Movie:Tidal Network Evolution: Difference between revisions

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|Animation model name=D'Alpaos Model  
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|First name contributor=Andrea
|First name contributor=Andrea
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{{Movie references1
|Key papers on movie if any=D'Alpaos, A., S. Lanzoni, M. Marani, S. Fagherazzi, and A. Rinaldo (2005), Tidal network ontogeny: channel initiation and early development, Journal of Geophysical Research--Earth Surface, 110, F02001, doi:10.1029/2004JF000182.
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{{Movie references1
|Key papers on movie if any=D'Alpaos, A., S. Lanzoni, S. M. Mudd, and S. Fagherazzi (2006), Modeling the influence of hydroperiod and vegetation on the cross-sectional formation of tidal channels, Estuarine Coastal Shelf Science, 69, 311-324, doi:10.1016/j.ecss.2006.05.02.
}}
{{Movie references1
|Key papers on movie if any=D'Alpaos, A., S. Lanzoni, M. Marani, and A. Rinaldo (2007), Landscape evolution in tidal embayments: modelling the interplay of erosion, sedimentation, and vegetation dynamics, Journal of Geophysical Research- Earth Surface, 112, F01008, doi:10.1029/2006JF000537.
}}
{{Movie references1
|Key papers on movie if any=D'Alpaos, A., S. Lanzoni, M. Marani, A. Bonometto, G. Cecconi, and A. Rinaldo (2007), Spontaneous tidal network formation within a constructed salt marsh: observations and morphodynamic modelling, Geomorphology, 91, 186–197, doi: 10.1016/j.geomorph.2007.04.013
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{{Movie references2}}
{{Movie references2}}
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Latest revision as of 16:36, 21 June 2017

Information Page: Tidal Network Evolution

Play Animation


Delta Evolution



Key Attributes

Domain: coastal
Keywords: Tidal network
Model name: D'Alpaos Model
Name: Andrea, D'Alpaos
Where: --
When: --


Short Description

Grade level: Graduate / Professional

Statement: Progressive incision of tidal channel networks

Abstract: Progressive incision of tidal channel networks in a theoretical domain, which is assumed to be surrounded by channels. The initial outlet is set to be in the middl of the lower boundary, the two other inlets are determined by internal dynamics. The water surface gradients are driving erosion, and headward incision takes place as long as local shear stress due to tidal expansion exceeds a threshold stress.

Theory

Links

References



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