Atlantic Water advection vs. glacier dynamics in northern Spitsbergen since early deglaciation
Atlantic Water (AW) advection plays an important role in climatic, oceanographic and environmental conditions in the eastern Arctic. Situated along the only deep connection between the Atlantic and the Arctic oceans, the Svalbard Archipelago is an ideal location to reconstruct the past AW advection...
Published in: | Climate of the Past |
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2017
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Online Access: | https://pure.au.dk/portal/da/publications/atlantic-water-advection-vs-glacier-dynamics-in-northern-spitsbergen-since-early-deglaciation(58d9bd90-877c-41b0-8283-e769c1bc88bf).html https://doi.org/10.5194/cp-13-1717-2017 https://pure.au.dk/ws/files/120110095/cp_13_1717_2017.pdf |
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ftuniaarhuspubl:oai:pure.atira.dk:publications/58d9bd90-877c-41b0-8283-e769c1bc88bf 2023-12-31T10:03:34+01:00 Atlantic Water advection vs. glacier dynamics in northern Spitsbergen since early deglaciation Bartels, Martin Titschack, Juergen Fahl, Kirsten Stein, Ruediger Seidenkrantz, Marit-Solveig Hillaire-Marcel, Claude Hebbeln, Dierk 2017-11-30 application/pdf https://pure.au.dk/portal/da/publications/atlantic-water-advection-vs-glacier-dynamics-in-northern-spitsbergen-since-early-deglaciation(58d9bd90-877c-41b0-8283-e769c1bc88bf).html https://doi.org/10.5194/cp-13-1717-2017 https://pure.au.dk/ws/files/120110095/cp_13_1717_2017.pdf eng eng https://pure.au.dk/portal/da/publications/atlantic-water-advection-vs-glacier-dynamics-in-northern-spitsbergen-since-early-deglaciation(58d9bd90-877c-41b0-8283-e769c1bc88bf).html info:eu-repo/semantics/openAccess Bartels , M , Titschack , J , Fahl , K , Stein , R , Seidenkrantz , M-S , Hillaire-Marcel , C & Hebbeln , D 2017 , ' Atlantic Water advection vs. glacier dynamics in northern Spitsbergen since early deglaciation ' , Climate of the Past , vol. 13 , no. 12 , pp. 1717-1749 . https://doi.org/10.5194/cp-13-1717-2017 SEA-ICE SHEET MODERN BENTHIC FORAMINIFERA RESERVOIR AGE CORRECTIONS QUATERNARY ARCTIC-OCEAN EASTERN FRAM STRAIT YOUNGER-DRYAS BARENTS SEA FRESH-WATER NORDIC SEAS MIDLATITUDE WEATHER article 2017 ftuniaarhuspubl https://doi.org/10.5194/cp-13-1717-2017 2023-12-07T00:02:24Z Atlantic Water (AW) advection plays an important role in climatic, oceanographic and environmental conditions in the eastern Arctic. Situated along the only deep connection between the Atlantic and the Arctic oceans, the Svalbard Archipelago is an ideal location to reconstruct the past AW advection history and document its linkage with local glacier dynamics, as illustrated in the present study of a 275ĝ€cm long sedimentary record from Woodfjorden (northern Spitsbergen; water depth: 171ĝ€m) spanning the last ĝ1/4 ĝ€15ĝ€500 years. Sedimentological, micropalaeontological and geochemical analyses were used to reconstruct changes in marine environmental conditions, sea ice cover and glacier activity. Data illustrate a partial break-up of the Svalbard-Barents Sea Ice Sheet from Heinrich Stadial 1 onwards (until ĝ1/4 ĝ€14.6ĝ€ka). During the Bølling-Allerød ( ĝ1/4 ĝ€14.6-12.7ĝ€ka), AW penetrated as a bottom water mass into the fjord system and contributed significantly to the destabilization of local glaciers. During the Younger Dryas ( ĝ1/4 