Scale patterns of the Sentinel-1 SAR-based snow depth product compared with station measurements and airborne LiDAR observations

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Abstract

Water storage in snowpacks in mountainous areas is critical for hydropower production, hydrological forecasting, and freshwater availability. Spaceborne synthetic aperture radar (SAR) is a powerful tool for quantitatively measuring snow mass because of its high spatial resolution and signal sensitivity to snow depth (SD). In particular, the first SAR SD product (C-snow) based on Sentinel-1 satellites displays high sensitivity to depolarization signals for dynamic SD monitoring in mountainous areas. Moreover, upscaled C-snow retrievals (e.g., 10 and 25 km) have been used to provide reference data to train machine learning models, improve passive microwave-based retrieval, and calibrate many hydrological models. However, to date, a systematic assessment of C-snow products at various scales has not been conducted. In this study, the performance of C-snow products at three scales (1, 10 and 25 km) is compared via station-based measurements and airborne LiDAR observations, and the scale patterns associated with the heterogeneity of the geographic environment and the representativeness of so-called true data are analyzed. The scale patterns of C-snow products vary across resolutions. They differ from the patterns observed in the station and airborne reference data. As the spatial scale increases from 1 to 25 km, the error of C-snow retrieval in reference to station measurements tends to increase (e.g., ubRMSE from 69.43 to 81.87 cm; bias from -8.89 to 11.66 cm), whereas it tends to decrease compared with Airborne Snow Observatory (ASO) data, with ubRMSE values ranging from 104.3 to 83.29 cm and bias values ranging from -91.31 to -52.73 cm. We also found that land cover types, e.g., tree cover and permanent ice, affect the C-snow product at various scales. Overestimation tends to occur in coarse pixels covered with even a small amount of permanent ice. The findings indicate that C-snow retrieval at three scales is characterized by high uncertainty. Therefore, researchers should focus on developing a robust SD retrieval algorithm by combining SAR backscattering signals and polarimetric and interferometric information.

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Ying, J., Yang, J., Jiang, L., Pan, J., & Xiong, C. (2026). Scale patterns of the Sentinel-1 SAR-based snow depth product compared with station measurements and airborne LiDAR observations. Cryosphere, 20(1), 227–244. https://doi.org/10.5194/tc-20-227-2026

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