1786 | | L |
1787 | | }}} |
1788 | | {{{#!td style="vertical-align:top" |
1789 | | .F. |
1790 | | }}} |
1791 | | {{{#!td |
1792 | | Parameter to switch on a y-shift for the recycled inflow turbulence.\\\\ |
1793 | | If '''recycling_yshift''' = .T., the recycled turbulence that is mapped from the recycling plane (see [#recycling_width recycling_width]) to the inflow boundary is shifted in y-direction. This parameter reduces persistent streaks that may occur within the recycling domain. The distance of the y-shift is INT([../d3par#npey npey] / 2), which is in most cases the best distance for effectively reducing streaks in the recycling domain. |
1794 | | |
1795 | | Note that '''recycling_yshift''' = .T. requires [#turbulent_inflow turbulent_inflow] = .T.. |
| 1786 | I |
| 1787 | }}} |
| 1788 | {{{#!td style="vertical-align:top" |
| 1789 | 0 |
| 1790 | }}} |
| 1791 | {{{#!td |
| 1792 | Parameter to define a y-shift for the recycled inflow turbulence, given in multiples of PE (may also be negative).\\\\ |
| 1793 | E.g. with recycling_yshift = 3 the turbulent fluctuations, obtained at the recycling plane, will be shifted by 3 processors in positive y-direction before being imposed on the inflow. This method can be used to avoid persistent streaks in the longitudinal wind component, that may form in a neutrally stratified boundary layer (detailed information about this method can be found in Munters 2016). |
| 1794 | |
| 1795 | Note that '''recycling_yshift''' \= 0 requires [#turbulent_inflow turbulent_inflow] = .T.. |