the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
SnowGalileo: A Pre-trained Earth Observation Transformer for Daily, 100 m Fractional Snow Cover Mapping
Abstract. Mountain snow is an important component of the cryosphere that directly affects downstream livelihoods. Accurate monitoring of mountain snow is crucial, yet remains challenging due to complex topography and frequent cloud cover. Although combining data from multiple Earth Observation (EO) satellites can improve spatial and temporal coverage, extracting Fractional Snow Cover (FSC) from sensors with different spatial and temporal resolutions remains difficult. AI-based Earth foundation models can process diverse sensor inputs and have been successfully applied to various remote sensing tasks; however, they often lack snow-specific design considerations. This paper presents SnowGalileo, a pre-trained transformer model designed to integrate EO data to map snow-covered areas. We evaluated SnowGalileo's potential for generating daily, gap-free FSC maps at 100m resolution in mountainous regions. SnowGalileo combines one week of satellite time-series data from multiple sensors, including Sentinel-1, Sentinel-2, Landsat, Sentinel-3, MODIS, and VIIRS, with topographic, land cover, and meteorological information to predict FSC for a given day. The model was pre-trained using masked autoencoding and fine-tuned using labeled data from various mountain ranges across the Northern Hemisphere. In addition to clear-sky conditions, SnowGalileo is evaluated under a wider variety of conditions than was previously possible, including cloud cover and lack of high-resolution (~10–30 m) satellite imagery. For the Canadian Rockies and the Swiss Alps, respectively, SnowGalileo achieves RMSEs of 0.099 and 0.124 on clear days, 0.144 and 0.209 on cloudy days, 0.185 and 0.262 on days without high-resolution imagery, and 0.200 and 0.299 on cloudy days without high-resolution imagery. SnowGalileo also consistently outperforms random forests, support vector regressors, and multi-layer perceptrons. While the current product is a proof of concept that has undergone limited validation across geographic regions, operates on 1km × 1km tiles rather than full maps, and has restricted capabilities in challenging conditions, this approach could ultimately enable the continuous, gap-free operational generation of FSC time series for mountain regions worldwide.
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Status: open (until 24 Oct 2026)
- RC1: 'Comment on egusphere-2026-3833', Anonymous Referee #1, 29 Sep 2026 reply
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- 1
The manuscript presents a novel methodology that adapts and fine-tunes the Galileo Earth Foundation Model (Tseng et al., 2025) for daily FSCA mapping at 100m. The model integrates multi-sensor satellite observations, climate reanalysis products, and other ancillary variables. The authors report that their model achieves much better performance compared to traditional ML models when evaluated in the Canadian Rockies and the Swiss Alps under various conditions (e.g., cloudy or cloud-free, with or without high resolution images, various canopy density).
The method shows scientific novelty, like the use of EFM, considering the temporal sequence to deal with the cloud contamination, the fusion of multi-sensor high resolution images with moderate high spatial resolution sensors for mapping of daily FSCA at finer spatial resolution, etc., and the results indicate value to the cryospheric remote sensing community. However, the manuscript in its current form is not suitable for publication.
I have a couple major concerns:
1) A major claim of this paper is its ability to overcome cloud contamination, which is one of the primary challenges in optical snow mapping. However, rather than evaluating the model on images contaminated with real clouds, the authors used an open-source cloud generator tool (Czerkawski et al., 2023) to simulate synthetic clouds. It is scientifically invalid to claim a methodology solves cloud contamination without validating it against satellite data with real cloud cover.
2) Additionally, the model is validated across a mere 16 scenes. For an EFM claiming broad generalizability across complex mountain terrains, this sample size is insufficient to prove scientific robustness. Extra validation datasets, such as lidar-based high-resolution snow cover or other high-resolution FSCA products across other mountain regions, are necessary to truly evaluate the transferability and generalization of this model.
3) Lastly, the uncertainty of the FSCA in the high-resolution Landsat and Sentinel datasets is not well discussed or evaluated. How do these uncertainties propagate into the EFM, and how do they ultimately impact the final FSCA accuracy? Furthermore, the labeled target FSCA appears to be based on an equation designed to convert MODIS NDSI to FSCA, which is not evaluated using a Landsat dataset. The authors must clarify how the labeled FSCA data was generated (Section 3.2.2). It appears the target data does not include images with clouds. I am curious: how does the model learn to correctly predict FSCA under clouds if it is never trained on target labels that exist under cloudy conditions?
The organization of the manuscript is highly circular and confusing, mixing methodology with results. Descriptions of the datasets used, the model introduction, the pre-training, and the fine-tuning processes are scattered across different sections, making it very difficult to understand what was actually done in this study versus what was already done in previous studies. Additionally, the Results section contains lengthy methodological explanations that do not belong there.
Some examples:
I strongly encourage the authors to completely revision the manuscript to provide a rigorous academic context, and to redesign the validation experiment using real (not simulated) cloud-contaminated data.
Specific comments:
Abstract
Introduction & Background
Some examples: