Articles | Volume 18, issue 12
https://doi.org/10.5194/acp-18-8571-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/acp-18-8571-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
High summertime aerosol organic functional group concentrations from marine and seabird sources at Ross Island, Antarctica, during AWARE
Scripps Institution of Oceanography, University of California, San Diego,
9500 Gilman Drive, La Jolla, CA 92093, USA
Jeramy Dedrick
Scripps Institution of Oceanography, University of California, San Diego,
9500 Gilman Drive, La Jolla, CA 92093, USA
now at: Texas A&M University, 400 Bizzell St, College Station, TX 77843, USA
Scripps Institution of Oceanography, University of California, San Diego,
9500 Gilman Drive, La Jolla, CA 92093, USA
Gunnar I. Senum
Environmental & Climate Sciences Department, Brookhaven National
Laboratory, Building 815-E, Upton, NY 11973-5000, USA
Janek Uin
Environmental & Climate Sciences Department, Brookhaven National
Laboratory, Building 815-E, Upton, NY 11973-5000, USA
Chongai Kuang
Environmental & Climate Sciences Department, Brookhaven National
Laboratory, Building 815-E, Upton, NY 11973-5000, USA
Stephen R. Springston
Environmental & Climate Sciences Department, Brookhaven National
Laboratory, Building 815-E, Upton, NY 11973-5000, USA
W. Richard Leaitch
Environment and Climate Change Canada (ECCC), Toronto, ON, Canada
Allison C. Aiken
Earth and Environmental Science, Earth Systems Observations, Los Alamos
National Laboratory, Los Alamos, New Mexico, USA
Dan Lubin
Scripps Institution of Oceanography, University of California, San Diego,
9500 Gilman Drive, La Jolla, CA 92093, USA
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Cited
31 citations as recorded by crossref.
- Wind‐Driven and Seasonal Effects on Marine Aerosol Production in the Bellingshausen Sea, Antarctica S. Dasarathy et al. 10.1029/2022GL099723
- New particle formation leads to enhanced cloud condensation nuclei concentrations on the Antarctic Peninsula J. Park et al. 10.5194/acp-23-13625-2023
- 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
- Measurement report: Cloud processes and the transport of biological emissions affect southern ocean particle and cloud condensation nuclei concentrations K. Sanchez et al. 10.5194/acp-21-3427-2021
- Nonturbulent Liquid‐Bearing Polar Clouds: Observed Frequency of Occurrence and Simulated Sensitivity to Gravity Waves I. Silber et al. 10.1029/2020GL087099
- Automated identification of local contamination in remote atmospheric composition time series I. Beck et al. 10.5194/amt-15-4195-2022
- Comparison of Antarctic and Arctic Single‐Layer Stratiform Mixed‐Phase Cloud Properties Using Ground‐Based Remote Sensing Measurements D. Zhang et al. 10.1029/2019JD030673
- Impact of ice-free oases on particulate matter over the East Antarctic: Inferences from the carbonaceous, water-soluble species and trace metals S. Boreddy et al. 10.1016/j.polar.2020.100520
- Organic composition of three different size ranges of aerosol particles over the Southern Ocean G. Saliba et al. 10.1080/02786826.2020.1845296
- Nontargeted Tandem Mass Spectrometry Analysis Reveals Diversity and Variability in Aerosol Functional Groups across Multiple Sites, Seasons, and Times of Day J. Ditto et al. 10.1021/acs.estlett.9b00702
- Simultaneous Detection of Alkylamines in the Surface Ocean and Atmosphere of the Antarctic Sympagic Environment M. Dall’Osto et al. 10.1021/acsearthspacechem.9b00028
- An assessment of the spatial extent of polar dust using satellite thermal data M. Bowen & R. Vincent 10.1038/s41598-020-79825-7
- Multi‐Year Seasonal Trends in Sea Ice, Chlorophyll Concentration, and Marine Aerosol Optical Depth in the Bellingshausen Sea S. Dasarathy et al. 10.1029/2021JD034737
- Ocean flux of salt, sulfate, and organic components to atmospheric aerosol L. Russell et al. 10.1016/j.earscirev.2023.104364
- Ocean-atmosphere interactions: Different organic components across Pacific and Southern Oceans J. Jang et al. 10.1016/j.scitotenv.2023.162969
