Ocean circulation changes off southern Greenland during the abrupt climate events of mid-to-late MIS3
Marine sediment cores from the North Atlantic and ice cores from the Greenland Ice Sheet serve as natural archives of past climate variability. Ice cores have revealed that during the last glacial period the climate comprises both relatively stable intervals such as the Last Glacial Maximum (LGM, ca...
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ftunivbergen:oai:bora.uib.no:11250/2732835 2023-05-15T16:00:06+02:00 Ocean circulation changes off southern Greenland during the abrupt climate events of mid-to-late MIS3 Griem, Lisa orcid:0000-0002-6515-6781 2021-03-03T08:03:06.098Z application/pdf https://hdl.handle.net/11250/2732835 eng eng The University of Bergen Paper I: Griem, L.; Voelker, A. H. L.; Berben, S. M. P.; Dokken, T. M. and Jansen, E.: Insolation and glacial meltwater influence on sea-ice and circulation variability in the northeastern Labrador Sea during the last glacial period. Paleoceanography and Paleoclimatology. 2019, 34(11):1689-1709. The article is available at: https://hdl.handle.net/11250/2726974 Paper II: Griem, L.; Storey, C.; Berben, S. M. P.; Dokken, T. M. and Jansen, E.: Climate and ice sheet responses in northern latitudes during Marine Isotope Stage 3: A provenance study of ice-rafted debris from the Eirik Drift. The article is not available in BORA. Paper III: Griem, L.; Dokken, T. M.; Risebrobakken, B.; Faber, A.-K.; Berben, S. M. P.; Vinther, B. M.; Sadatzki, H.; Gkinis, V. and Jansen, E.: Similar conditions in the North Atlantic region during the Last Glacial Maximum and interstadials: Evidence from ice core and sediment core records. The article is not available in BORA. container/3d/e1/ed/dc/3de1eddc-8ade-422d-8611-4600febefa1f urn:isbn:9788230867013 urn:isbn:9788230862698 https://hdl.handle.net/11250/2732835 Attribution-NonCommercial (CC BY-NC). This item's rights statement or license does not apply to the included articles in the thesis. https://creativecommons.org/licenses/by-nc/4.0/ Copyright the Author. Doctoral thesis 2021 ftunivbergen 2023-03-14T17:38:57Z Marine sediment cores from the North Atlantic and ice cores from the Greenland Ice Sheet serve as natural archives of past climate variability. Ice cores have revealed that during the last glacial period the climate comprises both relatively stable intervals such as the Last Glacial Maximum (LGM, ca. 26-19 ka) and unstable climate intervals such as Marine Isotope Stage 3 (MIS3, ca. 59-29 ka). The climate of MIS3 is characterized by abrupt changes from colder stadial to warmer interstadial conditions, well-known as Dansgaard-Oeschger events (DO). Although DO events had repercussions over the climate system outside of the high latitude Northern Hemisphere, they are especially pronounced in records from the North Atlantic region. North Atlantic marine sediments record changes in sea ice cover, surface productivity and iceberg discharge, which are all associated with DO events. Iceberg discharge from the Northern Hemisphere ice sheets, and hence release of fresh water into the North Atlantic was especially pronounced during so-called Heinrich (H) Stadials. H-Stadials occurred approximately every 7 to 10 kyrs and are particularly cold and long stadials within the DO event oscillations. The freshwater discharge further contributed to sea ice formation in the North Atlantic and Nordic Seas. This near-perennial sea ice cover during stadials prevented ocean-atmosphere interaction while during interstadials the Nordic Seas were seasonally ice-free. These interstadial periods allowed moisture to evaporate from the ocean´s surface where after it was transported towards the Northern Hemisphere Ice Sheets, and thereby sustain their growth during MIS3 and the LGM. This thesis aims to give insights into the complex interactions between ice sheets, sea ice and ocean circulation during MIS3 and the LGM. Herein, the main focus lies on changes along the South-East Greenland margin, complemented by thoroughly studied sediment core sites from the Nordic Seas and Greenland ice core records. Paper I investigates environmental ... Doctoral or Postdoctoral Thesis Dansgaard-Oeschger events East Greenland Greenland Greenland ice core ice core Ice Sheet Nordic Seas North Atlantic Sea ice University of Bergen: Bergen Open Research Archive (BORA-UiB) Greenland |
institution |
Open Polar |
collection |
University of Bergen: Bergen Open Research Archive (BORA-UiB) |
op_collection_id |
ftunivbergen |
language |
English |
description |
