Climate change is rapidly deteriorating the climatic signal in Svalbard glaciers
Abstract. The Svalbard archipelago is particularly sensitive to climate change due to the relatively low altitude of its main ice fields and its geographical location in the higher North Atlantic, where the effect of the Arctic Amplification is more significant. The largest temperature increases hav...
Main Authors: | , , , , , , , , , , , , , , , , , , , , , |
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Format: | Report |
Language: | English |
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HAL CCSD
2023
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Online Access: | https://hal.science/hal-04291485 https://doi.org/10.5194/tc-2023-96 |
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ftecolecentrlyon:oai:HAL:hal-04291485v1 |
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record_format |
openpolar |
institution |
Open Polar |
collection |
Portail HAL - Ecole Centrale de Lyon |
op_collection_id |
ftecolecentrlyon |
language |
English |
topic |
[SDU.STU.GL]Sciences of the Universe [physics]/Earth Sciences/Glaciology |
spellingShingle |
[SDU.STU.GL]Sciences of the Universe [physics]/Earth Sciences/Glaciology Spolaor, Andrea Scoto, Federico Larose, Catherine Barbaro, Elena Burgay, Francois Bjorkman, Mats Cappelletti, David Dallo, Federico de Blasi, Fabrizio Divine, Dmitry Dreossi, Giuliano Gabrieli, Jacopo Isaksson, Elisabeth Kohler, Jack Martma, Tonu Schmidt, Louise Schuler, Thomas Stenni, Barbara Turetta, Clara Luks, Bartłomiej Casado, Mathieu Gallet, Jean-Charles Climate change is rapidly deteriorating the climatic signal in Svalbard glaciers |
topic_facet |
[SDU.STU.GL]Sciences of the Universe [physics]/Earth Sciences/Glaciology |
description |
Abstract. The Svalbard archipelago is particularly sensitive to climate change due to the relatively low altitude of its main ice fields and its geographical location in the higher North Atlantic, where the effect of the Arctic Amplification is more significant. The largest temperature increases have been observed during winter, but increasing summer temperatures, above the melting point, have led to increased glacier melt. Here, we evaluate the impact of this increased melt on the preservation of the oxygen isotope signal (δ18O) in firn records. δ18O is commonly used as proxy for past atmospheric temperature reconstructions and, when preserved, it is a crucial parameter to date and align ice cores. By comparing four different firn cores collected in 2012, 2015, 2017 and 2019 at the top of the Holtedahlfonna ice field (1100 m. a.s.l.), we show a progressive deterioration of the isotope signal and we link its degradation to the increased occurrence and intensity of melt events. Although the δ18O signal still reflects the interannual temperature trend, more frequent melting events may in the future affect the interpretation of the isotopic signal, compromising the use of Svalbard ice cores. Our findings highlight the impact and the speed at which Arctic Amplification is affecting Svalbard's cryosphere. |
author2 |
Institute of Polar Sciences Venezia-Mestre (CNR-ISP) National Research Council of Italy CNR Institute of Atmospheric Sciences and Climate (ISAC) Ampère, Département Bioingénierie (BioIng) Ampère (AMPERE) École Centrale de Lyon (ECL) Université de Lyon-Université de Lyon-Université Claude Bernard Lyon 1 (UCBL) Université de Lyon-Institut National des Sciences Appliquées de Lyon (INSA Lyon) Université de Lyon-Institut National des Sciences Appliquées (INSA)-Institut National des Sciences Appliquées (INSA)-Centre National de la Recherche Scientifique (CNRS)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE)-École Centrale de Lyon (ECL) Université de Lyon-Institut National des Sciences Appliquées (INSA)-Institut National des Sciences Appliquées (INSA)-Centre National de la Recherche Scientifique (CNRS)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE) Laboratory of Environmental Chemistry Villigen (LUC) Paul Scherrer Institute (PSI) Göteborgs Universitet = University of Gothenburg (GU) Università degli Studi di Perugia = University of Perugia (UNIPG) University of Ca’ Foscari Venice, Italy Norwegian Polar Institute Tallinn University of Technology (TTÜ) University of Oslo (UiO) Polska Akademia Nauk = Polish Academy of Sciences = Académie polonaise des sciences (PAN) Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE) Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Direction de Recherche Fondamentale (CEA) (DRF (CEA)) Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA) |
format |
Report |
author |
Spolaor, Andrea Scoto, Federico Larose, Catherine Barbaro, Elena Burgay, Francois Bjorkman, Mats Cappelletti, David Dallo, Federico de Blasi, Fabrizio Divine, Dmitry Dreossi, Giuliano Gabrieli, Jacopo Isaksson, Elisabeth Kohler, Jack Martma, Tonu Schmidt, Louise Schuler, Thomas Stenni, Barbara Turetta, Clara Luks, Bartłomiej Casado, Mathieu Gallet, Jean-Charles |
author_facet |
Spolaor, Andrea Scoto, Federico Larose, Catherine Barbaro, Elena Burgay, Francois Bjorkman, Mats Cappelletti, David Dallo, Federico de Blasi, Fabrizio Divine, Dmitry Dreossi, Giuliano Gabrieli, Jacopo Isaksson, Elisabeth Kohler, Jack Martma, Tonu Schmidt, Louise Schuler, Thomas Stenni, Barbara Turetta, Clara Luks, Bartłomiej Casado, Mathieu Gallet, Jean-Charles |
