[1] | 1 | SUBROUTINE flow_statistics |
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| 2 | |
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| 3 | !------------------------------------------------------------------------------! |
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[254] | 4 | ! Current revisions: |
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[1] | 5 | ! ----------------- |
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[667] | 6 | ! When advection is computed with ws-scheme, turbulent fluxes are already |
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| 7 | ! computed in the respective advection routines and buffered in arrays |
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| 8 | ! sums_xx_ws_l(). This is due to a consistent treatment of statistics with the |
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| 9 | ! numerics and to avoid unphysical kinks near the surface. |
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| 10 | ! So some if requests has to be done to dicern between fluxes from ws-scheme |
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| 11 | ! other advection schemes. |
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| 12 | ! Furthermore the computation of z_i is only done if the heat flux exceeds a |
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| 13 | ! minimum value. This affects only simulations of a neutral boundary layer and |
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| 14 | ! is due to reasons of computations in the advection scheme. |
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[392] | 15 | ! |
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[667] | 16 | ! |
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[392] | 17 | ! Former revisions: |
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| 18 | ! ----------------- |
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| 19 | ! $Id: flow_statistics.f90 668 2010-12-23 13:22:58Z suehring $ |
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| 20 | ! |
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[668] | 21 | ! 667 2010-12-23 12:06:00Z suehring/gryschka |
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| 22 | ! When advection is computed with ws-scheme, turbulent fluxes are already |
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| 23 | ! computed in the respective advection routines and buffered in arrays |
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| 24 | ! sums_xx_ws_l(). This is due to a consistent treatment of statistics with the |
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| 25 | ! numerics and to avoid unphysical kinks near the surface. |
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| 26 | ! So some if requests has to be done to dicern between fluxes from ws-scheme |
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| 27 | ! other advection schemes. |
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| 28 | ! Furthermore the computation of z_i is only done if the heat flux exceeds a |
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| 29 | ! minimum value. This affects only simulations of a neutral boundary layer and |
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| 30 | ! is due to reasons of computations in the advection scheme. |
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| 31 | ! |
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[625] | 32 | ! 624 2010-12-10 11:46:30Z heinze |
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| 33 | ! Calculation of q*2 added |
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| 34 | ! |
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[623] | 35 | ! 622 2010-12-10 08:08:13Z raasch |
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| 36 | ! optional barriers included in order to speed up collective operations |
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| 37 | ! |
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[392] | 38 | ! 388 2009-09-23 09:40:33Z raasch |
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[388] | 39 | ! Vertical profiles of potential density and hydrostatic pressure are |
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| 40 | ! calculated. |
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[343] | 41 | ! Added missing timeseries calculation of w"q"(0), moved timeseries q* to the |
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| 42 | ! end. |
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[291] | 43 | ! Temperature gradient criterion for estimating the boundary layer height |
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| 44 | ! replaced by the gradient criterion of Sullivan et al. (1998). |
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[254] | 45 | ! Output of messages replaced by message handling routine. |
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[1] | 46 | ! |
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[198] | 47 | ! 197 2008-09-16 15:29:03Z raasch |
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| 48 | ! Spline timeseries splptx etc. removed, timeseries w'u', w'v', w'q' (k=0) |
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| 49 | ! added, |
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| 50 | ! bugfix: divide sums(k,8) (e) and sums(k,34) (e*) by ngp_2dh_s_inner(k,sr) |
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| 51 | ! (like other scalars) |
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| 52 | ! |
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[139] | 53 | ! 133 2007-11-20 10:10:53Z letzel |
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| 54 | ! Vertical profiles now based on nzb_s_inner; they are divided by |
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| 55 | ! ngp_2dh_s_inner (scalars, procucts of scalars) and ngp_2dh (staggered |
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| 56 | ! velocity components and their products, procucts of scalars and velocity |
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| 57 | ! components), respectively. |
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| 58 | ! |
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[110] | 59 | ! 106 2007-08-16 14:30:26Z raasch |
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| 60 | ! Prescribed momentum fluxes at the top surface are used, |
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| 61 | ! profiles for w*p* and w"e are calculated |
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| 62 | ! |
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[98] | 63 | ! 97 2007-06-21 08:23:15Z raasch |
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| 64 | ! Statistics for ocean version (salinity, density) added, |
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| 65 | ! calculation of z_i and Deardorff velocity scale adjusted to be used with |
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| 66 | ! the ocean version |
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| 67 | ! |
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[90] | 68 | ! 87 2007-05-22 15:46:47Z raasch |
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| 69 | ! Two more arguments added to user_statistics, which is now also called for |
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| 70 | ! user-defined profiles, |
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| 71 | ! var_hom and var_sum renamed pr_palm |
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| 72 | ! |
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[83] | 73 | ! 82 2007-04-16 15:40:52Z raasch |
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| 74 | ! Cpp-directive lcmuk changed to intel_openmp_bug |
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| 75 | ! |
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[77] | 76 | ! 75 2007-03-22 09:54:05Z raasch |
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| 77 | ! Collection of time series quantities moved from routine flow_statistics to |
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| 78 | ! here, routine user_statistics is called for each statistic region, |
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| 79 | ! moisture renamed humidity |
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| 80 | ! |
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[39] | 81 | ! 19 2007-02-23 04:53:48Z raasch |
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[77] | 82 | ! fluxes at top modified (tswst, qswst) |
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[39] | 83 | ! |
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[3] | 84 | ! RCS Log replace by Id keyword, revision history cleaned up |
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| 85 | ! |
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[1] | 86 | ! Revision 1.41 2006/08/04 14:37:50 raasch |
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| 87 | ! Error removed in non-parallel part (sums_l) |
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| 88 | ! |
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| 89 | ! Revision 1.1 1997/08/11 06:15:17 raasch |
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| 90 | ! Initial revision |
