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Scatterer Characterisation Using Polarimetric SAR Tomography

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<strong>Scatterer</strong> <strong>Characterisation</strong> <strong>Using</strong><br />

<strong>Polarimetric</strong> <strong>SAR</strong> <strong>Tomography</strong><br />

Stéphane Guillaso and Andreas Reigber<br />

Berlin University of Technology, Computer Vision and Remote Sensing<br />

Sekr. FR3-1, Franklinstr. 28/29, D-10587 Berlin, Germany<br />

Email: stephane@cs.tu-berlin.de, anderl@cs.tu-berlin.de<br />

Abstract— This paper presents the first step to characterise<br />

scatterers using polarimetric <strong>SAR</strong> tomography (POLTOM<strong>SAR</strong>).<br />

It is a logical extension of the tomographic data processing, which<br />

consists to use the vectorial properties of electromagnetic waves.<br />

An introduction to the estimation of the polarisation state of<br />

retrieved target is proposed. It is based on a modified signal<br />

model adapted to the MUSIC algorithm. This makes it possible<br />

to determinate the physical nature of detected object, which is not<br />

possible using classical approach, unless having the ground-truth<br />

of the scene under study. The experimental results are shown<br />

using a multibaseline data set acquired in L-band by DLR’s<br />

experimental <strong>SAR</strong> (E-<strong>SAR</strong>) on a test site near Oberpfaffenhofen<br />

/ Germany.<br />

I. INTRODUCTION<br />

<strong>SAR</strong> tomography is the extension of conventional twodimensional<br />

<strong>SAR</strong> imaging principle to three dimensions. A<br />

real three-dimensional imaging of a scene is achieved by<br />

the formation of an additional synthetic aperture in elevation,<br />

using a coherent combination of images acquired from several<br />

parallel flight tracks. The introduction of tomographic <strong>SAR</strong><br />

offers the possibility of a direct localisation of all scattering<br />

contributions in a volume [1], [2]. This greatly extends the<br />

potential of <strong>SAR</strong>, particularly for the analysis of volume<br />

structures, like for example forests or urban areas [3], [4].<br />

Up to now, different investigation of high-resolution approaches,<br />

like Capon [2], MUSIC [3], were proposed in<br />

order to improve the resolution achieved using the standard<br />

beamforming Fourier-based method [1]. These methods are<br />

often employed for so-called DoA (Direction-of-Arrical) of<br />

received waves using an antenna array. Basically, a multibaseline<br />

acquisition sustem represents an antenna array and<br />

these methods can be applied in order to determine the height<br />

of dominant scatterers. there are presented in section II. All<br />

these approaches make it possible to retrieve the position<br />

of scatterers over volumetric areas, but give any information<br />

about the nature of the scatterer itself unless having the<br />

ground-truth of the scene under study.<br />

A first approach to characterise the nature of retrieved target<br />

is presented in section III. It is based on a modified signal<br />

model adapted to MUSIC algorithm. This approach is applied<br />

to partial polarimetric data [3]. On the one hand, the MUSIC<br />

approach is able to give a higher precision about the scatterer<br />

height than using only single channel <strong>SAR</strong> data. On the<br />

other hand, polarimetric MUSIC approach makes it possible to<br />

0-7803-9051-2/05/$20.00 (C) 2005 IEEE<br />

retrieve a partial polarimetric characterisation of the scatterer<br />

observed.<br />

The efficiency of this polarimetric <strong>SAR</strong> tomography analysis<br />

is demonstrated using 14 fully polarimetric <strong>SAR</strong> images,<br />

obtained from DLR-E<strong>SAR</strong> airborne sensor in L-band repeatpass<br />

mode.<br />

II. MONOCHANNEL <strong>SAR</strong> TOMOGRAPHY<br />

L<br />

x<br />

z<br />

n<br />

r<br />

1<br />

2 ···<br />

K − 1<br />

K<br />

Fig. 1. Principle of multibaseline <strong>SAR</strong> tomography. An area is seen from<br />

