Model:HEBEM: Difference between revisions

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{{Model identity
|Model type=Single
}}
{{Model identity2
|ModelDomain=Terrestrial
|Spatial dimensions=2D
|One-line model description=Hydrologically Enhanced Basin Evolution Model
|Extended 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 representation, the model is able to investigate the interaction between hydrology and geomorpholgy.
}}
{{Start model keyword table}}
{{Model keywords
|Model keywords=basin evolution
}}
{{Model keywords
|Model keywords=hydrological
}}
{{Model keywords
|Model keywords=geomorphologic
}}
{{End a table}}
{{Modeler information
{{Modeler information
|First name=Jeffrey
|First name=Jeffrey
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|Postal code=80523
|Postal code=80523
|State=Colorado
|State=Colorado
|Country=USA
|Country=United States
|Email address=jniemann@engr.colostate.edu
|Email address=jniemann@engr.colostate.edu
|Phone=970 491 3517
|Phone=970 491 3517
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|Additional first name=Xiangjiang
|Additional first name=Xiangjiang
|Additional last name=Huang
|Additional last name=Huang
}}
{{Model identity
|Model type=Single
|Spatial dimensions=2D
|One-line model description=Hydrologically Enhanced Basin Evolution Model
|Extended 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 representation, the model is able to investigate the interaction between hydrology and geomorpholgy.
}}
}}
{{Model technical information
{{Model technical information
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|Program license type=Other
|Program license type=Other
|Program license type other=--
|Program license type other=--
|OpenMI compliant=No but possible
|CCA component=No but possible
|IRF interface=No but possible
|Memory requirements=--
|Memory requirements=--
|Typical run time=--
|Typical run time=--
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}}
}}
{{Documentation model
{{Documentation model
|Provide key papers on model if any=Huang, X., and J. D. Niemann, How do streamflow generation mechanisms affect watershed hypsometry? Earth Surface Processes and Landforms, 2007, doi:10.1002/esp.1573 (currently published online).
|Provide key papers on model if any=Key Papers:
Huang, X., and J. D. Niemann, An evaluation of the geomorphically effective event for fluvial processes over long periods, Journal of Geophysical Research, 111, F03015, 2006, doi:10.1029/2006JF000477.
* '''Huang, X., and J. D. Niemann, 2007. How do streamflow generation mechanisms affect watershed hypsometry? Earth Surface Processes and Landforms. Doi: ([http://dx.doi.org/10.1002/esp.1573 10.1002/esp.1573]).'''
Huang, X., and J. D. Niemann, Modeling the potential impacts of groundwater hydrology on long-term drainage basin evolution, Earth Surface Processes and Landforms, 31(14), 1802-1823, 2006, doi:10.1002/esp.1369.
 
* '''Huang, X., and J. D. Niemann, 2006. An evaluation of the geomorphically effective event for fluvial processes over long periods, Journal of Geophysical Research, 111, F03015. Doi: ([http://dx.doi.org/10.1029/2006JF000477 10.1029/2006JF000477]).'''
 
* '''Huang, X., and J. D. Niemann, 2006. Modeling the potential impacts of groundwater hydrology on long-term drainage basin evolution, Earth Surface Processes and Landforms, 31(14), 1802-1823. Doi: ([http://dx.doi.org/10.1002/esp.1369 10.1002/esp.1369]).'''
|Manual model available=No
|Manual model available=No
}}
}}
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|Comments=None
|Comments=None
}}
}}
{{Infobox Model
{{CSDMS staff part
|model name              = HEBEM
|OpenMI compliant=No but possible
|developer                = '''Niemann''', Jeffrey
|CCA component=No but possible
|one-line-description    = Hydrologically Enhanced Basin Evolution Model 
|IRF interface=No but possible
|type                    = Model
|CMT component=No but possible
|source                  = [[image:Red1.png]]
}}
}}
{{Start coupled table}}
{{End a table}}
{{End headertab}}
{{{{PAGENAME}}_autokeywords}}
{{NOINDEX}}
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== History ==
== History ==


== Papers ==
== References  ==
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{{#ifexist:Template:{{PAGENAME}}-citation-indices|{{{{PAGENAME}}-citation-indices}}|}}<br>
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== Issues ==
== Issues ==


