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...
Published in: | Climate Dynamics |
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Main Authors: | , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Springer
2021
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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 |
_version_ | 1821797064738078720 |
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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 |
collection | OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel) |
container_issue | 9-10 |
container_start_page | 3295 |
container_title | Climate Dynamics |
container_volume | 56 |
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 |
genre | arctic cryosphere Arctic glacier Global warming Svalbard Spitsbergen |
genre_facet | arctic cryosphere Arctic glacier Global warming Svalbard Spitsbergen |
geographic | Arctic Svalbard |
geographic_facet | Arctic Svalbard |
id | ftoceanrep:oai:oceanrep.geomar.de:51660 |
institution | Open Polar |
language | English |
op_collection_id | ftoceanrep |
op_container_end_page | 3303 |
op_doi | https://doi.org/10.1007/s00382-021-05642-x |
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 |
publishDate | 2021 |
publisher | Springer |
record_format | openpolar |
spelling | ftoceanrep:oai:oceanrep.geomar.de:51660 2025-01-16T20:00:35+00:00 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 |
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 |
title | 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_short | 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 |
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 |