Articles | Volume 19, issue 19
https://doi.org/10.5194/gmd-19-9581-2026
https://doi.org/10.5194/gmd-19-9581-2026
Development and technical paper
 | 
12 Oct 2026
Development and technical paper |  | 12 Oct 2026

Improving the CLASSIC (v1.8) snow model to better simulate Arctic snowpacks

Mickaël Lalande, Alexandre Roy, Libo Wang, Diana Verseghy, Vincent Vionnet, Florent Dominé, and Christophe Kinnard

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Cited articles

Abolafia-Rosenzweig, R., He, C., McKenzie Skiles, S., Chen, F., and Gochis, D.: Evaluation and Optimization of Snow Albedo Scheme in Noah-MP Land Surface Model Using In Situ Spectral Observations in the Colorado Rockies, J. Adv. Model. Earth Syst., 14, e2022MS003141, https://doi.org/10.1029/2022MS003141, 2022. a
Abolafia-Rosenzweig, R., He, C., Chen, F., and Barlage, M.: Evaluating and Enhancing Snow Compaction Process in the Noah-MP Land Surface Model, J. Adv. Model. Earth Syst., 16, e2023MS003869, https://doi.org/10.1029/2023MS003869, 2024. a
AMAP: AMAP Arctic Climate Change Update 2024: Key Trends and Impacts, AMAP – Arctic Monitoring and Assessment Programme, Tromsø, Norway, https://doi.org/10.21352/fz60-s852, 2024. a
Amory, C., Kittel, C., Le Toumelin, L., Agosta, C., Delhasse, A., Favier, V., and Fettweis, X.: Performance of MAR (v3.11) in Simulating the Drifting-Snow Climate and Surface Mass Balance of Adélie Land, East Antarctica, Geosci. Model Dev., 14, 3487–3510, https://doi.org/10.5194/gmd-14-3487-2021, 2021. a
Augas, J., Abbasnezhadi, K., Rousseau, A. N., and Baraer, M.: What Is the Trade-Off between Snowpack Stratification and Simulated Snow Water Equivalent in a Physically-Based Snow Model?, Water, 12, 3449, https://doi.org/10.3390/w12123449, 2020. a
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Short summary
This study enhances a snow model for Arctic environments by improving the heat exchanges within the snowpack and at its interfaces, revising the compaction scheme, and adding consideration of blowing snow sublimation losses. Simulations at ten Arctic, mid-latitude, and Alpine sites show significant reductions in simulated soil and snow temperature biases and improved simulated snow depth and density, which are key features to improve simulated energy, water, and carbon budgets in the Arctic.
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