Annualmeeting:2017 CSDMS meeting-054: Difference between revisions
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{{CSDMS meeting abstract template}} | |CSDMS meeting abstract title=Coupled Modeling of River and Coastal Processes: | ||
New Insights about Delta Morphodynamics, Avulsions, and Autogenic Sediment Flux Variability | |||
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|CSDMS meeting coauthor first name abstract=Katherine | |||
|CSDMS meeting coauthor last name abstract=Ratliff | |||
|CSDMS meeting coauthor institute / Organization=Duke Univ. | |||
|CSDMS meeting coauthor town-city=Durham | |||
|CSDMS meeting coauthor country=United States | |||
|State=North Carolina | |||
|CSDMS meeting coauthor email address=k.ratliff@duke.edu | |||
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|CSDMS meeting coauthor first name abstract=Eric | |||
|CSDMS meeting coauthor last name abstract=Hutton | |||
|CSDMS meeting coauthor institute / Organization=Univ. of Colorado | |||
|CSDMS meeting coauthor town-city=boulder | |||
|CSDMS meeting coauthor country=United States | |||
|State=Colorado | |||
|CSDMS meeting coauthor email address=huttone@colorado.edu | |||
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|CSDMS meeting abstract=Following pioneering modeling work examining the evolution of wave-influenced deltas (REF e.g. FAVORITE JAAP, ANDREW, LIVIU; ANDREW ET AL CSDMS PAPER), we coupled the River and Floodplain Evolution Model (RAFEM) to the Coastline Evolution Model (CEM). Results of a recent suite of model experiments (conducted using the CSDMS software stack and Dakota) lead to new insights: 1) The preferred location of avulsions (a distance from the river mouth scaling with the backwater length), previously observed in laboratory models and in the field, can arise for geometric reasons that are independent of those recently suggested (REF MIKE, VAMSI…). This alternative explanation applies when the river longitudinal profile tends to diffuse more rapidly than the floodplain longitudinal profile. 2) Although the timescale for avulsions is expected to increase with increasing wave influence (REF SWENSEN, JEROLMACK), we find that whether this is true or not depends on the angular wave distribution. When wave influence is strong and the angular mix of wave influences tends to smooth a nearly straight coastline (coastline diffusion), progradation is slowed and avulsions delayed. However if the angular wave distribution produces anti-diffusive coastline evolution, a strong wave influence still leads to cuspate delta shapes—but not to delayed avulsions. 3) Although increasing sea-level-rise rate is expected to cause more rapid avulsions, and does in laboratory deltas, we unexpectedly find that this is not true for river-dominated deltas in our model (or for anti-diffusive wave climates). The explanation, involving the role of sea-level-rise related transgression (or decreased progradation), raises potentially important questions about geometrical differences between laboratory deltas and natural deltas. 4) The magnitude and timescale of autogenic variability in sediment delivery rates at the river mouth depends on wave climate, sea-level-rise rate (for some wave climates), and on the amount of super elevation of the river channel (relative to the surrounding floodplain) required to trigger avulsions. | |||
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Revision as of 12:38, 9 March 2017
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=Coupled Modeling of River and Coastal Processes: New Insights about Delta Morphodynamics, Avulsions, and Autogenic Sediment Flux Variability=
[[Image:|300px|right|link=File:]]Following pioneering modeling work examining the evolution of wave-influenced deltas (REF e.g. FAVORITE JAAP, ANDREW, LIVIU; ANDREW ET AL CSDMS PAPER), we coupled the River and Floodplain Evolution Model (RAFEM) to the Coastline Evolution Model (CEM). Results of a recent suite of model experiments (conducted using the CSDMS software stack and Dakota) lead to new insights: 1) The preferred location of avulsions (a distance from the river mouth scaling with the backwater length), previously observed in laboratory models and in the field, can arise for geometric reasons that are independent of those recently suggested (REF MIKE, VAMSI…). This alternative explanation applies when the river longitudinal profile tends to diffuse more rapidly than the floodplain longitudinal profile. 2) Although the timescale for avulsions is expected to increase with increasing wave influence (REF SWENSEN, JEROLMACK), we find that whether this is true or not depends on the angular wave distribution. When wave influence is strong and the angular mix of wave influences tends to smooth a nearly straight coastline (coastline diffusion), progradation is slowed and avulsions delayed. However if the angular wave distribution produces anti-diffusive coastline evolution, a strong wave influence still leads to cuspate delta shapes—but not to delayed avulsions. 3) Although increasing sea-level-rise rate is expected to cause more rapid avulsions, and does in laboratory deltas, we unexpectedly find that this is not true for river-dominated deltas in our model (or for anti-diffusive wave climates). The explanation, involving the role of sea-level-rise related transgression (or decreased progradation), raises potentially important questions about geometrical differences between laboratory deltas and natural deltas. 4) The magnitude and timescale of autogenic variability in sediment delivery rates at the river mouth depends on wave climate, sea-level-rise rate (for some wave climates), and on the amount of super elevation of the river channel (relative to the surrounding floodplain) required to trigger avulsions.
