Changes between Version 54 and Version 55 of doc/tec/changelog_2018

Timestamp:

Jan 4, 2011 3:12:26 PM (14 years ago)

Author:

suehring

Comment:

--

doc/tec/changelog_2018

@@ -28 +28 @@
 }}}
 {{{#!td style="vertical-align:top"
-'''Most important changes:''' New advection scheme added ( Wicker and Skamarock 5th order ). For further information
-see [../../app/inipar/#momentum_advec momentum_advec] and [../../app/inipar/#scalar_advec scalar_advec]. (advec_ws)
-
-Changes in coupling: Different number of processors and different horizontal resolution in ocean and atmosphere is now allowed.
-Furthermore u and v from the ocean surface is now used as bottom boundary for the atmosphere.
-
-Bottom boundary conditions for u and v  changed from mirror to dirichlet boundary conditions.
-
-Inflow turbulence is now defined by fluctuations around spanwise mean.
-
-Removed mirror boundary conditions for u and v at the bottom in case of
-ibc_uv_b == 0. Instead, dirichlet boundary conditions (u=v=0) are set
-in init_3d_model. (boundary_conds)
-
-Exchange of parameters between ocean and atmosphere via PE0
+'''Most important changes:''' New advection scheme added. Different number of processors and different horizontal resolution in ocean and atmosphere is now allowed. Bottom boundary conditions for u and v  changed from mirror to dirichlet boundary conditions. Inflow turbulence is now defined by fluctuations around spanwise mean. 
+
+Advection scheme ( see [../../app/inipar/#momentum_advec momentum_advec] and [../../app/inipar/#scalar_advec scalar_advec] ) :
+
+New advection scheme added ( Wicker and Skamarock 5th order ). Turbulent fluxes are computed directly inside advection routines, removed from flow_statistics. (advec_ws)
+
 Check for illegal combination of ws-scheme and [../../app/inipar/#timestep_scheme timestep_scheme].
 Check for [../../app/inipar/#topography topography] and ws-scheme.
 Check for not cyclic boundary conditions in combination with ws-scheme and [../../app/inipar/#loop_optimization loop_optimization] = 'vector'.
-Check for [../../app/inipar#call_psolver_at_all_substeps call_psolver_at_all_substeps] and [../../app/inipar#momentum_advec momentum_advec] = 'ws-scheme'.
-Different processor/grid topology in atmosphere and ocean is now allowed! (check_parameters)
-
-Dynamic exchange of ghost points with nbgp_local to ensure that no useless 
-ghost points exchanged in case of multigrid. type_yz(0) and type_xz(0) used for
-normal grid, the remaining types used for the several grid levels. 
-Exchange is done via MPI-Vectors with a dynamic value of ghost points which 
-depend on the advection scheme. Exchange of left and right PEs is 10% faster
-with MPI-Vectors than without. (exchange_horiz, exchange_horiz_2d)
+Check for [../../app/inipar#call_psolver_at_all_substeps call_psolver_at_all_substeps] and [../../app/inipar#momentum_advec momentum_advec] = 'ws-scheme'. (check_parameters)
 
 When advection is computed with ws-scheme, turbulent fluxes are already 
@@ -64 +47 @@
 (flow_statistics)
 
