Paleodust Insights into Dust Impacts on Climate

Mineral dust acts both as a tracer and a forcing agent of climate change. Past dust variability, imprinted in paleodust records from natural archives, offers the unique opportunity to reconstruct the global dust cycle within a range of possibilities that plausibly encompass future variations in resp...

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Published in:Journal of Climate
Main Authors: Albani, Samuel, Mahowald, Natalie M.
Language:unknown
Published: 2023
Subjects:
Online Access:http://www.osti.gov/servlets/purl/1801718
https://www.osti.gov/biblio/1801718
https://doi.org/10.1175/jcli-d-18-0742.1
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spelling ftosti:oai:osti.gov:1801718 2023-07-30T04:01:30+02:00 Paleodust Insights into Dust Impacts on Climate Albani, Samuel Mahowald, Natalie M. 2023-07-04 application/pdf http://www.osti.gov/servlets/purl/1801718 https://www.osti.gov/biblio/1801718 https://doi.org/10.1175/jcli-d-18-0742.1 unknown http://www.osti.gov/servlets/purl/1801718 https://www.osti.gov/biblio/1801718 https://doi.org/10.1175/jcli-d-18-0742.1 doi:10.1175/jcli-d-18-0742.1 54 ENVIRONMENTAL SCIENCES 2023 ftosti https://doi.org/10.1175/jcli-d-18-0742.1 2023-07-11T10:04:45Z Mineral dust acts both as a tracer and a forcing agent of climate change. Past dust variability, imprinted in paleodust records from natural archives, offers the unique opportunity to reconstruct the global dust cycle within a range of possibilities that plausibly encompass future variations in response to climate change and land-cover and land-use changes. Dust itself has direct and indirect feedbacks on the climate system, through impacts on the atmosphere radiative budget and the carbon cycle. Starting from well-constrained reconstructions of the present and past dust cycle, we focus on quantifying dust direct impacts on the atmospheric radiation. We discuss the intrinsic effects of dust onto climate, and how changes in the global dust budget and surface conditions modulate the effective impacts on surface temperatures and precipitation. Most notably, the presence of dust tends to enhance the West African monsoon and warm the Arctic. We also highlight how different choices in terms of dust optical properties and size distributions may yield opposite results, and what are the observational constraints we can use to make an informed choice of model parameters. Finally, we discuss how dust variability might have influenced ongoing climate transitions in the past. In particular we found that a reduction in dust load, along with a reduced cryosphere cover, acted to offset Arctic warming during the deglaciation, potentially playing a role in shaping the Northern Hemisphere deglacial dynamics. Other/Unknown Material Arctic Climate change SciTec Connect (Office of Scientific and Technical Information - OSTI, U.S. Department of Energy) Arctic Journal of Climate 32 22 7897 7913
institution Open Polar
collection SciTec Connect (Office of Scientific and Technical Information - OSTI, U.S. Department of Energy)
op_collection_id ftosti
language unknown
topic 54 ENVIRONMENTAL SCIENCES
spellingShingle 54 ENVIRONMENTAL SCIENCES
Albani, Samuel
Mahowald, Natalie M.
Paleodust Insights into Dust Impacts on Climate
topic_facet 54 ENVIRONMENTAL SCIENCES
description Mineral dust acts both as a tracer and a forcing agent of climate change. Past dust variability, imprinted in paleodust records from natural archives, offers the unique opportunity to reconstruct the global dust cycle within a range of possibilities that plausibly encompass future variations in response to climate change and land-cover and land-use changes. Dust itself has direct and indirect feedbacks on the climate system, through impacts on the atmosphere radiative budget and the carbon cycle. Starting from well-constrained reconstructions of the present and past dust cycle, we focus on quantifying dust direct impacts on the atmospheric radiation. We discuss the intrinsic effects of dust onto climate, and how changes in the global dust budget and surface conditions modulate the effective impacts on surface temperatures and precipitation. Most notably, the presence of dust tends to enhance the West African monsoon and warm the Arctic. We also highlight how different choices in terms of dust optical properties and size distributions may yield opposite results, and what are the observational constraints we can use to make an informed choice of model parameters. Finally, we discuss how dust variability might have influenced ongoing climate transitions in the past. In particular we found that a reduction in dust load, along with a reduced cryosphere cover, acted to offset Arctic warming during the deglaciation, potentially playing a role in shaping the Northern Hemisphere deglacial dynamics.
author Albani, Samuel
Mahowald, Natalie M.
author_facet Albani, Samuel
Mahowald, Natalie M.
author_sort Albani, Samuel
title Paleodust Insights into Dust Impacts on Climate
title_short Paleodust Insights into Dust Impacts on Climate
title_full Paleodust Insights into Dust Impacts on Climate
title_fullStr Paleodust Insights into Dust Impacts on Climate
title_full_unstemmed Paleodust Insights into Dust Impacts on Climate
title_sort paleodust insights into dust impacts on climate
publishDate 2023
url http://www.osti.gov/servlets/purl/1801718
https://www.osti.gov/biblio/1801718
https://doi.org/10.1175/jcli-d-18-0742.1
geographic Arctic
geographic_facet Arctic
genre Arctic
Climate change
genre_facet Arctic
Climate change
op_relation http://www.osti.gov/servlets/purl/1801718
https://www.osti.gov/biblio/1801718
https://doi.org/10.1175/jcli-d-18-0742.1
doi:10.1175/jcli-d-18-0742.1
op_doi https://doi.org/10.1175/jcli-d-18-0742.1
container_title Journal of Climate
container_volume 32
container_issue 22
container_start_page 7897
op_container_end_page 7913
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