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1. Earth’s atmosphere protects the biosphere from nearby supernovae

Author: Christoudias, Theodoros, Kirkby, Jasper, Stolzenburg, Dominik, Pozzer, Andrea, Sommer, Eva, Brasseur, Guy P., Kulmala, Markku, and Lelieveld, Jos
Published: 2024
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2. Atmospheric new particle formation from the CERN CLOUD experiment

Author: Kirkby, Jasper, Amorim, António, Baltensperger, Urs, Carslaw, Kenneth S., Christoudias, Theodoros, Curtius, Joachim, Donahue, Neil M., Haddad, Imad El, Flagan, Richard C., Gordon, Hamish, Hansel, Armin, Harder, Hartwig, Junninen, Heikki, Kulmala, Markku, Kürten, Andreas, Laaksonen, Ari, Lehtipalo, Katrianne, Lelieveld, Jos, Möhler, Ottmar, Riipinen, Ilona, Stratmann, Frank, Tomé, Antonio, Virtanen, Annele, Volkamer, Rainer, Winkler, Paul M., and Worsnop, Douglas R.
Published: 2023
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3. The gas-phase formation mechanism of iodic acid as an atmospheric aerosol source

Author: Finkenzeller, Henning, Iyer, Siddharth, He, Xu-Cheng, Simon, Mario, Koenig, Theodore K., Lee, Christopher F., Valiev, Rashid, Hofbauer, Victoria, Amorim, Antonio, Baalbaki, Rima, Baccarini, Andrea, Beck, Lisa, Bell, David M., Caudillo, Lucía, Chen, Dexian, Chiu, Randall, Chu, Biwu, Dada, Lubna, Duplissy, Jonathan, Heinritzi, Martin, Kemppainen, Deniz, Kim, Changhyuk, Krechmer, Jordan, Kürten, Andreas, Kvashnin, Alexandr, Lamkaddam, Houssni, Lee, Chuan Ping, Lehtipalo, Katrianne, Li, Zijun, Makhmutov, Vladimir, Manninen, Hanna E., Marie, Guillaume, Marten, Ruby, Mauldin, Roy L., Mentler, Bernhard, Müller, Tatjana, Petäjä, Tuukka, Philippov, Maxim, Ranjithkumar, Ananth, Rörup, Birte, Shen, Jiali, Stolzenburg, Dominik, Tauber, Christian, Tham, Yee Jun, Tomé, António, Vazquez-Pufleau, Miguel, Wagner, Andrea C., Wang, Dongyu S., Wang, Mingyi, Wang, Yonghong, Weber, Stefan K., Nie, Wei, Wu, Yusheng, Xiao, Mao, Ye, Qing, Zauner-Wieczorek, Marcel, Hansel, Armin, Baltensperger, Urs, Brioude, Jérome, Curtius, Joachim, Donahue, Neil M., Haddad, Imad El, Flagan, Richard C., Kulmala, Markku, Kirkby, Jasper, Sipilä, Mikko, Worsnop, Douglas R., Kurten, Theo, Rissanen, Matti, and Volkamer, Rainer
Published: 2023
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4. Synergistic HNO3–H2SO4–NH3 upper tropospheric particle formation

Author: Wang, Mingyi, Xiao, Mao, Bertozzi, Barbara, Marie, Guillaume, Rörup, Birte, Schulze, Benjamin, Bardakov, Roman, He, Xu-Cheng, Shen, Jiali, Scholz, Wiebke, Marten, Ruby, Dada, Lubna, Baalbaki, Rima, Lopez, Brandon, Lamkaddam, Houssni, Manninen, Hanna E., Amorim, António, Ataei, Farnoush, Bogert, Pia, Brasseur, Zoé, Caudillo, Lucía, De Menezes, Louis-Philippe, Duplissy, Jonathan, Ekman, Annica M. L., Finkenzeller, Henning, Carracedo, Loïc Gonzalez, Granzin, Manuel, Guida, Roberto, Heinritzi, Martin, Hofbauer, Victoria, Höhler, Kristina, Korhonen, Kimmo, Krechmer, Jordan E., Kürten, Andreas, Lehtipalo, Katrianne, Mahfouz, Naser G. A., Makhmutov, Vladimir, Massabò, Dario, Mathot, Serge, Mauldin, Roy L., Mentler, Bernhard, Müller, Tatjana, Onnela, Antti, Petäjä, Tuukka, Philippov, Maxim, Piedehierro, Ana A., Pozzer, Andrea, Ranjithkumar, Ananth, Schervish, Meredith, Schobesberger, Siegfried, Simon, Mario, Stozhkov, Yuri, Tomé, António, Umo, Nsikanabasi Silas, Vogel, Franziska, Wagner, Robert, Wang, Dongyu S., Weber, Stefan K., Welti, André, Wu, Yusheng, Zauner-Wieczorek, Marcel, Sipilä, Mikko, Winkler, Paul M., Hansel, Armin, Baltensperger, Urs, Kulmala, Markku, Flagan, Richard C., Curtius, Joachim, Riipinen, Ilona, Gordon, Hamish, Lelieveld, Jos, El-Haddad, Imad, Volkamer, Rainer, Worsnop, Douglas R., Christoudias, Theodoros, Kirkby, Jasper, Möhler, Ottmar, and Donahue, Neil M.
Published: 2022
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5. Design and performance of the Cluster Ion Counter (CIC).

