[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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[697] | 6 | ! |
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[392] | 7 | ! |
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| 8 | ! Former revisions: |
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| 9 | ! ----------------- |
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| 10 | ! $Id: flow_statistics.f90 697 2011-03-18 07:10:52Z raasch $ |
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| 11 | ! |
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[697] | 12 | ! 696 2011-03-18 07:03:49Z raasch |
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| 13 | ! Bugfix: Summation of Wicker-Skamarock scheme fluxes and variances for all |
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| 14 | ! threads |
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| 15 | ! |
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[679] | 16 | ! 678 2011-02-02 14:31:56Z raasch |
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| 17 | ! Bugfix in calculation of the divergence of vertical flux of resolved scale |
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| 18 | ! energy, pressure fluctuations, and flux of pressure fluctuation itself |
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| 19 | ! |
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[674] | 20 | ! 673 2011-01-18 16:19:48Z suehring |
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| 21 | ! Top bc for the horizontal velocity variances added for ocean runs. |
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| 22 | ! Setting the corresponding bottom bc moved to advec_ws. |
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| 23 | ! |
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[668] | 24 | ! 667 2010-12-23 12:06:00Z suehring/gryschka |
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| 25 | ! When advection is computed with ws-scheme, turbulent fluxes are already |
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| 26 | ! computed in the respective advection routines and buffered in arrays |
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| 27 | ! sums_xx_ws_l(). This is due to a consistent treatment of statistics with the |
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| 28 | ! numerics and to avoid unphysical kinks near the surface. |
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| 29 | ! So some if requests has to be done to dicern between fluxes from ws-scheme |
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| 30 | ! other advection schemes. |
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| 31 | ! Furthermore the computation of z_i is only done if the heat flux exceeds a |
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| 32 | ! minimum value. This affects only simulations of a neutral boundary layer and |
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| 33 | ! is due to reasons of computations in the advection scheme. |
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| 34 | ! |
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[625] | 35 | ! 624 2010-12-10 11:46:30Z heinze |
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| 36 | ! Calculation of q*2 added |
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| 37 | ! |
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[623] | 38 | ! 622 2010-12-10 08:08:13Z raasch |
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| 39 | ! optional barriers included in order to speed up collective operations |
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| 40 | ! |
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[392] | 41 | ! 388 2009-09-23 09:40:33Z raasch |
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[388] | 42 | ! Vertical profiles of potential density and hydrostatic pressure are |
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| 43 | ! calculated. |
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[343] | 44 | ! Added missing timeseries calculation of w"q"(0), moved timeseries q* to the |
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| 45 | ! end. |
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[291] | 46 | ! Temperature gradient criterion for estimating the boundary layer height |
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| 47 | ! replaced by the gradient criterion of Sullivan et al. (1998). |
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[254] | 48 | ! Output of messages replaced by message handling routine. |
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[1] | 49 | ! |
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[198] | 50 | ! 197 2008-09-16 15:29:03Z raasch |
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| 51 | ! Spline timeseries splptx etc. removed, timeseries w'u', w'v', w'q' (k=0) |
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| 52 | ! added, |
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| 53 | ! bugfix: divide sums(k,8) (e) and sums(k,34) (e*) by ngp_2dh_s_inner(k,sr) |
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| 54 | ! (like other scalars) |
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| 55 | ! |
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[139] | 56 | ! 133 2007-11-20 10:10:53Z letzel |
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| 57 | ! Vertical profiles now based on nzb_s_inner; they are divided by |
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| 58 | ! ngp_2dh_s_inner (scalars, procucts of scalars) and ngp_2dh (staggered |
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| 59 | ! velocity components and their products, procucts of scalars and velocity |
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| 60 | ! components), respectively. |
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| 61 | ! |
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[110] | 62 | ! 106 2007-08-16 14:30:26Z raasch |
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| 63 | ! Prescribed momentum fluxes at the top surface are used, |
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| 64 | ! profiles for w*p* and w"e are calculated |
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| 65 | ! |
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[98] | 66 | ! 97 2007-06-21 08:23:15Z raasch |
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| 67 | ! Statistics for ocean version (salinity, density) added, |
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| 68 | ! calculation of z_i and Deardorff velocity scale adjusted to be used with |
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| 69 | ! the ocean version |
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| 70 | ! |
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[90] | 71 | ! 87 2007-05-22 15:46:47Z raasch |
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| 72 | ! Two more arguments added to user_statistics, which is now also called for |
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| 73 | ! user-defined profiles, |
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| 74 | ! var_hom and var_sum renamed pr_palm |
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| 75 | ! |
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[83] | 76 | ! 82 2007-04-16 15:40:52Z raasch |
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| 77 | ! Cpp-directive lcmuk changed to intel_openmp_bug |
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| 78 | ! |
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[77] | 79 | ! 75 2007-03-22 09:54:05Z raasch |
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| 80 | ! Collection of time series quantities moved from routine flow_statistics to |
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| 81 | ! here, routine user_statistics is called for each statistic region, |
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| 82 | ! moisture renamed humidity |
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| 83 | ! |
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[39] | 84 | ! 19 2007-02-23 04:53:48Z raasch |
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[77] | 85 | ! fluxes at top modified (tswst, qswst) |
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[39] | 86 | ! |
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[3] | 87 | ! RCS Log replace by Id keyword, revision history cleaned up |
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| 88 | ! |
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[1] | 89 | ! Revision 1.41 2006/08/04 14:37:50 raasch |
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| 90 | ! Error removed in non-parallel part (sums_l) |
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| 91 | ! |
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| 92 | ! Revision 1.1 1997/08/11 06:15:17 raasch |
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| 93 | ! Initial revision |
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| 94 | ! |
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| 95 | ! |
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| 96 | ! Description: |
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| 97 | ! ------------ |
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| 98 | ! Compute average profiles and further average flow quantities for the different |
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| 99 | ! user-defined (sub-)regions. The region indexed 0 is the total model domain. |
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| 100 | ! |
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[132] | 101 | ! NOTE: For simplicity, nzb_s_inner and nzb_diff_s_inner are being used as a |
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| 102 | ! ---- lower vertical index for k-loops for all variables, although strictly |
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| 103 | ! speaking the k-loops would have to be split up according to the staggered |
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| 104 | ! grid. However, this implies no error since staggered velocity components are |
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| 105 | ! zero at the walls and inside buildings. |
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[1] | 106 | !------------------------------------------------------------------------------! |
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| 107 | |
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| 108 | USE arrays_3d |
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| 109 | USE cloud_parameters |
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| 110 | USE cpulog |
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| 111 | USE grid_variables |
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| 112 | USE indices |
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| 113 | USE interfaces |
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| 114 | USE pegrid |
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| 115 | USE statistics |
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| 116 | USE control_parameters |
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| 117 | |
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| 118 | IMPLICIT NONE |
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| 119 | |
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| 120 | INTEGER :: i, j, k, omp_get_thread_num, sr, tn |
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| 121 | LOGICAL :: first |
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[291] | 122 | REAL :: dptdz_threshold, height, pts, sums_l_eper, sums_l_etot, ust, & |
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| 123 | ust2, u2, vst, vst2, v2, w2, z_i(2) |
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| 124 | REAL :: dptdz(nzb+1:nzt+1) |
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[1] | 125 | REAL :: sums_ll(nzb:nzt+1,2) |
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| 126 | |
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| 127 | CALL cpu_log( log_point(10), 'flow_statistics', 'start' ) |
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| 128 | |
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| 129 | ! |
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| 130 | !-- To be on the safe side, check whether flow_statistics has already been |
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| 131 | !-- called once after the current time step |
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| 132 | IF ( flow_statistics_called ) THEN |
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[254] | 133 | |
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[274] | 134 | message_string = 'flow_statistics is called two times within one ' // & |
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| 135 | 'timestep' |
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[254] | 136 | CALL message( 'flow_statistics', 'PA0190', 1, 2, 0, 6, 0 ) |
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| 137 | |
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[1] | 138 | ENDIF |
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| 139 | |
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| 140 | ! |
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| 141 | !-- Compute statistics for each (sub-)region |
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| 142 | DO sr = 0, statistic_regions |
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| 143 | |
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| 144 | ! |
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| 145 | !-- Initialize (local) summation array |
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| 146 | sums_l = 0.0 |
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| 147 | |
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| 148 | ! |
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| 149 | !-- Store sums that have been computed in other subroutines in summation |
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| 150 | !-- array |
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| 151 | sums_l(:,11,:) = sums_l_l(:,sr,:) ! mixing length from diffusivities |
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| 152 | !-- WARNING: next line still has to be adjusted for OpenMP |
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| 153 | sums_l(:,21,0) = sums_wsts_bc_l(:,sr) ! heat flux from advec_s_bc |
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[87] | 154 | sums_l(nzb+9,pr_palm,0) = sums_divold_l(sr) ! old divergence from pres |
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| 155 | sums_l(nzb+10,pr_palm,0) = sums_divnew_l(sr) ! new divergence from pres |
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[1] | 156 | |
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[667] | 157 | ! |
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| 158 | !-- Copy the turbulent quantities, evaluated in the advection routines to |
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| 159 | !-- the local array sums_l() for further computations |
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| 160 | IF ( ws_scheme_mom ) THEN |
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[696] | 161 | |
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[667] | 162 | ! |
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[673] | 163 | !-- According to the Neumann bc for the horizontal velocity components, |
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| 164 | !-- the corresponding fluxes has to satisfiy the same bc. |
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| 165 | IF ( ocean ) THEN |
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| 166 | sums_us2_ws_l(nzt+1,sr) = sums_us2_ws_l(nzt,sr) |
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| 167 | sums_vs2_ws_l(nzt+1,sr) = sums_vs2_ws_l(nzt,sr) |
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| 168 | ENDIF |
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[696] | 169 | |
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| 170 | DO i = 0, threads_per_task-1 |
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[667] | 171 | ! |
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[696] | 172 | !-- Swap the turbulent quantities evaluated in advec_ws. |
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| 173 | sums_l(:,13,i) = sums_wsus_ws_l(:,sr) ! w*u* |
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| 174 | sums_l(:,15,i) = sums_wsvs_ws_l(:,sr) ! w*v* |
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| 175 | sums_l(:,30,i) = sums_us2_ws_l(:,sr) ! u*2 |
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| 176 | sums_l(:,31,i) = sums_vs2_ws_l(:,sr) ! v*2 |
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| 177 | sums_l(:,32,i) = sums_ws2_ws_l(:,sr) ! w*2 |
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| 178 | sums_l(:,34,i) = sums_l(:,34,i) + 0.5 * & |
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| 179 | ( sums_us2_ws_l(:,sr) + sums_vs2_ws_l(:,sr) + & |
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| 180 | sums_ws2_ws_l(:,sr) ) ! e* |
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| 181 | DO k = nzb, nzt |
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| 182 | sums_l(nzb+5,pr_palm,i) = sums_l(nzb+5,pr_palm,i) + 0.5 * ( & |
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| 183 | sums_us2_ws_l(k,sr) + & |
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| 184 | sums_vs2_ws_l(k,sr) + & |
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| 185 | sums_ws2_ws_l(k,sr) ) |
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| 186 | ENDDO |
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[667] | 187 | ENDDO |
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[696] | 188 | |
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[667] | 189 | ENDIF |
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[696] | 190 | |
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[667] | 191 | IF ( ws_scheme_sca ) THEN |
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[696] | 192 | |
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| 193 | DO i = 0, threads_per_task-1 |
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| 194 | sums_l(:,17,i) = sums_wspts_ws_l(:,sr) ! w*pt* from advec_s_ws |