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| 91 | ! |
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| 92 | ! |
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| 93 | ! Description: |
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| 94 | ! ------------ |
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| 95 | ! Compute average profiles and further average flow quantities for the different |
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| 96 | ! user-defined (sub-)regions. The region indexed 0 is the total model domain. |
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| 97 | ! |
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[132] | 98 | ! NOTE: For simplicity, nzb_s_inner and nzb_diff_s_inner are being used as a |
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| 99 | ! ---- lower vertical index for k-loops for all variables, although strictly |
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| 100 | ! speaking the k-loops would have to be split up according to the staggered |
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| 101 | ! grid. However, this implies no error since staggered velocity components are |
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| 102 | ! zero at the walls and inside buildings. |
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[1] | 103 | !------------------------------------------------------------------------------! |
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| 104 | |
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| 105 | USE arrays_3d |
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| 106 | USE cloud_parameters |
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| 107 | USE cpulog |
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| 108 | USE grid_variables |
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| 109 | USE indices |
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| 110 | USE interfaces |
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| 111 | USE pegrid |
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| 112 | USE statistics |
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| 113 | USE control_parameters |
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| 114 | |
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| 115 | IMPLICIT NONE |
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| 116 | |
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| 117 | INTEGER :: i, j, k, omp_get_thread_num, sr, tn |
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| 118 | LOGICAL :: first |
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[291] | 119 | REAL :: dptdz_threshold, height, pts, sums_l_eper, sums_l_etot, ust, & |
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| 120 | ust2, u2, vst, vst2, v2, w2, z_i(2) |
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| 121 | REAL :: dptdz(nzb+1:nzt+1) |
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[1] | 122 | REAL :: sums_ll(nzb:nzt+1,2) |
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| 123 | |
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| 124 | CALL cpu_log( log_point(10), 'flow_statistics', 'start' ) |
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| 125 | |
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| 126 | ! |
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| 127 | !-- To be on the safe side, check whether flow_statistics has already been |
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| 128 | !-- called once after the current time step |
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| 129 | IF ( flow_statistics_called ) THEN |
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[254] | 130 | |
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[274] | 131 | message_string = 'flow_statistics is called two times within one ' // & |
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| 132 | 'timestep' |
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[254] | 133 | CALL message( 'flow_statistics', 'PA0190', 1, 2, 0, 6, 0 ) |
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| 134 | |
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[1] | 135 | ENDIF |
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| 136 | |
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| 137 | ! |
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| 138 | !-- Compute statistics for each (sub-)region |
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| 139 | DO sr = 0, statistic_regions |
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| 140 | |
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| 141 | ! |
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| 142 | !-- Initialize (local) summation array |
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| 143 | sums_l = 0.0 |
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| 144 | |
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| 145 | ! |
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| 146 | !-- Store sums that have been computed in other subroutines in summation |
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| 147 | !-- array |
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| 148 | sums_l(:,11,:) = sums_l_l(:,sr,:) ! mixing length from diffusivities |
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| 149 | !-- WARNING: next line still has to be adjusted for OpenMP |
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| 150 | sums_l(:,21,0) = sums_wsts_bc_l(:,sr) ! heat flux from advec_s_bc |
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[87] | 151 | sums_l(nzb+9,pr_palm,0) = sums_divold_l(sr) ! old divergence from pres |
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| 152 | sums_l(nzb+10,pr_palm,0) = sums_divnew_l(sr) ! new divergence from pres |
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[1] | 153 | |
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[667] | 154 | ! |
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| 155 | !-- Copy the turbulent quantities, evaluated in the advection routines to |
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| 156 | !-- the local array sums_l() for further computations |
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| 157 | IF ( ws_scheme_mom ) THEN |
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| 158 | ! |
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| 159 | !-- Boundary condition for u'u' and v'v', because below the surface no |
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| 160 | !-- computation for these quantities is done. |
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| 161 | DO i = nxl, nxr |
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| 162 | DO j = nys, nyn |
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| 163 | sums_us2_ws_l(nzb_u_inner(j,i),sr) = & |
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| 164 | sums_us2_ws_l(nzb_u_inner(j,i)+1,sr) |
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| 165 | sums_vs2_ws_l(nzb_v_inner(j,i),sr) = & |
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| 166 | sums_vs2_ws_l(nzb_v_inner(j,i)+1,sr) |
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| 167 | ENDDO |
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| 168 | ENDDO |
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| 169 | ! |
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| 170 | !-- Swap the turbulent quantities evaluated in advec_ws. |
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| 171 | sums_l(:,13,0) = sums_wsus_ws_l(:,sr) ! w*u* |
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| 172 | sums_l(:,15,0) = sums_wsvs_ws_l(:,sr) ! w*v* |
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| 173 | sums_l(:,30,0) = sums_us2_ws_l(:,sr) ! u*2 |
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| 174 | sums_l(:,31,0) = sums_vs2_ws_l(:,sr) ! v*2 |
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| 175 | sums_l(:,32,0) = sums_ws2_ws_l(:,sr) ! w*2 |
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| 176 | sums_l(:,34,0) = sums_l(:,34,0) + 0.5 * & |
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| 177 | (sums_us2_ws_l(:,sr) + sums_vs2_ws_l(:,sr) & |
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| 178 | + sums_ws2_ws_l(:,sr)) ! e* |
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| 179 | DO k = nzb, nzt |
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| 180 | sums_l(nzb+5,pr_palm,0) = sums_l(nzb+5,pr_palm,0) + 0.5 * ( & |
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| 181 | sums_us2_ws_l(k,sr) + sums_vs2_ws_l(k,sr) + & |
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| 182 | sums_ws2_ws_l(k,sr)) |
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| 183 | ENDDO |
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| 184 | ENDIF |
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| 185 | IF ( ws_scheme_sca ) THEN |
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| 186 | sums_l(:,17,0) = sums_wspts_ws_l(:,sr) ! w*pts* from advec_s_ws |
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| 187 | IF ( ocean ) sums_l(:,66,0) = sums_wssas_ws_l(:,sr) ! w*sa* |
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| 188 | IF ( humidity .OR. passive_scalar ) sums_l(:,49,0) = & |