Author: Mirme, Sander, Balbaaki, Rima, Manninen, Hanna Elina, Koemets, Paap, Sommer, Eva, Rörup, Birte, Wu, Yusheng, Almeida, Joao, Ehrhart, Sebastian, Weber, Stefan Karl, Pfeifer, Joschka, Kangasluoma, Juha, Kulmala, Markku, and Kirkby, Jasper
Subjects: GALACTIC cosmic rays, COMPLEX ions, COUNTER-ions, AIR flow, PARTICLE beams, ATMOSPHERIC nucleation
Abstract: A dilute plasma is continuously maintained in the troposphere by ionising particle radiation from galactic cosmic rays and radon decay. Small ions in the 1–2 nm size range play an important role in atmospheric processes such as ion-induced nucleation of aerosol particles. Consequently there is a need for precise and robust instruments to measure small ions both for atmospheric observations and for laboratory experiments that simulate the atmosphere. Here we describe the design and performance of the Cluster Ion Counter (CIC, Airel OÜ), which simultaneously measures the number concentrations of positively- and negatively-charged ions and particles below 5 nm mobility diameter, with low noise and fast time response. The detection efficiency is above 80 % for ions and charged particles between 1.2 and 2.0 nm, and above 90 % between 2.0 and 3.0 nm. The ion concentrations measured by the CIC agree well with reference instruments. The noise level (1 σ of background measurements) is typically between 20 and 30 ions cm-3 at 1 Hz sampling rate and an air flow rate of 7 l min-1 per analyzer. The noise level improves when higher flow rates and longer sampling periods are used. The CIC responds rapidly with 1 s time resolution to pulses of ionisation produced in the CLOUD chamber by a CERN particle beam. [ABSTRACT FROM AUTHOR]
Published: 2024
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6. Ammonium CI-Orbitrap: a tool for characterizing the reactivity of oxygenated organic molecules.

Author: Li, Dandan, Wang, Dongyu, Caudillo, Lucia, Scholz, Wiebke, Wang, Mingyi, Tomaz, Sophie, Marie, Guillaume, Surdu, Mihnea, Eccli, Elias, Gong, Xianda, Gonzalez-Carracedo, Loic, Granzin, Manuel, Pfeifer, Joschka, Rörup, Birte, Schulze, Benjamin, Rantala, Pekka, Perrier, Sébastien, Hansel, Armin, Curtius, Joachim, and Kirkby, Jasper
Subjects: MASS spectrometry, TIME-of-flight mass spectrometers, MASS spectrometers, ATMOSPHERIC ionization, ATMOSPHERIC aerosols, CHEMICAL ionization mass spectrometry
Abstract: Oxygenated organic molecules (OOMs) play an important role in the formation of atmospheric aerosols. Due to various analytical challenges with respect to measuring organic vapors, uncertainties remain regarding the formation and fate of OOMs. The chemical ionization Orbitrap (CI-Orbitrap) mass spectrometer has recently been shown to be a powerful technique that is able to accurately identify gaseous organic compounds due to its greater mass resolution. Here, we present the ammonium-ion-based CI-Orbitrap (NH4+ -Orbitrap) as a technique capable of measuring a wide range of gaseous OOMs. The performance of the NH4+ -Orbitrap is compared with that of state-of-the-art mass spectrometers, including a nitrate-ion-based chemical ionization atmospheric pressure interface coupled to a time-of-flight mass spectrometer (NO3- -LTOF), a new generation of proton transfer reaction-TOF mass spectrometer (PTR3-TOF), and an iodide-based CI-TOF mass spectrometer equipped with a Filter Inlet for Gases and AEROsols (I- -CIMS). The instruments were deployed simultaneously in the Cosmic Leaving OUtdoors Droplets (CLOUD) chamber at the European Organization for Nuclear Research (CERN) during the CLOUD14 campaign in 2019. Products generated from α -pinene ozonolysis under various experimental conditions were simultaneously measured by the mass spectrometers. The NH4+ -Orbitrap was able to identify the widest range of OOMs (i.e., O ≥ 2), from less-oxidized species to highly oxygenated organic molecules (HOMs). Excellent agreement was found between the NH4+ -Orbitrap and the NO3- -LTOF with respect to characterizing HOMs and with the PTR3-TOF for the less-oxidized monomeric species. OOM concentrations measured by NH4+ -Orbitrap were estimated using calibration factors derived from the OOMs with high time-series correlations during the side-by-side measurements. As with the other mass spectrometry techniques used during this campaign, the detection sensitivity of the NH4+ -Orbitrap to OOMs is greatly affected by relative humidity, which may be related to changes in ionization efficiency and/or multiphase chemistry. Overall, this study shows that NH4+ -ion-based chemistry associated with the high mass resolution of the Orbitrap mass analyzer can measure almost all inclusive compounds. As a result, it is now possible to cover the entire range of compounds, which can lead to a better understanding of the oxidation processes. [ABSTRACT FROM AUTHOR]
Published: 2024
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7. Rapid growth of organic aerosol nanoparticles over a wide tropospheric temperature range

