| 1 | MODULE nonoro_gwd_ran_mod |
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| 2 | |
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| 3 | IMPLICIT NONE |
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| 4 | |
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| 5 | REAL, allocatable, save :: du_nonoro_gwd(:, :) ! Zonal wind tendency due to GWD |
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| 6 | REAL, allocatable, save :: dv_nonoro_gwd(:, :) ! Meridional wind tendency due to GWD |
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| 7 | REAL, allocatable, save :: east_gwstress(:, :) ! Eastward stress profile |
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| 8 | REAL, allocatable, save :: west_gwstress(:, :) ! Westward stress profile |
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| 9 | !$OMP THREADPRIVATE(du_nonoro_gwd,dv_nonoro_gwd,east_gwstress,west_gwstress) |
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| 10 | CONTAINS |
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| 11 | |
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| 12 | SUBROUTINE nonoro_gwd_ran(ngrid, nlayer, dtime, pp, & |
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| 13 | zmax_therm, pt, pu, pv, pdt, pdu, pdv, & |
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| 14 | zustr, zvstr, d_t, d_u, d_v) |
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| 15 | |
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| 16 | !-------------------------------------------------------------------------------- |
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| 17 | ! Parametrization of the momentum flux deposition due to a discrete |
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| 18 | ! number of gravity waves. |
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| 19 | ! F. Lott |
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| 20 | ! Version 14, Gaussian distribution of the source |
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| 21 | ! LMDz model online version |
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| 22 | ! ADAPTED FOR VENUS / F. LOTT + S. LEBONNOIS |
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| 23 | ! Version adapted on 03/04/2013: |
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| 24 | ! - input flux compensated in the deepest layers |
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| 25 | ! |
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| 26 | ! ADAPTED FOR MARS G.GILLI 02/2016 |
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| 27 | ! Revision with F.Forget 06/2016 Variable EP-flux |
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| 28 | ! according to |
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| 29 | ! PBL variation (max |
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| 30 | ! velocity thermals) |
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| 31 | ! D.BARDET 01/2020 - reproductibility of |
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| 32 | ! the launching altitude |
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| 33 | ! calculation |
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| 34 | ! - wave characteristic |
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| 35 | ! calculation using MOD |
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| 36 | ! - adding east_gwstress |
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| 37 | ! and west_gwstress variables |
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| 38 | ! |
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| 39 | ! ADAPTED FOR GENERIC D.BARDET 01/2020 |
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| 40 | !--------------------------------------------------------------------------------- |
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| 41 | |
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| 42 | |
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| 43 | |
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| 44 | use comcstfi_mod, only: g, pi, cpp, r |
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| 45 | USE ioipsl_getin_p_mod, ONLY : getin_p |
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| 46 | use assert_m, only : assert |
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| 47 | use vertical_layers_mod, only : presnivs |
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| 48 | use callkeys_mod, only : epflux_max, & ! Max EP flux value at launching altitude (previous name: RUWMAX) |
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| 49 | gwd_convective_source |
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| 50 | use inifis_mod |
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| 51 | use geometry_mod, only: cell_area |
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| 52 | #ifdef CPP_XIOS |
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| 53 | use xios_output_mod, only: send_xios_field |
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| 54 | #endif |
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| 55 | implicit none |
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| 56 | |
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| 57 | ! 0. DECLARATIONS: |
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| 58 | |
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| 59 | ! 0.1 INPUTS |
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| 60 | |
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| 61 | INTEGER, intent(in):: ngrid, nlayer |
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| 62 | REAL, intent(in):: dtime ! Time step of the Physics |
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| 63 | REAL, intent(in):: zmax_therm(ngrid) ! Altitude of max velocity thermals (m) |
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| 64 | REAL, intent(in):: pp(ngrid, nlayer) ! Pressure at full levels |
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| 65 | REAL, intent(in):: pt(ngrid, nlayer) ! Temperature at full levels |
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| 66 | REAL, intent(in):: pu(ngrid, nlayer) ! Zonal wind at full levels |
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| 67 | REAL, intent(in):: pv(ngrid, nlayer) ! Meridional wind at full levels |
