Movie:A simulation of river bedforms: Difference between revisions

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(Created page with "{{Upload movie |Movie type=Movie |Upload movie=A8A2EGT6a2w |Upload image movie=Screen shot 2013-09-03 at 11.05.09 AM.png }} {{Attribute movie1 |Movie domain=hydrology }} {{Att...")
 
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{{Attribute movie3
{{Attribute movie3
|Animation model name=
|Animation model name=
|First name contributor=Mohammed  
|First name contributor=Mohammed
|Last name contributor=Nabi
|Last name contributor=Nabi
|Location movie=at the bottom of a river
|Location movie=at the bottom of a river
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|Grade level=Under graduate (13-16), Graduate / Professional
|Grade level=Under graduate (13-16), Graduate / Professional
|One-line movie description=Bedforms moving at the bottom of a river
|One-line movie description=Bedforms moving at the bottom of a river
|Extended movie description=Simulation of river bedform by large eddy simulation (LES), and sediment as spherical particles. Related papers are:
|Extended movie description=Simulation of river bedform by large eddy simulation (LES), and sediment as spherical particles.  
 
 
Related papers are:
doi: 10.1002/wrcr.20457
doi: 10.1002/wrcr.20457
doi: 10.1002/wrcr.20303
doi: 10.1002/wrcr.20303
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{{Movie theory2
{{Movie theory2
|Theory movie=The flow of water in rivers over loose sediments can lead to self organizing patterns, such as the ripples presented in this simulation.  
|Theory movie=The flow of water in rivers over loose sediments can lead to self organizing patterns, such as the ripples presented in this simulation.  
Generally, as the strength of the flow of water increases, low-flow bed forms evolve from a flat surface, to ripples, and then dunes. As higher flows occur, anti-dunes and eventually pools and chutes form.


For more information see the related papers:  
For more information see the related papers:  

Revision as of 11:22, 3 September 2013

Information Page: A simulation of river bedforms

Play Movie




Key Attributes

Domain: hydrology
Model name:
Name: Mohammed, Nabi
Where: at the bottom of a river
When: months


Short Description

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

Statement: Bedforms moving at the bottom of a river

Abstract: Simulation of river bedform by large eddy simulation (LES), and sediment as spherical particles.


Related papers are: doi: 10.1002/wrcr.20457 doi: 10.1002/wrcr.20303 doi: 10.1029/2012WR011911

Theory

The flow of water in rivers over loose sediments can lead to self organizing patterns, such as the ripples presented in this simulation.

Generally, as the strength of the flow of water increases, low-flow bed forms evolve from a flat surface, to ripples, and then dunes. As higher flows occur, anti-dunes and eventually pools and chutes form.

For more information see the related papers:

doi: 10.1002/wrcr.20457 doi: 10.1002/wrcr.20303 doi: 10.1029/2012WR011911

Links

http://ws3-er.eng.hokudai.ac.jp/dpr/dpr eng/?page id=455


References



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