Extent and Dynamics of the Scandinavian Ice Sheet during Oxygen Isotope Stage 3 (65,000–25,000 yr B.P.)
Abstract The climate of the middle Weichselian Glaciation, Marine Oxygen Isotope Stage 3 (OIS-3), a relatively mild period compared to the glacial maxima of OIS-4 and OIS-2, consisted of long warm interstades punctuated by brief cold excursions that grew colder and more frequent with time. The OIS-4...
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crcambridgeupr:10.1006/qres.2001.2298 2024-06-09T07:46:46+00:00 Extent and Dynamics of the Scandinavian Ice Sheet during Oxygen Isotope Stage 3 (65,000–25,000 yr B.P.) Arnold, Neil S. van Andel, Tjeerd H. Valen, Vidar 2002 http://dx.doi.org/10.1006/qres.2001.2298 http://api.elsevier.com/content/article/PII:S0033589401922987?httpAccept=text/xml http://api.elsevier.com/content/article/PII:S0033589401922987?httpAccept=text/plain https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0033589400010553 en eng Cambridge University Press (CUP) https://www.cambridge.org/core/terms Quaternary Research volume 57, issue 1, page 38-48 ISSN 0033-5894 1096-0287 journal-article 2002 crcambridgeupr https://doi.org/10.1006/qres.2001.2298 2024-05-15T13:00:58Z Abstract The climate of the middle Weichselian Glaciation, Marine Oxygen Isotope Stage 3 (OIS-3), a relatively mild period compared to the glacial maxima of OIS-4 and OIS-2, consisted of long warm interstades punctuated by brief cold excursions that grew colder and more frequent with time. The OIS-4 ice sheet is generally thought to have persisted throughout OIS-3, but evidence from dated OIS-3 interstadial deposits suggests that it was swiftly reduced to small remnants which only briefly expanded and retreated. Only 30,000 years ago the deteriorating climate initiated a sustained ice advance leading toward the final glacial maximum of OIS-2. Dynamic ice-sheet models support the existence of a prolonged ice-free interval during OIS-3 induced, perhaps, by low precipitation due to extensive sea-ice cover offshore. Article in Journal/Newspaper Ice Sheet Sea ice Cambridge University Press Quaternary Research 57 1 38 48 |
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Cambridge University Press |
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English |
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Abstract The climate of the middle Weichselian Glaciation, Marine Oxygen Isotope Stage 3 (OIS-3), a relatively mild period compared to the glacial maxima of OIS-4 and OIS-2, consisted of long warm interstades punctuated by brief cold excursions that grew colder and more frequent with time. The OIS-4 ice sheet is generally thought to have persisted throughout OIS-3, but evidence from dated OIS-3 interstadial deposits suggests that it was swiftly reduced to small remnants which only briefly expanded and retreated. Only 30,000 years ago the deteriorating climate initiated a sustained ice advance leading toward the final glacial maximum of OIS-2. Dynamic ice-sheet models support the existence of a prolonged ice-free interval during OIS-3 induced, perhaps, by low precipitation due to extensive sea-ice cover offshore. |
format |
Article in Journal/Newspaper |
author |
Arnold, Neil S. van Andel, Tjeerd H. Valen, Vidar |
spellingShingle |
Arnold, Neil S. van Andel, Tjeerd H. Valen, Vidar Extent and Dynamics of the Scandinavian Ice Sheet during Oxygen Isotope Stage 3 (65,000–25,000 yr B.P.) |
author_facet |
Arnold, Neil S. van Andel, Tjeerd H. Valen, Vidar |
author_sort |
Arnold, Neil S. |
title |
Extent and Dynamics of the Scandinavian Ice Sheet during Oxygen Isotope Stage 3 (65,000–25,000 yr B.P.) |
title_short |
Extent and Dynamics of the Scandinavian Ice Sheet during Oxygen Isotope Stage 3 (65,000–25,000 yr B.P.) |
title_full |
Extent and Dynamics of the Scandinavian Ice Sheet during Oxygen Isotope Stage 3 (65,000–25,000 yr B.P.) |
title_fullStr |
Extent and Dynamics of the Scandinavian Ice Sheet during Oxygen Isotope Stage 3 (65,000–25,000 yr B.P.) |
title_full_unstemmed |
Extent and Dynamics of the Scandinavian Ice Sheet during Oxygen Isotope Stage 3 (65,000–25,000 yr B.P.) |
title_sort |
extent and dynamics of the scandinavian ice sheet during oxygen isotope stage 3 (65,000–25,000 yr b.p.) |
publisher |
Cambridge University Press (CUP) |
publishDate |
2002 |
url |
http://dx.doi.org/10.1006/qres.2001.2298 http://api.elsevier.com/content/article/PII:S0033589401922987?httpAccept=text/xml http://api.elsevier.com/content/article/PII:S0033589401922987?httpAccept=text/plain https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0033589400010553 |
genre |
Ice Sheet Sea ice |
genre_facet |
Ice Sheet Sea ice |
op_source |
Quaternary Research volume 57, issue 1, page 38-48 ISSN 0033-5894 1096-0287 |
op_rights |
https://www.cambridge.org/core/terms |
op_doi |
https://doi.org/10.1006/qres.2001.2298 |
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Quaternary Research |
container_volume |
57 |
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1 |
container_start_page |
38 |
op_container_end_page |
48 |
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1801376755923025920 |