Application of the linear dispersion relation with respect to depth inversion and remotely sensed imagery

Remote sensing methods have been developed to estimate bathymetry through the use of a theoretical relationship between wave speed and water depth known as the linear, finite depth, dispersion equation for surface gravity waves. The authors describe a validation effort encompassing several hundred o...

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Veröffentlicht in:IEEE transactions on geoscience and remote sensing 2001-09, Vol.39 (9), p.2060-2072
1. Verfasser: Holland, T.K.
Format: Artikel
Sprache:eng
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