The evolution of Miocene ocean circulation controlled by the Greenland-Scotland Ridge
The Greenland-Scotland Ridge (GSR) is a crucial hydrographic barrier for the exchange of water masses between the Polar Seas and the North Atlantic Ocean. Through the Miocene (5-23 Myrs; Myrs=million years ago), the Greenland-Scotland Ridge deepened at 18 Myrs and 15.5 Myrs, and again at 12.5 Myrs b...
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ftawi:oai:epic.awi.de:35737 2024-09-15T17:53:37+00:00 The evolution of Miocene ocean circulation controlled by the Greenland-Scotland Ridge Stärz, Michael Lohmann, Gerrit Knorr, Gregor Jokat, Wilfried 2014 application/pdf https://epic.awi.de/id/eprint/35737/ https://epic.awi.de/id/eprint/35737/1/PASTgateways14_staerz.pdf https://hdl.handle.net/10013/epic.43716 https://hdl.handle.net/10013/epic.43716.d001 unknown https://epic.awi.de/id/eprint/35737/1/PASTgateways14_staerz.pdf https://hdl.handle.net/10013/epic.43716.d001 Stärz, M. , Lohmann, G. orcid:0000-0003-2089-733X , Knorr, G. orcid:0000-0002-8317-5046 and Jokat, W. orcid:0000-0002-7793-5854 (2014) The evolution of Miocene ocean circulation controlled by the Greenland-Scotland Ridge , Proceedings of the II PAST Gateways - International converence and workshop, Trieste, Italy, 19 May 2014 - 23 May 2014 . hdl:10013/epic.43716 EPIC3Proceedings of the II PAST Gateways - International converence and workshop, Trieste, Italy, 2014-05-19-2014-05-23 Conference notRev 2014 ftawi 2024-06-24T04:09:53Z The Greenland-Scotland Ridge (GSR) is a crucial hydrographic barrier for the exchange of water masses between the Polar Seas and the North Atlantic Ocean. Through the Miocene (5-23 Myrs; Myrs=million years ago), the Greenland-Scotland Ridge deepened at 18 Myrs and 15.5 Myrs, and again at 12.5 Myrs by changes of the Icelandic mantle plume activity, which has direct consequences for the evolution of Northern Component Water. In a sensitivity study, we investigate the effect of GSR depth variations with a global atmosphere-ocean-vegetation General Circulation Model. Oceanic characteristics of the quasi-enclosed Nordic Seas and Arctic Ocean are analyzed, as well as the critical depth threshold for the evolution of the North Atlantic Current and the East Greenland Current is examined and linked to changes in global ocean circulation. Conference Object Arctic Ocean East Greenland east greenland current Greenland Greenland-Scotland Ridge Nordic Seas north atlantic current North Atlantic Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) |
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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 Greenland-Scotland Ridge (GSR) is a crucial hydrographic barrier for the exchange of water masses between the Polar Seas and the North Atlantic Ocean. Through the Miocene (5-23 Myrs; Myrs=million years ago), the Greenland-Scotland Ridge deepened at 18 Myrs and 15.5 Myrs, and again at 12.5 Myrs by changes of the Icelandic mantle plume activity, which has direct consequences for the evolution of Northern Component Water. In a sensitivity study, we investigate the effect of GSR depth variations with a global atmosphere-ocean-vegetation General Circulation Model. Oceanic characteristics of the quasi-enclosed Nordic Seas and Arctic Ocean are analyzed, as well as the critical depth threshold for the evolution of the North Atlantic Current and the East Greenland Current is examined and linked to changes in global ocean circulation. |
format |
Conference Object |
author |
Stärz, Michael Lohmann, Gerrit Knorr, Gregor Jokat, Wilfried |
spellingShingle |
Stärz, Michael Lohmann, Gerrit Knorr, Gregor Jokat, Wilfried The evolution of Miocene ocean circulation controlled by the Greenland-Scotland Ridge |
author_facet |
Stärz, Michael Lohmann, Gerrit Knorr, Gregor Jokat, Wilfried |
author_sort |
Stärz, Michael |
title |
The evolution of Miocene ocean circulation controlled by the Greenland-Scotland Ridge |
title_short |
The evolution of Miocene ocean circulation controlled by the Greenland-Scotland Ridge |
title_full |
The evolution of Miocene ocean circulation controlled by the Greenland-Scotland Ridge |
title_fullStr |
The evolution of Miocene ocean circulation controlled by the Greenland-Scotland Ridge |
title_full_unstemmed |
The evolution of Miocene ocean circulation controlled by the Greenland-Scotland Ridge |
title_sort |
evolution of miocene ocean circulation controlled by the greenland-scotland ridge |
publishDate |
2014 |
url |
https://epic.awi.de/id/eprint/35737/ https://epic.awi.de/id/eprint/35737/1/PASTgateways14_staerz.pdf https://hdl.handle.net/10013/epic.43716 https://hdl.handle.net/10013/epic.43716.d001 |
genre |
Arctic Ocean East Greenland east greenland current Greenland Greenland-Scotland Ridge Nordic Seas north atlantic current North Atlantic |
genre_facet |
Arctic Ocean East Greenland east greenland current Greenland Greenland-Scotland Ridge Nordic Seas north atlantic current North Atlantic |
op_source |
EPIC3Proceedings of the II PAST Gateways - International converence and workshop, Trieste, Italy, 2014-05-19-2014-05-23 |
op_relation |
https://epic.awi.de/id/eprint/35737/1/PASTgateways14_staerz.pdf https://hdl.handle.net/10013/epic.43716.d001 Stärz, M. , Lohmann, G. orcid:0000-0003-2089-733X , Knorr, G. orcid:0000-0002-8317-5046 and Jokat, W. orcid:0000-0002-7793-5854 (2014) The evolution of Miocene ocean circulation controlled by the Greenland-Scotland Ridge , Proceedings of the II PAST Gateways - International converence and workshop, Trieste, Italy, 19 May 2014 - 23 May 2014 . hdl:10013/epic.43716 |
_version_ |
1810429524448378880 |