-Using nbgp recycling planes for a better resolution of the turbulent flow near
-the inflow. (inflow_turbulence)
-
 Definition of new array bounds nxlg, nxrg, nylg, nyng on each PE. 
-Furthermore the allocation of arrays and steering of loops is done with these
-parameters. In case of dirichlet boundary condition at the bottom zu(0)=0.0
-dzu_mg has to be set explicitly for a equally spaced grid near bottom.
-ddzu_pres added to use a equally spaced grid near bottom. (init_grid)
-
-Moved determination of target_id's from init_coupling.
-Determination of parameters needed for coupling (coupling_topology, ngp_a, ngp_o)
-with different grid/processor-topology in ocean and atmosphere
-Adaption of ngp_xy, ngp_y to a dynamic number of ghost points.
-The maximum_grid_level changed from 1 to 0. 0 is the normal grid, 1 to 
-maximum_grid_level the grids for multigrid, in which 0 and 1 are normal grids.
-This distinction is due to reasons of data exchange and performance for the 
-normal grid and grids in poismg.
-The definition of MPI-Vectors adapted to a dynamic number of ghost points.
-New MPI-Vectors for data exchange between left and right boundaries added. 
-This is due to reasons of performance (10% faster).
-ATTENTION: nnz_x undefined problem still has to be solved!!!!!!!!
-TEST OUTPUT (TO BE REMOVED) logging mpi2 ierr values. (init_pegrid)
+Furthermore the allocation of arrays and steering of loops is done with these parameters.
+( init_grid )
 
 Call ws_init to initialize arrays needed for statistical evaluation and
-optimization when ws-scheme is used. (init_3d_model)
+optimization when ws-scheme is used. (init_3d_model) 
 
 Module advec_ws added. (Makefile)
 
-Removed u_nzb_p1_for_vfc and v_nzb_p1_for_vfc
-For coupling with different resolution in ocean and atmosphere:
-+nx_a, +nx_o, +ny_a, +ny_o, +ngp_a, +ngp_o, +total_2d_o, +total_2d_a,
-+coupling_topology 
 Buffer arrays for the left sided advective fluxes added in arrays_3d.
 +flux_s_u, +flux_s_v, +flux_s_w, +diss_s_u, +diss_s_v, +diss_s_w,
@@ -116 +76 @@
 reasons of performance of the data_exchange. The same is done with p after
 poismg is called.
-nxl-1, nxr+1, nys-1, nyn+1 replaced by nxlg, nxrg, nysg, nyng when no 
-multigrid is used.
-Call of SOR routine is referenced with ddzu_pres. (pres)
 
 Calls of the advection routines with WS5 added.
@@ -124 +81 @@
 time step. (prognostic_equations)
 
+Coupling:
+
+
+Different processor/grid topology in atmosphere and ocean is now allowed! (check_parameters)
+
+Moved determination of target_id's from init_coupling.
+Exchange of parameters between ocean and atmosphere via PE0
+Determination of parameters needed for coupling (coupling_topology, ngp_a, ngp_o)
+with different grid/processor-topology in ocean and atmosphere
+Adaption of ngp_xy, ngp_y to a dynamic number of ghost points.
+ATTENTION: nnz_x undefined problem still has to be solved!!!!!!!!
+TEST OUTPUT (TO BE REMOVED) logging mpi2 ierr values. (init_pegrid)
+
+Removed u_nzb_p1_for_vfc and v_nzb_p1_for_vfc
+For coupling with different resolution in ocean and atmosphere:
++nx_a, +nx_o, +ny_a, +ny_o, +ngp_a, +ngp_o, +total_2d_o, +total_2d_a,
++coupling_topology (modules)
+
 Additional case for nonequivalent processor and grid topology in ocean and 
 atmosphere added (coupling_topology = 1).
@@ -129 +104 @@
 
