We present an experimental and theoretical study of whether a large displacement wave can lead to catastrophic erosional incision of a moraine damming a glacial lake. The laboratory experiments consist of reservoirs held by barriers of granular materials in a glass tank; the theoretical model combines the Saint-Venant equations of hydraulic engineering with an empirical prescription for erosion. The results of both the laboratory experiments and the numerical simulations indicate that a single wave is generally unable to break the dam, but a sufficiently large disturbance in an almost-filled reservoir creates a seiche that can repeatedly overtop the dam. In such a case, the combined effect of the multiple erosion events ultimately breaks the dam.

Dam breaking by wave-induced erosional incision

von Hardenberg J;Provenzale A;
2008

Abstract

We present an experimental and theoretical study of whether a large displacement wave can lead to catastrophic erosional incision of a moraine damming a glacial lake. The laboratory experiments consist of reservoirs held by barriers of granular materials in a glass tank; the theoretical model combines the Saint-Venant equations of hydraulic engineering with an empirical prescription for erosion. The results of both the laboratory experiments and the numerical simulations indicate that a single wave is generally unable to break the dam, but a sufficiently large disturbance in an almost-filled reservoir creates a seiche that can repeatedly overtop the dam. In such a case, the combined effect of the multiple erosion events ultimately breaks the dam.
2008
Istituto di Scienze dell'Atmosfera e del Clima - ISAC
erosional incision
glacial lakes
Saint-Venant
erosion
dams
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/20.500.14243/43878
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