== Help ==
== Help ==
{{#ifexist:Model_help:{{PAGENAME}}|[[Model_help:{{PAGENAME}}]]|}}


== Input Files ==
== Input Files ==


== Output Files ==
== Output Files ==
== Download ==
== Source ==


[[Category:Source code not available]]
[[Category:Source code not available]]

Latest revision as of 20:19, 16 September 2020



HEBEM


Metadata

Also known as
Model type Single
Model part of larger framework
Note on status model
Date note status model
Spatial dimensions 2D
Spatial extent
Model domain Terrestrial
One-line model description Hydrologically Enhanced Basin Evolution Model
Extended 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 representation, the model is able to investigate the interaction between hydrology and geomorpholgy.
Keywords:

basin evolution, hydrological, geomorphologic,

Name Jeffrey Niemann
Type of contact Model developer
Institute / Organization Colorado State University
Postal address 1 Dept of Civil and Environmental Engineering
Postal address 2 Campus Delivery 1372
Town / City Fort Collins
Postal code 80523
State Colorado
Country United States
Email address jniemann@engr.colostate.edu
Phone 970 491 3517
Fax 970 491 7727


Name Xiangjiang Huang
Type of contact
Institute / Organization
Postal address 1
Postal address 2
Town / City
Postal code
State
Country
Email address
Phone
Fax


Supported platforms
Unix
Other platform
Programming language

Fortran77, Fortran90, C

Other program language
Code optimized
Multiple processors implemented
Nr of distributed processors
Nr of shared processors
Start year development 2001
Does model development still take place? Yes
If above answer is no, provide end year model development
Code development status
When did you indicate the 'code development status'?
Model availability
Source code availability
(Or provide future intension)
Source web address
Source csdms web address
Program license type Other
Program license type other --
Memory requirements --
Typical run time --


Describe input parameters A grid with initial elevation. Hydrologic time step and geomorphic time step

Hydrologic paramters: average rainfall intensity, rainall duration, interstorm period, infiltration capacity, porosity, hydraulic conductivity, aquifer depth, specific yield, PET

Geomorphic parameters: baselevel lowering rate, diffusivity for hillslope processes, weathering rate, parameters for erosion and sediment transport model

Input format ASCII
Other input format
Describe output parameters elevations of all nodes elevation changes of all nodes
Output format ASCII
Other output format
Pre-processing software needed? No
Describe pre-processing software
Post-processing software needed? No
Describe post-processing software
Visualization software needed? No
If above answer is yes
Other visualization software


Describe processes represented by the model Hydrologic processes:

Precipitation, infiltration, evapotranspiration, overland flow, saturation-excess runoff, groundwater flow

Geomorphic processes: Baselevel lowering, weathering, hillslope processes, erosion, sediment transport

Describe key physical parameters and equations Infiltration capacity, water balance equation

Hydraulic conductivity, 2-D Dupuit groundwater movement equation

Describe length scale and resolution constraints A grid with 100x100 cells, Typical cells with a resolution of 40x40m
Describe time scale and resolution constraints Time scale of 10,000 years. Typical time step is 3 hour
Describe any numerical limitations and issues N/A


Describe available calibration data sets The hydrologic model was calibrated using hydrologic measurements of WE-38 watershed in PA
Upload calibration data sets if available:
Describe available test data sets N/A
Upload test data sets if available:
Describe ideal data for testing N/A


Do you have current or future plans for collaborating with other researchers? None
Is there a manual available? No
Upload manual if available:
Model website if any
Model forum / discussion board
Comments None


This part will be filled out by CSDMS staff

OpenMI compliant No but possible
BMI compliant No but possible
WMT component No but possible
PyMT component
Is this a data component
Can be coupled with:
Model info
Authors
Jeffrey Niemann
Huang
Source code
Model citations
Nr. of publications: --
Total citations: 0
h-index: --"--" is not a number.
m-quotient: 0
QR-code

Link to this page
Other models by author

Template:HEBEM autokeywords


Introduction

History

References



Nr. of publications: --
Total citations: 0
h-index: --"--" is not a number.
m-quotient: 0


See more publications of HEBEM

Issues

Help

Input Files

Output Files

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