[Earth Observation Research Center (EORC)] ALOS-2/PALSAR-2 Observation Results on M 6.2 earthquake in central Italy.

Posted: August 25, 2016, 8:00 (UTC)
Updated: September 1, 2016, 7:00 (UTC)
Updated: November 4, 2016, 8:00 (UTC)

On August 24, 2016 at 23:00 (UTC), an emergency observation with the Phased Array-type L-band Synthetic Aperture Radar-2 (PALSAR-2) aboard the Advanced Land Observing Satellite-2 (ALOS-2, “DAICHI-2”) was performed in response to the magnitude-6.2 earthquake in central Italy on August 24, 2016 at 1:36 (UTC). The second observation was performed on August 31, 2016 at 11:15 (UTC).
Another magnitude 6.1 and 6.6 earthquakes struck the same region on October 26 and 30, respectively. In response to these earthquakes, ALOS-2 performed observations on October 28 and November 2.
Japan Aerospace Exploration Agency (JAXA) has provided the acquired data to corresponding authorities.

Fig.1: Area of the emergency observation. (Green: observed on Aug. 24, Red: observed on Aug.31)
(Click to view enlarged image)

Fig. 2 shows a differential interferometry (DInSAR) result derived from the PALSAR-2 data acquired before (September 9, 2015; UTC) and after (August 24, 2016; UTC) the earthquake. Approximately 20 cm deformation away from the satellite (eastward and / or downward movement) is detected in the east region of the epicenter. The deformation area extends approx. 20 km from north to south and 10 km from west to east. The city of Amatrice places its south end.

Fig.2: Differential interferometry (DInSAR) result using the ALOS-2 PALSAR-2 data acquired before (September 9, 2015; UTC) and after (August 24, 2016; UTC) the earthquake.
(Click to view enlarged image)

» KMZ File is here

Fig. 3 and Fig. 4 show the damage proxy map of Amatrice and Illica generated by comparing the interferometric coherence values before and after the earthquake. The dense orange parts illustrate significant decrease of coherence caused by surface changes including collapse of buildings.

Fig.3: Damage proxy map of Amatrice generated by the interferometric coherence change analysis.
(Click to view enlarged image)

Fig.4: Damage proxy map of Illica generated by the interferometric coherence change analysis.
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Update on Sep. 1, 2016. Observation on Aug. 31, 2016.
Fig. 5 shows a differential interferometry (DInSAR) result derived from the PALSAR-2 data acquired before (May 25, 2016; UTC) and after (August 31, 2016; UTC) the earthquake. Approximately 25 cm deformation away from the satellite (westward and / or downward movement) is detected in the east region of the epicenter.

Fig.5: Differential interferometry (DInSAR) result using the ALOS-2 PALSAR-2 data acquired before (May 25, 2016; UTC) and after (August 31, 2016; UTC) the earthquake.
(Click to view enlarged image)

» KMZ File is here

Fig. 6 and Fig. 7 are the preliminary results of decomposition in east-west and vertical displacements using the interferograms from ascending orbit (Fig. 2) and descending orbit (Fig. 5). Approximately 15cm horizontal deformation and 20 cm vertical deformation are detected.

Fig.6: Decomposed east-west displacement
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» KMZ File is here

Fig.7: Decomposed up-down displacement
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» KMZ File is here

Update on Nov. 4, 2016. Observation on Oct. 28 and Nov. 2, 2016
Fig. 8 shows a DInSAR result derived from the PALSAR-2 data acquired before (February 5, 2016; UTC) and after (October 28, 2016; UTC) the earthquakes on August 24 and October 26.
Approximately 20cm deformation away from the satellite (eastward and / or downward movement) is detected for two earthquakes separately.

Fig.8: DInSAR result using the ALOS-2 PALSAR-2 data acquired before (February 5, 2016; UTC) and after (October 28, 2016; UTC) the earthquakes on August 24 and October 26.
(Click to view enlarged image)

» KMZ File is here

Fig. 9 shows a differential interferometry (DInSAR) result derived from the PALSAR-2 data acquired before (August 24, 2016; UTC) and after (November 2, 2016; UTC) the earthquakes on October 26 and 30. Approximately 60 cm deformation away from the satellite (eastward and / or downward movement) is detected at the city of Castelluccio while 30 cm deformation close to the satellite (westward and / or upward movement) at the city of Norcia.

Fig.9: DInSAR result using the ALOS-2 PALSAR-2 data acquired before (August 24, 2016; UTC) and after (November 2, 2016; UTC) the earthquakes on October 26 and 30.
(Click to view enlarged image)

» KMZ File is here

Fig. 10 shows a differential interferometry (DInSAR) result derived from the PALSAR-2 data acquired before (September 9, 2015; UTC) and after (November 2, 2016; UTC) the three earthquakes. The deformation area extends approx. 50 km from north to south and more than 40 km from west to east. The city of Amatrice places its south end and the city of Pievebovigliana places its north end.

Fig.10: DInSAR result using the ALOS-2 PALSAR-2 data acquired before (September 9, 2015; UTC) and after (November 2, 2016; UTC) the three earthquakes.
(Click to view enlarged image)

» KMZ File is here

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