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| 195 | IF ( ocean ) sums_l(:,66,i) = sums_wssas_ws_l(:,sr) ! w*sa* |
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| 196 | IF ( humidity .OR. passive_scalar ) sums_l(:,49,i) = & |
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| 197 | sums_wsqs_ws_l(:,sr) !w*q* |
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| 198 | ENDDO |
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| 199 | |
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[667] | 200 | ENDIF |
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[305] | 201 | ! |
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[1] | 202 | !-- Horizontally averaged profiles of horizontal velocities and temperature. |
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| 203 | !-- They must have been computed before, because they are already required |
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| 204 | !-- for other horizontal averages. |
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| 205 | tn = 0 |
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[667] | 206 | |
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[1] | 207 | !$OMP PARALLEL PRIVATE( i, j, k, tn ) |
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[82] | 208 | #if defined( __intel_openmp_bug ) |
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[1] | 209 | tn = omp_get_thread_num() |
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| 210 | #else |
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| 211 | !$ tn = omp_get_thread_num() |
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| 212 | #endif |
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| 213 | |
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| 214 | !$OMP DO |
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| 215 | DO i = nxl, nxr |
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| 216 | DO j = nys, nyn |
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[132] | 217 | DO k = nzb_s_inner(j,i), nzt+1 |
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[1] | 218 | sums_l(k,1,tn) = sums_l(k,1,tn) + u(k,j,i) * rmask(j,i,sr) |
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| 219 | sums_l(k,2,tn) = sums_l(k,2,tn) + v(k,j,i) * rmask(j,i,sr) |
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| 220 | sums_l(k,4,tn) = sums_l(k,4,tn) + pt(k,j,i) * rmask(j,i,sr) |
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| 221 | ENDDO |
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| 222 | ENDDO |
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| 223 | ENDDO |
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| 224 | |
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| 225 | ! |
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[96] | 226 | !-- Horizontally averaged profile of salinity |
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| 227 | IF ( ocean ) THEN |
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| 228 | !$OMP DO |
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| 229 | DO i = nxl, nxr |
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| 230 | DO j = nys, nyn |
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[132] | 231 | DO k = nzb_s_inner(j,i), nzt+1 |
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[96] | 232 | sums_l(k,23,tn) = sums_l(k,23,tn) + & |
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| 233 | sa(k,j,i) * rmask(j,i,sr) |
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| 234 | ENDDO |
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| 235 | ENDDO |
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| 236 | ENDDO |
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| 237 | ENDIF |
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| 238 | |
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| 239 | ! |
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[1] | 240 | !-- Horizontally averaged profiles of virtual potential temperature, |
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| 241 | !-- total water content, specific humidity and liquid water potential |
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| 242 | !-- temperature |
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[75] | 243 | IF ( humidity ) THEN |
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[1] | 244 | !$OMP DO |
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| 245 | DO i = nxl, nxr |
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| 246 | DO j = nys, nyn |
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[132] | 247 | DO k = nzb_s_inner(j,i), nzt+1 |
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[1] | 248 | sums_l(k,44,tn) = sums_l(k,44,tn) + & |
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| 249 | vpt(k,j,i) * rmask(j,i,sr) |
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| 250 | sums_l(k,41,tn) = sums_l(k,41,tn) + & |
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| 251 | q(k,j,i) * rmask(j,i,sr) |
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| 252 | ENDDO |
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| 253 | ENDDO |
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| 254 | ENDDO |
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| 255 | IF ( cloud_physics ) THEN |
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| 256 | !$OMP DO |
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| 257 | DO i = nxl, nxr |
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| 258 | DO j = nys, nyn |
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[132] | 259 | DO k = nzb_s_inner(j,i), nzt+1 |
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[1] | 260 | sums_l(k,42,tn) = sums_l(k,42,tn) + & |
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| 261 | ( q(k,j,i) - ql(k,j,i) ) * rmask(j,i,sr) |
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| 262 | sums_l(k,43,tn) = sums_l(k,43,tn) + ( & |
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| 263 | pt(k,j,i) + l_d_cp*pt_d_t(k) * ql(k,j,i) & |
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| 264 | ) * rmask(j,i,sr) |
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| 265 | ENDDO |
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| 266 | ENDDO |
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| 267 | ENDDO |
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| 268 | ENDIF |
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| 269 | ENDIF |
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| 270 | |
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| 271 | ! |
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| 272 | !-- Horizontally averaged profiles of passive scalar |
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| 273 | IF ( passive_scalar ) THEN |
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| 274 | !$OMP DO |
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| 275 | DO i = nxl, nxr |
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| 276 | DO j = nys, nyn |
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[132] | 277 | DO k = nzb_s_inner(j,i), nzt+1 |
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[1] | 278 | sums_l(k,41,tn) = sums_l(k,41,tn) + q(k,j,i) * rmask(j,i,sr) |
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| 279 | ENDDO |
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| 280 | ENDDO |
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| 281 | ENDDO |
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| 282 | ENDIF |
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| 283 | !$OMP END PARALLEL |
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| 284 | ! |
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| 285 | !-- Summation of thread sums |
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| 286 | IF ( threads_per_task > 1 ) THEN |
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| 287 | DO i = 1, threads_per_task-1 |
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| 288 | sums_l(:,1,0) = sums_l(:,1,0) + sums_l(:,1,i) |
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| 289 | sums_l(:,2,0) = sums_l(:,2,0) + sums_l(:,2,i) |
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| 290 | sums_l(:,4,0) = sums_l(:,4,0) + sums_l(:,4,i) |
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[96] | 291 | IF ( ocean ) THEN |
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| 292 | sums_l(:,23,0) = sums_l(:,23,0) + sums_l(:,23,i) |
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| 293 | ENDIF |
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[75] | 294 | IF ( humidity ) THEN |
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[1] | 295 | sums_l(:,41,0) = sums_l(:,41,0) + sums_l(:,41,i) |
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| 296 | sums_l(:,44,0) = sums_l(:,44,0) + sums_l(:,44,i) |
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| 297 | IF ( cloud_physics ) THEN |
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| 298 | sums_l(:,42,0) = sums_l(:,42,0) + sums_l(:,42,i) |
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| 299 | sums_l(:,43,0) = sums_l(:,43,0) + sums_l(:,43,i) |
