Articles | Volume 18, issue 1
https://doi.org/10.5194/tc-18-307-2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Special issue:
https://doi.org/10.5194/tc-18-307-2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
16 Jan 2024
Research article |
| 16 Jan 2024
| 16 Jan 2024
Climate change is rapidly deteriorating the climatic signal in Svalbard glaciers
CNR-Institute of Polar Science (ISP), Campus Scientifico, Via Torino 155, 30172 Venice-Mestre, Italy
Department of Environmental Sciences, Informatics and Statistics, Ca' Foscari University, Venice, Italy
Federico Scoto
Institute of Atmospheric Sciences and Climate, ISAC-CNR. Campus Ecotekne, 73100 Lecce, Italy
Department of Environmental Sciences, Informatics and Statistics, Ca' Foscari University, Venice, Italy
Catherine Larose
Institut des Géosciences de l'Environnement (IGE), Université Grenoble Alpes, CNRS, IRD, Grenoble INP, Grenoble 38000, France
Elena Barbaro
CNR-Institute of Polar Science (ISP), Campus Scientifico, Via Torino 155, 30172 Venice-Mestre, Italy
Department of Environmental Sciences, Informatics and Statistics, Ca' Foscari University, Venice, Italy
Francois Burgay
Laboratory of Environmental Chemistry (LUC), Paul Scherrer Institute, 5232 Villigen PSI, Switzerland
Department of Environmental Sciences, Informatics and Statistics, Ca' Foscari University, Venice, Italy
Mats P. Bjorkman
Department of Earth Sciences, University of Gothenburg, Box 460, 40530 Göteborg, Sweden
David Cappelletti
Dipartimento di Chimica, Biologia e Biotecnologie, Università degli Studi di Perugia, 06123 Perugia, Italy
Federico Dallo
Department of Environmental Sciences, Informatics and Statistics, Ca' Foscari University, Venice, Italy
Fabrizio de Blasi
CNR-Institute of Polar Science (ISP), Campus Scientifico, Via Torino 155, 30172 Venice-Mestre, Italy
Department of Environmental Sciences, Informatics and Statistics, Ca' Foscari University, Venice, Italy
Dmitry Divine
Norwegian Polar Institute, Tromsø 9296, Norway
Giuliano Dreossi
CNR-Institute of Polar Science (ISP), Campus Scientifico, Via Torino 155, 30172 Venice-Mestre, Italy
Department of Environmental Sciences, Informatics and Statistics, Ca' Foscari University, Venice, Italy
Jacopo Gabrieli
CNR-Institute of Polar Science (ISP), Campus Scientifico, Via Torino 155, 30172 Venice-Mestre, Italy
Department of Environmental Sciences, Informatics and Statistics, Ca' Foscari University, Venice, Italy
Elisabeth Isaksson
Norwegian Polar Institute, Tromsø 9296, Norway
Jack Kohler
Norwegian Polar Institute, Tromsø 9296, Norway
Tonu Martma
Department of Geology, Tallinn University of Technology, Ehitajate tee 5, 19086 Tallinn, Estonia
Louise S. Schmidt
Department of Geosciences, University of Oslo, Oslo, Norway
Thomas V. Schuler
Department of Geosciences, University of Oslo, Oslo, Norway
Barbara Stenni
Department of Environmental Sciences, Informatics and Statistics, Ca' Foscari University, Venice, Italy
Clara Turetta
CNR-Institute of Polar Science (ISP), Campus Scientifico, Via Torino 155, 30172 Venice-Mestre, Italy
Department of Environmental Sciences, Informatics and Statistics, Ca' Foscari University, Venice, Italy
Bartłomiej Luks
Institute of Geophysics, Polish Academy of Sciences, Księcia Janusza 64, 01-452 Warsaw, Poland
Mathieu Casado
Laboratoire des Sciences du Climat et de l'Environnement, CEA–CNRS–UVSQ–Paris-Saclay–IPSL, Gif-sur-Yvette, France
Jean-Charles Gallet
Norwegian Polar Institute, Tromsø 9296, Norway
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Latest update: 07 May 2024
Short summary
We evaluate the impact of the increased snowmelt on the preservation of the oxygen isotope (δ18O) signal in firn records recovered from the top of the Holtedahlfonna ice field located in the Svalbard archipelago. Thanks to a multidisciplinary approach we demonstrate a progressive deterioration of the isotope signal in the firn core. We link the degradation of the δ18O signal to the increased occurrence and intensity of melt events associated with the rapid warming occurring in the archipelago.
We evaluate the impact of the increased snowmelt on the preservation of the oxygen isotope...