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| 189 | sums_wsqs_ws_l(:,sr) !w*q* |
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| 190 | ENDIF |
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[305] | 191 | ! |
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[1] | 192 | !-- Horizontally averaged profiles of horizontal velocities and temperature. |
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| 193 | !-- They must have been computed before, because they are already required |
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| 194 | !-- for other horizontal averages. |
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| 195 | tn = 0 |
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[667] | 196 | |
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[1] | 197 | !$OMP PARALLEL PRIVATE( i, j, k, tn ) |
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[82] | 198 | #if defined( __intel_openmp_bug ) |
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[1] | 199 | tn = omp_get_thread_num() |
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| 200 | #else |
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| 201 | !$ tn = omp_get_thread_num() |
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| 202 | #endif |
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| 203 | |
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| 204 | !$OMP DO |
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| 205 | DO i = nxl, nxr |
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| 206 | DO j = nys, nyn |
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[132] | 207 | DO k = nzb_s_inner(j,i), nzt+1 |
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[1] | 208 | sums_l(k,1,tn) = sums_l(k,1,tn) + u(k,j,i) * rmask(j,i,sr) |
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| 209 | sums_l(k,2,tn) = sums_l(k,2,tn) + v(k,j,i) * rmask(j,i,sr) |
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| 210 | sums_l(k,4,tn) = sums_l(k,4,tn) + pt(k,j,i) * rmask(j,i,sr) |
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| 211 | ENDDO |
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| 212 | ENDDO |
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| 213 | ENDDO |
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| 214 | |
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| 215 | ! |
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[96] | 216 | !-- Horizontally averaged profile of salinity |
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| 217 | IF ( ocean ) THEN |
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| 218 | !$OMP DO |
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| 219 | DO i = nxl, nxr |
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| 220 | DO j = nys, nyn |
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[132] | 221 | DO k = nzb_s_inner(j,i), nzt+1 |
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[96] | 222 | sums_l(k,23,tn) = sums_l(k,23,tn) + & |
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| 223 | sa(k,j,i) * rmask(j,i,sr) |
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| 224 | ENDDO |
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| 225 | ENDDO |
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| 226 | ENDDO |
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| 227 | ENDIF |
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| 228 | |
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| 229 | ! |
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[1] | 230 | !-- Horizontally averaged profiles of virtual potential temperature, |
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| 231 | !-- total water content, specific humidity and liquid water potential |
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| 232 | !-- temperature |
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[75] | 233 | IF ( humidity ) THEN |
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[1] | 234 | !$OMP DO |
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| 235 | DO i = nxl, nxr |
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| 236 | DO j = nys, nyn |
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[132] | 237 | DO k = nzb_s_inner(j,i), nzt+1 |
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[1] | 238 | sums_l(k,44,tn) = sums_l(k,44,tn) + & |
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| 239 | vpt(k,j,i) * rmask(j,i,sr) |
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| 240 | sums_l(k,41,tn) = sums_l(k,41,tn) + & |
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| 241 | q(k,j,i) * rmask(j,i,sr) |
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| 242 | ENDDO |
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| 243 | ENDDO |
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| 244 | ENDDO |
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| 245 | IF ( cloud_physics ) THEN |
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| 246 | !$OMP DO |
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| 247 | DO i = nxl, nxr |
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| 248 | DO j = nys, nyn |
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[132] | 249 | DO k = nzb_s_inner(j,i), nzt+1 |
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[1] | 250 | sums_l(k,42,tn) = sums_l(k,42,tn) + & |
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| 251 | ( q(k,j,i) - ql(k,j,i) ) * rmask(j,i,sr) |
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| 252 | sums_l(k,43,tn) = sums_l(k,43,tn) + ( & |
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| 253 | pt(k,j,i) + l_d_cp*pt_d_t(k) * ql(k,j,i) & |
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| 254 | ) * rmask(j,i,sr) |
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| 255 | ENDDO |
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| 256 | ENDDO |
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| 257 | ENDDO |
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| 258 | ENDIF |
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| 259 | ENDIF |
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| 260 | |
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| 261 | ! |
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| 262 | !-- Horizontally averaged profiles of passive scalar |
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| 263 | IF ( passive_scalar ) THEN |
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| 264 | !$OMP DO |
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| 265 | DO i = nxl, nxr |
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| 266 | DO j = nys, nyn |
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[132] | 267 | DO k = nzb_s_inner(j,i), nzt+1 |
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[1] | 268 | sums_l(k,41,tn) = sums_l(k,41,tn) + q(k,j,i) * rmask(j,i,sr) |
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| 269 | ENDDO |
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| 270 | ENDDO |
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| 271 | ENDDO |
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| 272 | ENDIF |
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| 273 | !$OMP END PARALLEL |
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| 274 | ! |
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| 275 | !-- Summation of thread sums |
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| 276 | IF ( threads_per_task > 1 ) THEN |
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| 277 | DO i = 1, threads_per_task-1 |
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| 278 | sums_l(:,1,0) = sums_l(:,1,0) + sums_l(:,1,i) |
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| 279 | sums_l(:,2,0) = sums_l(:,2,0) + sums_l(:,2,i) |
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| 280 | sums_l(:,4,0) = sums_l(:,4,0) + sums_l(:,4,i) |
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[96] | 281 | IF ( ocean ) THEN |
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| 282 | sums_l(:,23,0) = sums_l(:,23,0) + sums_l(:,23,i) |
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| 283 | ENDIF |
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[75] | 284 | IF ( humidity ) THEN |
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[1] | 285 | sums_l(:,41,0) = sums_l(:,41,0) + sums_l(:,41,i) |
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| 286 | sums_l(:,44,0) = sums_l(:,44,0) + sums_l(:,44,i) |
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| 287 | IF ( cloud_physics ) THEN |
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| 288 | sums_l(:,42,0) = sums_l(:,42,0) + sums_l(:,42,i) |
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| 289 | sums_l(:,43,0) = sums_l(:,43,0) + sums_l(:,43,i) |
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| 290 | ENDIF |
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| 291 | ENDIF |
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| 292 | IF ( passive_scalar ) THEN |
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| 293 | sums_l(:,41,0) = sums_l(:,41,0) + sums_l(:,41,i) |
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| 294 | ENDIF |
