Vertical distribution of aerosols in dust storms during the Arctic winter
International audience High Latitude Dust (HLD) contributes 5% to the global dust budget, but HLD measurements are sparse. Iceland has the largest area of volcaniclastic sandy desert on Earth where dust is originating from volcanic, but also glaciogenic sediments. Total Icelandic desert areas cover...
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HAL CCSD
2020
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Online Access: | https://insu.hal.science/insu-03560743 https://insu.hal.science/insu-03560743/document https://insu.hal.science/insu-03560743/file/EGU2020-20488-print.pdf https://doi.org/10.5194/egusphere-egu2020-20488 |
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English |
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[SDU]Sciences of the Universe [physics] |
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[SDU]Sciences of the Universe [physics] Dagsson Waldhauserova, Pavla Renard, Jean-Baptiste Olafsson, Haraldur Vignelles, Damien Berthet, Gwenaël Verdier, Nicolas Vertical distribution of aerosols in dust storms during the Arctic winter |
topic_facet |
[SDU]Sciences of the Universe [physics] |
description |
International audience High Latitude Dust (HLD) contributes 5% to the global dust budget, but HLD measurements are sparse. Iceland has the largest area of volcaniclastic sandy desert on Earth where dust is originating from volcanic, but also glaciogenic sediments. Total Icelandic desert areas cover 44,000 km2 which makes Iceland the largest Arctic as well as European desert. Icelandic volcanic dust can be transported distances > 1700 km towards the Arctic and deposited on snow, ice and sea ice. It is estimated that about 7% of Icelandic dust can reach the high Arctic (N>80°). It is known that about 50% of Icelandic dust storms occurred during winter or subzero temperatures in the southern part of Iceland. The vertical distributions of dust aerosol in high atmospheric profiles during these winter storms and long-range transport of dust during polar vortex condition were unknown.Dust observations from Iceland provide dust aerosol distributions during the Arctic winter for the first time, profiling dust storms as well as clean air conditions. Five winter dust storms were captured during harsh conditions. Mean number concentrations during the non-dust flights were < 5 particles cm-3 for the particles 0.2-100 µm in diameter and > 40 particles cm-3 during dust storms. A moderate dust storm with > 250 particles cm-3 (2 km altitude) was captured on 10th January 2016 as a result of sediments suspended from glacial outburst flood Skaftahlaup in 2015. Similar particle number concentrations were reported previously in the Saharan air layer. Detected particle sizes were up to 20 µm close to the surface, up to 10 µm at 900 m altitude, up to 5 µm at 5 km altitude, and submicron at altitudes > 6 km.Dust sources in the Arctic are active during the winter and produce large amounts of particulate matter dispersed over long distances and high altitudes. HLD contributes to Arctic air pollution and has the potential to influence ice nucleation in mixed-phase clouds and Arctic amplification. ... |
author2 |
Laboratoire de Physique et Chimie de l'Environnement et de l'Espace (LPC2E) Observatoire des Sciences de l'Univers en région Centre (OSUC) Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire de Paris Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université d'Orléans (UO)-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire de Paris Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université d'Orléans (UO)-Centre National de la Recherche Scientifique (CNRS)-Centre National d’Études Spatiales Paris (CNES) Centre National d'Études Spatiales Toulouse (CNES) |
format |
Conference Object |
author |
Dagsson Waldhauserova, Pavla Renard, Jean-Baptiste Olafsson, Haraldur Vignelles, Damien Berthet, Gwenaël Verdier, Nicolas |
author_facet |
Dagsson Waldhauserova, Pavla Renard, Jean-Baptiste Olafsson, Haraldur Vignelles, Damien Berthet, Gwenaël Verdier, Nicolas |
author_sort |
Dagsson Waldhauserova, Pavla |
title |
Vertical distribution of aerosols in dust storms during the Arctic winter |
title_short |
Vertical distribution of aerosols in dust storms during the Arctic winter |
title_full |
Vertical distribution of aerosols in dust storms during the Arctic winter |
title_fullStr |
Vertical distribution of aerosols in dust storms during the Arctic winter |
title_full_unstemmed |
Vertical distribution of aerosols in dust storms during the Arctic winter |
title_sort |
vertical distribution of aerosols in dust storms during the arctic winter |
publisher |
HAL CCSD |
publishDate |
2020 |
url |
https://insu.hal.science/insu-03560743 https://insu.hal.science/insu-03560743/document https://insu.hal.science/insu-03560743/file/EGU2020-20488-print.pdf https://doi.org/10.5194/egusphere-egu2020-20488 |
