Younger Dryas Age Advance of Franz Josef Glacier in the Southern Alps of New Zealand

A corrected radiocarbon age of 11,050 ± 14 years before present for an advance of the Franz Josef Glacier to the Waiho Loop terminal moraine on the western flank of New Zealand's Southern Alps shows that glacier advance on a South Pacific island was synchronous with initiation of the Younger Dr...

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Published in:Science
Main Authors: Denton, G. H., Hendy, C. H.
Format: Article in Journal/Newspaper
Language:English
Published: American Association for the Advancement of Science (AAAS) 1994
Subjects:
Online Access:http://dx.doi.org/10.1126/science.264.5164.1434
https://www.science.org/doi/pdf/10.1126/science.264.5164.1434
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spelling craaas:10.1126/science.264.5164.1434 2024-04-28T08:29:43+00:00 Younger Dryas Age Advance of Franz Josef Glacier in the Southern Alps of New Zealand Denton, G. H. Hendy, C. H. 1994 http://dx.doi.org/10.1126/science.264.5164.1434 https://www.science.org/doi/pdf/10.1126/science.264.5164.1434 en eng American Association for the Advancement of Science (AAAS) Science volume 264, issue 5164, page 1434-1437 ISSN 0036-8075 1095-9203 Multidisciplinary journal-article 1994 craaas https://doi.org/10.1126/science.264.5164.1434 2024-04-09T06:41:11Z A corrected radiocarbon age of 11,050 ± 14 years before present for an advance of the Franz Josef Glacier to the Waiho Loop terminal moraine on the western flank of New Zealand's Southern Alps shows that glacier advance on a South Pacific island was synchronous with initiation of the Younger Dryas in the North Atlantic region. Hence, cooling at the beginning of the Younger Dryas probably reflects global rather than regional forcing. The source for Younger Dryas climatic cooling may thus lie in the atmosphere rather than in a North Atlantic thermohaline switch. Article in Journal/Newspaper North Atlantic AAAS Resource Center (American Association for the Advancement of Science) Science 264 5164 1434 1437
institution Open Polar
collection AAAS Resource Center (American Association for the Advancement of Science)
op_collection_id craaas
language English
topic Multidisciplinary
spellingShingle Multidisciplinary
Denton, G. H.
Hendy, C. H.
Younger Dryas Age Advance of Franz Josef Glacier in the Southern Alps of New Zealand
topic_facet Multidisciplinary
description A corrected radiocarbon age of 11,050 ± 14 years before present for an advance of the Franz Josef Glacier to the Waiho Loop terminal moraine on the western flank of New Zealand's Southern Alps shows that glacier advance on a South Pacific island was synchronous with initiation of the Younger Dryas in the North Atlantic region. Hence, cooling at the beginning of the Younger Dryas probably reflects global rather than regional forcing. The source for Younger Dryas climatic cooling may thus lie in the atmosphere rather than in a North Atlantic thermohaline switch.
format Article in Journal/Newspaper
author Denton, G. H.
Hendy, C. H.
author_facet Denton, G. H.
Hendy, C. H.
author_sort Denton, G. H.
title Younger Dryas Age Advance of Franz Josef Glacier in the Southern Alps of New Zealand
title_short Younger Dryas Age Advance of Franz Josef Glacier in the Southern Alps of New Zealand
title_full Younger Dryas Age Advance of Franz Josef Glacier in the Southern Alps of New Zealand
title_fullStr Younger Dryas Age Advance of Franz Josef Glacier in the Southern Alps of New Zealand
title_full_unstemmed Younger Dryas Age Advance of Franz Josef Glacier in the Southern Alps of New Zealand
title_sort younger dryas age advance of franz josef glacier in the southern alps of new zealand
publisher American Association for the Advancement of Science (AAAS)
publishDate 1994
url http://dx.doi.org/10.1126/science.264.5164.1434
https://www.science.org/doi/pdf/10.1126/science.264.5164.1434
genre North Atlantic
genre_facet North Atlantic
op_source Science
volume 264, issue 5164, page 1434-1437
ISSN 0036-8075 1095-9203
op_doi https://doi.org/10.1126/science.264.5164.1434
container_title Science
container_volume 264
container_issue 5164
container_start_page 1434
op_container_end_page 1437
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