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| 295 | ENDDO |
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| 296 | ENDIF |
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| 297 | |
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| 298 | #if defined( __parallel ) |
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| 299 | ! |
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| 300 | !-- Compute total sum from local sums |
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[622] | 301 | IF ( collective_wait ) CALL MPI_BARRIER( comm2d, ierr ) |
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[1] | 302 | CALL MPI_ALLREDUCE( sums_l(nzb,1,0), sums(nzb,1), nzt+2-nzb, MPI_REAL, & |
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| 303 | MPI_SUM, comm2d, ierr ) |
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[622] | 304 | IF ( collective_wait ) CALL MPI_BARRIER( comm2d, ierr ) |
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[1] | 305 | CALL MPI_ALLREDUCE( sums_l(nzb,2,0), sums(nzb,2), nzt+2-nzb, MPI_REAL, & |
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| 306 | MPI_SUM, comm2d, ierr ) |
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[622] | 307 | IF ( collective_wait ) CALL MPI_BARRIER( comm2d, ierr ) |
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[1] | 308 | CALL MPI_ALLREDUCE( sums_l(nzb,4,0), sums(nzb,4), nzt+2-nzb, MPI_REAL, & |
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| 309 | MPI_SUM, comm2d, ierr ) |
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[96] | 310 | IF ( ocean ) THEN |
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[622] | 311 | IF ( collective_wait ) CALL MPI_BARRIER( comm2d, ierr ) |
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[96] | 312 | CALL MPI_ALLREDUCE( sums_l(nzb,23,0), sums(nzb,23), nzt+2-nzb, & |
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| 313 | MPI_REAL, MPI_SUM, comm2d, ierr ) |
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| 314 | ENDIF |
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[75] | 315 | IF ( humidity ) THEN |
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[622] | 316 | IF ( collective_wait ) CALL MPI_BARRIER( comm2d, ierr ) |
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[1] | 317 | CALL MPI_ALLREDUCE( sums_l(nzb,44,0), sums(nzb,44), nzt+2-nzb, & |
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| 318 | MPI_REAL, MPI_SUM, comm2d, ierr ) |
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[622] | 319 | IF ( collective_wait ) CALL MPI_BARRIER( comm2d, ierr ) |
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[1] | 320 | CALL MPI_ALLREDUCE( sums_l(nzb,41,0), sums(nzb,41), nzt+2-nzb, & |
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| 321 | MPI_REAL, MPI_SUM, comm2d, ierr ) |
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| 322 | IF ( cloud_physics ) THEN |
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[622] | 323 | IF ( collective_wait ) CALL MPI_BARRIER( comm2d, ierr ) |
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[1] | 324 | CALL MPI_ALLREDUCE( sums_l(nzb,42,0), sums(nzb,42), nzt+2-nzb, & |
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| 325 | MPI_REAL, MPI_SUM, comm2d, ierr ) |
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[622] | 326 | IF ( collective_wait ) CALL MPI_BARRIER( comm2d, ierr ) |
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[1] | 327 | CALL MPI_ALLREDUCE( sums_l(nzb,43,0), sums(nzb,43), nzt+2-nzb, & |
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| 328 | MPI_REAL, MPI_SUM, comm2d, ierr ) |
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| 329 | ENDIF |
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| 330 | ENDIF |
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| 331 | |
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| 332 | IF ( passive_scalar ) THEN |
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[622] | 333 | IF ( collective_wait ) CALL MPI_BARRIER( comm2d, ierr ) |
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[1] | 334 | CALL MPI_ALLREDUCE( sums_l(nzb,41,0), sums(nzb,41), nzt+2-nzb, & |
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| 335 | MPI_REAL, MPI_SUM, comm2d, ierr ) |
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| 336 | ENDIF |
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| 337 | #else |
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| 338 | sums(:,1) = sums_l(:,1,0) |
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| 339 | sums(:,2) = sums_l(:,2,0) |
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| 340 | sums(:,4) = sums_l(:,4,0) |
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[96] | 341 | IF ( ocean ) sums(:,23) = sums_l(:,23,0) |
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[75] | 342 | IF ( humidity ) THEN |
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[1] | 343 | sums(:,44) = sums_l(:,44,0) |
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| 344 | sums(:,41) = sums_l(:,41,0) |
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| 345 | IF ( cloud_physics ) THEN |
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| 346 | sums(:,42) = sums_l(:,42,0) |
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| 347 | sums(:,43) = sums_l(:,43,0) |
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| 348 | ENDIF |
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| 349 | ENDIF |
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| 350 | IF ( passive_scalar ) sums(:,41) = sums_l(:,41,0) |
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| 351 | #endif |
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| 352 | |
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| 353 | ! |
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| 354 | !-- Final values are obtained by division by the total number of grid points |
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| 355 | !-- used for summation. After that store profiles. |
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[132] | 356 | sums(:,1) = sums(:,1) / ngp_2dh(sr) |
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| 357 | sums(:,2) = sums(:,2) / ngp_2dh(sr) |
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| 358 | sums(:,4) = sums(:,4) / ngp_2dh_s_inner(:,sr) |
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[1] | 359 | hom(:,1,1,sr) = sums(:,1) ! u |
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| 360 | hom(:,1,2,sr) = sums(:,2) ! v |
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| 361 | hom(:,1,4,sr) = sums(:,4) ! pt |
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| 362 | |
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[667] | 363 | |
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[1] | 364 | ! |
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[96] | 365 | !-- Salinity |
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| 366 | IF ( ocean ) THEN |
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[132] | 367 | sums(:,23) = sums(:,23) / ngp_2dh_s_inner(:,sr) |
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[96] | 368 | hom(:,1,23,sr) = sums(:,23) ! sa |
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| 369 | ENDIF |
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| 370 | |
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| 371 | ! |
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[1] | 372 | !-- Humidity and cloud parameters |
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[75] | 373 | IF ( humidity ) THEN |
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[132] | 374 | sums(:,44) = sums(:,44) / ngp_2dh_s_inner(:,sr) |
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| 375 | sums(:,41) = sums(:,41) / ngp_2dh_s_inner(:,sr) |
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[1] | 376 | hom(:,1,44,sr) = sums(:,44) ! vpt |
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| 377 | hom(:,1,41,sr) = sums(:,41) ! qv (q) |
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| 378 | IF ( cloud_physics ) THEN |
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[132] | 379 | sums(:,42) = sums(:,42) / ngp_2dh_s_inner(:,sr) |
---|
| 380 | sums(:,43) = sums(:,43) / ngp_2dh_s_inner(:,sr) |
---|
[1] | 381 | hom(:,1,42,sr) = sums(:,42) ! qv |
---|
| 382 | hom(:,1,43,sr) = sums(:,43) ! pt |
---|
| 383 | ENDIF |
---|
| 384 | ENDIF |
---|
| 385 | |
---|
| 386 | ! |
---|
| 387 | !-- Passive scalar |
---|
[132] | 388 | IF ( passive_scalar ) hom(:,1,41,sr) = sums(:,41) / & |
---|
| 389 | ngp_2dh_s_inner(:,sr) ! s (q) |
---|
[1] | 390 | |
---|
| 391 | ! |
---|
| 392 | !-- Horizontally averaged profiles of the remaining prognostic variables, |
---|
| 393 | !-- variances, the total and the perturbation energy (single values in last |
---|
| 394 | !-- column of sums_l) and some diagnostic quantities. |
---|
[132] | 395 | !-- NOTE: for simplicity, nzb_s_inner is used below, although strictly |
---|
[1] | 396 | !-- ---- speaking the following k-loop would have to be split up and |
---|
| 397 | !-- rearranged according to the staggered grid. |
---|
[132] | 398 | !-- However, this implies no error since staggered velocity components |
---|
| 399 | !-- are zero at the walls and inside buildings. |
---|
[1] | 400 | tn = 0 |
---|
