The climate of the Last Glacial period (10,000-110,000
years ago) was characterized by rapid millennial-scale climate fluctuations termed Dansgaard/Oeschger (D/O) and Heinrich (H) events. We present results from a speleothem-derived proxy of the South American Summer Monsoon (SASM) from 16,000-50,000 years ago that demonstrate the occurrence of D/O cycl...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.699.6155 2023-05-15T14:00:38+02:00 The climate of the Last Glacial period (10,000-110,000 The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.699.6155 en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.699.6155 Metadata may be used without restrictions as long as the oai identifier remains attached to it. https://www.geo.umass.edu/climate/papers2/Kanner_Science2012.pdf text ftciteseerx 2016-01-08T18:48:29Z years ago) was characterized by rapid millennial-scale climate fluctuations termed Dansgaard/Oeschger (D/O) and Heinrich (H) events. We present results from a speleothem-derived proxy of the South American Summer Monsoon (SASM) from 16,000-50,000 years ago that demonstrate the occurrence of D/O cycles and Heinrich events. This tropical Southern Hemisphere monsoon reconstruction illustrates an anti-phase relationship to Northern Hemisphere monsoon intensity at the millennial scale. Our results also show an influence of Antarctic millennial-scale climate fluctuations on the SASM. This high-resolution, precisely dated, tropical precipitation record can be used to establish the timing of climate events in the high latitudes of the Northern and Southern Hemispheres. Text Antarc* Antarctic Unknown Antarctic |
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ftciteseerx |
language |
English |
description |
years ago) was characterized by rapid millennial-scale climate fluctuations termed Dansgaard/Oeschger (D/O) and Heinrich (H) events. We present results from a speleothem-derived proxy of the South American Summer Monsoon (SASM) from 16,000-50,000 years ago that demonstrate the occurrence of D/O cycles and Heinrich events. This tropical Southern Hemisphere monsoon reconstruction illustrates an anti-phase relationship to Northern Hemisphere monsoon intensity at the millennial scale. Our results also show an influence of Antarctic millennial-scale climate fluctuations on the SASM. This high-resolution, precisely dated, tropical precipitation record can be used to establish the timing of climate events in the high latitudes of the Northern and Southern Hemispheres. |
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The Pennsylvania State University CiteSeerX Archives |
format |
Text |
title |
The climate of the Last Glacial period (10,000-110,000 |
spellingShingle |
The climate of the Last Glacial period (10,000-110,000 |
title_short |
The climate of the Last Glacial period (10,000-110,000 |
title_full |
The climate of the Last Glacial period (10,000-110,000 |
title_fullStr |
The climate of the Last Glacial period (10,000-110,000 |
title_full_unstemmed |
The climate of the Last Glacial period (10,000-110,000 |
title_sort |
climate of the last glacial period (10,000-110,000 |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.699.6155 |
geographic |
Antarctic |
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Antarctic |
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Antarc* Antarctic |
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Antarc* Antarctic |
op_source |
https://www.geo.umass.edu/climate/papers2/Kanner_Science2012.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.699.6155 |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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1766269867124588544 |