North Atlantic Versus Global Control on Dansgaard-Oeschger Events
The classic scenario for the generation of Dansgaard-Oeschger (DO) events assumes a link to changes in the Atlantic Meridional Overturning Circulation (AMOC) induced by North Atlantic freshwater perturbations. Recent proxy data emphasize the existence of leads and lags between DO fingerprints in Gre...
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ftawi:oai:epic.awi.de:49330 2024-09-15T17:44:32+00:00 North Atlantic Versus Global Control on Dansgaard-Oeschger Events Dima, Mihai Lohmann, Gerrit Knorr, Gregor 2018-12-16 application/pdf https://epic.awi.de/id/eprint/49330/ https://epic.awi.de/id/eprint/49330/1/dima_lohmann_knorr_do_hyteresis_grl_2018.pdf https://hdl.handle.net/10013/epic.f621f51b-867d-4476-ac45-14a3d2895e98 unknown Wiley https://epic.awi.de/id/eprint/49330/1/dima_lohmann_knorr_do_hyteresis_grl_2018.pdf Dima, M. , Lohmann, G. orcid:0000-0003-2089-733X and Knorr, G. orcid:0000-0002-8317-5046 (2018) North Atlantic Versus Global Control on Dansgaard-Oeschger Events , Geophysical Research Letters, 45 (23), pp. 12991-12998 . doi:10.1029/2018GL080035 <https://doi.org/10.1029/2018GL080035> , hdl:10013/epic.f621f51b-867d-4476-ac45-14a3d2895e98 EPIC3Geophysical Research Letters, Wiley, 45(23), pp. 12991-12998, ISSN: 0094-8276 Article isiRev 2018 ftawi https://doi.org/10.1029/2018GL080035 2024-06-24T04:22:11Z The classic scenario for the generation of Dansgaard-Oeschger (DO) events assumes a link to changes in the Atlantic Meridional Overturning Circulation (AMOC) induced by North Atlantic freshwater perturbations. Recent proxy data emphasize the existence of leads and lags between DO fingerprints in Greenland and Antarctic records, highlighting the potential of a Southern Hemisphere control on these events. Investigating this possibility, we provide a conceptual model resulting from phase space reconstructions based on the northern and southern ice core records. The resulting patterns closely resemble AMOC hysteresis, consistent with a northern abrupt warming linked to gradual global temperature changes. This suggests that rapid DO warmings associated with abrupt AMOC transitions from a relatively weak (cold stadial) state to a stronger (warm inter-stadial) state can be controlled by global forcing that can be linked to the Southern Hemisphere, rather than by the end of a local temporary forcing in the North Atlantic. Article in Journal/Newspaper Antarc* Antarctic Dansgaard-Oeschger events Greenland ice core North Atlantic Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) Geophysical Research Letters 45 23 |
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Open Polar |
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Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) |
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ftawi |
language |
unknown |
description |
The classic scenario for the generation of Dansgaard-Oeschger (DO) events assumes a link to changes in the Atlantic Meridional Overturning Circulation (AMOC) induced by North Atlantic freshwater perturbations. Recent proxy data emphasize the existence of leads and lags between DO fingerprints in Greenland and Antarctic records, highlighting the potential of a Southern Hemisphere control on these events. Investigating this possibility, we provide a conceptual model resulting from phase space reconstructions based on the northern and southern ice core records. The resulting patterns closely resemble AMOC hysteresis, consistent with a northern abrupt warming linked to gradual global temperature changes. This suggests that rapid DO warmings associated with abrupt AMOC transitions from a relatively weak (cold stadial) state to a stronger (warm inter-stadial) state can be controlled by global forcing that can be linked to the Southern Hemisphere, rather than by the end of a local temporary forcing in the North Atlantic. |
format |
Article in Journal/Newspaper |
author |
Dima, Mihai Lohmann, Gerrit Knorr, Gregor |
spellingShingle |
Dima, Mihai Lohmann, Gerrit Knorr, Gregor North Atlantic Versus Global Control on Dansgaard-Oeschger Events |
author_facet |
Dima, Mihai Lohmann, Gerrit Knorr, Gregor |
author_sort |
Dima, Mihai |
title |
North Atlantic Versus Global Control on Dansgaard-Oeschger Events |
title_short |
North Atlantic Versus Global Control on Dansgaard-Oeschger Events |
title_full |
North Atlantic Versus Global Control on Dansgaard-Oeschger Events |
title_fullStr |
North Atlantic Versus Global Control on Dansgaard-Oeschger Events |
title_full_unstemmed |
North Atlantic Versus Global Control on Dansgaard-Oeschger Events |
title_sort |
north atlantic versus global control on dansgaard-oeschger events |
publisher |
Wiley |
publishDate |
2018 |
url |
https://epic.awi.de/id/eprint/49330/ https://epic.awi.de/id/eprint/49330/1/dima_lohmann_knorr_do_hyteresis_grl_2018.pdf https://hdl.handle.net/10013/epic.f621f51b-867d-4476-ac45-14a3d2895e98 |
genre |
Antarc* Antarctic Dansgaard-Oeschger events Greenland ice core North Atlantic |
genre_facet |
Antarc* Antarctic Dansgaard-Oeschger events Greenland ice core North Atlantic |
op_source |
EPIC3Geophysical Research Letters, Wiley, 45(23), pp. 12991-12998, ISSN: 0094-8276 |
op_relation |
https://epic.awi.de/id/eprint/49330/1/dima_lohmann_knorr_do_hyteresis_grl_2018.pdf Dima, M. , Lohmann, G. orcid:0000-0003-2089-733X and Knorr, G. orcid:0000-0002-8317-5046 (2018) North Atlantic Versus Global Control on Dansgaard-Oeschger Events , Geophysical Research Letters, 45 (23), pp. 12991-12998 . doi:10.1029/2018GL080035 <https://doi.org/10.1029/2018GL080035> , hdl:10013/epic.f621f51b-867d-4476-ac45-14a3d2895e98 |
op_doi |
https://doi.org/10.1029/2018GL080035 |
container_title |
Geophysical Research Letters |
container_volume |
45 |
container_issue |
23 |
_version_ |
1810492166521225216 |