Author: Stolzenburg, Dominik, Fischer, Lukas, Vogel, Alexander L, Heinritzi, Martin, Schervish, Meredith, Simon, Mario, Wagner, Andrea C, Dada, Lubna, Ahonen, Lauri R, Amorim, Antonio, Baccarini, Andrea, Bauer, Paulus S, Baumgartner, Bernhard, Bergen, Anton, Bianchi, Federico, Breitenlechner, Martin, Brilke, Sophia, Mazon, Stephany Buenrostro, Chen, Dexian, Dias, António, Draper, Danielle C, Duplissy, Jonathan, Haddad, Imad El, Finkenzeller, Henning, Frege, Carla, Fuchs, Claudia, Garmash, Olga, Gordon, Hamish, He, Xucheng, Helm, Johanna, Hofbauer, Victoria, Hoyle, Christopher R, Kim, Changhyuk, Kirkby, Jasper, Kontkanen, Jenni, Kürten, Andreas, Lampilahti, Janne, Lawler, Michael, Lehtipalo, Katrianne, Leiminger, Markus, Mai, Huajun, Mathot, Serge, Mentler, Bernhard, Molteni, Ugo, Nie, Wei, Nieminen, Tuomo, Nowak, John B, Ojdanic, Andrea, Onnela, Antti, Passananti, Monica, Petäjä, Tuukka, Quéléver, Lauriane LJ, Rissanen, Matti P, Sarnela, Nina, Schallhart, Simon, Tauber, Christian, Tomé, António, Wagner, Robert, Wang, Mingyi, Weitz, Lena, Wimmer, Daniela, Xiao, Mao, Yan, Chao, Ye, Penglin, Zha, Qiaozhi, Baltensperger, Urs, Curtius, Joachim, Dommen, Josef, Flagan, Richard C, Kulmala, Markku, Smith, James N, Worsnop, Douglas R, Hansel, Armin, Donahue, Neil M, and Winkler, Paul M
Subjects: aerosols, nanoparticle growth, aerosol formation, CLOUD experiment, volatile organic compounds
Abstract: Nucleation and growth of aerosol particles from atmospheric vapors constitutes a major source of global cloud condensation nuclei (CCN). The fraction of newly formed particles that reaches CCN sizes is highly sensitive to particle growth rates, especially for particle sizes
Published: 2018

8. Potential pre-industrial–like new particle formation induced by pure biogenic organic vapors in Finnish peatland

Author: Huang, Wei, primary, Junninen, Heikki, additional, Garmash, Olga, additional, Lehtipalo, Katrianne, additional, Stolzenburg, Dominik, additional, Lampilahti, Janne L. P., additional, Ezhova, Ekaterina, additional, Schallhart, Simon, additional, Rantala, Pekka, additional, Aliaga, Diego, additional, Ahonen, Lauri, additional, Sulo, Juha, additional, Quéléver, Lauriane L. J., additional, Cai, Runlong, additional, Alekseychik, Pavel, additional, Mazon, Stephany B., additional, Yao, Lei, additional, Blichner, Sara M., additional, Zha, Qiaozhi, additional, Mammarella, Ivan, additional, Kirkby, Jasper, additional, Kerminen, Veli-Matti, additional, Worsnop, Douglas R., additional, Kulmala, Markku, additional, and Bianchi, Federico, additional
Published: 2024
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9. Potential pre-industrial–like new particle formation induced by pure biogenic organic vapors in Finnish peatland

Author: Huang, Wei, Junninen, Heikki, Garmash, Olga, Lehtipalo, Katrianne, Stolzenburg, Dominik, Lampilahti, Janne L. P., Ezhova, Ekaterina, Schallhart, Simon, Rantala, Pekka, Aliaga, Diego, Ahonen, Lauri, Sulo, Juha, Quéléver, Lauriane L. J., Cai, Runlong, Alekseychik, Pavel, Mazon, Stephany B., Yao, Lei, Blichner, Sara M., Zha, Qiaozhi, Mammarella, Ivan, Kirkby, Jasper, Kerminen, Veli-Matti, Worsnop, Douglas R., Kulmala, Markku, Bianchi, Federico, Huang, Wei, Junninen, Heikki, Garmash, Olga, Lehtipalo, Katrianne, Stolzenburg, Dominik, Lampilahti, Janne L. P., Ezhova, Ekaterina, Schallhart, Simon, Rantala, Pekka, Aliaga, Diego, Ahonen, Lauri, Sulo, Juha, Quéléver, Lauriane L. J., Cai, Runlong, Alekseychik, Pavel, Mazon, Stephany B., Yao, Lei, Blichner, Sara M., Zha, Qiaozhi, Mammarella, Ivan, Kirkby, Jasper, Kerminen, Veli-Matti, Worsnop, Douglas R., Kulmala, Markku, and Bianchi, Federico
Abstract: Pure biogenic new particle formation (NPF) induced by highly oxygenated organic molecules (HOMs) could be an important mechanism for pre-industrial aerosol formation. However, it has not been unambiguously confirmed in the ambient due to the scarcity of truly pristine continental locations in the present-day atmosphere or the lack of chemical characterization of NPF precursors. Here, we report ambient observations of pure biogenic HOM-driven NPF over a peatland in southern Finland. Meteorological decoupling processes formed an “air pocket” (i.e., a very shallow surface layer) at night and favored NPF initiated entirely by biogenic HOM from this peatland, whose atmospheric environment closely resembles that of the pre-industrial era. Our study sheds light on pre-industrial aerosol formation, which represents the baseline for estimating the impact of present and future aerosol on climate, as well as on future NPF, the features of which may revert toward pre-industrial–like conditions due to air pollution mitigation.
Published: 2024
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10. Neutral molecular cluster formation of sulfuric acid dimethylamine observed in real time under atmospheric conditions