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| 68 | REAL, intent(in):: pdt(ngrid, nlayer) ! Tendency on temperature |
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| 69 | REAL, intent(in):: pdu(ngrid, nlayer) ! Tendency on zonal wind |
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| 70 | REAL, intent(in):: pdv(ngrid, nlayer) ! Tendency on meridional wind |
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| 71 | |
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| 72 | ! 0.2 OUTPUTS |
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| 73 | |
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| 74 | REAL, intent(out):: zustr(ngrid) ! Zonal surface stress |
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| 75 | REAL, intent(out):: zvstr(ngrid) ! Meridional surface stress |
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| 76 | REAL, intent(out):: d_t(ngrid, nlayer) ! Tendency on temperature |
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| 77 | REAL, intent(out):: d_u(ngrid, nlayer) ! Tendency on zonal wind |
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| 78 | REAL, intent(out):: d_v(ngrid, nlayer) ! Tendency on meridional wind |
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| 79 | |
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| 80 | ! 0.3 INTERNAL ARRAYS |
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| 81 | |
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| 82 | REAL :: tt(ngrid, nlayer) ! Temperature at full levels |
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| 83 | REAL :: uu(ngrid, nlayer) ! Zonal wind at full levels |
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| 84 | REAL :: vv(ngrid, nlayer) ! Meridional wind at full levels |
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| 85 | REAL :: bvlow(ngrid) ! Qu est-ce ? |
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| 86 | REAL :: dz |
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| 87 | |
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| 88 | INTEGER ii, jj, ll |
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| 89 | |
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| 90 | ! 0.3.0 Time scale of the like cycle of the waves parametrized |
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| 91 | REAL, parameter:: deltat = 24. * 3600. |
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| 92 | |
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| 93 | ! 0.3.1 Gravity waves specifications |
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| 94 | INTEGER, parameter:: nk = 2 ! number of horizontal wavenumbers |
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| 95 | INTEGER, parameter:: np = 2 ! directions (eastward and westward) phase speed |
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| 96 | INTEGER, parameter:: no = 2 ! absolute values of phase speed |
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| 97 | INTEGER, parameter:: na = 5 ! Number of realizations to get the phase speed |
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| 98 | INTEGER, parameter:: nw = nk * np *no ! Total numbers of gravity waves |
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| 99 | INTEGER jk, jp, jo, jw |
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| 100 | REAL kstar ! Control value to constrain the min horizontal wavenumber by the horizontal resolution |
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| 101 | REAL, parameter:: kmax = 1.e-4 ! Max horizontal wavenumber=N/u, u(=30) zonal wind velocity at launch |
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| 102 | !REAL, parameter:: kmax = 4.e-5 ! Max horizontal wavenumber=N/u, u(=70) zonal wind velocity at launch |
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| 103 | REAL, parameter:: kmin = 2.e-6 ! Min horizontal wavenumber=1/sqrt(DxDy) Dx and Dy horizontal grid |
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| 104 | REAL, parameter:: cmax = 30. ! Max horizontal absolute phase velocity=zonal wind at launch |
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| 105 | !REAL, parameter:: cmax = 100. ! Test for Saturn: Max horizontal absolute phase velocity |
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| 106 | !REAL, parameter:: cmax = 70. ! Test for Saturn: Max horizontal absolute phase velocity |
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| 107 | REAL, parameter:: cmin = 1. ! Min horizontal absolute phase velocity |
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| 108 | REAL cpha ! absolute phase velocity frequency |
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| 109 | REAL zk(nw, ngrid) ! horizontal wavenumber amplitude |
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| 110 | REAL zp(nw, ngrid) ! horizontal wavenumber angle |
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| 111 | REAL zo(nw, ngrid) ! absolute frequency |
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| 112 | |
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| 113 | REAL intr_freq_m(nw, ngrid) ! Waves Intr. freq. at the 1/2 lev below the full level (previous name: ZOM) |
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| 114 | REAL intr_freq_p(nw, ngrid) ! Waves Intr. freq. at the 1/2 lev above the full level (previous name: ZOP) |
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| 115 | REAL wwm(nw, ngrid) ! Wave EP-fluxes at the 1/2 level below the full level |
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| 116 | REAL wwp(nw, ngrid) ! Wave EP-fluxes at the 1/2 level above the full level |
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| 117 | REAL u_epflux_p(nw, ngrid) ! Partial zonal flux (=for each wave) at the 1/2 level above the full level (previous name: RUWP) |
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| 118 | REAL v_epflux_p(nw, ngrid) ! Partial meridional flux (=for each wave) at the 1/2 level above the full level (previous name: RVWP) |
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| 119 | REAL u_epflux_tot(ngrid, nlayer + 1) ! Total zonal flux (=for all waves (nw)) at the 1/2 level above the full level (3D) (previous name: RUW) |
