SAR Tomographic imaging of tropical forests:
P and L-band
(1) Centre d’Ėtudes Spatiales de la Biosphère (CESBIO), Toulouse, France
(2) Dipartimento di Elettronica, Informazione e Bioingegneria, Politecnico di Milano, Italy
Dinh Ho Tong Minh1, Thuy Le Toan1, Stefano Tebaldini2, Fabio Rocca2
Frascati, PolInSAR 2015 – 1st BIOMASS Science workshop, 29 January
Airborne tomography TropiSAR campaign in Paracou and Nouragues
Data from TropiSAR 2009 – ESA
System Sethi - ONERA
Scene Tropical forests forest height : 20-40 m Biomass : 200-600 t/ha
Paracou
Nouragues
French Guiana
P-band SAR BIOMASS mission
P/L-Band 6 tracks Full-Pol 9-10 h, 24/08/2009
P-Band 5 tracks Full-Pol
TomoSAR (SAR Tomography)
x
y
z
o
New method Gain new knowledge
Ground spectrum
Heig
ht
[m]
Azimuth [m]
1000 1500 2000 2500 3000 3500 4000 4500 5000-20
0
20
40
60
Volume spectrum
Heig
ht
[m]
Azimuth [m]
1000 1500 2000 2500 3000 3500 4000 4500 5000-20
0
20
40
60
0 0.5 1
vvgg
K
k
kkk RCRCRCW 1
Jointly interferometry - polarimetry to gain vertical (altimetry) information
Ho Tong Minh et al., TGRS 2014
P-band BIOMASS: TomoSAR
(Tropical forest : Nouragues )
SAR Tomography over forested areas
sin2 maxb
rz
SAR Tomography (TomoSAR)
3D imaging of the forest structure
P-band TomoSAR yields the forest vertical structure
even in the tropical forests.
Nouragues, French Guiana , HV
Heig
ht [m
]
1500 4000
20
40
60
0
Paracou, French Guiana , HV
Range [m]
Azimuth [m]
Heig
ht [m
]
20
40
60
0
5500 4500
db
rjxrPxry nn
4exp,,,
Complex reflectivity along cross-range () direction and signal along image index are related by a Fourier Transform.
P-band tomographic analysis
Significant scattering contributions are observed at the canopy level in HH polarization, whereas this volume scattering contribution is dominating in HV polarization.
P-band TomoSAR to understand Scattering Mechanisms
The forest height can be readily determined, and it matches with LiDAR height.
Algorithm: Coherent focusing
HH channel
Heig
ht
[m]
4600 4800 5000 5200 5400 5600 5800
0
20
40
60
LiDAR height
HV channel
Heig
ht
[m]
4600 4800 5000 5200 5400 5600 5800
0
20
40
60
LiDAR height
0 0.1 0.2 0.3 0.4 0.5 0.6 0.7 0.8 0.9 1
Slant range [m]
P-band
P-band
4600 4800 5000 5200 5400 5600 5800-20
0
20
Heig
ht
[m]
Topography
Original image
Gro
un
d r
ange
[m
]
2000
4500
1 2
3
4 5
6
7 8
9
10
11 12
13
14
15
16
a
SAR resolution cell Intensity (dB) Intensity - biomass
Paracou
Original image, rP = 0.37, Slope = 0.51
1 2 3 4 5 6 -20
-15
-10
-5
0
g HV
[d
B]
100 t/ha
-20 -15 -10 -5 0 5 200 t/ha - 600 t/ha Best fit line in-situ Paracou in-situ Nouragues
a
0m
30m
TomoSAR resolution cell
30 m layer
Azimuth [m]
Gro
un
d r
ange
[m
]
500 3500
2000
4500
Height is always measured with respect to terrain elevation. Layer 30m, rP = 0.75, Slope = 1.84
1 2 3 4 5 6 -20
-15
-10
-5
0
g HV
[d
B]
15m
TomoSAR to understand how to retrieve biomass
Ho Tong Minh et al., TGRS 2014 - RSE 2015
200 t/ha - 600 t/ha
The effects of the ground contribution is minimized. Total AGB at large trees is well represented in 20-40 m layer.