Author: Kürten, Andreas, Jokinen, Tuija, Simon, Mario, Sipilä, Mikko, Sarnela, Nina, Junninen, Heikki, Adamov, Alexey, Almeida, João, Amorim, Antonio, Bianchi, Federico, Breitenlechner, Martin, Dommen, Josef, Donahue, Neil M., Duplissy, Jonathan, Ehrharta, Sebastian, Flagan, Richard C., Franchin, Alessandro, Hakala, Jani, Hansel, Armin, Heinritzia, Martin, Hutterli, Manuel, Kangasluoma, Juha, Kirkby, Jasper, Laaksonen, Ari, Lehtipalo, Katrianne, Leiminger, Markus, Makhmutov, Vladimir, Mathot, Serge, Onnela, Antti, Petäjä, Tuukka, Praplan, Arnaud P., Riccobono, Francesco, Rissanen, Matti P., Rondo, Linda, Schobesberger, Siegfried, Seinfeld, John H., Steiner, Gerhard, Tomé, António, Tröstl, Jasmin, Winkler, Paul M., Williamson, Christina, Wimmer, Daniela, Ye, Penglin, Baltensperger, Urs, Carslaw, Kenneth S., Kulmala, Markku, Worsnop, Douglas R., and Curtius, Joachim
Subjects: Physics - Atmospheric and Oceanic Physics, Physics - Chemical Physics
Abstract: For atmospheric sulfuric acid (SA) concentrations the presence of dimethylamine (DMA) at mixing ratios of several parts per trillion by volume can explain observed boundary layer new particle formation rates. However, the concentration and molecular composition of the neutral (uncharged) clusters have not been reported so far due to the lack of suitable instrumentation. Here we report on experiments from the Cosmics Leaving Outdoor Droplets chamber at the European Organization for Nuclear Research revealing the formation of neutral particles containing up to 14 SA and 16 DMA molecules, corresponding to a mobility diameter of about 2 nm, under atmospherically relevant conditions. These measurements bridge the gap between the molecular and particle perspectives of nucleation, revealing the fundamental processes involved in particle formation and growth. The neutral clusters are found to form at or close to the kinetic limit where particle formation is limited only by the collision rate of SA molecules. Even though the neutral particles are stable against evaporation from the SA dimer onward, the formation rates of particles at 1.7-nm size, which contain about 10 SA molecules, are up to 4 orders of magnitude smaller comparedwith those of the dimer due to coagulation and wall loss of particles before they reach 1.7 nm in diameter. This demonstrates that neither the atmospheric particle formation rate nor its dependence on SA can simply be interpreted in terms of cluster evaporation or the molecular composition of a critical nucleus., Comment: Main text plus SI
Published: 2015
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11. Nitrate Radicals Suppress Biogenic New Particle Formation from Monoterpene Oxidation

Author: Li, Dandan, primary, Huang, Wei, additional, Wang, Dongyu, additional, Wang, Mingyi, additional, Thornton, Joel A., additional, Caudillo, Lucía, additional, Rörup, Birte, additional, Marten, Ruby, additional, Scholz, Wiebke, additional, Finkenzeller, Henning, additional, Marie, Guillaume, additional, Baltensperger, Urs, additional, Bell, David M., additional, Brasseur, Zoé, additional, Curtius, Joachim, additional, Dada, Lubna, additional, Duplissy, Jonathan, additional, Gong, Xianda, additional, Hansel, Armin, additional, He, Xu-Cheng, additional, Hofbauer, Victoria, additional, Junninen, Heikki, additional, Krechmer, Jordan E., additional, Kürten, Andreas, additional, Lamkaddam, Houssni, additional, Lehtipalo, Katrianne, additional, Lopez, Brandon, additional, Ma, Yingge, additional, Mahfouz, Naser G. A., additional, Manninen, Hanna E., additional, Mentler, Bernhard, additional, Perrier, Sebastien, additional, Petäjä, Tuukka, additional, Pfeifer, Joschka, additional, Philippov, Maxim, additional, Schervish, Meredith, additional, Schobesberger, Siegfried, additional, Shen, Jiali, additional, Surdu, Mihnea, additional, Tomaz, Sophie, additional, Volkamer, Rainer, additional, Wang, Xinke, additional, Weber, Stefan K., additional, Welti, André, additional, Worsnop, Douglas R., additional, Wu, Yusheng, additional, Yan, Chao, additional, Zauner-Wieczorek, Marcel, additional, Kulmala, Markku, additional, Kirkby, Jasper, additional, Donahue, Neil M., additional, George, Christian, additional, El-Haddad, Imad, additional, Bianchi, Federico, additional, and Riva, Matthieu, additional
Published: 2024
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12. Assessing the importance of nitric acid and ammonia for particle growth in the polluted boundary layer

Author: Marten, Ruby, primary, Xiao, Mao, additional, Wang, Mingyi, additional, Kong, Weimeng, additional, He, Xu-Cheng, additional, Stolzenburg, Dominik, additional, Pfeifer, Joschka, additional, Marie, Guillaume, additional, Wang, Dongyu S., additional, Elser, Miriam, additional, Baccarini, Andrea, additional, Lee, Chuan Ping, additional, Amorim, Antonio, additional, Baalbaki, Rima, additional, Bell, David M., additional, Bertozzi, Barbara, additional, Caudillo, Lucía, additional, Dada, Lubna, additional, Duplissy, Jonathan, additional, Finkenzeller, Henning, additional, Heinritzi, Martin, additional, Lampimäki, Markus, additional, Lehtipalo, Katrianne, additional, Manninen, Hanna E., additional, Mentler, Bernhard, additional, Onnela, Antti, additional, Petäjä, Tuukka, additional, Philippov, Maxim, additional, Rörup, Birte, additional, Scholz, Wiebke, additional, Shen, Jiali, additional, Tham, Yee Jun, additional, Tomé, António, additional, Wagner, Andrea C., additional, Weber, Stefan K., additional, Zauner-Wieczorek, Marcel, additional, Curtius, Joachim, additional, Kulmala, Markku, additional, Volkamer, Rainer, additional, Worsnop, Douglas R., additional, Dommen, Josef, additional, Flagan, Richard C., additional, Kirkby, Jasper, additional, McPherson Donahue, Neil, additional, Lamkaddam, Houssni, additional, Baltensperger, Urs, additional, and El Haddad, Imad, additional
Published: 2024
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13. The role of low-volatility organic compounds in initial particle growth in the atmosphere