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| 120 | REAL v_epflux_tot(ngrid, nlayer + 1) ! Total meridional flux (=for all waves (nw)) at the 1/2 level above the full level (3D) (previous name: RVW) |
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| 121 | REAL epflux_0(nw, ngrid) ! Fluxes at launching level (previous name: RUW0) |
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| 122 | INTEGER launch ! Launching altitude |
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| 123 | REAL, parameter:: xlaunch = 0.2 ! Control the launching altitude |
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| 124 | REAL, parameter:: zmaxth_top = 8000. ! Top of convective layer in m (approx.) |
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| 125 | |
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| 126 | REAL prec(ngrid) ! precipitations |
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| 127 | REAL prmax ! Max value of precipitation |
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| 128 | |
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| 129 | ! 0.3.2 Parameters of waves dissipations |
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| 130 | REAL, parameter:: sat = 1. ! saturation parameter |
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| 131 | REAL, parameter:: rdiss = 1. ! coefficient of dissipation |
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| 132 | REAL, parameter:: zoisec = 1.e-6 ! security for intrinsic freguency |
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| 133 | |
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| 134 | ! 0.3.3 Background flow at 1/2 levels and vertical coordinate |
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| 135 | REAL H0bis(ngrid, nlayer) ! characteristic height of the atmosphere |
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| 136 | REAL, save:: H0 ! characteristic height of the atmosphere |
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| 137 | !REAL, parameter:: pr = 250 ! Reference pressure [Pa] |
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| 138 | !REAL, parameter:: tr = 220. ! Reference temperature [K] |
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| 139 | ! TEST FOR SATURN STRATOSPHERE |
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| 140 | REAL, parameter:: pr = 110 ! Reference pressure [Pa] |
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| 141 | REAL, parameter:: tr = 130. ! Reference temperature [K] |
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| 142 | REAL zh(ngrid, nlayer + 1) ! Log-pressure altitude (constant H0) |
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| 143 | REAL zhbis(ngrid, nlayer + 1) ! Log-pressure altitude (varying H) |
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| 144 | REAL uh(ngrid, nlayer + 1) ! Zonal wind at 1/2 levels |
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| 145 | REAL vh(ngrid, nlayer + 1) ! Meridional wind at 1/2 levels |
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| 146 | REAL ph(ngrid, nlayer + 1) ! Pressure at 1/2 levels |
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| 147 | REAL, parameter:: psec = 1.e-6 ! Security to avoid division by 0 pressure |
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| 148 | REAL bv(ngrid, nlayer + 1) ! Brunt Vaisala freq. at 1/2 levels |
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| 149 | REAL, parameter:: bvsec = 1.e-5 ! Security to avoid negative BV |
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| 150 | REAL href(nlayer + 1) ! Reference altitude for launching altitude |
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| 151 | |
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| 152 | |
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| 153 | |
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| 154 | REAL ran_num_1, ran_num_2, ran_num_3 |
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| 155 | |
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| 156 | |
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| 157 | LOGICAL, save :: firstcall = .true. |
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| 158 | |
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| 159 | !-------------------------------------------------------------------------------------------------- |
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| 160 | ! 1. INITIALISATION |
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| 161 | !------------------ |
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| 162 | IF (firstcall) THEN |
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| 163 | write(*,*) "nonoro_gwd_ran: FLott non-oro GW scheme is active!" |
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| 164 | ! Characteristic vertical scale height |
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| 165 | H0 = r * tr / g |
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| 166 | ! Control |
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| 167 | if (deltat .LT. dtime) THEN |
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| 168 | call abort_physic("nonoro_gwd_ran","gwd random: deltat lower than dtime!",1) |
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| 169 | endif |
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| 170 | if (nlayer .LT. nw) THEN |
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| 171 | call abort_physic("nonoro_gwd_ran","gwd random: nlayer lower than nw!",1) |
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| 172 | endif |
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| 173 | firstcall = .false. |
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| 174 | ENDIF |
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| 175 | gwd_convective_source = .false. |
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| 176 | |
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| 177 | ! Compute subroutine's current values of temperature and winds |
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| 178 | tt(:,:) = pt(:,:) + dtime * pdt(:,:) |
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| 179 | uu(:,:) = pu(:,:) + dtime * pdu(:,:) |
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| 180 | vv(:,:) = pv(:,:) + dtime * pdv(:,:) |
