(Table 1) Age determination of Barents Sea sediment cores ...

The separate roles of oceanic heat advection and orbital forcing on influencing early Holocene temperature variability in the eastern Nordic Seas is investigated. The effect of changing orbital forcing on the ocean temperatures is tested using the 1DICE model, and the 1DICE results are compared with...

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Main Authors: Risebrobakken, Bjørg, Dokken, Trond, Smedsrud, Lars Henrik, Andersson, Carin, Jansen, Eystein, Moros, Matthias, Ivanova, Elena V
Format: Dataset
Language:English
Published: PANGAEA 2014
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.829724
https://doi.pangaea.de/10.1594/PANGAEA.829724
id ftdatacite:10.1594/pangaea.829724
record_format openpolar
spelling ftdatacite:10.1594/pangaea.829724 2024-09-15T17:57:52+00:00 (Table 1) Age determination of Barents Sea sediment cores ... Risebrobakken, Bjørg Dokken, Trond Smedsrud, Lars Henrik Andersson, Carin Jansen, Eystein Moros, Matthias Ivanova, Elena V 2014 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.829724 https://doi.pangaea.de/10.1594/PANGAEA.829724 en eng PANGAEA https://dx.doi.org/10.1029/2011pa002117 https://dx.doi.org/10.1038/ngeo439 https://dx.doi.org/10.1134/s0001437010040132 https://dx.doi.org/10.2113/gsjfr.38.4.337 https://dx.doi.org/10.1029/2002pa000764 https://dx.doi.org/10.1177/0959683609356586 https://dx.doi.org/10.1111/j.1502-3885.2003.tb01227.x Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Event label Latitude of event Longitude of event Elevation of event Laboratory code/label DEPTH, sediment/rock Age, dated material Age, dated Age, dated standard deviation Reservoir effect/correction Reservoir effect/correction, standard deviation Age, minimum/young Age, maximum/old Probability Calendar age Comment Reference/source Kasten corer Calypso Corer Gravity corer Age, 14C AMS Age, 14C calibrated M7/2 MD101 MD114 PSh64 Meteor 1986 Marion Dufresne 1995 Professor Shtokman Dataset dataset Supplementary Dataset 2014 ftdatacite https://doi.org/10.1594/pangaea.82972410.1029/2011pa00211710.1038/ngeo43910.1134/s000143701004013210.2113/gsjfr.38.4.33710.1029/2002pa00076410.1177/095968360935658610.1111/j.1502-3885.2003.tb01227.x 2024-07-03T13:10:33Z The separate roles of oceanic heat advection and orbital forcing on influencing early Holocene temperature variability in the eastern Nordic Seas is investigated. The effect of changing orbital forcing on the ocean temperatures is tested using the 1DICE model, and the 1DICE results are compared with new and previously published temperature reconstructions from a transect of five cores located underneath the pathway of Atlantic water, from the Faroe-Shetland Channel in the south to the Barents Sea in the north. The stronger early Holocene summer insolation at high northern latitudes increased the summer mixed layer temperatures, however, ocean temperatures underneath the summer mixed layer did not increase significantly. The absolute maximum in summer mixed layer temperatures occurred between 9 and 6 ka BP, representing the Holocene Thermal Maximum in the eastern Nordic Seas. In contrast, maximum in northward oceanic heat transport through the Norwegian Atlantic Current occurred approximately 10 ka BP. The ... : Supplement to: Risebrobakken, Bjørg; Dokken, Trond; Smedsrud, Lars Henrik; Andersson, Carin; Jansen, Eystein; Moros, Matthias; Ivanova, Elena V (2011): Early Holocene temperature variability in the Nordic Seas: The role of oceanic heat advection versus changes in orbital forcing. Paleoceanography, 26(4), PA4206 ... Dataset Barents Sea Nordic Seas DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Event label
Latitude of event
Longitude of event
Elevation of event
Laboratory code/label
DEPTH, sediment/rock
Age, dated material
Age, dated
Age, dated standard deviation
Reservoir effect/correction
Reservoir effect/correction, standard deviation
Age, minimum/young
Age, maximum/old
Probability
Calendar age
Comment
Reference/source
Kasten corer
Calypso Corer
Gravity corer
Age, 14C AMS
Age, 14C calibrated
M7/2
MD101
MD114
PSh64
Meteor 1986
Marion Dufresne 1995
Professor Shtokman
spellingShingle Event label
Latitude of event
Longitude of event
Elevation of event
Laboratory code/label
DEPTH, sediment/rock
Age, dated material
Age, dated
Age, dated standard deviation
Reservoir effect/correction
Reservoir effect/correction, standard deviation
Age, minimum/young
Age, maximum/old
Probability
Calendar age
Comment
Reference/source
Kasten corer
Calypso Corer
Gravity corer
Age, 14C AMS
Age, 14C calibrated
M7/2
MD101
MD114
PSh64
Meteor 1986
Marion Dufresne 1995
Professor Shtokman
Risebrobakken, Bjørg
Dokken, Trond
Smedsrud, Lars Henrik
Andersson, Carin
Jansen, Eystein
Moros, Matthias
Ivanova, Elena V
(Table 1) Age determination of Barents Sea sediment cores ...
