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Wavelet Analysis of Low Observable Targets Within Sea Clutter

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Wavelet Analysis of Low Observable Targets Within Sea Clutter. G Davidson,H D Griffiths ... Aim is to detect low observable, slow moving targets (debris, ships, ... – PowerPoint PPT presentation

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Title: Wavelet Analysis of Low Observable Targets Within Sea Clutter


1
Wavelet Analysis of Low Observable Targets Within
Sea Clutter
  • G Davidson,H D Griffiths
  • University College London

2
Overview
  • Aim is to detect low observable, slow moving
    targets (debris, ships, others) in heavy sea
    clutter, within clutter Doppler spectrum.
  • 3GHz and 9GHz real aperture, experimental
    multifunction radars at metre resolution
    (QinetiQ).
  • Either the sea surface or the observing platform
    is moving and, this non-stationary velocity
    spectrum can mask targets of unknown varying
    velocity.
  • Strong clutter backscatter complicates CFAR
    detection. Doppler spectrum is analysed by a
    Wavelet transform to minimise the uncertainty in
    both time and velocity.
  • Clutter returns appear to consist of discrete
    scatterers with a characteristic lifetime.
    Thresholding this scatterer lifetime reveals a
    real target in real clutter that was difficult to
    detect in Intensity and Doppler.
  • This is not the correlation time of the surface.

3
Medium Sea Surface
4.3 metres Significant Wave Height
  • Whitecaps suggest different scattering event

4
Heavy Sea Surface
6.1 metres Significant Wave Height
  • Heavy seas cause shadowing

5
Recorded dB Backscatter
6
Non-Stationary Doppler
- Velocity
Time
Dsitribution Measure
- Velocity
Proportion Above Noise
- Velocity
7
Event Based Processing
  • Some justification for considering the
    backscatter as discrete events these are more
    obvious in Doppler.
  • Over sufficient time (30s), these events average
    out to a stable Doppler spectrum.
  • At shorter time scales (1s) identifying
    individual events may be useful for target
    detection.
  • But neither the velocity or the lifetime of the
    scatterers can be known a priori. Windowed
    Fourier is not well suited to this.
  • Wavelet Transform is useful for this case as it
    maintains constant uncertainty in time-frequency.
  • WT gives optimally smoothed Doppler Velocity-Time
    image of the sea surface.

8
Fourier vs Wavelet Transform
Frequency
Time
Time
  • Fourier
  • Arbitrary time window
  • Window determines frequency
  • Problems at boundaries
  • Wavelet
  • Forced constant ???t
  • Can choose frequency subset
  • Convolution over all time

9
Wavelet Filter Bank
  • Filter width proportional to frequency, log
    spaced filter bank

10
Simulated Target (No Noise)
FT1
FT3
Time
Time
Velocity Measure
FT2
WT
  • For stable, well defined signals FFT is best,
    but
  • At low PRF (1 second of 256 samples) the optimum
    window size for the Fourier transform (F1, F2,
    F3) is unknown.
  • The Wavelet transform (WT) gives an acceptable
    view.

11
Target Parameters
Velocity
Time
Intensity
  • Target simulated from observed parameters
    (Swerling 1-2)

12
Wavelet Maxima
Full Doppler via FFT
Power
Velocity
Doppler via WT
Velocity
Time
  • Single FFT Doppler is misleading, but WT maxima
    useful

13
Real Clutter/Simulated Target
Real Clutter 0dB Sim. Target (within clutter
spectrum)
Time
Real Clutter
Time
  • Doppler is misleading, but WT maxima useful

14
Detection Scheme
  • Instantaneous WT-Doppler spectrum is smooth
    (red).
  • Dominant event can be isolated without any
    thresholding
  • Length of dominant event (arrow) related to
    individual scatterer lifetime
  • Threshold this to reveal target

15
Lifetime Distribution
20 minutes of data 3GHz, VV 156Hz prf Grazing
angle
Real Data 0dB Sim.Target
Log10 Complementary Cumulative Distribution
Real Data
Scatterer Lifetime
  • Exponential distributed scatterer lifetime,
    agrees with Doppler spectral lineshape models
    Lee et al.

16
Doppler Real ClutterTarget
9GHz, VV 6m Range Resolution 500Hz
prf Significant wave ht. 2.4m 8ms-1 wind 1.5?
angle (grazing)
dB Intensity
17
Intensity Real ClutterTarget
Arbitrary Intensity
18
WT Real ClutterTarget
Lifetime
19
Conclusions
  • The sea surface backscatter can be considered as
    a collection of individual scattering events.
  • Event velocity and lifetime unknown so wavelet
    analysis is easier than FFT Doppler especially
    for fading targets with velocity varying over 1
    second.
  • WT minimises uncertainty in time and velocity.
  • Dominant scatterer lifetime can be easily
    measured, distribution is exponential in
    agreement with models.
  • Thresholding the lifetime of scattering events
    suggests targets can be detected within the
    Doppler spectrum. Real data and real target gave
    encouraging results.
  • Obviously, FFT/MTI is better for fast moving
    targets of relatively constant velocity outside
    clutter spectrum. The lifetime of these is
    determined by the range cell size.
  • Not measuring correlation length this averages
    all scatterers together and requires sampling
    window to be chosen.
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