| [3331] | 1 | SUBROUTINE stratosphere_mask(t_seri, pplay, xlat) |
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| 2 | |
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| 3 | !!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!! |
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| 4 | ! |
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| 5 | ! determination of tropopause height and temperature from gridded temperature data |
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| 6 | ! |
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| 7 | ! reference: Reichler, T., M. Dameris, and R. Sausen (2003): |
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| 8 | ! modified: 6/28/06 tjr |
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| 9 | ! adapted to LMDZ by C. Kleinschmitt (2016-02-15) |
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| 10 | ! |
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| 11 | ! input: temp(nlon,nlat,nlev) 3D-temperature field |
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| 12 | ! ps(nlon,nlat) 2D-surface pressure field |
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| 13 | ! zs(nlon,nlat) 2D-surface height |
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| 14 | ! nlon grid points in x |
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| 15 | ! nlat grid points in y |
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| 16 | ! pfull(nlon,nlat,nlev) full pressure levels in Pa |
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| 17 | ! plimu upper limit for tropopause pressure |
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| 18 | ! pliml lower limit for tropopause pressure |
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| 19 | ! gamma tropopause criterion, e.g. -0.002 K/m |
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| 20 | ! |
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| 21 | ! output: tp(nlon, nlat) tropopause pressure in Pa, -999. if undefined |
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| 22 | ! ttp(nlon, nlat) tropopause temperature in K, -999. if undefined |
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| 23 | ! ztp(nlon, nlat) tropopause height in m, -999. if undefined |
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| 24 | ! tperr # of undetermined values |
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| 25 | ! |
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| 26 | !!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!! |
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| 27 | |
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| 28 | USE dimphy |
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| 29 | USE phys_local_var_mod, ONLY: stratomask |
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| 30 | |
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| 31 | IMPLICIT NONE |
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| 32 | |
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| 33 | REAL,DIMENSION(klon,klev),INTENT(IN) :: t_seri ! Temperature |
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| 34 | REAL,DIMENSION(klon,klev),INTENT(IN) :: pplay ! pression pour le mileu de chaque couche (en Pa) |
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| 35 | REAL,DIMENSION(klon),INTENT(IN) :: xlat ! latitudes pour chaque point |
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| 36 | |
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| 37 | REAL, PARAMETER :: plimu=45000. |
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| 38 | REAL, PARAMETER :: pliml=7500. |
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| 39 | REAL, PARAMETER :: gamma=-0.002 |
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| 40 | LOGICAL, PARAMETER :: dofill=.true. |
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| 41 | REAL,DIMENSION(klon) :: tp, ttp, ztp |
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| 42 | REAL,DIMENSION(klev) :: t, p |
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| 43 | INTEGER :: tperr, i, k, invert, ifil |
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| 44 | REAL :: ptrp, ttrp, ztrp, psrf, zsrf, pi |
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| 45 | |
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| 46 | pi = 4.*ATAN(1.) |
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| 47 | |
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| 48 | tperr = 0 |
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| 49 | DO i=1,klon |
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| 50 | DO k=1,klev |
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| 51 | t(k)=t_seri(i,klev+1-k) |
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| 52 | p(k)=pplay(i,klev+1-k) |
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| 53 | ENDDO |
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| 54 | psrf=pplay(i,1) |
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| 55 | zsrf=0.0 |
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| 56 | call twmo(klev, t, p, psrf, zsrf, plimu, pliml, gamma, ptrp, ttrp, ztrp) |
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| 57 | tp(i)=ptrp |
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| 58 | ttp(i)=ttrp |
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| 59 | ztp(i)=ztrp |
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| 60 | IF (ptrp.lt.0.0) THEN |
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| 61 | tperr = tperr+1 |
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| 62 | ENDIF |
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| 63 | ENDDO |
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| 64 | |
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| 65 | ! fill holes |
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| 66 | IF (dofill) THEN |
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| 67 | ifil=0 |
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| 68 | DO i=1,klon |
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| 69 | IF (tp(i).lt.-990.) THEN |
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| 70 | !set missing values to very simple profile (neighbour averaging too expensive in LMDZ) |
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| 71 | tp(i)=50000.-20000.*cos(xlat(i)/360.*2.*pi) |
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| 72 | ifil=ifil+1 |
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| 73 | ENDIF |
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| 74 | ENDDO |
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| 75 | ! |
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| 76 | IF (ifil.ne.tperr) THEN |
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| 77 | CALL abort_physic('stratosphere_mask', 'inconsistency',1) |
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| 78 | ENDIF |
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| 79 | ENDIF |
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| 80 | ! |
