Continental Shelf Wave Propagation in the Mid-Atlantic Bight: A General Dispersion Relation
The authors address the propagation of continental shelf waves in the Mid-Atlantic Bight. An analytical model of the bathymetry in the region is constructed by representing the continental shelf as a gently sloping bottom, which deepens linearly with offshore distance to the place where it meets the...
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Published in | Journal of physical oceanography Vol. 42; no. 4; pp. 558 - 568 |
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Main Authors | , , |
Format | Journal Article |
Language | English |
Published |
Boston, MA
American Meteorological Society
01.04.2012
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Subjects | |
Online Access | Get full text |
ISSN | 0022-3670 1520-0485 |
DOI | 10.1175/JPO-D-11-098.1 |
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Abstract | The authors address the propagation of continental shelf waves in the Mid-Atlantic Bight. An analytical model of the bathymetry in the region is constructed by representing the continental shelf as a gently sloping bottom, which deepens linearly with offshore distance to the place where it meets the continental slope. Seaward of that point, the bathymetry is modeled with an exponentially decaying function of distance. The linearized, barotropic equations of hydrostatic motion, subject to the long-wave approximation, yield separate shelf and slope solutions, which are matched at the shelf break to specify the eigenfunctions. The associated eigenvalues define the dispersion relations for each of the modes. Wavenumber–frequency pairs derived from NOAA sea surface height stations along the coast are plotted on the first-mode dispersion curve, and the agreement is good. The theory also shows good agreement with the wave data of D. P. Wang. |
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AbstractList | The authors address the propagation of continental shelf waves in the Mid-Atlantic Bight. An analytical model of the bathymetry in the region is constructed by representing the continental shelf as a gently sloping bottom, which deepens linearly with offshore distance to the place where it meets the continental slope. Seaward of that point, the bathymetry is modeled with an exponentially decaying function of distance. The linearized, barotropic equations of hydrostatic motion, subject to the long-wave approximation, yield separate shelf and slope solutions, which are matched at the shelf break to specify the eigenfunctions. The associated eigenvalues define the dispersion relations for each of the modes. Wavenumber-frequency pairs derived from NOAA sea surface height stations along the coast are plotted on the first-mode dispersion curve, and the agreement is good. The theory also shows good agreement with the wave data of D. P. Wang. The authors address the propagation of continental shelf waves in the Mid-Atlantic Bight. An analytical model of the bathymetry in the region is constructed by representing the continental shelf as a gently sloping bottom, which deepens linearly with offshore distance to the place where it meets the continental slope. Seaward of that point, the bathymetry is modeled with an exponentially decaying function of distance. The linearized, barotropic equations of hydrostatic motion, subject to the long-wave approximation, yield separate shelf and slope solutions, which are matched at the shelf break to specify the eigenfunctions. The associated eigenvalues define the dispersion relations for each of the modes. Wavenumber-frequency pairs derived fromNOAAsea surface height stations along the coast are plotted on the first-mode dispersion curve, and the agreement is good. The theory also shows good agreement with the wave data of D. P. Wang. [PUBLICATION ABSTRACT] |
Author | Schulz, William J. Mied, Richard P. Snow, Charlotte M. |
Author_xml | – sequence: 1 givenname: William J. surname: Schulz fullname: Schulz, William J. organization: U.S. Naval Academy, Annapolis, Maryland – sequence: 2 givenname: Richard P. surname: Mied fullname: Mied, Richard P. organization: Naval Research Laboratory, Washington, D.C – sequence: 3 givenname: Charlotte M. surname: Snow fullname: Snow, Charlotte M. organization: Naval Research Laboratory, Washington, D.C |
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Cites_doi | 10.1175/1520-0485(1973)003<0073:CSWLFV>2.0.CO;2 10.1016/j.pocean.2007.07.001 10.1175/1520-0485(1988)018<0115:ANMIOT>2.0.CO;2 10.1016/j.csr.2010.10.005 10.1017/S0022112075001632 10.1175/1520-0485(1990)020<1206:CTWOTC>2.0.CO;2 10.1175/1520-0485(1983)013<1012:TGAPOS>2.0.CO;2 10.1029/JC084iC06p03227 10.1175/2009JPO4204.1 10.1016/j.dynatmoce.2004.12.003 10.1029/2006GL026395 10.1017/S0022112069001455 10.1175/1520-0485(1978)008<0481:SSLFAT>2.0.CO;2 10.1175/1520-0469(1975)032<0233:TGMAAT>2.0.CO;2 10.1029/JC083iC12p06083 10.1029/JZ067i013p05147 10.1175/1520-0485(1990)020<1219:OTDOFC>2.0.CO;2 |
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Keywords | continental slope models continental shelf eigenvalues Long wave Equation of motion Dispersion relation eigenfunction Linearized equation Wave propagation shelf-slope break bathymetry sea level |
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SubjectTerms | Bathymetry Continental shelves Continental slope Earth, ocean, space Exact sciences and technology External geophysics Marine Oceanography Physics of the oceans Propagation Remote sensing Studies Time series Wave propagation |
Title | Continental Shelf Wave Propagation in the Mid-Atlantic Bight: A General Dispersion Relation |
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