Reanalysing glacier mass balance measurement series

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 hav...

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Bibliographic Details
Published in:The Cryosphere
Main Authors: Zemp, M., Thibert, Emmanuel, Huss, M., Stumm, D., Rolstad Denby, C., Nuth, C., Nussbaumer, S.U., Moholdt, G., Mercer, A., Mayer, C., Joerg, P.C., Jansson, P., Hynek, B., Fischer, A., Escher-Vetter, H., Elvehoy, H., Andreassen, L.M.
Other Authors: Department of Geography, Universität 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), 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)
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2013
Subjects:
Online Access:https://hal.archives-ouvertes.fr/hal-00941911
https://hal.archives-ouvertes.fr/hal-00941911/document
https://hal.archives-ouvertes.fr/hal-00941911/file/gr2013-pub00039496.pdf
https://doi.org/10.5194/tc-7-1227-2013
Description
Summary: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.