| | 120 | }}} |
| | 121 | |---------------- |
| | 122 | {{{#!td style="vertical-align:top" |
| | 123 | [=#coupling_start_time '''coupling_start_time'''] |
| | 124 | }}} |
| | 125 | {{{#!td style="vertical-align:top" |
| | 126 | R |
| | 127 | }}} |
| | 128 | {{{#!td style="vertical-align:top" |
| | 129 | 0.0 |
| | 130 | }}} |
| | 131 | {{{#!td |
| | 132 | Simulation time of precursor run.\\\\ |
| | 133 | Sets the time period a precursor run shall run uncoupled. This parameter is used to set up the precursor run control for atmosphere-ocean-coupled runs. It has to be set individually to the atmospheric / oceanic precursor run. The time in the data output will show negative values during the precursor run. See documentation for further information. |
| | 134 | }}} |
| | 135 | |---------------- |
| | 136 | {{{#!td style="vertical-align:top" |
| | 137 | [=#<insert_parameter_name> '''<insert_parameter_name>'''] |
| | 138 | }}} |
| | 139 | {{{#!td style="vertical-align:top" |
| | 140 | <insert type> |
| | 141 | }}} |
| | 142 | {{{#!td style="vertical-align:top" |
| | 143 | <insert value> |
| | 144 | }}} |
| | 145 | {{{#!td |
| | 146 | <insert explanation> |
| | 147 | }}} |
| | 148 | |---------------- |
| | 149 | {{{#!td style="vertical-align:top" |
| | 150 | [=#<insert_parameter_name> '''<insert_parameter_name>'''] |
| | 151 | }}} |
| | 152 | {{{#!td style="vertical-align:top" |
| | 153 | <insert type> |
| | 154 | }}} |
| | 155 | {{{#!td style="vertical-align:top" |
| | 156 | <insert value> |
| | 157 | }}} |
| | 158 | {{{#!td |
| | 159 | <insert explanation> |
| | 160 | }}} |
| | 161 | |---------------- |
| | 162 | {{{#!td style="vertical-align:top" |
| | 163 | [=#<insert_parameter_name> '''<insert_parameter_name>'''] |
| | 164 | }}} |
| | 165 | {{{#!td style="vertical-align:top" |
| | 166 | <insert type> |
| | 167 | }}} |
| | 168 | {{{#!td style="vertical-align:top" |
| | 169 | <insert value> |
| | 170 | }}} |
| | 171 | {{{#!td |
| | 172 | <insert explanation> |
| 742 | | [=#<insert_parameter_name> '''<insert_parameter_name>'''] |
| 743 | | }}} |
| 744 | | {{{#!td style="vertical-align:top" |
| 745 | | <insert type> |
| 746 | | }}} |
| 747 | | {{{#!td style="vertical-align:top" |
| 748 | | <insert value> |
| 749 | | }}} |
| 750 | | {{{#!td |
| 751 | | <insert explanation> |
| | 795 | [=#cthf '''cthf'''] |
| | 796 | }}} |
| | 797 | {{{#!td style="vertical-align:top" |
| | 798 | R |
| | 799 | }}} |
| | 800 | {{{#!td style="vertical-align:top" |
| | 801 | 0.0 |
| | 802 | }}} |
| | 803 | {{{#!td |
| | 804 | Average heat flux that is prescribed at the top of the plant canopy.\\\\ |
| | 805 | If [#plant_canopy plant_canopy] is set ''.T.'', the user can prescribe a heat flux at the top of the plant canopy. |
| | 806 | It is assumed that solar radiation penetrates the canopy and warms the foliage which, in turn, warms the air in contact with it. |
| | 807 | '''Note:''' Instead of using the value prescribed by [#surface_heatflux surface_heatflux], the near surface heat flux is determined from an exponential function that is dependent on the cumulative leaf_area_index (Shaw and Schumann (1992, Boundary Layer Meteorol., '''61''', 47-64)). |