Hindcasting the continuum of Dansgaard–Oeschger variability: mechanisms, patterns and timing
Millennial-scale variability associated with Dansgaard–Oeschger events is arguably one of the most puzzling climate phenomena ever discovered in paleoclimate archives. Here, we set out to elucidate the underlying dynamics by conducting a transient global hindcast simulation with a 3-D intermediate c...
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ftdoajarticles:oai:doaj.org/article:03b33a01cceb4351a044d9234b0b06e8 2023-05-15T16:00:02+02:00 Hindcasting the continuum of Dansgaard–Oeschger variability: mechanisms, patterns and timing L. Menviel A. Timmermann T. Friedrich M. H. England 2014-01-01T00:00:00Z https://doi.org/10.5194/cp-10-63-2014 https://doaj.org/article/03b33a01cceb4351a044d9234b0b06e8 EN eng Copernicus Publications http://www.clim-past.net/10/63/2014/cp-10-63-2014.pdf https://doaj.org/toc/1814-9324 https://doaj.org/toc/1814-9332 1814-9324 1814-9332 doi:10.5194/cp-10-63-2014 https://doaj.org/article/03b33a01cceb4351a044d9234b0b06e8 Climate of the Past, Vol 10, Iss 1, Pp 63-77 (2014) Environmental pollution TD172-193.5 Environmental protection TD169-171.8 Environmental sciences GE1-350 article 2014 ftdoajarticles https://doi.org/10.5194/cp-10-63-2014 2022-12-31T15:38:51Z Millennial-scale variability associated with Dansgaard–Oeschger events is arguably one of the most puzzling climate phenomena ever discovered in paleoclimate archives. Here, we set out to elucidate the underlying dynamics by conducting a transient global hindcast simulation with a 3-D intermediate complexity earth system model covering the period 50 to 30 ka BP. The model is forced by time-varying external boundary conditions (greenhouse gases, orbital forcing, and ice-sheet orography and albedo) and anomalous North Atlantic freshwater fluxes, which mimic the effects of changing northern hemispheric ice volume on millennial timescales. Together these forcings generate a realistic global climate trajectory, as demonstrated by an extensive model/paleo data comparison. Our results are consistent with the idea that variations in ice-sheet calving and subsequent changes of the Atlantic Meridional Overturning Circulation were the main drivers for the continuum of glacial millennial-scale variability seen in paleorecords across the globe. Article in Journal/Newspaper Dansgaard-Oeschger events Ice Sheet North Atlantic Directory of Open Access Journals: DOAJ Articles Climate of the Past 10 1 63 77 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
Environmental pollution TD172-193.5 Environmental protection TD169-171.8 Environmental sciences GE1-350 |
spellingShingle |
Environmental pollution TD172-193.5 Environmental protection TD169-171.8 Environmental sciences GE1-350 L. Menviel A. Timmermann T. Friedrich M. H. England Hindcasting the continuum of Dansgaard–Oeschger variability: mechanisms, patterns and timing |
topic_facet |
Environmental pollution TD172-193.5 Environmental protection TD169-171.8 Environmental sciences GE1-350 |
description |
Millennial-scale variability associated with Dansgaard–Oeschger events is arguably one of the most puzzling climate phenomena ever discovered in paleoclimate archives. Here, we set out to elucidate the underlying dynamics by conducting a transient global hindcast simulation with a 3-D intermediate complexity earth system model covering the period 50 to 30 ka BP. The model is forced by time-varying external boundary conditions (greenhouse gases, orbital forcing, and ice-sheet orography and albedo) and anomalous North Atlantic freshwater fluxes, which mimic the effects of changing northern hemispheric ice volume on millennial timescales. Together these forcings generate a realistic global climate trajectory, as demonstrated by an extensive model/paleo data comparison. Our results are consistent with the idea that variations in ice-sheet calving and subsequent changes of the Atlantic Meridional Overturning Circulation were the main drivers for the continuum of glacial millennial-scale variability seen in paleorecords across the globe. |
format |
Article in Journal/Newspaper |
author |
L. Menviel A. Timmermann T. Friedrich M. H. England |
author_facet |
L. Menviel A. Timmermann T. Friedrich M. H. England |
author_sort |
L. Menviel |
title |
Hindcasting the continuum of Dansgaard–Oeschger variability: mechanisms, patterns and timing |
title_short |
Hindcasting the continuum of Dansgaard–Oeschger variability: mechanisms, patterns and timing |
title_full |
Hindcasting the continuum of Dansgaard–Oeschger variability: mechanisms, patterns and timing |
title_fullStr |
Hindcasting the continuum of Dansgaard–Oeschger variability: mechanisms, patterns and timing |
title_full_unstemmed |
Hindcasting the continuum of Dansgaard–Oeschger variability: mechanisms, patterns and timing |
title_sort |
hindcasting the continuum of dansgaard–oeschger variability: mechanisms, patterns and timing |
publisher |
Copernicus Publications |
publishDate |
2014 |
url |
https://doi.org/10.5194/cp-10-63-2014 https://doaj.org/article/03b33a01cceb4351a044d9234b0b06e8 |
genre |
Dansgaard-Oeschger events Ice Sheet North Atlantic |
genre_facet |
Dansgaard-Oeschger events Ice Sheet North Atlantic |
op_source |
Climate of the Past, Vol 10, Iss 1, Pp 63-77 (2014) |
op_relation |
http://www.clim-past.net/10/63/2014/cp-10-63-2014.pdf https://doaj.org/toc/1814-9324 https://doaj.org/toc/1814-9332 1814-9324 1814-9332 doi:10.5194/cp-10-63-2014 https://doaj.org/article/03b33a01cceb4351a044d9234b0b06e8 |
op_doi |
https://doi.org/10.5194/cp-10-63-2014 |
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Climate of the Past |
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10 |
container_issue |
1 |
container_start_page |
63 |
op_container_end_page |
77 |
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1766395904320864256 |