Model:SedPlume: Difference between revisions
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|Phone=44 1223-336574 | |Phone=44 1223-336574 | ||
|Fax=44 1223-336549 | |Fax=44 1223-336549 | ||
|Provide key papers on model if any=Mugford, R.I.; Dowdeswell, J.A. SedBerg and SedPlume Models: Simulating Sediment Delivery from Tidewater Glaciers to the Marine Environment. American Geophysical Union. 12/2009. | |||
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{{Model identity | {{Model identity | ||
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|One-line model description=SedPlume simulates glacial meltwater plume dynamics and sedimentation. | |One-line model description=SedPlume simulates glacial meltwater plume dynamics and sedimentation. | ||
|Extended model description=SedPlume is an integral model, solving the conservation equations of volume, momentum, buoyancy and sediment flux along the path of a turbulent plume injected into stably stratified ambient fluid. Sedimentation occurs from the plume when the radial component of the sediment fall velocity exceeds the entrainment velocity. When the plume reaches the surface, it is treated as a radially spreading surface gravity current, for which exact solutions exist for the sediment deposition rate. Flocculation of silt and clay particles is modeled using empirical measurements of particle settling velocities in fjords to adjust the settling velocity of fine-grained sediments. | |Extended model description=SedPlume is an integral model, solving the conservation equations of volume, momentum, buoyancy and sediment flux along the path of a turbulent plume injected into stably stratified ambient fluid. Sedimentation occurs from the plume when the radial component of the sediment fall velocity exceeds the entrainment velocity. When the plume reaches the surface, it is treated as a radially spreading surface gravity current, for which exact solutions exist for the sediment deposition rate. Flocculation of silt and clay particles is modeled using empirical measurements of particle settling velocities in fjords to adjust the settling velocity of fine-grained sediments. | ||
|Provide key papers on model if any=Mugford, R.I.; Dowdeswell, J.A. SedBerg and SedPlume Models: Simulating Sediment Delivery from Tidewater Glaciers to the Marine Environment. American Geophysical Union. 12/2009. | |||
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{{Model technical information | {{Model technical information | ||
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|Does model development still take place?=Yes | |Does model development still take place?=Yes | ||
|Model availability=As code | |Model availability=As code | ||
|Source code availability=Through | |Source code availability=Through owner | ||
|Program license type=Other | |Program license type=Other | ||
|Program license type other=Licence needs to be changes, see box above | |Program license type other=Licence needs to be changes, see box above | ||
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|Memory requirements=-- | |Memory requirements=-- | ||
|Typical run time=-- | |Typical run time=-- | ||
|Provide key papers on model if any=Mugford, R.I.; Dowdeswell, J.A. SedBerg and SedPlume Models: Simulating Sediment Delivery from Tidewater Glaciers to the Marine Environment. American Geophysical Union. 12/2009. | |||
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{{Input - Output description | {{Input - Output description | ||
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|Post-processing software needed?=No | |Post-processing software needed?=No | ||
|Visualization software needed?=No | |Visualization software needed?=No | ||
|Provide key papers on model if any=Mugford, R.I.; Dowdeswell, J.A. SedBerg and SedPlume Models: Simulating Sediment Delivery from Tidewater Glaciers to the Marine Environment. American Geophysical Union. 12/2009. | |||
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{{Process description model|Provide key papers on model if any=Mugford, R.I.; Dowdeswell, J.A. SedBerg and SedPlume Models: Simulating Sediment Delivery from Tidewater Glaciers to the Marine Environment. American Geophysical Union. 12/2009. | |||
}} | |||
{{Model testing|Provide key papers on model if any=Mugford, R.I.; Dowdeswell, J.A. SedBerg and SedPlume Models: Simulating Sediment Delivery from Tidewater Glaciers to the Marine Environment. American Geophysical Union. 12/2009. | |||
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{{Users groups model|Provide key papers on model if any=Mugford, R.I.; Dowdeswell, J.A. SedBerg and SedPlume Models: Simulating Sediment Delivery from Tidewater Glaciers to the Marine Environment. American Geophysical Union. 12/2009. | |||
}} | }} | ||
{{Documentation model | {{Documentation model | ||
|Manual model available=No | |||
|Provide key papers on model if any=Mugford, R.I.; Dowdeswell, J.A. SedBerg and SedPlume Models: Simulating Sediment Delivery from Tidewater Glaciers to the Marine Environment. American Geophysical Union. 12/2009. | |Provide key papers on model if any=Mugford, R.I.; Dowdeswell, J.A. SedBerg and SedPlume Models: Simulating Sediment Delivery from Tidewater Glaciers to the Marine Environment. American Geophysical Union. 12/2009. | ||
}} | }} | ||
{{Additional comments model}} | {{Additional comments model|Provide key papers on model if any=Mugford, R.I.; Dowdeswell, J.A. SedBerg and SedPlume Models: Simulating Sediment Delivery from Tidewater Glaciers to the Marine Environment. American Geophysical Union. 12/2009. | ||
}} | |||
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==Introduction== | ==Introduction== |
Revision as of 11:57, 22 February 2011
Contact
Name | Ruth Mugford |
Type of contact | Model developer |
Institute / Organization | University of Cambridge |
Postal address 1 | Lensfield Road |
Postal address 2 | |
Town / City | Cambridge |
Postal code | CB2 1 ER |
State | NO STATE |
Country | UK"UK" is not in the list (Afghanistan, Albania, Algeria, Andorra, Angola, Antigua and Barbuda, Argentina, Armenia, Australia, Austria, ...) of allowed values for the "Country" property. |
Email address | rm423@cam.ac.uk |
Phone | 44 1223-336574 |
Fax | 44 1223-336549 |
SedPlume
Metadata
Summary
Technical specs
In/Output
Process
Testing
Other
IntroductionSedPlume simulates glacial meltwater plume dynamics and sedimentation. SedPlume is an integral model, solving the conservation equations of volume, momentum, buoyancy and sediment flux along the path of a turbulent plume injected into stably stratified ambient fluid. Sedimentation occurs from the plume when the radial component of the sediment fall velocity exceeds the entrainment velocity. When the plume reaches the surface, it is treated as a radially spreading surface gravity current, for which exact solutions exist for the sediment deposition rate. Flocculation of silt and clay particles is modeled using empirical measurements of particle settling velocities in fjords to adjust the settling velocity of fine-grained sediments. HistoryThis model was developed by Ruth Mugford during her PhD work at Scott Polar Research Institute, University of Cambridge from 2004-2008. It is supplied "as is", so it may require some tweeking to get it running on your system. Feel free to contact Ruth if you are planning on using the model it as she is still working on it. PapersIssuesHelpInput FilesOutput FilesDownloadSource |