114 | | Instead of using the Morrison scheme as an extension of the Seifert Beheng scheme. The extension are used as a stand-alone scheme. Therefore, rain processes are neglected but explicit consideration of diffusional growth and activation with prognostic quantities of ''N'',,c,, and ''q'',,c,,. This scheme is computational inexpensive and appropiate for conditions where teh production of rain can be neglected (i.e. fog). |
| 114 | Instead of using the Morrison scheme as an extension of the Seifert Beheng scheme. The extension are used as a stand-alone scheme. Therefore, rain processes are neglected but explicit consideration of diffusional growth and activation with prognostic quantities of ''N'',,c,, and ''q'',,c,,. This scheme is computational inexpensive and appropriate for conditions where the production of rain can be neglected (i.e. fog). |
| 118 | }}} |
| 119 | |
| 120 | {{{#!td style="vertical-align:top; text-align:left" |
| 121 | '''Mixed phase microphysics''' |
| 122 | |
| 123 | Note, that at the mixed phase bulk microphysics is still under development but can already applied. However, instead of presribing it as an own scheme (as the others) it must be turned on as with ... and is implemented as an extension of the schemes of Seifert and Beheng (2006) and Morrison (2007). |
| 124 | At this state only processes for ice crystal are inclueded involving two further prognostic quantities: ice craystal number ''N'',,i,, and ice crystal mixing ratio ''q'',,i,,. |
| 125 | }}} |
| 126 | {{{#!td style="text-align:left;style=width: 50px" |
| 127 | [[Image(mixed_phase.png)]] |