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1000 Titel
  • Snow redistribution in an intermediate-complexity snow hydrology modelling framework
1000 Autor/in
  1. Quéno, Louis |
  2. Mott, Rebecca |
  3. Morin, Paul |
  4. Cluzet, Bertrand |
  5. Mazzotti, Giulia |
  6. Jonas, Tobias |
1000 Verlag Copernicus Publications
1000 Erscheinungsjahr 2024
1000 Publikationstyp
  1. Artikel |
1000 Online veröffentlicht
  • 2024-08-09
1000 Erschienen in
1000 Quellenangabe
  • 18(8):3533-3557
1000 Copyrightjahr
  • 2024
1000 Lizenz
1000 Verlagsversion
  • https://doi.org/10.5194/tc-18-3533-2024 |
1000 Publikationsstatus
1000 Begutachtungsstatus
1000 Sprache der Publikation
1000 Abstract/Summary
  • <jats:p>Abstract. Snow hydrological regimes in mountainous catchments are strongly influenced by snowpack heterogeneity resulting from wind- and gravity-induced redistribution processes, requiring them to be modelled at hectometre and finer resolutions. This study presents a novel modelling approach to address this issue, aiming at an intermediate-complexity solution to best represent these processes while maintaining operationally viable computational times. To this end, the physics-based snowpack model FSM2oshd was complemented by integrating the modules SnowTran-3D and SnowSlide to represent wind- and gravity-driven redistribution, respectively. This new modelling framework was further enhanced by implementing a density-dependent layering to account for erodible snow without the need to resolve microstructural properties. Seasonal simulations were performed over a 1180 km2 mountain range in the Swiss Alps at 25, 50 and 100 m resolution, using appropriate downscaling and snow data assimilation techniques to provide accurate meteorological forcing. In particular, wind fields were dynamically downscaled using WindNinja to better reflect topographically induced flow patterns. The model results were assessed using snow depths from airborne lidar measurements. We found a remarkable improvement in the representation of snow accumulation and erosion areas, with major contributions from saltation and suspension as well as avalanches and with modest contributions from snowdrift sublimation. The aggregated snow depth distribution curve, key to snowmelt dynamics, significantly and consistently matched the measured distribution better than reference simulations from the peak of winter to the end of the melt season, with improvements at all spatial resolutions. This outcome is promising for a better representation of snow hydrological processes within an operational framework. </jats:p>
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  1. https://orcid.org/0000-0003-3120-6805|https://frl.publisso.de/adhoc/uri/TW90dCwgUmViZWNjYQ==|https://frl.publisso.de/adhoc/uri/TW9yaW4sIFBhdWw=|https://orcid.org/0000-0003-3300-2056|https://orcid.org/0000-0003-3857-7449|https://frl.publisso.de/adhoc/uri/Sm9uYXMsIFRvYmlhcw==
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1000 Erstellt am 2024-10-02T17:45:48.267+0200
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