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| 81 | DO i=1, klon |
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| 82 | DO k=1, klev |
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| 83 | IF (pplay(i,k).LT.tp(i)) THEN |
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| 84 | stratomask(i,k)=1.0 |
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| 85 | ELSE |
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| 86 | stratomask(i,k)=0.0 |
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| 87 | ENDIF |
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| 88 | ENDDO |
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| 89 | ENDDO |
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| 90 | |
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| 91 | !!--diagnostic not used for now |
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| 92 | !!p_tropopause(:)=tp(:) |
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| 93 | |
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| 94 | IF (ifil.gt.0) THEN |
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| 95 | print *,'Tropopause: number of undetermined values =', ifil |
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| 96 | ENDIF |
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| 97 | |
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| 98 | RETURN |
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| 99 | END SUBROUTINE stratosphere_mask |
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| 100 | |
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| 101 | !!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!! |
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| 102 | ! twmo |
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| 103 | !!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!! |
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| 104 | |
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| 105 | subroutine twmo(level, t, p, ps, zs, plimu, pliml, gamma, ptrp, ttrp, ztrp) |
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| 106 | |
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| 107 | implicit none |
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| 108 | |
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| 109 | include "YOMCST.h" |
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| 110 | |
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| 111 | integer,intent(in) :: level |
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| 112 | real,intent(in),dimension(level):: t, p |
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| 113 | real,intent(in) :: plimu, pliml, gamma, ps, zs |
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| 114 | real,intent(out) :: ptrp, ttrp, ztrp |
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| 115 | |
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| 116 | real,parameter :: deltaz = 2000.0 |
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| 117 | |
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| 118 | real :: faktor |
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| 119 | real :: pmk, pm, a, b, tm, dtdp, dtdz, dlnp, tdlnp |
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| 120 | real :: ag, bg, ptph, ttph, a0, b0 |
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| 121 | real :: pm0, tm0, pmk0, dtdz0 |
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| 122 | real :: p2km, asum, aquer |
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| 123 | real :: pmk2, pm2, a2, b2, tm2, dtdp2, dtdz2 |
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| 124 | integer :: icount, jj, j |
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| 125 | |
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| 126 | ptrp=-999.0 |
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| 127 | ttrp=-999.0 |
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| 128 | ztrp=-999.0 |
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| 129 | |
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| 130 | faktor = -RG/R |
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| 131 | |
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| 132 | do j=level,2,-1 |
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| 133 | |
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| 134 | ! dt/dz |
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| 135 | pmk= 0.5 * (p(j-1)**rkappa+p(j)**rkappa) ! p**k at half level |
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| 136 | pm = pmk**(1./rkappa) ! p at half level |
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| 137 | a = (t(j-1)-t(j))/(p(j-1)**rkappa-p(j)**rkappa) ! dT/dp^k |
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| 138 | b = t(j)-(a*p(j)**rkappa) |
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| 139 | tm = a * pmk + b ! T at half level |
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| 140 | dtdp = a * rkappa * pm**(rkappa-1.) ! dT/dp at half level |
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| 141 | dtdz = faktor*dtdp*pm/tm ! dT/dz at half level |
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| 142 | |
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| 143 | ! dt/dz valid? |
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| 144 | if (j.eq.level) go to 999 ! no, start level, initialize first |
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| 145 | if (dtdz.le.gamma) go to 999 ! no, dt/dz < -2 K/km |
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| 146 | if (dtdz0.gt.gamma) go to 999 ! no, dt/dz below > -2 K/km |
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| 147 | if (pm.gt.plimu) go to 999 ! no, pm too low |
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| 148 | |
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| 149 | ! dtdz is valid, calculate tropopause pressure ptph |
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| 150 | ag = (dtdz-dtdz0) / (pmk-pmk0) |
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| 151 | bg = dtdz0 - (ag * pmk0) |
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| 152 | ptph = exp(log((gamma-bg)/ag)/rkappa) |
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| 153 | |
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| 154 | ! calculate temperature at this ptph assuming linear gamma |
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| 155 | ! interpolation |
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| 156 | ttph = tm0 |
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| 157 | ttph = ttph - (bg * log(pm0) + ag * (pm0**rkappa) /rkappa) / faktor*t(j) |
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| 158 | ttph = ttph + (bg * log(ptph) + ag * (ptph**rkappa)/rkappa) / faktor*t(j) |
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| 159 | |
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| 160 | if (ptph.lt.pliml) go to 999 |
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| 161 | if (ptph.gt.plimu) go to 999 |
