Preprints
https://doi.org/10.5194/egusphere-2025-6409
https://doi.org/10.5194/egusphere-2025-6409
12 Jan 2026
 | 12 Jan 2026
Status: this preprint is open for discussion and under review for Natural Hazards and Earth System Sciences (NHESS).

Optimizing SAR Flood Extent Mapping in Central Chile: The Critical Role of Image Timing

Lester Olivares and Gabriel González

Abstract. This study critically quantifies the temporal uncertainty inherent in flood extent estimation using Sentinel-1 SAR data in the high-relief, flash-flood-prone river systems of Central Chile, following the extreme events of 2023. We applied the iterative Jaccard optimization framework to five sites in the Maule and Mataquito watersheds, identifying the Difference Image Index (DII) as the most robust flood indicator. Our key finding is that the estimation of maximum flood extent is fundamentally limited by the timing of the SAR acquisition. River gauge analysis confirmed a flash-flood regime with an extremely rapid recession rate (river height dropping ∼ 50 % within four days of the peak). This rapid drainage means that a delay of 24–48 hours results in a severe underestimation of the true flood footprint. While the DII performed best, overall Jaccard scores remained low (≤ 0.6). We conclude that the method's accuracy is primarily constrained by physical limitations- namely, the rapid recession rate and complex topography- rather than the calibration technique itself. Relying solely on the Sentinel 1 revisit cycle is insufficient for operational mapping in such dynamic environments, and we recommend integrating SAR monitoring with hydraulic modeling or high-frequency aerial surveys to accurately interpolate the maximum flood extent.

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Lester Olivares and Gabriel González

Status: open (until 23 Feb 2026)

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Lester Olivares and Gabriel González
Lester Olivares and Gabriel González
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Short summary
In Central Chile's steep watersheds, floodwaters recede by 50 % within days of peaking. This rapid "flash-flood" drainage creates a temporal mismatch with satellite schedules. A radar image captured just 24 hours late misses the peak, recording only a minimum flood area rather than the true severity. In these high-relief environments, physical drainage limits satellite accuracy, making it essential to combine snapshots with models to reconstruct the full extent of the disaster.
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