Brief communication: Do 1.0, 1.5, or 2.0 °C matter for the future evolution of Alpine glaciers?
With the Paris Agreement, the urgency of limiting ongoing anthropogenic climate change has been recognised. More recent discussions have focused on the difference of limiting the increase in global average temperatures below 1.0, 1.5, or 2.0 ∘C compared to preindustrial levels. Here, we assess the i...
Main Authors: | , , , , , , , , |
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Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Copernicus
2021
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Subjects: | |
Online Access: | https://hdl.handle.net/20.500.11850/489966 https://doi.org/10.3929/ethz-b-000489966 |
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author | Compagno, Loris id_orcid:0 000-0002-5422-7281 Eggs, Sarah Huss, Matthias id_orcid:0 000-0002-2377-6923 Zekollari, Harry id_orcid:0 000-0002-7443-4034 Farinotti, Daniel id_orcid:0 000-0003-3417-4570 |
author_facet | Compagno, Loris id_orcid:0 000-0002-5422-7281 Eggs, Sarah Huss, Matthias id_orcid:0 000-0002-2377-6923 Zekollari, Harry id_orcid:0 000-0002-7443-4034 Farinotti, Daniel id_orcid:0 000-0003-3417-4570 |
author_sort | Compagno, Loris |
collection | ETH Zürich Research Collection |
description | With the Paris Agreement, the urgency of limiting ongoing anthropogenic climate change has been recognised. More recent discussions have focused on the difference of limiting the increase in global average temperatures below 1.0, 1.5, or 2.0 ∘C compared to preindustrial levels. Here, we assess the impacts that such different scenarios would have on both the future evolution of glaciers in the European Alps and the water resources they provide. Our results show that even half-degree differences in global temperature targets have important implications for the changes predicted until 2100, and that – for the most optimistic scenarios – glaciers might start to partially recover, owing to possibly decreasing temperatures after the end of the 21st century. ISSN:1994-0416 ISSN:1994-0424 |
format | Article in Journal/Newspaper |
genre | The Cryosphere |
genre_facet | The Cryosphere |
id | ftethz:oai:www.research-collection.ethz.ch:20.500.11850/489966 |
institution | Open Polar |
language | English |
op_collection_id | ftethz |
op_doi | https://doi.org/20.500.11850/48996610.3929/ethz-b-00048996610.5194/tc-15-2593-2021 |
op_relation | info:eu-repo/semantics/altIdentifier/doi/10.5194/tc-15-2593-2021 info:eu-repo/semantics/altIdentifier/wos/000663922000001 info:eu-repo/grantAgreement/SNF/Projekte MINT/184634 http://hdl.handle.net/20.500.11850/489966 |
op_rights | info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by/4.0/ Creative Commons Attribution 4.0 International |
op_source | The Cryosphere, 15 (6) |
publishDate | 2021 |
publisher | Copernicus |
record_format | openpolar |
spelling | ftethz:oai:www.research-collection.ethz.ch:20.500.11850/489966 2025-03-30T15:28:58+00:00 Brief communication: Do 1.0, 1.5, or 2.0 °C matter for the future evolution of Alpine glaciers? Compagno, Loris id_orcid:0 000-0002-5422-7281 Eggs, Sarah Huss, Matthias id_orcid:0 000-0002-2377-6923 Zekollari, Harry id_orcid:0 000-0002-7443-4034 Farinotti, Daniel id_orcid:0 000-0003-3417-4570 2021-06-15 application/application/pdf https://hdl.handle.net/20.500.11850/489966 https://doi.org/10.3929/ethz-b-000489966 en eng Copernicus info:eu-repo/semantics/altIdentifier/doi/10.5194/tc-15-2593-2021 info:eu-repo/semantics/altIdentifier/wos/000663922000001 info:eu-repo/grantAgreement/SNF/Projekte MINT/184634 http://hdl.handle.net/20.500.11850/489966 info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by/4.0/ Creative Commons Attribution 4.0 International The Cryosphere, 15 (6) info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2021 ftethz https://doi.org/20.500.11850/48996610.3929/ethz-b-00048996610.5194/tc-15-2593-2021 2025-03-05T22:09:16Z With the Paris Agreement, the urgency of limiting ongoing anthropogenic climate change has been recognised. More recent discussions have focused on the difference of limiting the increase in global average temperatures below 1.0, 1.5, or 2.0 ∘C compared to preindustrial levels. Here, we assess the impacts that such different scenarios would have on both the future evolution of glaciers in the European Alps and the water resources they provide. Our results show that even half-degree differences in global temperature targets have important implications for the changes predicted until 2100, and that – for the most optimistic scenarios – glaciers might start to partially recover, owing to possibly decreasing temperatures after the end of the 21st century. ISSN:1994-0416 ISSN:1994-0424 Article in Journal/Newspaper The Cryosphere ETH Zürich Research Collection |
spellingShingle | Compagno, Loris id_orcid:0 000-0002-5422-7281 Eggs, Sarah Huss, Matthias id_orcid:0 000-0002-2377-6923 Zekollari, Harry id_orcid:0 000-0002-7443-4034 Farinotti, Daniel id_orcid:0 000-0003-3417-4570 Brief communication: Do 1.0, 1.5, or 2.0 °C matter for the future evolution of Alpine glaciers? |
title | Brief communication: Do 1.0, 1.5, or 2.0 °C matter for the future evolution of Alpine glaciers? |
title_full | Brief communication: Do 1.0, 1.5, or 2.0 °C matter for the future evolution of Alpine glaciers? |
title_fullStr | Brief communication: Do 1.0, 1.5, or 2.0 °C matter for the future evolution of Alpine glaciers? |
title_full_unstemmed | Brief communication: Do 1.0, 1.5, or 2.0 °C matter for the future evolution of Alpine glaciers? |
title_short | Brief communication: Do 1.0, 1.5, or 2.0 °C matter for the future evolution of Alpine glaciers? |
title_sort | brief communication: do 1.0, 1.5, or 2.0 °c matter for the future evolution of alpine glaciers? |
url | https://hdl.handle.net/20.500.11850/489966 https://doi.org/10.3929/ethz-b-000489966 |