Assessment of ERS synthetic aperture radar wave spectra retrieved from the Max-Planck-Institut (MPI) scheme through intercomparisons of 1 year of directional buoy measurements
Assessment of ERS synthetic aperture radar wave spectra retrieved from the Max-Planck-Institut (MPI) scheme through intercomparisons of 1 year of directional buoy measurements
One year of directional buoy measurements comprising the period from May 1994 to April 1995 acquired in deep ocean waters by an offshore heave-pitch-roll buoy are used for the assessment of the directional wave spectra retrieved from synthetic aperture radar (SAR) images using the Max-Planck-Institut (MPI) scheme. SAR is the only sensor so far deployed from satellites that can provide measurements of the directional wave spectrum with high spatial and temporal coverage when operating in the so-called SAR wave mode. Millions of SAR wave mode imagettes have been and are still being acquired over all oceanic basins yielding a powerful data set for investigating wind waves. However, directional spectral information retrieved from SAR images has not yet been assessed against in situ measurements. For the first time, detailed validations of the main wave parameters, that is, significant wave height, mean direction of propagation, and mean wavelength, are performed. It is shown that in terms of these parameters the first-guess spectra taken from the wave model WAM are in better agreement with the buoy measurements than the MPI scheme retrievals. When considering only the longer waves in the part of the spectrum observed by SAR, on the other hand, the algorithm performs at least as well as the third-generation WAM wave model. In addition to the limitations of the MPI scheme in extending the spectral information beyond the high wave number cut-off, an observed misinterpretation of wind sea energy as swell by the MPI scheme is shown to be caused by the use of a quasi-linear approximation of the imaging model in the numerical iteration procedure.
remote sensing, wind waves, SWM SAR wave mode
C07019-[19pp]
Violante-Carvalho, N.
ab7c0274-f954-4fba-92dd-1a153b6da8c7
Robinson, I.S.
548399f7-f9eb-41ea-a28d-a248d3011edc
Schulz-Stellenfleth, J.
a5a19f96-e5b5-4110-94ca-92f9c5d398de
26 July 2005
Violante-Carvalho, N.
ab7c0274-f954-4fba-92dd-1a153b6da8c7
Robinson, I.S.
548399f7-f9eb-41ea-a28d-a248d3011edc
Schulz-Stellenfleth, J.
a5a19f96-e5b5-4110-94ca-92f9c5d398de
Violante-Carvalho, N., Robinson, I.S. and Schulz-Stellenfleth, J.
(2005)
Assessment of ERS synthetic aperture radar wave spectra retrieved from the Max-Planck-Institut (MPI) scheme through intercomparisons of 1 year of directional buoy measurements.
Journal of Geophysical Research, 110 (C7), .
(doi:10.1029/2004JC002382).
Abstract
One year of directional buoy measurements comprising the period from May 1994 to April 1995 acquired in deep ocean waters by an offshore heave-pitch-roll buoy are used for the assessment of the directional wave spectra retrieved from synthetic aperture radar (SAR) images using the Max-Planck-Institut (MPI) scheme. SAR is the only sensor so far deployed from satellites that can provide measurements of the directional wave spectrum with high spatial and temporal coverage when operating in the so-called SAR wave mode. Millions of SAR wave mode imagettes have been and are still being acquired over all oceanic basins yielding a powerful data set for investigating wind waves. However, directional spectral information retrieved from SAR images has not yet been assessed against in situ measurements. For the first time, detailed validations of the main wave parameters, that is, significant wave height, mean direction of propagation, and mean wavelength, are performed. It is shown that in terms of these parameters the first-guess spectra taken from the wave model WAM are in better agreement with the buoy measurements than the MPI scheme retrievals. When considering only the longer waves in the part of the spectrum observed by SAR, on the other hand, the algorithm performs at least as well as the third-generation WAM wave model. In addition to the limitations of the MPI scheme in extending the spectral information beyond the high wave number cut-off, an observed misinterpretation of wind sea energy as swell by the MPI scheme is shown to be caused by the use of a quasi-linear approximation of the imaging model in the numerical iteration procedure.
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Published date: 26 July 2005
Keywords:
remote sensing, wind waves, SWM SAR wave mode
Identifiers
Local EPrints ID: 20404
URI: http://eprints.soton.ac.uk/id/eprint/20404
ISSN: 0148-0227
PURE UUID: 7d414ef3-d717-4d74-b0b9-d03730a979c5
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Date deposited: 24 Feb 2006
Last modified: 15 Mar 2024 06:25
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Author:
N. Violante-Carvalho
Author:
J. Schulz-Stellenfleth
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