Absence of Cooling in New Zealand and the Adjacent Ocean During the Younger Dryas Chronozone
As the climate warmed at the end of the last glacial period, a rapid reversal in temperature, the Younger Dryas (YD) event, briefly returned much of the North Atlantic region to near full-glacial conditions. The event was associated with climate reversals in many other areas of the Northern Hemisphe...
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ftanucanberra:oai:openresearch-repository.anu.edu.au:1885/30345 2024-01-14T10:00:05+01:00 Absence of Cooling in New Zealand and the Adjacent Ocean During the Younger Dryas Chronozone Barrows, Timothy Lehman, Scott J. Fifield, L Keith De Deckker, Patrick http://hdl.handle.net/1885/30345 https://doi.org/10.1126/science.1145873 https://openresearch-repository.anu.edu.au/bitstream/1885/30345/5/ANUP1802.pdf.jpg https://openresearch-repository.anu.edu.au/bitstream/1885/30345/7/01_Barrows_Absence_of_Cooling_in_New_2007.pdf.jpg unknown American Association for the Advancement of Science 0036-8075 http://hdl.handle.net/1885/30345 doi:10.1126/science.1145873 https://openresearch-repository.anu.edu.au/bitstream/1885/30345/5/ANUP1802.pdf.jpg https://openresearch-repository.anu.edu.au/bitstream/1885/30345/7/01_Barrows_Absence_of_Cooling_in_New_2007.pdf.jpg Science Keywords: climate change Last Glacial marine environment temperature gradient article Atlantic cod Atlantic Ocean climate change cooling geology glacier latitude New Zealand priority journal Atlantic Ocean (North) Australasia New Zea Journal article ftanucanberra https://doi.org/10.1126/science.1145873 2023-12-15T09:35:59Z As the climate warmed at the end of the last glacial period, a rapid reversal in temperature, the Younger Dryas (YD) event, briefly returned much of the North Atlantic region to near full-glacial conditions. The event was associated with climate reversals in many other areas of the Northern Hemisphere and also with warming over and near Antarctica. However, the expression of the YD in the mid- to low latitudes of the Southern Hemisphere (and the southwest Pacific region in particular) is much more controversial. Here we show that the Waiho Loop advance of the Franz Josef Glacier in New Zealand was not a YD event, as previously thought, and that the adjacent ocean warmed throughout the YD. Article in Journal/Newspaper Antarc* Antarctica atlantic cod North Atlantic Australian National University: ANU Digital Collections Pacific New Zealand Science 318 5847 86 89 |
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Open Polar |
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Australian National University: ANU Digital Collections |
op_collection_id |
ftanucanberra |
language |
unknown |
topic |
Keywords: climate change Last Glacial marine environment temperature gradient article Atlantic cod Atlantic Ocean climate change cooling geology glacier latitude New Zealand priority journal Atlantic Ocean (North) Australasia New Zea |
spellingShingle |
Keywords: climate change Last Glacial marine environment temperature gradient article Atlantic cod Atlantic Ocean climate change cooling geology glacier latitude New Zealand priority journal Atlantic Ocean (North) Australasia New Zea Barrows, Timothy Lehman, Scott J. Fifield, L Keith De Deckker, Patrick Absence of Cooling in New Zealand and the Adjacent Ocean During the Younger Dryas Chronozone |
topic_facet |
Keywords: climate change Last Glacial marine environment temperature gradient article Atlantic cod Atlantic Ocean climate change cooling geology glacier latitude New Zealand priority journal Atlantic Ocean (North) Australasia New Zea |
description |
As the climate warmed at the end of the last glacial period, a rapid reversal in temperature, the Younger Dryas (YD) event, briefly returned much of the North Atlantic region to near full-glacial conditions. The event was associated with climate reversals in many other areas of the Northern Hemisphere and also with warming over and near Antarctica. However, the expression of the YD in the mid- to low latitudes of the Southern Hemisphere (and the southwest Pacific region in particular) is much more controversial. Here we show that the Waiho Loop advance of the Franz Josef Glacier in New Zealand was not a YD event, as previously thought, and that the adjacent ocean warmed throughout the YD. |
format |
Article in Journal/Newspaper |
author |
Barrows, Timothy Lehman, Scott J. Fifield, L Keith De Deckker, Patrick |
author_facet |
Barrows, Timothy Lehman, Scott J. Fifield, L Keith De Deckker, Patrick |
author_sort |
Barrows, Timothy |
title |
Absence of Cooling in New Zealand and the Adjacent Ocean During the Younger Dryas Chronozone |
title_short |
Absence of Cooling in New Zealand and the Adjacent Ocean During the Younger Dryas Chronozone |
title_full |
Absence of Cooling in New Zealand and the Adjacent Ocean During the Younger Dryas Chronozone |
title_fullStr |
Absence of Cooling in New Zealand and the Adjacent Ocean During the Younger Dryas Chronozone |
title_full_unstemmed |
Absence of Cooling in New Zealand and the Adjacent Ocean During the Younger Dryas Chronozone |
title_sort |
absence of cooling in new zealand and the adjacent ocean during the younger dryas chronozone |
publisher |
American Association for the Advancement of Science |
url |
http://hdl.handle.net/1885/30345 https://doi.org/10.1126/science.1145873 https://openresearch-repository.anu.edu.au/bitstream/1885/30345/5/ANUP1802.pdf.jpg https://openresearch-repository.anu.edu.au/bitstream/1885/30345/7/01_Barrows_Absence_of_Cooling_in_New_2007.pdf.jpg |
geographic |
Pacific New Zealand |
geographic_facet |
Pacific New Zealand |
genre |
Antarc* Antarctica atlantic cod North Atlantic |
genre_facet |
Antarc* Antarctica atlantic cod North Atlantic |
op_source |
Science |
op_relation |
0036-8075 http://hdl.handle.net/1885/30345 doi:10.1126/science.1145873 https://openresearch-repository.anu.edu.au/bitstream/1885/30345/5/ANUP1802.pdf.jpg https://openresearch-repository.anu.edu.au/bitstream/1885/30345/7/01_Barrows_Absence_of_Cooling_in_New_2007.pdf.jpg |
op_doi |
https://doi.org/10.1126/science.1145873 |
container_title |
Science |
container_volume |
318 |
container_issue |
5847 |
container_start_page |
86 |
op_container_end_page |
89 |
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1788063468998361088 |