Ionic composition of Antarctic aerosol at Dome C (2009-2018) ...
Year-round records of the ionic composition of Antarctic aerosol were obtained at the inland Dome C (DC) and coastal Neumayer (NM) sites, with additional observations of black carbon at NM. Discussions focus on the origin of ammonium in Antarctica. This first Antarctic atmospheric study of several s...
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Online Access: | https://dx.doi.org/10.1594/pangaea.931365 https://doi.pangaea.de/10.1594/PANGAEA.931365 |
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ftdatacite:10.1594/pangaea.931365 2024-09-15T17:40:08+00:00 Ionic composition of Antarctic aerosol at Dome C (2009-2018) ... Weller, Rolf Legrand, Michel 2021 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.931365 https://doi.pangaea.de/10.1594/PANGAEA.931365 en eng PANGAEA https://dx.doi.org/10.1029/2021gl092826 Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 aerosol ammonium biomass burning black carbon HEIGHT above ground DATE/TIME Duration Oxalate Ammonium Sulfate, non-sea-salt Methane sulfonic acid Ratio Ratio, standard error Monitoring station Ion chromatography dataset Dataset 2021 ftdatacite https://doi.org/10.1594/pangaea.93136510.1029/2021gl092826 2024-08-01T10:51:01Z Year-round records of the ionic composition of Antarctic aerosol were obtained at the inland Dome C (DC) and coastal Neumayer (NM) sites, with additional observations of black carbon at NM. Discussions focus on the origin of ammonium in Antarctica. This first Antarctic atmospheric study of several species emitted by biomass burning indicates that black carbon, oxalate, and fine potassium reach a maximum in October in relation to biomass burning activity in the southern hemisphere. Ammonium reaches a maximum two months later, suggesting that biomass burning remains a minor ammonium source there. The ammonium maximum in December coincides with the occurrence of diatom blooms in the austral ocean, suggesting that oceanic ammonia emissions are the main source of ammonium in Antarctica. The ammonium to sulfur-derived biogenic species molar ratio of 0.15 in summer suggests far lower ammonia emissions from the polar ocean than mid-latitude southern oceans. ... Dataset Antarc* Antarctic Antarctica Austral Ocean DataCite |
institution |
Open Polar |
collection |
DataCite |
op_collection_id |
ftdatacite |
language |
English |
topic |
aerosol ammonium biomass burning black carbon HEIGHT above ground DATE/TIME Duration Oxalate Ammonium Sulfate, non-sea-salt Methane sulfonic acid Ratio Ratio, standard error Monitoring station Ion chromatography |
spellingShingle |
aerosol ammonium biomass burning black carbon HEIGHT above ground DATE/TIME Duration Oxalate Ammonium Sulfate, non-sea-salt Methane sulfonic acid Ratio Ratio, standard error Monitoring station Ion chromatography Weller, Rolf Legrand, Michel Ionic composition of Antarctic aerosol at Dome C (2009-2018) ... |
topic_facet |
aerosol ammonium biomass burning black carbon HEIGHT above ground DATE/TIME Duration Oxalate Ammonium Sulfate, non-sea-salt Methane sulfonic acid Ratio Ratio, standard error Monitoring station Ion chromatography |
description |
Year-round records of the ionic composition of Antarctic aerosol were obtained at the inland Dome C (DC) and coastal Neumayer (NM) sites, with additional observations of black carbon at NM. Discussions focus on the origin of ammonium in Antarctica. This first Antarctic atmospheric study of several species emitted by biomass burning indicates that black carbon, oxalate, and fine potassium reach a maximum in October in relation to biomass burning activity in the southern hemisphere. Ammonium reaches a maximum two months later, suggesting that biomass burning remains a minor ammonium source there. The ammonium maximum in December coincides with the occurrence of diatom blooms in the austral ocean, suggesting that oceanic ammonia emissions are the main source of ammonium in Antarctica. The ammonium to sulfur-derived biogenic species molar ratio of 0.15 in summer suggests far lower ammonia emissions from the polar ocean than mid-latitude southern oceans. ... |
format |
Dataset |
author |
Weller, Rolf Legrand, Michel |
author_facet |
Weller, Rolf Legrand, Michel |
author_sort |
Weller, Rolf |
title |
Ionic composition of Antarctic aerosol at Dome C (2009-2018) ... |
title_short |
Ionic composition of Antarctic aerosol at Dome C (2009-2018) ... |
title_full |
Ionic composition of Antarctic aerosol at Dome C (2009-2018) ... |
title_fullStr |
Ionic composition of Antarctic aerosol at Dome C (2009-2018) ... |
title_full_unstemmed |
Ionic composition of Antarctic aerosol at Dome C (2009-2018) ... |
title_sort |
ionic composition of antarctic aerosol at dome c (2009-2018) ... |
publisher |
PANGAEA |
publishDate |
2021 |
url |
https://dx.doi.org/10.1594/pangaea.931365 https://doi.pangaea.de/10.1594/PANGAEA.931365 |
genre |
Antarc* Antarctic Antarctica Austral Ocean |
genre_facet |
Antarc* Antarctic Antarctica Austral Ocean |
op_relation |
https://dx.doi.org/10.1029/2021gl092826 |
op_rights |
Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 |
op_doi |
https://doi.org/10.1594/pangaea.93136510.1029/2021gl092826 |
_version_ |
1810485091060678656 |