author_sort |
Spolaor, Andrea |
title |
Climate change is rapidly deteriorating the climatic signal in Svalbard glaciers |
title_short |
Climate change is rapidly deteriorating the climatic signal in Svalbard glaciers |
title_full |
Climate change is rapidly deteriorating the climatic signal in Svalbard glaciers |
title_fullStr |
Climate change is rapidly deteriorating the climatic signal in Svalbard glaciers |
title_full_unstemmed |
Climate change is rapidly deteriorating the climatic signal in Svalbard glaciers |
title_sort |
climate change is rapidly deteriorating the climatic signal in svalbard glaciers |
publisher |
HAL CCSD |
publishDate |
2023 |
url |
https://hal.science/hal-04291485 https://doi.org/10.5194/tc-2023-96 |
long_lat |
ENVELOPE(13.730,13.730,79.011,79.011) |
geographic |
Arctic Svalbard Svalbard Archipelago Holtedahlfonna |
geographic_facet |
Arctic Svalbard Svalbard Archipelago Holtedahlfonna |
genre |
Arctic Climate change glacier North Atlantic Svalbard |
genre_facet |
Arctic Climate change glacier North Atlantic Svalbard |
op_source |
https://hal.science/hal-04291485 2023 |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.5194/tc-2023-96 hal-04291485 https://hal.science/hal-04291485 doi:10.5194/tc-2023-96 |
op_doi |
https://doi.org/10.5194/tc-2023-96 |
_version_ |
1801372685748404224 |
spelling |
ftecolecentrlyon:oai:HAL:hal-04291485v1 2024-06-09T07:43:50+00:00 Climate change is rapidly deteriorating the climatic signal in Svalbard glaciers Spolaor, Andrea Scoto, Federico Larose, Catherine Barbaro, Elena Burgay, Francois Bjorkman, Mats Cappelletti, David Dallo, Federico de Blasi, Fabrizio Divine, Dmitry Dreossi, Giuliano Gabrieli, Jacopo Isaksson, Elisabeth Kohler, Jack Martma, Tonu Schmidt, Louise Schuler, Thomas Stenni, Barbara Turetta, Clara Luks, Bartłomiej Casado, Mathieu Gallet, Jean-Charles Institute of Polar Sciences Venezia-Mestre (CNR-ISP) National Research Council of Italy CNR Institute of Atmospheric Sciences and Climate (ISAC) Ampère, Département Bioingénierie (BioIng) Ampère (AMPERE) École Centrale de Lyon (ECL) Université de Lyon-Université de Lyon-Université Claude Bernard Lyon 1 (UCBL) Université de Lyon-Institut National des Sciences Appliquées de Lyon (INSA Lyon) Université de Lyon-Institut National des Sciences Appliquées (INSA)-Institut National des Sciences Appliquées (INSA)-Centre National de la Recherche Scientifique (CNRS)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE)-École Centrale de Lyon (ECL) Université de Lyon-Institut National des Sciences Appliquées (INSA)-Institut National des Sciences Appliquées (INSA)-Centre National de la Recherche Scientifique (CNRS)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE) Laboratory of Environmental Chemistry Villigen (LUC) Paul Scherrer Institute (PSI) Göteborgs Universitet = University of Gothenburg (GU) Università degli Studi di Perugia = University of Perugia (UNIPG) University of Ca’ Foscari Venice, Italy Norwegian Polar Institute Tallinn University of Technology (TTÜ) University of Oslo (UiO) Polska Akademia Nauk = Polish Academy of Sciences = Académie polonaise des sciences (PAN) Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE) Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Direction de Recherche Fondamentale (CEA) (DRF (CEA)) Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA) 2023-11-17 https://hal.science/hal-04291485 https://doi.org/10.5194/tc-2023-96 en eng HAL CCSD info:eu-repo/semantics/altIdentifier/doi/10.5194/tc-2023-96 hal-04291485 https://hal.science/hal-04291485 doi:10.5194/tc-2023-96 https://hal.science/hal-04291485 2023 [SDU.STU.GL]Sciences of the Universe [physics]/Earth Sciences/Glaciology info:eu-repo/semantics/preprint Preprints, Working Papers, . 2023 ftecolecentrlyon https://doi.org/10.5194/tc-2023-96 2024-05-16T14:15:30Z Abstract. The Svalbard archipelago is particularly sensitive to climate change due to the relatively low altitude of its main ice fields and its geographical location in the higher North Atlantic, where the effect of the Arctic Amplification is more significant. The largest temperature increases have been observed during winter, but increasing summer temperatures, above the melting point, have led to increased glacier melt. Here, we evaluate the impact of this increased melt on the preservation of the oxygen isotope signal (δ18O) in firn records. δ18O is commonly used as proxy for past atmospheric temperature reconstructions and, when preserved, it is a crucial parameter to date and align ice cores. By comparing four different firn cores collected in 2012, 2015, 2017 and 2019 at the top of the Holtedahlfonna ice field (1100 m. a.s.l.), we show a progressive deterioration of the isotope signal and we link its degradation to the increased occurrence and intensity of melt events. Although the δ18O signal still reflects the interannual temperature trend, more frequent melting events may in the future affect the interpretation of the isotopic signal, compromising the use of Svalbard ice cores. Our findings highlight the impact and the speed at which Arctic Amplification is affecting Svalbard's cryosphere. Report Arctic Climate change glacier North Atlantic Svalbard Portail HAL - Ecole Centrale de Lyon Arctic Svalbard Svalbard Archipelago Holtedahlfonna ENVELOPE(13.730,13.730,79.011,79.011) |