[82] | 401 | #if defined( __intel_openmp_bug ) |
---|
[1] | 402 | !$OMP PARALLEL PRIVATE( i, j, k, pts, sums_ll, sums_l_eper, sums_l_etot, & |
---|
| 403 | !$OMP tn, ust, ust2, u2, vst, vst2, v2, w2 ) |
---|
| 404 | tn = omp_get_thread_num() |
---|
| 405 | #else |
---|
| 406 | !$OMP PARALLEL PRIVATE( i, j, k, pts, sums_ll, sums_l_eper, sums_l_etot, tn, ust, ust2, u2, vst, vst2, v2, w2 ) |
---|
| 407 | !$ tn = omp_get_thread_num() |
---|
| 408 | #endif |
---|
| 409 | !$OMP DO |
---|
| 410 | DO i = nxl, nxr |
---|
| 411 | DO j = nys, nyn |
---|
| 412 | sums_l_etot = 0.0 |
---|
[132] | 413 | DO k = nzb_s_inner(j,i), nzt+1 |
---|
[1] | 414 | ! |
---|
| 415 | !-- Prognostic and diagnostic variables |
---|
| 416 | sums_l(k,3,tn) = sums_l(k,3,tn) + w(k,j,i) * rmask(j,i,sr) |
---|
| 417 | sums_l(k,8,tn) = sums_l(k,8,tn) + e(k,j,i) * rmask(j,i,sr) |
---|
| 418 | sums_l(k,9,tn) = sums_l(k,9,tn) + km(k,j,i) * rmask(j,i,sr) |
---|
| 419 | sums_l(k,10,tn) = sums_l(k,10,tn) + kh(k,j,i) * rmask(j,i,sr) |
---|
| 420 | sums_l(k,40,tn) = sums_l(k,40,tn) + p(k,j,i) |
---|
| 421 | |
---|
| 422 | sums_l(k,33,tn) = sums_l(k,33,tn) + & |
---|
| 423 | ( pt(k,j,i)-hom(k,1,4,sr) )**2 * rmask(j,i,sr) |
---|
[624] | 424 | |
---|
| 425 | IF ( humidity ) THEN |
---|
| 426 | sums_l(k,70,tn) = sums_l(k,70,tn) + & |
---|
| 427 | ( q(k,j,i)-hom(k,1,41,sr) )**2 * rmask(j,i,sr) |
---|
| 428 | ENDIF |
---|
[667] | 429 | |
---|
[1] | 430 | sums_l_etot = sums_l_etot + & |
---|
[667] | 431 | 0.5 * ( u(k,j,i)**2 + v(k,j,i)**2 + & |
---|
| 432 | w(k,j,i)**2 ) * rmask(j,i,sr) |
---|
[1] | 433 | ENDDO |
---|
| 434 | ! |
---|
| 435 | !-- Total and perturbation energy for the total domain (being |
---|
| 436 | !-- collected in the last column of sums_l). Summation of these |
---|
| 437 | !-- quantities is seperated from the previous loop in order to |
---|
| 438 | !-- allow vectorization of that loop. |
---|
[87] | 439 | sums_l(nzb+4,pr_palm,tn) = sums_l(nzb+4,pr_palm,tn) + sums_l_etot |
---|
[1] | 440 | ! |
---|
| 441 | !-- 2D-arrays (being collected in the last column of sums_l) |
---|
[87] | 442 | sums_l(nzb,pr_palm,tn) = sums_l(nzb,pr_palm,tn) + & |
---|
[1] | 443 | us(j,i) * rmask(j,i,sr) |
---|
[87] | 444 | sums_l(nzb+1,pr_palm,tn) = sums_l(nzb+1,pr_palm,tn) + & |
---|
[1] | 445 | usws(j,i) * rmask(j,i,sr) |
---|
[87] | 446 | sums_l(nzb+2,pr_palm,tn) = sums_l(nzb+2,pr_palm,tn) + & |
---|
[1] | 447 | vsws(j,i) * rmask(j,i,sr) |
---|
[87] | 448 | sums_l(nzb+3,pr_palm,tn) = sums_l(nzb+3,pr_palm,tn) + & |
---|
[1] | 449 | ts(j,i) * rmask(j,i,sr) |
---|
[197] | 450 | IF ( humidity ) THEN |
---|
| 451 | sums_l(nzb+12,pr_palm,tn) = sums_l(nzb+12,pr_palm,tn) + & |
---|
| 452 | qs(j,i) * rmask(j,i,sr) |
---|
| 453 | ENDIF |
---|
[1] | 454 | ENDDO |
---|
| 455 | ENDDO |
---|
| 456 | |
---|
| 457 | ! |
---|
[667] | 458 | !-- Computation of statistics when ws-scheme is not used. Else these |
---|
| 459 | !-- quantities are evaluated in the advection routines. |
---|
| 460 | IF ( .NOT. ws_scheme_mom ) THEN |
---|
| 461 | !$OMP DO |
---|
| 462 | DO i = nxl, nxr |
---|
| 463 | DO j = nys, nyn |
---|
| 464 | sums_l_eper = 0.0 |
---|
| 465 | DO k = nzb_s_inner(j,i), nzt+1 |
---|
| 466 | u2 = u(k,j,i)**2 |
---|
| 467 | v2 = v(k,j,i)**2 |
---|
| 468 | w2 = w(k,j,i)**2 |
---|
| 469 | ust2 = ( u(k,j,i) - hom(k,1,1,sr) )**2 |
---|
| 470 | vst2 = ( v(k,j,i) - hom(k,1,2,sr) )**2 |
---|
| 471 | |
---|
| 472 | sums_l(k,30,tn) = sums_l(k,30,tn) + ust2 * rmask(j,i,sr) |
---|
| 473 | sums_l(k,31,tn) = sums_l(k,31,tn) + vst2 * rmask(j,i,sr) |
---|
| 474 | sums_l(k,32,tn) = sums_l(k,32,tn) + w2 * rmask(j,i,sr) |
---|
| 475 | ! |
---|
| 476 | !-- Higher moments |
---|
| 477 | !-- (Computation of the skewness of w further below) |
---|
| 478 | sums_l(k,38,tn) = sums_l(k,38,tn) + w(k,j,i) * w2 * & |
---|
| 479 | rmask(j,i,sr) |
---|
| 480 | ! |
---|
| 481 | !-- Perturbation energy |
---|
| 482 | |
---|
| 483 | sums_l(k,34,tn) = sums_l(k,34,tn) + 0.5 * & |
---|
| 484 | ( ust2 + vst2 + w2 ) * rmask(j,i,sr) |
---|
| 485 | sums_l_eper = sums_l_eper + & |
---|
| 486 | 0.5 * ( ust2+vst2+w2 ) * rmask(j,i,sr) |
---|
| 487 | |
---|
| 488 | ENDDO |
---|
| 489 | sums_l(nzb+5,pr_palm,tn) = sums_l(nzb+5,pr_palm,tn) & |
---|
| 490 | + sums_l_eper |
---|
| 491 | ENDDO |
---|
| 492 | ENDDO |
---|
| 493 | ELSE |
---|
| 494 | !$OMP DO |
---|
| 495 | DO i = nxl, nxr |
---|
| 496 | DO j = nys, nyn |
---|
| 497 | DO k = nzb_s_inner(j,i), nzt + 1 |
---|
| 498 | w2 = w(k,j,i)**2 |
---|
| 499 | ! |
---|
| 500 | !-- Higher moments |
---|
| 501 | !-- (Computation of the skewness of w further below) |
---|
| 502 | sums_l(k,38,tn) = sums_l(k,38,tn) + w(k,j,i) * w2 * & |
---|
| 503 | rmask(j,i,sr) |
---|
| 504 | ENDDO |
---|
| 505 | ENDDO |
---|
| 506 | ENDDO |
---|
| 507 | ENDIF |
---|
| 508 | |
---|
| 509 | ! |
---|
[1] | 510 | !-- Horizontally averaged profiles of the vertical fluxes |
---|
[667] | 511 | |
---|
[1] | 512 | !$OMP DO |
---|
| 513 | DO i = nxl, nxr |
---|
| 514 | DO j = nys, nyn |
---|
| 515 | ! |
---|
| 516 | !-- Subgridscale fluxes (without Prandtl layer from k=nzb, |
---|
| 517 | !-- oterwise from k=nzb+1) |
---|
[132] | 518 | !-- NOTE: for simplicity, nzb_diff_s_inner is used below, although |
---|
[1] | 519 | !-- ---- strictly speaking the following k-loop would have to be |
---|
| 520 | !-- split up according to the staggered grid. |
---|
[132] | 521 | !-- However, this implies no error since staggered velocity |
---|
| 522 | !-- components are zero at the walls and inside buildings. |
---|
| 523 | |
---|
| 524 | DO k = nzb_diff_s_inner(j,i)-1, nzt_diff |
---|
[1] | 525 | ! |
---|
| 526 | !-- Momentum flux w"u" |
---|
| 527 | sums_l(k,12,tn) = sums_l(k,12,tn) - 0.25 * ( & |
---|
| 528 | km(k,j,i)+km(k+1,j,i)+km(k,j,i-1)+km(k+1,j,i-1) & |
---|
| 529 | ) * ( & |
---|
| 530 | ( u(k+1,j,i) - u(k,j,i) ) * ddzu(k+1) & |
---|
| 531 | + ( w(k,j,i) - w(k,j,i-1) ) * ddx & |
---|
| 532 | ) * rmask(j,i,sr) |
---|
| 533 | ! |
---|
| 534 | !-- Momentum flux w"v" |
---|
| 535 | sums_l(k,14,tn) = sums_l(k,14,tn) - 0.25 * ( & |
---|
| 536 | km(k,j,i)+km(k+1,j,i)+km(k,j-1,i)+km(k+1,j-1,i) & |
---|
| 537 | ) * ( & |
---|
| 538 | ( v(k+1,j,i) - v(k,j,i) ) * ddzu(k+1) & |
---|
| 539 | + ( w(k,j,i) - w(k,j-1,i) ) * ddy & |
---|
| 540 | ) * rmask(j,i,sr) |
---|
| 541 | ! |
---|
| 542 | !-- Heat flux w"pt" |
---|
| 543 | sums_l(k,16,tn) = sums_l(k,16,tn) & |
---|
| 544 | - 0.5 * ( kh(k,j,i) + kh(k+1,j,i) ) & |
---|
| 545 | * ( pt(k+1,j,i) - pt(k,j,i) ) & |
---|
| 546 | * ddzu(k+1) * rmask(j,i,sr) |
---|
| 547 | |
---|
| 548 | |
---|
| 549 | ! |
---|
[96] | 550 | !-- Salinity flux w"sa" |
---|
| 551 | IF ( ocean ) THEN |
---|
| 552 | sums_l(k,65,tn) = sums_l(k,65,tn) & |
---|
| 553 | - 0.5 * ( kh(k,j,i) + kh(k+1,j,i) ) & |
---|
| 554 | * ( sa(k+1,j,i) - sa(k,j,i) ) & |
---|
| 555 | * ddzu(k+1) * rmask(j,i,sr) |
---|
| 556 | ENDIF |
---|
| 557 | |
---|
| 558 | ! |
---|
[1] | 559 | !-- Buoyancy flux, water flux (humidity flux) w"q" |
---|
[75] | 560 | IF ( humidity ) THEN |
---|
[1] | 561 | sums_l(k,45,tn) = sums_l(k,45,tn) & |
---|
| 562 | - 0.5 * ( kh(k,j,i) + kh(k+1,j,i) ) & |
---|
| 563 | * ( vpt(k+1,j,i) - vpt(k,j,i) ) & |
---|
| 564 | * ddzu(k+1) * rmask(j,i,sr) |
---|
| 565 | sums_l(k,48,tn) = sums_l(k,48,tn) & |
---|
| 566 | - 0.5 * ( kh(k,j,i) + kh(k+1,j,i) ) & |
---|
| 567 | * ( q(k+1,j,i) - q(k,j,i) ) & |
---|
| 568 | * ddzu(k+1) * rmask(j,i,sr) |
---|
| 569 | IF ( cloud_physics ) THEN |
---|
| 570 | sums_l(k,51,tn) = sums_l(k,51,tn) & |
---|
| 571 | - 0.5 * ( kh(k,j,i) + kh(k+1,j,i) ) & |
---|
| 572 | * ( ( q(k+1,j,i) - ql(k+1,j,i) )& |
---|
| 573 | - ( q(k,j,i) - ql(k,j,i) ) ) & |
---|
| 574 | * ddzu(k+1) * rmask(j,i,sr) |
---|
| 575 | ENDIF |
---|
| 576 | ENDIF |
---|
| 577 | |
---|
| 578 | ! |
---|
| 579 | !-- Passive scalar flux |
---|
| 580 | IF ( passive_scalar ) THEN |
---|
| 581 | sums_l(k,48,tn) = sums_l(k,48,tn) & |
---|
| 582 | - 0.5 * ( kh(k,j,i) + kh(k+1,j,i) ) & |
---|
| 583 | * ( q(k+1,j,i) - q(k,j,i) ) & |
---|
| 584 | * ddzu(k+1) * rmask(j,i,sr) |
---|
| 585 | ENDIF |
---|
| 586 | |
---|
| 587 | ENDDO |
---|
| 588 | |
---|
| 589 | ! |
---|
| 590 | !-- Subgridscale fluxes in the Prandtl layer |
---|
| 591 | IF ( use_surface_fluxes ) THEN |
---|
| 592 | sums_l(nzb,12,tn) = sums_l(nzb,12,tn) + & |
---|
| 593 | usws(j,i) * rmask(j,i,sr) ! w"u" |
---|
| 594 | sums_l(nzb,14,tn) = sums_l(nzb,14,tn) + & |
---|
| 595 | vsws(j,i) * rmask(j,i,sr) ! w"v" |
---|
| 596 | sums_l(nzb,16,tn) = sums_l(nzb,16,tn) + & |
---|
| 597 | shf(j,i) * rmask(j,i,sr) ! w"pt" |
---|
| 598 | sums_l(nzb,58,tn) = sums_l(nzb,58,tn) + & |
---|
| 599 | 0.0 * rmask(j,i,sr) ! u"pt" |
---|
| 600 | sums_l(nzb,61,tn) = sums_l(nzb,61,tn) + & |
---|
| 601 | 0.0 * rmask(j,i,sr) ! v"pt" |
---|
[96] | 602 | IF ( ocean ) THEN |
---|
| 603 | sums_l(nzb,65,tn) = sums_l(nzb,65,tn) + & |
---|
| 604 | saswsb(j,i) * rmask(j,i,sr) ! w"sa" |
---|
| 605 | ENDIF |
---|
[75] | 606 | IF ( humidity ) THEN |
---|
[1] | 607 | sums_l(nzb,48,tn) = sums_l(nzb,48,tn) + & |
---|
| 608 | qsws(j,i) * rmask(j,i,sr) ! w"q" (w"qv") |
---|
| 609 | IF ( cloud_physics ) THEN |
---|
| 610 | sums_l(nzb,45,tn) = sums_l(nzb,45,tn) + ( & |
---|
| 611 | ( 1.0 + 0.61 * q(nzb,j,i) ) * & |
---|
| 612 | shf(j,i) + 0.61 * pt(nzb,j,i) * & |
---|
| 613 | qsws(j,i) & |
---|
| 614 | ) |
---|
| 615 | ! |
---|