- Long-term variability in immersion-mode marine ice-nucleating particles from climate model simulations and observations A. Raman et al. 10.5194/acp-23-5735-2023
- On the annual variability of Antarctic aerosol size distributions at Halley Research Station T. Lachlan-Cope et al. 10.5194/acp-20-4461-2020
- Seasonal dynamics of airborne biomolecules influence the size distribution of Arctic aerosols E. Jang et al. 10.1016/j.ese.2024.100458
- Seasonal Differences and Variability of Concentrations, Chemical Composition, and Cloud Condensation Nuclei of Marine Aerosol Over the North Atlantic G. Saliba et al. 10.1029/2020JD033145
- Identifying a regional aerosol baseline in the eastern North Atlantic using collocated measurements and a mathematical algorithm to mask high-submicron-number-concentration aerosol events F. Gallo et al. 10.5194/acp-20-7553-2020
- 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
- Summertime High Abundances of Succinic, Citric, and Glyoxylic Acids in Antarctic Aerosols: Implications to Secondary Organic Aerosol Formation S. Boreddy et al. 10.1029/2021JD036172
- Evaluation of the CAM6 Climate Model Using Cloud Observations at McMurdo Station, Antarctica J. Yip et al. 10.1029/2021JD034653
- Small contributions of dust to PM2.5 and PM10 concentrations measured downwind of Oceano Dunes S. Lewis et al. 10.1016/j.atmosenv.2022.119515
- Persistent Supercooled Drizzle at Temperatures Below −25 °C Observed at McMurdo Station, Antarctica I. Silber et al. 10.1029/2019JD030882
- The hemispheric contrast in cloud microphysical properties constrains aerosol forcing I. McCoy et al. 10.1073/pnas.1922502117
- Characterization of the organic functional group composition and sources of summertime aerosols in an eastern city of China K. Xia et al. 10.1016/j.atmosenv.2022.119078
- Predicting Frigid Mixed‐Phase Clouds for Pristine Coastal Antarctica K. Hines et al. 10.1029/2021JD035112
- Highly supercooled riming and unusual triple-frequency radar signatures over McMurdo Station, Antarctica F. Tridon et al. 10.5194/acp-22-12467-2022
- Shipborne measurements of Antarctic submicron organic aerosols: an NMR perspective linking multiple sources and bioregions S. Decesari et al. 10.5194/acp-20-4193-2020
- Factors controlling marine aerosol size distributions and their climate effects over the northwest Atlantic Ocean region B. Croft et al. 10.5194/acp-21-1889-2021
31 citations as recorded by crossref.
- Wind‐Driven and Seasonal Effects on Marine Aerosol Production in the Bellingshausen Sea, Antarctica S. Dasarathy et al. 10.1029/2022GL099723
- New particle formation leads to enhanced cloud condensation nuclei concentrations on the Antarctic Peninsula J. Park et al. 10.5194/acp-23-13625-2023
- 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
- Measurement report: Cloud processes and the transport of biological emissions affect southern ocean particle and cloud condensation nuclei concentrations K. Sanchez et al. 10.5194/acp-21-3427-2021
- Nonturbulent Liquid‐Bearing Polar Clouds: Observed Frequency of Occurrence and Simulated Sensitivity to Gravity Waves I. Silber et al. 10.1029/2020GL087099
- Automated identification of local contamination in remote atmospheric composition time series I. Beck et al. 10.5194/amt-15-4195-2022
- Comparison of Antarctic and Arctic Single‐Layer Stratiform Mixed‐Phase Cloud Properties Using Ground‐Based Remote Sensing Measurements D. Zhang et al. 10.1029/2019JD030673
- Impact of ice-free oases on particulate matter over the East Antarctic: Inferences from the carbonaceous, water-soluble species and trace metals S. Boreddy et al. 10.1016/j.polar.2020.100520
- Organic composition of three different size ranges of aerosol particles over the Southern Ocean G. Saliba et al. 10.1080/02786826.2020.1845296
- Nontargeted Tandem Mass Spectrometry Analysis Reveals Diversity and Variability in Aerosol Functional Groups across Multiple Sites, Seasons, and Times of Day J. Ditto et al. 10.1021/acs.estlett.9b00702
