Ocean tides and Heinrich events
Climate varied enormously over the most recent ice age1 — for example, large pulses of ice-rafted debris2, originating mainly from the Labrador Sea3, were deposited into the North Atlantic at roughly 7,000-year intervals, with global climatic implications3. Here we show that ocean tides within the L...
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ftumdeepblue:oai:deepblue.lib.umich.edu:2027.42/84375 2024-09-15T18:17:15+00:00 Ocean tides and Heinrich events Arbic, Brian K. MacAyeal, Douglas Mitrovica, Jerry Milne, Glenn Geological Sciences, Department of Ann Arbor 2004 application/octet-stream application/msword https://hdl.handle.net/2027.42/84375 en_US eng Nature Publishing Group Arbic, B.K., MacAyeal, D.R., ,Mitrovica, J.X., and G.A. MIlne, 2004: Ocean tides and Heinrich events, 432, 460 <http://hdl.handle.net/2027.42/84375> https://hdl.handle.net/2027.42/84375 15565143 Nature Geological Sciences Science Article 2004 ftumdeepblue 2024-07-30T04:06:06Z Climate varied enormously over the most recent ice age1 — for example, large pulses of ice-rafted debris2, originating mainly from the Labrador Sea3, were deposited into the North Atlantic at roughly 7,000-year intervals, with global climatic implications3. Here we show that ocean tides within the Labrador Sea were exceptionally large over the period spanning these huge, abrupt ice movements, which are known as Heinrich events. We propose that tides played a catalytic role in liberating iceberg armadas during that time. Peer Reviewed http://deepblue.lib.umich.edu/bitstream/2027.42/84375/1/nature_tidesheinrich.pdf http://deepblue.lib.umich.edu/bitstream/2027.42/84375/2/432460a-s1.doc Article in Journal/Newspaper Labrador Sea North Atlantic University of Michigan: Deep Blue |
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University of Michigan: Deep Blue |
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ftumdeepblue |
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English |
topic |
Geological Sciences Science |
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Geological Sciences Science Arbic, Brian K. MacAyeal, Douglas Mitrovica, Jerry Milne, Glenn Ocean tides and Heinrich events |
topic_facet |
Geological Sciences Science |
description |
Climate varied enormously over the most recent ice age1 — for example, large pulses of ice-rafted debris2, originating mainly from the Labrador Sea3, were deposited into the North Atlantic at roughly 7,000-year intervals, with global climatic implications3. Here we show that ocean tides within the Labrador Sea were exceptionally large over the period spanning these huge, abrupt ice movements, which are known as Heinrich events. We propose that tides played a catalytic role in liberating iceberg armadas during that time. Peer Reviewed http://deepblue.lib.umich.edu/bitstream/2027.42/84375/1/nature_tidesheinrich.pdf http://deepblue.lib.umich.edu/bitstream/2027.42/84375/2/432460a-s1.doc |
author2 |
Geological Sciences, Department of Ann Arbor |
format |
Article in Journal/Newspaper |
author |
Arbic, Brian K. MacAyeal, Douglas Mitrovica, Jerry Milne, Glenn |
author_facet |
Arbic, Brian K. MacAyeal, Douglas Mitrovica, Jerry Milne, Glenn |
author_sort |
Arbic, Brian K. |
title |
Ocean tides and Heinrich events |
title_short |
Ocean tides and Heinrich events |
title_full |
Ocean tides and Heinrich events |
title_fullStr |
Ocean tides and Heinrich events |
title_full_unstemmed |
Ocean tides and Heinrich events |
title_sort |
ocean tides and heinrich events |
publisher |
Nature Publishing Group |
publishDate |
2004 |
url |
https://hdl.handle.net/2027.42/84375 |
genre |
Labrador Sea North Atlantic |
genre_facet |
Labrador Sea North Atlantic |
op_relation |
Arbic, B.K., MacAyeal, D.R., ,Mitrovica, J.X., and G.A. MIlne, 2004: Ocean tides and Heinrich events, 432, 460 <http://hdl.handle.net/2027.42/84375> https://hdl.handle.net/2027.42/84375 15565143 Nature |
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1810455253652340736 |