UNSUPERVISED CLASSIFICATION PowerPoint PPT Presentation

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Title: UNSUPERVISED CLASSIFICATION


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UNSUPERVISED CLASSIFICATION
Dr. Jakob J. van Zyl
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OUTLINE
  • LEVEL 0 CLASSIFICATION
  • Theoretical characteristics
  • Single frequency interpretation
  • Single frequency results
  • Dual frequency interpretation
  • Dual frequency results
  • LEVEL 1 CLASSIFICATION
  • Adding surface roughness and soil moisture

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THEORETICAL CHARACTERISTICS
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THEORETICAL CHARACTERISTICS ODD NUMBERS OF
REFLECTIONS
Pixels dominated by odd numbers of reflections
are typically characterized by
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THEORETICAL CHARACTERISTICS EVEN NUMBERS OF
REFLECTIONS
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THEORETICAL CHARACTERISTICS DIFFUSE SCATTERING
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SINGLE FREQUENCY INTERPRETATION
The definition of moderate vegetation is a
function of the frequency used when imaging the
scene and can be shown to be related to
the randomness of the orientation and the
thickness of the scattering cylinders relative to
the radar wavelength.
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LEVEL 0 LAND COVER CHARACTERIZATION DUAL
FREQUENCY INTERPRETATION
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LEVEL 1 LAND COVER CHARACTERIZATION
  • The next step is to further subdivide the bare
    surface class into five classes
  • This is done based on the dielectric constant and
    the roughness of the bare surface
  • The following classes are defined
  • Dry bare surfaces dielectric constant lt 6
  • Damp bare surfaces 6 lt dielectric constant lt 11
  • Wet bare surface 11 lt dielectric constant lt 15
  • Saturated surface / open water dielectric
    constant gt 15
  • Exposed rock surface 6 lt dielectric constant lt
    8, rms height gt 6 cm
  • The soil moisture algorithm published by Dubois
    et al. is used

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CLOUDES DECOMPOSITION THEOREM
  • Cloude showed that a general covariance matrix
    can be decomposed as follows
  • Here, are the eigenvalues of the
    covariance matrix, are its
    eigenvectors, and means the adjoint
    (complex conjugate transposed) of .
  • In the monostatic (backscatter) case, the
    covariance matrix has one zero eigenvalue, and
    the decomposition results in at most three
    nonzero covariance matrices.

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CLOUDES DECOMPOSITION THEOREM
  • Also useful in our discussions later is Cloude's
    definition of target entropy,
  • where
  • As pointed out by Cloude, the target entropy is a
    measure of target disorder, with for
    random targets and for simple
    (single) targets.

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CLOUDES DECOMPOSITION THEOREM AZIMUTHALLY
SYMMETRIC NATURAL TERRAIN
  • Borgeaud et al. showed, using a random medium
    model, that the average covariance matrix for
    azimuthally symmetrical terrain in the monostatic
    case has the general form
  • where
  • The superscript means complex conjugate, and
    all quantities are ensemble averages. The
    parameters and all depend on the
    size, shape and electrical properties of the
    scatterers, as well as their statistical angular
    distribution.

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CLOUDES DECOMPOSITION THEOREM AZIMUTHALLY
SYMMETRIC NATURAL TERRAIN
  • The eigenvalues of are
  • Note that the three eigenvalues are always real
    numbers greater than or equal to zero.

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CLOUDES DECOMPOSITION THEOREM AZIMUTHALLY
SYMMETRIC NATURAL TERRAIN
  • The corresponding three eigenvectors are

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CLOUDES DECOMPOSITION THEOREM AZIMUTHALLY
SYMMETRIC NATURAL TERRAIN
  • On the previous page we used the shorthand
    notation
  • We note that is always positive. Also note
    that we can write
  • where
  • Since is always positive, it follows that
    the ratio of to is always negative.
    This means that the first two eigenvectors
    represent scattering matrices that can be
    interpreted in terms of odd and even numbers of
    reflections.

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CLOUDE'S DECOMPOSITION THEOREMRANDOMLY ORIENTED
DIELECTRIC CYLINDERS
  • In general, the scattering matrix of a single
    dielectric cylinder oriented horizontally can be
    written as
  • where and are complex numbers whose
    magnitudes and phases are functions of cylinder
    dielectric constant, diameter and length.
  • Assuming a uniform distribution in angles about
    the line of sight, one can easily show that the
    resulting average covariance matrix for the
    monostatic case has the following parameters

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CLOUDE'S DECOMPOSITION THEOREMRANDOMLY ORIENTED
DIELECTRIC CYLINDERS
  • The eigenvalues are
  • The corresponding three eigenvectors are

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CLOUDE'S DECOMPOSITION THEOREMRANDOMLY ORIENTED
DIELECTRIC CYLINDERS
  • In the thin cylinder limit, , and we find
    that
  • In this case, equal amounts of scattering is
    contributed by the matrix that resembles
    scattering by a sphere and by the cross-polarized
    return, although a significant fraction of the
    total energy is also contained in the second
    matrix, which resembles a metal dihedral corner
    reflector.
  • The entropy in this case is 0.95 indicating a
    high degree of target disorder or randomness.
  • Note that the unsupervised classification scheme
    would classify this as diffuse scattering.

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CLOUDE'S DECOMPOSITION THEOREMRANDOMLY ORIENTED
DIELECTRIC CYLINDERS
  • In the thick cylinder limit, and we
    find that
  • In this case, only one eigenvalue is non-zero,
    and the average covariance matrix is identical to
    that of a sphere.
  • The entropy is 0, indicating no target
    randomness, even though we have calculated the
    average covariance matrix for randomly oriented
    thick cylinders!
  • The explanation for this result lies in the fact
    that when the cylinders are thick, the single
    cylinder scattering matrix becomes the identity
    matrix, which is insensitive to rotations.
  • Note that the unsupervised classification scheme
    would classify this as odd numbers of reflections.

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CLOUDE'S DECOMPOSITION THEOREMRADAR THIN
VEGETATION INDEX
  • Using the result for a cloud of randomly oriented
    thin cylinders, we note that
  • We now define a radar thin vegetation index (RVI)
    as
  • We expect RVI to vary between 0 and 1.

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CLOUDE'S DECOMPOSITION THEOREMRADAR THIN
VEGETATION INDEX
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CLOUDE'S DECOMPOSITION THEOREM EXAMPLE
VEGETATED CLEARCUT AREA
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CLOUDE'S DECOMPOSITION THEOREM EXAMPLE
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CLOUDES DECOMPOSITION THEOREM
  • Advantages
  • Rigorous mathematical technique
  • Provides quantitative information about
    scattering mechanisms
  • Disadvantages
  • Not physically based
  • Interpretation of results not unique
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