Black carbon snow sample analysis collected during the MOSAiC expedition

Black carbon (BC) is one of the predominating drivers concerning radiation budget modifications of snow surfaces as it can cause albedo decrease. Therefore, this leads to accelerated snow melting and thus to modifications of feedback mechanisms between components of the cryosphere and atmosphere. To...

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Main Authors: Jörss, A., Herber, A., Jurányi, Z.
Format: Conference Object
Language:English
Published: 2023
Subjects:
Online Access:https://gfzpublic.gfz-potsdam.de/pubman/item/item_5021982
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spelling ftgfzpotsdam:oai:gfzpublic.gfz-potsdam.de:item_5021982 2023-07-30T03:55:43+02:00 Black carbon snow sample analysis collected during the MOSAiC expedition Jörss, A. Herber, A. Jurányi, Z. 2023-07-11 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5021982 eng eng info:eu-repo/semantics/altIdentifier/doi/10.57757/IUGG23-4290 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5021982 XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG) info:eu-repo/semantics/conferenceObject 2023 ftgfzpotsdam https://doi.org/10.57757/IUGG23-4290 2023-07-16T23:40:30Z Black carbon (BC) is one of the predominating drivers concerning radiation budget modifications of snow surfaces as it can cause albedo decrease. Therefore, this leads to accelerated snow melting and thus to modifications of feedback mechanisms between components of the cryosphere and atmosphere. To investigate and quantify the detailed BC-induced processes in polar regions, snow samples collected during different campaigns in the Antarctic and the Arctic, especially during the MOSAiC expedition are analyzed in the chemical laboratory employing a Single Particle Soot Photometer (SP2) and the nebulizer Marin 5. Doing so, it was found that prevalent saline character of the snow collected on sea ice influences the results of SP2 analysis in a way that BC concentrations become significantly underestimated. We present here a method that was developed for quantification and correction of those effects since a significant number of the MOSAiC samples in particular include such sea salt impurities. Applying the methods to the whole MOSAiC data set will allow for the first time to quantify year-round human-caused pollution in the central Arctic and related changes of the surface energy budget. The samples from Antarctica will allow for a bipolar comparison of physical and chemical snow properties. Conference Object albedo Antarc* Antarctic Antarctica Arctic black carbon Sea ice GFZpublic (German Research Centre for Geosciences, Helmholtz-Zentrum Potsdam) Antarctic Arctic The Antarctic
institution Open Polar
collection GFZpublic (German Research Centre for Geosciences, Helmholtz-Zentrum Potsdam)
op_collection_id ftgfzpotsdam
language English
description Black carbon (BC) is one of the predominating drivers concerning radiation budget modifications of snow surfaces as it can cause albedo decrease. Therefore, this leads to accelerated snow melting and thus to modifications of feedback mechanisms between components of the cryosphere and atmosphere. To investigate and quantify the detailed BC-induced processes in polar regions, snow samples collected during different campaigns in the Antarctic and the Arctic, especially during the MOSAiC expedition are analyzed in the chemical laboratory employing a Single Particle Soot Photometer (SP2) and the nebulizer Marin 5. Doing so, it was found that prevalent saline character of the snow collected on sea ice influences the results of SP2 analysis in a way that BC concentrations become significantly underestimated. We present here a method that was developed for quantification and correction of those effects since a significant number of the MOSAiC samples in particular include such sea salt impurities. Applying the methods to the whole MOSAiC data set will allow for the first time to quantify year-round human-caused pollution in the central Arctic and related changes of the surface energy budget. The samples from Antarctica will allow for a bipolar comparison of physical and chemical snow properties.
format Conference Object
author Jörss, A.
Herber, A.
Jurányi, Z.
spellingShingle Jörss, A.
Herber, A.
Jurányi, Z.
Black carbon snow sample analysis collected during the MOSAiC expedition
author_facet Jörss, A.
Herber, A.
Jurányi, Z.
author_sort Jörss, A.
title Black carbon snow sample analysis collected during the MOSAiC expedition
title_short Black carbon snow sample analysis collected during the MOSAiC expedition
title_full Black carbon snow sample analysis collected during the MOSAiC expedition
title_fullStr Black carbon snow sample analysis collected during the MOSAiC expedition
title_full_unstemmed Black carbon snow sample analysis collected during the MOSAiC expedition
title_sort black carbon snow sample analysis collected during the mosaic expedition
publishDate 2023
url https://gfzpublic.gfz-potsdam.de/pubman/item/item_5021982
geographic Antarctic
Arctic
The Antarctic
geographic_facet Antarctic
Arctic
The Antarctic
genre albedo
Antarc*
Antarctic
Antarctica
Arctic
black carbon
Sea ice
genre_facet albedo
Antarc*
Antarctic
Antarctica
Arctic
black carbon
Sea ice
op_source XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG)
op_relation info:eu-repo/semantics/altIdentifier/doi/10.57757/IUGG23-4290
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5021982
op_doi https://doi.org/10.57757/IUGG23-4290
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