Articles | Volume 17, issue 22
https://doi.org/10.5194/acp-17-14055-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/acp-17-14055-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
24 Nov 2017
Research article |
| 24 Nov 2017
Year-round record of bulk and size-segregated aerosol composition in central Antarctica (Concordia site) – Part 2: Biogenic sulfur (sulfate and methanesulfonate) aerosol
Michel Legrand
CORRESPONDING AUTHOR
Université Grenoble Alpes, Institut des Géosciences de l'Environnement (IGE), Grenoble, 38402, France
CNRS, Institut des Géosciences de l'Environnement (IGE), Grenoble, 38402, France
Susanne Preunkert
Université Grenoble Alpes, Institut des Géosciences de l'Environnement (IGE), Grenoble, 38402, France
CNRS, Institut des Géosciences de l'Environnement (IGE), Grenoble, 38402, France
Rolf Weller
Alfred Wegener Institut für Polar und Meeresforschung,
Bremerhaven, 27570, Germany
Lars Zipf
Institut für Umweltphysik, University of Heidelberg, Heidelberg,
69120, Germany
Christoph Elsässer
Institut für Umweltphysik, University of Heidelberg, Heidelberg,
69120, Germany
Silke Merchel
Helmholtz-Zentrum Dresden-Rossendorf (HZDR), Dresden, 01328,
Germany
Georg Rugel
Helmholtz-Zentrum Dresden-Rossendorf (HZDR), Dresden, 01328,
Germany
Dietmar Wagenbach
Institut für Umweltphysik, University of Heidelberg, Heidelberg,
69120, Germany
deceased, December 2014
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- Low-cost production of a 7Be tracer from rainwater and purification: preliminary results R. Querfeld et al. 10.1007/s10967-017-5433-5
29 citations as recorded by crossref.
- Characterizing Atmospheric Transport Pathways to Antarctica and the Remote Southern Ocean Using Radon-222 S. Chambers et al. 10.3389/feart.2018.00190
- Homogeneous sulfur isotope signature in East Antarctica and implication for sulfur source shifts through the last glacial-interglacial cycle S. Ishino et al. 10.1038/s41598-019-48801-1
- Brief communication: Spatial and temporal variations in surface snow chemistry along a traverse from coastal East Antarctica to the ice sheet summit (Dome A) G. Shi et al. 10.5194/tc-15-1087-2021
- Simultaneous organic aerosol source apportionment at two Antarctic sites reveals large-scale and ecoregion-specific components M. Paglione et al. 10.5194/acp-24-6305-2024
- Ammonium in Antarctic Aerosol: Marine Biological Activity Versus Long‐Range Transport of Biomass Burning M. Legrand et al. 10.1029/2021GL092826
- Assessing the Seasonal Dynamics of Nitrate and Sulfate Aerosols at the South Pole Utilizing Stable Isotopes W. Walters et al. 10.1029/2019JD030517
- Seasonality of aerosol chemical composition at King Sejong Station (Antarctic Peninsula) in 2013 S. Hong et al. 10.1016/j.atmosenv.2019.117185
- The potential role of methanesulfonic acid (MSA) in aerosol formation and growth and the associated radiative forcings A. Hodshire et al. 10.5194/acp-19-3137-2019
- Persistent Draining of the Stratospheric 10Be Reservoir After the Samalas Volcanic Eruption (1257 CE) M. Baroni et al. 10.1029/2018JD029823
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- High summertime aerosol organic functional group concentrations from marine and seabird sources at Ross Island, Antarctica, during AWARE J. Liu et al. 10.5194/acp-18-8571-2018
- DMS oxidation and sulfur aerosol formation in the marine troposphere: a focus on reactive halogen and multiphase chemistry Q. Chen et al. 10.5194/acp-18-13617-2018
- Nitrate deposition and preservation in the snowpack along a traverse from coast to the ice sheet summit (Dome A) in East Antarctica G. Shi et al. 10.5194/tc-12-1177-2018
- Ion concentrations in ice wedges: An innovative approach to reconstruct past climate variability Y. Iizuka et al. 10.1016/j.epsl.2019.03.013
- Biogenic aerosol in central East Antarctic Plateau as a proxy for the ocean-atmosphere interaction in the Southern Ocean S. Becagli et al. 10.1016/j.scitotenv.2021.151285
- Heavy metal transport and evolution of atmospheric aerosols in the Antarctic region C. Marina-Montes et al. 10.1016/j.scitotenv.2020.137702
- Attempts to understand potential deficiencies in chemical procedures for AMS S. Merchel et al. 10.1016/j.nimb.2019.05.005
- Aerosol-Climate Interactions During the Last Glacial Maximum S. Albani et al. 10.1007/s40641-018-0100-7
- Year-round records of bulk aerosol composition over the Zhongshan Station, Coastal East Antarctica G. Xu et al. 10.1007/s11869-018-0642-9
- Regional Characteristics of Atmospheric Sulfate Formation in East Antarctica Imprinted on 17O‐Excess Signature S. Ishino et al. 10.1029/2020JD033583
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- Size distribution and ionic composition of marine summer aerosol at the continental Antarctic site Kohnen R. Weller et al. 10.5194/acp-18-2413-2018
- Contribution of Water-Soluble Organic Matter from Multiple Marine Geographic Eco-Regions to Aerosols around Antarctica M. Rinaldi et al. 10.1021/acs.est.0c00695
- Challenges associated with the climatic interpretation of water stable isotope records from a highly resolved firn core from Adélie Land, coastal Antarctica S. Goursaud et al. 10.5194/tc-13-1297-2019
- Simultaneous Detection of Alkylamines in the Surface Ocean and Atmosphere of the Antarctic Sympagic Environment M. Dall’Osto et al. 10.1021/acsearthspacechem.9b00028
- Sulfur aerosols in the Arctic, Antarctic, and Tibetan Plateau: Current knowledge and future perspectives Q. Pei et al. 10.1016/j.earscirev.2021.103753
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Latest update: 20 Nov 2024
Short summary
Levels of MSA and sulfate at inland Antarctica are documented from multiple year-round records of bulk and size-segregated aerosol samplings. A striking difference in the seasonality of sulfur aerosol composition, characterized by a MSA to nssSO4 ratio reaching a minimum in summer over the Antarctic plateau (0.05) and a maximum at the coast (up to 0.40), is clearly established. An efficient chemical destruction of MSA is suggested to take place over the Antarctic plateau in summer.
Levels of MSA and sulfate at inland Antarctica are documented from multiple year-round records...
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