Monsoonal Forcing of European Ice-Sheet Dynamics During the Late Quaternary
The dynamics of Northern Hemisphere ice sheets during Late Quaternary glacials have yet been dominantly examined from a Laurentide Ice Sheet perspective, which helped shaping the idea of moisture-starved glacials and small-scale ice volume variability. However, the waxing and waning of the European...
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ftunivutrecht:oai:dspace.library.uu.nl:1874/376773 2023-11-12T04:18:41+01:00 Monsoonal Forcing of European Ice-Sheet Dynamics During the Late Quaternary Kaboth-Bahr, Stefanie Bahr, André Zeeden, Christian Toucanne, Samuel Eynaud, Frédérique Jiménez-Espejo, Francisco Röhl, Ursula Friedrich, Oliver Pross, Jörg Löwemark, Ludvig Lourens, Lucas J. Stratigraphy & paleontology Stratigraphy and paleontology 2018-07-28 text/html https://dspace.library.uu.nl/handle/1874/376773 en eng 0094-8276 https://dspace.library.uu.nl/handle/1874/376773 info:eu-repo/semantics/OpenAccess European Ice Sheet dynamics glacial climate variability low-latitude forcing of high-latitude glaciations marine-terrestrial feedback in the Euro-Mediterranean realm Mediterranean Outflow variability Geophysics Earth and Planetary Sciences(all) Article 2018 ftunivutrecht 2023-11-01T23:19:50Z The dynamics of Northern Hemisphere ice sheets during Late Quaternary glacials have yet been dominantly examined from a Laurentide Ice Sheet perspective, which helped shaping the idea of moisture-starved glacials and small-scale ice volume variability. However, the waxing and waning of the European Ice Sheet (EIS) casts doubt on this perception. Understanding EIS dynamics under glacial boundary conditions is crucial because its meltwater pulses influence global climate by weakening deepwater formation in the North Atlantic Ocean. Here we show that the advection of subtropical water toward the continental margin of western Europe lead to enhanced moisture availability on the continent and fueled the growth of EIS lobes during glacials. This warm-water pooling was caused by monsoonally paced enhanced Mediterranean Outflow Water (MOW) entrainment that dragged subtropical surface waters toward the European margin. This mechanism presents a yet unrecognized marine-terrestrial pathway that allows low-latitude forcing to shape high-latitude glaciations. Article in Journal/Newspaper Ice Sheet North Atlantic Utrecht University Repository |
institution |
Open Polar |
collection |
Utrecht University Repository |
op_collection_id |
ftunivutrecht |
language |
English |
topic |
European Ice Sheet dynamics glacial climate variability low-latitude forcing of high-latitude glaciations marine-terrestrial feedback in the Euro-Mediterranean realm Mediterranean Outflow variability Geophysics Earth and Planetary Sciences(all) |
spellingShingle |
European Ice Sheet dynamics glacial climate variability low-latitude forcing of high-latitude glaciations marine-terrestrial feedback in the Euro-Mediterranean realm Mediterranean Outflow variability Geophysics Earth and Planetary Sciences(all) Kaboth-Bahr, Stefanie Bahr, André Zeeden, Christian Toucanne, Samuel Eynaud, Frédérique Jiménez-Espejo, Francisco Röhl, Ursula Friedrich, Oliver Pross, Jörg Löwemark, Ludvig Lourens, Lucas J. Monsoonal Forcing of European Ice-Sheet Dynamics During the Late Quaternary |
topic_facet |
European Ice Sheet dynamics glacial climate variability low-latitude forcing of high-latitude glaciations marine-terrestrial feedback in the Euro-Mediterranean realm Mediterranean Outflow variability Geophysics Earth and Planetary Sciences(all) |
description |
The dynamics of Northern Hemisphere ice sheets during Late Quaternary glacials have yet been dominantly examined from a Laurentide Ice Sheet perspective, which helped shaping the idea of moisture-starved glacials and small-scale ice volume variability. However, the waxing and waning of the European Ice Sheet (EIS) casts doubt on this perception. Understanding EIS dynamics under glacial boundary conditions is crucial because its meltwater pulses influence global climate by weakening deepwater formation in the North Atlantic Ocean. Here we show that the advection of subtropical water toward the continental margin of western Europe lead to enhanced moisture availability on the continent and fueled the growth of EIS lobes during glacials. This warm-water pooling was caused by monsoonally paced enhanced Mediterranean Outflow Water (MOW) entrainment that dragged subtropical surface waters toward the European margin. This mechanism presents a yet unrecognized marine-terrestrial pathway that allows low-latitude forcing to shape high-latitude glaciations. |
author2 |
Stratigraphy & paleontology Stratigraphy and paleontology |
format |
Article in Journal/Newspaper |
author |
Kaboth-Bahr, Stefanie Bahr, André Zeeden, Christian Toucanne, Samuel Eynaud, Frédérique Jiménez-Espejo, Francisco Röhl, Ursula Friedrich, Oliver Pross, Jörg Löwemark, Ludvig Lourens, Lucas J. |
author_facet |
Kaboth-Bahr, Stefanie Bahr, André Zeeden, Christian Toucanne, Samuel Eynaud, Frédérique Jiménez-Espejo, Francisco Röhl, Ursula Friedrich, Oliver Pross, Jörg Löwemark, Ludvig Lourens, Lucas J. |
author_sort |
Kaboth-Bahr, Stefanie |
title |
Monsoonal Forcing of European Ice-Sheet Dynamics During the Late Quaternary |
title_short |
Monsoonal Forcing of European Ice-Sheet Dynamics During the Late Quaternary |
title_full |
Monsoonal Forcing of European Ice-Sheet Dynamics During the Late Quaternary |
title_fullStr |
Monsoonal Forcing of European Ice-Sheet Dynamics During the Late Quaternary |
title_full_unstemmed |
Monsoonal Forcing of European Ice-Sheet Dynamics During the Late Quaternary |
title_sort |
monsoonal forcing of european ice-sheet dynamics during the late quaternary |
publishDate |
2018 |
url |
https://dspace.library.uu.nl/handle/1874/376773 |
genre |
Ice Sheet North Atlantic |
genre_facet |
Ice Sheet North Atlantic |
op_relation |
0094-8276 https://dspace.library.uu.nl/handle/1874/376773 |
op_rights |
info:eu-repo/semantics/OpenAccess |
_version_ |
1782335272708472832 |