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Title: A1258690354mzibv


1
Assessing the Impact of Structural Effects on the
Radiative Signature of Vegetation J-L.
Widlowski, B. Pinty, T. Lavergne, N. Gobron and
M. Verstraete Methods in Transport Workshop,
11th 16th September 2004, Granlibakken, USA
2
Overview
  • Origin of 3-D signatures in reflectance fields
  • Implications for 1-D RT model inversions
  • Spatial resolution limits for pixel-based
    inversion
  • Using photon spreading to speed-up MC
    simulations of reflectance fields
  • Origin of 3-D signatures in reflectance fields
  • Implications for 1-D RT model inversions
  • Spatial resolution limits for pixel-based
    inversion
  • Using photon spreading to speed-up MC
    simulations of reflectance fields

3
Radiation Transfer in Vegetation Canopies
  • conditioned by two important boundary conditions

At the top of the canopy, zTOC
  • Impinging radiation has a
  • direct and a diffuse component due to
    atmospheric scattering

Ref Govaerts, PhD Thesis, 1996
4
Leaf Optical Properties
  • Leaf reflection and transmission depend
    primarily on wavelength, plant species, growth
    condition, age and position in canopy.

Ref Govaerts et al. (1995) IEEE IGARS95
5
Foliage Structural Properties III
Vegetation foliage features characteristic
leaf-normal distributions, g(OL) with preferred
  • azimuthal orientations, g(fL)

6
Foliage Structural Properties III
In vegetation canopies the extinction coefficient
is directionally variant but wavelength
independent.
7
Foliage Structural Properties III
Extinction coefficient is wavelength independent,
but directionally variant.
For a volume of oriented, finite-sized scatterers
(1-D medium)
se(z, O, O0) ?(z) G(O) O(z, O, O0)
  • Leaf area density m2 / m3
  • Interception probability along O
  • Enhanced return-probability near
    retro-reflection direction

Ref Pinty et al. (1997) JAS Knyazikhin et al.
(1998) JGR
8
Tree Structural Properties
  • Actual trees are very complex, featuring
  • species-specific patterns of
  • foliage distribution
  • leaf orientation
  • crown shape and dimensions
  • branch trunk structures
  • growth processes

9
Canopy Structural Properties
Actual vegetation canopies include location-specif
ic
All of which have an impact on the
surface-leaving reflectance field.
Widlowski et al., 2003, EUR Report 20855
10
Multi-directional surface observations
Different fractionsof soil and foliage
contribute to the surface-leavingradiation if
targetarea is observedfrom different viewing
angles
11
Spectral Contrast between Vegetation Background
Leaf
soil
Reflectance
Wavelength
12
BRF shapes of Heterogeneous Canopies NIR
Sparse
Dense
Medium
Ref Pinty et al. (2004) JGR-Atmosphere
(submitted)
13
Spectral Contrast between Vegetation Background
RED
Soil back- scattering dominates over leaf
scattering in the red
Leaf
soil
Reflectance
Wavelength
14
BRF shapes of Heterogeneous Canopies Red
Sparse
Dense
Medium
Ref Pinty et al. (2004) JGR-Atmosphere
(submitted)
15
The RPV parametric model
BRF(z,O0 O) ?0 MI(k) FHG(T) H (?c)
?0 - controls amplitude level k - controls
bowl/bell shape T - controls forward/backward
scattering ?C - controls hot spot peak
Ref Rahman et al. (1993) JGR
16
The RPV parametric model
BRF(z,O0 O) ?0 MI(k) FHG(T) H (?c)
?0 - controls amplitude level k - controls
bowl/bell shape T - controls forward/backward
scattering ?C - controls hot spot peak
Ref Rahman et al. (1993) JGR
17
Impact of Canopy Structure on surface BRFs
SZA30o
?red
IFOV275 m
350 structurally different canopy architectures
18
Impact of Canopy Structure on surface BRFs
Bell shape
1.5
kred
SZA30o
?red
1.0
IFOV275 m
0.5
Bowl shape
Ref Widlowski et al. (2004), in print, Climatic
Change
19
Overview
  • Origin of 3-D signatures in reflectance fields
  • hot spot effect leaf/tree gap sizes, spectral
    contrast of soil/canopy
  • bowl/bell shape leaf/tree distribution, spectral
    contrast of soil/canopy
  • Implications for 1-D RT model inversions
  • Spatial resolution limits for pixel-based
    inversion
  • Using photon spreading to speed-up MC
    simulations of reflectance fields
  • Origin of 3-D signatures in reflectance fields
  • hot spot effect leaf/tree gap sizes, spectral
    contrast of soil/canopy
  • bowl/bell shape leaf/tree distribution, spectral
    contrast of soil/canopy
  • Implications for 1-D RT model inversions
  • Spatial resolution limits for pixel-based
    inversion
  • Using photon spreading to speed-up MC
    simulations of reflectance fields

