Radar imaging mechanism of marine sand waves at very low grazing angle illumination
Ingo Hennings and Dagmar Herbers
Abstract
The
investigations carried out between 2002-2004 during several field experiments
within the Operational radar and optical mapping in monitoring hydrodynamic,
morphodynamic and environmental parameters for coastal management project
(OROMA) aimed to improve the effectiveness of new monitoring technologies
such as shipborne imaging radars in coastal waters. The coastal monitoring
radar of the GKSS Research Centre, Geesthacht, Germany, is based on a Kelvin
Hughes RSR 1000 X-band (9.42 GHz) VV polarized river radar and was mounted on
board the research vessel Ludwig Prandtl
during the experiments in the Lister Tief, a tidal inlet of the German Bight in
the North Sea. The important progress realized in this investigation is the
availability of calibrated X-band radar data. Another central point of the
study is to demonstrate the applicability of the quasi-specular scattering
theory in combination with the weak hydrodynamic interaction theory for the
radar imaging mechanism of the sea bed. It is shown that specular point
scattering contributes significantly to the normalized radar cross section
(NRCS) modulation due to marine sand waves. According to the theory
quasi-specular scattering can be applied for wind speeds below 8 m/s. Measured
and simulated NRCS modulations caused by flood and ebb tide oriented marine
sand waves have been compared and agree fairly well.
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History
Submitted: 11 Jun 2005
Revised: 16 Dec 2005
Accepted: 17 Dec 2005
Citation
Hennings I & D Herbers, 2005. Radar imaging mechanism of marine sand waves at very low grazing angle illumination.
EARSeL eProceedings, 4(2), 226-240
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ISSN 1729-3782
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