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| 300 | ENDIF |
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| 301 | ENDIF |
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| 302 | IF ( passive_scalar ) THEN |
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| 303 | sums_l(:,41,0) = sums_l(:,41,0) + sums_l(:,41,i) |
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| 304 | ENDIF |
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| 305 | ENDDO |
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| 306 | ENDIF |
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| 307 | |
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| 308 | #if defined( __parallel ) |
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| 309 | ! |
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| 310 | !-- Compute total sum from local sums |
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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,1,0), sums(nzb,1), 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,2,0), sums(nzb,2), nzt+2-nzb, MPI_REAL, & |
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| 316 | MPI_SUM, comm2d, ierr ) |
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[622] | 317 | IF ( collective_wait ) CALL MPI_BARRIER( comm2d, ierr ) |
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[1] | 318 | CALL MPI_ALLREDUCE( sums_l(nzb,4,0), sums(nzb,4), nzt+2-nzb, MPI_REAL, & |
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| 319 | MPI_SUM, comm2d, ierr ) |
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[96] | 320 | IF ( ocean ) THEN |
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[622] | 321 | IF ( collective_wait ) CALL MPI_BARRIER( comm2d, ierr ) |
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[96] | 322 | CALL MPI_ALLREDUCE( sums_l(nzb,23,0), sums(nzb,23), nzt+2-nzb, & |
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| 323 | MPI_REAL, MPI_SUM, comm2d, ierr ) |
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| 324 | ENDIF |
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[75] | 325 | IF ( humidity ) THEN |
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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,44,0), sums(nzb,44), nzt+2-nzb, & |
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| 328 | MPI_REAL, MPI_SUM, comm2d, ierr ) |
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[622] | 329 | IF ( collective_wait ) CALL MPI_BARRIER( comm2d, ierr ) |
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[1] | 330 | CALL MPI_ALLREDUCE( sums_l(nzb,41,0), sums(nzb,41), nzt+2-nzb, & |
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| 331 | MPI_REAL, MPI_SUM, comm2d, ierr ) |
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| 332 | IF ( cloud_physics ) 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,42,0), sums(nzb,42), nzt+2-nzb, & |
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| 335 | MPI_REAL, MPI_SUM, comm2d, ierr ) |
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[622] | 336 | IF ( collective_wait ) CALL MPI_BARRIER( comm2d, ierr ) |
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[1] | 337 | CALL MPI_ALLREDUCE( sums_l(nzb,43,0), sums(nzb,43), nzt+2-nzb, & |
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| 338 | MPI_REAL, MPI_SUM, comm2d, ierr ) |
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| 339 | ENDIF |
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| 340 | ENDIF |
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| 341 | |
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| 342 | IF ( passive_scalar ) THEN |
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[622] | 343 | IF ( collective_wait ) CALL MPI_BARRIER( comm2d, ierr ) |
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[1] | 344 | CALL MPI_ALLREDUCE( sums_l(nzb,41,0), sums(nzb,41), nzt+2-nzb, & |
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| 345 | MPI_REAL, MPI_SUM, comm2d, ierr ) |
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| 346 | ENDIF |
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| 347 | #else |
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| 348 | sums(:,1) = sums_l(:,1,0) |
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| 349 | sums(:,2) = sums_l(:,2,0) |
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| 350 | sums(:,4) = sums_l(:,4,0) |
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[96] | 351 | IF ( ocean ) sums(:,23) = sums_l(:,23,0) |
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[75] | 352 | IF ( humidity ) THEN |
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[1] | 353 | sums(:,44) = sums_l(:,44,0) |
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| 354 | sums(:,41) = sums_l(:,41,0) |
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| 355 | IF ( cloud_physics ) THEN |
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| 356 | sums(:,42) = sums_l(:,42,0) |
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| 357 | sums(:,43) = sums_l(:,43,0) |
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| 358 | ENDIF |
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| 359 | ENDIF |
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| 360 | IF ( passive_scalar ) sums(:,41) = sums_l(:,41,0) |
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| 361 | #endif |
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| 362 | |
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| 363 | ! |
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| 364 | !-- Final values are obtained by division by the total number of grid points |
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| 365 | !-- used for summation. After that store profiles. |
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[132] | 366 | sums(:,1) = sums(:,1) / ngp_2dh(sr) |
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| 367 | sums(:,2) = sums(:,2) / ngp_2dh(sr) |
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| 368 | sums(:,4) = sums(:,4) / ngp_2dh_s_inner(:,sr) |
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[1] | 369 | hom(:,1,1,sr) = sums(:,1) ! u |
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| 370 | hom(:,1,2,sr) = sums(:,2) ! v |
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| 371 | hom(:,1,4,sr) = sums(:,4) ! pt |
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| 372 | |
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[667] | 373 | |
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[1] | 374 | ! |
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[96] | 375 | !-- Salinity |
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| 376 | IF ( ocean ) THEN |
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[132] | 377 | sums(:,23) = sums(:,23) / ngp_2dh_s_inner(:,sr) |
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[96] | 378 | hom(:,1,23,sr) = sums(:,23) ! sa |
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| 379 | ENDIF |
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| 380 | |
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| 381 | ! |
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[1] | 382 | !-- Humidity and cloud parameters |
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[75] | 383 | IF ( humidity ) THEN |
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[132] | 384 | sums(:,44) = sums(:,44) / ngp_2dh_s_inner(:,sr) |
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| 385 | sums(:,41) = sums(:,41) / ngp_2dh_s_inner(:,sr) |
---|
[1] | 386 | hom(:,1,44,sr) = sums(:,44) ! vpt |
---|
| 387 | hom(:,1,41,sr) = sums(:,41) ! qv (q) |
---|
| 388 | IF ( cloud_physics ) THEN |
---|
[132] | 389 | sums(:,42) = sums(:,42) / ngp_2dh_s_inner(:,sr) |
---|
| 390 | sums(:,43) = sums(:,43) / ngp_2dh_s_inner(:,sr) |
---|
[1] | 391 | hom(:,1,42,sr) = sums(:,42) ! qv |
---|
| 392 | hom(:,1,43,sr) = sums(:,43) ! pt |
---|
| 393 | ENDIF |
---|
| 394 | ENDIF |
---|
| 395 | |
---|
| 396 | ! |
---|
| 397 | !-- Passive scalar |
---|
[132] | 398 | IF ( passive_scalar ) hom(:,1,41,sr) = sums(:,41) / & |
---|
| 399 | ngp_2dh_s_inner(:,sr) ! s (q) |
---|
[1] | 400 | |
---|
| 401 | ! |
---|
| 402 | !-- Horizontally averaged profiles of the remaining prognostic variables, |
---|
| 403 | !-- variances, the total and the perturbation energy (single values in last |
---|
| 404 | !-- column of sums_l) and some diagnostic quantities. |
---|
[132] | 405 | !-- NOTE: for simplicity, nzb_s_inner is used below, although strictly |
---|
[1] | 406 | !-- ---- speaking the following k-loop would have to be split up and |
---|
| 407 | !-- rearranged according to the staggered grid. |
---|
[132] | 408 | !-- However, this implies no error since staggered velocity components |
---|
| 409 | !-- are zero at the walls and inside buildings. |
---|
[1] | 410 | tn = 0 |
---|
[82] | 411 | #if defined( __intel_openmp_bug ) |
---|
[1] | 412 | !$OMP PARALLEL PRIVATE( i, j, k, pts, sums_ll, sums_l_eper, sums_l_etot, & |
---|
| 413 | !$OMP tn, ust, ust2, u2, vst, vst2, v2, w2 ) |
---|
| 414 | tn = omp_get_thread_num() |
---|
| 415 | #else |
---|
| 416 | !$OMP PARALLEL PRIVATE( i, j, k, pts, sums_ll, sums_l_eper, sums_l_etot, tn, ust, ust2, u2, vst, vst2, v2, w2 ) |
