Large deglacial shifts of the Pacific Intertropical Convergence Zone

The position of the Intertropical Convergence Zone (ITCZ) is sensitive to changes in the balance of heat between the hemispheres which has fundamental implications for tropical hydrology and atmospheric circulation. Although the ITCZ is thought to experience the largest shifts in position during deg...

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Main Authors: Jacobel, Allison W., McManus, Jerry F., Anderson, Robert F., Winckler, Gisela
Format: Article in Journal/Newspaper
Language:English
Published: Nature Publishing Group 2016
Subjects:
Online Access:https://doi.org/10.7916/D8FN160G
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spelling ftcolumbiauniv:oai:academiccommons.columbia.edu:10.7916/D8FN160G 2023-05-15T17:32:44+02:00 Large deglacial shifts of the Pacific Intertropical Convergence Zone Jacobel, Allison W. McManus, Jerry F. Anderson, Robert F. Winckler, Gisela 2016 https://doi.org/10.7916/D8FN160G English eng Nature Publishing Group https://doi.org/10.7916/D8FN160G Atmospheric circulation Hydrology Intertropical convergence zone Paleoclimatology Articles 2016 ftcolumbiauniv https://doi.org/10.7916/D8FN160G 2019-04-04T08:14:03Z The position of the Intertropical Convergence Zone (ITCZ) is sensitive to changes in the balance of heat between the hemispheres which has fundamental implications for tropical hydrology and atmospheric circulation. Although the ITCZ is thought to experience the largest shifts in position during deglacial stadial events, the magnitude of shifts has proven difficult to reconstruct, in part because of a paucity of high-resolution records, particularly those including spatial components. Here we track the position of the ITCZ from 150 to 110 ka at three sites in the central equatorial Pacific at sub-millennial time resolution. Our results provide evidence of large, abrupt changes in tropical climate during the penultimate deglaciation, coincident with North Atlantic Heinrich Stadial 11 (~136–129 ka). We identify this event both as a Northern Hemisphere increase in aeolian dust and as a shift in the mean position of the ITCZ a minimum of 4° southwards at 160° W. Article in Journal/Newspaper North Atlantic Columbia University: Academic Commons Pacific
institution Open Polar
collection Columbia University: Academic Commons
op_collection_id ftcolumbiauniv
language English
topic Atmospheric circulation
Hydrology
Intertropical convergence zone
Paleoclimatology
spellingShingle Atmospheric circulation
Hydrology
Intertropical convergence zone
Paleoclimatology
Jacobel, Allison W.
McManus, Jerry F.
Anderson, Robert F.
Winckler, Gisela
Large deglacial shifts of the Pacific Intertropical Convergence Zone
topic_facet Atmospheric circulation
Hydrology
Intertropical convergence zone
Paleoclimatology
description The position of the Intertropical Convergence Zone (ITCZ) is sensitive to changes in the balance of heat between the hemispheres which has fundamental implications for tropical hydrology and atmospheric circulation. Although the ITCZ is thought to experience the largest shifts in position during deglacial stadial events, the magnitude of shifts has proven difficult to reconstruct, in part because of a paucity of high-resolution records, particularly those including spatial components. Here we track the position of the ITCZ from 150 to 110 ka at three sites in the central equatorial Pacific at sub-millennial time resolution. Our results provide evidence of large, abrupt changes in tropical climate during the penultimate deglaciation, coincident with North Atlantic Heinrich Stadial 11 (~136–129 ka). We identify this event both as a Northern Hemisphere increase in aeolian dust and as a shift in the mean position of the ITCZ a minimum of 4° southwards at 160° W.
format Article in Journal/Newspaper
author Jacobel, Allison W.
McManus, Jerry F.
Anderson, Robert F.
Winckler, Gisela
author_facet Jacobel, Allison W.
McManus, Jerry F.
Anderson, Robert F.
Winckler, Gisela
author_sort Jacobel, Allison W.
title Large deglacial shifts of the Pacific Intertropical Convergence Zone
title_short Large deglacial shifts of the Pacific Intertropical Convergence Zone
title_full Large deglacial shifts of the Pacific Intertropical Convergence Zone
title_fullStr Large deglacial shifts of the Pacific Intertropical Convergence Zone
title_full_unstemmed Large deglacial shifts of the Pacific Intertropical Convergence Zone
title_sort large deglacial shifts of the pacific intertropical convergence zone
publisher Nature Publishing Group
publishDate 2016
url https://doi.org/10.7916/D8FN160G
geographic Pacific
geographic_facet Pacific
genre North Atlantic
genre_facet North Atlantic
op_relation https://doi.org/10.7916/D8FN160G
op_doi https://doi.org/10.7916/D8FN160G
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