*IF DEF,A05_2A,OR,DEF,A05_2C,OR,DEF,A05_3B,OR,DEF,A05_3C AJX1F405.148 C ******************************COPYRIGHT****************************** GTS2F400.10189 C (c) CROWN COPYRIGHT 1995, METEOROLOGICAL OFFICE, All Rights Reserved. GTS2F400.10190 C GTS2F400.10191 C Use, duplication or disclosure of this code is subject to the GTS2F400.10192 C restrictions as set forth in the contract. GTS2F400.10193 C GTS2F400.10194 C Meteorological Office GTS2F400.10195 C London Road GTS2F400.10196 C BRACKNELL GTS2F400.10197 C Berkshire UK GTS2F400.10198 C RG12 2SZ GTS2F400.10199 C GTS2F400.10200 C If no contract has been raised with this copy of the code, the use, GTS2F400.10201 C duplication or disclosure of it is strictly prohibited. Permission GTS2F400.10202 C to do so must first be obtained in writing from the Head of Numerical GTS2F400.10203 C Modelling at the above address. GTS2F400.10204 C ******************************COPYRIGHT****************************** GTS2F400.10205 C GTS2F400.10206 CLL SUBROUTINE THETAR------------------------------------------------- THETAR1A.3 CLL THETAR1A.4 CLL PURPOSE : CALCULATES THE POTENTIAL TEMPERATURE OF THE DETRAINING THETAR1A.5 CLL AIR IN LAYER K AND ALSO THE DIFFERENCE IN THE THETAR1A.6 CLL WATER VAPOUR CONTENT OF THE DETRAINING AIR FROM THAT THETAR1A.7 CLL OF THE MEAN PARCEL IN LAYER K THETAR1A.8 CLL THETAR1A.9 CLL SUITABLE FOR SINGLE COLUMN MODEL USE THETAR1A.10 CLL THETAR1A.11 CLL CODE REWORKED FOR CRAY Y-MP BY D.GREGORY AUTUMN/WINTER 1989/90 THETAR1A.12 CLL THETAR1A.13 CLL MODEL MODIFICATION HISTORY FROM MODEL VERSION 3.0: THETAR1A.14 CLL VERSION DATE THETAR1A.15 CLL THETAR1A.16 CLL 4.1 6/6/96 Extra check added to ensure that API2F401.1 CLL negative values of parcel water API2F401.2 CLL content are not generated. API2F401.3 CLL Pete Inness. API2F401.4 CLL 4.5 Jul. 98 Kill the IBM specific lines (JCThil) AJC1F405.20 CLL PROGRAMMING STANDARDS : UNIFIED MODEL DOCUMENTATION PAPER NO. 4 THETAR1A.17 CLL VERSION NO. 1 THETAR1A.18 CLL THETAR1A.19 CLL LOGICAL COMPONENTS COVERED : P27 THETAR1A.20 CLL THETAR1A.21 CLL DOCUMENTATION : UNIFIED MODEL DOCUMENTATION PAPER P27 THETAR1A.22 CLL THETAR1A.23 CLLEND----------------------------------------------------------------- THETAR1A.24 C THETAR1A.25 C*L ARGUMENTS--------------------------------------------------------- THETAR1A.26 C THETAR1A.27SUBROUTINE THETAR (NPNTS,THRK,QRK,XSQR,BGMK,THEK,QEK,QPK,QSEK, 1,1THETAR1A.28 * DQSK,BWKP1,EXK,PK) THETAR1A.29 C THETAR1A.30 IMPLICIT NONE THETAR1A.31 C THETAR1A.32 C---------------------------------------------------------------------- THETAR1A.33 C MODEL CONSTANTS THETAR1A.34 C---------------------------------------------------------------------- THETAR1A.35 C THETAR1A.36 *CALL C_EPSLON
