The peer-reviewed scientific article is available online, from the publication date onwards, at http://www.the-cryosphere.net/recent_papers.html. Please contact the EGU Media and Communications Officer if you would like the final version of the paper before the publication date.The discussion paper (before peer review) and reviewers comments is available at
http://www.the-cryosphere-discuss.net/6/2477/2012/tcd-6-2477-2012-discussion.htmlThe team is composed of A. Rabatel (Laboratory of Glaciology and Geophysics of the Environment [LGGE], Joseph Fourier University, Grenoble, France), B. Francou (Laboratory for the Study of Transfers in Hydrology and Environment [LTHE], Joseph Fourier University, Grenoble, France), A. Soruco (Institute of Geological and Environmental Research, Universidad Mayor de San Andres [IGEMA-UMSA], La Paz, Bolivia), J. Gomez (National Water Authority, Glaciology and Water Resources Unit [ANA-UGRH], Huaraz, Peru), B. Cáceres (National Institute of Meteorology and Hydrology [INAMHI], Quito, Ecuador), J. L. Ceballos (Institute of Hydrology, Meteorology and Environmental Studies [IDEAM], Bogotá, Colombia), R. Basantes (LTHE -and- Department of Civil and Environmental Engineering, National Politechnic School [DICA-EPN], Quito, Ecuador), M. Vuille (Department of Atmospheric and Environmental Sciencies, University of Albany, New York, USA), J.-E. Sicart (LTHE), C. Huggel and M. Scheel (Department of Geography, University of Zurich, Switzerland), Y. Lejeune (Snow Research Centre, National Centre for Meteorological Research (CEN CNRM-GAME), Saint Martin d'Hères, France), Y. Arnaud (LTHE), M. Collet (LTHE -and- DICA-EPN), T. Condom (LTHE), G. Consoli (LTHE), V. Favier (LGGE), V. Jomelli (Laboratory of Physical Geography (LPG), University of Paris-Sud, Paris, France), R. Galarraga (DICA-EPN), P. Ginot (LGGE -and- Grenoble Observatory for the Sciences of the Universe (OSUG), Grenoble, France), L. Maisincho (INAMHI), J. Mendoza (Institute of Hydraulics and Hydrology, UMSA [IHH-UMSA], La Paz, Bolivia), M. Ménégoz (LGGE), E. Ramirez (IHH-UMSA), P. Ribstein (Sisyphe, University Pierre and Marie Curie, Paris, France), W. Suarez (National Service of Meteorology and Hydrology (SENAMHI), Lima, Peru), M. Villacis (DICA-EPN), and P. Wagnon (LTHE). Most of these researchers are members of the International Joint Laboratory GREAT-ICE, an initiative of the French Institute of Research for Development (IRD) and universities and institutions in Bolivia, Peru, Ecuador, and Colombia.
Dr. Bárbara Ferreira | European Geosciences Union (EGU)
Further reports about: > Andes Mountains > Bird Communication > Bolivia > EGU > Environment > Geography > Geophysics > Geosciences > Glacier > Glaciology > IPCC > LTHE > Open Access > Water Snake > cryosphere > environmental risk > hydrology > ice thickness > temperature change > tropical glaciers > water equivalent > water resource > water shortage > water supply
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A multi-institutional research collaboration has created a novel approach for fabricating three-dimensional micro-optics through the shape-defined formation of porous silicon (PSi), with broad impacts in integrated optoelectronics, imaging, and photovoltaics.
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In experiments with magnetic atoms conducted at extremely low temperatures, scientists have demonstrated a unique phase of matter: The atoms form a new type of quantum liquid or quantum droplet state. These so called quantum droplets may preserve their form in absence of external confinement because of quantum effects. The joint team of experimental physicists from Innsbruck and theoretical physicists from Hannover report on their findings in the journal Physical Review X.
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The Max Planck Institute for Physics (MPP) is opening up a new research field. A workshop from November 21 - 22, 2016 will mark the start of activities for an innovative axion experiment. Axions are still only purely hypothetical particles. Their detection could solve two fundamental problems in particle physics: What dark matter consists of and why it has not yet been possible to directly observe a CP violation for the strong interaction.
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