[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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[696] | 6 | ! Bugfix: Summation of Wicker-Skamarock scheme fluxes and variances for all |
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| 7 | ! threads |
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[392] | 8 | ! |
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| 9 | ! Former revisions: |
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| 10 | ! ----------------- |
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| 11 | ! $Id: flow_statistics.f90 696 2011-03-18 07:03:49Z raasch $ |
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| 12 | ! |
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[679] | 13 | ! 678 2011-02-02 14:31:56Z raasch |
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| 14 | ! Bugfix in calculation of the divergence of vertical flux of resolved scale |
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| 15 | ! energy, pressure fluctuations, and flux of pressure fluctuation itself |
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| 16 | ! |
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[674] | 17 | ! 673 2011-01-18 16:19:48Z suehring |
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| 18 | ! Top bc for the horizontal velocity variances added for ocean runs. |
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| 19 | ! Setting the corresponding bottom bc moved to advec_ws. |
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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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[696] | 158 | |
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[667] | 159 | ! |
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[673] | 160 | !-- According to the Neumann bc for the horizontal velocity components, |
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| 161 | !-- the corresponding fluxes has to satisfiy the same bc. |
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| 162 | IF ( ocean ) THEN |
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| 163 | sums_us2_ws_l(nzt+1,sr) = sums_us2_ws_l(nzt,sr) |
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| 164 | sums_vs2_ws_l(nzt+1,sr) = sums_vs2_ws_l(nzt,sr) |
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| 165 | ENDIF |
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[696] | 166 | |
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| 167 | DO i = 0, threads_per_task-1 |
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[667] | 168 | ! |
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[696] | 169 | !-- Swap the turbulent quantities evaluated in advec_ws. |
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| 170 | sums_l(:,13,i) = sums_wsus_ws_l(:,sr) ! w*u* |
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| 171 | sums_l(:,15,i) = sums_wsvs_ws_l(:,sr) ! w*v* |
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| 172 | sums_l(:,30,i) = sums_us2_ws_l(:,sr) ! u*2 |
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| 173 | sums_l(:,31,i) = sums_vs2_ws_l(:,sr) ! v*2 |
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| 174 | sums_l(:,32,i) = sums_ws2_ws_l(:,sr) ! w*2 |
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| 175 | sums_l(:,34,i) = sums_l(:,34,i) + 0.5 * & |
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| 176 | ( sums_us2_ws_l(:,sr) + sums_vs2_ws_l(:,sr) + & |
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| 177 | sums_ws2_ws_l(:,sr) ) ! e* |
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| 178 | DO k = nzb, nzt |
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| 179 | sums_l(nzb+5,pr_palm,i) = sums_l(nzb+5,pr_palm,i) + 0.5 * ( & |
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| 180 | sums_us2_ws_l(k,sr) + & |
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| 181 | 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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[667] | 184 | ENDDO |
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[696] | 185 | |
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[667] | 186 | ENDIF |
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[696] | 187 | |
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[667] | 188 | IF ( ws_scheme_sca ) THEN |
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[696] | 189 | |
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| 190 | DO i = 0, threads_per_task-1 |
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| 191 | sums_l(:,17,i) = sums_wspts_ws_l(:,sr) ! w*pt* from advec_s_ws |
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| 192 | IF ( ocean ) sums_l(:,66,i) = sums_wssas_ws_l(:,sr) ! w*sa* |
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| 193 | IF ( humidity .OR. passive_scalar ) sums_l(:,49,i) = & |
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| 194 | sums_wsqs_ws_l(:,sr) !w*q* |
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| 195 | ENDDO |
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| 196 | |
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[667] | 197 | ENDIF |
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[305] | 198 | ! |
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[1] | 199 | !-- Horizontally averaged profiles of horizontal velocities and temperature. |
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| 200 | !-- They must have been computed before, because they are already required |
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| 201 | !-- for other horizontal averages. |
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| 202 | tn = 0 |
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[667] | 203 | |
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[1] | 204 | !$OMP PARALLEL PRIVATE( i, j, k, tn ) |
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[82] | 205 | #if defined( __intel_openmp_bug ) |
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[1] | 206 | tn = omp_get_thread_num() |
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| 207 | #else |
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| 208 | !$ tn = omp_get_thread_num() |
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| 209 | #endif |
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| 210 | |
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| 211 | !$OMP DO |
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| 212 | DO i = nxl, nxr |
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| 213 | DO j = nys, nyn |
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[132] | 214 | DO k = nzb_s_inner(j,i), nzt+1 |
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[1] | 215 | sums_l(k,1,tn) = sums_l(k,1,tn) + u(k,j,i) * rmask(j,i,sr) |
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| 216 | sums_l(k,2,tn) = sums_l(k,2,tn) + v(k,j,i) * rmask(j,i,sr) |
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| 217 | sums_l(k,4,tn) = sums_l(k,4,tn) + pt(k,j,i) * rmask(j,i,sr) |
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| 218 | ENDDO |
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| 219 | ENDDO |
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| 220 | ENDDO |
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| 221 | |
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| 222 | ! |
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[96] | 223 | !-- Horizontally averaged profile of salinity |
