Late-Holocene diatom-inferred reconstruction of temperature variations of the West Greenland Current from Disko Bugt, central West Greenland

The diatom flora from a high-resolution core collected from Disko Bugt, central West Greenland, records variations in surface water temperature for the late Holocene (1600—300 cal. BP). Our data support the existence of a previously identified anti-phase relationship between the surface water temper...

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Published in:The Holocene
Main Authors: Krawczyk, Diana, Witkowski, Andrzej, Moros, Matthias, Lloyd, Jeremy, Kuijpers, Antoon, Kierzek, Agnieszka
Format: Article in Journal/Newspaper
Language:English
Published: SAGE Publications 2010
Subjects:
Online Access:http://dx.doi.org/10.1177/0959683610371993
http://journals.sagepub.com/doi/pdf/10.1177/0959683610371993
id crsagepubl:10.1177/0959683610371993
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spelling crsagepubl:10.1177/0959683610371993 2024-06-23T07:52:22+00:00 Late-Holocene diatom-inferred reconstruction of temperature variations of the West Greenland Current from Disko Bugt, central West Greenland Krawczyk, Diana Witkowski, Andrzej Moros, Matthias Lloyd, Jeremy Kuijpers, Antoon Kierzek, Agnieszka 2010 http://dx.doi.org/10.1177/0959683610371993 http://journals.sagepub.com/doi/pdf/10.1177/0959683610371993 en eng SAGE Publications http://journals.sagepub.com/page/policies/text-and-data-mining-license The Holocene volume 20, issue 5, page 659-666 ISSN 0959-6836 1477-0911 journal-article 2010 crsagepubl https://doi.org/10.1177/0959683610371993 2024-06-11T04:29:47Z The diatom flora from a high-resolution core collected from Disko Bugt, central West Greenland, records variations in surface water temperature for the late Holocene (1600—300 cal. BP). Our data support the existence of a previously identified anti-phase relationship between the surface water temperature from West Greenland and climate events recorded in the NE Atlantic and between surface and subsurface waters (identified from benthic foraminifera) of the West Greenland Current (WGC). The diatom flora record relatively cool surface water conditions during the end of the ‘Roman Warm Period’ and ‘Medieval Warm Period’ (MWP), and relatively warmer surface water conditions during the ‘Dark Ages Cold Period’ and ‘Little Ice Age’ (LIA). This is particularly pronounced during the MWP, experiencing the coldest conditions, and the LIA experiencing the warmest conditions through the whole sequence studied. The most likely explanation for this anti-phase relationship is linked to the flux of meltwater delivered to the WGC from sea ice and the Greenland ice sheet off the West Greenland margin. The generally warmer conditions of the MWP resulted in increased melting of sea ice and the Greenland ice sheet producing an increased meltwater flux and cooling of the surface waters of the WGC. In contrast, reduced meltwater flux during the relatively cold LIA resulted in reduced meltwater flux to the WGC, producing a relative warming of the surface waters recorded by the diatom flora. Article in Journal/Newspaper Disko bugt Greenland Ice Sheet Sea ice SAGE Publications Greenland The Holocene 20 5 659 666
institution Open Polar
collection SAGE Publications
op_collection_id crsagepubl
language English
description The diatom flora from a high-resolution core collected from Disko Bugt, central West Greenland, records variations in surface water temperature for the late Holocene (1600—300 cal. BP). Our data support the existence of a previously identified anti-phase relationship between the surface water temperature from West Greenland and climate events recorded in the NE Atlantic and between surface and subsurface waters (identified from benthic foraminifera) of the West Greenland Current (WGC). The diatom flora record relatively cool surface water conditions during the end of the ‘Roman Warm Period’ and ‘Medieval Warm Period’ (MWP), and relatively warmer surface water conditions during the ‘Dark Ages Cold Period’ and ‘Little Ice Age’ (LIA). This is particularly pronounced during the MWP, experiencing the coldest conditions, and the LIA experiencing the warmest conditions through the whole sequence studied. The most likely explanation for this anti-phase relationship is linked to the flux of meltwater delivered to the WGC from sea ice and the Greenland ice sheet off the West Greenland margin. The generally warmer conditions of the MWP resulted in increased melting of sea ice and the Greenland ice sheet producing an increased meltwater flux and cooling of the surface waters of the WGC. In contrast, reduced meltwater flux during the relatively cold LIA resulted in reduced meltwater flux to the WGC, producing a relative warming of the surface waters recorded by the diatom flora.
format Article in Journal/Newspaper
author Krawczyk, Diana
Witkowski, Andrzej
Moros, Matthias
Lloyd, Jeremy
Kuijpers, Antoon
Kierzek, Agnieszka
spellingShingle Krawczyk, Diana
Witkowski, Andrzej
Moros, Matthias
Lloyd, Jeremy
Kuijpers, Antoon
Kierzek, Agnieszka
Late-Holocene diatom-inferred reconstruction of temperature variations of the West Greenland Current from Disko Bugt, central West Greenland
author_facet Krawczyk, Diana
Witkowski, Andrzej
Moros, Matthias
Lloyd, Jeremy
Kuijpers, Antoon
Kierzek, Agnieszka
author_sort Krawczyk, Diana
title Late-Holocene diatom-inferred reconstruction of temperature variations of the West Greenland Current from Disko Bugt, central West Greenland
title_short Late-Holocene diatom-inferred reconstruction of temperature variations of the West Greenland Current from Disko Bugt, central West Greenland
title_full Late-Holocene diatom-inferred reconstruction of temperature variations of the West Greenland Current from Disko Bugt, central West Greenland
title_fullStr Late-Holocene diatom-inferred reconstruction of temperature variations of the West Greenland Current from Disko Bugt, central West Greenland
title_full_unstemmed Late-Holocene diatom-inferred reconstruction of temperature variations of the West Greenland Current from Disko Bugt, central West Greenland
title_sort late-holocene diatom-inferred reconstruction of temperature variations of the west greenland current from disko bugt, central west greenland
publisher SAGE Publications
publishDate 2010
url http://dx.doi.org/10.1177/0959683610371993
http://journals.sagepub.com/doi/pdf/10.1177/0959683610371993
geographic Greenland
geographic_facet Greenland
genre Disko bugt
Greenland
Ice Sheet
Sea ice
genre_facet Disko bugt
Greenland
Ice Sheet
Sea ice
op_source The Holocene
volume 20, issue 5, page 659-666
ISSN 0959-6836 1477-0911
op_rights http://journals.sagepub.com/page/policies/text-and-data-mining-license
op_doi https://doi.org/10.1177/0959683610371993
container_title The Holocene
container_volume 20
container_issue 5
container_start_page 659
op_container_end_page 666
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