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| 181 | ! print*,'epflux_max just after firstcall:', epflux_max |
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| 182 | |
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| 183 | |
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| 184 | ! 2. EVALUATION OF THE BACKGROUND FLOW AT SEMI-LEVELS |
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| 185 | !---------------------------------------------------- |
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| 186 | ! Pressure and Inv of pressure, temperature at 1/2 level |
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| 187 | DO ll = 2, nlayer |
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| 188 | ph(:, ll) = exp((log(pp(:, ll)) + log(pp(:, ll - 1))) / 2.) |
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| 189 | end DO |
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| 190 | |
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| 191 | ph(:, nlayer + 1) = 0. |
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| 192 | ph(:, 1) = 2. * pp(:, 1) - ph(:, 2) |
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| 193 | |
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| 194 | ! Launching altitude for reproductible case |
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| 195 | DO ll = 2, nlayer |
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| 196 | href(ll) = exp((log(presnivs(ll)) + log(presnivs(ll - 1))) / 2.) |
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| 197 | end DO |
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| 198 | href(nlayer + 1) = 0. |
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| 199 | href(1) = 2. * presnivs(1) - href(2) |
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| 200 | |
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| 201 | launch = 0. |
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| 202 | DO ll =1, nlayer |
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| 203 | IF (href (ll) / href(1) > xlaunch) launch = ll |
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| 204 | end DO |
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| 205 | |
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| 206 | ! Log-pressure vertical coordinate |
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| 207 | DO ll = 1, nlayer + 1 |
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| 208 | zh(:,ll) = H0 * log(pr / (ph(:,ll) + psec)) |
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| 209 | end DO |
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| 210 | |
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| 211 | ! Winds and Brunt Vaisala frequency |
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| 212 | DO ll = 2, nlayer |
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| 213 | uh(:, ll) = 0.5 * (uu(:, ll) + uu(:, ll - 1)) ! Zonal wind |
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| 214 | vh(:, ll) = 0.5 * (vv(:, ll) + vv(:, ll - 1)) ! Meridional wind |
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| 215 | |
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| 216 | bv(:, ll) = 0.5 * (tt(:, ll) + tt(:, ll - 1)) & |
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| 217 | * r**2 / cpp / H0**2 & |
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| 218 | + (tt(:, ll) - tt(:, ll - 1)) & |
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| 219 | / (zh(:, ll) - zh(:, ll - 1)) & |
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| 220 | * r / H0 |
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| 221 | bv(:, ll) = sqrt(max(bvsec, bv(:,ll))) |
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| 222 | end DO |
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| 223 | |
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| 224 | bv(:, 1) = bv(:, 2) |
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| 225 | uh(:, 1) = 0. |
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| 226 | vh(:, 1) = 0. |
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| 227 | bv(:, nlayer + 1) = bv(:, nlayer) |
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| 228 | uh(:, nlayer + 1) = uu(:, nlayer) |
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| 229 | vh(:, nlayer + 1) = vv(:, nlayer) |
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| 230 | |
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| 231 | ! 3. WAVES CHARACTERISTICS CHOSEN RANDOMLY |
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| 232 | !----------------------------------------- |
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| 233 | ! The mod function of here a weird arguments |
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| 234 | ! are used to produce the waves characteristics |
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| 235 | ! in a stochastic way |
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| 236 | DO jw = 1, nw |
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| 237 | DO ii = 1, ngrid |
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| 238 | |
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| 239 | ran_num_1 = mod(tt(ii, jw) * 10., 1.) |
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| 240 | ran_num_2 = mod(tt(ii, jw) * 100., 1.) |
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| 241 | |
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| 242 | ! angle (0 or pi so far) |
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| 243 | zp(jw, ii) = (sign(1., 0.5 - ran_num_1) & |
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| 244 | + 1.) * pi / 2. |
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| 245 | ! horizontal wavenumber amplitude |
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| 246 | ! TN+GG April/June 2020 |
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| 247 | ! "Individual waves are not supposed |
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| 248 | ! to occupy the entire domain, but |
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| 249 | ! only a faction of it" Lott+2012 |
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| 250 | |
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| 251 | !zk(jw, ii) = kmin + (kmax - kmin) * ran_num_2 |