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| 224 | IF ( ocean ) THEN |
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| 225 | !$OMP DO |
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| 226 | DO i = nxl, nxr |
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| 227 | DO j = nys, nyn |
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[132] | 228 | DO k = nzb_s_inner(j,i), nzt+1 |
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[96] | 229 | sums_l(k,23,tn) = sums_l(k,23,tn) + & |
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| 230 | sa(k,j,i) * rmask(j,i,sr) |
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| 231 | ENDDO |
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| 232 | ENDDO |
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| 233 | ENDDO |
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| 234 | ENDIF |
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| 235 | |
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| 236 | ! |
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[1] | 237 | !-- Horizontally averaged profiles of virtual potential temperature, |
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| 238 | !-- total water content, specific humidity and liquid water potential |
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| 239 | !-- temperature |
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[75] | 240 | IF ( humidity ) THEN |
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[1] | 241 | !$OMP DO |
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| 242 | DO i = nxl, nxr |
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| 243 | DO j = nys, nyn |
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[132] | 244 | DO k = nzb_s_inner(j,i), nzt+1 |
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[1] | 245 | sums_l(k,44,tn) = sums_l(k,44,tn) + & |
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| 246 | vpt(k,j,i) * rmask(j,i,sr) |
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| 247 | sums_l(k,41,tn) = sums_l(k,41,tn) + & |
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| 248 | q(k,j,i) * rmask(j,i,sr) |
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| 249 | ENDDO |
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| 250 | ENDDO |
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| 251 | ENDDO |
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| 252 | IF ( cloud_physics ) THEN |
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| 253 | !$OMP DO |
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| 254 | DO i = nxl, nxr |
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| 255 | DO j = nys, nyn |
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[132] | 256 | DO k = nzb_s_inner(j,i), nzt+1 |
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[1] | 257 | sums_l(k,42,tn) = sums_l(k,42,tn) + & |
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| 258 | ( q(k,j,i) - ql(k,j,i) ) * rmask(j,i,sr) |
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| 259 | sums_l(k,43,tn) = sums_l(k,43,tn) + ( & |
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| 260 | pt(k,j,i) + l_d_cp*pt_d_t(k) * ql(k,j,i) & |
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| 261 | ) * rmask(j,i,sr) |
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| 262 | ENDDO |
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| 263 | ENDDO |
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| 264 | ENDDO |
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| 265 | ENDIF |
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| 266 | ENDIF |
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| 267 | |
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| 268 | ! |
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| 269 | !-- Horizontally averaged profiles of passive scalar |
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| 270 | IF ( passive_scalar ) THEN |
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| 271 | !$OMP DO |
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| 272 | DO i = nxl, nxr |
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| 273 | DO j = nys, nyn |
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[132] | 274 | DO k = nzb_s_inner(j,i), nzt+1 |
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[1] | 275 | sums_l(k,41,tn) = sums_l(k,41,tn) + q(k,j,i) * rmask(j,i,sr) |
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| 276 | ENDDO |
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| 277 | ENDDO |
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| 278 | ENDDO |
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| 279 | ENDIF |
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| 280 | !$OMP END PARALLEL |
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| 281 | ! |
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| 282 | !-- Summation of thread sums |
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| 283 | IF ( threads_per_task > 1 ) THEN |
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| 284 | DO i = 1, threads_per_task-1 |
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| 285 | sums_l(:,1,0) = sums_l(:,1,0) + sums_l(:,1,i) |
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| 286 | sums_l(:,2,0) = sums_l(:,2,0) + sums_l(:,2,i) |
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| 287 | sums_l(:,4,0) = sums_l(:,4,0) + sums_l(:,4,i) |
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[96] | 288 | IF ( ocean ) THEN |
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| 289 | sums_l(:,23,0) = sums_l(:,23,0) + sums_l(:,23,i) |
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| 290 | ENDIF |
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[75] | 291 | IF ( humidity ) THEN |
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[1] | 292 | sums_l(:,41,0) = sums_l(:,41,0) + sums_l(:,41,i) |
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| 293 | sums_l(:,44,0) = sums_l(:,44,0) + sums_l(:,44,i) |
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| 294 | IF ( cloud_physics ) THEN |
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| 295 | sums_l(:,42,0) = sums_l(:,42,0) + sums_l(:,42,i) |
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| 296 | sums_l(:,43,0) = sums_l(:,43,0) + sums_l(:,43,i) |
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| 297 | ENDIF |
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| 298 | ENDIF |
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| 299 | IF ( passive_scalar ) THEN |
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| 300 | sums_l(:,41,0) = sums_l(:,41,0) + sums_l(:,41,i) |
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| 301 | ENDIF |
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| 302 | ENDDO |
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| 303 | ENDIF |
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| 304 | |
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| 305 | #if defined( __parallel ) |
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| 306 | ! |
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| 307 | !-- Compute total sum from local sums |
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[622] | 308 | IF ( collective_wait ) CALL MPI_BARRIER( comm2d, ierr ) |
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[1] | 309 | CALL MPI_ALLREDUCE( sums_l(nzb,1,0), sums(nzb,1), nzt+2-nzb, MPI_REAL, & |