- Simultaneous Detection of Alkylamines in the Surface Ocean and Atmosphere of the Antarctic Sympagic Environment M. Dall’Osto et al. 10.1021/acsearthspacechem.9b00028
- An assessment of the spatial extent of polar dust using satellite thermal data M. Bowen & R. Vincent 10.1038/s41598-020-79825-7
- Multi‐Year Seasonal Trends in Sea Ice, Chlorophyll Concentration, and Marine Aerosol Optical Depth in the Bellingshausen Sea S. Dasarathy et al. 10.1029/2021JD034737
- Ocean flux of salt, sulfate, and organic components to atmospheric aerosol L. Russell et al. 10.1016/j.earscirev.2023.104364
- Ocean-atmosphere interactions: Different organic components across Pacific and Southern Oceans J. Jang et al. 10.1016/j.scitotenv.2023.162969
- Long-term variability in immersion-mode marine ice-nucleating particles from climate model simulations and observations A. Raman et al. 10.5194/acp-23-5735-2023
- On the annual variability of Antarctic aerosol size distributions at Halley Research Station T. Lachlan-Cope et al. 10.5194/acp-20-4461-2020
- Seasonal dynamics of airborne biomolecules influence the size distribution of Arctic aerosols E. Jang et al. 10.1016/j.ese.2024.100458
- Seasonal Differences and Variability of Concentrations, Chemical Composition, and Cloud Condensation Nuclei of Marine Aerosol Over the North Atlantic G. Saliba et al. 10.1029/2020JD033145
- Identifying a regional aerosol baseline in the eastern North Atlantic using collocated measurements and a mathematical algorithm to mask high-submicron-number-concentration aerosol events F. Gallo et al. 10.5194/acp-20-7553-2020
- 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
- Summertime High Abundances of Succinic, Citric, and Glyoxylic Acids in Antarctic Aerosols: Implications to Secondary Organic Aerosol Formation S. Boreddy et al. 10.1029/2021JD036172
- Evaluation of the CAM6 Climate Model Using Cloud Observations at McMurdo Station, Antarctica J. Yip et al. 10.1029/2021JD034653
- Small contributions of dust to PM2.5 and PM10 concentrations measured downwind of Oceano Dunes S. Lewis et al. 10.1016/j.atmosenv.2022.119515
- Persistent Supercooled Drizzle at Temperatures Below −25 °C Observed at McMurdo Station, Antarctica I. Silber et al. 10.1029/2019JD030882
- The hemispheric contrast in cloud microphysical properties constrains aerosol forcing I. McCoy et al. 10.1073/pnas.1922502117
- Characterization of the organic functional group composition and sources of summertime aerosols in an eastern city of China K. Xia et al. 10.1016/j.atmosenv.2022.119078
- Predicting Frigid Mixed‐Phase Clouds for Pristine Coastal Antarctica K. Hines et al. 10.1029/2021JD035112
- Highly supercooled riming and unusual triple-frequency radar signatures over McMurdo Station, Antarctica F. Tridon et al. 10.5194/acp-22-12467-2022
- Shipborne measurements of Antarctic submicron organic aerosols: an NMR perspective linking multiple sources and bioregions S. Decesari et al. 10.5194/acp-20-4193-2020
- Factors controlling marine aerosol size distributions and their climate effects over the northwest Atlantic Ocean region B. Croft et al. 10.5194/acp-21-1889-2021
Discussed (final revised paper)
Latest update: 14 Dec 2024
Short summary
Observations of the organic components of the natural aerosol are scarce in Antarctica, which limits our understanding of natural aerosols and their connection to cloud albedo. We took yearlong measurements of organic aerosols at McMurdo Station. The natural organic aerosol was 150 times higher in summer than in winter. We showed the natural sources of OM were characterized by amide, which may be from seabird populations. Acid was high in summer and likely formed by secondary reactions.
Observations of the organic components of the natural aerosol are scarce in Antarctica, which...
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Final-revised paper
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