LiDAR Backscattering and Vegetation Structure Analysis

 
Backscattering of individual LiDAR pulses explained
by photogrammetrically derived vegetation structure
Ilkka Korpela, Aarne Hovi, Lauri Korhonen
UH
 and UEF
 
March13, 2013
OH
ES seminar
 
Background
Pulsed LiDAR sensors
 use time-stamped photons, short pulses
 are ranging devices
 are designed for topographic applications
 currently use a single 
 and divergence
 
1. Leica ALS60, GPS/IMU & electronics.
2. Oscilloscopes for the AD conversion
 
Some basic features
 
 Overall HOT-SPOT view-illumination geometry, 
low 
.
 Transmitted pulse ~  P(t), t = 0...10 ns; stability is essential for radiometry
 iFOV ~ some mrads, 
(Q how is the iFOV weight function?)
 beam divergence 0.1-0.3 mrad
 Received P has P
Sun
. Through a BPF and an aperture. (SNR)
 Receiver has a certain response; mapping input to output
 Signal has noise (speckle, photodiode, circuts, AD-conversion)
 
Aperture  of an ALS50-ii sensor. Oscillating mirror in
resting position, collimating lens on the right.
 
Intensity
 
Perpendicular dist from cables, m
 
Time-stamped photons on a deflected, yet known path
 
 scan zenith angles 0-20
 
 mirror angle; GNSS / imu
 Pulse path < 0.2-0.4 m in XY, < 0.1 m in Z
 Gaussian PSF
 
Hemispherical – conical reflectance factors @ 900 nm vs.
1064 nm backscattering (intensity)
 
’Flat’; 
 90 
; larger than footprint -surfaces
 
Vicarious refl. calibration for well-defined surfaces
 
grass
 
fine sand
 
old asphalt
 
bitumen
 
LiDAR – challenging radiometry in vegetation
 
Birch
 
Pine
 
Spruce
 
 
 
 
Single pulse ~ stochastic
 
Multiple pulses ~ structure, gaps,
joint distributions , spatial
dependencies, ...
=> constrain ill-posed  nature
 
Wafeform sampling – amplitude sequences
 
Waveform, WF(t) is the output, affected
by the system response, mm.
Reflectance properties and orientation of
the surface(s); their density and spatial
configuration in the iFOV of P(t)  + ’noise’
=> contributions to WF(t)
 
WFs ’tell more’ about the volumetric
scattering than discrete peak amplitude
data.
 
Experimental research
 
LiDAR pulse
 
Nominal scale
* mature trees
* understory trees
* forest floor flora
* mire flora samples
Ratio scale?
 
Viewing the pulse from
its tail; 
what can we see
and learn?
 
Photogrammetry in the forest
 
Geometry was essential
 
Geometry: 3D system of the images
 transformation to the 3D system
of the LIDAR data
 
XY
known
 
XY
known
 
XY
known
 
Z
LiDAR (known)
 
Photogrammetric XYZ +
(
X, 
Y, 
Z, rotation about Z) 
XYZ of LiDAR data
 
Remnant offsets < 5
10 cm
 
Camera
positions
 
Remaining geometric LiDAR inaccuracy
* Between-strip offsets and drifts
* Short-term ’noise’
 
 
 XY strip adjustment
     (local offset removal) using
     footprint silhouettes
     measured from the pulse
     tail -images, shifted ones.
      Correction for a site and
      LiDAR Strip.
 
Silhouette – backscatter strength
correlation peaked at some xy offset
 
XY LiDAR strip adjustment with detached branches
 
Silhouette area vs. Backscattering
 
Fig. 8b.
 Dependence between non-weighted relative silhouette area
(0-1) and the intensity of the first return in the 60-yr-old pine stand.
The figure shows data from a 1-km ALS60 strip (2012) and a 750-m
Riegl LMS-Q680i strip that had been found the best xy-match.
 
Silhouette area vs. Backscattering
 
Smallest echo/WF triggering targets?
 
Some notes
on results
 
 Close-range photogrammetry is feasible, an alternative to TLS (direct spherical).
 in-situ strip adjustment with branches,yes, but don’t recommend
 Silhouette explains 50
90% of signal level (shallow targets, single species)
 Smallest objects in the upper canopy triggering an observation can be quite small
 Could not verify that E (W/m2) has a Gaussian spread across the footprint.
 Calibration for ’real silhouette’ –> CC/LAI modeling
 What scatterers  contributed to the WF,  observable, to some degree
 
What next?
 Experimenting is tedious, slow and expensive, yet needed
 A good simulator would provide guidance (Aarne’s talk), but
   that is tedious too (basic data on scattering, morphology)
Interesting topics to look at (airborne LiDAR)
 Is the (long-term goal) idea of synthetic training data
  (imputation of LiDAR features) feasible with simulators?
 Multidivergent LiDAR data; better probing of canopy structure?
 WF analysis in  tree species recognition, species is bottleneck
 How far from optimal are the current sensors?
 Role of passive multispectral data to be combined?
 