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| 310 | MPI_SUM, comm2d, ierr ) |
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[622] | 311 | IF ( collective_wait ) CALL MPI_BARRIER( comm2d, ierr ) |
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[1] | 312 | CALL MPI_ALLREDUCE( sums_l(nzb,2,0), sums(nzb,2), nzt+2-nzb, MPI_REAL, & |
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| 313 | MPI_SUM, comm2d, ierr ) |
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[622] | 314 | IF ( collective_wait ) CALL MPI_BARRIER( comm2d, ierr ) |
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[1] | 315 | CALL MPI_ALLREDUCE( sums_l(nzb,4,0), sums(nzb,4), nzt+2-nzb, MPI_REAL, & |
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| 316 | MPI_SUM, comm2d, ierr ) |
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[96] | 317 | IF ( ocean ) THEN |
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[622] | 318 | IF ( collective_wait ) CALL MPI_BARRIER( comm2d, ierr ) |
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[96] | 319 | CALL MPI_ALLREDUCE( sums_l(nzb,23,0), sums(nzb,23), nzt+2-nzb, & |
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| 320 | MPI_REAL, MPI_SUM, comm2d, ierr ) |
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| 321 | ENDIF |
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[75] | 322 | IF ( humidity ) 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,44,0), sums(nzb,44), 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,41,0), sums(nzb,41), nzt+2-nzb, & |
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| 328 | MPI_REAL, MPI_SUM, comm2d, ierr ) |
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| 329 | IF ( cloud_physics ) THEN |
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[622] | 330 | IF ( collective_wait ) CALL MPI_BARRIER( comm2d, ierr ) |
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[1] | 331 | CALL MPI_ALLREDUCE( sums_l(nzb,42,0), sums(nzb,42), nzt+2-nzb, & |
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| 332 | MPI_REAL, MPI_SUM, comm2d, ierr ) |
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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,43,0), sums(nzb,43), 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 | ENDIF |
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| 338 | |
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| 339 | IF ( passive_scalar ) THEN |
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[622] | 340 | IF ( collective_wait ) CALL MPI_BARRIER( comm2d, ierr ) |
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[1] | 341 | CALL MPI_ALLREDUCE( sums_l(nzb,41,0), sums(nzb,41), nzt+2-nzb, & |
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| 342 | MPI_REAL, MPI_SUM, comm2d, ierr ) |
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| 343 | ENDIF |
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| 344 | #else |
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| 345 | sums(:,1) = sums_l(:,1,0) |
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| 346 | sums(:,2) = sums_l(:,2,0) |
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| 347 | sums(:,4) = sums_l(:,4,0) |
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[96] | 348 | IF ( ocean ) sums(:,23) = sums_l(:,23,0) |
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[75] | 349 | IF ( humidity ) THEN |
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[1] | 350 | sums(:,44) = sums_l(:,44,0) |
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| 351 | sums(:,41) = sums_l(:,41,0) |
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| 352 | IF ( cloud_physics ) THEN |
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| 353 | sums(:,42) = sums_l(:,42,0) |
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| 354 | sums(:,43) = sums_l(:,43,0) |
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| 355 | ENDIF |
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| 356 | ENDIF |
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| 357 | IF ( passive_scalar ) sums(:,41) = sums_l(:,41,0) |
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| 358 | #endif |
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| 359 | |
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| 360 | ! |
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| 361 | !-- Final values are obtained by division by the total number of grid points |
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| 362 | !-- used for summation. After that store profiles. |
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[132] | 363 | sums(:,1) = sums(:,1) / ngp_2dh(sr) |
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| 364 | sums(:,2) = sums(:,2) / ngp_2dh(sr) |
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| 365 | sums(:,4) = sums(:,4) / ngp_2dh_s_inner(:,sr) |
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[1] | 366 | hom(:,1,1,sr) = sums(:,1) ! u |
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| 367 | hom(:,1,2,sr) = sums(:,2) ! v |
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| 368 | hom(:,1,4,sr) = sums(:,4) ! pt |
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| 369 | |
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[667] | 370 | |
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[1] | 371 | ! |
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[96] | 372 | !-- Salinity |
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| 373 | IF ( ocean ) THEN |
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[132] | 374 | sums(:,23) = sums(:,23) / ngp_2dh_s_inner(:,sr) |
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[96] | 375 | hom(:,1,23,sr) = sums(:,23) ! sa |
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| 376 | ENDIF |
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| 377 | |
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| 378 | ! |
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[1] | 379 | !-- Humidity and cloud parameters |
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[75] | 380 | IF ( humidity ) THEN |
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[132] | 381 | sums(:,44) = sums(:,44) / ngp_2dh_s_inner(:,sr) |
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| 382 | sums(:,41) = sums(:,41) / ngp_2dh_s_inner(:,sr) |
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[1] | 383 | hom(:,1,44,sr) = sums(:,44) ! vpt |
---|
| 384 | hom(:,1,41,sr) = sums(:,41) ! qv (q) |
---|
| 385 | IF ( cloud_physics ) THEN |
---|
[132] | 386 | sums(:,42) = sums(:,42) / ngp_2dh_s_inner(:,sr) |
---|
| 387 | sums(:,43) = sums(:,43) / ngp_2dh_s_inner(:,sr) |
---|
[1] | 388 | hom(:,1,42,sr) = sums(:,42) ! qv |
---|
| 389 | hom(:,1,43,sr) = sums(:,43) ! pt |
---|
| 390 | ENDIF |
---|
| 391 | ENDIF |
---|
| 392 | |
---|
| 393 | ! |
---|
| 394 | !-- Passive scalar |
---|
[132] | 395 | IF ( passive_scalar ) hom(:,1,41,sr) = sums(:,41) / & |
---|
| 396 | ngp_2dh_s_inner(:,sr) ! s (q) |
---|
[1] | 397 | |
---|
| 398 | ! |
---|
| 399 | !-- Horizontally averaged profiles of the remaining prognostic variables, |
---|
| 400 | !-- variances, the total and the perturbation energy (single values in last |
---|
| 401 | !-- column of sums_l) and some diagnostic quantities. |
---|
[132] | 402 | !-- NOTE: for simplicity, nzb_s_inner is used below, although strictly |
---|
[1] | 403 | !-- ---- speaking the following k-loop would have to be split up and |
---|
| 404 | !-- rearranged according to the staggered grid. |
