Medium-resolution (10-30 m) burned area mapping is vital for monitoring wildfires and their impacts, but remains difficult to scale. Existing methods require either curated fire-specific imagery or dense time-series analysis. Here, we tested whether annual Earth-observation embeddings retain wildfire disturbance signals sufficiently to map burned areas without either requirement. Using Tessera and AlphaEarth embeddings, we tested individual burn-scar delineation, mapping of all same-year fires within an area, regional wall-to-wall mapping, cross-continental transfer, and intra-annual fire timing. Tessera strongly encoded wildfire disturbance, allowing even linear models to separate burned from unburned pixels; the signal was weaker in AlphaEarth. Models trained on a single Tessera embedding matched or exceeded equivalent models using paired pre- and post-fire HLS imagery, and outperformed post-fire imagery alone. The same approach mapped all same-year fires within benchmark scenes (F1 = 0.90). Applied across California, with no California fire data used for downstream training, it recovered 97% of reference burned area and detected substantially more small and medium-sized fires than GABAM or MCD64A1. Separately, a model trained on 2018-2021 US fires transferred without retraining to 88 European fires from 2024-2025 (F1 = 0.88). For well-detected fires, ignition timing was recovered with a mean absolute error of 13 days. Performance declined for fires ignited near the end of the calendar year, and wall-to-wall deployment produced systematic false positives in some unseen landscapes. Annual embeddings nevertheless achieve high segmentation accuracy while moving the burden of dense time series processing upstream, providing a promising path towards simpler regional burned area mapping.
Frozen Earth-observation embeddings are judged almost entirely by spatially blocked cross-validation inside one study region; it is shown that this number does not predict accuracy in a new region; it is shown why; and the one setting in which such a model does keep working is shown.
Philip Stark, A. Sopasakis, Ola Hall· arXiv.org· 0 citations
Ecological monitoring, carbon accounting and biodiversity assessment increasingly rely on annual Earth embeddings--learned vectors that compress a year of satellite observation for every ten-meter pixel on Earth, consumed in place of the imagery itself. What these vectors mean has not been established. Here we decompos...
Kelp forests are vital marine habitats with significant ecological, cultural, and economic importance. These ecosystems, found along coastlines, are susceptible to regional and global stressors including coastal development and climate change. This paper presents Satellite-based Kelp Mapping (SKeMa), a novel framework...
M. Ghanbari, Neil A. Ernst, Taylor Denouden et al.· Remote Sensing· 0 citations
TESSERA latent embeddings are a well-suitable input to fraction mapping, performing slightly better than spectral-temporal-metrics-based models in many cases, but spline coefficients generally perform best when sufficient high-quality observations are available.
Franz Schug, David Klehr, J. Mahler et al.· 0 citations
Reliable daily wildfire forecasting is essential for early warning, air-quality management, and reducing smoke-related health exposure. However, global approaches generally emphasize either fire-weather danger or pixel-wise occurrence prediction and do not explicitly represent temporal persistence, neighboring-grid c...
Tong Wu, Zhi-Jiong Huang, Jia-Shu Ye et al.· ACS ES&T Air· 0 citations
Flood peak depth on normally dry land governs damage and risk to life, but is observed only sparsely, by post-event high-water mark (HWM) surveys, and depth derived from satellite flood extent is produced after the event and inherits the vertical error of the digital elevation model (DEM) it is computed from. Deep-lear...
Wen Zhou, Shao-Wen Wang, Upmanu Lall et al.· 0 citations
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