Dust-climate couplings over the past 800,000 years from the EPICA Dome C ice core

Dust can affect the radiative balance of the atmosphere by absorbing or reflecting incoming solar radiation; it can also be a source of micronutrients, such as iron, to the ocean. It has been suggested that production, transport and deposition of dust is influenced by climatic changes on glacial-int...

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Published in:Nature
Main Authors: Lambert, F, Petit, JR, Bigler, M, Kaufmann, PR, Hutterli, MA, Stocker, TF, Ruth, U, Steffensen, JP, DELMONTE, BARBARA, MAGGI, VALTER
Other Authors: Delmonte, B, Petit, J, Kaufmann, P, Hutterli, M, Stocker, T, Steffensen, J, Maggi, V
Format: Article in Journal/Newspaper
Language:English
Published: Nature Publishing Group 2008
Subjects:
Online Access:http://hdl.handle.net/10281/6600
https://doi.org/10.1038/nature06763
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spelling ftunivmilanobic:oai:boa.unimib.it:10281/6600 2024-04-14T08:01:18+00:00 Dust-climate couplings over the past 800,000 years from the EPICA Dome C ice core Lambert, F Petit, JR Bigler, M Kaufmann, PR Hutterli, MA Stocker, TF Ruth, U Steffensen, JP DELMONTE, BARBARA MAGGI, VALTER Lambert, F Delmonte, B Petit, J Bigler, M Kaufmann, P Hutterli, M Stocker, T Ruth, U Steffensen, J Maggi, V 2008 http://hdl.handle.net/10281/6600 https://doi.org/10.1038/nature06763 eng eng Nature Publishing Group country:GB info:eu-repo/semantics/altIdentifier/pmid/18385736 info:eu-repo/semantics/altIdentifier/wos/WOS:000254567200042 volume:452 issue:7187 firstpage:616 lastpage:619 numberofpages:4 journal:NATURE http://hdl.handle.net/10281/6600 doi:10.1038/nature06763 info:eu-repo/semantics/altIdentifier/scopus/2-s2.0-41649092047 climate dust ice cores antarctica GEO/04 - GEOGRAFIA FISICA E GEOMORFOLOGIA info:eu-repo/semantics/article 2008 ftunivmilanobic https://doi.org/10.1038/nature06763 2024-03-21T16:26:14Z Dust can affect the radiative balance of the atmosphere by absorbing or reflecting incoming solar radiation; it can also be a source of micronutrients, such as iron, to the ocean. It has been suggested that production, transport and deposition of dust is influenced by climatic changes on glacial-interglacial timescales. Here we present a high-resolution record of aeolian dust from the EPICA Dome C ice core in East Antarctica, which provides an undisturbed climate sequence over the past eight climatic cycles. We find that there is a significant correlation between dust flux and temperature records during glacial periods that is absent during interglacial periods. Our data suggest that dust flux is increasingly correlated with Antarctic temperature as the climate becomes colder. We interpret this as progressive coupling of the climates of Antarctic and lower latitudes. Limited changes in glacial-interglacial atmospheric transport time suggest that the sources and lifetime of dust are the main factors controlling the high glacial dust input. We propose that the observed ∼25-fold increase in glacial dust flux over all eight glacial periods can be attributed to a strengthening of South American dust sources, together with a longer lifetime for atmospheric dust particles in the upper troposphere resulting from a reduced hydrological cycle during the ice ages. ©2008 Nature Publishing Group. Article in Journal/Newspaper Antarc* Antarctic Antarctica East Antarctica EPICA ice core Università degli Studi di Milano-Bicocca: BOA (Bicocca Open Archive) Antarctic East Antarctica Nature 452 7187 616 619
institution Open Polar
collection Università degli Studi di Milano-Bicocca: BOA (Bicocca Open Archive)
op_collection_id ftunivmilanobic
language English
topic climate