---|
[132] | 405 | !-- However, this implies no error since staggered velocity components |
---|
| 406 | !-- are zero at the walls and inside buildings. |
---|
[1] | 407 | tn = 0 |
---|
[82] | 408 | #if defined( __intel_openmp_bug ) |
---|
[1] | 409 | !$OMP PARALLEL PRIVATE( i, j, k, pts, sums_ll, sums_l_eper, sums_l_etot, & |
---|
| 410 | !$OMP tn, ust, ust2, u2, vst, vst2, v2, w2 ) |
---|
| 411 | tn = omp_get_thread_num() |
---|
| 412 | #else |
---|
| 413 | !$OMP PARALLEL PRIVATE( i, j, k, pts, sums_ll, sums_l_eper, sums_l_etot, tn, ust, ust2, u2, vst, vst2, v2, w2 ) |
---|
| 414 | !$ tn = omp_get_thread_num() |
---|
| 415 | #endif |
---|
| 416 | !$OMP DO |
---|
| 417 | DO i = nxl, nxr |
---|
| 418 | DO j = nys, nyn |
---|
| 419 | sums_l_etot = 0.0 |
---|
[132] | 420 | DO k = nzb_s_inner(j,i), nzt+1 |
---|
[1] | 421 | ! |
---|
| 422 | !-- Prognostic and diagnostic variables |
---|
| 423 | sums_l(k,3,tn) = sums_l(k,3,tn) + w(k,j,i) * rmask(j,i,sr) |
---|
| 424 | sums_l(k,8,tn) = sums_l(k,8,tn) + e(k,j,i) * rmask(j,i,sr) |
---|
| 425 | sums_l(k,9,tn) = sums_l(k,9,tn) + km(k,j,i) * rmask(j,i,sr) |
---|
| 426 | sums_l(k,10,tn) = sums_l(k,10,tn) + kh(k,j,i) * rmask(j,i,sr) |
---|
| 427 | sums_l(k,40,tn) = sums_l(k,40,tn) + p(k,j,i) |
---|
| 428 | |
---|
| 429 | sums_l(k,33,tn) = sums_l(k,33,tn) + & |
---|
| 430 | ( pt(k,j,i)-hom(k,1,4,sr) )**2 * rmask(j,i,sr) |
---|
[624] | 431 | |
---|
| 432 | IF ( humidity ) THEN |
---|
| 433 | sums_l(k,70,tn) = sums_l(k,70,tn) + & |
---|
| 434 | ( q(k,j,i)-hom(k,1,41,sr) )**2 * rmask(j,i,sr) |
---|
| 435 | ENDIF |
---|
[667] | 436 | |
---|
[1] | 437 | sums_l_etot = sums_l_etot + & |
---|
[667] | 438 | 0.5 * ( u(k,j,i)**2 + v(k,j,i)**2 + & |
---|
| 439 | w(k,j,i)**2 ) * rmask(j,i,sr) |
---|
[1] | 440 | ENDDO |
---|
| 441 | ! |
---|
| 442 | !-- Total and perturbation energy for the total domain (being |
---|
| 443 | !-- collected in the last column of sums_l). Summation of these |
---|
| 444 | !-- quantities is seperated from the previous loop in order to |
---|
| 445 | !-- allow vectorization of that loop. |
---|
[87] | 446 | sums_l(nzb+4,pr_palm,tn) = sums_l(nzb+4,pr_palm,tn) + sums_l_etot |
---|
[1] | 447 | ! |
---|
| 448 | !-- 2D-arrays (being collected in the last column of sums_l) |
---|
[87] | 449 | sums_l(nzb,pr_palm,tn) = sums_l(nzb,pr_palm,tn) + & |
---|
[1] | 450 | us(j,i) * rmask(j,i,sr) |
---|
[87] | 451 | sums_l(nzb+1,pr_palm,tn) = sums_l(nzb+1,pr_palm,tn) + & |
---|
[1] | 452 | usws(j,i) * rmask(j,i,sr) |
---|
[87] | 453 | sums_l(nzb+2,pr_palm,tn) = sums_l(nzb+2,pr_palm,tn) + & |
---|
[1] | 454 | vsws(j,i) * rmask(j,i,sr) |
---|
[87] | 455 | sums_l(nzb+3,pr_palm,tn) = sums_l(nzb+3,pr_palm,tn) + & |
---|
[1] | 456 | ts(j,i) * rmask(j,i,sr) |
---|
[197] | 457 | IF ( humidity ) THEN |
---|
| 458 | sums_l(nzb+12,pr_palm,tn) = sums_l(nzb+12,pr_palm,tn) + & |
---|
| 459 | qs(j,i) * rmask(j,i,sr) |
---|
| 460 | ENDIF |
---|
[1] | 461 | ENDDO |
---|
| 462 | ENDDO |
---|
| 463 | |
---|
| 464 | ! |
---|
[667] | 465 | !-- Computation of statistics when ws-scheme is not used. Else these |
---|
| 466 | !-- quantities are evaluated in the advection routines. |
---|
| 467 | IF ( .NOT. ws_scheme_mom ) THEN |
---|
| 468 | !$OMP DO |
---|
| 469 | DO i = nxl, nxr |
---|
| 470 | DO j = nys, nyn |
---|
| 471 | sums_l_eper = 0.0 |
---|
| 472 | DO k = nzb_s_inner(j,i), nzt+1 |
---|
| 473 | u2 = u(k,j,i)**2 |
---|
| 474 | v2 = v(k,j,i)**2 |
---|
| 475 | w2 = w(k,j,i)**2 |
---|
| 476 | ust2 = ( u(k,j,i) - hom(k,1,1,sr) )**2 |
---|
| 477 | vst2 = ( v(k,j,i) - hom(k,1,2,sr) )**2 |
---|
| 478 | |
---|
| 479 | sums_l(k,30,tn) = sums_l(k,30,tn) + ust2 * rmask(j,i,sr) |
---|
| 480 | sums_l(k,31,tn) = sums_l(k,31,tn) + vst2 * rmask(j,i,sr) |
---|
| 481 | sums_l(k,32,tn) = sums_l(k,32,tn) + w2 * rmask(j,i,sr) |
---|
| 482 | ! |
---|
| 483 | !-- Higher moments |
---|
| 484 | !-- (Computation of the skewness of w further below) |
---|
| 485 | sums_l(k,38,tn) = sums_l(k,38,tn) + w(k,j,i) * w2 * & |
---|
| 486 | rmask(j,i,sr) |
---|
| 487 | ! |
---|
| 488 | !-- Perturbation energy |
---|
| 489 | |
---|
| 490 | sums_l(k,34,tn) = sums_l(k,34,tn) + 0.5 * & |
---|
| 491 | ( ust2 + vst2 + w2 ) * rmask(j,i,sr) |
---|
| 492 | sums_l_eper = sums_l_eper + & |
---|
| 493 | 0.5 * ( ust2+vst2+w2 ) * rmask(j,i,sr) |
---|
| 494 | |
---|
| 495 | ENDDO |
---|
| 496 | sums_l(nzb+5,pr_palm,tn) = sums_l(nzb+5,pr_palm,tn) & |
---|
| 497 | + sums_l_eper |
---|
| 498 | ENDDO |
---|
| 499 | ENDDO |
---|
| 500 | ELSE |
---|
| 501 | !$OMP DO |
---|
| 502 | DO i = nxl, nxr |
---|
| 503 | DO j = nys, nyn |
---|
| 504 | DO k = nzb_s_inner(j,i), nzt + 1 |
---|
| 505 | w2 = w(k,j,i)**2 |
---|
| 506 | ! |
---|
| 507 | !-- Higher moments |
---|
| 508 | !-- (Computation of the skewness of w further below) |
---|
| 509 | sums_l(k,38,tn) = sums_l(k,38,tn) + w(k,j,i) * w2 * & |
---|
| 510 | rmask(j,i,sr) |
---|
| 511 | ENDDO |
---|
| 512 | ENDDO |
---|
| 513 | ENDDO |
---|
| 514 | ENDIF |
---|
| 515 | |
---|
| 516 | ! |
---|
[1] | 517 | !-- Horizontally averaged profiles of the vertical fluxes |
---|
[667] | 518 | |
---|
[1] | 519 | !$OMP DO |
---|
| 520 | DO i = nxl, nxr |
---|
| 521 | DO j = nys, nyn |
---|
| 522 | ! |
---|
| 523 | !-- Subgridscale fluxes (without Prandtl layer from k=nzb, |
---|
| 524 | !-- oterwise from k=nzb+1) |
---|
[132] | 525 | !-- NOTE: for simplicity, nzb_diff_s_inner is used below, although |
---|
[1] | 526 | !-- ---- strictly speaking the following k-loop would have to be |
---|
| 527 | !-- split up according to the staggered grid. |
---|
[132] | 528 | !-- However, this implies no error since staggered velocity |
---|
| 529 | !-- components are zero at the walls and inside buildings. |
---|
| 530 | |
---|
| 531 | DO k = nzb_diff_s_inner(j,i)-1, nzt_diff |
---|
[1] | 532 | ! |
---|
| 533 | !-- Momentum flux w"u" |
---|
| 534 | sums_l(k,12,tn) = sums_l(k,12,tn) - 0.25 * ( & |
---|
| 535 | km(k,j,i)+km(k+1,j,i)+km(k,j,i-1)+km(k+1,j,i-1) & |
---|
| 536 | ) * ( & |
---|
| 537 | ( u(k+1,j,i) - u(k,j,i) ) * ddzu(k+1) & |
---|
| 538 | + ( w(k,j,i) - w(k,j,i-1) ) * ddx & |
---|
| 539 | ) * rmask(j,i,sr) |
---|
| 540 | ! |
---|
| 541 | !-- Momentum flux w"v" |
---|
| 542 | sums_l(k,14,tn) = sums_l(k,14,tn) - 0.25 * ( & |
---|
| 543 | km(k,j,i)+km(k+1,j,i)+km(k,j-1,i)+km(k+1,j-1,i) & |
---|
| 544 | ) * ( & |
---|
| 545 | ( v(k+1,j,i) - v(k,j,i) ) * ddzu(k+1) & |
---|
| 546 | + ( w(k,j,i) - w(k,j-1,i) ) * ddy & |
---|
| 547 | ) * rmask(j,i,sr) |
---|
| 548 | ! |
---|
| 549 | !-- Heat flux w"pt" |
---|
| 550 | sums_l(k,16,tn) = sums_l(k,16,tn) & |
---|
| 551 | - 0.5 * ( kh(k,j,i) + kh(k+1,j,i) ) & |
---|
| 552 | * ( pt(k+1,j,i) - pt(k,j,i) ) & |
---|
| 553 | * ddzu(k+1) * rmask(j,i,sr) |
---|
| 554 | |
---|
| 555 | |
---|
| 556 | ! |
---|
[96] | 557 | !-- Salinity flux w"sa" |
---|
| 558 | IF ( ocean ) THEN |
---|
| 559 | sums_l(k,65,tn) = sums_l(k,65,tn) & |
---|
| 560 | - 0.5 * ( kh(k,j,i) + kh(k+1,j,i) ) & |
---|
| 561 | * ( sa(k+1,j,i) - sa(k,j,i) ) & |
---|
| 562 | * ddzu(k+1) * rmask(j,i,sr) |
---|
| 563 | ENDIF |
---|
| 564 | |
---|
| 565 | ! |
---|
[1] | 566 | !-- Buoyancy flux, water flux (humidity flux) w"q" |
---|
[75] | 567 | IF ( humidity ) THEN |
---|
[1] | 568 | sums_l(k,45,tn) = sums_l(k,45,tn) & |
---|
| 569 | - 0.5 * ( kh(k,j,i) + kh(k+1,j,i) ) & |
---|
| 570 | * ( vpt(k+1,j,i) - vpt(k,j,i) ) & |
---|
| 571 | * ddzu(k+1) * rmask(j,i,sr) |
---|
| 572 | sums_l(k,48,tn) = sums_l(k,48,tn) & |
---|
| 573 | - 0.5 * ( kh(k,j,i) + kh(k+1,j,i) ) & |
---|