| 616 | !-- Formula does not work if ql(nzb) /= 0.0 |
---|
| 617 | sums_l(nzb,51,tn) = sums_l(nzb,51,tn) + & ! w"q" (w"qv") |
---|
| 618 | qsws(j,i) * rmask(j,i,sr) |
---|
| 619 | ENDIF |
---|
| 620 | ENDIF |
---|
| 621 | IF ( passive_scalar ) THEN |
---|
| 622 | sums_l(nzb,48,tn) = sums_l(nzb,48,tn) + & |
---|
| 623 | qsws(j,i) * rmask(j,i,sr) ! w"q" (w"qv") |
---|
| 624 | ENDIF |
---|
| 625 | ENDIF |
---|
| 626 | |
---|
| 627 | ! |
---|
[19] | 628 | !-- Subgridscale fluxes at the top surface |
---|
| 629 | IF ( use_top_fluxes ) THEN |
---|
[550] | 630 | sums_l(nzt:nzt+1,12,tn) = sums_l(nzt:nzt+1,12,tn) + & |
---|
[102] | 631 | uswst(j,i) * rmask(j,i,sr) ! w"u" |
---|
[550] | 632 | sums_l(nzt:nzt+1,14,tn) = sums_l(nzt:nzt+1,14,tn) + & |
---|
[102] | 633 | vswst(j,i) * rmask(j,i,sr) ! w"v" |
---|
[550] | 634 | sums_l(nzt:nzt+1,16,tn) = sums_l(nzt:nzt+1,16,tn) + & |
---|
[19] | 635 | tswst(j,i) * rmask(j,i,sr) ! w"pt" |
---|
[550] | 636 | sums_l(nzt:nzt+1,58,tn) = sums_l(nzt:nzt+1,58,tn) + & |
---|
[19] | 637 | 0.0 * rmask(j,i,sr) ! u"pt" |
---|
[550] | 638 | sums_l(nzt:nzt+1,61,tn) = sums_l(nzt:nzt+1,61,tn) + & |
---|
| 639 | 0.0 * rmask(j,i,sr) ! v"pt" |
---|
| 640 | |
---|
[96] | 641 | IF ( ocean ) THEN |
---|
| 642 | sums_l(nzt,65,tn) = sums_l(nzt,65,tn) + & |
---|
| 643 | saswst(j,i) * rmask(j,i,sr) ! w"sa" |
---|
| 644 | ENDIF |
---|
[75] | 645 | IF ( humidity ) THEN |
---|
[19] | 646 | sums_l(nzt,48,tn) = sums_l(nzt,48,tn) + & |
---|
[388] | 647 | qswst(j,i) * rmask(j,i,sr) ! w"q" (w"qv") |
---|
[19] | 648 | IF ( cloud_physics ) THEN |
---|
| 649 | sums_l(nzt,45,tn) = sums_l(nzt,45,tn) + ( & |
---|
| 650 | ( 1.0 + 0.61 * q(nzt,j,i) ) * & |
---|
| 651 | tswst(j,i) + 0.61 * pt(nzt,j,i) * & |
---|
| 652 | qsws(j,i) & |
---|
| 653 | ) |
---|
| 654 | ! |
---|
| 655 | !-- Formula does not work if ql(nzb) /= 0.0 |
---|
| 656 | sums_l(nzt,51,tn) = sums_l(nzt,51,tn) + & ! w"q" (w"qv") |
---|
| 657 | qswst(j,i) * rmask(j,i,sr) |
---|
| 658 | ENDIF |
---|
| 659 | ENDIF |
---|
| 660 | IF ( passive_scalar ) THEN |
---|
| 661 | sums_l(nzt,48,tn) = sums_l(nzt,48,tn) + & |
---|
[388] | 662 | qswst(j,i) * rmask(j,i,sr) ! w"q" (w"qv") |
---|
[19] | 663 | ENDIF |
---|
| 664 | ENDIF |
---|
| 665 | |
---|
| 666 | ! |
---|
[1] | 667 | !-- Resolved fluxes (can be computed for all horizontal points) |
---|
[132] | 668 | !-- NOTE: for simplicity, nzb_s_inner is used below, although strictly |
---|
[1] | 669 | !-- ---- speaking the following k-loop would have to be split up and |
---|
| 670 | !-- rearranged according to the staggered grid. |
---|
[132] | 671 | DO k = nzb_s_inner(j,i), nzt |
---|
[1] | 672 | ust = 0.5 * ( u(k,j,i) - hom(k,1,1,sr) + & |
---|
| 673 | u(k+1,j,i) - hom(k+1,1,1,sr) ) |
---|
| 674 | vst = 0.5 * ( v(k,j,i) - hom(k,1,2,sr) + & |
---|
| 675 | v(k+1,j,i) - hom(k+1,1,2,sr) ) |
---|
| 676 | pts = 0.5 * ( pt(k,j,i) - hom(k,1,4,sr) + & |
---|
| 677 | pt(k+1,j,i) - hom(k+1,1,4,sr) ) |
---|
[667] | 678 | |
---|
[1] | 679 | !-- Higher moments |
---|
| 680 | sums_l(k,35,tn) = sums_l(k,35,tn) + pts * w(k,j,i)**2 * & |
---|
| 681 | rmask(j,i,sr) |
---|
| 682 | sums_l(k,36,tn) = sums_l(k,36,tn) + pts**2 * w(k,j,i) * & |
---|
| 683 | rmask(j,i,sr) |
---|
| 684 | |
---|
| 685 | ! |
---|
[96] | 686 | !-- Salinity flux and density (density does not belong to here, |
---|
[97] | 687 | !-- but so far there is no other suitable place to calculate) |
---|
[96] | 688 | IF ( ocean ) THEN |
---|
[667] | 689 | IF( .NOT. ws_scheme_sca ) THEN |
---|
| 690 | pts = 0.5 * ( sa(k,j,i) - hom(k,1,23,sr) + & |
---|
[96] | 691 | sa(k+1,j,i) - hom(k+1,1,23,sr) ) |
---|
[667] | 692 | sums_l(k,66,tn) = sums_l(k,66,tn) + pts * w(k,j,i) * & |
---|
[96] | 693 | rmask(j,i,sr) |
---|
[667] | 694 | ENDIF |
---|
[96] | 695 | sums_l(k,64,tn) = sums_l(k,64,tn) + rho(k,j,i) * & |
---|
| 696 | rmask(j,i,sr) |
---|
[388] | 697 | sums_l(k,71,tn) = sums_l(k,71,tn) + prho(k,j,i) * & |
---|
| 698 | rmask(j,i,sr) |
---|
[96] | 699 | ENDIF |
---|
| 700 | |
---|
| 701 | ! |
---|
[1] | 702 | !-- Buoyancy flux, water flux, humidity flux and liquid water |
---|
| 703 | !-- content |
---|
[75] | 704 | IF ( humidity ) THEN |
---|
[1] | 705 | pts = 0.5 * ( vpt(k,j,i) - hom(k,1,44,sr) + & |
---|
| 706 | vpt(k+1,j,i) - hom(k+1,1,44,sr) ) |
---|
| 707 | sums_l(k,46,tn) = sums_l(k,46,tn) + pts * w(k,j,i) * & |
---|
| 708 | rmask(j,i,sr) |
---|
[667] | 709 | |
---|
[1] | 710 | IF ( cloud_physics .OR. cloud_droplets ) THEN |
---|
| 711 | pts = 0.5 * & |
---|
| 712 | ( ( q(k,j,i) - ql(k,j,i) ) - hom(k,1,42,sr) & |
---|
| 713 | + ( q(k+1,j,i) - ql(k+1,j,i) ) - hom(k+1,1,42,sr) ) |
---|
| 714 | sums_l(k,52,tn) = sums_l(k,52,tn) + pts * w(k,j,i) * & |
---|
| 715 | rmask(j,i,sr) |
---|
| 716 | sums_l(k,54,tn) = sums_l(k,54,tn) + ql(k,j,i) * & |
---|
| 717 | rmask(j,i,sr) |
---|
| 718 | ENDIF |
---|
| 719 | ENDIF |
---|
| 720 | |
---|
| 721 | ! |
---|
| 722 | !-- Passive scalar flux |
---|
[667] | 723 | IF ( passive_scalar .AND. ( .NOT. ws_scheme_sca )) THEN |
---|
[1] | 724 | pts = 0.5 * ( q(k,j,i) - hom(k,1,41,sr) + & |
---|
| 725 | q(k+1,j,i) - hom(k+1,1,41,sr) ) |
---|
| 726 | sums_l(k,49,tn) = sums_l(k,49,tn) + pts * w(k,j,i) * & |
---|
| 727 | rmask(j,i,sr) |
---|
| 728 | ENDIF |
---|
| 729 | |
---|
| 730 | ! |
---|
| 731 | !-- Energy flux w*e* |
---|
[667] | 732 | !-- has to be adjusted |
---|
| 733 | sums_l(k,37,tn) = sums_l(k,37,tn) + w(k,j,i) * 0.5 * & |
---|
| 734 | ( ust**2 + vst**2 + w(k,j,i)**2 )& |
---|
| 735 | * rmask(j,i,sr) |
---|
[1] | 736 | ENDDO |
---|
| 737 | ENDDO |
---|
| 738 | ENDDO |
---|
[667] | 739 | !- for reasons of speed optimization the loop is splitted, to avoid if-else |
---|
| 740 | !- statements inside the loop |
---|
| 741 | !- Fluxes which have been computed in part directly inside the advection routines |
---|
| 742 | !- treated seperatly. |
---|
| 743 | !- First treat the momentum fluxes |
---|
| 744 | IF ( .NOT. ws_scheme_mom ) THEN |
---|
| 745 | !$OMP DO |
---|
| 746 | DO i = nxl, nxr |
---|
| 747 | DO j = nys, nyn |
---|
| 748 | DO k = nzb_diff_s_inner(j,i)-1, nzt_diff |
---|
| 749 | ust = 0.5 * ( u(k,j,i) - hom(k,1,1,sr) + & |
---|
| 750 | u(k+1,j,i) - hom(k+1,1,1,sr) ) |
---|
| 751 | vst = 0.5 * ( v(k,j,i) - hom(k,1,2,sr) + & |
---|
| 752 | v(k+1,j,i) - hom(k+1,1,2,sr) ) |
---|
| 753 | ! |
---|
| 754 | !-- Momentum flux w*u* |
---|
| 755 | sums_l(k,13,tn) = sums_l(k,13,tn) + 0.5 * & |
---|
| 756 | ( w(k,j,i-1) + w(k,j,i) ) & |
---|
| 757 | * ust * rmask(j,i,sr) |
---|
| 758 | ! |
---|
| 759 | !-- Momentum flux w*v* |
---|
| 760 | sums_l(k,15,tn) = sums_l(k,15,tn) + 0.5 * & |
---|
| 761 | ( w(k,j-1,i) + w(k,j,i) ) & |
---|
| 762 | * vst * rmask(j,i,sr) |
---|
| 763 | ENDDO |
---|
| 764 | ENDDO |
---|
| 765 | ENDDO |
---|
[1] | 766 | |
---|
[667] | 767 | ENDIF |
---|
| 768 | IF ( .NOT. ws_scheme_sca ) THEN |
---|
| 769 | !$OMP DO |
---|
| 770 | DO i = nxl, nxr |
---|
| 771 | DO j = nys, nyn |
---|
| 772 | DO k = nzb_diff_s_inner(j,i) - 1, nzt_diff |
---|
| 773 | !- vertical heat flux |
---|
| 774 | sums_l(k,17,tn) = sums_l(k,17,tn) + 0.5 * & |
---|
| 775 | ( pt(k,j,i) - hom(k,1,4,sr) + & |
---|
| 776 | pt(k+1,j,i) - hom(k+1,1,4,sr) ) & |
---|
| 777 | * w(k,j,i) * rmask(j,i,sr) |
---|
| 778 | IF ( humidity ) THEN |
---|
| 779 | pts = 0.5 * ( q(k,j,i) - hom(k,1,41,sr) + & |
---|
| 780 | q(k+1,j,i) - hom(k+1,1,41,sr) ) |
---|
| 781 | sums_l(k,49,tn) = sums_l(k,49,tn) + pts * w(k,j,i) * & |
---|
| 782 | rmask(j,i,sr) |
---|
| 783 | ENDIF |
---|
| 784 | ENDDO |
---|
| 785 | ENDDO |
---|
| 786 | ENDDO |
---|
| 787 | |
---|
| 788 | ENDIF |
---|
| 789 | |
---|
| 790 | |
---|
[1] | 791 | ! |
---|
[97] | 792 | !-- Density at top follows Neumann condition |
---|
[388] | 793 | IF ( ocean ) THEN |
---|
| 794 | sums_l(nzt+1,64,tn) = sums_l(nzt,64,tn) |
---|
| 795 | sums_l(nzt+1,71,tn) = sums_l(nzt,71,tn) |
---|
| 796 | ENDIF |
---|
[97] | 797 | |
---|
| 798 | ! |
---|
[1] | 799 | !-- Divergence of vertical flux of resolved scale energy and pressure |
---|
[106] | 800 | !-- fluctuations as well as flux of pressure fluctuation itself (68). |
---|
| 801 | !-- First calculate the products, then the divergence. |
---|
[1] | 802 | !-- Calculation is time consuming. Do it only, if profiles shall be plotted. |
---|
[106] | 803 | IF ( hom(nzb+1,2,55,0) /= 0.0 .OR. hom(nzb+1,2,68,0) /= 0.0 ) THEN |
---|
[1] | 804 | |
---|
| 805 | sums_ll = 0.0 ! local array |
---|
| 806 | |
---|
| 807 | !$OMP DO |
---|
| 808 | DO i = nxl, nxr |
---|
| 809 | DO j = nys, nyn |
---|
[132] | 810 | DO k = nzb_s_inner(j,i)+1, nzt |
---|
[1] | 811 | |
---|
| 812 | sums_ll(k,1) = sums_ll(k,1) + 0.5 * w(k,j,i) * ( & |
---|
| 813 | ( 0.25 * ( u(k,j,i)+u(k+1,j,i)+u(k,j,i+1)+u(k+1,j,i+1) & |
---|
| 814 | - 2.0 * ( hom(k,1,1,sr) + hom(k+1,1,1,sr) ) & |
---|
| 815 | ) )**2 & |
---|
| 816 | + ( 0.25 * ( v(k,j,i)+v(k+1,j,i)+v(k,j+1,i)+v(k+1,j+1,i) & |
---|
| 817 | - 2.0 * ( hom(k,1,2,sr) + hom(k+1,1,2,sr) ) & |
---|
| 818 | ) )**2 & |
---|
| 819 | + w(k,j,i)**2 ) |
---|
| 820 | |
---|
| 821 | sums_ll(k,2) = sums_ll(k,2) + 0.5 * w(k,j,i) & |
---|
| 822 | * ( p(k,j,i) + p(k+1,j,i) ) |
---|
| 823 | |
---|
| 824 | ENDDO |
---|
| 825 | ENDDO |
---|
| 826 | ENDDO |
---|
| 827 | sums_ll(0,1) = 0.0 ! because w is zero at the bottom |
---|
| 828 | sums_ll(nzt+1,1) = 0.0 |
---|
| 829 | sums_ll(0,2) = 0.0 |
---|
| 830 | sums_ll(nzt+1,2) = 0.0 |
---|
| 831 | |