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| 162 | |
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| 163 | ! 2nd test: dtdz above 2 km must not exceed gamma |
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| 164 | p2km = ptph + deltaz*(pm/tm)*faktor ! p at ptph + 2km |
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| 165 | asum = 0.0 ! dtdz above |
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| 166 | icount = 0 ! number of levels above |
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| 167 | |
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| 168 | ! test until apm < p2km |
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| 169 | do jj=j,2,-1 |
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| 170 | |
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| 171 | pmk2 = .5 * (p(jj-1)**rkappa+p(jj)**rkappa) ! p mean ^kappa |
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| 172 | pm2 = pmk2**(1/rkappa) ! p mean |
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| 173 | if(pm2.gt.ptph) go to 110 ! doesn't happen |
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| 174 | if(pm2.lt.p2km) go to 888 ! ptropo is valid |
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| 175 | |
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| 176 | a2 = (t(jj-1)-t(jj)) ! a |
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| 177 | a2 = a2/(p(jj-1)**rkappa-p(jj)**rkappa) |
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| 178 | b2 = t(jj)-(a2*p(jj)**rkappa) ! b |
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| 179 | tm2 = a2 * pmk2 + b2 ! T mean |
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| 180 | dtdp2 = a2 * rkappa * (pm2**(rkappa-1)) ! dt/dp |
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| 181 | dtdz2 = faktor*dtdp2*pm2/tm2 |
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| 182 | asum = asum+dtdz2 |
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| 183 | icount = icount+1 |
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| 184 | aquer = asum/float(icount) ! dt/dz mean |
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| 185 | |
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| 186 | ! discard ptropo ? |
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| 187 | if (aquer.le.gamma) go to 999 ! dt/dz above < gamma |
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| 188 | |
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| 189 | 110 continue |
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| 190 | enddo ! test next level |
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| 191 | |
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| 192 | 888 continue ! ptph is valid |
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| 193 | ptrp = ptph |
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| 194 | ttrp = ttph |
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| 195 | |
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| 196 | ! now calculate height of tropopause by integrating hypsometric equation |
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| 197 | ! from ps to ptrp |
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| 198 | ! linearly interpolate in p (results are identical to p^kappa) |
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| 199 | |
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| 200 | jj = LEVEL ! bottom |
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| 201 | do while ((P(jj).gt.PS) .or. (T(jj).lt.100)) ! T must be valid too |
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| 202 | jj=jj-1 |
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| 203 | enddo |
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| 204 | |
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| 205 | DLNP = log(PS/P(jj)) ! from surface pressure |
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| 206 | TM = T(jj) ! take TM of lowest level (better: extrapolate) |
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| 207 | TDLNP = TM*DLNP |
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| 208 | |
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| 209 | do while ( (JJ.ge.2) .and. (PTRP.lt.P(jj-1)) ) |
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| 210 | DLNP = log(P(jj)/P(jj-1)) |
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| 211 | TM = 0.5 * (T(jj) + T(jj-1)) |
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| 212 | TDLNP = TDLNP + TM*DLNP |
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| 213 | JJ=JJ-1 |
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| 214 | enddo |
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| 215 | |
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| 216 | DLNP = log(P(jj)/PTRP) ! up to tropopause pressure |
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| 217 | TM = 0.5 * (T(jj) + TTRP) ! use TTRP to get TM of this level |
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| 218 | TDLNP = TDLNP + TM*DLNP |
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| 219 | |
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| 220 | ZTRP = ZS + TDLNP*R/RG |
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| 221 | |
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| 222 | if (ZTRP .lt. 0) then |
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| 223 | print*,ZTRP |
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| 224 | print*,PS |
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| 225 | print*,P |
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| 226 | print*,T |
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| 227 | print*,ZS |
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| 228 | stop |
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| 229 | endif |
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| 230 | |
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| 231 | return |
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| 232 | |
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| 233 | 999 continue ! continue search at next higher level |
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| 234 | tm0 = tm |
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| 235 | pm0 = pm |
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| 236 | pmk0 = pmk |
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| 237 | dtdz0 = dtdz |
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| 238 | a0 = a |
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| 239 | b0 = b |
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| 240 | |
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| 241 | enddo |
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| 242 | |
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| 243 | ! no tropopouse found |
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| 244 | return |
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| 245 | end subroutine twmo |
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