Evidence of 550-year and 1000-year cyclicities in North Atlantic circulation patterns during the Holocene
Sedimentological colour data obtained from North Atlantic deep-sea sediment core NEAP15K pro vide a continuous climate record for the last 11500 yr with a mean sampling interval of <15 yr. Variations in sediment lightness, a proxy for changes in North Atlantic Deep Water (NADW) circulation, are c...
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Online Access: | http://dx.doi.org/10.1191/095968300671253196 http://journals.sagepub.com/doi/pdf/10.1191/095968300671253196 |
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crsagepubl:10.1191/095968300671253196 2024-09-15T18:09:52+00:00 Evidence of 550-year and 1000-year cyclicities in North Atlantic circulation patterns during the Holocene Chapman, Mark R. Shackleton, Nicholas J. 2000 http://dx.doi.org/10.1191/095968300671253196 http://journals.sagepub.com/doi/pdf/10.1191/095968300671253196 en eng SAGE Publications http://journals.sagepub.com/page/policies/text-and-data-mining-license The Holocene volume 10, issue 3, page 287-291 ISSN 0959-6836 1477-0911 journal-article 2000 crsagepubl https://doi.org/10.1191/095968300671253196 2024-08-19T04:27:45Z Sedimentological colour data obtained from North Atlantic deep-sea sediment core NEAP15K pro vide a continuous climate record for the last 11500 yr with a mean sampling interval of <15 yr. Variations in sediment lightness, a proxy for changes in North Atlantic Deep Water (NADW) circulation, are characterized by high-frequency fluctuations with periodicities equivalent to 550 and 1000 yr, as well as a <1600-yr cyclicity comparable to that reported in other studies of Holocene climate. Cross-spectral analysis suggests that the 550-yr and 1000-yr cyclical variations in NADW circulation were coherent with fluctuations in atmospheric con ditions over Greenland, where both these periodicities have been identified previously in the Holocene GISP2 d 18 O record (Stuiver et al., 1995). A similar statistical comparison provides evidence that high-frequency (550-yr) variability in NADW circulation patterns may have been linked to short-term variations in atmospheric 14 C values during the Holocene. In general, NADW production was lower and 14C levels were higher when colder climatic conditions prevailed. These results imply that the pattern of NADW production has been a significant factor affecting centennial-to millennial-scale Holocene climate variability in the North Atlantic region. Article in Journal/Newspaper Greenland NADW North Atlantic Deep Water North Atlantic SAGE Publications The Holocene 10 3 287 291 |
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English |
description |
Sedimentological colour data obtained from North Atlantic deep-sea sediment core NEAP15K pro vide a continuous climate record for the last 11500 yr with a mean sampling interval of <15 yr. Variations in sediment lightness, a proxy for changes in North Atlantic Deep Water (NADW) circulation, are characterized by high-frequency fluctuations with periodicities equivalent to 550 and 1000 yr, as well as a <1600-yr cyclicity comparable to that reported in other studies of Holocene climate. Cross-spectral analysis suggests that the 550-yr and 1000-yr cyclical variations in NADW circulation were coherent with fluctuations in atmospheric con ditions over Greenland, where both these periodicities have been identified previously in the Holocene GISP2 d 18 O record (Stuiver et al., 1995). A similar statistical comparison provides evidence that high-frequency (550-yr) variability in NADW circulation patterns may have been linked to short-term variations in atmospheric 14 C values during the Holocene. In general, NADW production was lower and 14C levels were higher when colder climatic conditions prevailed. These results imply that the pattern of NADW production has been a significant factor affecting centennial-to millennial-scale Holocene climate variability in the North Atlantic region. |
format |
Article in Journal/Newspaper |
author |
Chapman, Mark R. Shackleton, Nicholas J. |
spellingShingle |
Chapman, Mark R. Shackleton, Nicholas J. Evidence of 550-year and 1000-year cyclicities in North Atlantic circulation patterns during the Holocene |
author_facet |
Chapman, Mark R. Shackleton, Nicholas J. |
author_sort |
Chapman, Mark R. |
title |
Evidence of 550-year and 1000-year cyclicities in North Atlantic circulation patterns during the Holocene |
title_short |
Evidence of 550-year and 1000-year cyclicities in North Atlantic circulation patterns during the Holocene |
title_full |
Evidence of 550-year and 1000-year cyclicities in North Atlantic circulation patterns during the Holocene |
title_fullStr |
Evidence of 550-year and 1000-year cyclicities in North Atlantic circulation patterns during the Holocene |
title_full_unstemmed |
Evidence of 550-year and 1000-year cyclicities in North Atlantic circulation patterns during the Holocene |
title_sort |
evidence of 550-year and 1000-year cyclicities in north atlantic circulation patterns during the holocene |
publisher |
SAGE Publications |
publishDate |
2000 |
url |
http://dx.doi.org/10.1191/095968300671253196 http://journals.sagepub.com/doi/pdf/10.1191/095968300671253196 |
genre |
Greenland NADW North Atlantic Deep Water North Atlantic |
genre_facet |
Greenland NADW North Atlantic Deep Water North Atlantic |
op_source |
The Holocene volume 10, issue 3, page 287-291 ISSN 0959-6836 1477-0911 |
op_rights |
http://journals.sagepub.com/page/policies/text-and-data-mining-license |
op_doi |
https://doi.org/10.1191/095968300671253196 |
container_title |
The Holocene |
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10 |
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3 |
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287 |
op_container_end_page |
291 |
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1810447469972029440 |