---|
[132] | 832 | DO k = nzb_s_inner(j,i)+1, nzt |
---|
[1] | 833 | sums_l(k,55,tn) = ( sums_ll(k,1) - sums_ll(k-1,1) ) * ddzw(k) |
---|
| 834 | sums_l(k,56,tn) = ( sums_ll(k,2) - sums_ll(k-1,2) ) * ddzw(k) |
---|
[106] | 835 | sums_l(k,68,tn) = sums_ll(k,2) |
---|
[1] | 836 | ENDDO |
---|
| 837 | sums_l(nzb,55,tn) = sums_l(nzb+1,55,tn) |
---|
| 838 | sums_l(nzb,56,tn) = sums_l(nzb+1,56,tn) |
---|
[106] | 839 | sums_l(nzb,68,tn) = 0.0 ! because w* = 0 at nzb |
---|
[1] | 840 | |
---|
| 841 | ENDIF |
---|
| 842 | |
---|
| 843 | ! |
---|
[106] | 844 | !-- Divergence of vertical flux of SGS TKE and the flux itself (69) |
---|
| 845 | IF ( hom(nzb+1,2,57,0) /= 0.0 .OR. hom(nzb+1,2,69,0) /= 0.0 ) THEN |
---|
[1] | 846 | |
---|
| 847 | !$OMP DO |
---|
| 848 | DO i = nxl, nxr |
---|
| 849 | DO j = nys, nyn |
---|
[132] | 850 | DO k = nzb_s_inner(j,i)+1, nzt |
---|
[1] | 851 | |
---|
[106] | 852 | sums_l(k,57,tn) = sums_l(k,57,tn) - 0.5 * ( & |
---|
[1] | 853 | (km(k,j,i)+km(k+1,j,i)) * (e(k+1,j,i)-e(k,j,i)) * ddzu(k+1) & |
---|
| 854 | - (km(k-1,j,i)+km(k,j,i)) * (e(k,j,i)-e(k-1,j,i)) * ddzu(k) & |
---|
[106] | 855 | ) * ddzw(k) |
---|
[1] | 856 | |
---|
[106] | 857 | sums_l(k,69,tn) = sums_l(k,69,tn) - 0.5 * ( & |
---|
| 858 | (km(k,j,i)+km(k+1,j,i)) * (e(k+1,j,i)-e(k,j,i)) * ddzu(k+1) & |
---|
| 859 | ) |
---|
| 860 | |
---|
[1] | 861 | ENDDO |
---|
| 862 | ENDDO |
---|
| 863 | ENDDO |
---|
| 864 | sums_l(nzb,57,tn) = sums_l(nzb+1,57,tn) |
---|
[106] | 865 | sums_l(nzb,69,tn) = sums_l(nzb+1,69,tn) |
---|
[1] | 866 | |
---|
| 867 | ENDIF |
---|
| 868 | |
---|
| 869 | ! |
---|
| 870 | !-- Horizontal heat fluxes (subgrid, resolved, total). |
---|
| 871 | !-- Do it only, if profiles shall be plotted. |
---|
| 872 | IF ( hom(nzb+1,2,58,0) /= 0.0 ) THEN |
---|
| 873 | |
---|
| 874 | !$OMP DO |
---|
| 875 | DO i = nxl, nxr |
---|
| 876 | DO j = nys, nyn |
---|
[132] | 877 | DO k = nzb_s_inner(j,i)+1, nzt |
---|
[1] | 878 | ! |
---|
| 879 | !-- Subgrid horizontal heat fluxes u"pt", v"pt" |
---|
| 880 | sums_l(k,58,tn) = sums_l(k,58,tn) - 0.5 * & |
---|
| 881 | ( kh(k,j,i) + kh(k,j,i-1) ) & |
---|
| 882 | * ( pt(k,j,i-1) - pt(k,j,i) ) & |
---|
| 883 | * ddx * rmask(j,i,sr) |
---|
| 884 | sums_l(k,61,tn) = sums_l(k,61,tn) - 0.5 * & |
---|
| 885 | ( kh(k,j,i) + kh(k,j-1,i) ) & |
---|
| 886 | * ( pt(k,j-1,i) - pt(k,j,i) ) & |
---|
| 887 | * ddy * rmask(j,i,sr) |
---|
| 888 | ! |
---|
| 889 | !-- Resolved horizontal heat fluxes u*pt*, v*pt* |
---|
| 890 | sums_l(k,59,tn) = sums_l(k,59,tn) + & |
---|
| 891 | ( u(k,j,i) - hom(k,1,1,sr) ) & |
---|
| 892 | * 0.5 * ( pt(k,j,i-1) - hom(k,1,4,sr) + & |
---|
| 893 | pt(k,j,i) - hom(k,1,4,sr) ) |
---|
| 894 | pts = 0.5 * ( pt(k,j-1,i) - hom(k,1,4,sr) + & |
---|
| 895 | pt(k,j,i) - hom(k,1,4,sr) ) |
---|
| 896 | sums_l(k,62,tn) = sums_l(k,62,tn) + & |
---|
| 897 | ( v(k,j,i) - hom(k,1,2,sr) ) & |
---|
| 898 | * 0.5 * ( pt(k,j-1,i) - hom(k,1,4,sr) + & |
---|
| 899 | pt(k,j,i) - hom(k,1,4,sr) ) |
---|
| 900 | ENDDO |
---|
| 901 | ENDDO |
---|
| 902 | ENDDO |
---|
| 903 | ! |
---|
| 904 | !-- Fluxes at the surface must be zero (e.g. due to the Prandtl-layer) |
---|
[97] | 905 | sums_l(nzb,58,tn) = 0.0 |
---|
| 906 | sums_l(nzb,59,tn) = 0.0 |
---|
| 907 | sums_l(nzb,60,tn) = 0.0 |
---|
| 908 | sums_l(nzb,61,tn) = 0.0 |
---|
| 909 | sums_l(nzb,62,tn) = 0.0 |
---|
| 910 | sums_l(nzb,63,tn) = 0.0 |
---|
[1] | 911 | |
---|
| 912 | ENDIF |
---|
[87] | 913 | |
---|
| 914 | ! |
---|
| 915 | !-- Calculate the user-defined profiles |
---|
| 916 | CALL user_statistics( 'profiles', sr, tn ) |
---|
[1] | 917 | !$OMP END PARALLEL |
---|
| 918 | |
---|
| 919 | ! |
---|
| 920 | !-- Summation of thread sums |
---|
| 921 | IF ( threads_per_task > 1 ) THEN |
---|
| 922 | DO i = 1, threads_per_task-1 |
---|
| 923 | sums_l(:,3,0) = sums_l(:,3,0) + sums_l(:,3,i) |
---|
| 924 | sums_l(:,4:40,0) = sums_l(:,4:40,0) + sums_l(:,4:40,i) |
---|
[87] | 925 | sums_l(:,45:pr_palm,0) = sums_l(:,45:pr_palm,0) + & |
---|
| 926 | sums_l(:,45:pr_palm,i) |
---|
| 927 | IF ( max_pr_user > 0 ) THEN |
---|
| 928 | sums_l(:,pr_palm+1:pr_palm+max_pr_user,0) = & |
---|
| 929 | sums_l(:,pr_palm+1:pr_palm+max_pr_user,0) + & |
---|
| 930 | sums_l(:,pr_palm+1:pr_palm+max_pr_user,i) |
---|
| 931 | ENDIF |
---|
[1] | 932 | ENDDO |
---|
| 933 | ENDIF |
---|
| 934 | |
---|
| 935 | #if defined( __parallel ) |
---|
[667] | 936 | |
---|
[1] | 937 | ! |
---|
| 938 | !-- Compute total sum from local sums |
---|
[622] | 939 | IF ( collective_wait ) CALL MPI_BARRIER( comm2d, ierr ) |
---|
[1] | 940 | CALL MPI_ALLREDUCE( sums_l(nzb,1,0), sums(nzb,1), ngp_sums, MPI_REAL, & |
---|
| 941 | MPI_SUM, comm2d, ierr ) |
---|
| 942 | #else |
---|
| 943 | sums = sums_l(:,:,0) |
---|
| 944 | #endif |
---|
| 945 | |
---|
| 946 | ! |
---|
| 947 | !-- Final values are obtained by division by the total number of grid points |
---|
| 948 | !-- used for summation. After that store profiles. |
---|
| 949 | !-- Profiles: |
---|
| 950 | DO k = nzb, nzt+1 |
---|
[132] | 951 | sums(k,3) = sums(k,3) / ngp_2dh(sr) |
---|
[142] | 952 | sums(k,8:11) = sums(k,8:11) / ngp_2dh_s_inner(k,sr) |
---|
[132] | 953 | sums(k,12:22) = sums(k,12:22) / ngp_2dh(sr) |
---|
| 954 | sums(k,23:29) = sums(k,23:29) / ngp_2dh_s_inner(k,sr) |
---|
| 955 | sums(k,30:32) = sums(k,30:32) / ngp_2dh(sr) |
---|
[142] | 956 | sums(k,33:34) = sums(k,33:34) / ngp_2dh_s_inner(k,sr) |
---|
| 957 | sums(k,35:39) = sums(k,35:39) / ngp_2dh(sr) |
---|
[132] | 958 | sums(k,40) = sums(k,40) / ngp_2dh_s_inner(k,sr) |
---|
| 959 | sums(k,45:53) = sums(k,45:53) / ngp_2dh(sr) |
---|
| 960 | sums(k,54) = sums(k,54) / ngp_2dh_s_inner(k,sr) |
---|
| 961 | sums(k,55:63) = sums(k,55:63) / ngp_2dh(sr) |
---|
| 962 | sums(k,64) = sums(k,64) / ngp_2dh_s_inner(k,sr) |
---|
| 963 | sums(k,65:69) = sums(k,65:69) / ngp_2dh(sr) |
---|
| 964 | sums(k,70:pr_palm-2) = sums(k,70:pr_palm-2)/ ngp_2dh_s_inner(k,sr) |
---|
[1] | 965 | ENDDO |
---|
[667] | 966 | |
---|
[1] | 967 | !-- Upstream-parts |
---|
[87] | 968 | sums(nzb:nzb+11,pr_palm-1) = sums(nzb:nzb+11,pr_palm-1) / ngp_3d(sr) |
---|
[1] | 969 | !-- u* and so on |
---|
[87] | 970 | !-- As sums(nzb:nzb+3,pr_palm) are full 2D arrays (us, usws, vsws, ts) whose |
---|
[1] | 971 | !-- size is always ( nx + 1 ) * ( ny + 1 ), defined at the first grid layer |
---|
| 972 | !-- above the topography, they are being divided by ngp_2dh(sr) |
---|
[87] | 973 | sums(nzb:nzb+3,pr_palm) = sums(nzb:nzb+3,pr_palm) / & |
---|
[1] | 974 | ngp_2dh(sr) |
---|
[197] | 975 | sums(nzb+12,pr_palm) = sums(nzb+12,pr_palm) / & ! qs |
---|
| 976 | ngp_2dh(sr) |
---|
[1] | 977 | !-- eges, e* |
---|
[87] | 978 | sums(nzb+4:nzb+5,pr_palm) = sums(nzb+4:nzb+5,pr_palm) / & |
---|
[132] | 979 | ngp_3d(sr) |
---|
[1] | 980 | !-- Old and new divergence |
---|
[87] | 981 | sums(nzb+9:nzb+10,pr_palm) = sums(nzb+9:nzb+10,pr_palm) / & |
---|
[1] | 982 | ngp_3d_inner(sr) |
---|
| 983 | |
---|
[87] | 984 | !-- User-defined profiles |
---|
| 985 | IF ( max_pr_user > 0 ) THEN |
---|
| 986 | DO k = nzb, nzt+1 |
---|
| 987 | sums(k,pr_palm+1:pr_palm+max_pr_user) = & |
---|
| 988 | sums(k,pr_palm+1:pr_palm+max_pr_user) / & |
---|
[132] | 989 | ngp_2dh_s_inner(k,sr) |
---|
[87] | 990 | ENDDO |
---|
| 991 | ENDIF |
---|
[1] | 992 | ! |
---|
| 993 | !-- Collect horizontal average in hom. |
---|
| 994 | !-- Compute deduced averages (e.g. total heat flux) |
---|
| 995 | hom(:,1,3,sr) = sums(:,3) ! w |
---|
| 996 | hom(:,1,8,sr) = sums(:,8) ! e profiles 5-7 are initial profiles |
---|
| 997 | hom(:,1,9,sr) = sums(:,9) ! km |
---|
| 998 | hom(:,1,10,sr) = sums(:,10) ! kh |
---|
| 999 | hom(:,1,11,sr) = sums(:,11) ! l |
---|
| 1000 | hom(:,1,12,sr) = sums(:,12) ! w"u" |
---|
| 1001 | hom(:,1,13,sr) = sums(:,13) ! w*u* |
---|
| 1002 | hom(:,1,14,sr) = sums(:,14) ! w"v" |
---|
| 1003 | hom(:,1,15,sr) = sums(:,15) ! w*v* |
---|
| 1004 | hom(:,1,16,sr) = sums(:,16) ! w"pt" |
---|
| 1005 | hom(:,1,17,sr) = sums(:,17) ! w*pt* |
---|
| 1006 | hom(:,1,18,sr) = sums(:,16) + sums(:,17) ! wpt |
---|
| 1007 | hom(:,1,19,sr) = sums(:,12) + sums(:,13) ! wu |
---|
| 1008 | hom(:,1,20,sr) = sums(:,14) + sums(:,15) ! wv |
---|
| 1009 | hom(:,1,21,sr) = sums(:,21) ! w*pt*BC |
---|
| 1010 | hom(:,1,22,sr) = sums(:,16) + sums(:,21) ! wptBC |
---|
[96] | 1011 | ! profile 24 is initial profile (sa) |
---|
| 1012 | ! profiles 25-29 left empty for initial |
---|
[1] | 1013 | ! profiles |
---|
| 1014 | hom(:,1,30,sr) = sums(:,30) ! u*2 |
---|
| 1015 | hom(:,1,31,sr) = sums(:,31) ! v*2 |
---|
| 1016 | hom(:,1,32,sr) = sums(:,32) ! w*2 |
---|
| 1017 | hom(:,1,33,sr) = sums(:,33) ! pt*2 |
---|
| 1018 | hom(:,1,34,sr) = sums(:,34) ! e* |
---|
| 1019 | hom(:,1,35,sr) = sums(:,35) ! w*2pt* |
---|
| 1020 | hom(:,1,36,sr) = sums(:,36) ! w*pt*2 |
---|
| 1021 | hom(:,1,37,sr) = sums(:,37) ! w*e* |
---|
| 1022 | hom(:,1,38,sr) = sums(:,38) ! w*3 |
---|
| 1023 | hom(:,1,39,sr) = sums(:,38) / ( sums(:,32) + 1E-20 )**1.5 ! Sw |
---|
| 1024 | hom(:,1,40,sr) = sums(:,40) ! p |
---|
[531] | 1025 | hom(:,1,45,sr) = sums(:,45) ! w"vpt" |
---|
[1] | 1026 | hom(:,1,46,sr) = sums(:,46) ! w*vpt* |
---|
| 1027 | hom(:,1,47,sr) = sums(:,45) + sums(:,46) ! wvpt |
---|
| 1028 | hom(:,1,48,sr) = sums(:,48) ! w"q" (w"qv") |
---|
| 1029 | hom(:,1,49,sr) = sums(:,49) ! w*q* (w*qv*) |
---|
| 1030 | hom(:,1,50,sr) = sums(:,48) + sums(:,49) ! wq (wqv) |
