| 1 | MODULE trcsms_c14b |
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| 2 | !!====================================================================== |
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| 3 | !! *** MODULE trcsms_c14b *** |
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| 4 | !! TOP : Bomb C14 main module |
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| 5 | !!====================================================================== |
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| 6 | !! History - ! 1994-05 ( J. Orr ) origial code |
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| 7 | !! 1.0 ! 2006-02 ( J.M. Molines ) Free form + modularity |
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| 8 | !! 2.0 ! 2008-12 ( C. Ethe ) reorganisation |
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| 9 | !!---------------------------------------------------------------------- |
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| 10 | #if defined key_c14b |
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| 11 | !!---------------------------------------------------------------------- |
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| 12 | !! 'key_c14b' Bomb C14 tracer |
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| 13 | !!---------------------------------------------------------------------- |
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| 14 | !! trc_sms_c14b : compute and add C14 suface forcing to C14 trends |
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| 15 | !!---------------------------------------------------------------------- |
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| 16 | USE oce_trc ! Ocean variables |
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| 17 | USE par_trc ! TOP parameters |
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| 18 | USE trc ! TOP variables |
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| 19 | USE trdmod_oce |
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| 20 | USE trdmod_trc |
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| 21 | USE iom |
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| 22 | |
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| 23 | IMPLICIT NONE |
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| 24 | PRIVATE |
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| 25 | |
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| 26 | !! * Routine accessibility |
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| 27 | PUBLIC trc_sms_c14b ! called in ??? |
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| 28 | |
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| 29 | !! * Module variables |
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| 30 | INTEGER , PUBLIC, PARAMETER :: jpmaxrec = 240 ! temporal parameter |
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| 31 | INTEGER , PUBLIC, PARAMETER :: jpmaxrec2 = 2 * jpmaxrec ! |
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| 32 | INTEGER , PUBLIC, PARAMETER :: jpzon = 3 ! number of zones |
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| 33 | |
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| 34 | INTEGER , PUBLIC :: ndate_beg_b ! initial calendar date (aammjj) for C14 |
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| 35 | INTEGER , PUBLIC :: nyear_beg_b ! initial year for C14 |
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| 36 | INTEGER , PUBLIC :: nyear_res_b ! restoring time constant (year) |
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| 37 | INTEGER , PUBLIC :: nyear_beg ! initial year (aa) |
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| 38 | |
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| 39 | REAL(wp), PUBLIC, DIMENSION(jpmaxrec,jpzon) :: bomb !: C14 atm data (3 zones) |
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| 40 | REAL(wp), PUBLIC, DIMENSION(jpi,jpj ,jpzon) :: fareaz !: Spatial Interpolation Factors |
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| 41 | REAL(wp), PUBLIC, DIMENSION(jpmaxrec2) :: spco2 !: Atmospheric CO2 |
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| 42 | |
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| 43 | REAL(wp), PUBLIC, DIMENSION(jpi,jpj) :: qtr_c14 !: flux at surface |
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| 44 | REAL(wp), PUBLIC, DIMENSION(jpi,jpj) :: qint_c14 !: cumulative flux |
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| 45 | |
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| 46 | REAL(wp) :: xlambda, xdecay, xaccum ! C14 decay coef. |
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| 47 | |
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| 48 | REAL(wp) :: xconv1 = 1.0 ! conversion from to |
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| 49 | REAL(wp) :: xconv2 = 0.01/3600. ! conversion from cm/h to m/s: |
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| 50 | REAL(wp) :: xconv3 = 1.0e+3 ! conversion from mol/l/atm to mol/m3/atm |
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| 51 | |
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| 52 | !! * Substitutions |
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| 53 | # include "top_substitute.h90" |
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| 54 | |
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| 55 | !!---------------------------------------------------------------------- |
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| 56 | !! TOP 1.0 , LOCEAN-IPSL (2005) |
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| 57 | !! $Header: /home/opalod/NEMOCVSROOT/NEMO/TOP_SRC/SMS/trcc14bomb.F90,v 1.2 2005/11/14 16:42:43 opalod Exp $ |
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| 58 | !! This software is governed by the CeCILL licence see modipsl/doc/NEMO_CeCILL.txt |
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| 59 | !!---------------------------------------------------------------------- |
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| 60 | |
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| 61 | CONTAINS |
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| 62 | |
