Global glacier change in the 21st century: Every increase in temperature matters.


Journal

Science (New York, N.Y.)
ISSN: 1095-9203
Titre abrégé: Science
Pays: United States
ID NLM: 0404511

Informations de publication

Date de publication:
06 01 2023
Historique:
entrez: 5 1 2023
pubmed: 6 1 2023
medline: 10 1 2023
Statut: ppublish

Résumé

Glacier mass loss affects sea level rise, water resources, and natural hazards. We present global glacier projections, excluding the ice sheets, for shared socioeconomic pathways calibrated with data for each glacier. Glaciers are projected to lose 26 ± 6% (+1.5°C) to 41 ± 11% (+4°C) of their mass by 2100, relative to 2015, for global temperature change scenarios. This corresponds to 90 ± 26 to 154 ± 44 millimeters sea level equivalent and will cause 49 ± 9 to 83 ± 7% of glaciers to disappear. Mass loss is linearly related to temperature increase and thus reductions in temperature increase reduce mass loss. Based on climate pledges from the Conference of the Parties (COP26), global mean temperature is projected to increase by +2.7°C, which would lead to a sea level contribution of 115 ± 40 millimeters and cause widespread deglaciation in most mid-latitude regions by 2100.

Identifiants

pubmed: 36603094
doi: 10.1126/science.abo1324
doi:

Types de publication

Journal Article

Langues

eng

Sous-ensembles de citation

IM

Pagination

78-83

Commentaires et corrections

Type : CommentIn

Auteurs

David R Rounce (DR)

Department of Civil and Environmental Engineering, Carnegie Mellon University, Pittsburgh, PA, USA.
Geophysical Institute, University of Alaska Fairbanks, Fairbanks, AK, USA.

Regine Hock (R)

Geophysical Institute, University of Alaska Fairbanks, Fairbanks, AK, USA.
Department of Geosciences, University of Oslo, Oslo, Norway.

Fabien Maussion (F)

Department of Atmospheric and Cryospheric Sciences, University of Innsbruck, Innsbruck, Austria.

Romain Hugonnet (R)

Laboratory of Hydraulics, Hydrology and Glaciology (VAW), ETH Zürich, Zurich, Switzerland.
Swiss Federal Institute for Forest, Snow and Landscape Research (WSL), Birmensdorf, Switzerland.
LEGOS, Université de Toulouse, CNES, CNRS, IRD, UPS, Toulouse, France.

William Kochtitzky (W)

Department of Geography, Environment and Geomatics, University of Ottawa, Ottawa, Ontario, Canada.
School of Marine and Environmental Programs, University of New England, Biddeford, ME, USA.

Matthias Huss (M)

Laboratory of Hydraulics, Hydrology and Glaciology (VAW), ETH Zürich, Zurich, Switzerland.
Swiss Federal Institute for Forest, Snow and Landscape Research (WSL), Birmensdorf, Switzerland.
Department of Geosciences, University of Fribourg, Fribourg, Switzerland.

Etienne Berthier (E)

LEGOS, Université de Toulouse, CNES, CNRS, IRD, UPS, Toulouse, France.

Douglas Brinkerhoff (D)

Department of Computer Science, University of Montana, Missoula, MT, USA.

Loris Compagno (L)

Laboratory of Hydraulics, Hydrology and Glaciology (VAW), ETH Zürich, Zurich, Switzerland.
Swiss Federal Institute for Forest, Snow and Landscape Research (WSL), Birmensdorf, Switzerland.

Luke Copland (L)

Department of Geography, Environment and Geomatics, University of Ottawa, Ottawa, Ontario, Canada.

Daniel Farinotti (D)

Laboratory of Hydraulics, Hydrology and Glaciology (VAW), ETH Zürich, Zurich, Switzerland.
Swiss Federal Institute for Forest, Snow and Landscape Research (WSL), Birmensdorf, Switzerland.

Brian Menounos (B)

Geography Earth and Environmental Sciences, University of Northern British Columbia, Prince George, BC, Canada.
Hakai Institute, Campbell River, BC, Canada.

Robert W McNabb (RW)

School of Geography and Environmental Sciences, Ulster University, Coleraine, UK.

Classifications MeSH