Terrestrial Mo: Difference between revisions
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| class="model_col1"| Description: | | class="model_col1"| Description: | ||
| class="model_col2" colspan="2"| The Hydrologically Enhanced Basin Evolution Model (HEBEM) is a combined hydrologic/geomorphic model. The hydrologic model simulates precipitation with variability, infiltration, evapotranspiration, overland flow, and groundwater flow, thus producing a spatially and temporally varying water discharge Q that drives fluvial processes in the land surface. The geomorphic model accounts for tectonic forcing, hillslope processes, erosion, and sediment transport. The combined model uses multiple time steps for hydrologic and geomorphic processes. Due to its hydrologic represenation, the model is able to investigate the interaction between hydrology and geomorpholgy. | | class="model_col2" colspan="2"| The Hydrologically Enhanced Basin Evolution Model (HEBEM) is a combined hydrologic/geomorphic model. The hydrologic model simulates precipitation with variability, infiltration, evapotranspiration, overland flow, and groundwater flow, thus producing a spatially and temporally varying water discharge Q that drives fluvial processes in the land surface. The geomorphic model accounts for tectonic forcing, hillslope processes, erosion, and sediment transport. The combined model uses multiple time steps for hydrologic and geomorphic processes. Due to its hydrologic represenation, the model is able to investigate the interaction between hydrology and geomorpholgy. | ||
|- | |||
| class="model_section_header" colspan="3" | Technical information | |||
|- | |||
| class="model_col1"| Supported platforms: | |||
| class="model_col2" colspan="2"| Unix | |||
|- | |||
| class="model_col1"| Programming language: | |||
| class="model_col2" colspan="2"| Fortran77, Fortran90, C | |||
|- | |||
| class="model_col1"| Model was developed started from: | |||
| class="model_col2" colspan="2"| 2001 and development still takes place | |||
|- | |||
| class="model_col1"| To what degree will the model become available: | |||
| class="model_col2" colspan="2"| Not | |||
|- | |||
| class="model_col1"| Current license type: | |||
| class="model_col2" colspan="2"| -- | |||
|- | |||
| class="model_col1"| Memory requirements: | |||
| class="model_col2" colspan="2"| | |||
|- | |||
| class="model_col1"| Typical run time: | |||
| class="model_col2" colspan="2"| | |||
|- | |||
| class="model_section_header" colspan="3" | Input / Output description | |||
|- | |||
| class="model_col1"| Input parameters: | |||
| class="model_col2" colspan="2"| -- | |||
|- | |||
| class="model_col1"| Input format: | |||
| class="model_col2" colspan="2"| | |||
|- | |||
| class="model_col1"| Output parameters: | |||
| class="model_col2" colspan="2"| -- | |||
|- | |||
| class="model_col1"| Output format: | |||
| class="model_col2" colspan="2"| | |||
|- | |||
| class="model_col1"| Description of post-processing software (if needed): | |||
| class="model_col2" colspan="2"| | |||
|- | |||
| class="model_col1"| Description of visualization software (if needed): | |||
| class="model_col2" colspan="2"| | |||
|- | |||
|} | |} | ||
|} | |} | ||
Revision as of 14:54, 18 February 2008
| Model | Contact Person | Discussion Page |
|---|
| AquaTellus | Irina Overeem | Not yet |
|---|---|---|
| Contact information | ||
| Institute: | CSDMS, INSTAAR, University of Colorado | |
| City: | Boulder, CO | |
| Country: | USA | |
| Email: | irina.overeem@colorado.edu | |
| Caesar | Tom Coulthard | Not yet |
|---|---|---|
| Contact information | ||
| Institute: | University of Hull | |
| City: | Hull | |
| Country: | UK | |
| Email: | T.Coulthard@hull.ac.uk | |
| HEBEM | Jeffrey Niemann | Not yet |
|---|---|---|
| Contact information | ||
| Institute: | Colorado State University | |
| City: | Fort Collins, CO | |
| Country: | USA | |
| Email: | jniemann@engr.colostate.edu | |
| Model description | ||
| Model type: | Single model | |
| Description: | The Hydrologically Enhanced Basin Evolution Model (HEBEM) is a combined hydrologic/geomorphic model. The hydrologic model simulates precipitation with variability, infiltration, evapotranspiration, overland flow, and groundwater flow, thus producing a spatially and temporally varying water discharge Q that drives fluvial processes in the land surface. The geomorphic model accounts for tectonic forcing, hillslope processes, erosion, and sediment transport. The combined model uses multiple time steps for hydrologic and geomorphic processes. Due to its hydrologic represenation, the model is able to investigate the interaction between hydrology and geomorpholgy. | |
| Technical information | ||
| Supported platforms: | Unix | |
| Programming language: | Fortran77, Fortran90, C | |
| Model was developed started from: | 2001 and development still takes place | |
| To what degree will the model become available: | Not | |
| Current license type: | -- | |
| Memory requirements: | ||
| Typical run time: | ||
| Input / Output description | ||
| Input parameters: | -- | |
| Input format: | ||
| Output parameters: | -- | |
| Output format: | ||
| Description of post-processing software (if needed): | ||
| Description of visualization software (if needed): | ||
