Posters & presentations

Dell’Agnese, A., Comiti, F., Mao, L., Penna, D., Engel, M., Buzzi,
E., Bertoldi, G. (2012): Linking sediment transport to runoff dynamics in a
glacierized mountain basin (Saldur river, Eastern Italian Alps). International
workshop «Monitoring bedload and debris flows in mountain basins» –
Bozen-Bolzano, 10-12 October 2012.

Varolo, E. & Zerbe, S. (2012): Primary succession on the forefield of the Matsch glacier in South Tyrol: vegetation communities and driving factors. XXII congresso della Societá Italiana di Ecologia. Alessandria, September 10-13th  2012.

Varolo, E. & Zerbe, S.(2012): Primary succession on the foreland of the Matsch glacier, South Tyrol. VII convegno Ricerca Zoologica e Botanica in Alto Adige. Naturmuseum Südtirol, September 06-07th 2012.

Penna, D., Mao, L., Comiti, F., Engel, M., Dell’Agnese, A. and G. Bertoldi (2012): Il ruolo dell’acqua di fusione glaciale e nivale sui deflussi e sul trasporto di
sedimento in sospensione in un torrente alpino d’alta quota. Quaderni di
Idronomia Montana.

Ciccazzo S., Esposito A., Varolo E., Daffonchio D., Zerbe S. and
Brusetti L., Rhizobacterial communities of pioneering plants in freshly deglaciated alpine environments. III SIMTREA congress, Bari June 26-28th 2012.

Esposito A., Ciccazzo S., Daprà L., Brusetti L., A three scale analysis of bacterial communities involved in rock colonization and soil genesis. Best poster in the environmental session of the III SIMTREA congress, Bari June 26-28th 2012.

Engel, M., Bertoldi, G., Penna, D., Comiti, F. (2012): Tracer-based runoff modelling in a
glacierized alpine catchment. In: Geophysical Research Abstracts of EGU
General Assembly. Vienna, Austria, 22-27 April 2012, Vol. 14, EGU2012-2806.

Engel, M., Penna, D., Bertoldi G., Comiti, F. (2012): Tracer-basierte Modellkalibrierung von Abflussprozessen in einem vergletscherten Einzugsgebiet in den Alpen. In M.
Weiler (Eds.): Wasser ohne Grenzen – Proceedings Tag der Hydrology 2012, Forum
für Hydrologie und Wasserbewirtschaftung, Vol. 31, 85 – 90.