Movie:An Alpine Glacier's Drainage System: Gornergletscher drainage system: Difference between revisions
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|First name contributor=Mauro | |First name contributor=Mauro | ||
|Last name contributor =Werder | |Last name contributor=Werder | ||
|Location movie=Gornergletscher, Switzerland | |Location movie=Gornergletscher, Switzerland | ||
|Timespan movie=One Season | |Timespan movie=One Season | ||
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|Theory movie=Liquid water is thought to move through alpine glaciers 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 the Gornergletscher, an alpine glacier in Switzerland. | |Theory movie=Liquid water is thought to move through alpine glaciers 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 the Gornergletscher, an alpine glacier in Switzerland. | ||
A video of the talk Mauro Werder gave at the CSDMS 2013 annual meeting on glacial hydrology is available on the CSDMS website, | A video of the talk Mauro Werder gave at the CSDMS 2013 annual meeting on glacial hydrology is available on the CSDMS website, https://csdms.colorado.edu/wiki/CSDMS_2013_annual_meeting_Mauro_Werder | ||
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{{Movie references2 | {{Movie references2 |
Latest revision as of 17:17, 19 February 2018
Information Page: An Alpine Glacier's Drainage System: Gornergletscher drainage system
Play Movie
Key Attributes
Domain: | terrestrial, hydrology |
Model name: | Animation model name |
Name: | Mauro, Werder |
Where: | Gornergletscher, Switzerland |
When: | One Season |
Short Description
Grade level: Under graduate (13-16), Graduate / Professional
Statement: Liquid water routing in an alpine glacier
Abstract: Subglacial discharge simulated for Gornergletscher: arrows depict discharge in the distributed system, blue shows discharge in channels.
Theory
Liquid water is thought to move through alpine glaciers 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 the Gornergletscher, an alpine glacier in Switzerland.
A video of the talk Mauro Werder gave at the CSDMS 2013 annual meeting on glacial hydrology is available on the CSDMS website, https://csdms.colorado.edu/wiki/CSDMS_2013_annual_meeting_Mauro_Werder
Links
References
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