---|
| 417 | !$ tn = omp_get_thread_num() |
---|
| 418 | #endif |
---|
| 419 | !$OMP DO |
---|
| 420 | DO i = nxl, nxr |
---|
| 421 | DO j = nys, nyn |
---|
| 422 | sums_l_etot = 0.0 |
---|
[132] | 423 | DO k = nzb_s_inner(j,i), nzt+1 |
---|
[1] | 424 | ! |
---|
| 425 | !-- Prognostic and diagnostic variables |
---|
| 426 | sums_l(k,3,tn) = sums_l(k,3,tn) + w(k,j,i) * rmask(j,i,sr) |
---|
| 427 | sums_l(k,8,tn) = sums_l(k,8,tn) + e(k,j,i) * rmask(j,i,sr) |
---|
| 428 | sums_l(k,9,tn) = sums_l(k,9,tn) + km(k,j,i) * rmask(j,i,sr) |
---|
| 429 | sums_l(k,10,tn) = sums_l(k,10,tn) + kh(k,j,i) * rmask(j,i,sr) |
---|
| 430 | sums_l(k,40,tn) = sums_l(k,40,tn) + p(k,j,i) |
---|
| 431 | |
---|
| 432 | sums_l(k,33,tn) = sums_l(k,33,tn) + & |
---|
| 433 | ( pt(k,j,i)-hom(k,1,4,sr) )**2 * rmask(j,i,sr) |
---|
[624] | 434 | |
---|
| 435 | IF ( humidity ) THEN |
---|
| 436 | sums_l(k,70,tn) = sums_l(k,70,tn) + & |
---|
| 437 | ( q(k,j,i)-hom(k,1,41,sr) )**2 * rmask(j,i,sr) |
---|
| 438 | ENDIF |
---|
[667] | 439 | |
---|
[1] | 440 | sums_l_etot = sums_l_etot + & |
---|
[667] | 441 | 0.5 * ( u(k,j,i)**2 + v(k,j,i)**2 + & |
---|
| 442 | w(k,j,i)**2 ) * rmask(j,i,sr) |
---|
[1] | 443 | ENDDO |
---|
| 444 | ! |
---|
| 445 | !-- Total and perturbation energy for the total domain (being |
---|
| 446 | !-- collected in the last column of sums_l). Summation of these |
---|
| 447 | !-- quantities is seperated from the previous loop in order to |
---|
| 448 | !-- allow vectorization of that loop. |
---|
[87] | 449 | sums_l(nzb+4,pr_palm,tn) = sums_l(nzb+4,pr_palm,tn) + sums_l_etot |
---|
[1] | 450 | ! |
---|
| 451 | !-- 2D-arrays (being collected in the last column of sums_l) |
---|
[87] | 452 | sums_l(nzb,pr_palm,tn) = sums_l(nzb,pr_palm,tn) + & |
---|
[1] | 453 | us(j,i) * rmask(j,i,sr) |
---|
[87] | 454 | sums_l(nzb+1,pr_palm,tn) = sums_l(nzb+1,pr_palm,tn) + & |
---|
[1] | 455 | usws(j,i) * rmask(j,i,sr) |
---|
[87] | 456 | sums_l(nzb+2,pr_palm,tn) = sums_l(nzb+2,pr_palm,tn) + & |
---|
[1] | 457 | vsws(j,i) * rmask(j,i,sr) |
---|
[87] | 458 | sums_l(nzb+3,pr_palm,tn) = sums_l(nzb+3,pr_palm,tn) + & |
---|
[1] | 459 | ts(j,i) * rmask(j,i,sr) |
---|
[197] | 460 | IF ( humidity ) THEN |
---|
| 461 | sums_l(nzb+12,pr_palm,tn) = sums_l(nzb+12,pr_palm,tn) + & |
---|
| 462 | qs(j,i) * rmask(j,i,sr) |
---|
| 463 | ENDIF |
---|
[1] | 464 | ENDDO |
---|
| 465 | ENDDO |
---|
| 466 | |
---|
| 467 | ! |
---|
[667] | 468 | !-- Computation of statistics when ws-scheme is not used. Else these |
---|
| 469 | !-- quantities are evaluated in the advection routines. |
---|
| 470 | IF ( .NOT. ws_scheme_mom ) THEN |
---|
| 471 | !$OMP DO |
---|
| 472 | DO i = nxl, nxr |
---|
| 473 | DO j = nys, nyn |
---|
| 474 | sums_l_eper = 0.0 |
---|
| 475 | DO k = nzb_s_inner(j,i), nzt+1 |
---|
| 476 | u2 = u(k,j,i)**2 |
---|
| 477 | v2 = v(k,j,i)**2 |
---|
| 478 | w2 = w(k,j,i)**2 |
---|
| 479 | ust2 = ( u(k,j,i) - hom(k,1,1,sr) )**2 |
---|
| 480 | vst2 = ( v(k,j,i) - hom(k,1,2,sr) )**2 |
---|
| 481 | |
---|
| 482 | sums_l(k,30,tn) = sums_l(k,30,tn) + ust2 * rmask(j,i,sr) |
---|
| 483 | sums_l(k,31,tn) = sums_l(k,31,tn) + vst2 * rmask(j,i,sr) |
---|
| 484 | sums_l(k,32,tn) = sums_l(k,32,tn) + w2 * rmask(j,i,sr) |
---|
| 485 | ! |
---|
| 486 | !-- Higher moments |
---|
| 487 | !-- (Computation of the skewness of w further below) |
---|
| 488 | sums_l(k,38,tn) = sums_l(k,38,tn) + w(k,j,i) * w2 * & |
---|
| 489 | rmask(j,i,sr) |
---|
| 490 | ! |
---|
| 491 | !-- Perturbation energy |
---|
| 492 | |
---|
| 493 | sums_l(k,34,tn) = sums_l(k,34,tn) + 0.5 * & |
---|
| 494 | ( ust2 + vst2 + w2 ) * rmask(j,i,sr) |
---|
| 495 | sums_l_eper = sums_l_eper + & |
---|
| 496 | 0.5 * ( ust2+vst2+w2 ) * rmask(j,i,sr) |
---|
| 497 | |
---|
| 498 | ENDDO |
---|
| 499 | sums_l(nzb+5,pr_palm,tn) = sums_l(nzb+5,pr_palm,tn) & |
---|
| 500 | + sums_l_eper |
---|
| 501 | ENDDO |
---|
| 502 | ENDDO |
---|
| 503 | ELSE |
---|
| 504 | !$OMP DO |
---|
| 505 | DO i = nxl, nxr |
---|
| 506 | DO j = nys, nyn |
---|
| 507 | DO k = nzb_s_inner(j,i), nzt + 1 |
---|
| 508 | w2 = w(k,j,i)**2 |
---|
| 509 | ! |
---|
| 510 | !-- Higher moments |
---|
| 511 | !-- (Computation of the skewness of w further below) |
---|
| 512 | sums_l(k,38,tn) = sums_l(k,38,tn) + w(k,j,i) * w2 * & |
---|
| 513 | rmask(j,i,sr) |
---|
| 514 | ENDDO |
---|
| 515 | ENDDO |
---|
| 516 | ENDDO |
---|
| 517 | ENDIF |
---|
| 518 | |
---|
| 519 | ! |
---|
[1] | 520 | !-- Horizontally averaged profiles of the vertical fluxes |
---|
[667] | 521 | |
---|
[1] | 522 | !$OMP DO |
---|
| 523 | DO i = nxl, nxr |
---|
| 524 | DO j = nys, nyn |
---|
| 525 | ! |
---|
| 526 | !-- Subgridscale fluxes (without Prandtl layer from k=nzb, |
---|
| 527 | !-- oterwise from k=nzb+1) |
---|
[132] | 528 | !-- NOTE: for simplicity, nzb_diff_s_inner is used below, although |
---|
[1] | 529 | !-- ---- strictly speaking the following k-loop would have to be |
---|
| 530 | !-- split up according to the staggered grid. |
---|
[132] | 531 | !-- However, this implies no error since staggered velocity |
---|
| 532 | !-- components are zero at the walls and inside buildings. |
---|
| 533 | |
---|
| 534 | DO k = nzb_diff_s_inner(j,i)-1, nzt_diff |
---|
[1] | 535 | ! |
---|
| 536 | !-- Momentum flux w"u" |
---|
| 537 | sums_l(k,12,tn) = sums_l(k,12,tn) - 0.25 * ( & |
---|
| 538 | km(k,j,i)+km(k+1,j,i)+km(k,j,i-1)+km(k+1,j,i-1) & |
---|
| 539 | ) * ( & |
---|
| 540 | ( u(k+1,j,i) - u(k,j,i) ) * ddzu(k+1) & |
---|
| 541 | + ( w(k,j,i) - w(k,j,i-1) ) * ddx & |
---|
| 542 | ) * rmask(j,i,sr) |
---|
| 543 | ! |
---|
| 544 | !-- Momentum flux w"v" |
---|
| 545 | sums_l(k,14,tn) = sums_l(k,14,tn) - 0.25 * ( & |
---|
| 546 | km(k,j,i)+km(k+1,j,i)+km(k,j-1,i)+km(k+1,j-1,i) & |
---|
| 547 | ) * ( & |
---|
| 548 | ( v(k+1,j,i) - v(k,j,i) ) * ddzu(k+1) & |
---|
| 549 | + ( w(k,j,i) - w(k,j-1,i) ) * ddy & |
---|
| 550 | ) * rmask(j,i,sr) |
---|
| 551 | ! |
---|
| 552 | !-- Heat flux w"pt" |
---|
| 553 | sums_l(k,16,tn) = sums_l(k,16,tn) & |
---|
| 554 | - 0.5 * ( kh(k,j,i) + kh(k+1,j,i) ) & |
---|
| 555 | * ( pt(k+1,j,i) - pt(k,j,i) ) & |
---|
| 556 | * ddzu(k+1) * rmask(j,i,sr) |
---|
| 557 | |
---|
| 558 | |
---|
| 559 | ! |
---|
[96] | 560 | !-- Salinity flux w"sa" |
---|
| 561 | IF ( ocean ) THEN |
---|
| 562 | sums_l(k,65,tn) = sums_l(k,65,tn) & |
---|
| 563 | - 0.5 * ( kh(k,j,i) + kh(k+1,j,i) ) & |
---|
| 564 | * ( sa(k+1,j,i) - sa(k,j,i) ) & |
---|
| 565 | * ddzu(k+1) * rmask(j,i,sr) |
---|
| 566 | ENDIF |
---|
| 567 | |
---|
| 568 | ! |
---|
[1] | 569 | !-- Buoyancy flux, water flux (humidity flux) w"q" |
---|
[75] | 570 | IF ( humidity ) THEN |
---|
[1] | 571 | sums_l(k,45,tn) = sums_l(k,45,tn) & |
---|
| 572 | - 0.5 * ( kh(k,j,i) + kh(k+1,j,i) ) & |
---|
| 573 | * ( vpt(k+1,j,i) - vpt(k,j,i) ) & |
---|
| 574 | * ddzu(k+1) * rmask(j,i,sr) |
---|
| 575 | sums_l(k,48,tn) = sums_l(k,48,tn) & |
---|
| 576 | - 0.5 * ( kh(k,j,i) + kh(k+1,j,i) ) & |
---|
| 577 | * ( q(k+1,j,i) - q(k,j,i) ) & |
---|
| 578 | * ddzu(k+1) * rmask(j,i,sr) |
---|
| 579 | IF ( cloud_physics ) THEN |
---|
| 580 | sums_l(k,51,tn) = sums_l(k,51,tn) & |
---|
| 581 | - 0.5 * ( kh(k,j,i) + kh(k+1,j,i) ) & |
---|
| 582 | * ( ( q(k+1,j,i) - ql(k+1,j,i) )& |
---|
| 583 | - ( q(k,j,i) - ql(k,j,i) ) ) & |
---|
| 584 | * ddzu(k+1) * rmask(j,i,sr) |
---|
| 585 | ENDIF |
---|
| 586 | ENDIF |
---|
| 587 | |
---|
| 588 | ! |
---|
| 589 | !-- Passive scalar flux |
---|
| 590 | IF ( passive_scalar ) THEN |
---|
| 591 | sums_l(k,48,tn) = sums_l(k,48,tn) & |
---|
| 592 | - 0.5 * ( kh(k,j,i) + kh(k+1,j,i) ) & |
---|
| 593 | * ( q(k+1,j,i) - q(k,j,i) ) & |
---|
| 594 | * ddzu(k+1) * rmask(j,i,sr) |
---|
| 595 | ENDIF |
---|
| 596 | |
---|
| 597 | ENDDO |
---|
| 598 | |
---|
| 599 | ! |
---|
| 600 | !-- Subgridscale fluxes in the Prandtl layer |
---|
| 601 | IF ( use_surface_fluxes ) THEN |
---|
| 602 | sums_l(nzb,12,tn) = sums_l(nzb,12,tn) + & |
---|
| 603 | usws(j,i) * rmask(j,i,sr) ! w"u" |
---|
| 604 | sums_l(nzb,14,tn) = sums_l(nzb,14,tn) + & |
---|
| 605 | vsws(j,i) * rmask(j,i,sr) ! w"v" |
---|
| 606 | sums_l(nzb,16,tn) = sums_l(nzb,16,tn) + & |
---|
| 607 | shf(j,i) * rmask(j,i,sr) ! w"pt" |
---|
| 608 | sums_l(nzb,58,tn) = sums_l(nzb,58,tn) + & |
---|
| 609 | 0.0 * rmask(j,i,sr) ! u"pt" |
---|
| 610 | sums_l(nzb,61,tn) = sums_l(nzb,61,tn) + & |
---|
| 611 | 0.0 * rmask(j,i,sr) ! v"pt" |
---|
[96] | 612 | IF ( ocean ) THEN |
---|
| 613 | sums_l(nzb,65,tn) = sums_l(nzb,65,tn) + & |
---|
| 614 | saswsb(j,i) * rmask(j,i,sr) ! w"sa" |
---|
| 615 | ENDIF |
---|
[75] | 616 | IF ( humidity ) THEN |
---|
[1] | 617 | sums_l(nzb,48,tn) = sums_l(nzb,48,tn) + & |
---|
| 618 | qsws(j,i) * rmask(j,i,sr) ! w"q" (w"qv") |
---|
| 619 | IF ( cloud_physics ) THEN |
---|
| 620 | sums_l(nzb,45,tn) = sums_l(nzb,45,tn) + ( & |
---|
| 621 | ( 1.0 + 0.61 * q(nzb,j,i) ) * & |
---|
| 622 | shf(j,i) + 0.61 * pt(nzb,j,i) * & |
---|
| 623 | qsws(j,i) & |
---|
| 624 | ) |
---|
| 625 | ! |
---|
| 626 | !-- Formula does not work if ql(nzb) /= 0.0 |
---|
| 627 | sums_l(nzb,51,tn) = sums_l(nzb,51,tn) + & ! w"q" (w"qv") |
---|
| 628 | qsws(j,i) * rmask(j,i,sr) |
---|
| 629 | ENDIF |
---|
| 630 | ENDIF |
---|
| 631 | IF ( passive_scalar ) THEN |
---|