20
Matching surface BRFs with 1-D models
Assume you have a set of multi-directional
observations of a surface target and - in
absence of any a priori information regarding its
structure - wish to utilize a 1-D RT model to
retrieve information about that surface target.
Whats the impact of the structural differences
in both models?
Approach Use a large LUT (containing 47000
candidates) spanning the entire domain of
probable 1-D solutions, and find the best
matching candidate under identical conditions of
illumination and viewing.
21
Matching surface BRFs with 1-D models
Find the 1-D surface that is best at mimicking
the reflectance anisotropy of a 3-D target.
Heterogeneous discrete canopy 3-D
Widlowski, 2001, PhD Thesis
22
Matching surface BRFs with 1-D models
Find the 1-D surface that is best at mimicking
the reflectance anisotropy of a 3-D target.
?0 30o
Fitting criteria 7 BRF observations VZA 0, ?25,
?45 ,?60? ?red
Widlowski et al., 2004, JGR - submitted
23
Matching surface BRFs with 1-D models
1-D canopies that perfectly fit the surface
leaving BRFs of a 3-D target may be very accurate
in predicting the albedo but not the canopy
absorption, transmission etc.
Ref Widlowski et al. (2004), JGR, submitted
24
Impact of Canopy Structure on surface BRFs II
Bell shape
1.5
kred
1.0
0.5
Bowl shape
25
Impact of Canopy Structure on surface BRFs II
Leaf area index (LAI)
increases
Ref Pinty et al. (2002) IEEE TGRS
26
Impact of Canopy Structure on surface BRFs II
Ref Pinty et al. (2002) IEEE TGRS
27
Impact of Canopy Structure on surface BRFs
350 forest scenes
In general, the shape of the reflectance
anisotropy of a pure 3-D target tends to be
different from that of its IPA or 1-D
homologue k3-D ? k1-D

A 1-D canopy having a quasi-identical
reflectance anisotropy shape as a 3-D target is
almost certainly not its homologue!
Widlowski et al., 2004, JGR, submitted
28
Matching surface BRFs with 1-D models
  • 3-D surface targets tend to exhibit enhanced
    bell-shaped BRF patterns wrt. their 1-D
    homologues
  • higher nadir BRFs
  • lower BRFs at large VZA

29
Matching surface BRFs with 1-D models
  • 1-D canopy capable of mimicking BRFs of 3-D
    target consequently has
  • enhanced soil albedo, a1D
  • reduced LAI (as LAI3D increases)
  • reduced single scattering
  • albedo, ?1D (as LAI3Dincreases)
  • increase leaf interception at large VZA (as
    LAI3Dincreases)

Ref Widlowski et al. (2004), JGR, submitted
30
Matching surface BRFs with 1-D models
  • 1-D canopy capable of mimicking BRFs of 3-D
    target consequently has
  • enhanced soil albedo, a1D
  • reduced LAI (as LAI3D increases)
  • reduced single scattering
  • albedo, ?1D (as LAI3Dincreases)
  • increase leaf interception at large VZA (as
    LAI3Dincreases)

1-D leaf normal distribution
Ref Widlowski et al. (2004), JGR, submitted
31
Matching surface BRFs with 1-D models
The state variables of a 1-D canopy that is
capable of mimicking the reflectance anisotropy
of a 3-D target have to be interpreted
cautiously to account for 1) the structural
differences with the 3-D target, and 2) the lack
of information regarding canopy absorption
transmission.
Ref Widlowski et al. (2004), JGR, submitted
32
Overview
  • Origin of 3-D signatures in reflectance fields
  • hot spot effect leaf/tree gap sizes, spectral
    contrast of soil/canopy
  • bowl/bell shape leaf/tree distribution, spectral
    contrast of soil/canopy
  • Implications for 1-D RT model inversions
  • Pure 1D approach requires further interpretation
    of state variables
  • Given 3-D structure effective state variables can
    be found for 1-D
  • Spatial resolution limits for pixel-based
    inversion
  • Using photon spreading to speed-up MC
    simulations of reflectance fields
  • Origin of 3-D signatures in reflectance fields
  • hot spot effect leaf/tree gap sizes, spectral
    contrast of soil/canopy
  • bowl/bell shape leaf/tree distribution, spectral
    contrast of soil/canopy
  • Implications for 1-D RT model inversions
  • Pure 1D approach requires further interpretation
    of state variables
  • Given 3-D structure effective state variables can
    be found for 1-D
  • Spatial resolution limits for pixel-based
    inversion
  • Using photon spreading to speed-up MC
    simulations of reflectance fields