Author: Tröstl, Jasmin, Chuang, Wayne K, Gordon, Hamish, Heinritzi, Martin, Yan, Chao, Molteni, Ugo, Ahlm, Lars, Frege, Carla, Bianchi, Federico, Wagner, Robert, Simon, Mario, Lehtipalo, Katrianne, Williamson, Christina, Craven, Jill S, Duplissy, Jonathan, Adamov, Alexey, Almeida, Joao, Bernhammer, Anne-Kathrin, Breitenlechner, Martin, Brilke, Sophia, Dias, Antònio, Ehrhart, Sebastian, Flagan, Richard C, Franchin, Alessandro, Fuchs, Claudia, Guida, Roberto, Gysel, Martin, Hansel, Armin, Hoyle, Christopher R, Jokinen, Tuija, Junninen, Heikki, Kangasluoma, Juha, Keskinen, Helmi, Kim, Jaeseok, Krapf, Manuel, Kürten, Andreas, Laaksonen, Ari, Lawler, Michael, Leiminger, Markus, Mathot, Serge, Möhler, Ottmar, Nieminen, Tuomo, Onnela, Antti, Petäjä, Tuukka, Piel, Felix M, Miettinen, Pasi, Rissanen, Matti P, Rondo, Linda, Sarnela, Nina, Schobesberger, Siegfried, Sengupta, Kamalika, Sipilä, Mikko, Smith, James N, Steiner, Gerhard, Tomè, Antònio, Virtanen, Annele, Wagner, Andrea C, Weingartner, Ernest, Wimmer, Daniela, Winkler, Paul M, Ye, Penglin, Carslaw, Kenneth S, Curtius, Joachim, Dommen, Josef, Kirkby, Jasper, Kulmala, Markku, Riipinen, Ilona, Worsnop, Douglas R, Donahue, Neil M, and Baltensperger, Urs
Subjects: General Science & Technology
Abstract: About half of present-day cloud condensation nuclei originate from atmospheric nucleation, frequently appearing as a burst of new particles near midday. Atmospheric observations show that the growth rate of new particles often accelerates when the diameter of the particles is between one and ten nanometres. In this critical size range, new particles are most likely to be lost by coagulation with pre-existing particles, thereby failing to form new cloud condensation nuclei that are typically 50 to 100 nanometres across. Sulfuric acid vapour is often involved in nucleation but is too scarce to explain most subsequent growth, leaving organic vapours as the most plausible alternative, at least in the planetary boundary layer. Although recent studies predict that low-volatility organic vapours contribute during initial growth, direct evidence has been lacking. The accelerating growth may result from increased photolytic production of condensable organic species in the afternoon, and the presence of a possible Kelvin (curvature) effect, which inhibits organic vapour condensation on the smallest particles (the nano-Köhler theory), has so far remained ambiguous. Here we present experiments performed in a large chamber under atmospheric conditions that investigate the role of organic vapours in the initial growth of nucleated organic particles in the absence of inorganic acids and bases such as sulfuric acid or ammonia and amines, respectively. Using data from the same set of experiments, it has been shown that organic vapours alone can drive nucleation. We focus on the growth of nucleated particles and find that the organic vapours that drive initial growth have extremely low volatilities (saturation concentration less than 10(-4.5) micrograms per cubic metre). As the particles increase in size and the Kelvin barrier falls, subsequent growth is primarily due to more abundant organic vapours of slightly higher volatility (saturation concentrations of 10(-4.5) to 10(-0.5) micrograms per cubic metre). We present a particle growth model that quantitatively reproduces our measurements. Furthermore, we implement a parameterization of the first steps of growth in a global aerosol model and find that concentrations of atmospheric cloud concentration nuclei can change substantially in response, that is, by up to 50 per cent in comparison with previously assumed growth rate parameterizations.
Published: 2016

14. The effect of acid-base clustering and ions on the growth of atmospheric nano-particles.

Author: Lehtipalo, Katrianne, Rondo, Linda, Kontkanen, Jenni, Schobesberger, Siegfried, Jokinen, Tuija, Sarnela, Nina, Kürten, Andreas, Ehrhart, Sebastian, Franchin, Alessandro, Nieminen, Tuomo, Riccobono, Francesco, Sipilä, Mikko, Yli-Juuti, Taina, Duplissy, Jonathan, Adamov, Alexey, Ahlm, Lars, Almeida, João, Amorim, Antonio, Bianchi, Federico, Breitenlechner, Martin, Dommen, Josef, Downard, Andrew J, Dunne, Eimear M, Flagan, Richard C, Guida, Roberto, Hakala, Jani, Hansel, Armin, Jud, Werner, Kangasluoma, Juha, Kerminen, Veli-Matti, Keskinen, Helmi, Kim, Jaeseok, Kirkby, Jasper, Kupc, Agnieszka, Kupiainen-Määttä, Oona, Laaksonen, Ari, Lawler, Michael J, Leiminger, Markus, Mathot, Serge, Olenius, Tinja, Ortega, Ismael K, Onnela, Antti, Petäjä, Tuukka, Praplan, Arnaud, Rissanen, Matti P, Ruuskanen, Taina, Santos, Filipe D, Schallhart, Simon, Schnitzhofer, Ralf, Simon, Mario, Smith, James N, Tröstl, Jasmin, Tsagkogeorgas, Georgios, Tomé, António, Vaattovaara, Petri, Vehkamäki, Hanna, Vrtala, Aron E, Wagner, Paul E, Williamson, Christina, Wimmer, Daniela, Winkler, Paul M, Virtanen, Annele, Donahue, Neil M, Carslaw, Kenneth S, Baltensperger, Urs, Riipinen, Ilona, Curtius, Joachim, Worsnop, Douglas R, and Kulmala, Markku
Abstract: The growth of freshly formed aerosol particles can be the bottleneck in their survival to cloud condensation nuclei. It is therefore crucial to understand how particles grow in the atmosphere. Insufficient experimental data has impeded a profound understanding of nano-particle growth under atmospheric conditions. Here we study nano-particle growth in the CLOUD (Cosmics Leaving OUtdoors Droplets) chamber, starting from the formation of molecular clusters. We present measured growth rates at sub-3 nm sizes with different atmospherically relevant concentrations of sulphuric acid, water, ammonia and dimethylamine. We find that atmospheric ions and small acid-base clusters, which are not generally accounted for in the measurement of sulphuric acid vapour, can participate in the growth process, leading to enhanced growth rates. The availability of compounds capable of stabilizing sulphuric acid clusters governs the magnitude of these effects and thus the exact growth mechanism. We bring these observations into a coherent framework and discuss their significance in the atmosphere.
Published: 2016