| 632 | sums_l(nzb,48,tn) = sums_l(nzb,48,tn) + & |
---|
| 633 | qsws(j,i) * rmask(j,i,sr) ! w"q" (w"qv") |
---|
| 634 | ENDIF |
---|
| 635 | ENDIF |
---|
| 636 | |
---|
| 637 | ! |
---|
[19] | 638 | !-- Subgridscale fluxes at the top surface |
---|
| 639 | IF ( use_top_fluxes ) THEN |
---|
[550] | 640 | sums_l(nzt:nzt+1,12,tn) = sums_l(nzt:nzt+1,12,tn) + & |
---|
[102] | 641 | uswst(j,i) * rmask(j,i,sr) ! w"u" |
---|
[550] | 642 | sums_l(nzt:nzt+1,14,tn) = sums_l(nzt:nzt+1,14,tn) + & |
---|
[102] | 643 | vswst(j,i) * rmask(j,i,sr) ! w"v" |
---|
[550] | 644 | sums_l(nzt:nzt+1,16,tn) = sums_l(nzt:nzt+1,16,tn) + & |
---|
[19] | 645 | tswst(j,i) * rmask(j,i,sr) ! w"pt" |
---|
[550] | 646 | sums_l(nzt:nzt+1,58,tn) = sums_l(nzt:nzt+1,58,tn) + & |
---|
[19] | 647 | 0.0 * rmask(j,i,sr) ! u"pt" |
---|
[550] | 648 | sums_l(nzt:nzt+1,61,tn) = sums_l(nzt:nzt+1,61,tn) + & |
---|
| 649 | 0.0 * rmask(j,i,sr) ! v"pt" |
---|
| 650 | |
---|
[96] | 651 | IF ( ocean ) THEN |
---|
| 652 | sums_l(nzt,65,tn) = sums_l(nzt,65,tn) + & |
---|
| 653 | saswst(j,i) * rmask(j,i,sr) ! w"sa" |
---|
| 654 | ENDIF |
---|
[75] | 655 | IF ( humidity ) THEN |
---|
[19] | 656 | sums_l(nzt,48,tn) = sums_l(nzt,48,tn) + & |
---|
[388] | 657 | qswst(j,i) * rmask(j,i,sr) ! w"q" (w"qv") |
---|
[19] | 658 | IF ( cloud_physics ) THEN |
---|
| 659 | sums_l(nzt,45,tn) = sums_l(nzt,45,tn) + ( & |
---|
| 660 | ( 1.0 + 0.61 * q(nzt,j,i) ) * & |
---|
| 661 | tswst(j,i) + 0.61 * pt(nzt,j,i) * & |
---|
| 662 | qsws(j,i) & |
---|
| 663 | ) |
---|
| 664 | ! |
---|
| 665 | !-- Formula does not work if ql(nzb) /= 0.0 |
---|
| 666 | sums_l(nzt,51,tn) = sums_l(nzt,51,tn) + & ! w"q" (w"qv") |
---|
| 667 | qswst(j,i) * rmask(j,i,sr) |
---|
| 668 | ENDIF |
---|
| 669 | ENDIF |
---|
| 670 | IF ( passive_scalar ) THEN |
---|
| 671 | sums_l(nzt,48,tn) = sums_l(nzt,48,tn) + & |
---|
[388] | 672 | qswst(j,i) * rmask(j,i,sr) ! w"q" (w"qv") |
---|
[19] | 673 | ENDIF |
---|
| 674 | ENDIF |
---|
| 675 | |
---|
| 676 | ! |
---|
[1] | 677 | !-- Resolved fluxes (can be computed for all horizontal points) |
---|
[132] | 678 | !-- NOTE: for simplicity, nzb_s_inner is used below, although strictly |
---|
[1] | 679 | !-- ---- speaking the following k-loop would have to be split up and |
---|
| 680 | !-- rearranged according to the staggered grid. |
---|
[132] | 681 | DO k = nzb_s_inner(j,i), nzt |
---|
[1] | 682 | ust = 0.5 * ( u(k,j,i) - hom(k,1,1,sr) + & |
---|
| 683 | u(k+1,j,i) - hom(k+1,1,1,sr) ) |
---|
| 684 | vst = 0.5 * ( v(k,j,i) - hom(k,1,2,sr) + & |
---|
| 685 | v(k+1,j,i) - hom(k+1,1,2,sr) ) |
---|
| 686 | pts = 0.5 * ( pt(k,j,i) - hom(k,1,4,sr) + & |
---|
| 687 | pt(k+1,j,i) - hom(k+1,1,4,sr) ) |
---|
[667] | 688 | |
---|
[1] | 689 | !-- Higher moments |
---|
| 690 | sums_l(k,35,tn) = sums_l(k,35,tn) + pts * w(k,j,i)**2 * & |
---|
| 691 | rmask(j,i,sr) |
---|
| 692 | sums_l(k,36,tn) = sums_l(k,36,tn) + pts**2 * w(k,j,i) * & |
---|
| 693 | rmask(j,i,sr) |
---|
| 694 | |
---|
| 695 | ! |
---|
[96] | 696 | !-- Salinity flux and density (density does not belong to here, |
---|
[97] | 697 | !-- but so far there is no other suitable place to calculate) |
---|
[96] | 698 | IF ( ocean ) THEN |
---|
[667] | 699 | IF( .NOT. ws_scheme_sca ) THEN |
---|
| 700 | pts = 0.5 * ( sa(k,j,i) - hom(k,1,23,sr) + & |
---|
[96] | 701 | sa(k+1,j,i) - hom(k+1,1,23,sr) ) |
---|
[667] | 702 | sums_l(k,66,tn) = sums_l(k,66,tn) + pts * w(k,j,i) * & |
---|
[96] | 703 | rmask(j,i,sr) |
---|
[667] | 704 | ENDIF |
---|
[96] | 705 | sums_l(k,64,tn) = sums_l(k,64,tn) + rho(k,j,i) * & |
---|
| 706 | rmask(j,i,sr) |
---|
[388] | 707 | sums_l(k,71,tn) = sums_l(k,71,tn) + prho(k,j,i) * & |
---|
| 708 | rmask(j,i,sr) |
---|
[96] | 709 | ENDIF |
---|
| 710 | |
---|
| 711 | ! |
---|
[1] | 712 | !-- Buoyancy flux, water flux, humidity flux and liquid water |
---|
| 713 | !-- content |
---|
[75] | 714 | IF ( humidity ) THEN |
---|
[1] | 715 | pts = 0.5 * ( vpt(k,j,i) - hom(k,1,44,sr) + & |
---|
| 716 | vpt(k+1,j,i) - hom(k+1,1,44,sr) ) |
---|
| 717 | sums_l(k,46,tn) = sums_l(k,46,tn) + pts * w(k,j,i) * & |
---|
| 718 | rmask(j,i,sr) |
---|
[667] | 719 | |
---|
[1] | 720 | IF ( cloud_physics .OR. cloud_droplets ) THEN |
---|
| 721 | pts = 0.5 * & |
---|
| 722 | ( ( q(k,j,i) - ql(k,j,i) ) - hom(k,1,42,sr) & |
---|
| 723 | + ( q(k+1,j,i) - ql(k+1,j,i) ) - hom(k+1,1,42,sr) ) |
---|
| 724 | sums_l(k,52,tn) = sums_l(k,52,tn) + pts * w(k,j,i) * & |
---|
| 725 | rmask(j,i,sr) |
---|
| 726 | sums_l(k,54,tn) = sums_l(k,54,tn) + ql(k,j,i) * & |
---|
| 727 | rmask(j,i,sr) |
---|
| 728 | ENDIF |
---|
| 729 | ENDIF |
---|
| 730 | |
---|
| 731 | ! |
---|
| 732 | !-- Passive scalar flux |
---|
[667] | 733 | IF ( passive_scalar .AND. ( .NOT. ws_scheme_sca )) THEN |
---|
[1] | 734 | pts = 0.5 * ( q(k,j,i) - hom(k,1,41,sr) + & |
---|
| 735 | q(k+1,j,i) - hom(k+1,1,41,sr) ) |
---|
| 736 | sums_l(k,49,tn) = sums_l(k,49,tn) + pts * w(k,j,i) * & |
---|
| 737 | rmask(j,i,sr) |
---|
| 738 | ENDIF |
---|
| 739 | |
---|
| 740 | ! |
---|
| 741 | !-- Energy flux w*e* |
---|
[667] | 742 | !-- has to be adjusted |
---|
| 743 | sums_l(k,37,tn) = sums_l(k,37,tn) + w(k,j,i) * 0.5 * & |
---|
| 744 | ( ust**2 + vst**2 + w(k,j,i)**2 )& |
---|
| 745 | * rmask(j,i,sr) |
---|
[1] | 746 | ENDDO |
---|
| 747 | ENDDO |
---|
| 748 | ENDDO |
---|
[667] | 749 | !- for reasons of speed optimization the loop is splitted, to avoid if-else |
---|
| 750 | !- statements inside the loop |
---|
| 751 | !- Fluxes which have been computed in part directly inside the advection routines |
---|
| 752 | !- treated seperatly. |
---|
| 753 | !- First treat the momentum fluxes |
---|
| 754 | IF ( .NOT. ws_scheme_mom ) THEN |
---|
| 755 | !$OMP DO |
---|
| 756 | DO i = nxl, nxr |
---|
| 757 | DO j = nys, nyn |
---|
| 758 | DO k = nzb_diff_s_inner(j,i)-1, nzt_diff |
---|
| 759 | ust = 0.5 * ( u(k,j,i) - hom(k,1,1,sr) + & |
---|
| 760 | u(k+1,j,i) - hom(k+1,1,1,sr) ) |
---|
| 761 | vst = 0.5 * ( v(k,j,i) - hom(k,1,2,sr) + & |
---|
| 762 | v(k+1,j,i) - hom(k+1,1,2,sr) ) |
---|
| 763 | ! |
---|
| 764 | !-- Momentum flux w*u* |
---|
| 765 | sums_l(k,13,tn) = sums_l(k,13,tn) + 0.5 * & |
---|
| 766 | ( w(k,j,i-1) + w(k,j,i) ) & |
---|
| 767 | * ust * rmask(j,i,sr) |
---|
| 768 | ! |
---|
| 769 | !-- Momentum flux w*v* |
---|
| 770 | sums_l(k,15,tn) = sums_l(k,15,tn) + 0.5 * & |
---|
| 771 | ( w(k,j-1,i) + w(k,j,i) ) & |
---|
| 772 | * vst * rmask(j,i,sr) |
---|
| 773 | ENDDO |
---|
| 774 | ENDDO |
---|
| 775 | ENDDO |
---|
[1] | 776 | |
---|
[667] | 777 | ENDIF |
---|
| 778 | IF ( .NOT. ws_scheme_sca ) THEN |
---|
| 779 | !$OMP DO |
---|
| 780 | DO i = nxl, nxr |
---|
| 781 | DO j = nys, nyn |
---|
| 782 | DO k = nzb_diff_s_inner(j,i) - 1, nzt_diff |
---|
| 783 | !- vertical heat flux |
---|
| 784 | sums_l(k,17,tn) = sums_l(k,17,tn) + 0.5 * & |
---|
| 785 | ( pt(k,j,i) - hom(k,1,4,sr) + & |
---|
| 786 | pt(k+1,j,i) - hom(k+1,1,4,sr) ) & |
---|
| 787 | * w(k,j,i) * rmask(j,i,sr) |
---|
| 788 | IF ( humidity ) THEN |
---|
| 789 | pts = 0.5 * ( q(k,j,i) - hom(k,1,41,sr) + & |
---|
| 790 | q(k+1,j,i) - hom(k+1,1,41,sr) ) |
---|
| 791 | sums_l(k,49,tn) = sums_l(k,49,tn) + pts * w(k,j,i) * & |
---|
| 792 | rmask(j,i,sr) |
---|
| 793 | ENDIF |
---|
| 794 | ENDDO |
---|
| 795 | ENDDO |
---|
| 796 | ENDDO |
---|
| 797 | |
---|
| 798 | ENDIF |
---|
| 799 | |
---|
| 800 | |
---|
[1] | 801 | ! |
---|
[97] | 802 | !-- Density at top follows Neumann condition |
---|
[388] | 803 | IF ( ocean ) THEN |
---|
| 804 | sums_l(nzt+1,64,tn) = sums_l(nzt,64,tn) |
---|
| 805 | sums_l(nzt+1,71,tn) = sums_l(nzt,71,tn) |
---|
| 806 | ENDIF |
---|
[97] | 807 | |
---|
| 808 | ! |
---|
[1] | 809 | !-- Divergence of vertical flux of resolved scale energy and pressure |
---|
[106] | 810 | !-- fluctuations as well as flux of pressure fluctuation itself (68). |
---|
| 811 | !-- First calculate the products, then the divergence. |
---|
[1] | 812 | !-- Calculation is time consuming. Do it only, if profiles shall be plotted. |
---|
[106] | 813 | IF ( hom(nzb+1,2,55,0) /= 0.0 .OR. hom(nzb+1,2,68,0) /= 0.0 ) THEN |
---|
[1] | 814 | |
---|
| 815 | sums_ll = 0.0 ! local array |
---|
| 816 | |
---|
| 817 | !$OMP DO |
---|
| 818 | DO i = nxl, nxr |
---|
| 819 | DO j = nys, nyn |
---|
[132] | 820 | DO k = nzb_s_inner(j,i)+1, nzt |
---|
[1] | 821 | |
---|
| 822 | sums_ll(k,1) = sums_ll(k,1) + 0.5 * w(k,j,i) * ( & |
---|
| 823 | ( 0.25 * ( u(k,j,i)+u(k+1,j,i)+u(k,j,i+1)+u(k+1,j,i+1) & |
---|
[678] | 824 | - 0.5 * ( hom(k,1,1,sr) + hom(k+1,1,1,sr) ) & |
---|
[1] | 825 | ) )**2 & |
---|
| 826 | + ( 0.25 * ( v(k,j,i)+v(k+1,j,i)+v(k,j+1,i)+v(k+1,j+1,i) & |
---|
[678] | 827 | - 0.5 * ( hom(k,1,2,sr) + hom(k+1,1,2,sr) ) & |
---|
[1] | 828 | ) )**2 & |
---|
| 829 | + w(k,j,i)**2 ) |
---|
| 830 | |
---|
| 831 | sums_ll(k,2) = sums_ll(k,2) + 0.5 * w(k,j,i) & |
---|
| 832 | * ( p(k,j,i) + p(k+1,j,i) ) |
---|
| 833 | |
---|
| 834 | ENDDO |
---|
| 835 | ENDDO |
---|
| 836 | ENDDO |
---|
| 837 | sums_ll(0,1) = 0.0 ! because w is zero at the bottom |
---|
| 838 | sums_ll(nzt+1,1) = 0.0 |
---|
| 839 | sums_ll(0,2) = 0.0 |
---|
| 840 | sums_ll(nzt+1,2) = 0.0 |
---|
| 841 | |
---|
[678] | 842 | DO k = nzb+1, nzt |
---|
[1] | 843 | sums_l(k,55,tn) = ( sums_ll(k,1) - sums_ll(k-1,1) ) * ddzw(k) |
---|
