Late twentieth century increase in northern Spitsbergen (Svalbard) glacier-derived runoff tracked by coralline algal Ba/Ca ratios

The Arctic cryosphere is changing rapidly due to global warming. Northern Svalbard is a warming hotspot with a temperature rise of ~ 6 °C over the last three decades. Concurrently, modelled data suggest a marked increase in glacier runoff during recent decades in northern Svalbard, and runoff is pro...

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Published in:Climate Dynamics
Main Authors: Hetzinger, Steffen, Halfar, Jochen, Zajacz, Zoltan, Möller, Marco, Wisshak, Max
Format: Article in Journal/Newspaper
Language:English
Published: Springer 2021
Subjects:
Online Access:https://oceanrep.geomar.de/id/eprint/51660/
https://oceanrep.geomar.de/id/eprint/51660/1/Hetzinger.pdf
https://oceanrep.geomar.de/id/eprint/51660/7/382_2021_5642_MOESM2_ESM.pdf
https://oceanrep.geomar.de/id/eprint/51660/8/382_2021_5642_MOESM1_ESM.xlsx
https://oceanrep.geomar.de/id/eprint/51660/14/Hetzinger2021_Article_LateTwentiethCenturyIncreaseIn.pdf
https://doi.org/10.1007/s00382-021-05642-x
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spelling ftoceanrep:oai:oceanrep.geomar.de:51660 2024-02-11T09:59:52+01:00 Late twentieth century increase in northern Spitsbergen (Svalbard) glacier-derived runoff tracked by coralline algal Ba/Ca ratios Hetzinger, Steffen Halfar, Jochen Zajacz, Zoltan Möller, Marco Wisshak, Max 2021-01-24 text other https://oceanrep.geomar.de/id/eprint/51660/ https://oceanrep.geomar.de/id/eprint/51660/1/Hetzinger.pdf https://oceanrep.geomar.de/id/eprint/51660/7/382_2021_5642_MOESM2_ESM.pdf https://oceanrep.geomar.de/id/eprint/51660/8/382_2021_5642_MOESM1_ESM.xlsx https://oceanrep.geomar.de/id/eprint/51660/14/Hetzinger2021_Article_LateTwentiethCenturyIncreaseIn.pdf https://doi.org/10.1007/s00382-021-05642-x en eng Springer https://oceanrep.geomar.de/id/eprint/51660/1/Hetzinger.pdf https://oceanrep.geomar.de/id/eprint/51660/7/382_2021_5642_MOESM2_ESM.pdf https://oceanrep.geomar.de/id/eprint/51660/8/382_2021_5642_MOESM1_ESM.xlsx https://oceanrep.geomar.de/id/eprint/51660/14/Hetzinger2021_Article_LateTwentiethCenturyIncreaseIn.pdf Hetzinger, S. , Halfar, J., Zajacz, Z., Möller, M. and Wisshak, M. (2021) Late twentieth century increase in northern Spitsbergen (Svalbard) glacier-derived runoff tracked by coralline algal Ba/Ca ratios. Open Access Climate Dynamics, 56 . pp. 3295-3303. DOI 10.1007/s00382-021-05642-x <https://doi.org/10.1007/s00382-021-05642-x>. doi:10.1007/s00382-021-05642-x cc_by_4.0 info:eu-repo/semantics/openAccess Article PeerReviewed 2021 ftoceanrep https://doi.org/10.1007/s00382-021-05642-x 2024-01-15T00:22:57Z The Arctic cryosphere is changing rapidly due to global warming. Northern Svalbard is a warming hotspot with a temperature rise of ~ 6 °C over the last three decades. Concurrently, modelled data suggest a marked increase in glacier runoff during recent decades in northern Svalbard, and runoff is projected to increase. However, observational data from before anthropogenic influence are sparse and the potential effects on the surface ocean are unclear. Here, we present a 200-year record of Ba/Ca ratios measured in annual increment-forming coralline algae from northern Spitsbergen as a proxy for past glacier-derived meltwater input. Our record shows a significant increasing trend in algal Ba/Ca ratios from the late-1980s onwards matching modelled regional runoff data, suggesting a drastic increase in land-based runoff. The rate of increase is unprecedented during the last two centuries and captures the impact of amplified warming on the coastal surface ocean in the high Arctic. The algal Ba/Ca runoff proxy offers an opportunity to reconstruct past land-based runoff variability in Arctic settings in high resolution, providing important data for validating and improving climate modelling studies. Article in Journal/Newspaper arctic cryosphere Arctic glacier Global warming Svalbard Spitsbergen OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel) Arctic Svalbard Climate Dynamics 56 9-10 3295 3303
institution Open Polar
collection OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel)
op_collection_id ftoceanrep
language English
description The Arctic cryosphere is changing rapidly due to global warming. Northern Svalbard is a warming hotspot with a temperature rise of ~ 6 °C over the last three decades. Concurrently, modelled data suggest a marked increase in glacier runoff during recent decades in northern Svalbard, and runoff is projected to increase. However, observational data from before anthropogenic influence are sparse and the potential effects on the surface ocean are unclear. Here, we present a 200-year record of Ba/Ca ratios measured in annual increment-forming coralline algae from northern Spitsbergen as a proxy for past glacier-derived meltwater input. Our record shows a significant increasing trend in algal Ba/Ca ratios from the late-1980s onwards matching modelled regional runoff data, suggesting a drastic increase in land-based runoff. The rate of increase is unprecedented during the last two centuries and captures the impact of amplified warming on the coastal surface ocean in the high Arctic. The algal Ba/Ca runoff proxy offers an opportunity to reconstruct past land-based runoff variability in Arctic settings in high resolution, providing important data for validating and improving climate modelling studies.