15. Rapid growth of new atmospheric particles by nitric acid and ammonia condensation

Author: Wang, Mingyi, Kong, Weimeng, Marten, Ruby, He, Xu-Cheng, Chen, Dexian, Pfeifer, Joschka, Heitto, Arto, Kontkanen, Jenni, Dada, Lubna, Kürten, Andreas, Yli-Juuti, Taina, Manninen, Hanna E., Amanatidis, Stavros, Amorim, António, Baalbaki, Rima, Baccarini, Andrea, Bell, David M., Bertozzi, Barbara, Bräkling, Steffen, Brilke, Sophia, Murillo, Lucía Caudillo, Chiu, Randall, Chu, Biwu, De Menezes, Louis-Philippe, Duplissy, Jonathan, Finkenzeller, Henning, Carracedo, Loic Gonzalez, Granzin, Manuel, Guida, Roberto, Hansel, Armin, Hofbauer, Victoria, Krechmer, Jordan, Lehtipalo, Katrianne, Lamkaddam, Houssni, Lampimäki, Markus, Lee, Chuan Ping, Makhmutov, Vladimir, Marie, Guillaume, Mathot, Serge, Mauldin, Roy L., Mentler, Bernhard, Müller, Tatjana, Onnela, Antti, Partoll, Eva, Petäjä, Tuukka, Philippov, Maxim, Pospisilova, Veronika, Ranjithkumar, Ananth, Rissanen, Matti, Rörup, Birte, Scholz, Wiebke, Shen, Jiali, Simon, Mario, Sipilä, Mikko, Steiner, Gerhard, Stolzenburg, Dominik, Tham, Yee Jun, Tomé, António, Wagner, Andrea C., Wang, Dongyu S., Wang, Yonghong, Weber, Stefan K., Winkler, Paul M., Wlasits, Peter J., Wu, Yusheng, Xiao, Mao, Ye, Qing, Zauner-Wieczorek, Marcel, Zhou, Xueqin, Volkamer, Rainer, Riipinen, Ilona, Dommen, Josef, Curtius, Joachim, Baltensperger, Urs, Kulmala, Markku, Worsnop, Douglas R., Kirkby, Jasper, Seinfeld, John H., El-Haddad, Imad, Flagan, Richard C., and Donahue, Neil M.
Published: 2020
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16. Role of sesquiterpenes in biogenic new particle formation

Author: Dada, Lubna, primary, Stolzenburg, Dominik, additional, Simon, Mario, additional, Fischer, Lukas, additional, Heinritzi, Martin, additional, Wang, Mingyi, additional, Xiao, Mao, additional, Vogel, Alexander L., additional, Ahonen, Lauri, additional, Amorim, Antonio, additional, Baalbaki, Rima, additional, Baccarini, Andrea, additional, Baltensperger, Urs, additional, Bianchi, Federico, additional, Daellenbach, Kaspar R., additional, DeVivo, Jenna, additional, Dias, Antonio, additional, Dommen, Josef, additional, Duplissy, Jonathan, additional, Finkenzeller, Henning, additional, Hansel, Armin, additional, He, Xu-Cheng, additional, Hofbauer, Victoria, additional, Hoyle, Christopher R., additional, Kangasluoma, Juha, additional, Kim, Changhyuk, additional, Kürten, Andreas, additional, Kvashnin, Aleksander, additional, Mauldin, Roy, additional, Makhmutov, Vladimir, additional, Marten, Ruby, additional, Mentler, Bernhard, additional, Nie, Wei, additional, Petäjä, Tuukka, additional, Quéléver, Lauriane L. J., additional, Saathoff, Harald, additional, Tauber, Christian, additional, Tome, Antonio, additional, Molteni, Ugo, additional, Volkamer, Rainer, additional, Wagner, Robert, additional, Wagner, Andrea C., additional, Wimmer, Daniela, additional, Winkler, Paul M., additional, Yan, Chao, additional, Zha, Qiaozhi, additional, Rissanen, Matti, additional, Gordon, Hamish, additional, Curtius, Joachim, additional, Worsnop, Douglas R., additional, Lehtipalo, Katrianne, additional, Donahue, Neil M., additional, Kirkby, Jasper, additional, El Haddad, Imad, additional, and Kulmala, Markku, additional
Published: 2023
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17. Cosmic Rays and Climate

