ASI-SRV web pages

The Project called Sistema Rischio Vulcanico (SRV) is funded  by the Italian Space Agency (ASI) in the frame of the National Space Plan 2003-2005 under the Earth Observations section for natural risks management. The SRV Project is coordinated by the Istituto Nazionale di Geofisica e Vulcanologia (INGV) which is responsible at national level for the volcanic monitoring. The ASI-SRV is devoted to the development of an integrated system based on EO and Non EO data to respond to specific needs of the Italian Civil Protection Department (DPC). SRV provides the capability to import many different EO and Non EO data into the system, it maintains a repository where the acquired data have to be stored and generates selected products which will be functional to the different volcanic activity phases. The Italian Civil Protection department represents the unique END USER of the ASI-SRV project. The Civil Protection organisms represent the National Authority which will get benefit form the space technology derived products for Volcanic Risk management and monitoring. The ASI-SRV service is based on the integration of products derived from EO data and products derived from non EO data, in order to manage the volcanic risks. All the products are delivered by means of dedicated password protected WEBGIS interface. The main functionalities of the developed WEBGIS are contained in DEMO (120 mb AVI format, about 10 minutes).

SO2 flux estimated by means of ASTER and MODIS data aquired on July 29, 2001

    

 

Preliminary results obtained wihtin ASI-SRV project relevant the 4 April 2010 Earthquake: (left) Terrain displacement map using ASAR-ENVISAT descending orbit  (18 November 2009 – 07 April 2010, Bperp=77m). Preliminary DORIS-POR orbits have been used. Dashed box includes the coseismic area (2-3 April 2010 seismic swarm). Along Pernicana fault has been identified 1 fringe of deformation (about 2,8 cm). (right) Terrain displacement map using ASAR-ENVISAT descending orbit (27 January 2010 – 07 April 2010,  Bperp=106m). Preliminary DORIS-POR orbits have been used. Dashed box includes the coseismic area (2-3 April 2010 seismic swarm). Decorrelation has been attributed to the presence of snow (higher portion of the volcano) and probable presence of atmosphere effect along the eastern flank.

Two collaborative areas are available for document management & dissemination (ktdms.acsys.it) and bug & issue tracking (jira.acsys.it)

Both these areas are for internal use and are password protected.