Time Series Analysis of Post-Tsunami Coastal Recovery on the Sendai Coastline Using Dynamic Time Warping and Persistent Homology

This study presents a computational framework combining Dynamic Time Warping (DTW) and Persistent Homology to quantify the long-term morphological evolution of the Sendai coastline following the 2011 Tōhoku tsunami. Using multispectral satellite imagery from Landsat 5 TM, Landsat 8 OLI, and Sentinel-2 MSI (2010–2024), instantaneous shorelines were extracted via the Modified Normalized Difference Water Index (MNDWI) and reconstructed with parametric B-spline curves. DTW analysis indicated severe initial deformation, with a 90,927 m difference between pre- and post-tsunami instantaneous shorelines, followed by gradual stabilization as distances declined to 59,584 m by 2024. Persistent Homology revealed a more complex topological trajectory, with the number of 1-dimensional features (H1) rising sharply after the tsunami, consolidating by 2015, and expanding again to over 8000 by 2020–2024. The Stable Distance of Persistent Homology (SDPH) identified 2015–2020 as the key phase of transformation (38,088 m), marking a shift toward higher morphological complexity. A weak negative correlation (r = −0.362) between DTW and SDPH confirmed their complementarity in describing geometric and topological change. Overall, the results suggest that post-tsunami recovery followed a non-linear path toward a new dynamic equilibrium characterized by increased structural complexity and resilience.

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Publication Details

Journal
Remote Sensing
Published
2025-12-09
DOI
https://doi.org/10.3390/rs17243972
Primary Topic
earthquake and tectonic studies
Type
article
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article

Time Series Analysis of Post-Tsunami Coastal Recovery on the Sendai Coastline Using Dynamic Time Warping and Persistent Homology

Muhammad Daniel Iman bin Hussain, Arnob Bormudoi, Masahiko Nagai
Remote Sensing
earthquake and tectonic studies
article

Time Series Analysis of Post-Tsunami Coastal Recovery on the Sendai Coastline Using Dynamic Time Warping and Persistent Homology

Muhammad Daniel Iman bin Hussain, Arnob Bormudoi, Masahiko Nagai
article en

Abstract

This study presents a computational framework combining Dynamic Time Warping (DTW) and Persistent Homology to quantify the long-term morphological evolution of the Sendai coastline following the 2011 Tōhoku tsunami. Using multispectral satellite imagery from Landsat 5 TM, Landsat 8 OLI, and Sentinel-2 MSI (2010–2024), instantaneous shorelines were extracted via the Modified Normalized Difference Water Index (MNDWI) and reconstructed with parametric B-spline curves. DTW analysis indicated severe initial deformation, with a 90,927 m difference between pre- and post-tsunami instantaneous shorelines, followed by gradual stabilization as distances declined to 59,584 m by 2024. Persistent Homology revealed a more complex topological trajectory, with the number of 1-dimensional features (H1) rising sharply after the tsunami, consolidating by 2015, and expanding again to over 8000 by 2020–2024. The Stable Distance of Persistent Homology (SDPH) identified 2015–2020 as the key phase of transformation (38,088 m), marking a shift toward higher morphological complexity. A weak negative correlation (r = −0.362) between DTW and SDPH confirmed their complementarity in describing geometric and topological change. Overall, the results suggest that post-tsunami recovery followed a non-linear path toward a new dynamic equilibrium characterized by increased structural complexity and resilience.

Remote SensingVol. 17(24)
Yamaguchi University (JP), National Intelligence University (US), Assam Down Town University (IN)
Openalex Percentile: Top 60%
earthquake and tectonic studies
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Time Series Analysis of Post-Tsunami Coastal Recovery on the Sendai Coastline Using Dynamic Time Warping and Persistent Homology — Muhammad Daniel Iman bin Hussain, Arnob Bormudoi, et al. · Remote Sensing (2025) | TGRS Research Map | TGRS