Estimating ocean frontal surface velocity distributions from radar imagery signatures

An inversion algorithm for inferring the surface velocity field of buoyant plume frontal features from observed radar imagery has been developed. The inversion technique is based upon an assumption, suggested by Alpers and Hennings' (AH) relaxation model (1984), that near strongly convergent fr...

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Veröffentlicht in:	IEEE transactions on geoscience and remote sensing 2001-11, Vol.39 (11), p.2454-2464
Hauptverfasser:	Cooper, A.L., Chubb, S.R., Sletten, M.A., Trump, C.L.
Format:	Artikel
Sprache:	eng
Schlagworte:	Applied geophysics Backscatter Backscattering Brackish Convergence of numerical methods Earth sciences Earth, ocean, space Exact sciences and technology Frequency Image converters Internal geophysics Inversions Marine geology Mathematical models Oceans Plumes Radar cross section Radar imagery Radar imaging Radar scattering Sea surface Signatures Velocity control X-band
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