| 574 | * ( q(k+1,j,i) - q(k,j,i) ) & |
---|
| 575 | * ddzu(k+1) * rmask(j,i,sr) |
---|
| 576 | IF ( cloud_physics ) THEN |
---|
| 577 | sums_l(k,51,tn) = sums_l(k,51,tn) & |
---|
| 578 | - 0.5 * ( kh(k,j,i) + kh(k+1,j,i) ) & |
---|
| 579 | * ( ( q(k+1,j,i) - ql(k+1,j,i) )& |
---|
| 580 | - ( q(k,j,i) - ql(k,j,i) ) ) & |
---|
| 581 | * ddzu(k+1) * rmask(j,i,sr) |
---|
| 582 | ENDIF |
---|
| 583 | ENDIF |
---|
| 584 | |
---|
| 585 | ! |
---|
| 586 | !-- Passive scalar flux |
---|
| 587 | IF ( passive_scalar ) THEN |
---|
| 588 | sums_l(k,48,tn) = sums_l(k,48,tn) & |
---|
| 589 | - 0.5 * ( kh(k,j,i) + kh(k+1,j,i) ) & |
---|
| 590 | * ( q(k+1,j,i) - q(k,j,i) ) & |
---|
| 591 | * ddzu(k+1) * rmask(j,i,sr) |
---|
| 592 | ENDIF |
---|
| 593 | |
---|
| 594 | ENDDO |
---|
| 595 | |
---|
| 596 | ! |
---|
| 597 | !-- Subgridscale fluxes in the Prandtl layer |
---|
| 598 | IF ( use_surface_fluxes ) THEN |
---|
| 599 | sums_l(nzb,12,tn) = sums_l(nzb,12,tn) + & |
---|
| 600 | usws(j,i) * rmask(j,i,sr) ! w"u" |
---|
| 601 | sums_l(nzb,14,tn) = sums_l(nzb,14,tn) + & |
---|
| 602 | vsws(j,i) * rmask(j,i,sr) ! w"v" |
---|
| 603 | sums_l(nzb,16,tn) = sums_l(nzb,16,tn) + & |
---|
| 604 | shf(j,i) * rmask(j,i,sr) ! w"pt" |
---|
| 605 | sums_l(nzb,58,tn) = sums_l(nzb,58,tn) + & |
---|
| 606 | 0.0 * rmask(j,i,sr) ! u"pt" |
---|
| 607 | sums_l(nzb,61,tn) = sums_l(nzb,61,tn) + & |
---|
| 608 | 0.0 * rmask(j,i,sr) ! v"pt" |
---|
[96] | 609 | IF ( ocean ) THEN |
---|
| 610 | sums_l(nzb,65,tn) = sums_l(nzb,65,tn) + & |
---|
| 611 | saswsb(j,i) * rmask(j,i,sr) ! w"sa" |
---|
| 612 | ENDIF |
---|
[75] | 613 | IF ( humidity ) THEN |
---|
[1] | 614 | sums_l(nzb,48,tn) = sums_l(nzb,48,tn) + & |
---|
| 615 | qsws(j,i) * rmask(j,i,sr) ! w"q" (w"qv") |
---|
| 616 | IF ( cloud_physics ) THEN |
---|
| 617 | sums_l(nzb,45,tn) = sums_l(nzb,45,tn) + ( & |
---|
| 618 | ( 1.0 + 0.61 * q(nzb,j,i) ) * & |
---|
| 619 | shf(j,i) + 0.61 * pt(nzb,j,i) * & |
---|
| 620 | qsws(j,i) & |
---|
| 621 | ) |
---|
| 622 | ! |
---|
| 623 | !-- Formula does not work if ql(nzb) /= 0.0 |
---|
| 624 | sums_l(nzb,51,tn) = sums_l(nzb,51,tn) + & ! w"q" (w"qv") |
---|
| 625 | qsws(j,i) * rmask(j,i,sr) |
---|
| 626 | ENDIF |
---|
| 627 | ENDIF |
---|
| 628 | IF ( passive_scalar ) THEN |
---|
| 629 | sums_l(nzb,48,tn) = sums_l(nzb,48,tn) + & |
---|
| 630 | qsws(j,i) * rmask(j,i,sr) ! w"q" (w"qv") |
---|
| 631 | ENDIF |
---|
| 632 | ENDIF |
---|
| 633 | |
---|
| 634 | ! |
---|
[19] | 635 | !-- Subgridscale fluxes at the top surface |
---|
| 636 | IF ( use_top_fluxes ) THEN |
---|
[550] | 637 | sums_l(nzt:nzt+1,12,tn) = sums_l(nzt:nzt+1,12,tn) + & |
---|
[102] | 638 | uswst(j,i) * rmask(j,i,sr) ! w"u" |
---|
[550] | 639 | sums_l(nzt:nzt+1,14,tn) = sums_l(nzt:nzt+1,14,tn) + & |
---|
[102] | 640 | vswst(j,i) * rmask(j,i,sr) ! w"v" |
---|
[550] | 641 | sums_l(nzt:nzt+1,16,tn) = sums_l(nzt:nzt+1,16,tn) + & |
---|
[19] | 642 | tswst(j,i) * rmask(j,i,sr) ! w"pt" |
---|
[550] | 643 | sums_l(nzt:nzt+1,58,tn) = sums_l(nzt:nzt+1,58,tn) + & |
---|
[19] | 644 | 0.0 * rmask(j,i,sr) ! u"pt" |
---|
[550] | 645 | sums_l(nzt:nzt+1,61,tn) = sums_l(nzt:nzt+1,61,tn) + & |
---|
| 646 | 0.0 * rmask(j,i,sr) ! v"pt" |
---|
| 647 | |
---|
[96] | 648 | IF ( ocean ) THEN |
---|
| 649 | sums_l(nzt,65,tn) = sums_l(nzt,65,tn) + & |
---|
| 650 | saswst(j,i) * rmask(j,i,sr) ! w"sa" |
---|
| 651 | ENDIF |
---|
[75] | 652 | IF ( humidity ) THEN |
---|
[19] | 653 | sums_l(nzt,48,tn) = sums_l(nzt,48,tn) + & |
---|
[388] | 654 | qswst(j,i) * rmask(j,i,sr) ! w"q" (w"qv") |
---|
[19] | 655 | IF ( cloud_physics ) THEN |
---|
| 656 | sums_l(nzt,45,tn) = sums_l(nzt,45,tn) + ( & |
---|
| 657 | ( 1.0 + 0.61 * q(nzt,j,i) ) * & |
---|
| 658 | tswst(j,i) + 0.61 * pt(nzt,j,i) * & |
---|
| 659 | qsws(j,i) & |
---|
| 660 | ) |
---|
| 661 | ! |
---|
| 662 | !-- Formula does not work if ql(nzb) /= 0.0 |
---|
| 663 | sums_l(nzt,51,tn) = sums_l(nzt,51,tn) + & ! w"q" (w"qv") |
---|
| 664 | qswst(j,i) * rmask(j,i,sr) |
---|
| 665 | ENDIF |
---|
| 666 | ENDIF |
---|
| 667 | IF ( passive_scalar ) THEN |
---|
| 668 | sums_l(nzt,48,tn) = sums_l(nzt,48,tn) + & |
---|
[388] | 669 | qswst(j,i) * rmask(j,i,sr) ! w"q" (w"qv") |
---|
[19] | 670 | ENDIF |
---|
| 671 | ENDIF |
---|
| 672 | |
---|
| 673 | ! |
---|
[1] | 674 | !-- Resolved fluxes (can be computed for all horizontal points) |
---|
[132] | 675 | !-- NOTE: for simplicity, nzb_s_inner is used below, although strictly |
---|
[1] | 676 | !-- ---- speaking the following k-loop would have to be split up and |
---|
| 677 | !-- rearranged according to the staggered grid. |
---|
[132] | 678 | DO k = nzb_s_inner(j,i), nzt |
---|
[1] | 679 | ust = 0.5 * ( u(k,j,i) - hom(k,1,1,sr) + & |
---|
| 680 | u(k+1,j,i) - hom(k+1,1,1,sr) ) |
---|
| 681 | vst = 0.5 * ( v(k,j,i) - hom(k,1,2,sr) + & |
---|
| 682 | v(k+1,j,i) - hom(k+1,1,2,sr) ) |
---|
| 683 | pts = 0.5 * ( pt(k,j,i) - hom(k,1,4,sr) + & |
---|
| 684 | pt(k+1,j,i) - hom(k+1,1,4,sr) ) |
---|
[667] | 685 | |
---|
[1] | 686 | !-- Higher moments |
---|
| 687 | sums_l(k,35,tn) = sums_l(k,35,tn) + pts * w(k,j,i)**2 * & |
---|
| 688 | rmask(j,i,sr) |
---|
| 689 | sums_l(k,36,tn) = sums_l(k,36,tn) + pts**2 * w(k,j,i) * & |
---|
| 690 | rmask(j,i,sr) |
---|
| 691 | |
---|
| 692 | ! |
---|
[96] | 693 | !-- Salinity flux and density (density does not belong to here, |
---|
[97] | 694 | !-- but so far there is no other suitable place to calculate) |
---|
[96] | 695 | IF ( ocean ) THEN |
---|
[667] | 696 | IF( .NOT. ws_scheme_sca ) THEN |
---|
| 697 | pts = 0.5 * ( sa(k,j,i) - hom(k,1,23,sr) + & |
---|
[96] | 698 | sa(k+1,j,i) - hom(k+1,1,23,sr) ) |
---|
[667] | 699 | sums_l(k,66,tn) = sums_l(k,66,tn) + pts * w(k,j,i) * & |
---|
[96] | 700 | rmask(j,i,sr) |
---|
[667] | 701 | ENDIF |
---|
[96] | 702 | sums_l(k,64,tn) = sums_l(k,64,tn) + rho(k,j,i) * & |
---|
| 703 | rmask(j,i,sr) |
---|
[388] | 704 | sums_l(k,71,tn) = sums_l(k,71,tn) + prho(k,j,i) * & |
---|
| 705 | rmask(j,i,sr) |
---|
[96] | 706 | ENDIF |
---|
| 707 | |
---|
| 708 | ! |
---|
[1] | 709 | !-- Buoyancy flux, water flux, humidity flux and liquid water |
---|
| 710 | !-- content |
---|
[75] | 711 | IF ( humidity ) THEN |
---|
[1] | 712 | pts = 0.5 * ( vpt(k,j,i) - hom(k,1,44,sr) + & |
---|
| 713 | vpt(k+1,j,i) - hom(k+1,1,44,sr) ) |
---|
| 714 | sums_l(k,46,tn) = sums_l(k,46,tn) + pts * w(k,j,i) * & |
---|
| 715 | rmask(j,i,sr) |
---|
[667] | 716 | |
---|
[1] | 717 | IF ( cloud_physics .OR. cloud_droplets ) THEN |
---|
| 718 | pts = 0.5 * & |
---|
| 719 | ( ( q(k,j,i) - ql(k,j,i) ) - hom(k,1,42,sr) & |
---|
| 720 | + ( q(k+1,j,i) - ql(k+1,j,i) ) - hom(k+1,1,42,sr) ) |
---|
| 721 | sums_l(k,52,tn) = sums_l(k,52,tn) + pts * w(k,j,i) * & |
---|
| 722 | rmask(j,i,sr) |
---|
| 723 | sums_l(k,54,tn) = sums_l(k,54,tn) + ql(k,j,i) * & |
---|
| 724 | rmask(j,i,sr) |
---|
| 725 | ENDIF |
---|
| 726 | ENDIF |
---|
| 727 | |
---|
| 728 | ! |
---|
| 729 | !-- Passive scalar flux |
---|
[667] | 730 | IF ( passive_scalar .AND. ( .NOT. ws_scheme_sca )) THEN |
---|
[1] | 731 | pts = 0.5 * ( q(k,j,i) - hom(k,1,41,sr) + & |
---|
| 732 | q(k+1,j,i) - hom(k+1,1,41,sr) ) |
---|
| 733 | sums_l(k,49,tn) = sums_l(k,49,tn) + pts * w(k,j,i) * & |
---|
| 734 | rmask(j,i,sr) |
---|
| 735 | ENDIF |
---|
| 736 | |
---|
| 737 | ! |
---|
| 738 | !-- Energy flux w*e* |
---|
[667] | 739 | !-- has to be adjusted |
---|
| 740 | sums_l(k,37,tn) = sums_l(k,37,tn) + w(k,j,i) * 0.5 * & |
---|
| 741 | ( ust**2 + vst**2 + w(k,j,i)**2 )& |
---|
| 742 | * rmask(j,i,sr) |
---|
[1] | 743 | ENDDO |
