1 | !------------------------------------------------------------------------------- |
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2 | ! |
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3 | ! ###################################### |
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4 | REAL FUNCTION QSAT_SEAWATER(PT,PP) |
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5 | ! ###################################### |
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6 | ! |
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7 | !!**** *QSATW * - function to compute saturation vapor humidity from |
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8 | !! temperature |
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9 | !! |
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10 | !! PURPOSE |
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11 | !! ------- |
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12 | ! The purpose of this function is to compute the saturation vapor |
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13 | ! pressure from temperature over saline seawater |
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14 | ! |
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15 | ! |
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16 | !!** METHOD |
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17 | !! ------ |
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18 | !! Given temperature T (PT), the saturation vapor pressure es(T) |
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19 | !! (FOES(PT)) is computed by integration of the Clapeyron equation |
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20 | !! from the triple point temperature Tt (XTT) and the saturation vapor |
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21 | !! pressure of the triple point es(Tt) (XESTT), i.e |
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22 | !! The reduction due to salinity is compute with the factor 0.98 (reduction of 2%) |
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23 | !! |
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24 | !! es(T)= 0.98*EXP( alphaw - betaw /T - gammaw Log(T) ) |
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25 | !! |
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26 | !! with : |
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27 | !! alphaw (XALPW) = LOG(es(Tt))+ betaw/Tt + gammaw Log(Tt) |
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28 | !! betaw (XBETAW) = Lv(Tt)/Rv + gammaw Tt |
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29 | !! gammaw (XGAMW) = (Cl -Cpv) /Rv |
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30 | !! |
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31 | !! Then, the specific humidity at saturation is deduced. |
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32 | !! |
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33 | !! |
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34 | !! EXTERNAL |
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35 | !! -------- |
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36 | !! NONE |
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37 | !! |
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38 | !! IMPLICIT ARGUMENTS |
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39 | !! ------------------ |
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40 | !! Module MODD_CST : comtains physical constants |
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41 | !! XALPW : Constant for saturation vapor pressure function |
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42 | !! XBETAW : Constant for saturation vapor pressure function |
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43 | !! XGAMW : Constant for saturation vapor pressure function |
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44 | !! |
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45 | !! REFERENCE |
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46 | !! --------- |
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47 | !! Book2 of documentation of Meso-NH |
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48 | !! Zeng, X., Zhao, M., and Dickinson, R. E., 1998 : Intercomparaison of bulk |
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49 | !! aerodynamic algorithm for the computation of sea surface fluxes using |
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50 | !! TOGA COARE and TAO data. Journal of Climate, vol 11, n°10, pp 2628--2644 |
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51 | !! |
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52 | !! |
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53 | !! AUTHOR |
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54 | !! ------ |
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55 | !! C. Lebeaupin * Meteo France * |
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56 | !! |
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57 | !! MODIFICATIONS |
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58 | !! ------------- |
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59 | !! Original 6/04/2005 |
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60 | !------------------------------------------------------------------------------- |
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61 | ! |
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62 | !* 0. DECLARATIONS |
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63 | ! ------------ |
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64 | ! |
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65 | USE MODD_CSTS |
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66 | USE dimphy |
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67 | USE indice_sol_mod |
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68 | ! |
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69 | IMPLICIT NONE |
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70 | ! |
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71 | !* 0.1 Declarations of arguments and results |
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72 | ! |
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73 | ! |
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74 | |
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75 | REAL, DIMENSION(klon), INTENT(IN) :: PT ! Temperature |
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76 | ! (Kelvin) |
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77 | REAL, DIMENSION(klon), INTENT(IN) :: PP ! Pressure |
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78 | ! (Pa) |
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79 | REAL, DIMENSION(SIZE(PT)) :: PQSAT ! saturation vapor |
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80 | ! specific humidity |
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81 | ! with respect to |
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82 | ! water (kg/kg) |
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83 | |
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84 | ! |
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85 | !* 0.2 Declarations of local variables |
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86 | ! |
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87 | REAL, DIMENSION(SIZE(PT)) :: ZFOES ! saturation vapor |
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88 | ! pressure |
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89 | ! (Pascal) |
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90 | ! |
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91 | REAL, DIMENSION(SIZE(PT)) :: ZWORK1 |
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92 | REAL :: ZWORK2 |
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93 | !REAL(KIND=JPRB) :: ZHOOK_HANDLE |
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94 | !------------------------------------------------------------------------------- |
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95 | ! |
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96 | !IF (LHOOK) CALL DR_HOOK('MODE_THERMOS:QSATSEAW_1D',0,ZHOOK_HANDLE) |
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97 | ! |
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98 | !ZFOES = 1 !PSAT(PT(:)) |
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99 | !ZFOES = 0.98*ZFOES |
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100 | !ZFOES(:) = ZFOES(:)*1013.25E+02 !convert from atm to Pa |
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101 | ZFOES = 0.98*EXP( XALPW - XBETAW/PT - XGAMW*LOG(PT) ) |
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102 | ! vapor pressure reduction of 2% over saline seawater could have a significant |
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103 | ! impact on the computation of surface latent heat flux under strong wind |
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104 | ! conditions (Zeng et al, 1998). |
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105 | ! |
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106 | ZWORK1 = ZFOES/PP |
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107 | ZWORK2 = XRD/XRV |
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108 | ! |
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109 | !* 2. COMPUTE SATURATION HUMIDITY |
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110 | ! --------------------------- |
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111 | ! |
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112 | PQSAT = ZWORK2*ZWORK1 / (1.+(ZWORK2-1.)*ZWORK1) |
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113 | ! |
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114 | !IF (LHOOK) CALL DR_HOOK('MODE_THERMOS:QSATSEAW_1D',1,ZHOOK_HANDLE) |
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115 | !------------------------------------------------------------------------------- |
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116 | ! |
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117 | END FUNCTION QSAT_SEAWATER |
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118 | ! |
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119 | !------------------------------------------------------------------------------- |
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