Leveraging Weekly Snow Cover Time Series for Improved Glacier Monitoring and Modeling

Abstract Seasonal snow and ice melt strongly influence glacier mass balance, yet sparse sub‐annual observations limit our understanding of seasonal dynamics. Here we construct and analyze weekly snow cover time series for 200 glaciers across western North America from 2013 to 2023 using an automated image processing pipeline. Snow cover varied widely across the region: snow minima timing varied with latitude — from August from 62 to 64N to October from 48 to 50N—and accumulation area ratios ranged from near‐zero to 0.92 (median of 0.52). A comparison of snowlines from observations and the PyGEM glacier mass balance model revealed seasonally evolving but spatially consistent biases in modeled snowlines: observed snowlines rose earlier, but at a slower rate throughout the melt season, than modeled snowlines. Beyond capturing glacier state, snowline observations efficiently provide sub‐seasonal mass balance constraints and empirically represent unresolved processes like snow redistribution, refining model gradients and improving projections.

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Publication Details

Journal
Geophysical Research Letters
Published
2025-06-30
DOI
https://doi.org/10.1029/2025gl115523
Citations
1
Primary Topic
Cryospheric studies and observations
Type
article
Field-Weighted Citation Impact
1.30

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article

Leveraging Weekly Snow Cover Time Series for Improved Glacier Monitoring and Modeling

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Cryospheric studies and observations
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article

Leveraging Weekly Snow Cover Time Series for Improved Glacier Monitoring and Modeling

B. S. Tober, S. O’Neel, David R. Rounce, Alexandra Friel, Ellyn M. Enderlin, Rainey Aberle
article en
1 citations

Abstract

Abstract Seasonal snow and ice melt strongly influence glacier mass balance, yet sparse sub‐annual observations limit our understanding of seasonal dynamics. Here we construct and analyze weekly snow cover time series for 200 glaciers across western North America from 2013 to 2023 using an automated image processing pipeline. Snow cover varied widely across the region: snow minima timing varied with latitude — from August from 62 to 64N to October from 48 to 50N—and accumulation area ratios ranged from near‐zero to 0.92 (median of 0.52). A comparison of snowlines from observations and the PyGEM glacier mass balance model revealed seasonally evolving but spatially consistent biases in modeled snowlines: observed snowlines rose earlier, but at a slower rate throughout the melt season, than modeled snowlines. Beyond capturing glacier state, snowline observations efficiently provide sub‐seasonal mass balance constraints and empirically represent unresolved processes like snow redistribution, refining model gradients and improving projections.

Geophysical Research LettersVol. 52(13)
Boise State University (US), United States Army Corps of Engineers (US), Cold Regions Research and Engineering Laboratory (US), Carnegie Mellon University (US)
National Aeronautics and Space Administration, Idaho Space Grant Consortium
Openalex Percentile: Top 21%
Cryospheric studies and observations
1.30
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