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| 63 | SUBROUTINE trc_sms_c14b( kt ) |
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| 64 | !!---------------------------------------------------------------------- |
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| 65 | !! *** ROUTINE trc_sms_c14b *** |
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| 66 | !! |
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| 67 | !! ** Purpose : Compute the surface boundary contition on C14bomb |
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| 68 | !! passive tracer associated with air-mer fluxes and add it to |
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| 69 | !! the general trend of tracers equations. |
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| 70 | !! |
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| 71 | !! ** Original comments from J. Orr : |
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| 72 | !! |
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| 73 | !! Calculates the input of Bomb C-14 to the surface layer of OPA |
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| 74 | !! |
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| 75 | !! James Orr, LMCE, 28 October 1992 |
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| 76 | !! |
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| 77 | !! Initial approach mimics that of Toggweiler, Dixon, & Bryan (1989) |
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| 78 | !! (hereafter referred to as TDB) with constant gas exchange, |
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| 79 | !! although in this case, a perturbation approach is used for |
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| 80 | !! bomb-C14 so that both the ocean and atmosphere begin at zero. |
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| 81 | !! This saves tremendous amounts of computer time since no |
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| 82 | !! equilibrum run is first required (i.e., for natural C-14). |
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| 83 | !! Note: Many sensitivity tests can be run with this approach and |
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| 84 | !! one never has to make a run for natural C-14; otherwise, |
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| 85 | !! a run for natural C-14 must be run each time that one |
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| 86 | !! changes a model parameter! |
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| 87 | !! |
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| 88 | !! |
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| 89 | !! 19 August 1993: Modified to consider Atmospheric C-14 fom IPCC. |
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| 90 | !! That is, the IPCC has provided a C-14 atmospheric record (courtesy |
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| 91 | !! of Martin Heimann) for model calibration. This model spans from |
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| 92 | !! preindustrial times to present, in a format different than that |
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| 93 | !! given by TDB. It must be converted to the ORR C-14 units used |
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| 94 | !! here, although in this case, the perturbation includes not only |
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| 95 | !! bomb C-14 but changes due to the Suess effect. |
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| 96 | !! |
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| 97 | !!---------------------------------------------------------------------- |
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| 98 | !! * Arguments |
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| 99 | INTEGER, INTENT( in ) :: kt ! ocean time-step index |
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| 100 | |
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| 101 | !! * Local declarations |
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| 102 | INTEGER :: & |
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| 103 | ji, jj, jk, jz |
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| 104 | |
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| 105 | INTEGER :: & |
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| 106 | iyear_beg, & |
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| 107 | iyear_beg1, iyear_end1, & |
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| 108 | imonth1, im1, im2, & |
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| 109 | iyear_beg2, iyear_end2, & |
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| 110 | imonth2, in1, in2 |
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| 111 | |
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| 112 | REAL(wp), DIMENSION(jpi,jpj) :: & |
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| 113 | zatmbc14 |
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| 114 | |
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| 115 | REAL(wp), DIMENSION(jpzon) :: & |
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| 116 | zonbc14 !: time interp atm C14 |
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| 117 | |
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| 118 | REAL(wp) :: & |
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| 119 | zpco2at !: time interp atm C02 |
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| 120 | |
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| 121 | REAL(wp) :: & !: dummy variables |
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| 122 | zt, ztp, zsk, & |
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| 123 | zsol , & !: solubility |
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| 124 | zsch , & !: schmidt number |
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| 125 | zv2 , & !: wind speed ( square) |
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| 126 | zpv , & !: piston velocity |
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| 127 | zdemi, ztra |
