March 11th Japan Earthquake and Tsunami, Beyond the Frontiers: What we observed by radar polarimetry2. March 11th Japan Earthquake and Tsunami
Beyond the Frontiers:
What we observed by radar polarimetry
Motoyuki Sato
Si-we Chen
Tohoku University
12. Mar 12th, 2011
20
Backscattered Power(dB)
10 HH
HV
0
VV
-10
-20
-30
-40
-50
-60
0 0.5 1 1.5 2 2.5 3
Distance(km)
Mar 18th, 2011,
20
HH
Backscattered Power(dB)
10
HV
0 VV
-10
-20
-30
-40
-50
-60
0 0.5 1 1.5 2 2.5 3
Distance(km)
13. Pauli Decomposition
S HH S HV 1 0 1 0 0 1
SVH SVV 0 1 0 1 1 0
Single Double Volumetric
Bounce Bounce Scattering
S HH SVV
Single
Bounce 2
S HH SVV
Double 2
Bounce
SHV
16. Pd Yamaguchi decomposition
(red),
Pv
(green), and
Ps
Pd(red), Pv (green),Ps (blue).
(blue).
Nov 21st, 2010. Apr 8th, 2011
18. Jun 25th,2010 Apr 6th, 2011 Old Kitalami River
Pd
(red),
Pv
(green), and
Ps
Optical image
Yamaguchi
decomposition
Pd(red)
Pv (green)
Ps (blue)
0 0.2 0.4 0.6 0.8 1
19. Jun 25th,2010 Apr 6th, 2011,
0 10 20 30 40 50 60 70 80 90 (deg)
Entropy
22. Polarization Orientation Angle
Induced by Ground Surface Patch
Jong-Sen Lee, Dale L. Schuler, et al.
The induced polarization orientation
angle shift θis represented,
tan
tan
tan cos sin
Where tanω is the azimuth slope,
tanγ is the range slope, φ is the radar look angle.
Induced by Dihedral Structure
Hiroshi Kimura, et al.
tan
tan
cos
Where tanα is the target azimuth angle,
φ is the radar look angle.
27. Jun 25th,2010 Apr 6th, 2011 Ishinomaki
Pd
(red),
Pv
ALOS/PALSAR
(green), and
Optical images
Yamaguchi
decomposition
Pd(red),
Pv (green)
Ps (blue).
-40 -30 -20 -10 0 10 20 30 40 (deg)
Polarization
orientation angle.
28. How Radar Polarimetry
can be used for detection
of Damaged Areas?
•Differential Time?
•Interferometry ?
•High Resolution?