Observation Results of the 2007 Noto Peninsular Earthquake by the Advanced Land Observing Satellite "Daichi"

At around 9:42 a.m. on March 25, 2007, Japan Standard Time (JST, all dates and times hereinafter are in JST,) a major earthquake, later named the "2007 Noto Peninsular Earthquake," hit the Noto region of Japan. The epicenter was offshore from the Noto Peninsular (about 40 km west-south-west of the city of Wajima.) The Japan Aerospace Exploration Agency (JAXA) detected a rise in the surface of the land due to the earthquake by analyzing observation images acquired by the Advanced Land Observing Satellite "Daichi" on April 10.


Figure 1 shows the diastrophism by processing the image taken by one of the Daichi onboard sensors, the PALSAR*1, at 10:27 p.m. on April 10 and one also taken by the PALSAR on February 23, 2007, (Figure 2) using the differential interferometric method*2. The change of distance between the Daichi and the Earth in 47 days between Feb. 23 and April 10 is indicated by the two-dimensional colors in the image. We can observe a maximum of 45 centimeters of rise mainly in the western part of Monzen Town in the city of Wajima. The rises were concentrated within about a 40 km radius around the town. The Geographical Survey Institution of Japan also detected the diastrophism through GPS observations of a gap in a fault and other methods, and we were able to support their detection through data acquisition by the Daichi.

Figure 1: Diastrophism around the Noto Peninsular

Figure 1: Diastrophism around the Noto Peninsular
(Click to View Enlarged Image)

Color changes are more obvious near the epicenter. We measured a maximum of 45 centimeters in the rise of the land. One cycle of colors indicates 11.8 centimeters of change.

Figure 2: The Noto Peninsular Observed by the PALSAR on April 10, 2007

Figure 2: The Noto Peninsular Observed by the PALSAR on April 10, 2007
(Click to View Enlarged Image)

©JAXA EORC

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