An assessment of the spatial extent of polar dust using satellite thermal data

Abstract The effect of mineral dust aerosols and subsequent deposition in polar regions has historically been underestimated in climate models. Dust aerosols increase melt rates by reducing surface albedo and modifying atmospheric radiative properties. In this study 127,413 satellite images covering...

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Autores principales: M. Bowen, R. F. Vincent
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Lenguaje:EN
Publicado: Nature Portfolio 2021
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Acceso en línea:https://doaj.org/article/e053d6592db0495a95cbe112ca61a750
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spelling oai:doaj.org-article:e053d6592db0495a95cbe112ca61a7502021-12-02T14:12:48ZAn assessment of the spatial extent of polar dust using satellite thermal data10.1038/s41598-020-79825-72045-2322https://doaj.org/article/e053d6592db0495a95cbe112ca61a7502021-01-01T00:00:00Zhttps://doi.org/10.1038/s41598-020-79825-7https://doaj.org/toc/2045-2322Abstract The effect of mineral dust aerosols and subsequent deposition in polar regions has historically been underestimated in climate models. Dust aerosols increase melt rates by reducing surface albedo and modifying atmospheric radiative properties. In this study 127,413 satellite images covering the Arctic and Antarctic from 2007 to 2019 were assessed for dust content using thermal infrared wavelengths. The results show a strong linear trend in which the relative spatial extent of dust (RSED) increased annually by 0.31% in the Arctic (8.5% to 12.1%) and 0.19% in the Antarctic (5.2% to 7.5%). Seasonally, the maximum aggregated average RSED occurred in the Arctic during boreal winter (11.2%), while the Antarctic peaked in austral spring (9.5%). Maximum RSED rates occurred in boreal winter/austral summer (Dec–Jan–Feb) for both polar regions. The data suggests that finer dust particles are more efficiently distributed by aeolian processes leading to higher RSED values that are not necessarily reflective of polar dust loading models.M. BowenR. F. VincentNature PortfolioarticleMedicineRScienceQENScientific Reports, Vol 11, Iss 1, Pp 1-9 (2021)
institution DOAJ
collection DOAJ
language EN
topic Medicine
R
Science
Q
spellingShingle Medicine
R
Science
Q
M. Bowen
R. F. Vincent
An assessment of the spatial extent of polar dust using satellite thermal data
description Abstract The effect of mineral dust aerosols and subsequent deposition in polar regions has historically been underestimated in climate models. Dust aerosols increase melt rates by reducing surface albedo and modifying atmospheric radiative properties. In this study 127,413 satellite images covering the Arctic and Antarctic from 2007 to 2019 were assessed for dust content using thermal infrared wavelengths. The results show a strong linear trend in which the relative spatial extent of dust (RSED) increased annually by 0.31% in the Arctic (8.5% to 12.1%) and 0.19% in the Antarctic (5.2% to 7.5%). Seasonally, the maximum aggregated average RSED occurred in the Arctic during boreal winter (11.2%), while the Antarctic peaked in austral spring (9.5%). Maximum RSED rates occurred in boreal winter/austral summer (Dec–Jan–Feb) for both polar regions. The data suggests that finer dust particles are more efficiently distributed by aeolian processes leading to higher RSED values that are not necessarily reflective of polar dust loading models.
format article
author M. Bowen
R. F. Vincent
author_facet M. Bowen
R. F. Vincent
author_sort M. Bowen
title An assessment of the spatial extent of polar dust using satellite thermal data
title_short An assessment of the spatial extent of polar dust using satellite thermal data
title_full An assessment of the spatial extent of polar dust using satellite thermal data
title_fullStr An assessment of the spatial extent of polar dust using satellite thermal data
title_full_unstemmed An assessment of the spatial extent of polar dust using satellite thermal data
title_sort assessment of the spatial extent of polar dust using satellite thermal data
publisher Nature Portfolio
publishDate 2021
url https://doaj.org/article/e053d6592db0495a95cbe112ca61a750
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