---|
| 744 | ENDDO |
---|
| 745 | ENDDO |
---|
[667] | 746 | !- for reasons of speed optimization the loop is splitted, to avoid if-else |
---|
| 747 | !- statements inside the loop |
---|
| 748 | !- Fluxes which have been computed in part directly inside the advection routines |
---|
| 749 | !- treated seperatly. |
---|
| 750 | !- First treat the momentum fluxes |
---|
| 751 | IF ( .NOT. ws_scheme_mom ) THEN |
---|
| 752 | !$OMP DO |
---|
| 753 | DO i = nxl, nxr |
---|
| 754 | DO j = nys, nyn |
---|
| 755 | DO k = nzb_diff_s_inner(j,i)-1, nzt_diff |
---|
| 756 | ust = 0.5 * ( u(k,j,i) - hom(k,1,1,sr) + & |
---|
| 757 | u(k+1,j,i) - hom(k+1,1,1,sr) ) |
---|
| 758 | vst = 0.5 * ( v(k,j,i) - hom(k,1,2,sr) + & |
---|
| 759 | v(k+1,j,i) - hom(k+1,1,2,sr) ) |
---|
| 760 | ! |
---|
| 761 | !-- Momentum flux w*u* |
---|
| 762 | sums_l(k,13,tn) = sums_l(k,13,tn) + 0.5 * & |
---|
| 763 | ( w(k,j,i-1) + w(k,j,i) ) & |
---|
| 764 | * ust * rmask(j,i,sr) |
---|
| 765 | ! |
---|
| 766 | !-- Momentum flux w*v* |
---|
| 767 | sums_l(k,15,tn) = sums_l(k,15,tn) + 0.5 * & |
---|
| 768 | ( w(k,j-1,i) + w(k,j,i) ) & |
---|
| 769 | * vst * rmask(j,i,sr) |
---|
| 770 | ENDDO |
---|
| 771 | ENDDO |
---|
| 772 | ENDDO |
---|
[1] | 773 | |
---|
[667] | 774 | ENDIF |
---|
| 775 | IF ( .NOT. ws_scheme_sca ) THEN |
---|
| 776 | !$OMP DO |
---|
| 777 | DO i = nxl, nxr |
---|
| 778 | DO j = nys, nyn |
---|
| 779 | DO k = nzb_diff_s_inner(j,i) - 1, nzt_diff |
---|
| 780 | !- vertical heat flux |
---|
| 781 | sums_l(k,17,tn) = sums_l(k,17,tn) + 0.5 * & |
---|
| 782 | ( pt(k,j,i) - hom(k,1,4,sr) + & |
---|
| 783 | pt(k+1,j,i) - hom(k+1,1,4,sr) ) & |
---|
| 784 | * w(k,j,i) * rmask(j,i,sr) |
---|
| 785 | IF ( humidity ) THEN |
---|
| 786 | pts = 0.5 * ( q(k,j,i) - hom(k,1,41,sr) + & |
---|
| 787 | q(k+1,j,i) - hom(k+1,1,41,sr) ) |
---|
| 788 | sums_l(k,49,tn) = sums_l(k,49,tn) + pts * w(k,j,i) * & |
---|
| 789 | rmask(j,i,sr) |
---|
| 790 | ENDIF |
---|
| 791 | ENDDO |
---|
| 792 | ENDDO |
---|
| 793 | ENDDO |
---|
| 794 | |
---|
| 795 | ENDIF |
---|
| 796 | |
---|
| 797 | |
---|
[1] | 798 | ! |
---|
[97] | 799 | !-- Density at top follows Neumann condition |
---|
[388] | 800 | IF ( ocean ) THEN |
---|
| 801 | sums_l(nzt+1,64,tn) = sums_l(nzt,64,tn) |
---|
| 802 | sums_l(nzt+1,71,tn) = sums_l(nzt,71,tn) |
---|
| 803 | ENDIF |
---|
[97] | 804 | |
---|
| 805 | ! |
---|
[1] | 806 | !-- Divergence of vertical flux of resolved scale energy and pressure |
---|
[106] | 807 | !-- fluctuations as well as flux of pressure fluctuation itself (68). |
---|
| 808 | !-- First calculate the products, then the divergence. |
---|
[1] | 809 | !-- Calculation is time consuming. Do it only, if profiles shall be plotted. |
---|
[106] | 810 | IF ( hom(nzb+1,2,55,0) /= 0.0 .OR. hom(nzb+1,2,68,0) /= 0.0 ) THEN |
---|
[1] | 811 | |
---|
| 812 | sums_ll = 0.0 ! local array |
---|
| 813 | |
---|
| 814 | !$OMP DO |
---|
| 815 | DO i = nxl, nxr |
---|
| 816 | DO j = nys, nyn |
---|
[132] | 817 | DO k = nzb_s_inner(j,i)+1, nzt |
---|
[1] | 818 | |
---|
| 819 | sums_ll(k,1) = sums_ll(k,1) + 0.5 * w(k,j,i) * ( & |
---|
| 820 | ( 0.25 * ( u(k,j,i)+u(k+1,j,i)+u(k,j,i+1)+u(k+1,j,i+1) & |
---|
[678] | 821 | - 0.5 * ( hom(k,1,1,sr) + hom(k+1,1,1,sr) ) & |
---|
[1] | 822 | ) )**2 & |
---|
| 823 | + ( 0.25 * ( v(k,j,i)+v(k+1,j,i)+v(k,j+1,i)+v(k+1,j+1,i) & |
---|
[678] | 824 | - 0.5 * ( hom(k,1,2,sr) + hom(k+1,1,2,sr) ) & |
---|
[1] | 825 | ) )**2 & |
---|
| 826 | + w(k,j,i)**2 ) |
---|
| 827 | |
---|
| 828 | sums_ll(k,2) = sums_ll(k,2) + 0.5 * w(k,j,i) & |
---|
| 829 | * ( p(k,j,i) + p(k+1,j,i) ) |
---|
| 830 | |
---|
| 831 | ENDDO |
---|
| 832 | ENDDO |
---|
| 833 | ENDDO |
---|
| 834 | sums_ll(0,1) = 0.0 ! because w is zero at the bottom |
---|
| 835 | sums_ll(nzt+1,1) = 0.0 |
---|
| 836 | sums_ll(0,2) = 0.0 |
---|
| 837 | sums_ll(nzt+1,2) = 0.0 |
---|
| 838 | |
---|
[678] | 839 | DO k = nzb+1, nzt |
---|
[1] | 840 | sums_l(k,55,tn) = ( sums_ll(k,1) - sums_ll(k-1,1) ) * ddzw(k) |
---|
| 841 | sums_l(k,56,tn) = ( sums_ll(k,2) - sums_ll(k-1,2) ) * ddzw(k) |
---|
[106] | 842 | sums_l(k,68,tn) = sums_ll(k,2) |
---|
[1] | 843 | ENDDO |
---|
| 844 | sums_l(nzb,55,tn) = sums_l(nzb+1,55,tn) |
---|
| 845 | sums_l(nzb,56,tn) = sums_l(nzb+1,56,tn) |
---|
[106] | 846 | sums_l(nzb,68,tn) = 0.0 ! because w* = 0 at nzb |
---|
[1] | 847 | |
---|
| 848 | ENDIF |
---|
| 849 | |
---|
| 850 | ! |
---|
[106] | 851 | !-- Divergence of vertical flux of SGS TKE and the flux itself (69) |
---|
| 852 | IF ( hom(nzb+1,2,57,0) /= 0.0 .OR. hom(nzb+1,2,69,0) /= 0.0 ) THEN |
---|
[1] | 853 | |
---|
| 854 | !$OMP DO |
---|
| 855 | DO i = nxl, nxr |
---|
| 856 | DO j = nys, nyn |
---|
[132] | 857 | DO k = nzb_s_inner(j,i)+1, nzt |
---|
[1] | 858 | |
---|
[106] | 859 | sums_l(k,57,tn) = sums_l(k,57,tn) - 0.5 * ( & |
---|
[1] | 860 | (km(k,j,i)+km(k+1,j,i)) * (e(k+1,j,i)-e(k,j,i)) * ddzu(k+1) & |
---|
| 861 | - (km(k-1,j,i)+km(k,j,i)) * (e(k,j,i)-e(k-1,j,i)) * ddzu(k) & |
---|
[106] | 862 | ) * ddzw(k) |
---|
[1] | 863 | |
---|
[106] | 864 | sums_l(k,69,tn) = sums_l(k,69,tn) - 0.5 * ( & |
---|
| 865 | (km(k,j,i)+km(k+1,j,i)) * (e(k+1,j,i)-e(k,j,i)) * ddzu(k+1) & |
---|
| 866 | ) |
---|
| 867 | |
---|
[1] | 868 | ENDDO |
---|
| 869 | ENDDO |
---|
| 870 | ENDDO |
---|
| 871 | sums_l(nzb,57,tn) = sums_l(nzb+1,57,tn) |
---|
[106] | 872 | sums_l(nzb,69,tn) = sums_l(nzb+1,69,tn) |
---|
[1] | 873 | |
---|
| 874 | ENDIF |
---|
| 875 | |
---|
| 876 | ! |
---|
| 877 | !-- Horizontal heat fluxes (subgrid, resolved, total). |
---|
| 878 | !-- Do it only, if profiles shall be plotted. |
---|
| 879 | IF ( hom(nzb+1,2,58,0) /= 0.0 ) THEN |
---|
| 880 | |
---|
| 881 | !$OMP DO |
---|
| 882 | DO i = nxl, nxr |
---|
| 883 | DO j = nys, nyn |
---|
[132] | 884 | DO k = nzb_s_inner(j,i)+1, nzt |
---|
[1] | 885 | ! |
---|
| 886 | !-- Subgrid horizontal heat fluxes u"pt", v"pt" |
---|
| 887 | sums_l(k,58,tn) = sums_l(k,58,tn) - 0.5 * & |
---|
| 888 | ( kh(k,j,i) + kh(k,j,i-1) ) & |
---|
| 889 | * ( pt(k,j,i-1) - pt(k,j,i) ) & |
---|
| 890 | * ddx * rmask(j,i,sr) |
---|
| 891 | sums_l(k,61,tn) = sums_l(k,61,tn) - 0.5 * & |
---|
| 892 | ( kh(k,j,i) + kh(k,j-1,i) ) & |
---|
| 893 | * ( pt(k,j-1,i) - pt(k,j,i) ) & |
---|
| 894 | * ddy * rmask(j,i,sr) |
---|
| 895 | ! |
---|
| 896 | !-- Resolved horizontal heat fluxes u*pt*, v*pt* |
---|
| 897 | sums_l(k,59,tn) = sums_l(k,59,tn) + & |
---|
| 898 | ( u(k,j,i) - hom(k,1,1,sr) ) & |
---|
| 899 | * 0.5 * ( pt(k,j,i-1) - hom(k,1,4,sr) + & |
---|
| 900 | pt(k,j,i) - hom(k,1,4,sr) ) |
---|
| 901 | pts = 0.5 * ( pt(k,j-1,i) - hom(k,1,4,sr) + & |
---|
| 902 | pt(k,j,i) - hom(k,1,4,sr) ) |
---|
| 903 | sums_l(k,62,tn) = sums_l(k,62,tn) + & |
---|
| 904 | ( v(k,j,i) - hom(k,1,2,sr) ) & |
---|
| 905 | * 0.5 * ( pt(k,j-1,i) - hom(k,1,4,sr) + & |
---|
| 906 | pt(k,j,i) - hom(k,1,4,sr) ) |
---|
| 907 | ENDDO |
---|
| 908 | ENDDO |
---|
| 909 | ENDDO |
---|
| 910 | ! |
---|
| 911 | !-- Fluxes at the surface must be zero (e.g. due to the Prandtl-layer) |
---|
[97] | 912 | sums_l(nzb,58,tn) = 0.0 |
---|
| 913 | sums_l(nzb,59,tn) = 0.0 |
---|
| 914 | sums_l(nzb,60,tn) = 0.0 |
---|
| 915 | sums_l(nzb,61,tn) = 0.0 |
---|
| 916 | sums_l(nzb,62,tn) = 0.0 |
---|
| 917 | sums_l(nzb,63,tn) = 0.0 |
---|
[1] | 918 | |
---|
| 919 | ENDIF |
---|
[87] | 920 | |
---|
| 921 | ! |
---|
| 922 | !-- Calculate the user-defined profiles |
---|
| 923 | CALL user_statistics( 'profiles', sr, tn ) |
---|
[1] | 924 | !$OMP END PARALLEL |
---|
| 925 | |
---|
| 926 | ! |
---|
