Articles | Volume 15, issue 19
https://doi.org/10.5194/acp-15-11399-2015
© Author(s) 2015. 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-15-11399-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Natural new particle formation at the coastal Antarctic site Neumayer
Alfred Wegener Institute for Polar and Marine Research, Am Handelshafen 12, 27570 Bremerhaven, Germany
K. Schmidt
Alfred Wegener Institute for Polar and Marine Research, Am Handelshafen 12, 27570 Bremerhaven, Germany
K. Teinilä
Finnish Meteorological Institute, Erik Palménin aukio 1, 00101 Helsinki, Finland
R. Hillamo
Finnish Meteorological Institute, Erik Palménin aukio 1, 00101 Helsinki, Finland
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38 citations as recorded by crossref.
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- Ion-induced sulfuric acid–ammonia nucleation drives particle formation in coastal Antarctica T. Jokinen et al. 10.1126/sciadv.aat9744
- Atmospheric new particle formation characteristics in the Arctic as measured at Mount Zeppelin, Svalbard, from 2016 to 2018 H. Lee et al. 10.5194/acp-20-13425-2020
- Particle number size distribution and new particle formation under the influence of biomass burning at a high altitude background site at Mt. Yulong (3410 m), China D. Shang et al. 10.5194/acp-18-15687-2018
- One year of aerosol refractive index measurement from a coastal Antarctic site Z. Jurányi & R. Weller 10.5194/acp-19-14417-2019
- CCN measurements at the Princess Elisabeth Antarctica research station during three austral summers P. Herenz et al. 10.5194/acp-19-275-2019
- Atmospheric new particle formation and growth: review of field observations V. Kerminen et al. 10.1088/1748-9326/aadf3c
- Effect of Prudhoe Bay emissions on atmospheric aerosol growth events observed in Utqiaġvik (Barrow), Alaska K. Kolesar et al. 10.1016/j.atmosenv.2016.12.019
- Low‐Volatility Vapors and New Particle Formation Over the Southern Ocean During the Antarctic Circumnavigation Expedition A. Baccarini et al. 10.1029/2021JD035126
- New particle formation events observed at King Sejong Station, Antarctic Peninsula – Part 1: Physical characteristics and contribution to cloud condensation nuclei J. Kim et al. 10.5194/acp-19-7583-2019
- Long-term measurement of sub-3 nm particles and their precursor gases in the boreal forest J. Sulo et al. 10.5194/acp-21-695-2021
- Estimation of sulfuric acid concentration using ambient ion composition and concentration data obtained with atmospheric pressure interface time-of-flight ion mass spectrometer L. Beck et al. 10.5194/amt-15-1957-2022
- Particle growth in an isoprene-rich forest: Influences of urban, wildfire, and biogenic air masses M. Gunsch et al. 10.1016/j.atmosenv.2018.01.058
- New particle formation and its effect on cloud condensation nuclei abundance in the summer Arctic: a case study in the Fram Strait and Barents Sea S. Kecorius et al. 10.5194/acp-19-14339-2019
- Year-round records of bulk aerosol composition over the Zhongshan Station, Coastal East Antarctica G. Xu et al. 10.1007/s11869-018-0642-9
- Open ocean and coastal new particle formation from sulfuric acid and amines around the Antarctic Peninsula J. Brean et al. 10.1038/s41561-021-00751-y
- Seasonal variations in physical characteristics of aerosol particles at the King Sejong Station, Antarctic Peninsula J. Kim et al. 10.5194/acp-17-12985-2017
- Primary sources control the variability of aerosol optical properties in the Antarctic Peninsula E. Asmi et al. 10.1080/16000889.2017.1414571
- Key challenges for tropospheric chemistry in the Southern Hemisphere C. Paton-Walsh et al. 10.1525/elementa.2021.00050
- Particle Number Size Distribution of Wintertime Alpine Aerosols and Their Activation as Cloud Condensation Nuclei in the Guanzhong Plain, Northwest China Y. Chen et al. 10.1029/2022JD037877
- New particle formation leads to enhanced cloud condensation nuclei concentrations on the Antarctic Peninsula J. Park et al. 10.5194/acp-23-13625-2023
- Characterization of aerosol number size distributions and their effect on cloud properties at Syowa Station, Antarctica K. Hara et al. 10.5194/acp-21-12155-2021
- The role of Antarctic overwintering teams and their significance for German polar research S. Franke et al. 10.5194/polf-90-65-2022
- Evidence for secondary ice production in Southern Ocean open cellular convection Y. Huang et al. 10.1002/qj.3041
- Investigation of new particle formation mechanisms and aerosol processes at Marambio Station, Antarctic Peninsula L. Quéléver et al. 10.5194/acp-22-8417-2022
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- Atmospheric nanoparticle growth D. Stolzenburg et al. 10.1103/RevModPhys.95.045002
- Applications and limitations of constrained high-resolution peak fitting on low resolving power mass spectra from the ToF-ACSM H. Timonen et al. 10.5194/amt-9-3263-2016
- Role of Iodine-Assisted Aerosol Particle Formation in Antarctica C. Xavier et al. 10.1021/acs.est.3c09103
- On the annual variability of Antarctic aerosol size distributions at Halley Research Station T. Lachlan-Cope et al. 10.5194/acp-20-4461-2020
- Dimethyl Sulfide‐Induced Increase in Cloud Condensation Nuclei in the Arctic Atmosphere K. Park et al. 10.1029/2021GB006969
- Comparison of new particle formation events in urban, agricultural, and arctic environments H. Lee et al. 10.1016/j.atmosenv.2024.120634
- New particle formation events observed at the King Sejong Station, Antarctic Peninsula – Part 2: Link with the oceanic biological activities E. Jang et al. 10.5194/acp-19-7595-2019
- Aerosol size distribution seasonal characteristics measured in Tiksi, Russian Arctic E. Asmi et al. 10.5194/acp-16-1271-2016
- 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
- Overview of the Antarctic Circumnavigation Expedition: Study of Preindustrial-like Aerosols and Their Climate Effects (ACE-SPACE) J. Schmale et al. 10.1175/BAMS-D-18-0187.1
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Short summary
We measured condensation particle (CP) concentrations and particle size distributions at the coastal Antarctic station Neumayer. Several nucleation events were observed, but particles did not grow up to sizes required for acting as cloud condensation nuclei. A simple estimation indicated that apart from sulfuric acid, the derived growth rates required other low volatile precursor vapours.
We measured condensation particle (CP) concentrations and particle size distributions at the...
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