3D Tomographic reconstruction
H ≈ 4000 m B = 125 MHz
Airborne data
1
2
BIOMASS data
H = 650 Km B = 6 MHz
3
Generation of 6 MHz data
2. Degrading the resolution of 125 MHz airborne data through linear filtering (ONERA)
1. Back projection of airborne tomographic data onto BIOMASS geometry.
Two different processing approaches have been considered :
Impulse Response Function
Simulated Orbits +
(6 MHz filtering airborne geometry)
(6 MHz simulation spaceborne geometry)
Implications : BIOMASS @ 6 MHz Simulation
6 MHz spaceborne geometry
0 100 200 300 400 500 600 0
100
200
300
400
500
600
In situ above-ground biomass (t/ha)
Ret
riev
ed b
iom
ass
(t/h
a)
RMSE = 35.02 (t/ha) = 9.86 (%)
Observation 6 MHz airborne geometry
0 100 200 300 400 500 600 0
100
200
300
400
500
600
In situ above-ground biomass (t/ha)
Re
trie
ved
bio
mas
s (t
/ha)
RMSE = 35.39 (t/ha)
= 9.97 (%)
0 100 200 300 400 500 600 0
100
200
300
400
500
600
RMSE = 18.74 (t/ha)
= 5.28 (%)
In situ above-ground biomass (t/ha)
Re
trie
ved
bio
mas
s (t
/ha)
Observation 125 MHz
rP = 0.94
R2 = 0.89
p << 0.00001
rP = 0.83
R2 = 0.69
p = 0.00008
rP = 0.84
R2 = 0.70
p = 0.00005
D. Ho Tong Minh, S. Tebaldini, F. Rocca, T. Le Toan, L. Villard, and P. Dubois-Fernandez, "Capabilities of BIOMASS Tomography for Investigating Tropical Forests," Geoscience and Remote Sensing, IEEE Transactions on , vol.53, no.2, pp.965,975, Feb. 2015
D. Ho Tong Minh, T. Le Toan, F. Rocca, S. Tebaldini, M. Mariotti d’Alessandro, and L. Villard, “Relating P-band SAR tomography to tropical forest biomass”, IEEE Transactions on Geoscience and Remote Sensing, Vol. 52, No. 2, pp. 967-979, Feb. 2014.
Results at 6 MHz in both the spaceborne geometry and the airborne geometry appear to be well consistent with those observed in the 125-MHz case, indicating that the 30-m layer appears to be the most informative about the AGB.
Paracou forest: Plot size 250 m x 250 m
Algorithm: Coherent focusing
L-band tomographic analysis
Penetration of L and P-band signal in a tropical forest
P band
1000 2000 3000 4000 5000 6000 7000 8000
500
1000
1500
2000-3
-2
-1
0
1
2
3
L band
2000 4000 6000 8000 10000 12000 14000
500
1000
1500
2000
2500 -3
-2
-1
0
1
2
3
Co-polar phase HH-VV
Optical image at Paracou – tropical forest
L-band
P-band
0 →
- →
or
HV
Tomogram P-band
Azimuth [m]
1000 1500 2000 2500 3000 3500 4000 4500 5000
0
20
40
60
Tomogram L-band
Azimuth [m]
0
20
40
60
1000 1500 2000 2500 3000 3500 4000 4500 5000
2D Intensity
Azimuth [m]
4500
5000
5500
6000
6500
1000 1500 2000 2500 3000 3500 4000 4500 5000
Algorithm: Capon spectrum
2D Intensity L-band
Azimuth [m]
Sla
nt
range [
m]
6000 6500 7000 7500 8000 8500 9000 9500 10000
4500
5000
5500
6000
Tomogram L-band
Azimuth [m]
Heig
ht
[m]
6000 6500 7000 7500 8000 8500 9000 9500 10000
0
20
40
60
Azimuth [m]
heig
ht
[m]
Tomogram P-band
6000 6500 7000 7500 8000 8500 9000 9500 10000
0
20
40
60
L-band
P-band
L-band
P-band
L and P-band tomographic profiles
Tropical forest : Paracou Boreal forest : Krycklan
0
5
10
15
20
25
30
35
40
-10
-5
0
5
10
Intensity [dB]
Tree top height [m] Topographic slope [°]
-20
-15
-10
-5
0
5
10
-20
-15
-10
-5
0
5
10
-20
-15
-10
-5
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-5
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5
10
Original SLC Ground layer
Original SLC Ground layer L-band, HH
P-band,HH
Intensity [dB]
Imaging the Ground scattering
L-band
P-band
Imaging the Ground scattering
Co-polar phase HH-VV
0 →
- →
or
L-band P-band
Co-p
ol phase [°]
Ground slope [°]
-10 -5 0 5 10
-150
-100
-50
0
50
100
150
Ground slope [°]
Co-p
ola
r phase [°]
-10 -5 0 5 10
-150
-100
-50
0
50
100
150
Co-p
ol phase [°]
Ground slope [°]
-10 -5 0 5 10
-150
-100
-50
0
50
100
150
0
0.2
0.4
0.6
0.8
1
Ground slope [°]
Co-p
ola
r phase [°]
-10 -5 0 5 10
-150
-100
-50
0
50
100
150 Original SLC Ground layer
Original SLC Ground layer
Conclusions
The vertical structure of the forest in a dense tropical forest:
• Ground scattering is strongly visible
• Volume scattering is significantly related to the biomass from 200 t/ha –
500t/ha (even @ 6 MHz, RMSE 10% at 6.25-ha plots).
• Forest height can be readily determined, and it matches with LiDAR height.
At P-band
• Ground scattering is partly visible
• The L-band tomographic profile is quite disturbed as compared to the P-band profile. In this condition, the use of tomographic imaging at L-band in tropical forests appears limited.
• However, when the forest top height is roughly below 20 m (e.g. in forest regrowth), the tomographic results are expected to be the same as in boreal forests.
At L-band