[1989] | 1 | SUBROUTINE SUAERV & |
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| 2 | & ( KLEV , PETAH,& |
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| 3 | & PVDAES, PVDAEL, PVDAEU, PVDAED,& |
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| 4 | & PTRBGA, PVOBGA, PSTBGA, PAEOPS, PAEOPL, PAEOPU,& |
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| 5 | & PAEOPD, PTRPT , PAEADK, PAEADM, PAEROS & |
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| 6 | & ) |
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| 7 | |
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| 8 | !**** *SUAERV* - PARAMETERS FOR THE VERTICAL DISTRIBUTIONS OF AEROSOLS. |
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| 9 | |
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| 10 | ! PURPOSE. |
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| 11 | ! -------- |
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| 12 | |
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| 13 | ! THIS ROUTINE COMPUTES THE VALUES *PVDAEN* (*N=*S,*L,*U OR *D |
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| 14 | ! FOR SEA,LAND,URBAN OR DESERT) OF A SURFACE-NORMALISED VERTICAL |
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| 15 | ! DISTRIBUTION OF AEROSOLS' OPTICAL DEPHTS FROM THE ARGUMENT *PETAH* |
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| 16 | ! (VERTICAL COORDINATE) AT *KLEVP1* LEVELS. IT ALSO SETS VALUES FOR |
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| 17 | ! NON-GEOGRAPHICALLY WEIGHTED TOTAL OPTICAL DEPTHS (AT 0.55 E-06 |
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| 18 | ! WAVE-LENGTH) *PAEOPN* FOR THE SAME FOUR TYPES AND SIMILEAR OPTICAL |
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| 19 | ! DEPHTS DIVIDED BY PRESSURE FOR BACKGROUND WELL-MIXED AEROSOLS |
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| 20 | ! OF THREE TYPES *PMNBGA* (*MN*=*TR*,*VO* OR *ST* FOR TROPOSPHERIC, |
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| 21 | ! VOLCANIC (STRATOSPHERIC ASHES) OR STRATOSPHERIC (SULFURIC TYPE)). |
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| 22 | ! IT FINALLY SET VALUES FOR THE POWER TO BE APPLIED TO A TEMPERATURE |
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| 23 | ! RATIO SMALLER THAN ONE IN ORDER TO OBTAIN AN IDEX ONE IN THE |
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| 24 | ! STRATOSPHERE AND ZERO IN THE TROPOSPHERE WITH A RELATIVELY SMOOTH |
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| 25 | ! TRANSITION (*PTRPT*), AS WELL AS FOR ADSORPTION COEFFICIENTS FOR |
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| 26 | ! WATER TO THE THREE TYPE OF TROPOSPHERIC AEROSOLS (*PAEADK*) WITH |
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| 27 | ! A MINIMUM VALUE (IN THE WHOLE ATMOSPHERE) FOR THE SUM OF THE |
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| 28 | ! PRODUCTS OF *PAEADK* BY THE OPTICAL DEPTHS DIVIDED BY PRESURE |
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| 29 | ! THICKNESS: *PAEADM*. |
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| 30 | |
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| 31 | !** INTERFACE. |
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| 32 | ! ---------- |
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| 33 | |
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| 34 | ! *SUAERV* IS CALLED FROM *SUECRAD*. |
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| 35 | ! THERE ARE SIXTEEN DUMMY ARGUMENTS: *PETAH* IS THE VERTICAL |
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| 36 | ! COORDINATE. |
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| 37 | ! *PVDAEN* (*N=*S,*L,*U OR |
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| 38 | ! *D) ARE THE NORMALISED VERTICAL DISTRIBUTIONS. |
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| 39 | ! *KLEVP1* IS THE NUMBER OF |
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| 40 | ! LEVELS. |
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| 41 | ! *PMNBGA* (*MN*=*TR*,*VO* |
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| 42 | ! OR *ST*) ARE THE BACKGROUND OPTICAL DEPTHS DIVIDED BY PRESSURE. |
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| 43 | ! *PAEOPN* (*N=*S,*L,*U OR |
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| 44 | ! *D) ARE THE TOTAL OPTICAL DEPHTS FOR THE VERTICALLY VARYING |
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| 45 | ! AEROSOLS. |
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| 46 | ! *PTRPT* IS THE TEMPERATURE |
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| 47 | ! EXPONENT FOR THE STRATOSPHERIC DEFINITION. |
