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  5. The VELISAR initiative for the measurement of ground velocity in italian seismogenic areas
 
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The VELISAR initiative for the measurement of ground velocity in italian seismogenic areas

Author(s)
Salvi, S.  
Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italia  
Atzori, S.  
Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italia  
Brunori, C. A.  
Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italia  
Doumaz, F.  
Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italia  
Ricciardi, G. P.  
CNR - IREA, Napoli, Italy  
Solaro, G.  
CNR - IREA, Napoli, Italy  
Stramondo, S.  
Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italia  
Tolomei, C.  
Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italia  
Lanari, R.  
CNR - IREA , Napoli, Italy  
Pepe, A.  
CNR - IREA, Napoli, Italy  
Ferretti, A.  
Cespa, S.  
Tele Rilevamento Europa S.R.L. Milano, Italy  
Type
Poster session
Language
English
Status
Published
Journal
European Geoscience Union General Assembly 2007  
Date Issued
April 15, 2007
Conference Location
Vienna, Austria
URI
https://www.earth-prints.org/handle/2122/2107
Subjects
04. Solid Earth::04.03. Geodesy::04.03.01. Crustal deformations  
04. Solid Earth::04.03. Geodesy::04.03.06. Measurements and monitoring  
04. Solid Earth::04.03. Geodesy::04.03.07. Satellite geodesy  
04. Solid Earth::04.03. Geodesy::04.03.09. Instruments and techniques  
Subjects

SAR

Inteferometry

Small Baseline Sunset...

SBAS

Permanent Scatterers

PS

Ground Velocity

seismogenic area

Abstract
VELISAR (Ground VELocity in Italian Seismogenic Areas) is a scientific research
initiative aimed at producing a map of the ground deformation over most of the seismogenic
areas of Italy, using the space-based technique of multitemporal Synthetic
Aperture Radar Interferometry (InSAR). The ground velocities derived from InSAR
data will be validated by means of ground based data obtained from GPS, optical leveling,
seismological and neotectonic studies. The scope of the project is to produce
a high-resolution ground deformation dataset useful to model the seismic cycle of
strain accumulation and release at the scale of the single faults. The main objective of
VELISAR is to produce maps of ground velocity with the following characteristics:
- A ground resolution better than 100 m. - Average uncertainty of LoS velocity measurements
smaller than 2 mm/yr . - Temporal coverage of at least 7 years. - Retrieval
of East and Up components from ascending and descending LoS.
VELISAR will exploit the potential of the long time series (1992-2000) of ERS InSAR
data maintained in the ESA archives; over 4000 ERS images will have to be processed
to accomplish its objectives. Presently, two InSAR techniques for the measurement
of slow ground deformation are used in VELISAR: the Permanent Scatterers (PS)
technique developed by the Politecnico of Milano (POLIMI), and the Small Baseline
Subset (SBAS) technique, developed by the Institute for Remote Sensing of Environment
(IREA-CNR), in Napoli. The PS technique is applied by TRE preferably over
areas characterised by diffuse temporal decorrelation due to, for instance, erodible
lithologies, agricultural land use and strong vegetation cover. In these areas we expect
to obtain good temporal coherence mainly on sparse point scatterers. The SBAS
technique is applied by IREA and INGV mostly over areas where limited temporal
decorrelation is expected: urban areas, scarcely vegetated areas. The ground resolution
at which these data are originally processed is 80 m. An important goal of the
VELISAR initiative is to disseminate the information on the InSAR-derived ground
velocity measurements, to the scientific community and to the public in general. Such
goal is accomplished through a dedicated web site, where the velocity maps of the
italian seismogenic areas will be progressively published. We will present the initiative,
its scope and objectives, the technical details and the data processing strategies,
and some examples of ground velocity maps.
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