Comment on ‘Possible contribution of triboelectricity to snow–air interactions’
Thorsten Bartels-Rausch A C and Martin Schneebeli BA Paul Scherrer Institute, Laboratory of Radiochemistry and Environmental Chemistry, CH-5232 Villigen PSI, Switzerland.
B WSL Institute for Snow and Avalanche Research SLF, CH-7260 Davos, Switzerland. Email: schneebeli@slf.ch
C Corresponding author. Email: thorsten.bartels-rausch@psi.ch
Thorsten Bartels-Rausch studied chemistry at the University of Würzburg, Germany, the Norwegian University of Science and Technology in Trondheim, Norway, and the Swiss Federal Institute of Technology in Zürich (ETH), Switzerland. In 2003, he received his Ph.D. from the University of Bern, Switzerland, for which he investigated the uptake of trace gases to ice surfaces. After a postdoctoral stay at the University of Toronto, he returned to Switzerland and joined the Surface Chemistry group of the Laboratory of Radiochemistry and Environmental Chemistry at the Paul Scherrer Institute, Villigen, Switzerland. His current activities include laboratory studies of mechanisms and kinetics of gas–ice partitioning and reactions in snow and ice. |
Martin Schneebeli is a Senior Scientist with the WSL Institute for Snow and Avalanche Research in Davos, Switzerland. He received his Ph.D. in Soil Physics at ETH Zurich in 1991, before starting to work on snow. In recent years, the focus of his research group is on microstructural characterisation using in-situ tomography of snow and modelling snow properties, developing a better understanding of the processes from the micro- to the macroscale. Recent expeditions to Antarctica helped to understand the extremes of snow metamorphism. |
Environmental Chemistry 9(2) 119-120 https://doi.org/10.1071/EN11147
Submitted: 30 November 2011 Accepted: 20 February 2012 Published:
Journal Compilation © CSIRO Publishing 2012 Open Access CC BY-NC-ND
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