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| 252 | kstar = pi / sqrt(cell_area(ii)) |
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| 253 | zk(jw, ii) = max(kmin,kstar) + (kmax - max(kmin,kstar)) * ran_num_2 |
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| 254 | ! horizontal phase speed |
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| 255 | cpha = 0. |
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| 256 | DO jj = 1, na |
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| 257 | ran_num_3 = mod(tt(ii, jw + 3 * jj)**2, 1.) |
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| 258 | cpha = cpha + 2. * cmax * & |
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| 259 | (ran_num_3 - 0.5) * & |
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| 260 | sqrt(3.) / sqrt(na * 1.) |
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| 261 | end DO |
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| 262 | IF (cpha < 0.) THEN |
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| 263 | cpha = - 1. * cpha |
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| 264 | zp (jw, ii) = zp(jw, ii) + pi |
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| 265 | ENDIF |
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| 266 | ! Intrinsic frequency |
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| 267 | zo(jw, ii) = cpha * zk(jw, ii) |
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| 268 | ! Intrinsic frequency is imposed |
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| 269 | zo(jw, ii) = zo(jw, ii) & |
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| 270 | + zk(jw, ii) * cos(zp(jw, ii)) * uh(ii, launch) & |
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| 271 | + zk(jw, ii) * sin(zp(jw, ii)) * vh(ii, launch) |
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| 272 | ! Momentum flux at launch level |
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| 273 | epflux_0(jw, ii) = epflux_max & |
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| 274 | * mod(100. * (uu(ii, jw)**2 + vv(ii, jw)**2), 1.) |
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| 275 | |
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| 276 | end DO |
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| 277 | end DO |
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| 278 | |
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| 279 | ! print*,'epflux_max just after waves charac. ramdon:', epflux_max |
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| 280 | ! print*,'epflux_0 just after waves charac. ramdon:', epflux_0 |
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| 281 | ! 4. COMPUTE THE FLUXES |
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| 282 | !---------------------- |
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| 283 | ! 4.1 Vertical velocity at launching altitude to ensure |
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| 284 | ! the correct value to the imposed fluxes. |
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| 285 | !------------------------------------------------------ |
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| 286 | DO jw = 1, nw |
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| 287 | ! Evaluate intrinsic frequency at launching altutide: |
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| 288 | intr_freq_p(jw, :) = zo(jw, :) & |
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| 289 | - zk(jw, :) * cos(zp(jw, :)) * uh(:, launch) & |
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| 290 | - zk(jw, :) * sin(zp(jw, :)) * vh(:, launch) |
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| 291 | end DO |
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| 292 | |
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| 293 | IF (gwd_convective_source) THEN |
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| 294 | DO jw = 1, nw |
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| 295 | ! VERSION WITH CONVECTIVE SOURCE ! designed for Earth |
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| 296 | |
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| 297 | ! Vertical velocity at launch level, value to ensure the |
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| 298 | ! imposed mmt flux factor related to the convective forcing: |
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| 299 | ! precipitations. |
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| 300 | |
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| 301 | ! tanh limitation to values above prmax: |
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| 302 | ! WWP(JW, :) = epflux_0(JW, :) & |
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| 303 | ! * (r / cpp / H0 * RLVTT * PRMAX * TANH(PREC(:) / PRMAX))**2 |
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| 304 | ! Here, we neglected the kinetic energy providing of the thermodynamic |
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| 305 | ! phase change |
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| 306 | |
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| 307 | ! |
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| 308 | |
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| 309 | ! Factor related to the characteristics of the waves: |
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| 310 | wwp(jw, :) = wwp(jw, :) * zk(jw, :)**3 / kmin / bvlow(:) & |
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| 311 | / MAX(ABS(intr_freq_p(jw, :)), zoisec)**3 |
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| 312 | |
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| 313 | ! Moderation by the depth of the source (dz here): |
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| 314 | wwp(jw, :) = wwp(jw, :) & |
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| 315 | * exp(- bvlow(:)**2 / max(abs(intr_freq_p(jw, :)), zoisec)**2 & |
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| 316 | * zk(jw, :)**2 * dz**2) |
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| 317 | |
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| 318 | ! Put the stress in the right direction: |
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| 319 | u_epflux_p(jw, :) = intr_freq_p(jw, :) / max(abs(intr_freq_p(jw, :)), zoisec)**2 & |