 
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-
-}}}
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-{{{#!td style="vertical-align:top;width: 50px"
-
-}}}
-{{{#!td style="vertical-align:top;width: 50px"
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-}}}
-{{{#!td style="vertical-align:top;width: 75px"
-
-}}}
-{{{#!td style="vertical-align:top"
-
-}}}
-{{{#!td style="vertical-align:top"
-C
-}}}
-{{{#!td style="vertical-align:top"
+Bottom BC:
+
+Removed mirror boundary conditions for u and v at the bottom in case of
+ibc_uv_b == 0. Instead, dirichlet boundary conditions (u=v=0) are set
+in init_3d_model. (boundary_conds)
+
+dzu_mg has to be set explicitly for a equally spaced grid near bottom.
+ddzu_pres added to use a equally spaced grid near bottom. 
+In case of dirichlet boundary condition at the bottom zu(0)=0.0. (init_grid)
+
+Call of SOR routine is referenced with ddzu_pres. (pres)
+
+Turbulent inflow:
+
+Using nbgp recycling planes for a better resolution of the turbulent flow near
+the inflow. (inflow_turbulence)
+
+}}}
+|----------------
+{{{#!td style="vertical-align:top;width: 50px"
+
+}}}
+{{{#!td style="vertical-align:top;width: 50px"
+
+}}}
+{{{#!td style="vertical-align:top;width: 75px"
+
+}}}
+{{{#!td style="vertical-align:top"
+
+}}}
+{{{#!td style="vertical-align:top"
+C
+}}}
+{{{#!td style="vertical-align:top"
+
+Advection scheme:
+
+The maximum_grid_level changed from 1 to 0. 0 is the normal grid, 1 to 
+maximum_grid_level the grids for multigrid, in which 0 and 1 are normal grids.
+This distinction is due to reasons of data exchange and performance for the 
+normal grid and grids in poismg.
+The definition of MPI-Vectors adapted to a dynamic number of ghost points.
+New MPI-Vectors for data exchange between left and right boundaries added. 
+This is due to reasons of performance (10% faster). (init_pegrid)
+
+Dynamic exchange of ghost points with nbgp_local to ensure that no useless 
+ghost points exchanged in case of multigrid. type_yz(0) and type_xz(0) used for
+normal grid, the remaining types used for the several grid levels. 
+Exchange is done via MPI-Vectors with a dynamic value of ghost points which 
+depend on the advection scheme. Exchange of left and right PEs is 10% faster
+with MPI-Vectors than without. (exchange_horiz, exchange_horiz_2d)
+
+Calls of exchange_horiz modified. (advec_particles, data_output_2d, 
+data_output_3d, data_output_mask, diffusivities, init_3d_model, 
+init_pt_anomaly, init_rankine, poismg, sor, time_integration)
+
 Default of [../../app/inipar/#momentum_advec momentum_advec] and [../../app/inipar/#scalar_advec scalar_advec] changed to 'ws-scheme'. (modules)
 
@@ -159 +171 @@
 user_..., wall_fluxes)
 
-Calls of exchange_horiz modified. (advec_particles, data_output_2d, 
-data_output_3d, data_output_mask, diffusivities, init_3d_model, 
-init_pt_anomaly, init_rankine, poismg, sor, time_integration)
-
 Allocation of arrays, output of array bounds and skip values adapted to a 
 dynamic number of ghost points with nbgp. (check_open, data_output_3d,
 global_min_max, read_3d_binary, user_read_restart_data, write_compressed)
 
+Coupling:
+
+determination of target_id's moved to init_pegrid. (init_coupling)
+
+Changed surface boundary conditions for u and v in case of ibc_uv_b == 0 from
+mirror bc to dirichlet boundary conditions (u=v=0), so that k=nzb is
+representative for the height z0. (init_3d_model)
+
+Bottom BC:
+
 Changed surface boundary conditions for u and v from mirror bc to dirichelt bc,
 therefore u(uzb,:,:) and v(nzb,:,:) is now representative for the height z0. 
 (prandtl_fluxes)
 
-determination of target_id's moved to init_pegrid. (init_coupling)
+Other:
 
 Initial volume flow is now calculated by using the variable hom_sum.
 Therefore the correction of initial volume flow for non-flat topography
-removed (removed u_nzb_p1_for_vfc and v_nzb_p1_for_vfc)
-Changed surface boundary conditions for u and v in case of ibc_uv_b == 0 from
-mirror bc to dirichlet boundary conditions (u=v=0), so that k=nzb is
-representative for the height z0. (init_3d_model)
+removed (removed u_nzb_p1_for_vfc and v_nzb_p1_for_vfc) (init_3d_model)
+
+
+
+
 
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