| 927 | !-- Summation of thread sums |
---|
| 928 | IF ( threads_per_task > 1 ) THEN |
---|
| 929 | DO i = 1, threads_per_task-1 |
---|
| 930 | sums_l(:,3,0) = sums_l(:,3,0) + sums_l(:,3,i) |
---|
| 931 | sums_l(:,4:40,0) = sums_l(:,4:40,0) + sums_l(:,4:40,i) |
---|
[87] | 932 | sums_l(:,45:pr_palm,0) = sums_l(:,45:pr_palm,0) + & |
---|
| 933 | sums_l(:,45:pr_palm,i) |
---|
| 934 | IF ( max_pr_user > 0 ) THEN |
---|
| 935 | sums_l(:,pr_palm+1:pr_palm+max_pr_user,0) = & |
---|
| 936 | sums_l(:,pr_palm+1:pr_palm+max_pr_user,0) + & |
---|
| 937 | sums_l(:,pr_palm+1:pr_palm+max_pr_user,i) |
---|
| 938 | ENDIF |
---|
[1] | 939 | ENDDO |
---|
| 940 | ENDIF |
---|
| 941 | |
---|
| 942 | #if defined( __parallel ) |
---|
[667] | 943 | |
---|
[1] | 944 | ! |
---|
| 945 | !-- Compute total sum from local sums |
---|
[622] | 946 | IF ( collective_wait ) CALL MPI_BARRIER( comm2d, ierr ) |
---|
[1] | 947 | CALL MPI_ALLREDUCE( sums_l(nzb,1,0), sums(nzb,1), ngp_sums, MPI_REAL, & |
---|
| 948 | MPI_SUM, comm2d, ierr ) |
---|
| 949 | #else |
---|
| 950 | sums = sums_l(:,:,0) |
---|
| 951 | #endif |
---|
| 952 | |
---|
| 953 | ! |
---|
| 954 | !-- Final values are obtained by division by the total number of grid points |
---|
| 955 | !-- used for summation. After that store profiles. |
---|
| 956 | !-- Profiles: |
---|
| 957 | DO k = nzb, nzt+1 |
---|
[132] | 958 | sums(k,3) = sums(k,3) / ngp_2dh(sr) |
---|
[142] | 959 | sums(k,8:11) = sums(k,8:11) / ngp_2dh_s_inner(k,sr) |
---|
[132] | 960 | sums(k,12:22) = sums(k,12:22) / ngp_2dh(sr) |
---|
| 961 | sums(k,23:29) = sums(k,23:29) / ngp_2dh_s_inner(k,sr) |
---|
| 962 | sums(k,30:32) = sums(k,30:32) / ngp_2dh(sr) |
---|
[142] | 963 | sums(k,33:34) = sums(k,33:34) / ngp_2dh_s_inner(k,sr) |
---|
| 964 | sums(k,35:39) = sums(k,35:39) / ngp_2dh(sr) |
---|
[132] | 965 | sums(k,40) = sums(k,40) / ngp_2dh_s_inner(k,sr) |
---|
| 966 | sums(k,45:53) = sums(k,45:53) / ngp_2dh(sr) |
---|
| 967 | sums(k,54) = sums(k,54) / ngp_2dh_s_inner(k,sr) |
---|
| 968 | sums(k,55:63) = sums(k,55:63) / ngp_2dh(sr) |
---|
| 969 | sums(k,64) = sums(k,64) / ngp_2dh_s_inner(k,sr) |
---|
| 970 | sums(k,65:69) = sums(k,65:69) / ngp_2dh(sr) |
---|
| 971 | sums(k,70:pr_palm-2) = sums(k,70:pr_palm-2)/ ngp_2dh_s_inner(k,sr) |
---|
[1] | 972 | ENDDO |
---|
[667] | 973 | |
---|
[1] | 974 | !-- Upstream-parts |
---|
[87] | 975 | sums(nzb:nzb+11,pr_palm-1) = sums(nzb:nzb+11,pr_palm-1) / ngp_3d(sr) |
---|
[1] | 976 | !-- u* and so on |
---|
[87] | 977 | !-- As sums(nzb:nzb+3,pr_palm) are full 2D arrays (us, usws, vsws, ts) whose |
---|
[1] | 978 | !-- size is always ( nx + 1 ) * ( ny + 1 ), defined at the first grid layer |
---|
| 979 | !-- above the topography, they are being divided by ngp_2dh(sr) |
---|
[87] | 980 | sums(nzb:nzb+3,pr_palm) = sums(nzb:nzb+3,pr_palm) / & |
---|
[1] | 981 | ngp_2dh(sr) |
---|
[197] | 982 | sums(nzb+12,pr_palm) = sums(nzb+12,pr_palm) / & ! qs |
---|
| 983 | ngp_2dh(sr) |
---|
[1] | 984 | !-- eges, e* |
---|
[87] | 985 | sums(nzb+4:nzb+5,pr_palm) = sums(nzb+4:nzb+5,pr_palm) / & |
---|
[132] | 986 | ngp_3d(sr) |
---|
[1] | 987 | !-- Old and new divergence |
---|
[87] | 988 | sums(nzb+9:nzb+10,pr_palm) = sums(nzb+9:nzb+10,pr_palm) / & |
---|
[1] | 989 | ngp_3d_inner(sr) |
---|
| 990 | |
---|
[87] | 991 | !-- User-defined profiles |
---|
| 992 | IF ( max_pr_user > 0 ) THEN |
---|
| 993 | DO k = nzb, nzt+1 |
---|
| 994 | sums(k,pr_palm+1:pr_palm+max_pr_user) = & |
---|
| 995 | sums(k,pr_palm+1:pr_palm+max_pr_user) / & |
---|
[132] | 996 | ngp_2dh_s_inner(k,sr) |
---|
[87] | 997 | ENDDO |
---|
| 998 | ENDIF |
---|
[1] | 999 | ! |
---|
| 1000 | !-- Collect horizontal average in hom. |
---|
| 1001 | !-- Compute deduced averages (e.g. total heat flux) |
---|
| 1002 | hom(:,1,3,sr) = sums(:,3) ! w |
---|
| 1003 | hom(:,1,8,sr) = sums(:,8) ! e profiles 5-7 are initial profiles |
---|
| 1004 | hom(:,1,9,sr) = sums(:,9) ! km |
---|
| 1005 | hom(:,1,10,sr) = sums(:,10) ! kh |
---|
| 1006 | hom(:,1,11,sr) = sums(:,11) ! l |
---|
| 1007 | hom(:,1,12,sr) = sums(:,12) ! w"u" |
---|
| 1008 | hom(:,1,13,sr) = sums(:,13) ! w*u* |
---|
| 1009 | hom(:,1,14,sr) = sums(:,14) ! w"v" |
---|
| 1010 | hom(:,1,15,sr) = sums(:,15) ! w*v* |
---|
| 1011 | hom(:,1,16,sr) = sums(:,16) ! w"pt" |
---|
| 1012 | hom(:,1,17,sr) = sums(:,17) ! w*pt* |
---|
| 1013 | hom(:,1,18,sr) = sums(:,16) + sums(:,17) ! wpt |
---|
| 1014 | hom(:,1,19,sr) = sums(:,12) + sums(:,13) ! wu |
---|
| 1015 | hom(:,1,20,sr) = sums(:,14) + sums(:,15) ! wv |
---|
| 1016 | hom(:,1,21,sr) = sums(:,21) ! w*pt*BC |
---|
| 1017 | hom(:,1,22,sr) = sums(:,16) + sums(:,21) ! wptBC |
---|
[96] | 1018 | ! profile 24 is initial profile (sa) |
---|
| 1019 | ! profiles 25-29 left empty for initial |
---|
[1] | 1020 | ! profiles |
---|
| 1021 | hom(:,1,30,sr) = sums(:,30) ! u*2 |
---|
| 1022 | hom(:,1,31,sr) = sums(:,31) ! v*2 |
---|
| 1023 | hom(:,1,32,sr) = sums(:,32) ! w*2 |
---|
| 1024 | hom(:,1,33,sr) = sums(:,33) ! pt*2 |
---|
| 1025 | hom(:,1,34,sr) = sums(:,34) ! e* |
---|
| 1026 | hom(:,1,35,sr) = sums(:,35) ! w*2pt* |
---|
| 1027 | hom(:,1,36,sr) = sums(:,36) ! w*pt*2 |
---|
| 1028 | hom(:,1,37,sr) = sums(:,37) ! w*e* |
---|
| 1029 | hom(:,1,38,sr) = sums(:,38) ! w*3 |
---|
| 1030 | hom(:,1,39,sr) = sums(:,38) / ( sums(:,32) + 1E-20 )**1.5 ! Sw |
---|
| 1031 | hom(:,1,40,sr) = sums(:,40) ! p |
---|
[531] | 1032 | hom(:,1,45,sr) = sums(:,45) ! w"vpt" |
---|
[1] | 1033 | hom(:,1,46,sr) = sums(:,46) ! w*vpt* |
---|
| 1034 | hom(:,1,47,sr) = sums(:,45) + sums(:,46) ! wvpt |
---|
| 1035 | hom(:,1,48,sr) = sums(:,48) ! w"q" (w"qv") |
---|
| 1036 | hom(:,1,49,sr) = sums(:,49) ! w*q* (w*qv*) |
---|
| 1037 | hom(:,1,50,sr) = sums(:,48) + sums(:,49) ! wq (wqv) |
---|
| 1038 | hom(:,1,51,sr) = sums(:,51) ! w"qv" |
---|
| 1039 | hom(:,1,52,sr) = sums(:,52) ! w*qv* |
---|
| 1040 | hom(:,1,53,sr) = sums(:,52) + sums(:,51) ! wq (wqv) |
---|
| 1041 | hom(:,1,54,sr) = sums(:,54) ! ql |
---|
| 1042 | hom(:,1,55,sr) = sums(:,55) ! w*u*u*/dz |
---|
| 1043 | hom(:,1,56,sr) = sums(:,56) ! w*p*/dz |
---|
[106] | 1044 | hom(:,1,57,sr) = sums(:,57) ! ( w"e + w"p"/rho )/dz |
---|
[1] | 1045 | hom(:,1,58,sr) = sums(:,58) ! u"pt" |
---|
| 1046 | hom(:,1,59,sr) = sums(:,59) ! u*pt* |
---|
| 1047 | hom(:,1,60,sr) = sums(:,58) + sums(:,59) ! upt_t |
---|
| 1048 | hom(:,1,61,sr) = sums(:,61) ! v"pt" |
---|
| 1049 | hom(:,1,62,sr) = sums(:,62) ! v*pt* |
---|
| 1050 | hom(:,1,63,sr) = sums(:,61) + sums(:,62) ! vpt_t |
---|
[96] | 1051 | hom(:,1,64,sr) = sums(:,64) ! rho |
---|
| 1052 | hom(:,1,65,sr) = sums(:,65) ! w"sa" |
---|
| 1053 | hom(:,1,66,sr) = sums(:,66) ! w*sa* |
---|
| 1054 | hom(:,1,67,sr) = sums(:,65) + sums(:,66) ! wsa |
---|
[106] | 1055 | hom(:,1,68,sr) = sums(:,68) ! w*p* |
---|
| 1056 | hom(:,1,69,sr) = sums(:,69) ! w"e + w"p"/rho |
---|
[197] | 1057 | hom(:,1,70,sr) = sums(:,70) ! q*2 |
---|
[388] | 1058 | hom(:,1,71,sr) = sums(:,71) ! prho |
---|
[531] | 1059 | hom(:,1,72,sr) = hyp * 1E-4 ! hyp in dbar |
---|
[1] | 1060 | |
---|
[87] | 1061 | hom(:,1,pr_palm-1,sr) = sums(:,pr_palm-1) |
---|
[1] | 1062 | ! upstream-parts u_x, u_y, u_z, v_x, |
---|
| 1063 | ! v_y, usw. (in last but one profile) |
---|
[667] | 1064 | hom(:,1,pr_palm,sr) = sums(:,pr_palm) |
---|
[1] | 1065 | ! u*, w'u', w'v', t* (in last profile) |
---|
| 1066 | |
---|
[87] | 1067 | IF ( max_pr_user > 0 ) THEN ! user-defined profiles |
---|
| 1068 | hom(:,1,pr_palm+1:pr_palm+max_pr_user,sr) = & |
---|
| 1069 | sums(:,pr_palm+1:pr_palm+max_pr_user) |
---|