K sensors on parallel flight tracks.<br />

<strong>SAR</strong> tomography consis in focusing several <strong>SAR</strong> images in<br />

the third dimension, in order to image volumetric areas, such<br />

as forests or cities. This means to form a synthetic aperture<br />

along the direction perpendicular to azimuth and to the radar<br />

line of sight. This principle is illustrated by Fig. 1.<br />

The geometry of a tomographic data acquisition uses typically<br />

K interferometric tracks non uniformly spaced, which<br />

observe the same scene. From the K images, 3D profiles might<br />

be extracted. This makes it possible to detect target under a<br />

covered volume or to generate 3D representation of the scene<br />

under study.<br />

Commonly, tomographic <strong>SAR</strong> data are processed using<br />

a two steps SPECAN (SPECtral ANalysis) algorithm. The<br />

first step is a deramping of the signal, which corrects the<br />

quadratic phase variation, occuring during tomographic data<br />

acquisition [1]. After deramping, the spatial frequency of the<br />

signals depends only on the height of the occurring scattering<br />

processes. Thereby, the height of a scatterer can be revealed<br />

by a spectral estimation method. The second step is the signal<br />

y


focussing, which is performed using standard high resolution<br />

methods such as Fourier, Capon, and MUSIC [5].<br />

A tomographic data acquisition system is constitued by K<br />

sensors, or interferometric paths. The signals xk received by<br />

each sensor k provided by D scatterers localised at height<br />

{zd} D d=1 are arranged in the K × 1 vector �x:<br />

�x =[A]�s + �n (1)<br />

where �s represents the backscattered power of the D scatterers<br />

and �n denotes a vector formed by scalar nk representing a<br />

circular Gaussian white noise. The [A] matrix, with dimension<br />

K × D, contains the phase response due to the sensor<br />

geometry only. This matrix is made up various vectors �a(zd)<br />

representing the steering vector, which corresponds to the d-th<br />

scatterer:<br />

�a(zd) =[e iφ1(zd) iφK(zd) T<br />

···e ] (2)<br />

where φk(zd) = − 4π<br />

λ<br />

each term is define by Fig. 2.<br />

zs<br />

H0<br />

√ (H0−zd+zs) 2 +(ygr+ys+ z d<br />

tan θ )2, where<br />

ys<br />

θ<br />

Ck<br />

ygr<br />

z<br />

tan θ<br />

θ z<br />

Fig. 2. Geometric parameters used during tomographic data processing.<br />

All high resolution methods are based on a covariance<br />

matrix formulation defined as:<br />

[R] =〈�x�x † 〉 which is estimated by [ ˆ N�<br />

R]=<br />

(3)<br />

n=1<br />

�xn�x † n<br />

where N > K represents the number of sample used,<br />

necessary to obtain a non-singular matrix [ ˆ R].<br />

To focus tomographic <strong>SAR</strong> data, two approaches based on<br />

high resolution methods are existing: classical- and subspacebased.<br />

Classical methods are the famous Fourier- and Caponbased<br />

approaches. The main idea is to focus the system on<br />

a certain height, corresponding to the height of a scatterer.<br />

To do that, the range of valid heights is scanned in order<br />

to find the maximum of power. The estimated powers given<br />

by Fourier- and Capon-based, ˆ PF (z) and ˆ PC(z) respectively,<br />

beamforming approaches are function of the height z:<br />

ˆPF (z) = �a(z)† [ ˆ R]�a(z)<br />

K2 and ˆ 1<br />

PC(z) =<br />

�a(z) † [ ˆ R] −1 (4)<br />

�a(z)<br />

where �a(z) represents the steering vector given by Eq. 2.<br />

The second category is based on the principle of subspace<br />

estimation. It gives an estimation of the scatterer height with<br />

an infinite resolution, independently of the signal-to-noise<br />

ratio (SNR). The must known subspace methods are MUSIC,<br />

ESPRIT, WSF [5]. In the case of tomographic <strong>SAR</strong> data<br />

processing, the MUSIC method has been used. The pseudobeamforming<br />

of MUSIC, ˆ PM(z), is given by:<br />

ˆPM(z) =<br />

1<br />

�a † ([ ÊN ][ ÊN ] † )�a<br />

where [ ÊN ] represents the noise subspace obtained after an<br />

eigendecomposition of the observed covariance matrix, [ ˆ R]=<br />

[ Ê][ˆ Λ][ Ê]† [5]. The term pseudo-beamforming is employed<br />

here because the position of the retrieved power is using only<br />

to localise the target height.<br />

The different methods presented above have been applied<br />

