(j) = PHEAT(j)*0.7 |
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| 179 | c endif |
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| 180 | c if (PPB(j).gt.1.) then |
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| 181 | c PHEAT(j) = PHEAT(j)*2. |
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| 182 | c endif |
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| 183 | c-------------- |
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| 184 | enddo |
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| 185 | |
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| 186 | return |
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| 187 | end |
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| 188 | |
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