Electronic Supplement to
The February 2014 Cephalonia Earthquake (Greece): 3D Deformation Field and Source Modeling from Multiple SAR Techniques
by John Peter Merryman Boncori, Ioannis Papoutsis, Giuseppe Pezzo, Cristiano Tolomei, Simone Atzori, Athanassios Ganas, Vassilios Karastathis, Stefano Salvi, Charalampos Kontoes, and A. Antonioli
Table S3. Differences between East, North and Up Components of the Coseismic Displacement Gradients between KEFA and VLSM cGPS Stations* Due to the 3 February 2014 Event
| Component |
KEFA–VLSM Displacement (cm) |
| GPS |
SAR |
SAR-GPS |
Predicted Error (σ) |
| East |
4.7 |
6.2 |
1.5 |
3.1 |
| North |
−8.2 |
−5.5 |
2.7 |
2.9 |
| Up |
1.5 |
2.9 |
1.4 |
3.7 |
SAR values are averaged over a 400 m × 400 m area centered on each cGPS station location. The last column represents the predicted error standard deviation of the difference between SAR and GPS measurements.
* See Figure 3 of the main article.
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