Two dimensional bispectral estimates from ocean SAR images

被引:6
作者
Le Caillec, J. M. [1 ]
Garello, R. [1 ]
Chapron, B. [2 ]
机构
[1] Telecom Bretagne Dept ITI, BP 832, F-29285 Brest, France
[2] IFREMER, DRO OS, Plouzane, France
关键词
D O I
10.5194/npg-3-196-1996
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Synthetic Aperture Radar (SAR) images of the ocean yield a lot of information on the sea-state surface providing that the mapping process between the surface and the image is clearly defined. However it is well known that SAR images exhibit non-gaussian statistics and that the motion of the scatterers on the surface, while the image is being formed, may yield to nonlinearities. The detection and quantification of these nonlinearities are made possible by using Higher Order Spectra (HOS) methods and more specifically, bispectrum estimation, The development of the latter method allowed us to find phase relations between different parts of the image and to recognise their level of coupling, i.e. if and how waves of different wavelengths interacted nonlinearly. This information is quite important as the usual models assume strong nonlinearities when the waves are propagating in the azimuthal direction (i.e. along the satellite track) and almost no nonlinearities when propagating in the range direction. In this paper, the mapping of the ocean surface to the SAR image is reinterpreted and a specific model (i.e. a Second Order Volterra Model) is introduced. The nonlinearities are thus explained as either produced by a nonlinear system or due to waves propagating into selected directions (azimuth or range) and interacting during image formation. It is shown that quadratic nonlinearities occur for waves propagating near the range direction while for those travelling in the azimuthal direction the nonlinearities, when present, are mostly due to wave interactions but are almost completely removed by the filtering effect coming from the surface motion itself (azimuth cut-off). An inherent quadratic interaction filtering (azimuth high pass filter) is also present. But some other effects, apparently nonlinear, are not detected with the methods described here, meaning that either the usual relation developed for the Ocean-to-SAR, transform is somewhat incomplete, although the mechanisms leading to its formulation seem to be correct, or that these nonlinearities cannot be detected in the classical bispectrum theory.
引用
收藏
页码:196 / 215
页数:20
相关论文
共 27 条
[1]   ON THE DETECTABILITY OF OCEAN SURFACE-WAVES BY REAL AND SYNTHETIC APERTURE RADAR [J].
ALPERS, WR ;
ROSS, DB ;
RUFENACH, CL .
JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS, 1981, 86 (NC7) :6481-6498
[2]   ON THE RELATIVE IMPORTANCE OF MOTION-RELATED CONTRIBUTIONS TO THE SAR IMAGING MECHANISM OF OCEAN SURFACE-WAVES [J].
ALPERS, WR ;
BRUENING, C .
IEEE TRANSACTIONS ON GEOSCIENCE AND REMOTE SENSING, 1986, 24 (06) :873-885
[3]   VALIDATION OF A SYNTHETIC APERTURE RADAR OCEAN WAVE IMAGING THEORY BY THE SHUTTLE IMAGING RADAR-B EXPERIMENT OVER THE NORTH-SEA [J].
BRUNING, C ;
ALPERS, W ;
ZAMBRESKY, LF ;
TILLEY, DG .
JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS, 1988, 93 (C12) :15403-&
[4]   MONTE-CARLO SIMULATION STUDIES OF THE NONLINEAR IMAGING OF A 2-DIMENSIONAL SURFACE-WAVE FIELD BY A SYNTHETIC APERTURE RADAR [J].
BRUNING, C ;
ALPERS, W ;
HASSELMANN, K .
INTERNATIONAL JOURNAL OF REMOTE SENSING, 1990, 11 (10) :1695-1727
[5]   BISPECTRAL ANALYSIS OF 2-DIMENSIONAL RANDOM-PROCESSES [J].
CHANDRAN, V ;
ELGAR, S .
IEEE TRANSACTIONS ON ACOUSTICS SPEECH AND SIGNAL PROCESSING, 1990, 38 (12) :2181-2186
[6]  
Erdem A. T., 1992, Higher Order Statistics. Proceedings of the International Signal Processing Workshop, P99
[7]  
Garello R, 1996, ETUDE METHODES SPECT
[8]  
Giannakis G, 1988, IEEE T ASSP, V38, P478
[9]   CUMULANT-BASED ORDER DETERMINATION OF NON-GAUSSIAN ARMA MODELS [J].
GIANNAKIS, GB ;
MENDEL, JM .
IEEE TRANSACTIONS ON ACOUSTICS SPEECH AND SIGNAL PROCESSING, 1990, 38 (08) :1411-1423
[10]   HYDRODYNAMIC MODULATION OF SHORT WIND-WAVE SPECTRA BY LONG WAVES AND ITS MEASUREMENT USING MICROWAVE BACKSCATTER [J].
HARA, T ;
PLANT, WJ .
JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS, 1994, 99 (C5) :9767-9784