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Online, France |
geographic |
Arctic |
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Arctic |
genre |
Arctic Iceland Sea ice |
genre_facet |
Arctic Iceland Sea ice |
op_source |
22nd EGU General Assembly https://insu.hal.science/insu-03560743 22nd EGU General Assembly, 2020, Online, France. ⟨10.5194/egusphere-egu2020-20488⟩ |
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info:eu-repo/semantics/altIdentifier/doi/10.5194/egusphere-egu2020-20488 insu-03560743 https://insu.hal.science/insu-03560743 https://insu.hal.science/insu-03560743/document https://insu.hal.science/insu-03560743/file/EGU2020-20488-print.pdf BIBCODE: 2020EGUGA.2220488D doi:10.5194/egusphere-egu2020-20488 |
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http://creativecommons.org/licenses/by/ info:eu-repo/semantics/OpenAccess |
op_doi |
https://doi.org/10.5194/egusphere-egu2020-20488 |
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1788058374489767936 |
spelling |
ftccsdartic:oai:HAL:insu-03560743v1 2024-01-14T10:03:39+01:00 Vertical distribution of aerosols in dust storms during the Arctic winter Dagsson Waldhauserova, Pavla Renard, Jean-Baptiste Olafsson, Haraldur Vignelles, Damien Berthet, Gwenaël Verdier, Nicolas Laboratoire de Physique et Chimie de l'Environnement et de l'Espace (LPC2E) Observatoire des Sciences de l'Univers en région Centre (OSUC) Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire de Paris Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université d'Orléans (UO)-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire de Paris Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université d'Orléans (UO)-Centre National de la Recherche Scientifique (CNRS)-Centre National d’Études Spatiales Paris (CNES) Centre National d'Études Spatiales Toulouse (CNES) Online, France 2020 https://insu.hal.science/insu-03560743 https://insu.hal.science/insu-03560743/document https://insu.hal.science/insu-03560743/file/EGU2020-20488-print.pdf https://doi.org/10.5194/egusphere-egu2020-20488 en eng HAL CCSD info:eu-repo/semantics/altIdentifier/doi/10.5194/egusphere-egu2020-20488 insu-03560743 https://insu.hal.science/insu-03560743 https://insu.hal.science/insu-03560743/document https://insu.hal.science/insu-03560743/file/EGU2020-20488-print.pdf BIBCODE: 2020EGUGA.2220488D doi:10.5194/egusphere-egu2020-20488 http://creativecommons.org/licenses/by/ info:eu-repo/semantics/OpenAccess 22nd EGU General Assembly https://insu.hal.science/insu-03560743 22nd EGU General Assembly, 2020, Online, France. ⟨10.5194/egusphere-egu2020-20488⟩ [SDU]Sciences of the Universe [physics] info:eu-repo/semantics/conferenceObject Conference papers 2020 ftccsdartic https://doi.org/10.5194/egusphere-egu2020-20488 2023-12-17T00:24:14Z International audience High Latitude Dust (HLD) contributes 5% to the global dust budget, but HLD measurements are sparse. Iceland has the largest area of volcaniclastic sandy desert on Earth where dust is originating from volcanic, but also glaciogenic sediments. Total Icelandic desert areas cover 44,000 km2 which makes Iceland the largest Arctic as well as European desert. Icelandic volcanic dust can be transported distances > 1700 km towards the Arctic and deposited on snow, ice and sea ice. It is estimated that about 7% of Icelandic dust can reach the high Arctic (N>80°). It is known that about 50% of Icelandic dust storms occurred during winter or subzero temperatures in the southern part of Iceland. The vertical distributions of dust aerosol in high atmospheric profiles during these winter storms and long-range transport of dust during polar vortex condition were unknown.Dust observations from Iceland provide dust aerosol distributions during the Arctic winter for the first time, profiling dust storms as well as clean air conditions. Five winter dust storms were captured during harsh conditions. Mean number concentrations during the non-dust flights were < 5 particles cm-3 for the particles 0.2-100 µm in diameter and > 40 particles cm-3 during dust storms. A moderate dust storm with > 250 particles cm-3 (2 km altitude) was captured on 10th January 2016 as a result of sediments suspended from glacial outburst flood Skaftahlaup in 2015. Similar particle number concentrations were reported previously in the Saharan air layer. Detected particle sizes were up to 20 µm close to the surface, up to 10 µm at 900 m altitude, up to 5 µm at 5 km altitude, and submicron at altitudes > 6 km.Dust sources in the Arctic are active during the winter and produce large amounts of particulate matter dispersed over long distances and high altitudes. HLD contributes to Arctic air pollution and has the potential to influence ice nucleation in mixed-phase clouds and Arctic amplification. ... Conference Object Arctic Iceland Sea ice Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe) Arctic |