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| 48 | ! *PAEADK* (1,2,3) AND |
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| 49 | ! AND *PAEADM* ARE THE CONSTANTS FOR THE DEFINITION OF THE QUANTITY |
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| 50 | ! OF WATER VAPOUR THAT WILL BE ADSORBED TO THE DRY AEROSOLS TO FORM |
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| 51 | ! MOIST AEROSOLS. |
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| 52 | |
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| 53 | ! METHOD. |
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| 54 | ! ------- |
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| 55 | |
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| 56 | ! STRAIGHTFORWARD, EQUIVALENT HEIGTHS ARE GIVEN IN METERS (8434 |
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| 57 | ! FOR THE ATMOSPHERE) AND TROPOSPHERIC AND STRATOSPHERIC PRESSURE |
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| 58 | ! BOUNDARY VALUES ARE SET AT 101325 AND 19330 *PASCAL. |
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| 59 | |
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| 60 | ! EXTERNALS. |
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| 61 | ! ---------- |
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| 62 | |
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| 63 | ! NONE. |
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| 64 | |
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| 65 | ! REFERENCE. |
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| 66 | ! ---------- |
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| 67 | |
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| 68 | ! NONE. |
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| 69 | |
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| 70 | ! AUTHOR |
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| 71 | ! ------ |
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| 72 | ! J.-F. GELEYN E.C.M.W.F. 04/11/82. |
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| 73 | |
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| 74 | ! MODIFICATIONS |
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| 75 | ! ------------- |
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| 76 | ! J.-J. MORCRETTE E.C.M.W.F. 91/07/14 ADAPTATION TO I.F.S. |
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| 77 | ! JJ Morcrette 960903 block data SUAERH moved after end of SUAERV |
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| 78 | ! M.Hamrud 01-Oct-2003 CY28 Cleaning |
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| 79 | |
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| 80 | ! ------------------------------------------------------------------ |
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| 81 | |
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| 82 | USE PARKIND1 ,ONLY : JPIM ,JPRB |
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| 83 | USE YOMHOOK ,ONLY : LHOOK, DR_HOOK |
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| 84 | |
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| 85 | IMPLICIT NONE |
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| 86 | |
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| 87 | INTEGER(KIND=JPIM),INTENT(IN) :: KLEV |
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| 88 | REAL(KIND=JPRB) ,INTENT(IN) :: PETAH(KLEV+1) |
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| 89 | REAL(KIND=JPRB) ,INTENT(OUT) :: PVDAES(KLEV+1) |
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| 90 | REAL(KIND=JPRB) ,INTENT(OUT) :: PVDAEL(KLEV+1) |
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| 91 | REAL(KIND=JPRB) ,INTENT(OUT) :: PVDAEU(KLEV+1) |
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| 92 | REAL(KIND=JPRB) ,INTENT(OUT) :: PVDAED(KLEV+1) |
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| 93 | REAL(KIND=JPRB) ,INTENT(OUT) :: PTRBGA |
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| 94 | REAL(KIND=JPRB) ,INTENT(OUT) :: PVOBGA |
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| 95 | REAL(KIND=JPRB) ,INTENT(OUT) :: PSTBGA |
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| 96 | REAL(KIND=JPRB) ,INTENT(OUT) :: PAEOPS |
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| 97 | REAL(KIND=JPRB) ,INTENT(OUT) :: PAEOPL |
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| 98 | REAL(KIND=JPRB) ,INTENT(OUT) :: PAEOPU |
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| 99 | REAL(KIND=JPRB) ,INTENT(OUT) :: PAEOPD |
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| 100 | REAL(KIND=JPRB) ,INTENT(OUT) :: PTRPT |
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| 101 | REAL(KIND=JPRB) ,INTENT(OUT) :: PAEADK(3) |