Thanks!
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Exploring the intricacies of LiDAR pulse backscattering in relation to vegetation structure analysis using photogrammetry-derived data. Discussing the technical aspects of pulsed LiDAR sensors, hot-spot view geometry, time-stamped photons, vicarious reflectance calibration, and challenges in radiometry within vegetation. Emphasizing waveform sampling, amplitude sequences, and their significance in understanding volumetric scattering.

  • LiDAR
  • Backscattering
  • Vegetation Structure
  • Photogrammetry
  • Radiometry

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  1. Backscattering of individual LiDAR pulses explained by photogrammetrically derived vegetation structure Ilkka Korpela, Aarne Hovi, Lauri Korhonen UH and UEF March13, 2013 OH ES seminar

  2. Background Pulsed LiDAR sensors use time-stamped photons, short pulses are ranging devices are designed for topographic applications currently use a single and divergence r4 r3 r2 r1 Clock Laser PD WF digitizer AGC / amplifier 1. Leica ALS60, GPS/IMU & electronics. 2. Oscilloscopes for the AD conversion

  3. Some basic features Overall HOT-SPOT view-illumination geometry, low . Transmitted pulse ~ P(t), t = 0...10 ns; stability is essential for radiometry iFOV ~ some mrads, (Q how is the iFOV weight function?) beam divergence 0.1-0.3 mrad Received P has PSun. Through a BPF and an aperture. (SNR) Receiver has a certain response; mapping input to output Signal has noise (speckle, photodiode, circuts, AD-conversion) Aperture of an ALS50-ii sensor. Oscillating mirror in resting position, collimating lens on the right.

  4. Time-stamped photons on a deflected, yet known path scan zenith angles 0-20 mirror angle; GNSS / imu Pulse path < 0.2-0.4 m in XY, < 0.1 m in Z Gaussian PSF Intensity Perpendicular dist from cables, m

  5. Vicarious refl. calibration for well-defined surfaces grass fine sand old asphalt bitumen Hemispherical conical reflectance factors @ 900 nm vs. 1064 nm backscattering (intensity) Flat ; 90 ; larger than footprint -surfaces

  6. LiDAR challenging radiometry in vegetation Pine Birch Spruce Single pulse ~ stochastic Multiple pulses ~ structure, gaps, joint distributions , spatial dependencies, ... => constrain ill-posed nature

  7. Wafeform sampling amplitude sequences Waveform, WF(t) is the output, affected by the system response, mm. Reflectance properties and orientation of the surface(s); their density and spatial configuration in the iFOV of P(t) + noise => contributions to WF(t) WFs tell more about the volumetric scattering than discrete peak amplitude data.

  8. Experimental research Nominal scale * mature trees * understory trees * forest floor flora * mire flora samples Ratio scale? Viewing the pulse from its tail; what can we see and learn?

  9. Photogrammetry in the forest

  10. Geometry was essential

  11. Geometry: 3D system of the images transformation to the 3D system of the LIDAR data Photogrammetric XYZ + ( X, Y, Z, rotation about Z) XYZ of LiDAR data Remnant offsets < 5 10 cm Camera positions XYknown XYknown XYknown ZLiDAR (known)

  12. Remaining geometric LiDAR inaccuracy * Between-strip offsets and drifts * Short-term noise XY strip adjustment (local offset removal) using footprint silhouettes measured from the pulse tail -images, shifted ones. Correction for a site and LiDAR Strip.

  13. XY LiDAR strip adjustment with detached branches Silhouette backscatter strength correlation peaked at some xy offset

  14. Silhouette area vs. Backscattering Fig. 8b. Dependence between non-weighted relative silhouette area (0-1) and the intensity of the first return in the 60-yr-old pine stand. The figure shows data from a 1-km ALS60 strip (2012) and a 750-m Riegl LMS-Q680i strip that had been found the best xy-match.

  15. Silhouette area vs. Backscattering

  16. Smallest echo/WF triggering targets? Adjacent path Pseudoechoes First echo or start-of-WF- recording

  17. Some notes on results Close-range photogrammetry is feasible, an alternative to TLS (direct spherical). in-situ strip adjustment with branches,yes, but don t recommend Silhouette explains 50 90% of signal level (shallow targets, single species) Smallest objects in the upper canopy triggering an observation can be quite small Could not verify that E (W/m2) has a Gaussian spread across the footprint. Calibration for real silhouette > CC/LAI modeling What scatterers contributed to the WF, observable, to some degree

  18. What next? Experimenting is tedious, slow and expensive, yet needed A good simulator would provide guidance (Aarne s talk), but that is tedious too (basic data on scattering, morphology) Interesting topics to look at (airborne LiDAR) Is the (long-term goal) idea of synthetic training data (imputation of LiDAR features) feasible with simulators? Multidivergent LiDAR data; better probing of canopy structure? WF analysis in tree species recognition, species is bottleneck How far from optimal are the current sensors? Role of passive multispectral data to be combined?

  19. Thanks!

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