Method to generate a three-dimensional image of a ground...

Communications: directive radio wave systems and devices (e.g. – Synthetic aperture radar

Reexamination Certificate

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C342S191000, C342S192000, C342S194000, C342S195000

Reexamination Certificate

active

06384766

ABSTRACT:

BACKGROUND OF THE INVENTION
1. Field of the Invention
The present invention relates to a method for generating a three-dimensional image of a ground area using a radar with a synthetic aperture, a SAR radar. Important applications are, inter alia,
three-dimensional positioning of the ground surface and/or objects close to the ground surface,
topographic mapping where no ground check points are available, and
topographic mapping of various ground layers, especially underlying ground surface in wooded areas.
2. Description of the Related Art
SAR is an established technique for two-dimensional ground mapping with a high resolutions in this technique, short radar pulse are transmitted, or longer pulses which am compressed using a pulse compression technique, from a platform, e.g. aircraft or satellite, moving along a nominal straight path over the area of ground that is to be studied, and the change of the return signal during the movement of the platform is analysed.
The short pulse allows a high range resolution, transversely of the straight path, while a linear combination of the signals along the straight path results in a high azimuth resolution, along the straight path. The latter is equivalent to an extended antenna aperture, which is synthesised by signal processing. The condition for achieving a high azimuth resolution is that the relative amplitude and phase of the transmitted and received radar pulse are known, and that the position of the antenna is measured with great accuracy along the aperture.
The SAR technique has in realised over a wide frequency band, between about 20 MHz and 100 GHz, which corresponds to electromagnetic wavelengths between 3 mm and 15 m. Since the interaction of the reflecting structures with the electro-magnetic wave is wavelength-dependent the imaging of various surface structures differs to a considerable extent according to the frequency at which they are illuminated.
As a rule, the penetration of the wave and also the size of the dominating scattering elements decrease for higher frequencies, both being of wavelength order. For woods, for instance, this means that it is fundamentally transparent for low frequencies (<100 MHz) while high frequencies (>10 GHz) image the tree tops. By a suitable selection of frequency, it is thus possible to image layers on different levels in vegetation. Layers below th ground surface can be reproduced in similar ways. Polarisation and angle of incidence also affect the penetration of the wave and the scattering elements, even if this dependence is normally subordinated to the wavelength dependence.
Each point in the grid of the SAR image corresponds to a two-dimensional position defined by the transverse distance to a ground object and its position along the path. The position thus is unambiguous if the topography of the ground surface is known except for its mirror image through the flight path. The latter, however, can be distinguished by using the directivity of the antenna system.
The position of the ground is thus obtained as the intersection between a circular cylinder with the flight path as symmetry axis, the range cylinder, and two surfaces, one of which is a semiplane perpendicular to the cylinder axis, the azimuth plane, and the other represents the ground surface, see FIG.
1
. This fact also means that the topography must be known a priori if the SAR image is to be registered to a map projection, which in most cases is a requirement made by those who are going to use the images in practice.
If, on the other hand, the topography of the ground surface is not known, the two-dimensional geometry of the SAR image means that ground structures with the same range and azimuth co-ordinates cannot possibly be distinguished from each other. It would thus be great progress of the SAR technique could be improved such that also the topography of the ground surface could be unambiguously determined on the basis of the SAR signal.
Narrow band SAR interferometry and stereo SAR are prior-art techniques for approximately determining the topography of the ground. Here a combination is made of measurements from two parallel-displaced paths, which is illustrated in FIG.
2
. These techniques are based on the use of narrow band SAR systems which in the interferometry case result in ambiguity and in the stereo case result in insufficient height resolution. They are both based on the principle that the difference in range between two surface structures differs in the two images owing to the change in measurement geometry which is related to a difference in height. By using narrow band SAR, there will, however, be speckle noise in the image owing to the fact that the geometric resolution is much greater than the electromagnetic wavelength.
In these cases, the resolution volume generally contains multiple scattering elements which each backscatter the incident wave, which are superposed with amplitude and phase in the reconstructed image element. Superposition is equal to interference between to backscattered waves, and the resulting ground reflex thus is dependent on the angle of observation of the radar relative to the resolution volume.
In narrow band SAR where the resolution is much greater than the wavelength, the interference pattern changes very rapidly when the direction of observation changes. If, on the other hand, the resolution is of wavelength size, such as in broadband SAR, the direction of observation can change considerably without significantly affecting the interference pattern.
Normally the resolution volume contains many independent scattering elements, which results in random amplitude and phase between different resolution cells, so-called speckle noise. The interference pattern is reproducible if exactly the same measurement geometry is repeated, but it changes if the angle of observation or the character of the ground changes. The angle through which the interference pattern is correlated in inverse proportion to the extent of the resolution volume and is in proportion to half the wavelength, which is illustrated in FIG.
3
.
Narrow band SAR interferometry uses the fact that the speckle noise is correlated when the change in measurement geometry is small. In this way, changes in the difference in range are determined with an accuracy which is a fraction of a wavelength. It is disadvantageous, however, that the measurement of the difference in range is ambiguous with a multiple of half the wavelength. If the maximum acceptable change in measurement geometry with retained correlation is taken into consideration, defined as a change in range difference between neighbouring resolution cells which is smaller than half the wavelength, the height resolution is of the same order as the range resolution. In practice, this means a vertical error in the order of 1-10 m for the currently most advanced narrow band SAR systems. A drawback of the method, however, is the ambiguity which must be solved by using special algorithms, “phase unwrapping”. A further drawback is that a measurement error of wavelength size, for instance an extra delay in the atmosphere, results in a great vertical error. To determine an unambiguous topographic height manual corrections therefore are necessary.
Narrow band stereo SAR uses the fact that certain structures can be recognised in the amplitude images. However, the speckle pattern is not correlated in the two images, which means that only relatively large structures can be measured. By amplitude correlation over the image, the distances to the structure in the two images are thus determined, which is converted to a height. Stereo SAR is disadvantageous above all by the speckle noise in the two images being uncorrelated, which results in the range difference being only determinable with an error which is considerably greater than the range resolution. In practice, this means that the vertical error is in the order of 10-100 m. A further drawback of the stereo technique is that it is based on the recognition of noisy structures in two images, which requires robust pattern r

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