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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Main Authors: Hetzinger, Steffen, Halfar, Jochen, Zajacz, Zoltan, Möller, Marco, Wisshak, Max
Format: Article in Journal/Newspaper
Language:English
Published: Humboldt-Universität zu Berlin 2021
Subjects:
Online Access:http://edoc.hu-berlin.de/18452/27287
https://nbn-resolving.org/urn:nbn:de:kobv:11-110-18452/27287-7
https://doi.org/10.1007/s00382-021-05642-x
https://doi.org/10.18452/26590
id fthuberlin:oai:edoc.hu-berlin.de:18452/27287
record_format openpolar
spelling fthuberlin:oai:edoc.hu-berlin.de:18452/27287 2023-12-03T10:15:34+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 application/pdf http://edoc.hu-berlin.de/18452/27287 https://nbn-resolving.org/urn:nbn:de:kobv:11-110-18452/27287-7 https://doi.org/10.1007/s00382-021-05642-x https://doi.org/10.18452/26590 eng eng Humboldt-Universität zu Berlin 0930-7575 http://edoc.hu-berlin.de/18452/27287 urn:nbn:de:kobv:11-110-18452/27287-7 doi:10.1007/s00382-021-05642-x http://dx.doi.org/10.18452/26590 1432-0894 (CC BY 4.0) Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/ Ba/Ca Runoff proxy Glacier Freshwater Coralline algae Svalbard 550 Geowissenschaften ddc:550 article doc-type:article publishedVersion 2021 fthuberlin https://doi.org/10.1007/s00382-021-05642-x10.18452/26590 2023-11-05T23:36:29Z 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. Deutsche Forschungsgemeinschaft http://dx.doi.org/10.13039/501100001659 Canadian Network for Research and Innovation in Machining Technology, Natural Sciences and Engineering Research Council of Canada (CA) Projekt DEAL Peer Reviewed Article in Journal/Newspaper arctic cryosphere Arctic glacier glacier* Global warming Svalbard Spitsbergen Open-Access-Publikationsserver der Humboldt-Universität: edoc-Server Arctic Canada Svalbard
institution Open Polar
collection Open-Access-Publikationsserver der Humboldt-Universität: edoc-Server
op_collection_id fthuberlin
language English
topic Ba/Ca
Runoff proxy
Glacier
Freshwater
Coralline algae
Svalbard
550 Geowissenschaften
ddc:550
spellingShingle Ba/Ca
Runoff proxy
Glacier
Freshwater
Coralline algae
Svalbard
550 Geowissenschaften
ddc:550
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
topic_facet Ba/Ca
Runoff proxy
Glacier
Freshwater
Coralline algae
Svalbard
550 Geowissenschaften
ddc:550
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. Deutsche Forschungsgemeinschaft http://dx.doi.org/10.13039/501100001659 Canadian Network for Research and Innovation in Machining Technology, Natural Sciences and Engineering Research Council of Canada (CA) Projekt DEAL Peer Reviewed
format Article in Journal/Newspaper
author Hetzinger, Steffen
Halfar, Jochen
Zajacz, Zoltan
Möller, Marco
Wisshak, Max
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 Humboldt-Universität zu Berlin
publishDate 2021
url http://edoc.hu-berlin.de/18452/27287
https://nbn-resolving.org/urn:nbn:de:kobv:11-110-18452/27287-7
https://doi.org/10.1007/s00382-021-05642-x
https://doi.org/10.18452/26590
geographic Arctic
Canada
Svalbard
geographic_facet Arctic
Canada
Svalbard
genre arctic cryosphere
Arctic
glacier
glacier*
Global warming
Svalbard
Spitsbergen
genre_facet arctic cryosphere
Arctic
glacier
glacier*
Global warming
Svalbard
Spitsbergen
op_relation 0930-7575
http://edoc.hu-berlin.de/18452/27287
urn:nbn:de:kobv:11-110-18452/27287-7
doi:10.1007/s00382-021-05642-x
http://dx.doi.org/10.18452/26590
1432-0894
op_rights (CC BY 4.0) Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.1007/s00382-021-05642-x10.18452/26590
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