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Optimally Resolving Lambertian Surface Orientation

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Title: Optimally Resolving Lambertian Surface Orientation


1
Optimally Resolving Lambertian Surface Orientation
  • Ioannis Bertsatos
  • Research Advisor Nicholas C. Makris
  • Massachusetts Institute of Technology

2
Motivation
  • Resolve surface slope and shape from intensity
    images corrupted by speckle noise
  • Sonar images of the ocean environment
  • Relative motion between source, surface
  • and receiver results in field fluctuations
  • Optical and radar images of planetary bodies
  • Natural light sources (sun, stars, light bulbs!)
  • Machine vision

Examples
3
Overview
  • Scattering from Rough Surfaces
  • Radiometry, Lambertian Surfaces
  • Measurement Statistics
  • Asymptotic Optimality Conditions
  • 1D Surface Slope Estimation
  • 2D Albedo and Slope Estimation
  • 3D General Surface Orientation Estimation

4
Surface Types
  • Smooth surfaces Specular reflection
  • Rough surface Scattering function
  • (Scale of roughness gt ?incident)
  • Lambertian surfaces perfect diffuse scatterers
  • (All incident energy reflected uniformly)

5
Radiometry
subtended solid angle d?i cos?i dA / r2 ? cos?i
dO
intercepted flux dFi I cos?i dO
irradiance dFi d?i cos?i dA ? Fi Ei cos?i dA

dFi (Li cos?i dO) dA ? Li dEi / (cos?i dO)
Lr dEr / (cos?r dO)
dFr Lr cos?r dO dA
6
dFr Lr d?r dA Lr cos?r dO dA
Total flux reflected
For a Lambertian surface, Lr constant
For non-Lambertian surfaces, ? ?(?i,fi,?r,fr)
7
Approach
  • Sonar images of remote surfaces resolved by a
    pencil beam (2D sonar) array
  • Attain specified design criteria from 2D sonar or
    optical measurements
  • Design specifications are met when both
    conditions are satisfied
  • Estimate becomes unbiased, and attains the
    Cramer-Rao Lower Bound (CRLB)
  • CRLB is within the design specifications

Goals
8
Surface Orientation from Reflected Intensity
  • Lamberts Law
  • Measure
  • Non-linear estimation problem

surface radiance
random
known constant
9
Measurement PDF
  • a a1 aj orientation parameters
  • R R1 R2 Rk RN
  • Rk are Independent Identically Distributed (IID)
    measurements corrupted by signal-dependent noise
    (speckle) due to Circular Complex Gaussian Random
    (CCGR) field fluctuations
  • ltRkgt ? sk(a)
  • µk is a measure of the number of independent
    intensity fluctuations in the measurement Rk
  • Can be interpreted as the signal-to-noise ratio
  • SNR ? ltRkgt2/var(Rk) µk

N. C. Makris, 1997
10
Necessary Conditions for Asymptotic Optimality of
MLE
  • Maximum Likelihood Estimate (MLE)
  • For large sample sizes or SNR, the MLE becomes
    unbiased, and attains the Cramer-Rao Lower Bound
    (CRLB)
  • Using asymptotic expansions of the type
  • We can derive necessary conditions on SNR

for unbiased estimate for minimum variance
estimate
Naftali and Makris, 2001
11
Slope Estimation
  • parameter a ?i
  • lt R gt s(?i) ? cos?i

12
  • To attain design specifications on resolution of
    ?i
  • Determine necessary SNR to achieve unbiased,
    minimum variance estimate, then
  • Specify SNR so that the CRLB is within the design
    specs

13
Illustrative Example
  • For the 1D case, the necessary conditions on SNR
    introduced earlier become
  • If ?i 10o, then in order to achieve an
    unbiased, minimum variance estimate, we require
    that
  • SNRv is the limiting value. For SNR ? SNRv the
    estimate asymptotically attains minimum variance,
    so that
  • If the design criteria specify a maximum variance
    of 1o, then we require that
  • If, instead, ?i 80o, then to satisfy the same
    design criteria we now only require that

14
2D Parameter estimate Albedo and Slope
  • Incident directions must be distinct so that 2
    independent equations exist for ? and ?i
  • 2 unknowns incident angle (?) and albedo (?)
  • Assume s1, s2 as shown
  • It is impossible to invert for both parameters in
    this arrangement
  • s1 cannot be collinear to s2

15
3D Surface Orientation Estimation
  • Define S source matrix
  • ST s1 s2 sk sN
  • lt Rk gt ? sk(a) ? skT n
  • lt R gt ? S n
  • 3 orientation
  • parameters
  • a ?, ?, f, or
  • a ?, p, q, or
  • a nx, ny, nz

16
Incident Directions must be Distinct
  • 3 unknowns 3 illumination vectors
  • If all si are coplanar, then we cannot estimate
  • the orientation
  • parameters
  • Need 3 distinct
  • illumination vectors
  • (i.e. 3 equations) to estimate all the unknowns
  • s1 (s2 ? s3) ? 0 ? si must span some
    volume

all si on this plane
n
17
Illustrative Examples
  • Estimate of a ?, p, q, given
  • Specified
  • Fixed
  • Varying
  • ? 1/p

18
Illustrative Examples
  • Estimate of a ?, ?, f, given
  • ? 1/p
  • In order to achieve an unbiased, minimum variance
    estimation, we require that
  • SNRv is the limiting value. For SNR ? SNRv the
    estimate asymptotically attains minimum variance,
    so that
  • If design criteria require that the maximum
    allowable variance is 1o, then

19
Shallow s1, s2 Variable s3
Steep s1, s2 Variable s3
SNR for minimum variance estimation
SNR for minimum variance estimation
(dB)
(dB)
20
Conclusions
  • Optimality conditions for the estimation of
    Lambertian surface orientation can be derived
    from asymptotic expansions of the MLE.
  • For slope estimation (with known albedo), it is
    shown that it is more efficient to illuminate the
    surface from shallow grazing angles.
  • For 3D estimation it is shown that the incident
    vectors must also span some volume.
  • Given fixed source/illumination vectors spanning
    non-zero volume, it is possible to come up with
    specific SNR conditions, so that any resolution
    criteria for surface orientation are met.

21
Background
  • Stochastic behavior of optical, radar, and
    acoustic fields received from fluctuating sources
    and/or scatterers can be described by Circular
    Complex Gaussian Random (CCGR) statistics
  • Intensity images derived from CCGR fields exhibit
    signal-dependent noise, or speckle
  • Lamberts Law is often appropriate to model
    surface radiant intensity
  • Maximum likelihood estimators (MLE) for
    Lambertian surface orientation are used
  • N. C. Makris, 1997
  • Optimality criteria for MLE are applied
  • Naftali and Makris, 2001

22
Physical Model
  • Assume a planar surface with wave-scale roughness
    in free space. A surface patch of scale gtgt ? is
    resolved. It is characterized by a specific
    orientation wrt a fixed coordinate system
  • Sonar images are obtained a source illuminates
    the target surface and reflected intensity is
    measured at a receiver

Lamberts Law
  • Surface Radiance, L, is defined as radiant power
    in a given direction, per unit solid angle, per
    unit projected area of the source, as viewed from
    the given direction
  • Lambertian surfaces are defined as those surface
    for which, L, is constant throughout space
  • The measured reflected intensity does not depend
    on the observation direction, but contains
    information about the angle of incidence of the
    illumination direction
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