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| 320 | * bv(:, launch) * cos(zp(jw, :)) * wwp(jw, :)**2 |
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| 321 | v_epflux_p(JW, :) = intr_freq_p(jw, :) / max(abs(intr_freq_p(jw, :)), zoisec)**2 & |
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| 322 | * bv(:, launch) * sin(zp(jw, :)) * wwp(jw, :)**2 |
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| 323 | end DO |
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| 324 | ELSE ! VERSION WITHOUT CONVECTIVE SOURCE |
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| 325 | ! Vertical velocity at launch level, value to ensure the imposed |
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| 326 | ! mom flux: |
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| 327 | DO jw = 1, nw |
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| 328 | ! WW is directly a flux, here, not vertical velocity anymore |
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| 329 | wwp(jw, :) = epflux_0(JW,:) |
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| 330 | u_epflux_p(jw, :) = cos(zp(jw, :)) * sign(1., intr_freq_p(jw, :)) * epflux_0(jw, :) |
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| 331 | v_epflux_p(jw, :) = sin(zp(jw, :)) * sign(1., intr_freq_p(jw, :)) * epflux_0(jw, :) |
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| 332 | |
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| 333 | end DO |
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| 334 | ENDIF |
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| 335 | |
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| 336 | ! 4.2 Initial flux at launching altitude |
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| 337 | !--------------------------------------- |
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| 338 | u_epflux_tot(:, launch) = 0. |
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| 339 | v_epflux_tot(:, launch) = 0. |
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| 340 | DO jw = 1, nw |
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| 341 | u_epflux_tot(:, launch) = u_epflux_tot(:, launch) + u_epflux_p(jw, :) |
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| 342 | v_epflux_tot(:, launch) = v_epflux_tot(:, launch) + v_epflux_p(jw, :) |
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| 343 | end DO |
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| 344 | |
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| 345 | ! 4.3 Loop over altitudes, with passage from one level to the next done by: |
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| 346 | !-------------------------------------------------------------------------- |
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| 347 | ! i) conserving the EP flux, |
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| 348 | ! ii) dissipating a little, |
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| 349 | ! iii) testing critical levels, |
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| 350 | ! iv) testing the breaking. |
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| 351 | !-------------------------------------------------------------------------- |
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| 352 | DO ll = launch, nlayer - 1 |
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| 353 | ! Warning! all the physics is here (passage from one level to the next |
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| 354 | DO jw = 1, nw |
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| 355 | intr_freq_m(jw, :) = intr_freq_p(jw, :) |
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| 356 | wwm(jw, :) = wwp(jw, :) |
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| 357 | ! Intrinsic frequency |
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| 358 | intr_freq_p(jw, :) = zo(jw, :) - zk(jw, :) * cos(zp(jw, :)) * uh(:, ll + 1) & |
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| 359 | - zk(jw, :) * sin(zp(jw, :)) * vh(:, ll + 1) |
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| 360 | ! Vertical velocity in flux formulation |
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| 361 | wwp(jw, :) = min( & |
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| 362 | ! No breaking (Eq. 6): |
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| 363 | wwm(jw, :) & |
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| 364 | ! Dissipation (Eq. 8): |
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| 365 | * exp(-rdiss * pr / (ph(:, ll + 1) + ph (:, ll)) & |
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| 366 | * ((bv(:, ll + 1) + bv (:, ll)) / 2.)**3 & |
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| 367 | / max(abs(intr_freq_p(jw, :) + intr_freq_m(jw, :)) / 2., zoisec)**4 & |
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| 368 | * zk(jw, :)**3 * (zh(:, ll + 1) - zh(:, ll))) , & |
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| 369 | ! Critical levels (forced to zero if intrinsic frequency |
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| 370 | ! changes sign) |
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| 371 | max(0., sign(1., intr_freq_p(jw, :) * intr_freq_m(jw, :))) & |
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| 372 | ! Saturation (Eq. 12) |
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| 373 | * abs(intr_freq_p(jw, :))**3 / bv(:, ll + 1) & |
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| 374 | * exp(-zh(:, ll + 1) / H0) & |
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| 375 | * sat**2 * kmin**2 / zk(jw, :)**4) |
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| 376 | end DO |
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| 377 | |
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| 378 | ! Evaluate EP-flux from Eq. 7 and give the right orientation to the stress |
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| 379 | DO jw = 1, nw |
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| 380 | u_epflux_p(jw, :) = sign(1., intr_freq_p(jw, :)) * cos(zp(jw, :)) * wwp(jw, :) |
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| 381 | v_epflux_p(jw, :) = sign(1., intr_freq_p(jw, :)) * sin(zp(jw, :)) * wwp(jw, :) |
