| 52 | }}} |
| 53 | |---------------- |
| 54 | {{{#!td style="vertical-align:top" |
| 55 | [=#cloud_scheme '''cloud_scheme'''] |
| 56 | }}} |
| 57 | {{{#!td style="vertical-align:top" |
| 58 | C*20 |
| 59 | }}} |
| 60 | {{{#!td style="vertical-align:top" |
| 61 | '' 'seifert_beheng' '' |
| 62 | }}} |
| 63 | {{{#!td |
| 64 | Parameter to choose the cloud microphysics scheme.\\\\ |
| 65 | The following values are allowed:\\\\ |
| 66 | '' 'seifert_beheng' ''\\\\ |
| 67 | Cloud microphysics according to Seifert and Beheng (2006). \\\\ |
| 68 | '' 'kessler' ''\\\\ |
| 69 | Cloud microphysics according to Kessler (1969).\\\\ |
| 70 | Both schemes are based on a 0%-100%-scheme to diagnose the cloud water content and differ in the precipitation process. Therefore, it is not allowed to choose [#cloud_scheme cloud_scheme] = 'seifert_beheng' if precipitation is not allowed ([#precipitation precipitation] = .F.) in order to save computational resources. |
| 2654 | {{{#!td style="vertical-align:top;width: 150px" |
| 2655 | [=#drizzle '''drizzle'''] |
| 2656 | }}} |
| 2657 | {{{#!td style="vertical-align:top;width: 50px" |
| 2658 | L |
| 2659 | }}} |
| 2660 | {{{#!td style="vertical-align:top;width: 75px" |
| 2661 | .T. |
| 2662 | }}} |
| 2663 | {{{#!td |
| 2664 | Parameter to consider drizzle according to Heus et al. (2010). |
| 2665 | |
| 2666 | This parameter only comes into effect if the microphysical cloud scheme according to Seifert and Beheng (2006) is used ([#cloud_scheme cloud_scheme] = 'seifert_beheng'). |
| 2667 | }}} |
| 2668 | |---------------- |
| 2669 | {{{#!td style="vertical-align:top;width: 150px" |
| 2670 | [=#mu_constant '''mu_constant'''] |
| 2671 | }}} |
| 2672 | {{{#!td style="vertical-align:top;width: 50px" |
| 2673 | L |
| 2674 | }}} |
| 2675 | {{{#!td style="vertical-align:top;width: 75px" |
| 2676 | .F. |
| 2677 | }}} |
| 2678 | {{{#!td |
| 2679 | Parameter to set the shape parameter of the gamma distribution to a constant value given by [#mu_constant_value mu_constant_value]. Otherwise the shape parameter will be parameterized (Milbrandt and Yau, 2005; Stevens and Seifert, 2008). |
| 2680 | |
| 2681 | This parameter only comes into effect if the microphysical cloud scheme according to Seifert and Beheng (2006) is used ([#cloud_scheme cloud_scheme] = 'seifert_beheng'). |
| 2682 | }}} |
| 2683 | |---------------- |
| 2684 | {{{#!td style="vertical-align:top;width: 150px" |
| 2685 | [=#mu_constant_value '''mu_constant_value'''] |
| 2686 | }}} |
| 2687 | {{{#!td style="vertical-align:top;width: 50px" |
| 2688 | R |
| 2689 | }}} |
| 2690 | {{{#!td style="vertical-align:top;width: 75px" |
| 2691 | 0.0 |
| 2692 | }}} |
| 2693 | {{{#!td |
| 2694 | Value of constant shape parameter of the gamma distribution. This parameter only comes into effect if [#mu_constant mu_constant] = .T.. |
| 2695 | |
| 2696 | This parameter only comes into effect if the microphysical cloud scheme according to Seifert and Beheng (2006) is used ([#cloud_scheme cloud_scheme] = 'seifert_beheng'). |
| 2697 | }}} |
| 2698 | |---------------- |
| 2699 | {{{#!td style="vertical-align:top;width: 150px" |
| 2700 | [=#ventilation_effect '''ventilation_effect'''] |
| 2701 | }}} |
| 2702 | {{{#!td style="vertical-align:top;width: 50px" |
| 2703 | L |
| 2704 | }}} |
| 2705 | {{{#!td style="vertical-align:top;width: 75px" |
| 2706 | .F. |
| 2707 | }}} |
| 2708 | {{{#!td |
| 2709 | Parameter to consider the ventilation effect on evaporation of rain drops according to Seifert (2008). |
| 2710 | |
| 2711 | This parameter only comes into effect if the microphysical cloud scheme according to Seifert and Beheng (2006) is used ([#cloud_scheme cloud_scheme] = 'seifert_beheng'). |
| 2712 | }}} |
| 2713 | |---------------- |