33
Spatial resolution limit
  • RT model based interpretation of multi-angular
    BRF measurements of individual pixels is limited
    to spatial resolutions where net horizontal
    fluxes are close to zero radiatively independent
    volume
  • What are the typical distances that photons
    travel laterally in between their points of entry
    and exit at the top of the canopy?
  • At what spatial resolution do horizontal fluxes
    affect pixel-based model inversions?

34
Horizontal divergence of radiation
  • What are the typical distances that photons
    travel between their points of entry and exit at
    the top of the canopy?

Red
NIR
Widlowski et al., 2004, JGR, submitted
35
Horizontal divergence of radiation
  • What are the typical distances that photons
    travel between their points of entry and exit at
    the top of the canopy?
  • canopy structure controls extinction
    coefficient and the most likely distance, d

Red - NIR
  • multiple-scattering makes photons in NIR travel
    longer distances than in red
  • 0.5 (1 ) of all photons in red (NIR) have d
    lt 100m

Widlowski et al., 2004, JGR, submitted
36
Assessment of Horizontal Fluxes
  • What are the typical flux quantities that
    travel through the lateral sides of some canopy
    volume, V at a spatial resolution, S?

f0
O0
f0
zTOC
V
S
37
Magnitude of Net Horizontal Flux Components
Red
Maximum minimum flux across the
lateral sides of voxel that are
perpendicular to f0
?0 0o, 15o, 30o, 55o
3D forest with 300 stem/ha
Widlowski et al., 2004, JGR, submitted
38
Magnitude of Net Horizontal Flux Components
Red
Maximum minimum flux across the
lateral sides of voxel that are
perpendicular to f0
Maximum minimum flux across the
lateral sides of voxel that are parallel
to f0
ve values ? more photons enter
voxel than exit
-ve values ? more photons exit voxel
than enter
?0 0o, 15o, 30o, 55o
3D forest with 300 stem/ha
Widlowski et al., 2004, JGR, submitted
39
Magnitude of Total Net Horizontal Flux
?0 30o
?0 60o
maximum and minimum net horizontal
flux into voxel
maximum and minimum net horizontal
flux into voxel
ve values ? more photons enter
voxel than exit
? NIR, Red
-ve values ? more photons exit voxel
than enter
3D forest with 300 stem/ha
Widlowski et al., 2004, JGR, submitted
40
Impact of Net Horizontal Fluxes
Depends on magnitude ofsurface-leaving radiation!
Red
?0 30o
31m
18m
Since ?FHor is larger in red than NIR, and F?
larger inNIR than red look at red
5
For sensor with BRF accuracy of 5 in red
spatial resolution gt 31 mrequired for
pixel-basedBRF interpretation
-5
29m
18m
Tree density 300, 600, 1200, 1800 stem/ha
Widlowski et al., 2004, JGR, submitted
41
Overview
  • Origin of 3-D signatures in reflectance fields
  • hot spot effect leaf/tree gap sizes, spectral
    contrast of soil/canopy
  • bowl/bell shape leaf/tree distribution, spectral
    contrast of soil/canopy
  • Implications for 1-D RT model inversions
  • Pure 1D approach requires interpretation of
    state variables
  • Given 3-D structure effective state variables can
    be found for 1-D
  • Spatial resolution limits for pixel-based
    inversion
  • Stay above 30 m for 5 sensor accuracy
  • Using photon spreading to speed-up MC
    simulations of reflectance fields
  • Origin of 3-D signatures in reflectance fields
  • hot spot effect leaf/tree gap sizes, spectral
    contrast of soil/canopy
  • bowl/bell shape leaf/tree distribution, spectral
    contrast of soil/canopy
  • Implications for 1-D RT model inversions
  • Pure 1D approach requires interpretation of
    state variables
  • Given 3-D structure effective state variables can
    be found for 1-D
  • Spatial resolution limits for pixel-based
    inversion
  • Stay above 30 m for 5 sensor accuracy
  • Using photon spreading to speed-up MC
    simulations of reflectance fields

