Journal article
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Brief communication: Ad hoc estimation of glacier contributions to sea-level rise from the latest glaciological observations
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Zemp, Michael
Department of Geography, University of Zurich, Zurich, 8057, Switzerland
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Huss, Matthias
Laboratory of Hydraulics, Hydrology and Glaciology (VAW), ETH Zurich, Zurich, 8093, Switzerland - Department of Geosciences, University of Fribourg, Fribourg, 1700, Switzerland - Swiss Federal Institute for Forest, Snow and Landscape Research (WSL), Birmensdorf, Switzerland
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Eckert, Nicolas
Université Grenoble Alpes, INRAE, UR ETGR, Grenoble, 38402, France
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Thibert, Emmanuel
Université Grenoble Alpes, INRAE, UR ETGR, Grenoble, 38402, France
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Paul, Frank
Department of Geography, University of Zurich, Zurich, 8057, Switzerland
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Nussbaumer, Samuel U.
Department of Geography, University of Zurich, Zurich, 8057, Switzerland - Department of Geosciences, University of Fribourg, Fribourg, 1700, Switzerland
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Gärtner-Roer, Isabelle
Department of Geography, University of Zurich, Zurich, 8057, Switzerland
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Published in:
- The Cryosphere. - 2020, vol. 14, no. 3, p. 1043–1050
English
Comprehensive assessments of global glacier mass changes based on a variety of observations and prevailing methodologies have been published at multi-annual intervals. For the years in between, the glaciological method provides annual observations of specific mass changes but is suspected to not be representative at the regional to global scales due to uneven glacier distribution with respect to the full sample. Here, we present a simple approach to estimate and correct for this bias in the glaciological sample and, hence, to provide an ad hoc estimate of global glacier mass changes and corresponding sea-level equivalents for the latest years, i.e. about −300±250 Gt in 2016/17 and −500±200 Gt in 2017/18.
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Faculty
- Faculté des sciences et de médecine
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Department
- Département de Géosciences
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Language
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Classification
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Hydrology
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License
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License undefined
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Identifiers
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Persistent URL
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https://folia.unifr.ch/unifr/documents/308457
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