| 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). |
| | 114 | Instead of using the Morrison scheme as an extension of the [#seifert2001 Seifert and Beheng (2001],[#seifert2006 2006)] 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). |
| 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,,. |
| | 123 | Note, that at the mixed phase bulk microphysics is still under development but can already applied. However, instead of prescribing 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 [#seifert2006 Seifert and Beheng (2006)] and [#morrison2007 Morrison et al. (2007)]. |
| | 124 | At this state only processes for ice crystal are included involving two further prognostic quantities: ice crystal number ''N'',,i,, and ice crystal mixing ratio ''q'',,i,,. |
