Paleo±Dust: Quantifying uncertainty in paleo-dust deposition across archive types
- Autores
- Cosentino, Nicolas Juan; Torre, Gabriela; Lambert, Fabrice; Albani, Samuel; de Vleeschouwer, Francois; Bory, Aloys J.-M.
- Año de publicación
- 2024
- Idioma
- inglés
- Tipo de recurso
- artículo
- Estado
- versión publicada
- Descripción
- Mineral dust aerosol concentrations in the atmosphere varied greatly on glacial-interglacial timescales. The greatest changes in global dust activity occurred in response to changes in orbital parameters that affect dust emission intensity through glacial activity, and dust lifetime in the atmosphere through changes in the global hydrological cycle.Long-term changes in surface dust deposition rate are registered in geological archives such as loess, peats, lakes, marine sediments, and ice. Data provided by these archives is crucial for guiding simulations of dust, and for better understanding the natural global dust cycle. However, the methods employed to derive paleo-dust deposition rates differ markedly between archives and are subject to different sources of uncertainty. Here, we present Paleo±Dust, an updated compilation of bulk and <10-μm paleo-dust deposition rate with quantitative 1-σ uncertainties that are inter-comparable among archive types.Paleo±Dust incorporates a total of 284 pre-industrial Holocene (pi-HOL) and 208 Last Glacial Maximum (LGM) dust flux constraints from studies published until December 2022, including for the first time peat records. We also recalculate previously published dust fluxes to exclude data from the last deglaciation and thus obtain more representative constraints for the last pre-industrial interglacial and glacial end-member climate states. Based on Paleo±Dust, the global LGM:pi-HOL ratio of <10-μm dust deposition rate is 3.1 ± 0.8 (1σ). We expect Paleo±Dust to be of use for future paleoclimate dust studies and simulations using Earth system models of high to intermediate complexity.
Fil: Cosentino, Nicolas Juan. Pontificia Universidad Católica de Chile; Chile. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Centro de Investigaciones del Mar y la Atmósfera. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Centro de Investigaciones del Mar y la Atmósfera; Argentina. Università degli Studi di Milano; Italia. Instituto Franco-Argentino sobre Estudios del Clima y sus Impactos; Argentina
Fil: Torre, Gabriela. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Córdoba. Centro de Investigaciones en Ciencias de la Tierra. Universidad Nacional de Córdoba. Facultad de Ciencias Exactas Físicas y Naturales. Centro de Investigaciones en Ciencias de la Tierra; Argentina
Fil: Lambert, Fabrice. Pontificia Universidad Católica de Chile; Chile
Fil: Albani, Samuel. Università degli Studi di Milano; Italia
Fil: de Vleeschouwer, Francois. Instituto Franco-argentino Sobre Estudios del Clima y Sus Impactos.; Argentina
Fil: Bory, Aloys J.-M.. Laboratoire d'Océanologie et de Géosciences; Francia - Materia
-
DUST
DEPOSITION
ARCHIVES - Nivel de accesibilidad
- acceso abierto
- Condiciones de uso
- https://creativecommons.org/licenses/by/2.5/ar/
- Repositorio
- Institución
- Consejo Nacional de Investigaciones Científicas y Técnicas
- OAI Identificador
- oai:ri.conicet.gov.ar:11336/256845
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Paleo±Dust: Quantifying uncertainty in paleo-dust deposition across archive typesCosentino, Nicolas JuanTorre, GabrielaLambert, FabriceAlbani, Samuelde Vleeschouwer, FrancoisBory, Aloys J.-M.DUSTDEPOSITIONARCHIVEShttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1Mineral dust aerosol concentrations in the atmosphere varied greatly on glacial-interglacial timescales. The greatest changes in global dust activity occurred in response to changes in orbital parameters that affect dust emission intensity through glacial activity, and dust lifetime in the atmosphere through changes in the global hydrological cycle.Long-term changes in surface dust deposition rate are registered in geological archives such as loess, peats, lakes, marine sediments, and ice. Data provided by these archives is crucial for guiding simulations of dust, and for better understanding the natural global dust cycle. However, the methods employed to derive paleo-dust deposition rates differ markedly between archives and are subject to different sources of uncertainty. Here, we present Paleo±Dust, an updated compilation of bulk and <10-μm paleo-dust deposition rate with quantitative 1-σ uncertainties that are inter-comparable among archive types.Paleo±Dust incorporates a total of 284 pre-industrial Holocene (pi-HOL) and 208 Last Glacial Maximum (LGM) dust flux constraints from studies published until December 2022, including for the first time peat records. We also recalculate previously published dust fluxes to exclude data from the last deglaciation and thus obtain more representative constraints for the last pre-industrial interglacial and glacial end-member climate states. Based on Paleo±Dust, the global LGM:pi-HOL ratio of <10-μm dust deposition rate is 3.1 ± 0.8 (1σ). We expect Paleo±Dust to be of use for future paleoclimate dust studies and simulations using Earth system models of high to intermediate complexity.Fil: Cosentino, Nicolas Juan. Pontificia Universidad Católica de Chile; Chile. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Centro de Investigaciones del Mar y la Atmósfera. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Centro de Investigaciones del Mar y la Atmósfera; Argentina. Università degli Studi di Milano; Italia. Instituto Franco-Argentino sobre Estudios del Clima y sus Impactos; ArgentinaFil: Torre, Gabriela. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Córdoba. Centro de Investigaciones en Ciencias de la Tierra. Universidad Nacional de Córdoba. Facultad de Ciencias Exactas Físicas y Naturales. Centro de Investigaciones en Ciencias de la Tierra; ArgentinaFil: Lambert, Fabrice. Pontificia Universidad Católica de Chile; ChileFil: Albani, Samuel. Università degli Studi di Milano; ItaliaFil: de Vleeschouwer, Francois. Instituto Franco-argentino Sobre Estudios del Clima y Sus Impactos.; ArgentinaFil: Bory, Aloys J.-M.. Laboratoire d'Océanologie et de Géosciences; FranciaCopernicus Publications2024-02info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/256845Cosentino, Nicolas Juan; Torre, Gabriela; Lambert, Fabrice; Albani, Samuel; de Vleeschouwer, Francois; et al.; Paleo±Dust: Quantifying uncertainty in paleo-dust deposition across archive types; Copernicus Publications; Earth System Science Data; 16; 2; 2-2024; 941-9591866-3516CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/url/https://essd.copernicus.org/articles/16/941/2024/essd-16-941-2024-discussion.htmlinfo:eu-repo/semantics/altIdentifier/doi/10.5194/essd-16-941-2024info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-10-15T15:35:02Zoai:ri.conicet.gov.ar:11336/256845instacron:CONICETInstitucionalhttp://ri.conicet.gov.ar/Organismo científico-tecnológicoNo correspondehttp://ri.conicet.gov.ar/oai/requestdasensio@conicet.gov.ar; lcarlino@conicet.gov.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:34982025-10-15 15:35:03.081CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse |
dc.title.none.fl_str_mv |
Paleo±Dust: Quantifying uncertainty in paleo-dust deposition across archive types |
title |
Paleo±Dust: Quantifying uncertainty in paleo-dust deposition across archive types |
spellingShingle |
Paleo±Dust: Quantifying uncertainty in paleo-dust deposition across archive types Cosentino, Nicolas Juan DUST DEPOSITION ARCHIVES |
title_short |
Paleo±Dust: Quantifying uncertainty in paleo-dust deposition across archive types |
title_full |
Paleo±Dust: Quantifying uncertainty in paleo-dust deposition across archive types |
title_fullStr |
Paleo±Dust: Quantifying uncertainty in paleo-dust deposition across archive types |
title_full_unstemmed |
Paleo±Dust: Quantifying uncertainty in paleo-dust deposition across archive types |
title_sort |
Paleo±Dust: Quantifying uncertainty in paleo-dust deposition across archive types |
dc.creator.none.fl_str_mv |
Cosentino, Nicolas Juan Torre, Gabriela Lambert, Fabrice Albani, Samuel de Vleeschouwer, Francois Bory, Aloys J.-M. |
author |
Cosentino, Nicolas Juan |
author_facet |
Cosentino, Nicolas Juan Torre, Gabriela Lambert, Fabrice Albani, Samuel de Vleeschouwer, Francois Bory, Aloys J.-M. |
author_role |
author |
author2 |
Torre, Gabriela Lambert, Fabrice Albani, Samuel de Vleeschouwer, Francois Bory, Aloys J.-M. |
author2_role |
author author author author author |
dc.subject.none.fl_str_mv |
DUST DEPOSITION ARCHIVES |
topic |
DUST DEPOSITION ARCHIVES |
purl_subject.fl_str_mv |
https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 |
dc.description.none.fl_txt_mv |
Mineral dust aerosol concentrations in the atmosphere varied greatly on glacial-interglacial timescales. The greatest changes in global dust activity occurred in response to changes in orbital parameters that affect dust emission intensity through glacial activity, and dust lifetime in the atmosphere through changes in the global hydrological cycle.Long-term changes in surface dust deposition rate are registered in geological archives such as loess, peats, lakes, marine sediments, and ice. Data provided by these archives is crucial for guiding simulations of dust, and for better understanding the natural global dust cycle. However, the methods employed to derive paleo-dust deposition rates differ markedly between archives and are subject to different sources of uncertainty. Here, we present Paleo±Dust, an updated compilation of bulk and <10-μm paleo-dust deposition rate with quantitative 1-σ uncertainties that are inter-comparable among archive types.Paleo±Dust incorporates a total of 284 pre-industrial Holocene (pi-HOL) and 208 Last Glacial Maximum (LGM) dust flux constraints from studies published until December 2022, including for the first time peat records. We also recalculate previously published dust fluxes to exclude data from the last deglaciation and thus obtain more representative constraints for the last pre-industrial interglacial and glacial end-member climate states. Based on Paleo±Dust, the global LGM:pi-HOL ratio of <10-μm dust deposition rate is 3.1 ± 0.8 (1σ). We expect Paleo±Dust to be of use for future paleoclimate dust studies and simulations using Earth system models of high to intermediate complexity. Fil: Cosentino, Nicolas Juan. Pontificia Universidad Católica de Chile; Chile. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Centro de Investigaciones del Mar y la Atmósfera. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Centro de Investigaciones del Mar y la Atmósfera; Argentina. Università degli Studi di Milano; Italia. Instituto Franco-Argentino sobre Estudios del Clima y sus Impactos; Argentina Fil: Torre, Gabriela. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Córdoba. Centro de Investigaciones en Ciencias de la Tierra. Universidad Nacional de Córdoba. Facultad de Ciencias Exactas Físicas y Naturales. Centro de Investigaciones en Ciencias de la Tierra; Argentina Fil: Lambert, Fabrice. Pontificia Universidad Católica de Chile; Chile Fil: Albani, Samuel. Università degli Studi di Milano; Italia Fil: de Vleeschouwer, Francois. Instituto Franco-argentino Sobre Estudios del Clima y Sus Impactos.; Argentina Fil: Bory, Aloys J.-M.. Laboratoire d'Océanologie et de Géosciences; Francia |
description |
Mineral dust aerosol concentrations in the atmosphere varied greatly on glacial-interglacial timescales. The greatest changes in global dust activity occurred in response to changes in orbital parameters that affect dust emission intensity through glacial activity, and dust lifetime in the atmosphere through changes in the global hydrological cycle.Long-term changes in surface dust deposition rate are registered in geological archives such as loess, peats, lakes, marine sediments, and ice. Data provided by these archives is crucial for guiding simulations of dust, and for better understanding the natural global dust cycle. However, the methods employed to derive paleo-dust deposition rates differ markedly between archives and are subject to different sources of uncertainty. Here, we present Paleo±Dust, an updated compilation of bulk and <10-μm paleo-dust deposition rate with quantitative 1-σ uncertainties that are inter-comparable among archive types.Paleo±Dust incorporates a total of 284 pre-industrial Holocene (pi-HOL) and 208 Last Glacial Maximum (LGM) dust flux constraints from studies published until December 2022, including for the first time peat records. We also recalculate previously published dust fluxes to exclude data from the last deglaciation and thus obtain more representative constraints for the last pre-industrial interglacial and glacial end-member climate states. Based on Paleo±Dust, the global LGM:pi-HOL ratio of <10-μm dust deposition rate is 3.1 ± 0.8 (1σ). We expect Paleo±Dust to be of use for future paleoclimate dust studies and simulations using Earth system models of high to intermediate complexity. |
publishDate |
2024 |
dc.date.none.fl_str_mv |
2024-02 |
dc.type.none.fl_str_mv |
info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion http://purl.org/coar/resource_type/c_6501 info:ar-repo/semantics/articulo |
format |
article |
status_str |
publishedVersion |
dc.identifier.none.fl_str_mv |
http://hdl.handle.net/11336/256845 Cosentino, Nicolas Juan; Torre, Gabriela; Lambert, Fabrice; Albani, Samuel; de Vleeschouwer, Francois; et al.; Paleo±Dust: Quantifying uncertainty in paleo-dust deposition across archive types; Copernicus Publications; Earth System Science Data; 16; 2; 2-2024; 941-959 1866-3516 CONICET Digital CONICET |
url |
http://hdl.handle.net/11336/256845 |
identifier_str_mv |
Cosentino, Nicolas Juan; Torre, Gabriela; Lambert, Fabrice; Albani, Samuel; de Vleeschouwer, Francois; et al.; Paleo±Dust: Quantifying uncertainty in paleo-dust deposition across archive types; Copernicus Publications; Earth System Science Data; 16; 2; 2-2024; 941-959 1866-3516 CONICET Digital CONICET |
dc.language.none.fl_str_mv |
eng |
language |
eng |
dc.relation.none.fl_str_mv |
info:eu-repo/semantics/altIdentifier/url/https://essd.copernicus.org/articles/16/941/2024/essd-16-941-2024-discussion.html info:eu-repo/semantics/altIdentifier/doi/10.5194/essd-16-941-2024 |
dc.rights.none.fl_str_mv |
info:eu-repo/semantics/openAccess https://creativecommons.org/licenses/by/2.5/ar/ |
eu_rights_str_mv |
openAccess |
rights_invalid_str_mv |
https://creativecommons.org/licenses/by/2.5/ar/ |
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application/pdf application/pdf application/pdf |
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Copernicus Publications |
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Copernicus Publications |
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CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicas |
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dasensio@conicet.gov.ar; lcarlino@conicet.gov.ar |
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13.22299 |