to a L-band data set of the E-<strong>SAR</strong>. The data were acquired<br />

in May 1998 on the test site of Oberpfaffenhofen/Germany.<br />

During the campaign fully polarimetric data sets were recorded<br />

from K =14 parallel flight tracks with a respective distance<br />

of approximatively 20 meters. The airplane used by the E-<br />

<strong>SAR</strong> is equipped with a high-precision positioning system,<br />

which allows an absolute estimation of the antenna tracks<br />

with an accuracy of few centimetres. With this data the errors<br />

arising from the aircraft movements are compensated by a new<br />

approach of motion compensation during <strong>SAR</strong> processing [6].<br />

Additionally, a very precise velocity and range delay variation<br />

compensation have been carried out. To minimise small errors<br />

in the absolute positioning of the aircraft, also a calibration<br />

of the image phases, based on the response of a single corner<br />

reflectors is performed.<br />

height (m)<br />

height (m)<br />

660<br />

650<br />

640<br />

630<br />

Fourier - HH<br />

street<br />

forest<br />

building corner<br />

reflector<br />

surface<br />

620<br />

0<br />

surface<br />

100 200 300 400 500<br />

azimuth position (pixels)<br />

MUSIC (1) - HH<br />

660<br />

street<br />

650<br />

640<br />

630<br />

forest<br />

building corner<br />

reflector<br />

surface<br />

620<br />

0<br />

surface<br />

100 200 300 400 500<br />

azimuth position (pixels)<br />

height (m)<br />

height (m)<br />

660<br />

650<br />

640<br />

630<br />

CAPON - HH<br />

street<br />

forest<br />

building corner<br />

reflector<br />

surface<br />

(5)<br />

620<br />

0<br />

surface<br />

100 200 300 400 500<br />

azimuth position (pixels)<br />

MUSIC (5) - HH<br />

660<br />

street<br />

650<br />

640<br />

630<br />

forest<br />

building corner<br />

reflector<br />

surface<br />

620<br />

0<br />

surface<br />

100 200 300 400 500<br />

azimuth position (pixels)<br />

Fig. 3. Fourier-, Capon-, MUSIC 1-, MUSIC 5-based height/azimuth slice<br />

tomograms.<br />

Fig. 3 represent height/azimuth slices of tomograms obtained<br />

using Fourier, Capon, and MUSIC approaches, respectively.<br />

The left part of the scene is constituted by a dense<br />

spruce forest with a height of 15 to 20 meters [1]. Then, the<br />

azimuth slice crosses a street, some bushes and a building.<br />

The right part of the scene consists of nearly flat grass land<br />

with a corner reflector.<br />

The Capon-based approach makes it possible to reduce the<br />

sidelobes, particularly strong in case of the building and the<br />

corner reflector. The ground under the forest is better visible<br />

with Capon-based approach. Indeed, the reflectivity of the


grass land is less visible than the ground under the forest. This<br />

indicates that the scattering mechanisms detected under the<br />

forest canopy and the grass land are different. Like the grass<br />

land possesses a surface reflection, the scattering mechanism<br />

under the forest canopy corresponds essentially to a doublebounce<br />

ground-trunk, which gives the ground location. The<br />

same holds for the canopy density. It is also possible to<br />

determinate a height of about 20 meters for the trees.<br />

In the MUSIC-based approach, on the one hand, only one<br />

scatterer was assumed, on the other hand, 5 scatterers where<br />

considered in the processing. The shape of the building is<br />

better visualised, as well as the ground of the grass field, when<br />

only one scatterer is assumed. It is also possible to estimate<br />

the height of the corner reflector. Over the forest, ground and<br />

canopy reflection can be expected. These results are better<br />

when using 5 scatterers, but make no sense for the building<br />

and specially for the grass area.<br />

The result interpretation is possible thanks to a precise<br />

knowledge of the ground-truth of the area under study. Otherwise,<br />

the used high resolution methods give any information<br />

about the physical nature of the detected object. In order to be<br />

able to characterise the nature of the detected objects, it is necessary<br />

to use polarimetric <strong>SAR</strong> data. Indeed <strong>SAR</strong> polarimetry<br />

