Fulltext

Aerodynamic Roughness Length of Fresh Snow

Gromke, Christof ; Manes, Costantino ; Walter, Benjamin ; Lehning, Michael ; Guala, Michele

In: Boundary-Layer Meteorology, 2011, vol. 141, no. 1, p. 21-34

Zum persönliche Liste hinzufügen
    Titel
    • Aerodynamic Roughness Length of Fresh Snow
    Autor
    • Gromke, Christof. WSL Institute for Snow and Avalanche Research SLF, Flueelastr. 11, 7260, Davos, Switzerland
    • Manes, Costantino. Dipartimento di Idraulica, Trasporti e Infrastrutture Civili, Politecnico di Torino, Torino, Italy
    • Walter, Benjamin. WSL Institute for Snow and Avalanche Research SLF, Flueelastr. 11, 7260, Davos, Switzerland
    • Lehning, Michael. WSL Institute for Snow and Avalanche Research SLF, Flueelastr. 11, 7260, Davos, Switzerland
    • Guala, Michele. Saint Anthony Falls Laboratories, University of Minnesota, Minneapolis, MN, USA
    Dokumententyp
    • Postprint
    Sprache
    • Englisch
    Veröffentlicht in
    • Boundary-Layer Meteorology, 2011, vol. 141, no. 1, p. 21-34. Springer Netherlands
    Andere elektronische Ausgabe
    OAI-PMH-ID
    • oai:doc.rero.ch:318455
    Summary
    This study presents the results from a series of wind-tunnel experiments designed to investigate the aerodynamic roughness length z 0 of fresh snow under no-drift conditions. A two-component hot-film anemometer was employed to obtain vertical profiles of velocity statistics in a zero pressure gradient turbulent boundary layer for flow over naturally deposited snow surfaces. The roughness of these snow surfaces was measured by means of digital photography to capture characteristic length scales that can be related to z 0. Our results show that, under aerodynamically rough conditions, the mean value of the roughness length for fresh snow is $${\langle{z}_{0}\rangle= 0.24}$$ mm with a standard deviation σ(z 0)= 0.05 mm. In this study, we show that variations in z 0 are associated with variations in the roughness geometry. The roughness measurements suggest that the estimated values of z 0 are consistent with the presence of irregular roughness structures that develop during snowfalls that mimic ballistic deposition processes