Dissolved Neodymium Isotopes Trace Origin and Spatiotemporal Evolution of Modern Arctic Sea Ice
The lifetime and thickness of Arctic sea ice have markedly decreased in the recent past. This affects Arctic marine ecosystems and the biological pump, given that sea ice acts as platform and transport medium of marine and atmospheric nutrients. At the same time sea ice reduces light penetration to...
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ftawi:oai:epic.awi.de:54373 2024-09-15T17:50:36+00:00 Dissolved Neodymium Isotopes Trace Origin and Spatiotemporal Evolution of Modern Arctic Sea Ice Laukert, Georgi Bauch, Dorothea Peeken, Ilka Krumpen, Thomas Werner, Kirstin Hathorne, Ed Gutjahr, Marcus Kassens, Heidemarie Frank, Martin 2020 https://epic.awi.de/id/eprint/54373/ https://doi.org/10.5194/egusphere-egu2020-7782 https://hdl.handle.net/10013/epic.43afb6f9-1154-4dc6-9011-2682f7c382c8 unknown Laukert, G. , Bauch, D. , Peeken, I. orcid:0000-0003-1531-1664 , Krumpen, T. , Werner, K. , Hathorne, E. , Gutjahr, M. , Kassens, H. and Frank, M. (2020) Dissolved Neodymium Isotopes Trace Origin and Spatiotemporal Evolution of Modern Arctic Sea Ice , EGU General Assembly 2020, 4 May 2020 - 8 May 2020 . doi:10.5194/egusphere-egu2020-7782 <https://doi.org/10.5194/egusphere-egu2020-7782> , hdl:10013/epic.43afb6f9-1154-4dc6-9011-2682f7c382c8 EPIC3EGU General Assembly 2020, 2020-05-04-2020-05-08Dissolved Neodymium Isotopes Trace Origin and Spatiotemporal Evolution of Modern Arctic Sea Ice Conference notRev 2020 ftawi https://doi.org/10.5194/egusphere-egu2020-7782 2024-06-24T04:27:29Z The lifetime and thickness of Arctic sea ice have markedly decreased in the recent past. This affects Arctic marine ecosystems and the biological pump, given that sea ice acts as platform and transport medium of marine and atmospheric nutrients. At the same time sea ice reduces light penetration to the Arctic Ocean and restricts ocean/atmosphere exchange. In order to understand the ongoing changes and their implications, reconstructions of source regions and drift trajectories of Arctic sea ice are imperative. Automated ice tracking approaches based on satellite-derived sea-ice motion products (e.g. ICETrack) currently perform well in dense ice fields, but provide limited information at the ice edge or in poorly ice-covered areas. Radiogenic neodymium (Nd) isotopes (εNd) have the potential to serve as a chemical tracer of sea-ice provenance and thus may provide information beyond what can be expected from satellite-based assessments. This potential results from pronounced εNd differences between the distinct marine and riverine sources, which feed the surface waters of the different sea-ice formation regions. We present the first dissolved (< 0.45 µm) Nd isotope and concentration data obtained from optically clean Arctic first- and multi-year sea ice (ice cores) collected from different ice floes across the Fram Strait during the RV POLARSTERN cruise PS85 in 2014. Our data confirm the preservation of the seawater εNdsignatures in sea ice despite low Nd concentrations (on average ~ 6 pmol/kg) resulting from efficient brine rejection. The large range in εNd signatures (~ -10 to -30) mirrors that of surface waters in various parts of the Arctic Ocean, indicating that differences between ice floes but also between various sections in an individual ice core reflect the origin and evolution of the sea ice over time. Most ice cores have εNd signatures of around -10, suggesting that the sea ice was formed in well-mixed waters in the central Arctic Ocean and transported directly to the Fram Strait via the Transpolar ... Conference Object Arctic Arctic Ocean Fram Strait ice core Sea ice ice covered areas Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) |
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Open Polar |
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Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) |
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ftawi |
language |
unknown |
description |