dust
ice cores
antarctica
GEO/04 - GEOGRAFIA FISICA E GEOMORFOLOGIA
spellingShingle climate
dust
ice cores
antarctica
GEO/04 - GEOGRAFIA FISICA E GEOMORFOLOGIA
Lambert, F
Petit, JR
Bigler, M
Kaufmann, PR
Hutterli, MA
Stocker, TF
Ruth, U
Steffensen, JP
DELMONTE, BARBARA
MAGGI, VALTER
Dust-climate couplings over the past 800,000 years from the EPICA Dome C ice core
topic_facet climate
dust
ice cores
antarctica
GEO/04 - GEOGRAFIA FISICA E GEOMORFOLOGIA
description Dust can affect the radiative balance of the atmosphere by absorbing or reflecting incoming solar radiation; it can also be a source of micronutrients, such as iron, to the ocean. It has been suggested that production, transport and deposition of dust is influenced by climatic changes on glacial-interglacial timescales. Here we present a high-resolution record of aeolian dust from the EPICA Dome C ice core in East Antarctica, which provides an undisturbed climate sequence over the past eight climatic cycles. We find that there is a significant correlation between dust flux and temperature records during glacial periods that is absent during interglacial periods. Our data suggest that dust flux is increasingly correlated with Antarctic temperature as the climate becomes colder. We interpret this as progressive coupling of the climates of Antarctic and lower latitudes. Limited changes in glacial-interglacial atmospheric transport time suggest that the sources and lifetime of dust are the main factors controlling the high glacial dust input. We propose that the observed ∼25-fold increase in glacial dust flux over all eight glacial periods can be attributed to a strengthening of South American dust sources, together with a longer lifetime for atmospheric dust particles in the upper troposphere resulting from a reduced hydrological cycle during the ice ages. ©2008 Nature Publishing Group.
author2 Lambert, F
Delmonte, B
Petit, J
Bigler, M
Kaufmann, P
Hutterli, M
Stocker, T
Ruth, U
Steffensen, J
Maggi, V
format Article in Journal/Newspaper
author Lambert, F
Petit, JR
Bigler, M
Kaufmann, PR
Hutterli, MA
Stocker, TF
Ruth, U
Steffensen, JP
DELMONTE, BARBARA
MAGGI, VALTER
author_facet Lambert, F
Petit, JR
Bigler, M
Kaufmann, PR
Hutterli, MA
Stocker, TF
Ruth, U
Steffensen, JP
DELMONTE, BARBARA
MAGGI, VALTER
author_sort Lambert, F
title Dust-climate couplings over the past 800,000 years from the EPICA Dome C ice core
title_short Dust-climate couplings over the past 800,000 years from the EPICA Dome C ice core
title_full Dust-climate couplings over the past 800,000 years from the EPICA Dome C ice core
title_fullStr Dust-climate couplings over the past 800,000 years from the EPICA Dome C ice core
title_full_unstemmed Dust-climate couplings over the past 800,000 years from the EPICA Dome C ice core
title_sort dust-climate couplings over the past 800,000 years from the epica dome c ice core
publisher Nature Publishing Group
publishDate 2008
url http://hdl.handle.net/10281/6600
https://doi.org/10.1038/nature06763
geographic Antarctic
East Antarctica
geographic_facet Antarctic
East Antarctica
genre Antarc*
Antarctic
Antarctica
East Antarctica
EPICA
ice core
genre_facet Antarc*
Antarctic
Antarctica
East Antarctica
EPICA
ice core
op_relation info:eu-repo/semantics/altIdentifier/pmid/18385736
info:eu-repo/semantics/altIdentifier/wos/WOS:000254567200042
volume:452
issue:7187
firstpage:616
lastpage:619
numberofpages:4
journal:NATURE
http://hdl.handle.net/10281/6600
doi:10.1038/nature06763
info:eu-repo/semantics/altIdentifier/scopus/2-s2.0-41649092047
op_doi https://doi.org/10.1038/nature06763
container_title Nature
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container_issue 7187
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