Movie:Modelling subglacial drainage coupled to ice flow in Greenland: Difference between revisions

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{{Attribute movie1
{{Attribute movie1
|Movie domain = terrestrial, hydrology
|Movie domain=terrestrial, hydrology
}}
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{{Attribute movie3
{{Attribute movie3
|Animation model name =
|First name contributor=Mauro
|First name contributor=Mauro
|Last name contributor =Werder
|Last name contributor=Werder
|Location movie=Southwest Greenland
|Location movie=Southwest Greenland
|Timespan movie=Seasonal
|Timespan movie=Seasonal
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{{Movie description
{{Movie description
|Grade level=Under graduate (13-16), Graduate / Professional
|Grade level=Under graduate (13-16), Graduate / Professional
|One-line movie description = Modeled subglacial drainage of the Greenland Ice Sheet
|One-line movie description=Modeled subglacial drainage of the Greenland Ice Sheet
|Extended movie description=The animation shows the modeled evolution of the subglacial drainage system and associated ice sliding speed for a catchment south of Jakobshavn Isbræ (Greenland) in 2011. The left panel shows contours of the hydraulic potential and the network of channels; the right panel shows the sliding speed and channels; and the bottom panel shows the meltwater forcing.
|Extended movie description=The animation shows the modeled evolution of the subglacial drainage system and associated ice sliding speed for a catchment south of Jakobshavn Isbræ (Greenland) in 2011. The left panel shows contours of the hydraulic potential and the network of channels; the right panel shows the sliding speed and channels; and the bottom panel shows the meltwater forcing.
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Revision as of 16:27, 21 June 2017

Information Page: Modelling subglacial drainage coupled to ice flow in Greenland

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Key Attributes

Domain: terrestrial, hydrology
Model name: Animation model name
Name: Mauro, Werder
Where: Southwest Greenland
When: Seasonal


Short Description

Grade level: Under graduate (13-16), Graduate / Professional

Statement: Modeled subglacial drainage of the Greenland Ice Sheet

Abstract: The animation shows the modeled evolution of the subglacial drainage system and associated ice sliding speed for a catchment south of Jakobshavn Isbræ (Greenland) in 2011. The left panel shows contours of the hydraulic potential and the network of channels; the right panel shows the sliding speed and channels; and the bottom panel shows the meltwater forcing.

Theory

Liquid water is thought to move through the Greenland Ice Sheet as diffuse and channelized flow, and is governed by the pressure field created by the weight of overlying ice. This 2-D model combines the governing equations for both types of flow to model the movement of water in the Greenland Ice Sheet.

A video of the talk Mauro Werder gave at the CSDMS 2013 annual meeting is available on the CSDMS website, http://csdms.colorado.edu/wiki/CSDMS_2013_annual_meeting_Mauro_Werder

Links

http://www.sfu.ca/~mawerder/


References



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