GA2015 SAR applicazioni frane parte1

Page 1

Department of Earth Sciences

CENTRE OF COMPETENCE OF THE CIVIL PROTECTION DEPARTMENT PRESIDENCY OF THE COUNCIL OF MINISTERS

Radar interferometry applications for the detection and monitoring of ground displacements Filippo Catani


Scheme of presentation •  Materials and methods –  Satellite SAR interferometry –  Ground-based SAR interferometry

•  Applications –  Inventory and motion survey –  Monitoring and interpretation –  Rapid mapping –  Instant mapping –  Failure forecasting –  Early-warning –  Emergency management


Sarno, 5 May 1998

Debris flows 153 victims Hundreds of homeless


Law n.267/1998: Landslide risk zonation Regional landslide inventories 2 million landslides mapped at 1:10.000 Lanslide risk areas ca. 10.000 areas classified at extremely high risk (R4) Social impact ca. 60 victims per year Economic impact ca. 1 - 2 billion Euro per year (0.15% of GDP) Unstable urban areas 1,306 to be stabilized 323 to be relocated


National risk zonation Risk class

Level

Description

Measures

R4

Very high

Major risk for human life. Desctruction of buildings and infrastructures

Reconstruction forbidden, relocation or stabilization compulsory

R3

High

Major losses for buildings and infrastructures. Possible risk for human life

Severe building restrictions. Stabilization works required.

R2

Medium

Expected damage for buildings and infrastructures. No risk for life

Medium building restrictions

R1

Low

Limited expected loss

General risk prevention measures

R0

Negligible

No expected loss

None


Photo interpretation

I1: Scarps, terraces, counterslopes I2: Sharp variation of curvature in the longitudinal profile I3: Irregular drainage system, water ponds, internal drainage depressions, stream channel deviation I4: Bedrock outcrops, soil erosion, denudation I5: Presence of rapid-growth vegetation I6: Sharp difference in vegetation inside/ outside the landslide


State of activity and risk zonation 1. Active (moving) – R4 2. Suspended (seasonally) – R4 3. Dormant (recurrent) – R3 5. Naturally stabilized – R2-R1 6. Artificially stabilized – R2-R1 7. Relict – R0 UNESCO WP/WLI (1993)


Department of Earth Sciences

CENTRE OF COMPETENCE OF THE CIVIL PROTECTION DEPARTMENT PRESIDENCY OF THE COUNCIL OF MINISTERS

Satellite SAR interferometry PS technique


Radar Satellites SAR = Synthetic Aperture Radar

θ=23°


Radar satellites


Cosmo Sky Med


Etna


SAR interferometry Time

T0 R1

Time

T0+Δt

R1= R2

Δr 1’ acquisition

2’ acquisition

Permits to assess ground deformations with centimetric accuracy

Laion Landslide


Permanent Scatterers technique pixel by pixel analysis ESA - ERS San Francisco International Airport

multi-image processing

San Francisco Bay

tempo

Processing technique of SAR images which allows to assess deformations with millimetric accuracy on single specific points (PS), coincident with highly reflective elements on the ground surface

35 giorni

100 Km 100 Km

Dataset of SAR images


Ascending and descending data


Department of Earth Sciences

CENTRE OF COMPETENCE OF THE CIVIL PROTECTION DEPARTMENT PRESIDENCY OF THE COUNCIL OF MINISTERS

Ground-based SAR interferometry LiSA technique


Ground based SAR interferometry

Portable SAR apparatus known as LISA (Linear Synthetic Aperture Radar), developed by the Joint Research Centre of the European Commission


Ground-based InSAR Continuous-wave stepped-frequency (CW-SF) radar based on a Network Analyser (NWA) operating in the frequency band 17.0-17.1 GHz

target area

Tx

Rx

sled

linear rail 2.8m

source NWA

:

computer

The synthetic aperture is obtained sliding the antennas along a linear rail European Commission Joint Research Centre



Acquisition of raw data

Network Analyzer


Interferometry Image 1

LOS displacement (mm)

Image 2

phase wrapping

Interferogram (phase difference)


Phase wrapping and decorrelation Phase Wrapping: Large displacement generates fringes

Decorrelation: Rapid motion causes “salt & pepper� texture

Coherence ( 0 <Γ <1) gives an estimate of the error in measured differential phase


Interferogram on DTM


Department of Earth Sciences

CENTRE OF COMPETENCE OF THE CIVIL PROTECTION DEPARTMENT PRESIDENCY OF THE COUNCIL OF MINISTERS

Inventory and motion survey Arno River Basin



PS ERS descending 1992-2002 total: 327 942 PS


PS ERS ascending 1992-2002 total: 263 321 PS


Landslide inventory map

74% earth slides and flows 19% shallow landslides and creep 5% debris flows 2% others

27 270 mapped landslides 8.8 % landslide density


PS and landslide map

Legend Landslide polygons

Landslide lines

attiv

attiv

instab

inatt

quiesc

PS ascending

PS Descending

Vel (mm/y)

