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Mott, R.; Gromke, C.; Grünewald, T.; Lehning, M., 2012:
Relative importance of advective heat transport and boundary layer decoupling in the melt dynamics of a patchy snow cover. Adv. Water Resour. doi.org/10.1016/j.advwatres.2012.03.001. online first, 10 p.

Lehning, M.; Gru¨newald, T.; Marty, C.; Mott, R.; Stähli, M., 2012:
Kleinräumige Schneeverteilung und Einfluss der Topographie. Alpine Schnee- und Wasserresourcen gestern, heute, morgen. Forum für Wissen. 2012: 13-18.

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Mott, R.; Gromke, C.; Grünewald, T.; Lehning, M., 2012:
Advective heat transport and boundary layer decoupling controlling the melt dynamics of a patchy snow cover. [Abstract] Geophys. Res. Abstr. 14: EGU2012-10708.

Mott, R.; Scipion, D.; Berne, A.; Dawes, N.; Lehning, M., 2012:
Dynamics of small-scale precipitation enhancement in moutainous terrain. [Abstract] Geophys. Res. Abstr. 14: EGU2012-7531.

Groot Zwaaftink, C.D.; Löwe, H.; Mott, R.; Bavay, M.; Lehning, M., 2011:
Drifiting snow sublimation: A high-resolution 3-D model with temperature and moisture feedbacks. J. Geophys. Res. 116, D16107, doi: 10.1029/2011JD015754. 14 p.

Mott, R.; Egli, L.; Grünewald, T.; Dawes, N.; Manes, C.; Bavay, M.; Lehning, M., 2011:
Micrometeorological processes driving snow ablation in an Alpine catchment. Cryosphere 5, 4: 1083-1098.

Groot Zwaaftink, C.D.; Löwe, H.; Mott, R.; Bavay, M.; Lehning, M., 2011:
Drifting snow sublimation: A high-resolution 3-D model with temperature and moisture feedbacks. J. Geophys. Res. 116, D16107, doi: 10.1029/2011JD015754: 14 p.

Mott, R.; Schirmer, M.; Lehning, M., 2011:
Scaling properties of wind and snow depth distribution in an Alpine catchment. J. Geophys. Res. 116, D06106, doi:10.1029/2010JD014886. 8 p.

Grünewald, T.; Schirmer, M.; Mott, R.; Lehning, M., 2010:
Spatial and temporal variability of snow depth and SWE in a small mountain catchment. Cryosphere Discuss. 4: 1-30.

Mott, R.; Schirmer, M.; Bavay, M.; Grünewald, T.; Lehning, M., 2010:
Understanding snow-transport processes shaping the mountain snow-cover. Cryosphere 4: 545-559.