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Physical Sciences and Mathematics Commons

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Oceanography and Atmospheric Sciences and Meteorology

University of New Hampshire

2008

Bottom type

Articles 1 - 1 of 1

Full-Text Articles in Physical Sciences and Mathematics

Very Shallow Water Bathymetry Retrieval From Hyperspectral Imagery At The Virginia Coast Reserve (Vcr'07) Multi-Sensor Campaign, Charles M. Bachmann, Marcos J. Montes, Robert A. Fusina, Christopher Parrish, Jon Sellars, Alan Weidemann, Wesley Goode, C Reid Nichols, Patrick Woodward, Kevin Mcilhany, Victoria Hill, Richard Zimmerman, Daniel Korwan, Barry Truitt, A. Schwarzschild Jul 2008

Very Shallow Water Bathymetry Retrieval From Hyperspectral Imagery At The Virginia Coast Reserve (Vcr'07) Multi-Sensor Campaign, Charles M. Bachmann, Marcos J. Montes, Robert A. Fusina, Christopher Parrish, Jon Sellars, Alan Weidemann, Wesley Goode, C Reid Nichols, Patrick Woodward, Kevin Mcilhany, Victoria Hill, Richard Zimmerman, Daniel Korwan, Barry Truitt, A. Schwarzschild

Center for Coastal and Ocean Mapping

A number of institutions, including the Naval Research Laboratory (NRL), have developed look up tables for remote retrieval of bathymetry and in-water optical properties from hyperspectral imagery (HSI) [6]. For bathymetry retrieval, the lower limit is the very shallow water case (here defined as < 2m), a depth zone which is not well resolved by many existing bathymetric LIDAR sensors, such as SHOALS [4]. The ability to rapidly model these shallow water depths from HSI directly has potential benefits for combined HSI/LIDAR systems such as the Compact Hydrographic Airborne Rapid Total Survey (CHARTS) [10]. In this study, we focused on the validation of a near infra-red feature, corresponding to a local minimum in absorption (and therefore a local peak in reflectance), which can be correlated directly to bathymetry with a high degree of confidence. Compared to other VNIR wavelengths, this particular near-IR feature corresponds to a peak in the correlation with depth in this very shallow water regime, and this is a spectral range where reflectance depends primarily on water depth (water absorption) and bottom type, with suspended constituents playing a secondary role.