Observations of surface-gravity-wave scattering and dissipation by an isolated shoal related to a cuspate foreland

Author:

Paniagua-Arroyave Juan F.,Adams Peter N.,Parra Sabrina M.,Valle-Levinson Arnoldo

Funder

U.S. Department of the Interior

Bureau of Ocean Energy Management

Environmental Studies Program

Fulbright Commission

U.S. Department of State

Ministry of Education of Colombia

University of Florida College of Liberal Arts and Sciences and Department of Geological Sciences

EAFIT University

American Society for Engineering Education

Naval Research Laboratory Postdoctoral Fellow Program

Publisher

Elsevier BV

Subject

Geology,Aquatic Science,Oceanography

Reference95 articles.

1. Infragravity wave contribution to surf zone sediment transport - the role of advection;Aagaard;Mar. Geol.,2008

2. Sediment transport and beach profile evolution induced by bi-chromatic wave groups with different group periods;Alsina;Coast. Eng.,2016

3. High-angle wave instability and emergent shoreline shapes: 1. Modeling of sand waves, flying spits, and capes;Ashton;J. Geophys. Res.,2006

4. Nonlinear infragravity-wave interactions on a gently sloping laboratory beach;de Bakker;J. Phys. Oceanogr.,2015

5. Beach steepness effects on nonlinear infragravity-wave interactions: a numerical study;de Bakker;J. Geophys. Res.,2016

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