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| 128 | #if defined key_diatrc && defined key_iomput |
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| 129 | REAL(wp), DIMENSION(jpi,jpj,jpk) :: zw3d |
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| 130 | #endif |
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| 131 | !!---------------------------------------------------------------------- |
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| 132 | |
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| 133 | IF( kt == nittrc000 ) THEN |
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| 134 | ! Computation of decay coeffcient |
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| 135 | zdemi = 5730. |
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| 136 | xlambda = LOG(2.) / zdemi / ( nyear_len(1) * rday ) |
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| 137 | xdecay = EXP( - xlambda * rdt ) |
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| 138 | xaccum = 1.0 - xdecay |
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| 139 | ENDIF |
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| 140 | |
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| 141 | ! Temporal interpolation |
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| 142 | ! ---------------------- |
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| 143 | iyear_beg = nyear - 1954 + ( nyear_res_b - 1700 - nyear_beg_b ) ! JMM Very dangerous |
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| 144 | ! nyear=0001 for 1955 |
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| 145 | ! For Atmospheric C14 concentrations: |
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| 146 | iyear_beg1 = iyear_beg |
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| 147 | imonth1 = nmonth |
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| 148 | IF ( imonth1 <= 6 ) THEN |
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| 149 | iyear_beg1 = iyear_beg1 - 1 |
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| 150 | im1 = 6 - imonth1 + 1 |
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| 151 | im2 = 6 + imonth1 - 1 |
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| 152 | ELSE |
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| 153 | im1 = 12 - imonth1 + 7 |
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| 154 | im2 = imonth1 - 7 |
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| 155 | ENDIF |
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| 156 | iyear_end1 = iyear_beg1 + 1 |
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| 157 | |
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| 158 | iyear_beg1 = MAX( iyear_beg1, 1 ) |
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| 159 | iyear_end1 = MIN( iyear_end1, 241 ) |
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| 160 | |
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| 161 | |
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| 162 | ! For Atmospheric CO2 concentrations: |
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| 163 | iyear_beg2 = 2 * iyear_beg - 1 |
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| 164 | imonth2 = INT( nmonth / 2. ) |
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| 165 | |
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| 166 | IF ( imonth2 <= 3 ) THEN |
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| 167 | iyear_beg2 = iyear_beg2 - 1 |
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| 168 | in1 = 3 - imonth2 + 1 |
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| 169 | in2 = 3 + imonth2 - 1 |
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| 170 | ELSE |
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| 171 | in1 = 6 - imonth2 + 4 |
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| 172 | in2 = imonth2 - 4 |
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| 173 | ENDIF |
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| 174 | |
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| 175 | iyear_end2 = iyear_beg2 + 1 |
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| 176 | |
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| 177 | iyear_beg2 = MAX( iyear_beg2, 1 ) |
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| 178 | iyear_end2 = MIN( iyear_end2, 482 ) |
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| 179 | |
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| 180 | |
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| 181 | ! ---------------------------------------------------------------- |
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| 182 | ! As explained by the TDB 89 papers, C-14/C-12 is the same |
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| 183 | ! as C-14 concentration in this special case (no fractionation |
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| 184 | ! effects in this model, which thus allow direct comparison |
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| 185 | ! to del-C-14, after unit change from above). |
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| 186 | ! ----------------------------------------------------------------------- |
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| 187 | ! Calc C-14 in atmosphere based on interp of IPCC (M. Heimann) data |
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| 188 | ! - Compare input to calculated C-14 for each time in record |
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| 189 | !------------------------------------------------------------------------- |
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| 190 | |
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| 191 | |
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| 192 | ! Temporal and spatial interpolation at time k |
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| 193 | ! -------------------------------------------------- |
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| 194 | |
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| 195 | ! Compute atmospheric C-14 for each zone (90-20S, 20S-20N, 20-90N) |
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| 196 | DO jz = 1, jpzon |