THETAR1A.37 C THETAR1A.38 C---------------------------------------------------------------------- THETAR1A.39 C VECTOR LENGTHS AND LOOP COUNTERS THETAR1A.40 C---------------------------------------------------------------------- THETAR1A.41 C THETAR1A.42 INTEGER NPNTS ! VECTOR LENGTH THETAR1A.46 C THETAR1A.47 INTEGER I ! LOOP COUNTER THETAR1A.48 C THETAR1A.49 C THETAR1A.50 C---------------------------------------------------------------------- THETAR1A.51 C VARIABLES THAT ARE INPUT THETAR1A.52 C---------------------------------------------------------------------- THETAR1A.53 C THETAR1A.54 REAL THEK(NPNTS) ! IN ENVIRONMENT POTENTIAL TEMPERATURE THETAR1A.55 ! IN LAYER K (K) THETAR1A.56 C THETAR1A.57 REAL QEK(NPNTS) ! IN ENVIRONMENT MIXING RATIO THETAR1A.58 ! IN LAYER K (KG/KG) THETAR1A.59 C THETAR1A.60 REAL QPK(NPNTS) ! IN PARCEL MIXING RATIO IN LAYER K THETAR1A.61 ! (KG/KG) THETAR1A.62 C THETAR1A.63 REAL QSEK(NPNTS) ! IN SATURATION MIXING RATIO OF THE THETAR1A.64 ! ENVIRONMENT IN LAYER K (KG/KG) THETAR1A.65 C THETAR1A.66 REAL DQSK(NPNTS) ! IN GRADIENT OF SATURATION MIXING RATIO THETAR1A.67 ! WITH POTENTIAL TEMPERATURE FOR THE THETAR1A.68 ! ENVIRONMENT OF LAYER K (KG/KG/K) THETAR1A.69 C THETAR1A.70 LOGICAL BGMK(NPNTS) ! IN MASK FOR PARCELS SATURATED IN LAYER K THETAR1A.71 C THETAR1A.72 LOGICAL BWKP1(NPNTS) ! IN MASK FOR POINTS AT WHICH CONDENSATE THETAR1A.73 ! IS LIQUID IN LAYER K+1 THETAR1A.74 C THETAR1A.75 REAL EXK(NPNTS) ! IN EXNER RATIO FOR LEVEL K THETAR1A.76 C THETAR1A.77 REAL PK(NPNTS) ! IN PRESSURE AT LEVEL K (PA) THETAR1A.78 C THETAR1A.79 C THETAR1A.80 C---------------------------------------------------------------------- THETAR1A.81 C VARIABLES THAT ARE OUTPUT THETAR1A.82 C---------------------------------------------------------------------- THETAR1A.83 C THETAR1A.84 REAL THRK(NPNTS) ! OUT PARCEL DETRAINMENT POTENTIAL THETAR1A.85 ! TEMPERATURE IN LAYER K (K) THETAR1A.86 C THETAR1A.87 REAL QRK(NPNTS) ! OUT PARCEL DETRAINMENT MIXING RATIO THETAR1A.88 ! IN LAYER K (KG/KG) THETAR1A.89 C THETAR1A.90 REAL XSQR(NPNTS) ! OUT EXCESS WATER VAPOUR OF THETAR1A.91 ! DETRAINING AIR (KG/KG) THETAR1A.92 C THETAR1A.93 C THETAR1A.94 C---------------------------------------------------------------------- THETAR1A.95 C VARIABLES THAT ARE DEFINED LOCALLY THETAR1A.96 C THETAR1A.97 REAL TT(NPNTS) ! TEMPORARY TEMPERATURE FOR CALCULATION THETAR1A.108 ! OF SATURATION MIXING RATIO (K) THETAR1A.109 C THETAR1A.110 C THETAR1A.112 C---------------------------------------------------------------------- THETAR1A.113 C EXTERNAL ROUTINES CALLED THETAR1A.114 C---------------------------------------------------------------------- THETAR1A.115 C THETAR1A.116 EXTERNAL