Marine sediment cores from the North Atlantic and ice cores from the Greenland Ice Sheet serve as natural archives of past climate variability. Ice cores have revealed that during the last glacial period the climate comprises both relatively stable intervals such as the Last Glacial Maximum (LGM, ca. 26-19 ka) and unstable climate intervals such as Marine Isotope Stage 3 (MIS3, ca. 59-29 ka). The climate of MIS3 is characterized by abrupt changes from colder stadial to warmer interstadial conditions, well-known as Dansgaard-Oeschger events (DO). Although DO events had repercussions over the climate system outside of the high latitude Northern Hemisphere, they are especially pronounced in records from the North Atlantic region. North Atlantic marine sediments record changes in sea ice cover, surface productivity and iceberg discharge, which are all associated with DO events. Iceberg discharge from the Northern Hemisphere ice sheets, and hence release of fresh water into the North Atlantic was especially pronounced during so-called Heinrich (H) Stadials. H-Stadials occurred approximately every 7 to 10 kyrs and are particularly cold and long stadials within the DO event oscillations. The freshwater discharge further contributed to sea ice formation in the North Atlantic and Nordic Seas. This near-perennial sea ice cover during stadials prevented ocean-atmosphere interaction while during interstadials the Nordic Seas were seasonally ice-free. These interstadial periods allowed moisture to evaporate from the ocean´s surface where after it was transported towards the Northern Hemisphere Ice Sheets, and thereby sustain their growth during MIS3 and the LGM. This thesis aims to give insights into the complex interactions between ice sheets, sea ice and ocean circulation during MIS3 and the LGM. Herein, the main focus lies on changes along the South-East Greenland margin, complemented by thoroughly studied sediment core sites from the Nordic Seas and Greenland ice core records. Paper I investigates environmental ... |
author2 |
orcid:0000-0002-6515-6781 |
format |
Doctoral or Postdoctoral Thesis |
author |
Griem, Lisa |
spellingShingle |
Griem, Lisa Ocean circulation changes off southern Greenland during the abrupt climate events of mid-to-late MIS3 |
author_facet |
Griem, Lisa |
author_sort |
Griem, Lisa |
title |
Ocean circulation changes off southern Greenland during the abrupt climate events of mid-to-late MIS3 |
title_short |
Ocean circulation changes off southern Greenland during the abrupt climate events of mid-to-late MIS3 |
title_full |
Ocean circulation changes off southern Greenland during the abrupt climate events of mid-to-late MIS3 |
title_fullStr |
Ocean circulation changes off southern Greenland during the abrupt climate events of mid-to-late MIS3 |
title_full_unstemmed |
Ocean circulation changes off southern Greenland during the abrupt climate events of mid-to-late MIS3 |
title_sort |
ocean circulation changes off southern greenland during the abrupt climate events of mid-to-late mis3 |
publisher |
The University of Bergen |
publishDate |
2021 |
url |
https://hdl.handle.net/11250/2732835 |
geographic |
Greenland |
geographic_facet |
Greenland |
genre |
Dansgaard-Oeschger events East Greenland Greenland Greenland ice core ice core Ice Sheet Nordic Seas North Atlantic Sea ice |
genre_facet |
Dansgaard-Oeschger events East Greenland Greenland Greenland ice core ice core Ice Sheet Nordic Seas North Atlantic Sea ice |
op_relation |
Paper I: Griem, L.; Voelker, A. H. L.; Berben, S. M. P.; Dokken, T. M. and Jansen, E.: Insolation and glacial meltwater influence on sea-ice and circulation variability in the northeastern Labrador Sea during the last glacial period. Paleoceanography and Paleoclimatology. 2019, 34(11):1689-1709. The article is available at: https://hdl.handle.net/11250/2726974 Paper II: Griem, L.; Storey, C.; Berben, S. M. P.; Dokken, T. M. and Jansen, E.: Climate and ice sheet responses in northern latitudes during Marine Isotope Stage 3: A provenance study of ice-rafted debris from the Eirik Drift. The article is not available in BORA. Paper III: Griem, L.; Dokken, T. M.; Risebrobakken, B.; Faber, A.-K.; Berben, S. M. P.; Vinther, B. M.; Sadatzki, H.; Gkinis, V. and Jansen, E.: Similar conditions in the North Atlantic region during the Last Glacial Maximum and interstadials: Evidence from ice core and sediment core records. The article is not available in BORA. container/3d/e1/ed/dc/3de1eddc-8ade-422d-8611-4600febefa1f urn:isbn:9788230867013 urn:isbn:9788230862698 https://hdl.handle.net/11250/2732835 |
op_rights |
Attribution-NonCommercial (CC BY-NC). This item's rights statement or license does not apply to the included articles in the thesis. https://creativecommons.org/licenses/by-nc/4.0/ Copyright the Author. |
_version_ |
1766395965629005824 |