Author: Kirkby, Jasper
Subjects: Physics - Atmospheric and Oceanic Physics
Abstract: Among the most puzzling questions in climate change is that of solar-climate variability, which has attracted the attention of scientists for more than two centuries. Until recently, even the existence of solar-climate variability has been controversial - perhaps because the observations had largely involved temporary correlations between climate and the sunspot cycle. Over the last few years, however, diverse reconstructions of past climate change have revealed clear associations with cosmic ray variations recorded in cosmogenic isotope archives, providing persuasive evidence for solar or cosmic ray forcing of the climate. However, despite the increasing evidence of its importance, solar climate variability is likely to remain controversial until a physical mechanism is established. Although this remains a mystery, observations suggest that cloud cover may be influenced by cosmic rays, which are modulated by the solar wind and, on longer time scales, by the geomagnetic field and by the galactic environment of Earth. Two different classes of microphysical mechanisms have been proposed to connect cosmic rays with clouds: firstly, an influence of cosmic rays on the production of cloud condensation nuclei and, secondly, an influence of cosmic rays on the global electrical circuit in the atmosphere and, in turn, on ice nucleation and other cloud microphysical processes. Considerable progress on understanding ion-aerosol-cloud processes has been made in recent years, and the results are suggestive of a physically- plausible link between cosmic rays, clouds and climate. However, a concerted effort is now required to carry out definitive laboratory measurements of the fundamental physical and chemical processes involved, and to evaluate their climatic significance with dedicated field observations and modelling studies., Comment: 42 pages, 19 figures
Published: 2008
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18. Beam Measurements of a CLOUD (Cosmics Leaving OUtdoor Droplets) Chamber

Author: Kirkby, Jasper
Subjects: Physics - Atmospheric and Oceanic Physics, High Energy Physics - Experiment, Physics - Geophysics, Physics - Space Physics
Abstract: A striking correlation has recently been observed between global cloud cover and the flux of incident cosmic rays. The effect of natural variations in the cosmic ray flux is large, causing estimated changes in the Earth's energy radiation balance that are comparable to those attributed to greenhouse gases from the burning of fossil fuels since the Industrial Revolution. However a direct link between cosmic rays and cloud formation has not been unambiguously established. We therefore propose to experimentally measure cloud (water droplet) formation under controlled conditions in a test beam at CERN with a CLOUD chamber, duplicating the conditions prevailing in the troposphere. These data, which have never been previously obtained, will allow a detailed understanding of the possible effects of cosmic rays on clouds and confirm, or otherwise, a direct link between cosmic rays, global cloud cover and the Earth's climate. The measurements will, in turn, allow more reliable calculations to be made of the residual effect on global temperatures of the burning of fossil fuels, an issue of profound importance to society. Furthermore, light radio-isotope records indicate a correlation has existed between global climate and the cosmic ray flux extending back over the present inter-glacial and perhaps earlier. This suggests it may eventually become possible to make long-term (10-1,000 year) predictions of changes in the Earth's climate, provided a deeper understanding can be achieved of the ``geomagnetic climate'' of the Sun and Earth that modulates the cosmic-ray flux., Comment: More information and higher resolution drawings at http://cern.ch/Cloud Improved figure quality
Published: 2001

19. Ammonium CI-Orbitrap: a tool for characterizing the reactivity of oxygenated organic molecules

Author: Li, Dandan, primary, Wang, Dongyu, additional, Caudillo, Lucia, additional, Scholz, Wiebke, additional, Wang, Mingyi, additional, Tomaz, Sophie, additional, Marie, Guillaume, additional, Surdu, Mihnea, additional, Eccli, Elias, additional, Gong, Xianda, additional, Gonzalez-Carracedo, Loic, additional, Granzin, Manuel, additional, Pfeifer, Joschka, additional, Rörup, Birte, additional, Schulze, Benjamin, additional, Rantala, Pekka, additional, Perrier, Sébastien, additional, Hansel, Armin, additional, Curtius, Joachim, additional, Kirkby, Jasper, additional, Donahue, Neil M., additional, George, Christian, additional, El-Haddad, Imad, additional, and Riva, Matthieu, additional
Published: 2023
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20. Supplementary material to "Ammonium CI-Orbitrap: a tool for characterizing the reactivity of oxygenated organic molecules"

Author: Li, Dandan, primary, Wang, Dongyu, additional, Caudillo, Lucia, additional, Scholz, Wiebke, additional, Wang, Mingyi, additional, Tomaz, Sophie, additional, Marie, Guillaume, additional, Surdu, Mihnea, additional, Eccli, Elias, additional, Gong, Xianda, additional, Gonzalez-Carracedo, Loic, additional, Granzin, Manuel, additional, Pfeifer, Joschka, additional, Rörup, Birte, additional, Schulze, Benjamin, additional, Rantala, Pekka, additional, Perrier, Sébastien, additional, Hansel, Armin, additional, Curtius, Joachim, additional, Kirkby, Jasper, additional, Donahue, Neil M., additional, George, Christian, additional, El-Haddad, Imad, additional, and Riva, Matthieu, additional
Published: 2023
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21. An intercomparison study of four different techniques for measuring the chemical composition of nanoparticles

