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| 19 | {{{#!td style="vertical-align:top;width: 50px" |
| 20 | 15/06/17 |
| 21 | }}} |
| 22 | {{{#!td style="vertical-align:top;width: 50px" |
| 23 | JS |
| 24 | }}} |
| 25 | {{{#!td style="vertical-align:top;width: 75px" |
| 26 | r2292 |
| 27 | }}} |
| 28 | {{{#!td style="vertical-align:top" |
| 29 | 4.0 |
| 30 | }}} |
| 31 | {{{#!td style="vertical-align:top" |
| 32 | N |
| 33 | }}} |
| 34 | {{{#!td style="vertical-align:top" |
| 35 | Implementation of new microphysic scheme: cloud_scheme = 'morrison' |
| 36 | includes two more prognostic equations for cloud drop concentration (nc) |
| 37 | and cloud water content (qc). |
| 38 | * The process of activation is parameterized with a simple Twomey |
| 39 | activion scheme or with considering solution and curvature |
| 40 | effects (Khvorostyanov and Curry ,2006). |
| 41 | * The saturation adjustment scheme is replaced by the parameterization |
| 42 | of condensation rates (Khairoutdinov and Kogan, 2000, Mon. Wea. Rev.,128). |
| 43 | * All other microphysical processes of Seifert and Beheng are used. |
| 44 | Additionally, in those processes the reduction of cloud number concentration |
| 45 | is considered. |
| 46 | (advec_s_bc, advec_ws, average_3d_data, boundary_conds, calc_liquid_water_content, check_parameters, data_output_2d, data_output_3d, data_output_mask, flow_statistics, init_3d_model, init_masks, microphysics_mod, modules, netcdf_interface_mod, palm, parin, pmc_interface_mod, prognostic_eqautions, read_3d_binary, sum_up_3d_data, surface_layer_fluxes_mod, surface_mod, swap_timelevel, time_integration, wrtie_3d_binary) |
| 47 | }}} |