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! $Id$ |
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module o3_chem_m |
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IMPLICIT none |
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private o3_prod |
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contains |
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subroutine o3_chem(julien, gmtime, t_seri, zmasse, pdtphys, rlat, rlon, q) |
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! This procedure evolves the ozone mass fraction through a time |
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! step taking only chemistry into account. |
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! All the 2-dimensional arrays are on the partial "physics" grid. |
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! Their shape is "(/klon, nbp_lev/)". |
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! Index "(i, :)" is for longitude "rlon(i)", latitude "rlat(i)". |
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use assert_m, only: assert |
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use dimphy, only: klon |
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use regr_pr_comb_coefoz_m, only: c_Mob, a4_mass, a2, r_het_interm |
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use mod_grid_phy_lmdz, only: nbp_lev |
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use nrtype, only: pi |
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integer, intent(in):: julien ! jour julien, 1 <= julien <= 360 |
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real, intent(in):: gmtime ! heure de la journ�e en fraction de jour |
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real, intent(in):: t_seri(:, :) ! (klon, nbp_lev) temperature, in K |
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real, intent(in):: zmasse(:, :) ! (klon, nbp_lev) |
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! (column-density of mass of air in a cell, in kg m-2) |
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! "zmasse(:, k)" is for layer "k".) |
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real, intent(in):: pdtphys ! time step for physics, in s |
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REAL, intent(in):: rlat(:), rlon(:) |
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! (longitude and latitude of each horizontal position, in degrees) |
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real, intent(inout):: q(:, :) ! (klon, nbp_lev) mass fraction of ozone |
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! "q(:, k)" is at middle of layer "k".) |
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! Variables local to the procedure: |
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! (for "pi") |
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integer k |
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real c(klon, nbp_lev) |
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! (constant term during a time step in the net mass production |
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! rate of ozone by chemistry, per unit mass of air, in s-1) |
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! "c(:, k)" is at middle of layer "k".) |
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real b(klon, nbp_lev) |
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! (coefficient of "q" in the net mass production |
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! rate of ozone by chemistry, per unit mass of air, in s-1) |
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! "b(:, k)" is at middle of layer "k".) |
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real dq_o3_chem(klon, nbp_lev) |
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! (variation of ozone mass fraction due to chemistry during a time step) |
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! "dq_o3_chem(:, k)" is at middle of layer "k".) |
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real earth_long |
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! (longitude vraie de la Terre dans son orbite solaire, par |
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! rapport au point vernal (21 mars), en degr�s) |
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real pmu0(klon) ! mean of cosine of solar zenith angle during "pdtphys" |
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real trash1 |
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real trash2(klon) |
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!------------------------------------------------------------- |
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call assert(klon == (/size(q, 1), size(t_seri, 1), size(zmasse, 1), & |
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size(rlat), size(rlon)/), "o3_chem klon") |
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call assert(nbp_lev == (/size(q, 2), size(t_seri, 2), size(zmasse, 2)/), & |
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"o3_chem nbp_lev") |
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c = c_Mob + a4_mass * t_seri |
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! Compute coefficient "b": |
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! Heterogeneous chemistry is only at low temperature: |
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where (t_seri < 195.) |
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b = r_het_interm |
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elsewhere |
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b = 0. |
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end where |
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! Heterogeneous chemistry is only during daytime: |
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call orbite(real(julien), earth_long, trash1) |
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call zenang(earth_long, gmtime, pdtphys, rlat, rlon, pmu0, trash2) |
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forall (k = 1: nbp_lev) |
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where (pmu0 <= cos(87. / 180. * pi)) b(:, k) = 0. |
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end forall |
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b = b + a2 |
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! Midpoint method: |
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! Trial step to the midpoint: |
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dq_o3_chem = o3_prod(q, zmasse, c, b) * pdtphys / 2 |
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! "Real" step across the whole interval: |
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dq_o3_chem = o3_prod(q + dq_o3_chem, zmasse, c, b) * pdtphys |
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q = q + dq_o3_chem |
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! Confine the mass fraction: |
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q = min(max(q, 0.), .01) |
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end subroutine o3_chem |
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!************************************************* |
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function o3_prod(q, zmasse, c, b) |
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! This function computes the production rate of ozone by chemistry. |
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! All the 2-dimensional arrays are on the partial "physics" grid. |
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! Their shape is "(/klon, nbp_lev/)". |
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! Index "(i, :)" is for longitude "rlon(i)", latitude "rlat(i)". |
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use regr_pr_comb_coefoz_m, only: a6_mass |
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use assert_m, only: assert |
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use dimphy, only: klon |
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use mod_grid_phy_lmdz, only: nbp_lev |
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real, intent(in):: q(:, :) ! mass fraction of ozone |
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! "q(:, k)" is at middle of layer "k".) |
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real, intent(in):: zmasse(:, :) |
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! (column-density of mass of air in a layer, in kg m-2) |
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! ("zmasse(:, k)" is for layer "k".) |
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real, intent(in):: c(:, :) |
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! (constant term during a time step in the net mass production |
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! rate of ozone by chemistry, per unit mass of air, in s-1) |
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! "c(:, k)" is at middle of layer "k".) |
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real, intent(in):: b(:, :) |
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! (coefficient of "q" in the net mass production rate of ozone by |
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! chemistry, per unit mass of air, in s-1) |
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! ("b(:, k)" is at middle of layer "k".) |
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real o3_prod(klon, nbp_lev) |
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! (net mass production rate of ozone by chemistry, per unit mass |
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! of air, in s-1) |
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! ("o3_prod(:, k)" is at middle of layer "k".) |
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! Variables local to the procedure: |
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real sigma_mass(klon, nbp_lev) |
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! (mass column-density of ozone above point, in kg m-2) |
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! ("sigma_mass(:, k)" is at middle of layer "k".) |
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integer k |
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!------------------------------------------------------------------- |
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call assert(klon == (/size(q, 1), size(zmasse, 1), size(c, 1), & |
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size(b, 1)/), "o3_prod 1") |
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call assert(nbp_lev == (/size(q, 2), size(zmasse, 2), size(c, 2), & |
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size(b, 2)/), "o3_prod 2") |
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! Compute the column-density above the base of layer |
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! "k", and, as a first approximation, take it as column-density |
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! above the middle of layer "k": |
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sigma_mass(:, nbp_lev) = zmasse(:, nbp_lev) * q(:, nbp_lev) ! top layer |
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do k = nbp_lev - 1, 1, -1 |
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sigma_mass(:, k) = sigma_mass(:, k+1) + zmasse(:, k) * q(:, k) |
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end do |
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o3_prod = c + b * q + a6_mass * sigma_mass |
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end function o3_prod |
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end module o3_chem_m |
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