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| 102 | REAL(KIND=JPRB) ,INTENT(OUT) :: PAEADM |
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| 103 | REAL(KIND=JPRB) ,INTENT(OUT) :: PAEROS |
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| 104 | ! ------------------------------------------------------------------ |
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| 105 | INTEGER(KIND=JPIM) :: JK |
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| 106 | |
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| 107 | REAL(KIND=JPRB) :: ZHSD, ZHSL, ZHSS, ZHSU |
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| 108 | REAL(KIND=JPRB) :: ZHOOK_HANDLE |
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| 109 | |
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| 110 | ! ------------------------------------------------------------------ |
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| 111 | |
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| 112 | !* 1. COMPUTATIONS. |
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| 113 | ! ------------- |
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| 114 | |
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| 115 | IF (LHOOK) CALL DR_HOOK('SUAERV',0,ZHOOK_HANDLE) |
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| 116 | ZHSS=MAX(1.0_JPRB,8434._JPRB/1000._JPRB) |
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| 117 | ZHSL=MAX(1.0_JPRB,8434._JPRB/1000._JPRB) |
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| 118 | ZHSU=MAX(1.0_JPRB,8434._JPRB/1000._JPRB) |
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| 119 | ZHSD=MAX(1.0_JPRB,8434._JPRB/3000._JPRB) |
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| 120 | PVDAES(1)=0._JPRB |
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| 121 | PVDAEL(1)=0._JPRB |
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| 122 | PVDAEU(1)=0._JPRB |
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| 123 | PVDAED(1)=0._JPRB |
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| 124 | IF(PETAH(1) /= 0.0_JPRB) THEN |
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| 125 | PVDAES(1)=PETAH(1)**ZHSS |
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| 126 | PVDAEL(1)=PETAH(1)**ZHSL |
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| 127 | PVDAEU(1)=PETAH(1)**ZHSU |
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| 128 | PVDAED(1)=PETAH(1)**ZHSD |
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| 129 | ENDIF |
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| 130 | DO JK=2,KLEV+1 |
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| 131 | PVDAES(JK)=PETAH(JK)**ZHSS |
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| 132 | PVDAEL(JK)=PETAH(JK)**ZHSL |
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| 133 | PVDAEU(JK)=PETAH(JK)**ZHSU |
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| 134 | PVDAED(JK)=PETAH(JK)**ZHSD |
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| 135 | ENDDO |
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| 136 | PTRBGA= 0.03_JPRB/(101325._JPRB-19330._JPRB) |
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| 137 | PVOBGA= 0.007_JPRB/19330._JPRB |
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| 138 | PSTBGA= 0.045_JPRB/19330._JPRB |
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| 139 | PAEOPS= 0.05_JPRB |
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| 140 | PAEOPL= 0.2_JPRB |
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| 141 | PAEOPU= 0.1_JPRB |
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| 142 | PAEOPD= 1.9_JPRB |
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| 143 | PTRPT = 30._JPRB |
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| 144 | PAEADK(1)=+.3876E-03_JPRB |
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| 145 | PAEADK(2)=+.6693E-02_JPRB |
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| 146 | PAEADK(3)=+.8563E-03_JPRB |
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| 147 | PAEADM = 2.6E-10_JPRB |
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| 148 | |
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| 149 | PAEROS = 0.1462E-16_JPRB |
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| 150 | |
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| 151 | ! ------------------------------------------------------------------ |
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| 152 | |
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| 153 | IF (LHOOK) CALL DR_HOOK('SUAERV',1,ZHOOK_HANDLE) |
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| 154 | END SUBROUTINE SUAERV |
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