Millenial-Scale Climatic Oscillations in New Zealand During the Last Glacial Cycle; PEP III Transect

Millennial-Scale Climatic Oscillations in New Zealand During the Last Glacial Cycle: PEP III Transect Paleoclimate records from Greenland ice cores and North Atlantic sediments indicate that the glacial climate over the North Atlantic basin was punctuated with large and frequent abrupt climatic chan...

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Main Author: Denton, George H.
Format: Text
Language:unknown
Published: DigitalCommons@UMaine 2004
Subjects:
Online Access:https://digitalcommons.library.umaine.edu/orsp_reports/89
https://digitalcommons.library.umaine.edu/cgi/viewcontent.cgi?article=1096&context=orsp_reports
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spelling ftmaineuniv:oai:digitalcommons.library.umaine.edu:orsp_reports-1096 2023-05-15T16:28:53+02:00 Millenial-Scale Climatic Oscillations in New Zealand During the Last Glacial Cycle; PEP III Transect Denton, George H. 2004-02-25T08:00:00Z application/pdf https://digitalcommons.library.umaine.edu/orsp_reports/89 https://digitalcommons.library.umaine.edu/cgi/viewcontent.cgi?article=1096&context=orsp_reports unknown DigitalCommons@UMaine https://digitalcommons.library.umaine.edu/orsp_reports/89 https://digitalcommons.library.umaine.edu/cgi/viewcontent.cgi?article=1096&context=orsp_reports This Item is protected by copyright and/or related rights. You are free to use this Item in any way that is permitted by the copyright and related rights legislation that applies to your use. In addition, no permission is required from the rights-holder(s) for educational uses. For other uses, you need to obtain permission from the rights-holder(s). University of Maine Office of Research Administration: Grant Reports Paleoclimate Climate Change Climate Environmental Indicators and Impact Assessment Environmental Sciences text 2004 ftmaineuniv 2023-03-12T19:15:10Z Millennial-Scale Climatic Oscillations in New Zealand During the Last Glacial Cycle: PEP III Transect Paleoclimate records from Greenland ice cores and North Atlantic sediments indicate that the glacial climate over the North Atlantic basin was punctuated with large and frequent abrupt climatic changes (Dansgaard-Oeschger and Henrich events). Because the events first appeared to have been regionally restricted, most explanations have invoked regional forcing mechanisms. But quite a different perspective would emerge if these events were shown to be of this global-scale. SGER award supports a reconnaissance study of the glacial and vegetative paleoclimate record of the massive morainal deposits of the Southern Alps of New Zealand This will establish the paleoclimate potential of this record to contribute to our understanding of interhemispheric climatic linkages and forcing mechanisms for the last glacial cycle. Text Greenland Greenland ice cores North Atlantic The University of Maine: DigitalCommons@UMaine Greenland New Zealand
institution Open Polar
collection The University of Maine: DigitalCommons@UMaine
op_collection_id ftmaineuniv
language unknown
topic Paleoclimate
Climate Change
Climate
Environmental Indicators and Impact Assessment
Environmental Sciences
spellingShingle Paleoclimate
Climate Change
Climate
Environmental Indicators and Impact Assessment
Environmental Sciences
Denton, George H.
Millenial-Scale Climatic Oscillations in New Zealand During the Last Glacial Cycle; PEP III Transect
topic_facet Paleoclimate
Climate Change
Climate
Environmental Indicators and Impact Assessment
Environmental Sciences
description Millennial-Scale Climatic Oscillations in New Zealand During the Last Glacial Cycle: PEP III Transect Paleoclimate records from Greenland ice cores and North Atlantic sediments indicate that the glacial climate over the North Atlantic basin was punctuated with large and frequent abrupt climatic changes (Dansgaard-Oeschger and Henrich events). Because the events first appeared to have been regionally restricted, most explanations have invoked regional forcing mechanisms. But quite a different perspective would emerge if these events were shown to be of this global-scale. SGER award supports a reconnaissance study of the glacial and vegetative paleoclimate record of the massive morainal deposits of the Southern Alps of New Zealand This will establish the paleoclimate potential of this record to contribute to our understanding of interhemispheric climatic linkages and forcing mechanisms for the last glacial cycle.
format Text
author Denton, George H.
author_facet Denton, George H.
author_sort Denton, George H.
title Millenial-Scale Climatic Oscillations in New Zealand During the Last Glacial Cycle; PEP III Transect
title_short Millenial-Scale Climatic Oscillations in New Zealand During the Last Glacial Cycle; PEP III Transect
title_full Millenial-Scale Climatic Oscillations in New Zealand During the Last Glacial Cycle; PEP III Transect
title_fullStr Millenial-Scale Climatic Oscillations in New Zealand During the Last Glacial Cycle; PEP III Transect
title_full_unstemmed Millenial-Scale Climatic Oscillations in New Zealand During the Last Glacial Cycle; PEP III Transect
title_sort millenial-scale climatic oscillations in new zealand during the last glacial cycle; pep iii transect
publisher DigitalCommons@UMaine
publishDate 2004
url https://digitalcommons.library.umaine.edu/orsp_reports/89
https://digitalcommons.library.umaine.edu/cgi/viewcontent.cgi?article=1096&context=orsp_reports
geographic Greenland
New Zealand
geographic_facet Greenland
New Zealand
genre Greenland
Greenland ice cores
North Atlantic
genre_facet Greenland
Greenland ice cores
North Atlantic
op_source University of Maine Office of Research Administration: Grant Reports
op_relation https://digitalcommons.library.umaine.edu/orsp_reports/89
https://digitalcommons.library.umaine.edu/cgi/viewcontent.cgi?article=1096&context=orsp_reports
op_rights This Item is protected by copyright and/or related rights. You are free to use this Item in any way that is permitted by the copyright and related rights legislation that applies to your use. In addition, no permission is required from the rights-holder(s) for educational uses. For other uses, you need to obtain permission from the rights-holder(s).
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