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| 382 | end DO |
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| 383 | |
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| 384 | u_epflux_tot(:, ll + 1) = 0. |
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| 385 | v_epflux_tot(:, ll + 1) = 0. |
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| 386 | DO jw = 1, nw |
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| 387 | u_epflux_tot(:, ll + 1) = u_epflux_tot(:, ll + 1) + u_epflux_p(jw, :) |
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| 388 | v_epflux_tot(:, ll + 1) = v_epflux_tot(:, ll + 1) + v_epflux_p(jw, :) |
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| 389 | east_gwstress(:, ll) = east_gwstress(:, ll) & |
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| 390 | + max(0., u_epflux_p(jw, :)) / float(nw) |
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| 391 | west_gwstress(:, ll) = west_gwstress(:, ll) & |
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| 392 | + min(0., u_epflux_p(jw, ll)) / float(nw) |
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| 393 | end DO |
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| 394 | end DO ! DO LL = LAUNCH, nlayer - 1 |
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| 395 | |
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| 396 | ! print*,'u_epflux_tot just after launching:', u_epflux_tot |
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| 397 | ! print*,'v_epflux_tot just after launching:', v_epflux_tot |
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| 398 | ! print*,'u_epflux_p just after launching:', maxval(u_epflux_p), minval(u_epflux_p) |
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| 399 | ! print*,'v_epflux_p just after launching:', maxval(v_epflux_p), minval(v_epflux_p) |
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| 400 | |
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| 401 | ! 5. TENDENCY CALCULATIONS |
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| 402 | !------------------------- |
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| 403 | ! 5.1 Flow rectification at the top and in the low layers |
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| 404 | ! -------------------------------------------------------- |
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| 405 | ! Warning, this is the total on all GW... |
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| 406 | |
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| 407 | u_epflux_tot(:, nlayer + 1) = 0. |
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| 408 | v_epflux_tot(:, nlayer + 1) = 0. |
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| 409 | |
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| 410 | ! Here, big change compared to FLott version: |
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| 411 | ! We compensate (u_epflux_(:, LAUNCH), ie total emitted upward flux |
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| 412 | ! over the layers max(1,LAUNCH-3) to LAUNCH-1 |
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| 413 | DO LL = 1, max(1,LAUNCH-3) |
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| 414 | u_epflux_tot(:, LL) = 0. |
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| 415 | v_epflux_tot(:, LL) = 0. |
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| 416 | end DO |
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| 417 | DO LL = max(2,LAUNCH-2), LAUNCH-1 |
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| 418 | u_epflux_tot(:, LL) = u_epflux_tot(:, LL - 1) & |
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| 419 | + u_epflux_tot(:, LAUNCH) * (PH(:,LL)-PH(:,LL-1)) & |
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| 420 | / (PH(:,LAUNCH)-PH(:,max(1,LAUNCH-3))) |
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| 421 | v_epflux_tot(:, LL) = v_epflux_tot(:, LL - 1) & |
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| 422 | + v_epflux_tot(:, LAUNCH) * (PH(:,LL)-PH(:,LL-1)) & |
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| 423 | / (PH(:,LAUNCH)-PH(:,max(1,LAUNCH-3))) |
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| 424 | east_gwstress(:,LL) = east_gwstress(:, LL - 1) & |
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| 425 | + east_gwstress(:, LAUNCH) * (PH(:,LL)-PH(:,LL-1)) & |
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| 426 | / (PH(:,LAUNCH)-PH(:,max(1,LAUNCH-3))) |
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| 427 | west_gwstress(:,LL) = west_gwstress(:, LL - 1) & |
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| 428 | + west_gwstress(:, LAUNCH) * (PH(:,LL)-PH(:,LL-1)) & |
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| 429 | / (PH(:,LAUNCH)-PH(:,max(1,LAUNCH-3))) |
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| 430 | end DO |
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| 431 | ! This way, the total flux from GW is zero, but there is a net transport |
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| 432 | ! (upward) that should be compensated by circulation |
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| 433 | ! and induce additional friction at the surface |
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| 434 | |
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| 435 | ! 5.2 AR-1 RECURSIVE FORMULA (13) IN VERSION 4 |
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| 436 | !--------------------------------------------- |
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| 437 | DO LL = 1, nlayer |
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| 438 | d_u(:, LL) = (u_epflux_tot(:, LL + 1) - u_epflux_tot(:, LL))! & |
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| 439 | !d_u(:, LL) = G * (u_epflux_tot(:, LL + 1) - u_epflux_tot(:, LL))! & |
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| 440 | ! / (PH(:, LL + 1) - PH(:, LL)) * DTIME |
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| 441 | d_v(:, LL) = (v_epflux_tot(:, LL + 1) - v_epflux_tot(:, LL))! & |
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| 442 | !d_v(:, LL) = G * (v_epflux_tot(:, LL + 1) - v_epflux_tot(:, LL))! & |
