Centennial oscillation of the climatic crescendo during the last glacial maximum: evidence from Lake Estancia, central New Mexico

Sediments deposited in late Pleistocene Lake Estancia, central New Mexico, contain a paleoclimatic record that includes the last glacial maximum and deglacial episode. Stratigraphic reconstruction of an interval representing the highstand of the lake that occurred during the last glacial maximum rev...

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Main Authors: Allen, Bruce D., Anderson, Roger Y.
Format: Other/Unknown Material
Language:English
Published: 1992
Subjects:
Online Access:http://hdl.handle.net/1834/31447
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spelling ftoceandocs:oai:aquadocs.org:1834/31447 2023-05-15T16:40:39+02:00 Centennial oscillation of the climatic crescendo during the last glacial maximum: evidence from Lake Estancia, central New Mexico Allen, Bruce D. Anderson, Roger Y. 1992 application/pdf 13-18 http://hdl.handle.net/1834/31447 en eng http://hdl.handle.net/1834/31447 http://aquaticcommons.org/id/eprint/15627 8 2014-11-13 19:11:57 15627 Atmospheric Sciences Earth Sciences Limnology PACLIM conference_item 1992 ftoceandocs 2023-04-06T17:04:26Z Sediments deposited in late Pleistocene Lake Estancia, central New Mexico, contain a paleoclimatic record that includes the last glacial maximum and deglacial episode. Stratigraphic reconstruction of an interval representing the highstand of the lake that occurred during the last glacial maximum reveals ~2000-, ~600-, and ~200-year oscillations in lake level and climate. Shifting position of the polar jetstream in response to expansion and contraction of the North American ice sheet may be partly responsible for the millenial-scale changes in Lake Estancia but probably does not explain the centennial-scale oscillations. Other/Unknown Material Ice Sheet IODE-UNESCO: OceanDocs - E-Repository of Ocean Publications
institution Open Polar
collection IODE-UNESCO: OceanDocs - E-Repository of Ocean Publications
op_collection_id ftoceandocs
language English
topic Atmospheric Sciences
Earth Sciences
Limnology
PACLIM
spellingShingle Atmospheric Sciences
Earth Sciences
Limnology
PACLIM
Allen, Bruce D.
Anderson, Roger Y.
Centennial oscillation of the climatic crescendo during the last glacial maximum: evidence from Lake Estancia, central New Mexico
topic_facet Atmospheric Sciences
Earth Sciences
Limnology
PACLIM
description Sediments deposited in late Pleistocene Lake Estancia, central New Mexico, contain a paleoclimatic record that includes the last glacial maximum and deglacial episode. Stratigraphic reconstruction of an interval representing the highstand of the lake that occurred during the last glacial maximum reveals ~2000-, ~600-, and ~200-year oscillations in lake level and climate. Shifting position of the polar jetstream in response to expansion and contraction of the North American ice sheet may be partly responsible for the millenial-scale changes in Lake Estancia but probably does not explain the centennial-scale oscillations.
format Other/Unknown Material
author Allen, Bruce D.
Anderson, Roger Y.
author_facet Allen, Bruce D.
Anderson, Roger Y.
author_sort Allen, Bruce D.
title Centennial oscillation of the climatic crescendo during the last glacial maximum: evidence from Lake Estancia, central New Mexico
title_short Centennial oscillation of the climatic crescendo during the last glacial maximum: evidence from Lake Estancia, central New Mexico
title_full Centennial oscillation of the climatic crescendo during the last glacial maximum: evidence from Lake Estancia, central New Mexico
title_fullStr Centennial oscillation of the climatic crescendo during the last glacial maximum: evidence from Lake Estancia, central New Mexico
title_full_unstemmed Centennial oscillation of the climatic crescendo during the last glacial maximum: evidence from Lake Estancia, central New Mexico
title_sort centennial oscillation of the climatic crescendo during the last glacial maximum: evidence from lake estancia, central new mexico
publishDate 1992
url http://hdl.handle.net/1834/31447
genre Ice Sheet
genre_facet Ice Sheet
op_source http://aquaticcommons.org/id/eprint/15627
8
2014-11-13 19:11:57
15627
op_relation http://hdl.handle.net/1834/31447
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