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| 197 | zonbc14(jz) = ( bomb(iyear_beg1,jz) * FLOAT( im1 ) & |
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| 198 | & + bomb(iyear_end1,jz) * FLOAT( im2 ) ) / 12. |
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| 199 | ! C-14 exactly starts at zero : |
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| 200 | ! JMM +Zouhair : Slightly negative values are set to 0 (when perturbation approaches) |
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| 201 | zonbc14(jz) = MAX( zonbc14(jz), 0. ) |
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| 202 | END DO |
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| 203 | |
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| 204 | |
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| 205 | ! For each (i,j)-box, with information from the fractional area |
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| 206 | ! (zonmean), computes area-weighted mean to give the atmospheric C-14 |
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| 207 | ! ---------------------------------------------------------------- |
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| 208 | DO jj = 1, jpj |
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| 209 | DO ji = 1, jpi |
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| 210 | zatmbc14(ji,jj) = zonbc14(1) * fareaz(ji,jj,1) & |
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| 211 | & + zonbc14(2) * fareaz(ji,jj,2) & |
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| 212 | & + zonbc14(3) * fareaz(ji,jj,3) |
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| 213 | END DO |
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| 214 | END DO |
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| 215 | |
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| 216 | ! time interpolation of CO2 concentrations to it time step |
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| 217 | zpco2at = ( spco2(iyear_beg2) * FLOAT( in1 ) & |
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| 218 | & + spco2(iyear_end2) * FLOAT( in2 ) ) / 6. |
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| 219 | |
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| 220 | IF (lwp) THEN |
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| 221 | WRITE(numout, *) 'time : ', kt, ' CO2 year begin/end :',iyear_beg2,'/',iyear_end2, & |
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| 222 | & ' CO2 concen : ',zpco2at |
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| 223 | WRITE(numout, *) 'time : ', kt, ' C14 year begin/end :',iyear_beg1,'/',iyear_end1, & |
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| 224 | & ' C14B concen (Z1/Z2/Z3) : ',zonbc14(1),'/',zonbc14(2),'/',zonbc14(3) |
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| 225 | ENDIF |
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| 226 | |
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| 227 | ! Determine seasonally variable gas exchange coefficient |
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| 228 | !---------------------------------------------------------- |
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| 229 | ! Computes the Schmidt number of CO2 in seawater using the formulation |
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| 230 | ! presented by Wanninkhof (1992, J. Geophys. Res., 97,7373-7382). |
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| 231 | ! ------------------------------------------------------------------- |
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| 232 | DO jj = 1, jpj |
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| 233 | DO ji = 1, jpi |
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| 234 | ! Computation of solubility |
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| 235 | IF (tmask(ji,jj,1) > 0.) THEN |
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| 236 | ztp = ( tn(ji,jj,1) + 273.16 ) * 0.01 |
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| 237 | zsk = 0.023517 + ztp * ( -0.023656 + 0.0047036 * ztp ) |
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| 238 | zsol = EXP( -60.2409 + 93.4517 / ztp + 23.3585 * LOG( ztp ) + zsk * sn(ji,jj,1) ) |
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| 239 | ! convert solubilities [mol/(l * atm)] -> [mol/(m^3 * ppm)] |
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| 240 | zsol = zsol * 1.0e-03 |
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| 241 | ELSE |
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| 242 | zsol = 0. |
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| 243 | ENDIF |
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| 244 | |
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| 245 | ! speed transfert : Formulation of Wanninkhof (1992, JGR, 97,7373-7382) |
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| 246 | ! JMM/Zouhair : coef of 0.25 rather than 0.3332 for CORe wind speed |
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| 247 | |
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| 248 | ! Computes the Schmidt number of CO2 in seawater |
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| 249 | zt = tn(ji,jj,1) |
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| 250 | zsch = 2073.1 + zt * ( -125.62 + zt * (3.6276 - 0.043219 * zt ) ) |
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| 251 | |
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| 252 | ! Wanninkhof Piston velocity and convert from units [cm/hr] -> [m/s] |
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| 253 | zv2 = wndm(ji,jj) * wndm(ji,jj) |
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| 254 | zsch = zsch / 660. |
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| 255 | zpv = ( 0.25 * zv2 / SQRT(zsch) ) * xconv2 * tmask(ji,jj,1) |
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| 256 | |
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| 257 | ! Flux of Bomb C-14 from air-sea : speed*(conc. at equil-conc. at surf) |
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| 258 | ! in C-14 (orr-model-units) / m**2 * s |