---|
| 1031 | hom(:,1,51,sr) = sums(:,51) ! w"qv" |
---|
| 1032 | hom(:,1,52,sr) = sums(:,52) ! w*qv* |
---|
| 1033 | hom(:,1,53,sr) = sums(:,52) + sums(:,51) ! wq (wqv) |
---|
| 1034 | hom(:,1,54,sr) = sums(:,54) ! ql |
---|
| 1035 | hom(:,1,55,sr) = sums(:,55) ! w*u*u*/dz |
---|
| 1036 | hom(:,1,56,sr) = sums(:,56) ! w*p*/dz |
---|
[106] | 1037 | hom(:,1,57,sr) = sums(:,57) ! ( w"e + w"p"/rho )/dz |
---|
[1] | 1038 | hom(:,1,58,sr) = sums(:,58) ! u"pt" |
---|
| 1039 | hom(:,1,59,sr) = sums(:,59) ! u*pt* |
---|
| 1040 | hom(:,1,60,sr) = sums(:,58) + sums(:,59) ! upt_t |
---|
| 1041 | hom(:,1,61,sr) = sums(:,61) ! v"pt" |
---|
| 1042 | hom(:,1,62,sr) = sums(:,62) ! v*pt* |
---|
| 1043 | hom(:,1,63,sr) = sums(:,61) + sums(:,62) ! vpt_t |
---|
[96] | 1044 | hom(:,1,64,sr) = sums(:,64) ! rho |
---|
| 1045 | hom(:,1,65,sr) = sums(:,65) ! w"sa" |
---|
| 1046 | hom(:,1,66,sr) = sums(:,66) ! w*sa* |
---|
| 1047 | hom(:,1,67,sr) = sums(:,65) + sums(:,66) ! wsa |
---|
[106] | 1048 | hom(:,1,68,sr) = sums(:,68) ! w*p* |
---|
| 1049 | hom(:,1,69,sr) = sums(:,69) ! w"e + w"p"/rho |
---|
[197] | 1050 | hom(:,1,70,sr) = sums(:,70) ! q*2 |
---|
[388] | 1051 | hom(:,1,71,sr) = sums(:,71) ! prho |
---|
[531] | 1052 | hom(:,1,72,sr) = hyp * 1E-4 ! hyp in dbar |
---|
[1] | 1053 | |
---|
[87] | 1054 | hom(:,1,pr_palm-1,sr) = sums(:,pr_palm-1) |
---|
[1] | 1055 | ! upstream-parts u_x, u_y, u_z, v_x, |
---|
| 1056 | ! v_y, usw. (in last but one profile) |
---|
[667] | 1057 | hom(:,1,pr_palm,sr) = sums(:,pr_palm) |
---|
[1] | 1058 | ! u*, w'u', w'v', t* (in last profile) |
---|
| 1059 | |
---|
[87] | 1060 | IF ( max_pr_user > 0 ) THEN ! user-defined profiles |
---|
| 1061 | hom(:,1,pr_palm+1:pr_palm+max_pr_user,sr) = & |
---|
| 1062 | sums(:,pr_palm+1:pr_palm+max_pr_user) |
---|
| 1063 | ENDIF |
---|
| 1064 | |
---|
[1] | 1065 | ! |
---|
| 1066 | !-- Determine the boundary layer height using two different schemes. |
---|
[94] | 1067 | !-- First scheme: Starting from the Earth's (Ocean's) surface, look for the |
---|
| 1068 | !-- first relative minimum (maximum) of the total heat flux. |
---|
| 1069 | !-- The corresponding height is assumed as the boundary layer height, if it |
---|
| 1070 | !-- is less than 1.5 times the height where the heat flux becomes negative |
---|
| 1071 | !-- (positive) for the first time. |
---|
[1] | 1072 | z_i(1) = 0.0 |
---|
| 1073 | first = .TRUE. |
---|
[667] | 1074 | |
---|
[97] | 1075 | IF ( ocean ) THEN |
---|
| 1076 | DO k = nzt, nzb+1, -1 |
---|
[667] | 1077 | IF ( first .AND. hom(k,1,18,sr) < 0.0 & |
---|
| 1078 | .AND. abs(hom(k,1,18,sr)) > 1.0E-8) THEN |
---|
[97] | 1079 | first = .FALSE. |
---|
| 1080 | height = zw(k) |
---|
| 1081 | ENDIF |
---|
| 1082 | IF ( hom(k,1,18,sr) < 0.0 .AND. & |
---|
[667] | 1083 | abs(hom(k,1,18,sr)) > 1.0E-8 .AND. & |
---|
[97] | 1084 | hom(k-1,1,18,sr) > hom(k,1,18,sr) ) THEN |
---|
| 1085 | IF ( zw(k) < 1.5 * height ) THEN |
---|
| 1086 | z_i(1) = zw(k) |
---|
| 1087 | ELSE |
---|
| 1088 | z_i(1) = height |
---|
| 1089 | ENDIF |
---|
| 1090 | EXIT |
---|
| 1091 | ENDIF |
---|
| 1092 | ENDDO |
---|
| 1093 | ELSE |
---|
[94] | 1094 | DO k = nzb, nzt-1 |
---|
[667] | 1095 | IF ( first .AND. hom(k,1,18,sr) < 0.0 & |
---|
| 1096 | .AND. abs(hom(k,1,18,sr)) > 1.0E-8 ) THEN |
---|
[94] | 1097 | first = .FALSE. |
---|
| 1098 | height = zw(k) |
---|
[1] | 1099 | ENDIF |
---|
[667] | 1100 | IF ( hom(k,1,18,sr) < 0.0 .AND. & |
---|
| 1101 | abs(hom(k,1,18,sr)) > 1.0E-8 .AND. & |
---|
[94] | 1102 | hom(k+1,1,18,sr) > hom(k,1,18,sr) ) THEN |
---|
| 1103 | IF ( zw(k) < 1.5 * height ) THEN |
---|
| 1104 | z_i(1) = zw(k) |
---|
| 1105 | ELSE |
---|
| 1106 | z_i(1) = height |
---|
| 1107 | ENDIF |
---|
| 1108 | EXIT |
---|
| 1109 | ENDIF |
---|
| 1110 | ENDDO |
---|
[97] | 1111 | ENDIF |
---|
[1] | 1112 | |
---|
| 1113 | ! |
---|
[291] | 1114 | !-- Second scheme: Gradient scheme from Sullivan et al. (1998), modified |
---|
| 1115 | !-- by Uhlenbrock(2006). The boundary layer height is the height with the |
---|
| 1116 | !-- maximal local temperature gradient: starting from the second (the last |
---|
| 1117 | !-- but one) vertical gridpoint, the local gradient must be at least |
---|
| 1118 | !-- 0.2K/100m and greater than the next four gradients. |
---|
| 1119 | !-- WARNING: The threshold value of 0.2K/100m must be adjusted for the |
---|
| 1120 | !-- ocean case! |
---|
[1] | 1121 | z_i(2) = 0.0 |
---|
[291] | 1122 | DO k = nzb+1, nzt+1 |
---|
| 1123 | dptdz(k) = ( hom(k,1,4,sr) - hom(k-1,1,4,sr) ) * ddzu(k) |
---|
| 1124 | ENDDO |
---|
| 1125 | dptdz_threshold = 0.2 / 100.0 |
---|
| 1126 | |
---|
[97] | 1127 | IF ( ocean ) THEN |
---|
[291] | 1128 | DO k = nzt+1, nzb+5, -1 |
---|
| 1129 | IF ( dptdz(k) > dptdz_threshold .AND. & |
---|
| 1130 | dptdz(k) > dptdz(k-1) .AND. dptdz(k) > dptdz(k-2) .AND. & |
---|
| 1131 | dptdz(k) > dptdz(k-3) .AND. dptdz(k) > dptdz(k-4) ) THEN |
---|
| 1132 | z_i(2) = zw(k-1) |
---|
[97] | 1133 | EXIT |
---|
| 1134 | ENDIF |
---|
| 1135 | ENDDO |
---|
| 1136 | ELSE |
---|
[291] | 1137 | DO k = nzb+1, nzt-3 |
---|
| 1138 | IF ( dptdz(k) > dptdz_threshold .AND. & |
---|
| 1139 | dptdz(k) > dptdz(k+1) .AND. dptdz(k) > dptdz(k+2) .AND. & |
---|
| 1140 | dptdz(k) > dptdz(k+3) .AND. dptdz(k) > dptdz(k+4) ) THEN |
---|
| 1141 | z_i(2) = zw(k-1) |
---|
[97] | 1142 | EXIT |
---|
| 1143 | ENDIF |
---|
| 1144 | ENDDO |
---|
| 1145 | ENDIF |
---|
[1] | 1146 | |
---|
[87] | 1147 | hom(nzb+6,1,pr_palm,sr) = z_i(1) |
---|
| 1148 | hom(nzb+7,1,pr_palm,sr) = z_i(2) |
---|
[1] | 1149 | |
---|
| 1150 | ! |
---|
| 1151 | !-- Computation of both the characteristic vertical velocity and |
---|
| 1152 | !-- the characteristic convective boundary layer temperature. |
---|
| 1153 | !-- The horizontal average at nzb+1 is input for the average temperature. |
---|
[667] | 1154 | IF ( hom(nzb,1,18,sr) > 0.0 .AND. abs(hom(nzb,1,18,sr)) > 1.0E-8 & |
---|
| 1155 | .AND. z_i(1) /= 0.0 ) THEN |
---|
[87] | 1156 | hom(nzb+8,1,pr_palm,sr) = ( g / hom(nzb+1,1,4,sr) * & |
---|
[94] | 1157 | hom(nzb,1,18,sr) * & |
---|
| 1158 | ABS( z_i(1) ) )**0.333333333 |
---|
[1] | 1159 | !-- so far this only works if Prandtl layer is used |
---|
[87] | 1160 | hom(nzb+11,1,pr_palm,sr) = hom(nzb,1,16,sr) / hom(nzb+8,1,pr_palm,sr) |
---|
[1] | 1161 | ELSE |
---|
[87] | 1162 | hom(nzb+8,1,pr_palm,sr) = 0.0 |
---|
| 1163 | hom(nzb+11,1,pr_palm,sr) = 0.0 |
---|
[1] | 1164 | ENDIF |
---|
| 1165 | |
---|
[48] | 1166 | ! |
---|
| 1167 | !-- Collect the time series quantities |
---|
[87] | 1168 | ts_value(1,sr) = hom(nzb+4,1,pr_palm,sr) ! E |
---|
| 1169 | ts_value(2,sr) = hom(nzb+5,1,pr_palm,sr) ! E* |
---|
[48] | 1170 | ts_value(3,sr) = dt_3d |
---|
[87] | 1171 | ts_value(4,sr) = hom(nzb,1,pr_palm,sr) ! u* |
---|
| 1172 | ts_value(5,sr) = hom(nzb+3,1,pr_palm,sr) ! th* |
---|
[48] | 1173 | ts_value(6,sr) = u_max |
---|
| 1174 | ts_value(7,sr) = v_max |
---|
| 1175 | ts_value(8,sr) = w_max |
---|
[87] | 1176 | ts_value(9,sr) = hom(nzb+10,1,pr_palm,sr) ! new divergence |
---|
| 1177 | ts_value(10,sr) = hom(nzb+9,1,pr_palm,sr) ! old Divergence |
---|
| 1178 | ts_value(11,sr) = hom(nzb+6,1,pr_palm,sr) ! z_i(1) |
---|
| 1179 | ts_value(12,sr) = hom(nzb+7,1,pr_palm,sr) ! z_i(2) |
---|
| 1180 | ts_value(13,sr) = hom(nzb+8,1,pr_palm,sr) ! w* |
---|
[48] | 1181 | ts_value(14,sr) = hom(nzb,1,16,sr) ! w'pt' at k=0 |
---|
| 1182 | ts_value(15,sr) = hom(nzb+1,1,16,sr) ! w'pt' at k=1 |
---|
| 1183 | ts_value(16,sr) = hom(nzb+1,1,18,sr) ! wpt at k=1 |
---|
| 1184 | ts_value(17,sr) = hom(nzb,1,4,sr) ! pt(0) |
---|
| 1185 | ts_value(18,sr) = hom(nzb+1,1,4,sr) ! pt(zp) |
---|
[197] | 1186 | ts_value(19,sr) = hom(nzb+1,1,pr_palm,sr) ! u'w' at k=0 |
---|
| 1187 | ts_value(20,sr) = hom(nzb+2,1,pr_palm,sr) ! v'w' at k=0 |
---|
[343] | 1188 | ts_value(21,sr) = hom(nzb,1,48,sr) ! w"q" at k=0 |
---|
[197] | 1189 | |
---|
[48] | 1190 | IF ( ts_value(5,sr) /= 0.0 ) THEN |
---|
| 1191 | ts_value(22,sr) = ts_value(4,sr)**2 / & |
---|
| 1192 | ( kappa * g * ts_value(5,sr) / ts_value(18,sr) ) ! L |
---|
| 1193 | ELSE |
---|
| 1194 | ts_value(22,sr) = 10000.0 |
---|
| 1195 | ENDIF |
---|
[1] | 1196 | |
---|
[343] | 1197 | ts_value(23,sr) = hom(nzb+12,1,pr_palm,sr) ! q* |
---|
[1] | 1198 | ! |
---|
[48] | 1199 | !-- Calculate additional statistics provided by the user interface |
---|
[87] | 1200 | CALL user_statistics( 'time_series', sr, 0 ) |
---|
[1] | 1201 | |
---|
[48] | 1202 | ENDDO ! loop of the subregions |
---|
| 1203 | |
---|
[1] | 1204 | ! |
---|
| 1205 | !-- If required, sum up horizontal averages for subsequent time averaging |
---|
| 1206 | IF ( do_sum ) THEN |
---|
| 1207 | IF ( average_count_pr == 0 ) hom_sum = 0.0 |
---|
| 1208 | hom_sum = hom_sum + hom(:,1,:,:) |
---|
| 1209 | average_count_pr = average_count_pr + 1 |
---|
| 1210 | do_sum = .FALSE. |
---|
| 1211 | ENDIF |
---|
| 1212 | |
---|
| 1213 | ! |
---|
| 1214 | !-- Set flag for other UPs (e.g. output routines, but also buoyancy). |
---|
| 1215 | !-- This flag is reset after each time step in time_integration. |
---|
| 1216 | flow_statistics_called = .TRUE. |
---|
| 1217 | |
---|
| 1218 | CALL cpu_log( log_point(10), 'flow_statistics', 'stop' ) |
---|
| 1219 | |
---|
| 1220 | |
---|
| 1221 | END SUBROUTINE flow_statistics |
---|
| 1222 | |
---|
| 1223 | |
---|
| 1224 | |
---|