The lifetime and thickness of Arctic sea ice have markedly decreased in the recent past. This affects Arctic marine ecosystems and the biological pump, given that sea ice acts as platform and transport medium of marine and atmospheric nutrients. At the same time sea ice reduces light penetration to the Arctic Ocean and restricts ocean/atmosphere exchange. In order to understand the ongoing changes and their implications, reconstructions of source regions and drift trajectories of Arctic sea ice are imperative. Automated ice tracking approaches based on satellite-derived sea-ice motion products (e.g. ICETrack) currently perform well in dense ice fields, but provide limited information at the ice edge or in poorly ice-covered areas. Radiogenic neodymium (Nd) isotopes (εNd) have the potential to serve as a chemical tracer of sea-ice provenance and thus may provide information beyond what can be expected from satellite-based assessments. This potential results from pronounced εNd differences between the distinct marine and riverine sources, which feed the surface waters of the different sea-ice formation regions. We present the first dissolved (< 0.45 µm) Nd isotope and concentration data obtained from optically clean Arctic first- and multi-year sea ice (ice cores) collected from different ice floes across the Fram Strait during the RV POLARSTERN cruise PS85 in 2014. Our data confirm the preservation of the seawater εNdsignatures in sea ice despite low Nd concentrations (on average ~ 6 pmol/kg) resulting from efficient brine rejection. The large range in εNd signatures (~ -10 to -30) mirrors that of surface waters in various parts of the Arctic Ocean, indicating that differences between ice floes but also between various sections in an individual ice core reflect the origin and evolution of the sea ice over time. Most ice cores have εNd signatures of around -10, suggesting that the sea ice was formed in well-mixed waters in the central Arctic Ocean and transported directly to the Fram Strait via the Transpolar ... |
format |
Conference Object |
author |
Laukert, Georgi Bauch, Dorothea Peeken, Ilka Krumpen, Thomas Werner, Kirstin Hathorne, Ed Gutjahr, Marcus Kassens, Heidemarie Frank, Martin |
spellingShingle |
Laukert, Georgi Bauch, Dorothea Peeken, Ilka Krumpen, Thomas Werner, Kirstin Hathorne, Ed Gutjahr, Marcus Kassens, Heidemarie Frank, Martin Dissolved Neodymium Isotopes Trace Origin and Spatiotemporal Evolution of Modern Arctic Sea Ice |
author_facet |
Laukert, Georgi Bauch, Dorothea Peeken, Ilka Krumpen, Thomas Werner, Kirstin Hathorne, Ed Gutjahr, Marcus Kassens, Heidemarie Frank, Martin |
author_sort |
Laukert, Georgi |
title |
Dissolved Neodymium Isotopes Trace Origin and Spatiotemporal Evolution of Modern Arctic Sea Ice |
title_short |
Dissolved Neodymium Isotopes Trace Origin and Spatiotemporal Evolution of Modern Arctic Sea Ice |
title_full |
Dissolved Neodymium Isotopes Trace Origin and Spatiotemporal Evolution of Modern Arctic Sea Ice |
title_fullStr |
Dissolved Neodymium Isotopes Trace Origin and Spatiotemporal Evolution of Modern Arctic Sea Ice |
title_full_unstemmed |
Dissolved Neodymium Isotopes Trace Origin and Spatiotemporal Evolution of Modern Arctic Sea Ice |
title_sort |
dissolved neodymium isotopes trace origin and spatiotemporal evolution of modern arctic sea ice |
publishDate |
2020 |
url |
https://epic.awi.de/id/eprint/54373/ https://doi.org/10.5194/egusphere-egu2020-7782 https://hdl.handle.net/10013/epic.43afb6f9-1154-4dc6-9011-2682f7c382c8 |
genre |
Arctic Arctic Ocean Fram Strait ice core Sea ice ice covered areas |
genre_facet |
Arctic Arctic Ocean Fram Strait ice core Sea ice ice covered areas |
op_source |
EPIC3EGU General Assembly 2020, 2020-05-04-2020-05-08Dissolved Neodymium Isotopes Trace Origin and Spatiotemporal Evolution of Modern Arctic Sea Ice |
op_relation |
Laukert, G. , Bauch, D. , Peeken, I. orcid:0000-0003-1531-1664 , Krumpen, T. , Werner, K. , Hathorne, E. , Gutjahr, M. , Kassens, H. and Frank, M. (2020) Dissolved Neodymium Isotopes Trace Origin and Spatiotemporal Evolution of Modern Arctic Sea Ice , EGU General Assembly 2020, 4 May 2020 - 8 May 2020 . doi:10.5194/egusphere-egu2020-7782 <https://doi.org/10.5194/egusphere-egu2020-7782> , hdl:10013/epic.43afb6f9-1154-4dc6-9011-2682f7c382c8 |
op_doi |
https://doi.org/10.5194/egusphere-egu2020-7782 |
_version_ |
1810292411833778176 |