Reanalysing glacier mass balance measurement series

Autor: Michael Zemp, Matthias Huss, Philip C. Joerg, H. Escher-Vetter, Samuel U. Nussbaumer, D. Stumm, Hallgeir Elvehøy, C. Rolstad Denby, Bernhard Hynek, Andrew Mercer, Andrea Fischer, Christopher Nuth, Christoph Mayer, Emmanuel Thibert, Geir Moholdt, Peter Jansson, Liss M. Andreassen
Přispěvatelé: Department of Geography, University of Zürich [Zürich] (UZH), Erosion torrentielle neige et avalanches (UR ETGR (ETNA)), Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA), Department of Geosciences, Albert-Ludwigs-Universität Freiburg, International Centre for Integrated Mountain Development, ICIMOD, Norwegian University of Life Sciences (NMBU), University of Oslo (UiO), Stockholm University Library (SUB), Stockholm University, Commission for Geodesy and Glaciology, Bavarian Academy of Sciences and Humanities, aucun, Zentralanstalt für Meteorologie und Geodynamik (ZAMG), Institute for Interdisciplinary Mountain Research, Austrian Academy of Sciences, Norwegian Institute for Water Research (NIVA), University of Zurich, Zemp, Michael, Universität Zürich [Zürich] = University of Zurich (UZH), International Centre for Integrated Mountain Development (ICIMOD), Marcus Wallenberg Foundation for International Cooperation in Science, Wenner-Gren Foundations, International Union of Geology and Geophysics (IUGG) through the International Association of Cryospheric Sciences (IACS), International Glaciological Society (IGS)
Jazyk: angličtina
Rok vydání: 2013
Předmět:
Zdroj: The Cryosphere, Vol 7, Iss 4, Pp 1227-1245 (2013)
The Cryosphere
The Cryosphere, Copernicus 2013, 7 (4), p. 1227-p. 1245. ⟨10.5194/tc-7-1227-2013⟩
ISSN: 1994-0424
1994-0416
DOI: 10.5194/tc-7-1227-2013⟩
Popis: Glacier-wide mass balance has been measured for more than sixty years and is widely used as an indicator of climate change and to assess the glacier contribution to runoff and sea level rise. Until recently, comprehensive uncertainty assessments have rarely been carried out and mass balance data have often been applied using rough error estimation or without consideration of errors. In this study, we propose a framework for reanalysing glacier mass balance series that includes conceptual and statistical toolsets for assessment of random and systematic errors, as well as for validation and calibration (if necessary) of the glaciological with the geodetic balance results. We demonstrate the usefulness and limitations of the proposed scheme, drawing on an analysis that comprises over 50 recording periods for a dozen glaciers, and we make recommendations to investigators and users of glacier mass balance data. Reanalysing glacier mass balance series needs to become a standard procedure for every monitoring programme to improve data quality, including reliable uncertainty estimates.
Databáze: OpenAIRE