Evaluates vegetation impacts from monsoon floods in Himalayan ecosystems, highlighting monitoring techniques.
Extreme hydrometeorological events are increasingly threatening high-mountain environments such as the Himalayas. Sediment-rich debris floods in high-mountain environment pose challenges for satellite-based flood detection, as high turbidity and sediment mixing obscure conventional water spectral signature. This study evaluates the performance of multiple Sentinel-2 spectral indices (normalized difference vegetation index [NDVI], normalized differences water index [NDWI], modified NDWI [MNDWI], and water ratio index [WRI]) for mapping the June 2021 Melamchi River debris flood in central Nepal and assesses post-event vegetation dynamics using NDVI time-series analysis (2019–2024) within Google Earth Engine (GEE). Index-based threshold calibration using stratified random sampling captured open-water areas but tended to overestimate inundation under turbid conditions. In contrast, NDVI decline delineated zones of vegetation removal and sediment burial associated with high-energy debris flows, achieving an overall mapping accuracy of 83% with lower commission error relative to water indices. NDVI is therefore interpreted not as direct water detectors. but as a disturbance proxy in sediment-dominated flood environment. Seasonally consistent NDVI composites were used to assess multi-year vegetation trends. Results indicated that 73.85% of the mapped flood corridors exhibited negative NDVI slope between 2019 and 2024 with degradation spatially concentrated within flood-affected zones. While regional climate variability may also influence vegetation dynamics, the spatial coincidence of degradation with mapped sediment-dominated flood corridors suggests strong geomorphic disturbance effects. The study demonstrates a reproducible, cloud-based workflow for integrating flood extent mapping with multi-year vegetation monitoring in data-scarce mountain regions. These findings highlight the importance of combining disturbance sensitive vegetation indices with conventional water indices when assessing sediment-dominated flood events.
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Thapa et al. (2026) studied this question.
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