Full text: XVIIIth Congress (Part B7)

  
approach by the subspace method is explained, 
along with an experimental results derived from 
Compact Airborne Spectral Imager (CAST) data to 
compare this new method with conventional 
approaches. 
2. UNMIXING BY SUBSPACE METHOD 
2.1 Statistical unmixing methods 
Conventional statistical unmixing methods 
assume that the mixel spectral vector is a 
weighted mean of the class spectral vector which 
constitutes the mixel. Within each mixel, there are 
several mixed classes with area fractions which 
correspond to the weights of the model. These 
weights are estimated by the unmixing method. 
In a remotely sensed image with p channels Æ 
land cover classes exist in the image and area 
fraction of classw(1) is fi . A linear mixel model 
assumes that the observed p dimensional vector r 
is expressed as 
K 
r=Mf+n=> fm +n (D) 
i=l 
Where M is a p x p matrix which has class 
spectral vectors mi as column vectors, fis a vector 
which has £i as components, and the n stands for 
noise vector. 
Statistical unmixing methods include, unmixing 
by least squares, factor analysis and singular 
value decomposition (Malinowski, 1991; Settle and 
Drake 1993) By comparison, unmixing by 
subspace method does not assume a linear 
statistical model. 
2.2 The Principle of subspace method 
The basic idea behind the subspace method is 
that the class spectral vector lies mainly in a small 
class specific subspace instead of within the entire 
dimension of the spectral space. If the class 
subspace is determined from the training sample 
of each class, class membership values can be 
calculated by the projection of the mixel 
observation spectral vector from the corresponding 
subspaces from which the training samples were 
drawn(Watanabe 1969; Kohonen 1977). 
There are 3 ways of calculateing the subspace in 
the subspace method. These are algebraic, 
statistical and learning subspace method (Oja, 
1984). In this paper, a statisitical subspace method 
called | CLAFIC(CLAss-Featuring Information 
Compression) algorithm is used. This method is 
known to be fast and effective in the case where 
782 
the volume of training data is moderate. 
2.3 Subspace determination by enhanced 
CLAFIC method 
The CLAFIC algorithm determines the class 
subspace in order to maximize the projection of the 
class vector on the corresponding class subspace. 
However, by maximizing the projections for all 
classes at the same time, the separation between 
the similar classes decreases. 
In order to avoid this drawback, we have 
employed the Enhanced CLAFIC algorithm which 
maximizes the projection on the class subspace to 
which the training vector belongs and also 
minimizes the projection on the other subspaces at 
the same time. In the following, the Enhanced 
CLAFIC algorithm is described. 
In the enhanced CLAFIC method, the class 
subspace L® which corresponds to a land cover 
classesw(i) (I-1..,K) , is determined so as to 
maximize the expected projection of vector x which 
belongs to the classw(1) . It also minimizes the 
expected projection of vector x which belongs to 
the other classes is 99 ( #1). The problem here 
is to determine the subspace L9 to satisfy these 
conditions at the same time as formulating the 
next minimization problem. 
K 
V EC P? dx e aq? ) — E(x' P? xax e?) (2) 
j*i 
= 
where P% is the projection matrix to the L@ 
The first term of equation (2) is the expected 
projection of sample vectors which do not belong to 
the class w(i), and the second term is the expected 
projection of vectors which belong to the class w(2). 
By minimizing term (2), we can determine the 
subspace L/? which minimizes the first term and 
maximizes the second term of (2). 
Projection matrix Æ is expressed using 
orthogonal normal bases |ui ,...,upe 9 | of 
subspace Lf as 
(i) 
PO — Y uu (3) 
k=] 
By substituting equation (3) into (2) and 
rewriting (2) using base vector ux? (k=1,...,p9), 
K (0 0) 
S$ EG? yIx eq?) S$ Ecru? Ixew”) (4) 
2 k=1 k=1 
Calculating the expectation first, (4) becomes, 
K (1) 0} 
3 $0000 t Y uo goo (5) 
Zi k=1 k=1 
f 
International Archives of Photogrammetry and Remote Sensing. Vol. XXXI, Part B7. Vienna 1996 
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