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| 443 | ! / (PH(:, LL + 1) - PH(:, LL)) * DTIME |
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| 444 | ENDDO |
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| 445 | d_t(:,:) = 0. |
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| 446 | |
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| 447 | ! 5.3 Update tendency of wind with the previous (and saved) values |
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| 448 | !----------------------------------------------------------------- |
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| 449 | d_u(:,:) = DTIME/DELTAT/REAL(NW) * d_u(:,:) & |
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| 450 | + (1.-DTIME/DELTAT) * du_nonoro_gwd(:,:) |
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| 451 | d_v(:,:) = DTIME/DELTAT/REAL(NW) * d_v(:,:) & |
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| 452 | + (1.-DTIME/DELTAT) * dv_nonoro_gwd(:,:) |
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| 453 | du_nonoro_gwd(:,:) = d_u(:,:) |
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| 454 | dv_nonoro_gwd(:,:) = d_v(:,:) |
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| 455 | |
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| 456 | ! print*,'u_epflux_tot just after tendency:', u_epflux_tot |
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| 457 | ! print*,'v_epflux_tot just after tendency:', v_epflux_tot |
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| 458 | ! print*,'d_u just after tendency:', maxval(d_u(:,:)), minval(d_u) |
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| 459 | ! print*,'d_v just after tendency:', maxval(d_v(:,:)), minval(d_v) |
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| 460 | ! Cosmetic: evaluation of the cumulated stress |
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| 461 | |
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| 462 | ZUSTR(:) = 0. |
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| 463 | ZVSTR(:) = 0. |
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| 464 | DO LL = 1, nlayer |
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| 465 | ZUSTR(:) = ZUSTR(:) + D_U(:, LL) !/ g * (PH(:, LL + 1) - PH(:, LL)) |
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| 466 | ZVSTR(:) = ZVSTR(:) + D_V(:, LL) !/ g * (PH(:, LL + 1) - PH(:, LL)) |
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| 467 | ENDDO |
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| 468 | |
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| 469 | #ifdef CPP_XIOS |
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| 470 | call send_xios_field("du_nonoro", d_u) |
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| 471 | call send_xios_field("dv_nonoro", d_v) |
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| 472 | call send_xios_field("east_gwstress", east_gwstress) |
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| 473 | call send_xios_field("west_gwstress", west_gwstress) |
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| 474 | #endif |
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| 475 | |
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| 476 | END SUBROUTINE nonoro_gwd_ran |
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| 477 | |
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| 478 | ! =================================================================== |
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| 479 | ! Subroutines used to write variables of memory in start files |
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| 480 | ! =================================================================== |
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| 481 | |
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| 482 | SUBROUTINE ini_nonoro_gwd_ran(ngrid,nlayer) |
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| 483 | |
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| 484 | IMPLICIT NONE |
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| 485 | |
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| 486 | INTEGER, INTENT (in) :: ngrid ! number of atmospheric columns |
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| 487 | INTEGER, INTENT (in) :: nlayer ! number of atmospheric layers |
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| 488 | |
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| 489 | allocate(du_nonoro_gwd(ngrid, nlayer)) |
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| 490 | allocate(dv_nonoro_gwd(ngrid, nlayer)) |
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| 491 | allocate(east_gwstress(ngrid, nlayer)) |
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| 492 | allocate(west_gwstress(ngrid, nlayer)) |
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| 493 | |
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| 494 | END SUBROUTINE ini_nonoro_gwd_ran |
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| 495 | ! ---------------------------------- |
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| 496 | SUBROUTINE end_nonoro_gwd_ran |
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| 497 | |
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| 498 | IMPLICIT NONE |
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| 499 | |
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| 500 | if (allocated(du_nonoro_gwd)) deallocate(du_nonoro_gwd) |
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| 501 | if (allocated(dv_nonoro_gwd)) deallocate(dv_nonoro_gwd) |
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| 502 | if (allocated(east_gwstress)) deallocate(east_gwstress) |
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| 503 | if (allocated(west_gwstress)) deallocate(west_gwstress) |
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| 504 | |
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| 505 | END SUBROUTINE end_nonoro_gwd_ran |
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| 506 | |
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| 507 | END MODULE nonoro_gwd_ran_mod |
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| 508 | |
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