studies the behaviour of the electromagnetic scattering from<br />

the observed scene. This provides physical information on<br />

scatterers in terms of separation and identification of scattering<br />

mechanisms inside a resolution cell [7].<br />

III. POLARIMETRIC <strong>SAR</strong> TOMOGRAPHY<br />

To visualise the importance of the polarisation in the <strong>SAR</strong><br />

tomography field, the Capon-based approach has been applied<br />

to <strong>SAR</strong> data with different polarisation. The Capon-based<br />

approach is selected because it is sensitive to the power of<br />

the detected backscatterer and reduce the sidelobes.<br />

height (m)<br />

660<br />

650<br />

640<br />

630<br />

CAPON - HH<br />

street<br />

forest<br />

building corner<br />

reflector<br />

surface<br />

height (m)<br />

620<br />

0<br />

surface<br />

100 200 300 400 500<br />

620<br />

0<br />

surface<br />

100 200 300 400 500<br />

azimuth position (pixels)<br />

azimuth position (pixels)<br />

CAPON - HV<br />

660<br />

street<br />

650<br />

640<br />

630<br />

forest<br />

building corner<br />

reflector<br />

surface<br />

height (m)<br />

660<br />

650<br />

640<br />

630<br />

620<br />

0<br />

surface<br />

100 200 300 400 500<br />

azimuth position (pixels)<br />

CAPON - VV<br />

street<br />

forest<br />

building corner<br />

reflector<br />

surface<br />

Fig. 4. Capon-based height/azimuth slice tomograms using <strong>SAR</strong> data with<br />

different polarisation.<br />

Fig. 4 shows the results obtained using the Capon-based<br />

approach with different polarisation data. They are different<br />

according to the selected polarisation. Over the forest, it can<br />

be observed that the ground is less visible using a vertical<br />

polarisation (VV) and disappear in the cross-polarisation data<br />

(HV). On the contrary, the canopy density becomes more<br />

explicit by using HV data. The corner reflector misses in the<br />

HV data, which is one of the principal characteristic of the<br />

HV data. on the other hand, the reflection over the building is<br />

the strongest with VV data.<br />

This first result interpretation using data with diverse polarisations<br />

shows that the nature of the observed scattering<br />

mechanisms can be estimated. But, like previously, this interpretation<br />

is valid only if the ground-truth is known. Like the<br />

Capon-based obtained data are not coherent, it is not possible<br />

to apply simple polarimetric decomposition, like Pauli-based<br />

decomposition, which can inform about the physical nature of<br />

the detected scatterer. Thereby, the tomographic <strong>SAR</strong> approach<br />

is extended to the use of the vectorial properties of electromagnetic<br />

waves as a logical extension to the tomographic DATA<br />

processing.<br />

An extension of the MUSIC algorithm [8] allows to retrieve<br />

the polarisation information associate to dominant scatterers<br />

[3]. This approach is based on the use of Jones-vector formulation.<br />

The polarisation state of an electromagnetic wave<br />

is defined by its Jones-vector, � E, which contains complete<br />

information about amplitudes and phases of electromagnetic<br />

field components. The Jones-vector can be written using two<br />

polarisation angles: γ and δ, and the polarisation ratio ρ � E :<br />

�E def<br />

= E<br />

� cos γ<br />

sin γe iδ<br />

� �<br />

1<br />

= E cos γ<br />

with ρ � E = tan γe iδ .<br />

<strong>Using</strong> a similar form than Eq. 2, let �y, �s, and �n denote the<br />