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| 259 | qtr_c14(ji,jj) = -zpv * zsol * zpco2at & |
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| 260 | & * ( trb(ji,jj,1,jpc14) - zatmbc14(ji,jj) ) & |
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| 261 | #if defined key_degrad |
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| 262 | & * facvol(ji,jj,1) & |
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| 263 | #endif |
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| 264 | & * tmask(ji,jj,1) * ( 1. - fr_i(ji,jj) ) / 2. |
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| 265 | |
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| 266 | ! Add the surface flux to the trend |
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| 267 | tra(ji,jj,1,jpc14) = tra(ji,jj,1,jpc14) + qtr_c14(ji,jj) / fse3t(ji,jj,1) |
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| 268 | |
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| 269 | ! cumulation of surface flux at each time step |
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| 270 | qint_c14(ji,jj) = qint_c14(ji,jj) + qtr_c14(ji,jj) * rdt |
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| 271 | |
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| 272 | # if defined key_diatrc && ! defined key_iomput |
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| 273 | ! Save 2D diagnostics |
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| 274 | trc2d(ji,jj,jp_c14b0_2d ) = qtr_c14 (ji,jj) |
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| 275 | trc2d(ji,jj,jp_c14b0_2d + 1) = qint_c14(ji,jj) |
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| 276 | # endif |
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| 277 | END DO |
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| 278 | END DO |
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| 279 | |
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| 280 | ! Computation of decay effects on tracer concentration |
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| 281 | DO jk = 1, jpk |
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| 282 | DO jj = 1, jpj |
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| 283 | DO ji = 1, jpi |
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| 284 | #if ! defined key_degrad |
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| 285 | ztra = trn(ji,jj,jk,jpc14) * xaccum |
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| 286 | #else |
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| 287 | ztra = trn(ji,jj,jk,jpc14) * ( 1. - EXP( -xlambda * rdt * facvol(ji,jj,jk) ) ) |
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| 288 | #endif |
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| 289 | tra(ji,jj,jk,jpc14) = tra(ji,jj,jk,jpc14) - ztra / rdt |
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| 290 | #if defined key_diatrc |
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| 291 | ! Save 3D diagnostics |
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| 292 | # if ! defined key_iomput |
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| 293 | trc3d(ji,jj,jk,jp_c14b0_3d ) = ztra ! radioactive decay |
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| 294 | # else |
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| 295 | zw3d(ji,jj,jk) = ztra ! radioactive decay |
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| 296 | # endif |
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| 297 | #endif |
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| 298 | END DO |
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| 299 | END DO |
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| 300 | END DO |
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| 301 | |
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| 302 | #if defined key_diatrc && defined key_iomput |
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| 303 | CALL iom_put( "qtrC14b" , qtr_c14 ) |
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| 304 | CALL iom_put( "qintC14b" , qint_c14 ) |
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| 305 | #endif |
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| 306 | #if defined key_diatrc && defined key_iomput |
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| 307 | CALL iom_put( "fdecay" , zw3d ) |
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| 308 | #endif |
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| 309 | IF( l_trdtrc ) THEN |
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| 310 | CALL trd_mod_trc( tra(:,:,:,jpc14), jpc14, jptra_trd_sms, kt ) ! save trends |
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| 311 | END IF |
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| 312 | |
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| 313 | END SUBROUTINE trc_sms_c14b |
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| 314 | |
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| 315 | #else |
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| 316 | !!---------------------------------------------------------------------- |
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| 317 | !! Default option Dummy module |
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| 318 | !!---------------------------------------------------------------------- |
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| 319 | CONTAINS |
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| 320 | SUBROUTINE trc_sms_c14b( kt ) ! Empty routine |
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| 321 | WRITE(*,*) 'trc_freons: You should not have seen this print! error?', kt |
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| 322 | END SUBROUTINE trc_sms_c14b |
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| 323 | #endif |
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| 324 | |
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| 325 | !!====================================================================== |
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| 326 | END MODULE trcsms_c14b |
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