Articles | Volume 13, issue 1
https://doi.org/10.5194/tc-13-325-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/tc-13-325-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Global glacier volume projections under high-end climate change scenarios
Sarah Shannon
CORRESPONDING AUTHOR
School of Geography, University of Exeter, The Queen's Drive,
Exeter, Devon, EX4 4QJ, UK
Bristol Glaciology Centre, Department of Geographical Science,
University Road, University of Bristol, BS8 1SS, UK
Robin Smith
NCAS-Climate, Department of Meteorology, University of Reading,
Reading, RG6 6BB, UK
Andy Wiltshire
Met Office, Fitzroy Road, Exeter, Devon, EX1 3PB, UK
Tony Payne
Bristol Glaciology Centre, Department of Geographical Science,
University Road, University of Bristol, BS8 1SS, UK
Matthias Huss
Department of Geosciences, University of Fribourg, Fribourg,
Switzerland
Laboratory of Hydraulics, Hydrology and Glaciology, ETH Zurich,
Zurich, Switzerland
Richard Betts
School of Geography, University of Exeter, The Queen's Drive,
Exeter, Devon, EX4 4QJ, UK
Met Office, Fitzroy Road, Exeter, Devon, EX1 3PB, UK
John Caesar
Met Office, Fitzroy Road, Exeter, Devon, EX1 3PB, UK
Aris Koutroulis
School of Environmental Engineering, Technical University of Crete,
Akrotiri, 73100 Chania, Greece
Darren Jones
University of Exeter, Penryn Campus, Treliever Road, Penryn, Cornwall,
TR10 9FE, UK
Stephan Harrison
University of Exeter, Penryn Campus, Treliever Road, Penryn, Cornwall,
TR10 9FE, UK
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2 citations as recorded by crossref.
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Latest update: 20 Nov 2024
Short summary
We present global glacier volume projections for the end of this century, under a range of high-end climate change scenarios, defined as exceeding 2 °C global average warming. The ice loss contribution to sea level rise for all glaciers excluding those on the peripheral of the Antarctic ice sheet is 215.2 ± 21.3 mm. Such large ice losses will have consequences for sea level rise and for water supply in glacier-fed river systems.
We present global glacier volume projections for the end of this century, under a range of...