| 844 | sums_l(k,56,tn) = ( sums_ll(k,2) - sums_ll(k-1,2) ) * ddzw(k) |
---|
[106] | 845 | sums_l(k,68,tn) = sums_ll(k,2) |
---|
[1] | 846 | ENDDO |
---|
| 847 | sums_l(nzb,55,tn) = sums_l(nzb+1,55,tn) |
---|
| 848 | sums_l(nzb,56,tn) = sums_l(nzb+1,56,tn) |
---|
[106] | 849 | sums_l(nzb,68,tn) = 0.0 ! because w* = 0 at nzb |
---|
[1] | 850 | |
---|
| 851 | ENDIF |
---|
| 852 | |
---|
| 853 | ! |
---|
[106] | 854 | !-- Divergence of vertical flux of SGS TKE and the flux itself (69) |
---|
| 855 | IF ( hom(nzb+1,2,57,0) /= 0.0 .OR. hom(nzb+1,2,69,0) /= 0.0 ) THEN |
---|
[1] | 856 | |
---|
| 857 | !$OMP DO |
---|
| 858 | DO i = nxl, nxr |
---|
| 859 | DO j = nys, nyn |
---|
[132] | 860 | DO k = nzb_s_inner(j,i)+1, nzt |
---|
[1] | 861 | |
---|
[106] | 862 | sums_l(k,57,tn) = sums_l(k,57,tn) - 0.5 * ( & |
---|
[1] | 863 | (km(k,j,i)+km(k+1,j,i)) * (e(k+1,j,i)-e(k,j,i)) * ddzu(k+1) & |
---|
| 864 | - (km(k-1,j,i)+km(k,j,i)) * (e(k,j,i)-e(k-1,j,i)) * ddzu(k) & |
---|
[106] | 865 | ) * ddzw(k) |
---|
[1] | 866 | |
---|
[106] | 867 | sums_l(k,69,tn) = sums_l(k,69,tn) - 0.5 * ( & |
---|
| 868 | (km(k,j,i)+km(k+1,j,i)) * (e(k+1,j,i)-e(k,j,i)) * ddzu(k+1) & |
---|
| 869 | ) |
---|
| 870 | |
---|
[1] | 871 | ENDDO |
---|
| 872 | ENDDO |
---|
| 873 | ENDDO |
---|
| 874 | sums_l(nzb,57,tn) = sums_l(nzb+1,57,tn) |
---|
[106] | 875 | sums_l(nzb,69,tn) = sums_l(nzb+1,69,tn) |
---|
[1] | 876 | |
---|
| 877 | ENDIF |
---|
| 878 | |
---|
| 879 | ! |
---|
| 880 | !-- Horizontal heat fluxes (subgrid, resolved, total). |
---|
| 881 | !-- Do it only, if profiles shall be plotted. |
---|
| 882 | IF ( hom(nzb+1,2,58,0) /= 0.0 ) THEN |
---|
| 883 | |
---|
| 884 | !$OMP DO |
---|
| 885 | DO i = nxl, nxr |
---|
| 886 | DO j = nys, nyn |
---|
[132] | 887 | DO k = nzb_s_inner(j,i)+1, nzt |
---|
[1] | 888 | ! |
---|
| 889 | !-- Subgrid horizontal heat fluxes u"pt", v"pt" |
---|
| 890 | sums_l(k,58,tn) = sums_l(k,58,tn) - 0.5 * & |
---|
| 891 | ( kh(k,j,i) + kh(k,j,i-1) ) & |
---|
| 892 | * ( pt(k,j,i-1) - pt(k,j,i) ) & |
---|
| 893 | * ddx * rmask(j,i,sr) |
---|
| 894 | sums_l(k,61,tn) = sums_l(k,61,tn) - 0.5 * & |
---|
| 895 | ( kh(k,j,i) + kh(k,j-1,i) ) & |
---|
| 896 | * ( pt(k,j-1,i) - pt(k,j,i) ) & |
---|
| 897 | * ddy * rmask(j,i,sr) |
---|
| 898 | ! |
---|
| 899 | !-- Resolved horizontal heat fluxes u*pt*, v*pt* |
---|
| 900 | sums_l(k,59,tn) = sums_l(k,59,tn) + & |
---|
| 901 | ( u(k,j,i) - hom(k,1,1,sr) ) & |
---|
| 902 | * 0.5 * ( pt(k,j,i-1) - hom(k,1,4,sr) + & |
---|
| 903 | pt(k,j,i) - hom(k,1,4,sr) ) |
---|
| 904 | pts = 0.5 * ( pt(k,j-1,i) - hom(k,1,4,sr) + & |
---|
| 905 | pt(k,j,i) - hom(k,1,4,sr) ) |
---|
| 906 | sums_l(k,62,tn) = sums_l(k,62,tn) + & |
---|
| 907 | ( v(k,j,i) - hom(k,1,2,sr) ) & |
---|
| 908 | * 0.5 * ( pt(k,j-1,i) - hom(k,1,4,sr) + & |
---|
| 909 | pt(k,j,i) - hom(k,1,4,sr) ) |
---|
| 910 | ENDDO |
---|
| 911 | ENDDO |
---|
| 912 | ENDDO |
---|
| 913 | ! |
---|
| 914 | !-- Fluxes at the surface must be zero (e.g. due to the Prandtl-layer) |
---|
[97] | 915 | sums_l(nzb,58,tn) = 0.0 |
---|
| 916 | sums_l(nzb,59,tn) = 0.0 |
---|
| 917 | sums_l(nzb,60,tn) = 0.0 |
---|
| 918 | sums_l(nzb,61,tn) = 0.0 |
---|
| 919 | sums_l(nzb,62,tn) = 0.0 |
---|
| 920 | sums_l(nzb,63,tn) = 0.0 |
---|
[1] | 921 | |
---|
| 922 | ENDIF |
---|
[87] | 923 | |
---|
| 924 | ! |
---|
| 925 | !-- Calculate the user-defined profiles |
---|
| 926 | CALL user_statistics( 'profiles', sr, tn ) |
---|
[1] | 927 | !$OMP END PARALLEL |
---|
| 928 | |
---|
| 929 | ! |
---|
| 930 | !-- Summation of thread sums |
---|
| 931 | IF ( threads_per_task > 1 ) THEN |
---|
| 932 | DO i = 1, threads_per_task-1 |
---|
| 933 | sums_l(:,3,0) = sums_l(:,3,0) + sums_l(:,3,i) |
---|
| 934 | sums_l(:,4:40,0) = sums_l(:,4:40,0) + sums_l(:,4:40,i) |
---|
[87] | 935 | sums_l(:,45:pr_palm,0) = sums_l(:,45:pr_palm,0) + & |
---|
| 936 | sums_l(:,45:pr_palm,i) |
---|
| 937 | IF ( max_pr_user > 0 ) THEN |
---|
| 938 | sums_l(:,pr_palm+1:pr_palm+max_pr_user,0) = & |
---|
| 939 | sums_l(:,pr_palm+1:pr_palm+max_pr_user,0) + & |
---|
| 940 | sums_l(:,pr_palm+1:pr_palm+max_pr_user,i) |
---|
| 941 | ENDIF |
---|
[1] | 942 | ENDDO |
---|
| 943 | ENDIF |
---|
| 944 | |
---|
| 945 | #if defined( __parallel ) |
---|
[667] | 946 | |
---|
[1] | 947 | ! |
---|
| 948 | !-- Compute total sum from local sums |
---|
[622] | 949 | IF ( collective_wait ) CALL MPI_BARRIER( comm2d, ierr ) |
---|
[1] | 950 | CALL MPI_ALLREDUCE( sums_l(nzb,1,0), sums(nzb,1), ngp_sums, MPI_REAL, & |
---|
| 951 | MPI_SUM, comm2d, ierr ) |
---|
| 952 | #else |
---|
| 953 | sums = sums_l(:,:,0) |
---|
| 954 | #endif |
---|
| 955 | |
---|
| 956 | ! |
---|
| 957 | !-- Final values are obtained by division by the total number of grid points |
---|
| 958 | !-- used for summation. After that store profiles. |
---|
| 959 | !-- Profiles: |
---|
| 960 | DO k = nzb, nzt+1 |
---|
[132] | 961 | sums(k,3) = sums(k,3) / ngp_2dh(sr) |
---|
[142] | 962 | sums(k,8:11) = sums(k,8:11) / ngp_2dh_s_inner(k,sr) |
---|
[132] | 963 | sums(k,12:22) = sums(k,12:22) / ngp_2dh(sr) |
---|
| 964 | sums(k,23:29) = sums(k,23:29) / ngp_2dh_s_inner(k,sr) |
---|
| 965 | sums(k,30:32) = sums(k,30:32) / ngp_2dh(sr) |
---|
[142] | 966 | sums(k,33:34) = sums(k,33:34) / ngp_2dh_s_inner(k,sr) |
---|
| 967 | sums(k,35:39) = sums(k,35:39) / ngp_2dh(sr) |
---|
[132] | 968 | sums(k,40) = sums(k,40) / ngp_2dh_s_inner(k,sr) |
---|
| 969 | sums(k,45:53) = sums(k,45:53) / ngp_2dh(sr) |
---|
| 970 | sums(k,54) = sums(k,54) / ngp_2dh_s_inner(k,sr) |
---|
| 971 | sums(k,55:63) = sums(k,55:63) / ngp_2dh(sr) |
---|
| 972 | sums(k,64) = sums(k,64) / ngp_2dh_s_inner(k,sr) |
---|
| 973 | sums(k,65:69) = sums(k,65:69) / ngp_2dh(sr) |
---|
| 974 | sums(k,70:pr_palm-2) = sums(k,70:pr_palm-2)/ ngp_2dh_s_inner(k,sr) |
---|
[1] | 975 | ENDDO |
---|
[667] | 976 | |
---|
[1] | 977 | !-- Upstream-parts |
---|
[87] | 978 | sums(nzb:nzb+11,pr_palm-1) = sums(nzb:nzb+11,pr_palm-1) / ngp_3d(sr) |
---|
[1] | 979 | !-- u* and so on |
---|
[87] | 980 | !-- As sums(nzb:nzb+3,pr_palm) are full 2D arrays (us, usws, vsws, ts) whose |
---|
[1] | 981 | !-- size is always ( nx + 1 ) * ( ny + 1 ), defined at the first grid layer |
---|
| 982 | !-- above the topography, they are being divided by ngp_2dh(sr) |
---|
[87] | 983 | sums(nzb:nzb+3,pr_palm) = sums(nzb:nzb+3,pr_palm) / & |
---|
[1] | 984 | ngp_2dh(sr) |
---|
[197] | 985 | sums(nzb+12,pr_palm) = sums(nzb+12,pr_palm) / & ! qs |
---|
| 986 | ngp_2dh(sr) |
---|
[1] | 987 | !-- eges, e* |
---|
[87] | 988 | sums(nzb+4:nzb+5,pr_palm) = sums(nzb+4:nzb+5,pr_palm) / & |
---|
[132] | 989 | ngp_3d(sr) |
---|
[1] | 990 | !-- Old and new divergence |
---|
[87] | 991 | sums(nzb+9:nzb+10,pr_palm) = sums(nzb+9:nzb+10,pr_palm) / & |
---|
[1] | 992 | ngp_3d_inner(sr) |
---|
| 993 | |
---|
[87] | 994 | !-- User-defined profiles |
---|
| 995 | IF ( max_pr_user > 0 ) THEN |
---|
| 996 | DO k = nzb, nzt+1 |
---|
| 997 | sums(k,pr_palm+1:pr_palm+max_pr_user) = & |
---|
| 998 | sums(k,pr_palm+1:pr_palm+max_pr_user) / & |
---|
[132] | 999 | ngp_2dh_s_inner(k,sr) |
---|
[87] | 1000 | ENDDO |
---|
| 1001 | ENDIF |
---|
[1] | 1002 | ! |
---|
| 1003 | !-- Collect horizontal average in hom. |
---|
| 1004 | !-- Compute deduced averages (e.g. total heat flux) |
---|
| 1005 | hom(:,1,3,sr) = sums(:,3) ! w |
---|
| 1006 | hom(:,1,8,sr) = sums(:,8) ! e profiles 5-7 are initial profiles |
---|
| 1007 | hom(:,1,9,sr) = sums(:,9) ! km |
---|
| 1008 | hom(:,1,10,sr) = sums(:,10) ! kh |
---|
| 1009 | hom(:,1,11,sr) = sums(:,11) ! l |
---|
| 1010 | hom(:,1,12,sr) = sums(:,12) ! w"u" |
---|
| 1011 | hom(:,1,13,sr) = sums(:,13) ! w*u* |
---|
| 1012 | hom(:,1,14,sr) = sums(:,14) ! w"v" |
---|
| 1013 | hom(:,1,15,sr) = sums(:,15) ! w*v* |
---|
| 1014 | hom(:,1,16,sr) = sums(:,16) ! w"pt" |
---|
| 1015 | hom(:,1,17,sr) = sums(:,17) ! w*pt* |
---|
| 1016 | hom(:,1,18,sr) = sums(:,16) + sums(:,17) ! wpt |
---|
| 1017 | hom(:,1,19,sr) = sums(:,12) + sums(:,13) ! wu |
---|
| 1018 | hom(:,1,20,sr) = sums(:,14) + sums(:,15) ! wv |
---|
| 1019 | hom(:,1,21,sr) = sums(:,21) ! w*pt*BC |
---|
| 1020 | hom(:,1,22,sr) = sums(:,16) + sums(:,21) ! wptBC |
---|
[96] | 1021 | ! profile 24 is initial profile (sa) |
---|
| 1022 | ! profiles 25-29 left empty for initial |
---|
[1] | 1023 | ! profiles |
---|
| 1024 | hom(:,1,30,sr) = sums(:,30) ! u*2 |
---|
| 1025 | hom(:,1,31,sr) = sums(:,31) ! v*2 |
---|
| 1026 | hom(:,1,32,sr) = sums(:,32) ! w*2 |
---|
| 1027 | hom(:,1,33,sr) = sums(:,33) ! pt*2 |
---|
| 1028 | hom(:,1,34,sr) = sums(:,34) ! e* |
---|
| 1029 | hom(:,1,35,sr) = sums(:,35) ! w*2pt* |
---|
| 1030 | hom(:,1,36,sr) = sums(:,36) ! w*pt*2 |
---|
| 1031 | hom(:,1,37,sr) = sums(:,37) ! w*e* |
---|
| 1032 | hom(:,1,38,sr) = sums(:,38) ! w*3 |
---|
| 1033 | hom(:,1,39,sr) = sums(:,38) / ( sums(:,32) + 1E-20 )**1.5 ! Sw |
---|
| 1034 | hom(:,1,40,sr) = sums(:,40) ! p |
---|
[531] | 1035 | hom(:,1,45,sr) = sums(:,45) ! w"vpt" |
---|
[1] | 1036 | hom(:,1,46,sr) = sums(:,46) ! w*vpt* |
---|
| 1037 | hom(:,1,47,sr) = sums(:,45) + sums(:,46) ! wvpt |
---|
| 1038 | hom(:,1,48,sr) = sums(:,48) ! w"q" (w"qv") |
---|
| 1039 | hom(:,1,49,sr) = sums(:,49) ! w*q* (w*qv*) |
---|
| 1040 | hom(:,1,50,sr) = sums(:,48) + sums(:,49) ! wq (wqv) |
---|
| 1041 | hom(:,1,51,sr) = sums(:,51) ! w"qv" |
