Abstract
On 22 December 2018, parts of the Anak Krakatau edifice collapsed, triggering a deadly tsunami. To investigate pre-collapse surface displacements, we analyzed Interferometric Synthetic Aperture Radar satellite geodetic data from 2006 to 2018, acquired from ALOS-1 (2006–2011), COSMO-SkyMED (2012–2018), and Sentinel-1 (2014–2018). We identified line-of-sight displacements on the southwestern flank throughout the study period. Inversion of COSMO-SkyMED data revealed a rectangular dislocation with a cumulative slip of 12 m from April 2012 to December 2018. Fixing the fault geometry, we found the optimal slip for time periods corresponding to slip rate changes, ranging from 1.2 to 3.1 m/yr. The slip estimates for ALOS-1 and Sentinel-1 data were 0.88 m/yr and 1.1 m/yr, respectively, over their individual time periods. Overall, the detachment fault experienced approximately 15 m of slip from 2006 to 2018 with acceleration and deceleration periods, and a notable acceleration prior to the 2018 collapse.
| Original language | English (US) |
|---|---|
| Article number | e2024GL112296 |
| Journal | Geophysical Research Letters |
| Volume | 51 |
| Issue number | 22 |
| DOIs | |
| State | Published - Nov 28 2024 |
All Science Journal Classification (ASJC) codes
- Geophysics
- General Earth and Planetary Sciences
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