42
Raytran a 3-D Monte Carlo ray-tracing model
  • Raytran describes the radiation transfer on a
    ray-by-ray basis, following individual
    ray-trajectories from their source through all
    relevant interactions until an eventual
    absorption or exiting from the simulated scene
    occurs.
  • Information is subsequently extracted from
    ray paths BRFi pNi / N?Oi

Ref Govaerts (1996) EU Report 16394 EN
43
Improving the speed of the Raytran model
Only 7 (18 ) of injected rays in the red (in
NIR) contribute towards estimation of surface
albedo substantially less for individual BRFs.
  • Enhance the contribution of individual photons in
    Raytran model via the photon spreading variance
    reduction technique
  • Ross Marshak, 1988
  • Calculation of Canopy Bidirectional Reflectance
    Using the Monte Carlo Method
  • absorption is probabilistic (photons carry
    weights)
  • fictitious flight towards detectors yields BRF
  • Thompson Goel, 1998
  • Two Models for Rapidly Calculating Bidirectional
    Reflectance of Complex Vegetation Scenes Photon
    Spread (PS) model and Statistical Photon Spread
    (SPS) Model
  • absorption is deterministic (Monte Carlo
    scheme)
  • photon spreading towards detectors yields BRF

44
Developing the Rayspread model
Principle of Rayspread.
At each physical interaction in the main ray
path, a secondary spreading ray is aimed at
each sensor. The probability of reaching the
detector without physical interactions is
calculated and added to its radiance counter.
45
Developing the Rayspread model
Principle of Rayspread.
At each physical interaction in the main ray
path, a secondary spreading ray is aimed at
each sensor. The probability of reaching the
detector without physical interactions is
calculated and added to its radiance counter.
P3
P2
P4
P1
46
Developing the Rayspread model
Principle of Rayspread.
At each physical interaction in the main ray
path, a secondary spreading ray is aimed at
each sensor. The probability of reaching the
detector without physical interactions is
calculated and added to its radiance counter.
P3
P2
P4
P1
P5
Each sensor has already 2 (1) contribution(s)
47
Developing the Rayspread model
Principle of Rayspread.
At each physical interaction in the main ray
path, a secondary spreading ray is aimed at
each sensor. The probability of reaching the
detector without physical interactions is
calculated and added to its radiance counter.
Pr(x,y,z,q0,f0d) Prsurf.Refl.(q0,f0q1,f1)
Prtravel(x,y,zd)
Prsurf. Refl.(q0,f0q1,f1) Lambertian, specular,
etc.
n
q0
q1
x,y,z
48
Developing the Rayspread model
Principle of Rayspread.
At each physical interaction in the main ray
path, a secondary spreading ray is aimed at
each sensor. The probability of reaching the
detector without physical interactions is
calculated and added to its radiance counter.
Pr(x,y,z,q0,f0d) Prsurf.Refl.(q0,f0q1,f1)
Prtravel(x,y,zd)
Prsurf. Refl.(q0,f0q1,f1) Lambertian, specular,
etc.
n
d
q0
d
q1
l
M
v
x,y,z
Prtravel(x,y,zd)0
Prtravel(x,y,zd)f(l,v,M)
49
Developing the Rayspread model
Principle of Rayspread.
At each physical interaction in the main ray
path, a secondary spreading ray is aimed at
each sensor. The probability of reaching the
detector without physical interactions is
calculated and added to its radiance counter.
On the sensors side
50
Developing the Rayspread model
50mx50m forest scene. 250 trees. 153000 objects

Raytran 400 million rays TNIR 16h20
(980mn) TRED 8h24 (504mn)
Rayspread 50,000 rays TNIR 15mn TRED 10mn
51
Developing the Rayspread model
RAdiation transfer Model Intercomparison exercise
(RAMI)
Mean-0.01
  • Rayspread Linux Cluster
  • 10 nodes (PIII 450 / 380MB Ram)
  • 52 RAMI Homogeneous
  • (Turbid and Discrete) experiments.

Speed-up roughly 100
52
Overview
  • Origin of 3-D signatures in reflectance fields
  • hot spot effect leaf/tree gap sizes, spectral
    contrast of soil/canopy
  • bowl/bell shape leaf/tree distribution, spectral
    contrast of soil/canopy
  • Implications for 1-D RT model inversions
  • Pure 1D approach requires interpretation of
    state variables
  • Given 3-D structure effective state variables can
    be found for 1-D
  • Spatial resolution limits for pixel-based
    inversion
  • Stay above 30 m for 5 sensor accuracy
  • Using photon spreading to speed-up MC
    simulations of reflectance fields
  • Speed-up by a factor of 100

53
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