---|
| 1042 | hom(:,1,52,sr) = sums(:,52) ! w*qv* |
---|
| 1043 | hom(:,1,53,sr) = sums(:,52) + sums(:,51) ! wq (wqv) |
---|
| 1044 | hom(:,1,54,sr) = sums(:,54) ! ql |
---|
| 1045 | hom(:,1,55,sr) = sums(:,55) ! w*u*u*/dz |
---|
| 1046 | hom(:,1,56,sr) = sums(:,56) ! w*p*/dz |
---|
[106] | 1047 | hom(:,1,57,sr) = sums(:,57) ! ( w"e + w"p"/rho )/dz |
---|
[1] | 1048 | hom(:,1,58,sr) = sums(:,58) ! u"pt" |
---|
| 1049 | hom(:,1,59,sr) = sums(:,59) ! u*pt* |
---|
| 1050 | hom(:,1,60,sr) = sums(:,58) + sums(:,59) ! upt_t |
---|
| 1051 | hom(:,1,61,sr) = sums(:,61) ! v"pt" |
---|
| 1052 | hom(:,1,62,sr) = sums(:,62) ! v*pt* |
---|
| 1053 | hom(:,1,63,sr) = sums(:,61) + sums(:,62) ! vpt_t |
---|
[96] | 1054 | hom(:,1,64,sr) = sums(:,64) ! rho |
---|
| 1055 | hom(:,1,65,sr) = sums(:,65) ! w"sa" |
---|
| 1056 | hom(:,1,66,sr) = sums(:,66) ! w*sa* |
---|
| 1057 | hom(:,1,67,sr) = sums(:,65) + sums(:,66) ! wsa |
---|
[106] | 1058 | hom(:,1,68,sr) = sums(:,68) ! w*p* |
---|
| 1059 | hom(:,1,69,sr) = sums(:,69) ! w"e + w"p"/rho |
---|
[197] | 1060 | hom(:,1,70,sr) = sums(:,70) ! q*2 |
---|
[388] | 1061 | hom(:,1,71,sr) = sums(:,71) ! prho |
---|
[531] | 1062 | hom(:,1,72,sr) = hyp * 1E-4 ! hyp in dbar |
---|
[1] | 1063 | |
---|
[87] | 1064 | hom(:,1,pr_palm-1,sr) = sums(:,pr_palm-1) |
---|
[1] | 1065 | ! upstream-parts u_x, u_y, u_z, v_x, |
---|
| 1066 | ! v_y, usw. (in last but one profile) |
---|
[667] | 1067 | hom(:,1,pr_palm,sr) = sums(:,pr_palm) |
---|
[1] | 1068 | ! u*, w'u', w'v', t* (in last profile) |
---|
| 1069 | |
---|
[87] | 1070 | IF ( max_pr_user > 0 ) THEN ! user-defined profiles |
---|
| 1071 | hom(:,1,pr_palm+1:pr_palm+max_pr_user,sr) = & |
---|
| 1072 | sums(:,pr_palm+1:pr_palm+max_pr_user) |
---|
| 1073 | ENDIF |
---|
| 1074 | |
---|
[1] | 1075 | ! |
---|
| 1076 | !-- Determine the boundary layer height using two different schemes. |
---|
[94] | 1077 | !-- First scheme: Starting from the Earth's (Ocean's) surface, look for the |
---|
| 1078 | !-- first relative minimum (maximum) of the total heat flux. |
---|
| 1079 | !-- The corresponding height is assumed as the boundary layer height, if it |
---|
| 1080 | !-- is less than 1.5 times the height where the heat flux becomes negative |
---|
| 1081 | !-- (positive) for the first time. |
---|
[1] | 1082 | z_i(1) = 0.0 |
---|
| 1083 | first = .TRUE. |
---|
[667] | 1084 | |
---|
[97] | 1085 | IF ( ocean ) THEN |
---|
| 1086 | DO k = nzt, nzb+1, -1 |
---|
[667] | 1087 | IF ( first .AND. hom(k,1,18,sr) < 0.0 & |
---|
| 1088 | .AND. abs(hom(k,1,18,sr)) > 1.0E-8) THEN |
---|
[97] | 1089 | first = .FALSE. |
---|
| 1090 | height = zw(k) |
---|
| 1091 | ENDIF |
---|
| 1092 | IF ( hom(k,1,18,sr) < 0.0 .AND. & |
---|
[667] | 1093 | abs(hom(k,1,18,sr)) > 1.0E-8 .AND. & |
---|
[97] | 1094 | hom(k-1,1,18,sr) > hom(k,1,18,sr) ) THEN |
---|
| 1095 | IF ( zw(k) < 1.5 * height ) THEN |
---|
| 1096 | z_i(1) = zw(k) |
---|
| 1097 | ELSE |
---|
| 1098 | z_i(1) = height |
---|
| 1099 | ENDIF |
---|
| 1100 | EXIT |
---|
| 1101 | ENDIF |
---|
| 1102 | ENDDO |
---|
| 1103 | ELSE |
---|
[94] | 1104 | DO k = nzb, nzt-1 |
---|
[667] | 1105 | IF ( first .AND. hom(k,1,18,sr) < 0.0 & |
---|
| 1106 | .AND. abs(hom(k,1,18,sr)) > 1.0E-8 ) THEN |
---|
[94] | 1107 | first = .FALSE. |
---|
| 1108 | height = zw(k) |
---|
[1] | 1109 | ENDIF |
---|
[667] | 1110 | IF ( hom(k,1,18,sr) < 0.0 .AND. & |
---|
| 1111 | abs(hom(k,1,18,sr)) > 1.0E-8 .AND. & |
---|
[94] | 1112 | hom(k+1,1,18,sr) > hom(k,1,18,sr) ) THEN |
---|
| 1113 | IF ( zw(k) < 1.5 * height ) THEN |
---|
| 1114 | z_i(1) = zw(k) |
---|
| 1115 | ELSE |
---|
| 1116 | z_i(1) = height |
---|
| 1117 | ENDIF |
---|
| 1118 | EXIT |
---|
| 1119 | ENDIF |
---|
| 1120 | ENDDO |
---|
[97] | 1121 | ENDIF |
---|
[1] | 1122 | |
---|
| 1123 | ! |
---|
[291] | 1124 | !-- Second scheme: Gradient scheme from Sullivan et al. (1998), modified |
---|
| 1125 | !-- by Uhlenbrock(2006). The boundary layer height is the height with the |
---|
| 1126 | !-- maximal local temperature gradient: starting from the second (the last |
---|
| 1127 | !-- but one) vertical gridpoint, the local gradient must be at least |
---|
| 1128 | !-- 0.2K/100m and greater than the next four gradients. |
---|
| 1129 | !-- WARNING: The threshold value of 0.2K/100m must be adjusted for the |
---|
| 1130 | !-- ocean case! |
---|
[1] | 1131 | z_i(2) = 0.0 |
---|
[291] | 1132 | DO k = nzb+1, nzt+1 |
---|
| 1133 | dptdz(k) = ( hom(k,1,4,sr) - hom(k-1,1,4,sr) ) * ddzu(k) |
---|
| 1134 | ENDDO |
---|
| 1135 | dptdz_threshold = 0.2 / 100.0 |
---|
| 1136 | |
---|
[97] | 1137 | IF ( ocean ) THEN |
---|
[291] | 1138 | DO k = nzt+1, nzb+5, -1 |
---|
| 1139 | IF ( dptdz(k) > dptdz_threshold .AND. & |
---|
| 1140 | dptdz(k) > dptdz(k-1) .AND. dptdz(k) > dptdz(k-2) .AND. & |
---|
| 1141 | dptdz(k) > dptdz(k-3) .AND. dptdz(k) > dptdz(k-4) ) THEN |
---|
| 1142 | z_i(2) = zw(k-1) |
---|
[97] | 1143 | EXIT |
---|
| 1144 | ENDIF |
---|
| 1145 | ENDDO |
---|
| 1146 | ELSE |
---|
[291] | 1147 | DO k = nzb+1, nzt-3 |
---|
| 1148 | IF ( dptdz(k) > dptdz_threshold .AND. & |
---|
| 1149 | dptdz(k) > dptdz(k+1) .AND. dptdz(k) > dptdz(k+2) .AND. & |
---|
| 1150 | dptdz(k) > dptdz(k+3) .AND. dptdz(k) > dptdz(k+4) ) THEN |
---|
| 1151 | z_i(2) = zw(k-1) |
---|
[97] | 1152 | EXIT |
---|
| 1153 | ENDIF |
---|
| 1154 | ENDDO |
---|
| 1155 | ENDIF |
---|
[1] | 1156 | |
---|
[87] | 1157 | hom(nzb+6,1,pr_palm,sr) = z_i(1) |
---|
| 1158 | hom(nzb+7,1,pr_palm,sr) = z_i(2) |
---|
[1] | 1159 | |
---|
| 1160 | ! |
---|
| 1161 | !-- Computation of both the characteristic vertical velocity and |
---|
| 1162 | !-- the characteristic convective boundary layer temperature. |
---|
| 1163 | !-- The horizontal average at nzb+1 is input for the average temperature. |
---|
[667] | 1164 | IF ( hom(nzb,1,18,sr) > 0.0 .AND. abs(hom(nzb,1,18,sr)) > 1.0E-8 & |
---|
| 1165 | .AND. z_i(1) /= 0.0 ) THEN |
---|
[87] | 1166 | hom(nzb+8,1,pr_palm,sr) = ( g / hom(nzb+1,1,4,sr) * & |
---|
[94] | 1167 | hom(nzb,1,18,sr) * & |
---|
| 1168 | ABS( z_i(1) ) )**0.333333333 |
---|
[1] | 1169 | !-- so far this only works if Prandtl layer is used |
---|
[87] | 1170 | hom(nzb+11,1,pr_palm,sr) = hom(nzb,1,16,sr) / hom(nzb+8,1,pr_palm,sr) |
---|
[1] | 1171 | ELSE |
---|
[87] | 1172 | hom(nzb+8,1,pr_palm,sr) = 0.0 |
---|
| 1173 | hom(nzb+11,1,pr_palm,sr) = 0.0 |
---|
[1] | 1174 | ENDIF |
---|
| 1175 | |
---|
[48] | 1176 | ! |
---|
| 1177 | !-- Collect the time series quantities |
---|
[87] | 1178 | ts_value(1,sr) = hom(nzb+4,1,pr_palm,sr) ! E |
---|
| 1179 | ts_value(2,sr) = hom(nzb+5,1,pr_palm,sr) ! E* |
---|
[48] | 1180 | ts_value(3,sr) = dt_3d |
---|
[87] | 1181 | ts_value(4,sr) = hom(nzb,1,pr_palm,sr) ! u* |
---|
| 1182 | ts_value(5,sr) = hom(nzb+3,1,pr_palm,sr) ! th* |
---|
[48] | 1183 | ts_value(6,sr) = u_max |
---|
| 1184 | ts_value(7,sr) = v_max |
---|
| 1185 | ts_value(8,sr) = w_max |
---|
[87] | 1186 | ts_value(9,sr) = hom(nzb+10,1,pr_palm,sr) ! new divergence |
---|
| 1187 | ts_value(10,sr) = hom(nzb+9,1,pr_palm,sr) ! old Divergence |
---|
| 1188 | ts_value(11,sr) = hom(nzb+6,1,pr_palm,sr) ! z_i(1) |
---|
| 1189 | ts_value(12,sr) = hom(nzb+7,1,pr_palm,sr) ! z_i(2) |
---|
| 1190 | ts_value(13,sr) = hom(nzb+8,1,pr_palm,sr) ! w* |
---|
[48] | 1191 | ts_value(14,sr) = hom(nzb,1,16,sr) ! w'pt' at k=0 |
---|
| 1192 | ts_value(15,sr) = hom(nzb+1,1,16,sr) ! w'pt' at k=1 |
---|
| 1193 | ts_value(16,sr) = hom(nzb+1,1,18,sr) ! wpt at k=1 |
---|
| 1194 | ts_value(17,sr) = hom(nzb,1,4,sr) ! pt(0) |
---|
| 1195 | ts_value(18,sr) = hom(nzb+1,1,4,sr) ! pt(zp) |
---|
[197] | 1196 | ts_value(19,sr) = hom(nzb+1,1,pr_palm,sr) ! u'w' at k=0 |
---|
| 1197 | ts_value(20,sr) = hom(nzb+2,1,pr_palm,sr) ! v'w' at k=0 |
---|
[343] | 1198 | ts_value(21,sr) = hom(nzb,1,48,sr) ! w"q" at k=0 |
---|
[197] | 1199 | |
---|
[48] | 1200 | IF ( ts_value(5,sr) /= 0.0 ) THEN |
---|
| 1201 | ts_value(22,sr) = ts_value(4,sr)**2 / & |
---|
| 1202 | ( kappa * g * ts_value(5,sr) / ts_value(18,sr) ) ! L |
---|
| 1203 | ELSE |
---|
| 1204 | ts_value(22,sr) = 10000.0 |
---|
| 1205 | ENDIF |
---|
[1] | 1206 | |
---|
[343] | 1207 | ts_value(23,sr) = hom(nzb+12,1,pr_palm,sr) ! q* |
---|
[1] | 1208 | ! |
---|
[48] | 1209 | !-- Calculate additional statistics provided by the user interface |
---|
[87] | 1210 | CALL user_statistics( 'time_series', sr, 0 ) |
---|
[1] | 1211 | |
---|
[48] | 1212 | ENDDO ! loop of the subregions |
---|
| 1213 | |
---|
[1] | 1214 | ! |
---|
| 1215 | !-- If required, sum up horizontal averages for subsequent time averaging |
---|
| 1216 | IF ( do_sum ) THEN |
---|
| 1217 | IF ( average_count_pr == 0 ) hom_sum = 0.0 |
---|
| 1218 | hom_sum = hom_sum + hom(:,1,:,:) |
---|
| 1219 | average_count_pr = average_count_pr + 1 |
---|
| 1220 | do_sum = .FALSE. |
---|
| 1221 | ENDIF |
---|
| 1222 | |
---|
| 1223 | ! |
---|
| 1224 | !-- Set flag for other UPs (e.g. output routines, but also buoyancy). |
---|
| 1225 | !-- This flag is reset after each time step in time_integration. |
---|
| 1226 | flow_statistics_called = .TRUE. |
---|
| 1227 | |
---|
| 1228 | CALL cpu_log( log_point(10), 'flow_statistics', 'stop' ) |
---|
| 1229 | |
---|
| 1230 | |
---|
| 1231 | END SUBROUTINE flow_statistics |
---|
| 1232 | |
---|
| 1233 | |
---|
| 1234 | |
---|