Neoglacial transition of atmospheric circulation patterns over Fennoscandia recorded in Holocene Lake Tornetrask sediments
Atmospheric circulation over the North Atlantic has undergone significant fluctuations during the Holocene. To better constrain these changes and their impacts on the Fennoscandian subarctic, we investigated molecular and inorganic proxies as well as plant wax D/H isotopes (D-C28) in a Holocene sedi...
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ftubkoeln:oai:USBKOELN.ub.uni-koeln.de:15211 2023-05-15T15:02:53+02:00 Neoglacial transition of atmospheric circulation patterns over Fennoscandia recorded in Holocene Lake Tornetrask sediments Thienemann, Matthias Kusch, Stephanie Vogel, Hendrik Ritter, Benedikt Schefuss, Enno Rethemeyer, Janet 2019 https://kups.ub.uni-koeln.de/15211/ eng eng WILEY Thienemann, Matthias, Kusch, Stephanie orcid:0000-0002-2708-4975 , Vogel, Hendrik orcid:0000-0002-9902-8120 , Ritter, Benedikt, Schefuss, Enno and Rethemeyer, Janet (2019). Neoglacial transition of atmospheric circulation patterns over Fennoscandia recorded in Holocene Lake Tornetrask sediments. Boreas, 48 (2). S. 287 - 299. HOBOKEN: WILEY. ISSN 1502-3885 ddc:no doc-type:article publishedVersion 2019 ftubkoeln 2022-11-09T07:15:00Z Atmospheric circulation over the North Atlantic has undergone significant fluctuations during the Holocene. To better constrain these changes and their impacts on the Fennoscandian subarctic, we investigated molecular and inorganic proxies as well as plant wax D/H isotopes (D-C28) in a Holocene sedimentary record from Lake Tornetrask (Sweden). These data indicate a thermal maximum c. 8100 to 6300cal. a BP with reduced soil organic matter input, followed by a long-term cooling trend with increasing soil erosion. D data suggest a stable atmospheric circulation with predominance of westerly flow and North Atlantic moisture sourcing during the Early and Middle Holocene. Asubstantial depletion in D followed by increased flood frequency starting at c. 5300cal. a BP and intensifying c. 1500cal. a BP suggests a reorganization of the atmospheric circulation from zonal towards meridional flow with predominantly Arctic Ocean and Baltic Sea moisture sourcing. Article in Journal/Newspaper Arctic Arctic Ocean Fennoscandia Fennoscandian North Atlantic Subarctic Cologne University: KUPS Arctic Arctic Ocean |
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Open Polar |
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Cologne University: KUPS |
op_collection_id |
ftubkoeln |
language |
English |
topic |
ddc:no |
spellingShingle |
ddc:no Thienemann, Matthias Kusch, Stephanie Vogel, Hendrik Ritter, Benedikt Schefuss, Enno Rethemeyer, Janet Neoglacial transition of atmospheric circulation patterns over Fennoscandia recorded in Holocene Lake Tornetrask sediments |
topic_facet |
ddc:no |
description |
Atmospheric circulation over the North Atlantic has undergone significant fluctuations during the Holocene. To better constrain these changes and their impacts on the Fennoscandian subarctic, we investigated molecular and inorganic proxies as well as plant wax D/H isotopes (D-C28) in a Holocene sedimentary record from Lake Tornetrask (Sweden). These data indicate a thermal maximum c. 8100 to 6300cal. a BP with reduced soil organic matter input, followed by a long-term cooling trend with increasing soil erosion. D data suggest a stable atmospheric circulation with predominance of westerly flow and North Atlantic moisture sourcing during the Early and Middle Holocene. Asubstantial depletion in D followed by increased flood frequency starting at c. 5300cal. a BP and intensifying c. 1500cal. a BP suggests a reorganization of the atmospheric circulation from zonal towards meridional flow with predominantly Arctic Ocean and Baltic Sea moisture sourcing. |
format |
Article in Journal/Newspaper |
author |
Thienemann, Matthias Kusch, Stephanie Vogel, Hendrik Ritter, Benedikt Schefuss, Enno Rethemeyer, Janet |
author_facet |
Thienemann, Matthias Kusch, Stephanie Vogel, Hendrik Ritter, Benedikt Schefuss, Enno Rethemeyer, Janet |
author_sort |
Thienemann, Matthias |
title |
Neoglacial transition of atmospheric circulation patterns over Fennoscandia recorded in Holocene Lake Tornetrask sediments |
title_short |
Neoglacial transition of atmospheric circulation patterns over Fennoscandia recorded in Holocene Lake Tornetrask sediments |
title_full |
Neoglacial transition of atmospheric circulation patterns over Fennoscandia recorded in Holocene Lake Tornetrask sediments |
title_fullStr |
Neoglacial transition of atmospheric circulation patterns over Fennoscandia recorded in Holocene Lake Tornetrask sediments |
title_full_unstemmed |
Neoglacial transition of atmospheric circulation patterns over Fennoscandia recorded in Holocene Lake Tornetrask sediments |
title_sort |
neoglacial transition of atmospheric circulation patterns over fennoscandia recorded in holocene lake tornetrask sediments |
publisher |
WILEY |
publishDate |
2019 |
url |
https://kups.ub.uni-koeln.de/15211/ |
geographic |
Arctic Arctic Ocean |
geographic_facet |
Arctic Arctic Ocean |
genre |
Arctic Arctic Ocean Fennoscandia Fennoscandian North Atlantic Subarctic |
genre_facet |
Arctic Arctic Ocean Fennoscandia Fennoscandian North Atlantic Subarctic |
op_relation |
Thienemann, Matthias, Kusch, Stephanie orcid:0000-0002-2708-4975 , Vogel, Hendrik orcid:0000-0002-9902-8120 , Ritter, Benedikt, Schefuss, Enno and Rethemeyer, Janet (2019). Neoglacial transition of atmospheric circulation patterns over Fennoscandia recorded in Holocene Lake Tornetrask sediments. Boreas, 48 (2). S. 287 - 299. HOBOKEN: WILEY. ISSN 1502-3885 |
_version_ |
1766334790798147584 |