format Article in Journal/Newspaper
author Hetzinger, Steffen
Halfar, Jochen
Zajacz, Zoltan
Möller, Marco
Wisshak, Max
spellingShingle Hetzinger, Steffen
Halfar, Jochen
Zajacz, Zoltan
Möller, Marco
Wisshak, Max
Late twentieth century increase in northern Spitsbergen (Svalbard) glacier-derived runoff tracked by coralline algal Ba/Ca ratios
author_facet Hetzinger, Steffen
Halfar, Jochen
Zajacz, Zoltan
Möller, Marco
Wisshak, Max
author_sort Hetzinger, Steffen
title Late twentieth century increase in northern Spitsbergen (Svalbard) glacier-derived runoff tracked by coralline algal Ba/Ca ratios
title_short Late twentieth century increase in northern Spitsbergen (Svalbard) glacier-derived runoff tracked by coralline algal Ba/Ca ratios
title_full Late twentieth century increase in northern Spitsbergen (Svalbard) glacier-derived runoff tracked by coralline algal Ba/Ca ratios
title_fullStr Late twentieth century increase in northern Spitsbergen (Svalbard) glacier-derived runoff tracked by coralline algal Ba/Ca ratios
title_full_unstemmed Late twentieth century increase in northern Spitsbergen (Svalbard) glacier-derived runoff tracked by coralline algal Ba/Ca ratios
title_sort late twentieth century increase in northern spitsbergen (svalbard) glacier-derived runoff tracked by coralline algal ba/ca ratios
publisher Springer
publishDate 2021
url https://oceanrep.geomar.de/id/eprint/51660/
https://oceanrep.geomar.de/id/eprint/51660/1/Hetzinger.pdf
https://oceanrep.geomar.de/id/eprint/51660/7/382_2021_5642_MOESM2_ESM.pdf
https://oceanrep.geomar.de/id/eprint/51660/8/382_2021_5642_MOESM1_ESM.xlsx
https://oceanrep.geomar.de/id/eprint/51660/14/Hetzinger2021_Article_LateTwentiethCenturyIncreaseIn.pdf
https://doi.org/10.1007/s00382-021-05642-x
geographic Arctic
Svalbard
geographic_facet Arctic
Svalbard
genre arctic cryosphere
Arctic
glacier
Global warming
Svalbard
Spitsbergen
genre_facet arctic cryosphere
Arctic
glacier
Global warming
Svalbard
Spitsbergen
op_relation https://oceanrep.geomar.de/id/eprint/51660/1/Hetzinger.pdf
https://oceanrep.geomar.de/id/eprint/51660/7/382_2021_5642_MOESM2_ESM.pdf
https://oceanrep.geomar.de/id/eprint/51660/8/382_2021_5642_MOESM1_ESM.xlsx
https://oceanrep.geomar.de/id/eprint/51660/14/Hetzinger2021_Article_LateTwentiethCenturyIncreaseIn.pdf
Hetzinger, S. , Halfar, J., Zajacz, Z., Möller, M. and Wisshak, M. (2021) Late twentieth century increase in northern Spitsbergen (Svalbard) glacier-derived runoff tracked by coralline algal Ba/Ca ratios. Open Access Climate Dynamics, 56 . pp. 3295-3303. DOI 10.1007/s00382-021-05642-x <https://doi.org/10.1007/s00382-021-05642-x>.
doi:10.1007/s00382-021-05642-x
op_rights cc_by_4.0
info:eu-repo/semantics/openAccess
op_doi https://doi.org/10.1007/s00382-021-05642-x
container_title Climate Dynamics
container_volume 56
container_issue 9-10
container_start_page 3295
op_container_end_page 3303
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