QSAT THETAR1A.117 C THETAR1A.118 C*---------------------------------------------------------------------- THETAR1A.119 C THETAR1A.120 DO 20 I=1,NPNTS THETAR1A.121 CL THETAR1A.122 CL---------------------------------------------------------------------- THETAR1A.123 CL CALCULATE THE POTENTIAL TEMPERATURE OF DETRAINING AIR THETAR1A.124 CL THETAR1A.125 CL UM DOCUMENTATION PAPER P27 THETAR1A.126 CL SECTION (6), EQUATION (26) THETAR1A.127 CL---------------------------------------------------------------------- THETAR1A.128 CL THETAR1A.129 IF (.NOT.BGMK(I)) THEN THETAR1A.130 THRK(I)=THEK(I) * (1. + C_VIRTUAL*QEK(I)) / THETAR1A.131 * (1. + C_VIRTUAL*QPK(I)) THETAR1A.132 ELSE THETAR1A.133 THRK(I) = THEK(I)*(1.0 + C_VIRTUAL*(QEK(I)-QSEK(I))/ THETAR1A.134 * (1.0 + C_VIRTUAL*THEK(I)*DQSK(I))) THETAR1A.135 ENDIF THETAR1A.136 CL THETAR1A.137 CL---------------------------------------------------------------------- THETAR1A.138 CL CALCULATE THE MIXING RATIO OF THE DETRAINING AIR AIR THE THETAR1A.139 CL DIFFERENCE BETWEEN THIS AND THE MIXING RATIO OF THE MEAN THETAR1A.140 CL PARCEL IN LAYER K THETAR1A.141 CL THETAR1A.142 CL THE MOISTURE DIFFERENCE IS USED TO CALCULATE THE THETAR1A.143 CL COND_DET_K TERM OF EQUATION (30), SECTION (6), THETAR1A.144 CL UM DOCUMENTATIONM PAPER P27 THETAR1A.145 CL---------------------------------------------------------------------- THETAR1A.146 CL THETAR1A.147 C THETAR1A.148 C----------------------------------------------------------------------- THETAR1A.149 C CONVERT POTENTIAL TEMPERATURE TO TEMPERATURE AND CALCULATE THETAR1A.150 C PRESSURE OF LAYER K FOR CALCULATION OF SATURATED THETAR1A.151 C MIXING RATIO THETAR1A.152 C----------------------------------------------------------------------- THETAR1A.153 C THETAR1A.154 TT(I) = THRK(I)*EXK(I) THETAR1A.155 20 CONTINUE THETAR1A.156 CALL QSAT
(XSQR,TT,PK,NPNTS) THETAR1A.157 C THETAR1A.158 DO 30 I=1,NPNTS THETAR1A.159 CL---------------------------------------------------------------------- API2F401.5 CL SMALL NUMERICAL APPROXIMATIONS IN THE ABOVE CALCULATIONS CAN MEAN API2F401.6 CL THAT THE DETRAINING PARCEL IS NO LONGER SATURATED AT THRK. ADD A API2F401.7 CL CHECK TO SEE IF THE PARCEL IS STILL SATURATED, AND RESET BGMK TO API2F401.8 CL FALSE IF IT IS NOT. API2F401.9 CL--------------------------------------------------------------------- API2F401.10 IF(XSQR(I).GT.QPK(I))BGMK(I)=.FALSE. API2F401.11 API2F401.12 API2F401.13 IF (BGMK(I)) THEN THETAR1A.160 QRK(I) = XSQR(I) THETAR1A.161 XSQR(I) = QPK(I) - XSQR(I) THETAR1A.162 ELSE THETAR1A.163 QRK(I) = QPK(I) THETAR1A.164 XSQR(I) = 0. THETAR1A.165 ENDIF THETAR1A.166 30 CONTINUE THETAR1A.167 C THETAR1A.168 RETURN THETAR1A.169 END THETAR1A.170 *ENDIF THETAR1A.171