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TH4.T07: Special session on the great earthquake of East Japan on March 11, 2011

March 11th Japan Earthquake and Tsunami, Beyond the Frontiers: What we observed by radar polarimetry

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Page 1: March 11th Japan Earthquake and Tsunami, Beyond the Frontiers: What we observed by radar polarimetry

TH4.T07: Special session on the great earthquake of East Japan on March 11, 2011

Page 2: March 11th Japan Earthquake and Tsunami, Beyond the Frontiers: What we observed by radar polarimetry

March 11th Japan Earthquake and Tsunami Beyond the Frontiers: What we observed by radar polarimetry

Motoyuki Sato

Si-we Chen Tohoku University

Page 3: March 11th Japan Earthquake and Tsunami, Beyond the Frontiers: What we observed by radar polarimetry

Tohoku University

Page 4: March 11th Japan Earthquake and Tsunami, Beyond the Frontiers: What we observed by radar polarimetry

Sendai International Center

Page 5: March 11th Japan Earthquake and Tsunami, Beyond the Frontiers: What we observed by radar polarimetry

Polarimetric SAR Image-Sendai

HH:R

HV:G

VV:B

Pi-SAR

(NICT)

0 1HHHH HV j HV

VH VV VH VV

S S Se

S S S S

S

Page 6: March 11th Japan Earthquake and Tsunami, Beyond the Frontiers: What we observed by radar polarimetry

Sendai-Natori

Page 7: March 11th Japan Earthquake and Tsunami, Beyond the Frontiers: What we observed by radar polarimetry
Page 10: March 11th Japan Earthquake and Tsunami, Beyond the Frontiers: What we observed by radar polarimetry

Pi-SAR2

(NICT) Mar

12th 2011

HH:R

HV:G

VV:B

Sendai-Natori

Page 11: March 11th Japan Earthquake and Tsunami, Beyond the Frontiers: What we observed by radar polarimetry

Pi-SAR2

(NICT)

Mar 18th 2011

HH:R

HV:G

VV:B

Page 12: March 11th Japan Earthquake and Tsunami, Beyond the Frontiers: What we observed by radar polarimetry

0 0.5 1 1.5 2 2.5 3-60

-50

-40

-30

-20

-10

0

10

20

Distance(km)

Ba

cksca

tte

red

Po

we

r(d

B)

HH

HV

VV

0 0.5 1 1.5 2 2.5 3-60

-50

-40

-30

-20

-10

0

10

20

Distance(km)

Ba

cksca

tte

red

Po

we

r(d

B)

HH

HV

VV

Mar 12th

, 2011

Mar 18th

, 2011,

Page 13: March 11th Japan Earthquake and Tsunami, Beyond the Frontiers: What we observed by radar polarimetry

Pauli Decomposition

1 0 1 0 0 1

0 1 0 1 1 0

HH HV

VH VV

S S

S S

2

HH VVS S

2

HH VVS S

HVS

Single

Bounce

Double

Bounce

Volumetric

Scattering

Single

Bounce

Double

Bounce

Page 14: March 11th Japan Earthquake and Tsunami, Beyond the Frontiers: What we observed by radar polarimetry

ALOS/PALSAR Pauli Decomposition

Ishinomaki-Onagawa

II

I

Slave

II

I

R:HH-VV,G:HV, B:HH+VV

Nov 21st, 2010. Apr 8th, 2011

Page 15: March 11th Japan Earthquake and Tsunami, Beyond the Frontiers: What we observed by radar polarimetry

Onagawa

Page 16: March 11th Japan Earthquake and Tsunami, Beyond the Frontiers: What we observed by radar polarimetry

Yamaguchi decomposition

dP

vP

sP

(red),

(green), and

(blue).

Nov 21st, 2010. Apr 8th, 2011

Pd(red), Pv (green),Ps (blue).

Page 17: March 11th Japan Earthquake and Tsunami, Beyond the Frontiers: What we observed by radar polarimetry

Cloude-Pottier decomposition Entropy

0

0.2

0.4

0.6

0.8

1

Nov 21st, 2010. Apr 8th, 2011

Page 18: March 11th Japan Earthquake and Tsunami, Beyond the Frontiers: What we observed by radar polarimetry

0 0.2 0.4 0.6 0.8 1

dP

vP

sP

(red),

(green), and

Jun 25th,2010 Apr 6th, 2011 Old Kitalami River

Yamaguchi

decomposition

Pd(red) Pv (green) Ps (blue)

Optical image

Page 19: March 11th Japan Earthquake and Tsunami, Beyond the Frontiers: What we observed by radar polarimetry

0 10 20 30 40 50 60 70 80 90(deg)

Entropy

Jun 25th,2010 Apr 6th, 2011,

Page 20: March 11th Japan Earthquake and Tsunami, Beyond the Frontiers: What we observed by radar polarimetry
Page 21: March 11th Japan Earthquake and Tsunami, Beyond the Frontiers: What we observed by radar polarimetry
Page 22: March 11th Japan Earthquake and Tsunami, Beyond the Frontiers: What we observed by radar polarimetry

日本地球惑星科学連合2008年大会

Polarization Orientation Angle

Induced by Ground Surface Patch

Jong-Sen Lee, Dale L. Schuler, et al.

Induced by Dihedral Structure Hiroshi Kimura, et al.

tantan

tan cos sin

Where tanω is the azimuth slope,

tanγ is the range slope, φ is the radar look angle.

tantan

cos

Where tanα is the target azimuth angle,

φ is the radar look angle.

The induced polarization orientation

angle shift θis represented,

Page 23: March 11th Japan Earthquake and Tsunami, Beyond the Frontiers: What we observed by radar polarimetry

Sendai (Pi-SAR)

L-band, HH-VV, 2HV, HH+VV

X-band, HH-VV, 2HV, HH+VV

Residential block

1250m*1250m Estimated PO Angle θ

Estimated PO Angle θ

Page 24: March 11th Japan Earthquake and Tsunami, Beyond the Frontiers: What we observed by radar polarimetry
Page 25: March 11th Japan Earthquake and Tsunami, Beyond the Frontiers: What we observed by radar polarimetry
Page 27: March 11th Japan Earthquake and Tsunami, Beyond the Frontiers: What we observed by radar polarimetry

Jun 25th,2010 Apr 6th, 2011 Ishinomaki

dP

vP (red),

(green), and

Polarization

orientation angle.

Optical images

Yamaguchi

decomposition

Pd(red), Pv (green) Ps (blue).

-40 -30 -20 -10 0 10 20 30 40 (deg)

ALOS/PALSAR

Page 28: March 11th Japan Earthquake and Tsunami, Beyond the Frontiers: What we observed by radar polarimetry

How Radar Polarimetry

can be used for detection

of Damaged Areas?

•Differential Time?

•Interferometry ?

•High Resolution?

Page 29: March 11th Japan Earthquake and Tsunami, Beyond the Frontiers: What we observed by radar polarimetry