Vel (mm/y)

")

-29.18 - -5.00

$ +

-29.18 - -5.00

")

-4.99 - -3.00

$ +

-4.99 - -3.00

")

-2.99 - -1.25

$ +

-2.99 - -1.25

")

-1.24 - 1.25

$ +

-1.24 - 1.25

")

1.26 - 3.00

$ +

1.26 - 3.00

")

3.01 - 5.00

$ +

3.01 - 5.00

5.01 - 29.05

$ +

5.01 - 29.05

")

G

PS_rufina


Updating landslide inventory Landslide A Activity: confirmed Boundary: modified Landslide B Activity: modified Boundary: modified

A

B F

active inactive active inactive dormant

active inactive dormant

C Landslide F Activity: modified Boundary: confirmed Landslide C Activity: modified Boundary: modified

D C’ E

Landslide D New detection Landslide E New detection


Activity matrix

MATRIX OF ACTIVITY

ERS < 2mm

ERS > 2mm

ENVISAT < 2 mm

Stable

Dormant

ENVISAT > 2 mm

Active (reactivated)

Active (continuos)


HAZARD MAP


Risk Map: R= H路V路E

Expected loss: R = ~ 5.6 billion Euro in 30 years (0.5掳/掳 GDP)


Revised hazard area with PS information


Effectiveness of stabilization measures Stabilization works (drainage wells & subhorizontal drainages) Landslide attiv Active

Arno River

instab Inactive

quiesc Dormant

B

stabilizzata Stabilized

B

APSA Vel (mm/y)

5 A

A 5

The Carbonile landslide

!(

-29.18 - -5.00

!(

-4.99 - -3.00

!(

-2.99 - -1.25

!(

-1.24 - 1.25

!(

1.26 - 3.00

!(

3.01 - 5.00

!(

5.01 - 29.05


Department of Earth Sciences

CENTRE OF COMPETENCE OF THE CIVIL PROTECTION DEPARTMENT PRESIDENCY OF THE COUNCIL OF MINISTERS

Monitoring and interpretation Cirò Marina



PS RADARSAT

ascending 2003-2005

Displacement = 4-12 mm/ year


PS RADARSAT

descending 2003-2005

Displacement= 4-8 mm/year


Reconstruction of the slip surface •  Graphical method for reconstructing the slip surface (Carter & Bentley, 1985; Cruden, 1986) used in Structural Geology •  Input data: position of the main scarp and displacement vectors within the landslide mass •  Assumption: rigid deformation within each slice (Mertie, 1947)


Reconstruction of the slip surface O4

Sezione EF N1

O1

N3

O2

N5

N4

Prodondità (m p.c.)

V2 V3

V4

V5 V6 V7 V8

Distanza (m)

Prodondità (m p.c.)

Sezione CD

Distanza (m)

N6

N7

N8


Interpolation N

0

depth (m)

250

Interpolation of multiple sections Data available only above the sea level


Extrapolation N

0 350

depth (m)

Extrapolation of the sections below the sea level based on a constant reduction of the local inclination of the slip surface


Possible interpretation

ProfonditĂ

Sezione Porto Turistico

Distanza (m)

Presence of multiple slip surfaces Shallow landslide in the area of the harbour


N

0

350

depth (m b.s.l.)


Comparison with bathymetry

0

depth (m) 350

Multi-beam by UNIROMA1-DST (F. Chiocci)

Estimated landslide volume = 1 billion m3 = 1 km3


Department of Earth Sciences

CENTRE OF COMPETENCE OF THE CIVIL PROTECTION DEPARTMENT PRESIDENCY OF THE COUNCIL OF MINISTERS

Rapid mapping Cerzeto (CZ)



Cavallerizzo di Cerzeto: 7 march 2005



Satellite ERS1/2 Orbit descendent Startdate 15/09/1992 Enddate 05/01/2001 No. of images 70 No. of PS 4642


Satellite RADARSAT Orbit ascendent Startdate 18/03/2003 Enddate 26/11/2005 No. of images 38 No. of PS 7869



Ikonos image rendered on DEM and PS


Cavallerizzo di Cerzeto Initial landslide map (PAI)


Cavallerizzo di Cerzeto after photointerpretation


Cavallerizzo di Cerzeto after radarinterpretation of ERS/ ENVISAT data


Cavallerizzo di Cerzeto after radarinterpretation of RADARSAT data


Department of Earth Sciences

CENTRE OF COMPETENCE OF THE CIVIL PROTECTION DEPARTMENT PRESIDENCY OF THE COUNCIL OF MINISTERS

Instant mapping Tufillo


Tufillo









GPRS data transmission


ENVISAT ascending 2002-2006


Punto Tufillo 469120E 4640895N (UTM 33) 20

18

16

Displacement [mm]

14

12

10

8

6

4

2

0 24/05/2002

10/12/2002

28/06/2003

14/01/2004

01/08/2004

17/02/2005

Time [days]

velocity = 9 mm/year

05/09/2005

24/03/2006

10/10/2006


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