received signal, the source amplitude, and the noise vectors.<br />

Then, �y has the following form:<br />

ρ � E<br />

�<br />

(6)<br />

�y =[A]�s + �n (7)<br />

where the 2K × D matrix [A] is the steering matrix with<br />

columns �ad as the steering vectors:<br />

�ad =[ � E T d e iφA(zd)<br />

··· � E T d e iφK(zd) ] T<br />

where { � Ed = [cos γd sin γdeiδd T D ] } d=1 and φk(zd) is given<br />

by Eq. 2.<br />

In [8], a polarisation estimation method using the noise<br />

subspace eigenvectors of [ ˆ R] is described. It can be shown<br />

that each steering vector �ad may be written as the linear<br />

combination of two direction vectors �b1(zd) and �b2(zd), which<br />

are associated to the scattering height zd and two arbitrary<br />

orthogonal polarisations. The steering vector �ad can be written<br />

as:<br />

�ad =[Bd] � fd<br />

(9)<br />

where {[Bd] =[ � b1(zd) � b2(zd)]} D d=1 and � fd represents a 2×1<br />

vector consisting of the linear combination coefficients.<br />

For the sake of simplicity, { � b1(zd)} D d=1 and {� b2(zd)} D d=1<br />

are normalised:<br />

� b ′ 1(zd) = � b1(zd)<br />

� � b1(zd)� and � b ′ 2(zd) = � b2(zd)<br />

� � b2(zd)�<br />

(8)<br />

(10)


Let define �a ′ d = �ad/��ad� = [B ′ d ] � f ′ d as the normalised<br />

steering vector of �ad with {[B ′ d ]=[�b ′ 1(zd) �b ′ 2(zd)]} D d=1 .It<br />

can be shown that the ratio between the two elements of � f ′ d<br />

corresponds to the polarisation ratio ρEd � . The estimation of<br />

�f ′ d is given by calculating the eigenvector of the Hermitian<br />

matrix [B ′ d ]† [EN ][EN ] † [B ′ d ], corresponding the the smallest<br />

eigenvalue.<br />

Finally, the two polarimetric angles {γd} D d=1 and {δd} D d=1<br />

can be determined uniquely from:<br />

γd = tan −1<br />

� �<br />

�<br />

� 1<br />

�<br />

�<br />

� �<br />

�ρEd<br />

� � with δd = − arg ρEd � (11)<br />

From the spheric angle, it is possible to estimate the<br />

orientation φ and the ellipticity τ angles characterising the<br />

polarisation ellipse. The relations between all different angles<br />

are:<br />

tan 2φ = tan 2γ cos δ<br />

sin 2τ = sin2γsin δ (12)<br />

height (m)<br />

height (m)<br />

655<br />

645<br />

635<br />

625<br />

655<br />

645<br />

635<br />

625<br />

forest<br />

MUSIC (5) - PHI<br />

street<br />

building<br />

corner<br />

reflector<br />

ground<br />

0 100 200 300 400 500<br />

azimuth position (pixels)<br />

MUSIC (5) - TAU<br />

forest<br />

street<br />

building<br />

corner<br />

reflector<br />

ground<br />

0 100 200 300 400 500<br />

azimuth position (pixels)<br />

+15 ◦<br />

angles (deg) −15◦<br />

+15 ◦<br />

angles (deg) −15◦<br />

Fig. 5. Angles characterising the polarisation ellipse. Top Orientation angle<br />

