Journal
JOURNAL OF WATERWAY PORT COASTAL AND OCEAN ENGINEERING
Volume 137, Issue 2, Pages 95-106Publisher
ASCE-AMER SOC CIVIL ENGINEERS
DOI: 10.1061/(ASCE)WW.1943-5460.0000068
Keywords
Water depth; Surf zone; Remote sensing; Wave velocity; Breaking waves; Wave equations
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Funding
- U.S. National Geospatial-Intelligence Agency
- U.S. Geological Survey
- South Carolina Sea Grant
- National Oceanographic Partnership Program
- Korea Ocean Research and Development Institute (KORDI) [PE 98452, 98453]
- National Research Foundation of Korea (NRF) [M062003000101390]
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A process is described for computation of bathymetry in and near the surf zone, from spatially varying celerity and breakpoint location data. The procedure involves the use of three submodels: (1) a wave shoaling model (outside of the surf zone); (2) a wave breaking model (defining the offshore boundary of the surf zone); and (3) a wave dissipation model (inside the surf zone). Influence of wave amplitude on the wave dispersion relation and celerity is included. Output includes wave height and water depth throughout the domain. In the application described here, oblique digital video served as the initial data source, although the model could be applied to data derived from other sources. Results are compared with data recorded by in situ sensors and beach profile survey data acquired by traditional means. Results suggest that water depths can be computed within 15% normalized error (equally, less than 0.1 m in biased depth error) for in and near the surf zone characterized by high wave nonlinearity. DOI: 10.1061/(ASCE)WW.1943-5460.0000068. (c) 2011 American Society of Civil Engineers.
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