topic_facet Event label
Latitude of event
Longitude of event
Elevation of event
Laboratory code/label
DEPTH, sediment/rock
Age, dated material
Age, dated
Age, dated standard deviation
Reservoir effect/correction
Reservoir effect/correction, standard deviation
Age, minimum/young
Age, maximum/old
Probability
Calendar age
Comment
Reference/source
Kasten corer
Calypso Corer
Gravity corer
Age, 14C AMS
Age, 14C calibrated
M7/2
MD101
MD114
PSh64
Meteor 1986
Marion Dufresne 1995
Professor Shtokman
description The separate roles of oceanic heat advection and orbital forcing on influencing early Holocene temperature variability in the eastern Nordic Seas is investigated. The effect of changing orbital forcing on the ocean temperatures is tested using the 1DICE model, and the 1DICE results are compared with new and previously published temperature reconstructions from a transect of five cores located underneath the pathway of Atlantic water, from the Faroe-Shetland Channel in the south to the Barents Sea in the north. The stronger early Holocene summer insolation at high northern latitudes increased the summer mixed layer temperatures, however, ocean temperatures underneath the summer mixed layer did not increase significantly. The absolute maximum in summer mixed layer temperatures occurred between 9 and 6 ka BP, representing the Holocene Thermal Maximum in the eastern Nordic Seas. In contrast, maximum in northward oceanic heat transport through the Norwegian Atlantic Current occurred approximately 10 ka BP. The ... : Supplement to: Risebrobakken, Bjørg; Dokken, Trond; Smedsrud, Lars Henrik; Andersson, Carin; Jansen, Eystein; Moros, Matthias; Ivanova, Elena V (2011): Early Holocene temperature variability in the Nordic Seas: The role of oceanic heat advection versus changes in orbital forcing. Paleoceanography, 26(4), PA4206 ...
format Dataset
author Risebrobakken, Bjørg
Dokken, Trond
Smedsrud, Lars Henrik
Andersson, Carin
Jansen, Eystein
Moros, Matthias
Ivanova, Elena V
author_facet Risebrobakken, Bjørg
Dokken, Trond
Smedsrud, Lars Henrik
Andersson, Carin
Jansen, Eystein
Moros, Matthias
Ivanova, Elena V
author_sort Risebrobakken, Bjørg
title (Table 1) Age determination of Barents Sea sediment cores ...
title_short (Table 1) Age determination of Barents Sea sediment cores ...
title_full (Table 1) Age determination of Barents Sea sediment cores ...
title_fullStr (Table 1) Age determination of Barents Sea sediment cores ...
title_full_unstemmed (Table 1) Age determination of Barents Sea sediment cores ...
title_sort (table 1) age determination of barents sea sediment cores ...
publisher PANGAEA
publishDate 2014
url https://dx.doi.org/10.1594/pangaea.829724
https://doi.pangaea.de/10.1594/PANGAEA.829724
genre Barents Sea
Nordic Seas
genre_facet Barents Sea
Nordic Seas
op_relation https://dx.doi.org/10.1029/2011pa002117
https://dx.doi.org/10.1038/ngeo439
https://dx.doi.org/10.1134/s0001437010040132
https://dx.doi.org/10.2113/gsjfr.38.4.337
https://dx.doi.org/10.1029/2002pa000764
https://dx.doi.org/10.1177/0959683609356586
https://dx.doi.org/10.1111/j.1502-3885.2003.tb01227.x
op_rights Creative Commons Attribution 3.0 Unported
https://creativecommons.org/licenses/by/3.0/legalcode
cc-by-3.0
op_doi https://doi.org/10.1594/pangaea.82972410.1029/2011pa00211710.1038/ngeo43910.1134/s000143701004013210.2113/gsjfr.38.4.33710.1029/2002pa00076410.1177/095968360935658610.1111/j.1502-3885.2003.tb01227.x
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