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TerraSAR-X image of the month: L'Aquila after the earthquake on 6 April 2009

26 May 2009

 Area around the Italian town of L'Aquila following the magnitude 6.3 earthquake on 6 April 2009
zum Bild Area around the Italian town of L'Aquila following the magnitude 6.3 earthquake on 6 April 2009

The image from the German TerraSAR-X radar satellite shows the area around the Italian town of L'Aquila after the magnitude 6.3 earthquake struck on 6 April 2009. Two images from the satellite were combined for the picture, taken before and after the earthquake, to create an interferogram.

The 'coloured rings' around L'Aquila stand out. These rings represent, in colour coding, the ground movement caused by the earthquake.  One colour sequence represents a shift of about 1.6 centimetres; at the centre, there was a maximum subsidence of up to 20 centimetres.  The movement primarily occurred at the normal fault located northeast of L'Aquila, marked in red on the image.  The topographical influence on the interferogram was removed using a digital elevation model in order to highlight the movement to a greater extent.

Region at risk of earthquakes

This interferogram represents a measurement of the effects of the quake; it does not predict possible future earthquakes.  However, the information it provides supports the subsequent modelling of the geological processes and enables a detailed understanding of the causes.

The town of L'Aquila is situated in the Apennines, an approximately 1,500 kilometre-long mountain range which extends along the Italian peninsula.  They are an alpidic (i.e. belonging to the Alps) fold and thrust belt, which began to arise about 50 million years ago. The complex tectonic events in this region are determined by the collision of the Eurasian and African plates, the subduction (one plate moving under another) of the Adriatic microplate and the opening of the Tyrrhenian basin. The simultaneously occurring compression and expansion movements are the cause of the repeated earthquakes in this region.

For the analysis, two TerraSAR-X images, acquired in stripmap mode were used with a resolution of 1.7 x 3.4 metres.  The first image was taken on 6 February 2009, the second on 13 April 2009. Since the earthquake occurred during the time these two images were taken, this pair is very well suited for observing its effects. The two radar images were processed using the operational interferometric processing system 'PSI Genesis' developed by the German Aerospace Centre (DLR).

The TerraSAR-X mission

TerraSAR-X is the first German satellite that has been manufactured under what is known as a Public-Private Partnership (PPP) between the German Aerospace Center (Deutsches Zentrum fuer Luft- und Raumfahrt; DLR) and Astrium GmbH in Friedrichshafen. The satellite travels around the Earth in a polar orbit and records unique, high-quality X-band radar data about the entire planet using its active antenna. TerraSAR-X works regardless of weather conditions, cloud cover or absence of daylight, and is able to provide radar data with a resolution of down to one metre.

DLR is responsible for using TerraSAR-X data for scientific purposes. It is also responsible for planning and implementing the mission as well as controlling the satellite. Astrium built the satellite and shares the costs of developing and using it. Infoterra GmbH, a subsidiary company founded specifically for this purpose by Astrium, is responsible for marketing the data commercially.


Contact
Elke Heinemann
German Aerospace Center (DLR)

Corporate Communications
, Online Communication - DLR Web Portal
Tel.: +49 2203 601-2867

Fax: +49 2203 601-3249


Christian Minet
German Aerospace Center (DLR)

Remote Sensing Technology Institute
, SAR Signal Processing
Tel.: +49 8153 28-3323

Fax: +49 8153 28-1420


Last update: 08/07/2009 09:02:31