ĝ€12.7-11.7ĝ€ka), it intruded into intermediate waters while evidence for a glacier advance is lacking. A short-term deepening of the halocline occurred at the very end of this interval. During the early Holocene ( ĝ1/4 ĝ€11.7-7.8ĝ€ka), mild conditions led to glacier retreat, a reduced sea ice cover and increasing sea surface temperatures, with a brief interruption during the Preboreal Oscillation ( ĝ1/4 ĝ€11.1-10.8ĝ€ka). Due to a ĝ1/4 ĝ€6000-year gap, the mid-Holocene is not recorded in this sediment core. During the late Holocene ( ĝ1/4 ĝ€1.8-0.4ĝ€ka), a slightly reduced AW inflow and lower sea surface temperatures compared to the early Holocene are reconstructed. Glaciers, which previously retreated to the shallower inner parts of the Woodfjorden system, likely advanced during the late Holocene. In particular, topographic control in concert with the reduced summer insolation partly decoupled glacier dynamics from AW advection during this recent interval. Article in Journal/Newspaper Arctic Arctic Ocean Barents Sea Foraminifera* Fram Strait glacier Ice Sheet Nordic Seas Sea ice Svalbard Svalbard-Barents Sea Ice sheet Woodfjord* Woodfjorden Spitsbergen Aarhus University: Research Climate of the Past 13 12 1717 1749 |
institution |
Open Polar |
collection |
Aarhus University: Research |
op_collection_id |
ftuniaarhuspubl |
language |
English |
topic |
SEA-ICE SHEET MODERN BENTHIC FORAMINIFERA RESERVOIR AGE CORRECTIONS QUATERNARY ARCTIC-OCEAN EASTERN FRAM STRAIT YOUNGER-DRYAS BARENTS SEA FRESH-WATER NORDIC SEAS MIDLATITUDE WEATHER |
spellingShingle |
SEA-ICE SHEET MODERN BENTHIC FORAMINIFERA RESERVOIR AGE CORRECTIONS QUATERNARY ARCTIC-OCEAN EASTERN FRAM STRAIT YOUNGER-DRYAS BARENTS SEA FRESH-WATER NORDIC SEAS MIDLATITUDE WEATHER Bartels, Martin Titschack, Juergen Fahl, Kirsten Stein, Ruediger Seidenkrantz, Marit-Solveig Hillaire-Marcel, Claude Hebbeln, Dierk Atlantic Water advection vs. glacier dynamics in northern Spitsbergen since early deglaciation |
topic_facet |
SEA-ICE SHEET MODERN BENTHIC FORAMINIFERA RESERVOIR AGE CORRECTIONS QUATERNARY ARCTIC-OCEAN EASTERN FRAM STRAIT YOUNGER-DRYAS BARENTS SEA FRESH-WATER NORDIC SEAS MIDLATITUDE WEATHER |
description |
Atlantic Water (AW) advection plays an important role in climatic, oceanographic and environmental conditions in the eastern Arctic. Situated along the only deep connection between the Atlantic and the Arctic oceans, the Svalbard Archipelago is an ideal location to reconstruct the past AW advection history and document its linkage with local glacier dynamics, as illustrated in the present study of a 275ĝ€cm long sedimentary record from Woodfjorden (northern Spitsbergen; water depth: 171ĝ€m) spanning the last ĝ1/4 ĝ€15ĝ€500 years. Sedimentological, micropalaeontological and geochemical analyses were used to reconstruct changes in marine environmental conditions, sea ice cover and glacier activity. Data illustrate a partial break-up of the Svalbard-Barents Sea Ice Sheet from Heinrich Stadial 1 onwards (until ĝ1/4 ĝ€14.6ĝ€ka). During the Bølling-Allerød ( ĝ1/4 ĝ€14.6-12.7ĝ€ka), AW penetrated as a bottom water mass into the fjord system and contributed significantly to the destabilization of local glaciers. During the Younger Dryas ( ĝ1/4 ĝ€12.7-11.7ĝ€ka), it intruded into intermediate waters while evidence for a glacier advance is lacking. A short-term deepening of the halocline