φ. Bottom Ellipticity angle τ<br />

Fig. 5 presents results of this polarimetric approach of<br />

the <strong>SAR</strong> tomography, using HH and VH polarisation data.<br />

It represents the orientation φ and the ellipticity τ angles<br />

retrieved using the polarimetric MUSIC approach, assuming 5<br />

scatterers. These results show that the retrieved polarisations<br />

are media depending. The polarisation state responses of the<br />

forest ground and the grass field are not the same. The<br />

response of the ground over the forest is a linear polarisation<br />

(τ =0◦ ) with an orientation about 15◦ , whereas the polarisation<br />

over the grass field is horizontal linear polarisation,<br />

characteristic of a surface reflection by a wave emitted in<br />

a horizontal polarisation. Over the building, the polarisation<br />

state is similar with that the ground under the forest. Over the<br />

forest canopy, polarimetric responses are random, as it can be<br />

expected from the random behaviour of this kind of media.<br />

This polarimetric approach of the <strong>SAR</strong> tomography shows<br />

that the polarimetric behaviour is depending with the media<br />

observed and make it possible to characterise partially targets<br />

in terms of height position but also by their physical properties.<br />

IV. CONCLUSION<br />

This paper presents the first step into polarimetric <strong>SAR</strong><br />

tomography. In a first part, hight resolution methods were used<br />

to generate high quality tomograms. The results obtained show<br />

an improvement compared to the initial results, and different<br />

scatterers have been detected. Nevertheless, unless having<br />

the ground-truth of the area under study, the mono-channel<br />

approach of the <strong>SAR</strong> tomography does not make it possible<br />

to identify the nature of the scattering mechanism detected.<br />

For stage with this disadvantage, a polarimetric approach of<br />

the <strong>SAR</strong> tomography approach is proposed. Like the Caponbased<br />

result data are not coherent and it is not possible to apply<br />

to the obtained data a simple polarimetric decomposition like,<br />

for instance, the Pauli decomposition, which is related to some<br />

basic scattering mechanisms, a polarisation state estimation<br />

based on a extension of the MUSIC algorithm has been<br />

proposed. This method takes into account partially polarised<br />

data. It is shown that the polarimetric behaviour is depending<br />

with the observed media and the partial characterisation of the<br />

target is possible. In the future, a use of fully polarimetric data<br />

will be necessary to completely characterize the objects.<br />

ACKNOWLEDGMENT<br />

This work was supported by the German Science Foundation<br />

DFG, under project No. RE 1698/1.<br />

REFERENCES<br />

[1] A. Reigber and A. Moreira, “First Demonstration of Airborne <strong>SAR</strong><br />

<strong>Tomography</strong> using Multibaseline L-band Data,” IEEE Trans. Geosci.<br />

Remote Sensing, vol. 38, pp. 2142–2152, September 2000.<br />

[2] F. Lombardini and A. Reigber, “Adaptive Spectral Estimation for<br />

Multibaseline <strong>SAR</strong> <strong>Tomography</strong> with Airborne L-band Data,” in Proc.<br />

IGARSS’03, (Toulouse, France), July 2003.<br />

[3] S. Guillaso and A. Reigber, “<strong>Polarimetric</strong> <strong>SAR</strong> <strong>Tomography</strong>,” in Proc.<br />

POLI<strong>SAR</strong>’05, (Frascati, Italy), 2005.<br />

[4] S. Guillaso, A. Reigber, and L. Ferro-Famil, “Evaluation of the ESPRIT<br />

Approach in <strong>Polarimetric</strong> Interferometric <strong>SAR</strong>,” in Proc. IGARSS’05,<br />

(Seoul, Korea), Jul. 2005.<br />

[5] P. Stoica and R. Moses, Introduction to Spectral Analysis. N. J.: Prentice<br />

Hall, 1997.<br />

[6] A. Reigber, P. Prats, and J. J. Mallorqui, “Refined estimation of<br />

time-varying baseline errors in airborne <strong>SAR</strong> interferometry,” in Proc.<br />

IGARSS’05, (Seoul, Korea), Jul. 2005.<br />

[7] S. R. Cloude and E. Pottier, “An Entropy Based Classification Scheme<br />

for Land Applications of <strong>Polarimetric</strong> <strong>SAR</strong>,” IEEE Trans. Geosci. Remote<br />

Sensing, vol. 35, pp. 68–78, Jan. 1997.<br />

[8] E. Ferrara and T. Parks, “Direction finding with an array of antennas<br />

having diverse polarizations,” IEEE Trans. Antennas Propagat., vol.AP-<br />

31, pp. 231–236, March 1983.

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