| 1070 | ENDIF |
---|
| 1071 | |
---|
[1] | 1072 | ! |
---|
| 1073 | !-- Determine the boundary layer height using two different schemes. |
---|
[94] | 1074 | !-- First scheme: Starting from the Earth's (Ocean's) surface, look for the |
---|
| 1075 | !-- first relative minimum (maximum) of the total heat flux. |
---|
| 1076 | !-- The corresponding height is assumed as the boundary layer height, if it |
---|
| 1077 | !-- is less than 1.5 times the height where the heat flux becomes negative |
---|
| 1078 | !-- (positive) for the first time. |
---|
[1] | 1079 | z_i(1) = 0.0 |
---|
| 1080 | first = .TRUE. |
---|
[667] | 1081 | |
---|
[97] | 1082 | IF ( ocean ) THEN |
---|
| 1083 | DO k = nzt, nzb+1, -1 |
---|
[667] | 1084 | IF ( first .AND. hom(k,1,18,sr) < 0.0 & |
---|
| 1085 | .AND. abs(hom(k,1,18,sr)) > 1.0E-8) THEN |
---|
[97] | 1086 | first = .FALSE. |
---|
| 1087 | height = zw(k) |
---|
| 1088 | ENDIF |
---|
| 1089 | IF ( hom(k,1,18,sr) < 0.0 .AND. & |
---|
[667] | 1090 | abs(hom(k,1,18,sr)) > 1.0E-8 .AND. & |
---|
[97] | 1091 | hom(k-1,1,18,sr) > hom(k,1,18,sr) ) THEN |
---|
| 1092 | IF ( zw(k) < 1.5 * height ) THEN |
---|
| 1093 | z_i(1) = zw(k) |
---|
| 1094 | ELSE |
---|
| 1095 | z_i(1) = height |
---|
| 1096 | ENDIF |
---|
| 1097 | EXIT |
---|
| 1098 | ENDIF |
---|
| 1099 | ENDDO |
---|
| 1100 | ELSE |
---|
[94] | 1101 | DO k = nzb, nzt-1 |
---|
[667] | 1102 | IF ( first .AND. hom(k,1,18,sr) < 0.0 & |
---|
| 1103 | .AND. abs(hom(k,1,18,sr)) > 1.0E-8 ) THEN |
---|
[94] | 1104 | first = .FALSE. |
---|
| 1105 | height = zw(k) |
---|
[1] | 1106 | ENDIF |
---|
[667] | 1107 | IF ( hom(k,1,18,sr) < 0.0 .AND. & |
---|
| 1108 | abs(hom(k,1,18,sr)) > 1.0E-8 .AND. & |
---|
[94] | 1109 | hom(k+1,1,18,sr) > hom(k,1,18,sr) ) THEN |
---|
| 1110 | IF ( zw(k) < 1.5 * height ) THEN |
---|
| 1111 | z_i(1) = zw(k) |
---|
| 1112 | ELSE |
---|
| 1113 | z_i(1) = height |
---|
| 1114 | ENDIF |
---|
| 1115 | EXIT |
---|
| 1116 | ENDIF |
---|
| 1117 | ENDDO |
---|
[97] | 1118 | ENDIF |
---|
[1] | 1119 | |
---|
| 1120 | ! |
---|
[291] | 1121 | !-- Second scheme: Gradient scheme from Sullivan et al. (1998), modified |
---|
| 1122 | !-- by Uhlenbrock(2006). The boundary layer height is the height with the |
---|
| 1123 | !-- maximal local temperature gradient: starting from the second (the last |
---|
| 1124 | !-- but one) vertical gridpoint, the local gradient must be at least |
---|
| 1125 | !-- 0.2K/100m and greater than the next four gradients. |
---|
| 1126 | !-- WARNING: The threshold value of 0.2K/100m must be adjusted for the |
---|
| 1127 | !-- ocean case! |
---|
[1] | 1128 | z_i(2) = 0.0 |
---|
[291] | 1129 | DO k = nzb+1, nzt+1 |
---|
| 1130 | dptdz(k) = ( hom(k,1,4,sr) - hom(k-1,1,4,sr) ) * ddzu(k) |
---|
| 1131 | ENDDO |
---|
| 1132 | dptdz_threshold = 0.2 / 100.0 |
---|
| 1133 | |
---|
[97] | 1134 | IF ( ocean ) THEN |
---|
[291] | 1135 | DO k = nzt+1, nzb+5, -1 |
---|
| 1136 | IF ( dptdz(k) > dptdz_threshold .AND. & |
---|
| 1137 | dptdz(k) > dptdz(k-1) .AND. dptdz(k) > dptdz(k-2) .AND. & |
---|
| 1138 | dptdz(k) > dptdz(k-3) .AND. dptdz(k) > dptdz(k-4) ) THEN |
---|
| 1139 | z_i(2) = zw(k-1) |
---|
[97] | 1140 | EXIT |
---|
| 1141 | ENDIF |
---|
| 1142 | ENDDO |
---|
| 1143 | ELSE |
---|
[291] | 1144 | DO k = nzb+1, nzt-3 |
---|
| 1145 | IF ( dptdz(k) > dptdz_threshold .AND. & |
---|
| 1146 | dptdz(k) > dptdz(k+1) .AND. dptdz(k) > dptdz(k+2) .AND. & |
---|
| 1147 | dptdz(k) > dptdz(k+3) .AND. dptdz(k) > dptdz(k+4) ) THEN |
---|
| 1148 | z_i(2) = zw(k-1) |
---|
[97] | 1149 | EXIT |
---|
| 1150 | ENDIF |
---|
| 1151 | ENDDO |
---|
| 1152 | ENDIF |
---|
[1] | 1153 | |
---|
[87] | 1154 | hom(nzb+6,1,pr_palm,sr) = z_i(1) |
---|
| 1155 | hom(nzb+7,1,pr_palm,sr) = z_i(2) |
---|
[1] | 1156 | |
---|
| 1157 | ! |
---|
| 1158 | !-- Computation of both the characteristic vertical velocity and |
---|
| 1159 | !-- the characteristic convective boundary layer temperature. |
---|
| 1160 | !-- The horizontal average at nzb+1 is input for the average temperature. |
---|
[667] | 1161 | IF ( hom(nzb,1,18,sr) > 0.0 .AND. abs(hom(nzb,1,18,sr)) > 1.0E-8 & |
---|
| 1162 | .AND. z_i(1) /= 0.0 ) THEN |
---|
[87] | 1163 | hom(nzb+8,1,pr_palm,sr) = ( g / hom(nzb+1,1,4,sr) * & |
---|
[94] | 1164 | hom(nzb,1,18,sr) * & |
---|
| 1165 | ABS( z_i(1) ) )**0.333333333 |
---|
[1] | 1166 | !-- so far this only works if Prandtl layer is used |
---|
[87] | 1167 | hom(nzb+11,1,pr_palm,sr) = hom(nzb,1,16,sr) / hom(nzb+8,1,pr_palm,sr) |
---|
[1] | 1168 | ELSE |
---|
[87] | 1169 | hom(nzb+8,1,pr_palm,sr) = 0.0 |
---|
| 1170 | hom(nzb+11,1,pr_palm,sr) = 0.0 |
---|
[1] | 1171 | ENDIF |
---|
| 1172 | |
---|
[48] | 1173 | ! |
---|
| 1174 | !-- Collect the time series quantities |
---|
[87] | 1175 | ts_value(1,sr) = hom(nzb+4,1,pr_palm,sr) ! E |
---|
| 1176 | ts_value(2,sr) = hom(nzb+5,1,pr_palm,sr) ! E* |
---|
[48] | 1177 | ts_value(3,sr) = dt_3d |
---|
[87] | 1178 | ts_value(4,sr) = hom(nzb,1,pr_palm,sr) ! u* |
---|
| 1179 | ts_value(5,sr) = hom(nzb+3,1,pr_palm,sr) ! th* |
---|
[48] | 1180 | ts_value(6,sr) = u_max |
---|
| 1181 | ts_value(7,sr) = v_max |
---|
| 1182 | ts_value(8,sr) = w_max |
---|
[87] | 1183 | ts_value(9,sr) = hom(nzb+10,1,pr_palm,sr) ! new divergence |
---|
| 1184 | ts_value(10,sr) = hom(nzb+9,1,pr_palm,sr) ! old Divergence |
---|
| 1185 | ts_value(11,sr) = hom(nzb+6,1,pr_palm,sr) ! z_i(1) |
---|
| 1186 | ts_value(12,sr) = hom(nzb+7,1,pr_palm,sr) ! z_i(2) |
---|
| 1187 | ts_value(13,sr) = hom(nzb+8,1,pr_palm,sr) ! w* |
---|
[48] | 1188 | ts_value(14,sr) = hom(nzb,1,16,sr) ! w'pt' at k=0 |
---|
| 1189 | ts_value(15,sr) = hom(nzb+1,1,16,sr) ! w'pt' at k=1 |
---|
| 1190 | ts_value(16,sr) = hom(nzb+1,1,18,sr) ! wpt at k=1 |
---|
| 1191 | ts_value(17,sr) = hom(nzb,1,4,sr) ! pt(0) |
---|
| 1192 | ts_value(18,sr) = hom(nzb+1,1,4,sr) ! pt(zp) |
---|
[197] | 1193 | ts_value(19,sr) = hom(nzb+1,1,pr_palm,sr) ! u'w' at k=0 |
---|
| 1194 | ts_value(20,sr) = hom(nzb+2,1,pr_palm,sr) ! v'w' at k=0 |
---|
[343] | 1195 | ts_value(21,sr) = hom(nzb,1,48,sr) ! w"q" at k=0 |
---|
[197] | 1196 | |
---|
[48] | 1197 | IF ( ts_value(5,sr) /= 0.0 ) THEN |
---|
| 1198 | ts_value(22,sr) = ts_value(4,sr)**2 / & |
---|
| 1199 | ( kappa * g * ts_value(5,sr) / ts_value(18,sr) ) ! L |
---|
| 1200 | ELSE |
---|
| 1201 | ts_value(22,sr) = 10000.0 |
---|
| 1202 | ENDIF |
---|
[1] | 1203 | |
---|
[343] | 1204 | ts_value(23,sr) = hom(nzb+12,1,pr_palm,sr) ! q* |
---|
[1] | 1205 | ! |
---|
[48] | 1206 | !-- Calculate additional statistics provided by the user interface |
---|
[87] | 1207 | CALL user_statistics( 'time_series', sr, 0 ) |
---|
[1] | 1208 | |
---|
[48] | 1209 | ENDDO ! loop of the subregions |
---|
| 1210 | |
---|
[1] | 1211 | ! |
---|
| 1212 | !-- If required, sum up horizontal averages for subsequent time averaging |
---|
| 1213 | IF ( do_sum ) THEN |
---|
| 1214 | IF ( average_count_pr == 0 ) hom_sum = 0.0 |
---|
| 1215 | hom_sum = hom_sum + hom(:,1,:,:) |
---|
| 1216 | average_count_pr = average_count_pr + 1 |
---|
| 1217 | do_sum = .FALSE. |
---|
| 1218 | ENDIF |
---|
| 1219 | |
---|
| 1220 | ! |
---|
| 1221 | !-- Set flag for other UPs (e.g. output routines, but also buoyancy). |
---|
| 1222 | !-- This flag is reset after each time step in time_integration. |
---|
| 1223 | flow_statistics_called = .TRUE. |
---|
| 1224 | |
---|
| 1225 | CALL cpu_log( log_point(10), 'flow_statistics', 'stop' ) |
---|
| 1226 | |
---|
| 1227 | |
---|
| 1228 | END SUBROUTINE flow_statistics |
---|
| 1229 | |
---|
| 1230 | |
---|
| 1231 | |
---|