occurred at the very end of this interval. During the early Holocene ( ĝ1/4 ĝ€11.7-7.8ĝ€ka), mild conditions led to glacier retreat, a reduced sea ice cover and increasing sea surface temperatures, with a brief interruption during the Preboreal Oscillation ( ĝ1/4 ĝ€11.1-10.8ĝ€ka). Due to a ĝ1/4 ĝ€6000-year gap, the mid-Holocene is not recorded in this sediment core. During the late Holocene ( ĝ1/4 ĝ€1.8-0.4ĝ€ka), a slightly reduced AW inflow and lower sea surface temperatures compared to the early Holocene are reconstructed. Glaciers, which previously retreated to the shallower inner parts of the Woodfjorden system, likely advanced during the late Holocene. In particular, topographic control in concert with the reduced summer insolation partly decoupled glacier dynamics from AW advection during this recent interval. |
format |
Article in Journal/Newspaper |
author |
Bartels, Martin Titschack, Juergen Fahl, Kirsten Stein, Ruediger Seidenkrantz, Marit-Solveig Hillaire-Marcel, Claude Hebbeln, Dierk |
author_facet |
Bartels, Martin Titschack, Juergen Fahl, Kirsten Stein, Ruediger Seidenkrantz, Marit-Solveig Hillaire-Marcel, Claude Hebbeln, Dierk |
author_sort |
Bartels, Martin |
title |
Atlantic Water advection vs. glacier dynamics in northern Spitsbergen since early deglaciation |
title_short |
Atlantic Water advection vs. glacier dynamics in northern Spitsbergen since early deglaciation |
title_full |
Atlantic Water advection vs. glacier dynamics in northern Spitsbergen since early deglaciation |
title_fullStr |
Atlantic Water advection vs. glacier dynamics in northern Spitsbergen since early deglaciation |
title_full_unstemmed |
Atlantic Water advection vs. glacier dynamics in northern Spitsbergen since early deglaciation |
title_sort |
atlantic water advection vs. glacier dynamics in northern spitsbergen since early deglaciation |
publishDate |
2017 |
url |
https://pure.au.dk/portal/da/publications/atlantic-water-advection-vs-glacier-dynamics-in-northern-spitsbergen-since-early-deglaciation(58d9bd90-877c-41b0-8283-e769c1bc88bf).html https://doi.org/10.5194/cp-13-1717-2017 https://pure.au.dk/ws/files/120110095/cp_13_1717_2017.pdf |
genre |
Arctic Arctic Ocean Barents Sea Foraminifera* Fram Strait glacier Ice Sheet Nordic Seas Sea ice Svalbard Svalbard-Barents Sea Ice sheet Woodfjord* Woodfjorden Spitsbergen |
genre_facet |
Arctic Arctic Ocean Barents Sea Foraminifera* Fram Strait glacier Ice Sheet Nordic Seas Sea ice Svalbard Svalbard-Barents Sea Ice sheet Woodfjord* Woodfjorden Spitsbergen |
op_source |
Bartels , M , Titschack , J , Fahl , K , Stein , R , Seidenkrantz , M-S , Hillaire-Marcel , C & Hebbeln , D 2017 , ' Atlantic Water advection vs. glacier dynamics in northern Spitsbergen since early deglaciation ' , Climate of the Past , vol. 13 , no. 12 , pp. 1717-1749 . https://doi.org/10.5194/cp-13-1717-2017 |
op_relation |
https://pure.au.dk/portal/da/publications/atlantic-water-advection-vs-glacier-dynamics-in-northern-spitsbergen-since-early-deglaciation(58d9bd90-877c-41b0-8283-e769c1bc88bf).html |
op_rights |
info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.5194/cp-13-1717-2017 |
container_title |
Climate of the Past |
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13 |
container_issue |
12 |
container_start_page |
1717 |
op_container_end_page |
1749 |
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