| 6 | | At first, the laminar scenario conditions from [wiki:Gryschka Gryschka M. et.al (2005)] are used to generate self organized roll convection via turbulent inflow according to Lund, T. et al. (1998). \\\\ |
| 7 | | In the second part, results of [wiki:Gryschka Gryschka M. et.al (2008)] are used for investigate the influence of ice inhomogeneities to so called forced rolls. Therefore the subjection of explicit ice gabs-variation to roll-reaching in flow direction will be studied. |
| | 6 | At first, the laminar scenario conditions from [../../publications#y2005 Gryschka M. et.al (2005)] are used to generate self organized roll convection via turbulent inflow according to Lund, T. et al. (1998). \\\\ |
| | 7 | In the second part, results of [../../publications#y2008 Gryschka M. et.al (2008)] are used for investigate the influence of ice inhomogeneities to so called forced rolls. Therefore the subjection of explicit ice gabs-variation to roll-reaching in flow direction will be studied. |