Author: Caudillo, Lucía, primary, Surdu, Mihnea, additional, Lopez, Brandon, additional, Wang, Mingyi, additional, Thoma, Markus, additional, Bräkling, Steffen, additional, Buchholz, Angela, additional, Simon, Mario, additional, Wagner, Andrea C., additional, Müller, Tatjana, additional, Granzin, Manuel, additional, Heinritzi, Martin, additional, Amorim, Antonio, additional, Bell, David M., additional, Brasseur, Zoé, additional, Dada, Lubna, additional, Duplissy, Jonathan, additional, Finkenzeller, Henning, additional, He, Xu-Cheng, additional, Lamkaddam, Houssni, additional, Mahfouz, Naser G. A., additional, Makhmutov, Vladimir, additional, Manninen, Hanna E., additional, Marie, Guillaume, additional, Marten, Ruby, additional, Mauldin, Roy L., additional, Mentler, Bernhard, additional, Onnela, Antti, additional, Petäjä, Tuukka, additional, Pfeifer, Joschka, additional, Philippov, Maxim, additional, Piedehierro, Ana A., additional, Rörup, Birte, additional, Scholz, Wiebke, additional, Shen, Jiali, additional, Stolzenburg, Dominik, additional, Tauber, Christian, additional, Tian, Ping, additional, Tomé, António, additional, Umo, Nsikanabasi Silas, additional, Wang, Dongyu S., additional, Wang, Yonghong, additional, Weber, Stefan K., additional, Welti, André, additional, Zauner-Wieczorek, Marcel, additional, Baltensperger, Urs, additional, Flagan, Richard C., additional, Hansel, Armin, additional, Kirkby, Jasper, additional, Kulmala, Markku, additional, Lehtipalo, Katrianne, additional, Worsnop, Douglas R., additional, Haddad, Imad El, additional, Donahue, Neil M., additional, Vogel, Alexander L., additional, Kürten, Andreas, additional, and Curtius, Joachim, additional
Published: 2023
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22. NO at low concentration can enhance the formation of highly oxygenated biogenic molecules in the atmosphere

Author: Nie, Wei, primary, Yan, Chao, additional, Yang, Liwen, additional, Roldin, Pontus, additional, Liu, Yuliang, additional, Vogel, Alexander L., additional, Molteni, Ugo, additional, Stolzenburg, Dominik, additional, Finkenzeller, Henning, additional, Amorim, Antonio, additional, Bianchi, Federico, additional, Curtius, Joachim, additional, Dada, Lubna, additional, Draper, Danielle C., additional, Duplissy, Jonathan, additional, Hansel, Armin, additional, He, Xu-Cheng, additional, Hofbauer, Victoria, additional, Jokinen, Tuija, additional, Kim, Changhyuk, additional, Lehtipalo, Katrianne, additional, Nichman, Leonid, additional, Mauldin, Roy L., additional, Makhmutov, Vladimir, additional, Mentler, Bernhard, additional, Mizelli-Ojdanic, Andrea, additional, Petäjä, Tuukka, additional, Quéléver, Lauriane L. J., additional, Schallhart, Simon, additional, Simon, Mario, additional, Tauber, Christian, additional, Tomé, António, additional, Volkamer, Rainer, additional, Wagner, Andrea C., additional, Wagner, Robert, additional, Wang, Mingyi, additional, Ye, Penglin, additional, Li, Haiyan, additional, Huang, Wei, additional, Qi, Ximeng, additional, Lou, Sijia, additional, Liu, Tengyu, additional, Chi, Xuguang, additional, Dommen, Josef, additional, Baltensperger, Urs, additional, El Haddad, Imad, additional, Kirkby, Jasper, additional, Worsnop, Douglas, additional, Kulmala, Markku, additional, Donahue, Neil M., additional, Ehn, Mikael, additional, and Ding, Aijun, additional
Published: 2023
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23. Global atmospheric particle formation from CERN CLOUD measurements

Author: Dunne, Eimear M., Gordon, Hamish, Kürten, Andreas, Almeida, João, Duplissy, Jonathan, Williamson, Christina, Ortega, Ismael K., Pringle, Kirsty J., Adamov, Alexey, Baltensperger, Urs, Barmet, Peter, Benduhn, Francois, Bianchi, Federico, Breitenlechner, Martin, Clarke, Antony, Curtius, Joachim, Dommen, Josef, Donahue, Neil M., Ehrhart, Sebastian, Flagan, Richard C., Franchin, Alessandro, Guida, Roberto, Hakala, Jani, Hansel, Armin, Heinritzi, Martin, Jokinen, Tuija, Kangasluoma, Juha, Kirkby, Jasper, Kulmala, Markku, Kupc, Agnieszka, Lawler, Michael J., Lehtipalo, Katrianne, Makhmutov, Vladimir, Mann, Graham, Mathot, Serge, Merikanto, Joonas, Miettinen, Pasi, Nenes, Athanasios, Onnela, Antti, Rap, Alexandra, Reddington, Carly L. S., Riccobono, Francesco, Richards, Nigel A. D., Rissanen, Matti P., Rondo, Linda, Sarnela, Nina, Schobesberger, Siegfried, Sengupta, Kamalika, Simon, Mario, Sipilä, Mikko, Smith, James N., Stozkhov, Yuri, Tomé, Antonio, Tröstl, Jasmin, Wagner, Paul E., Wimmer, Daniela, Winkler, Paul M., Worsnop, Douglas R., and Carslaw, Kenneth S.
Published: 2016

24. Measurement of the collision rate coefficients between atmospheric ions and multiply charged aerosol particles in the CERN CLOUD chamber

Author: Pfeifer, Joschka, Mahfouz, Naser G. A., Schulze, Benjamin C., Mathot, Serge, Stolzenburg, Dominik, Baalbaki, Rima, Brasseur, Zoé, Caudillo, Lucia, Dada, Lubna, Granzin, Manuel, He, Xu-Cheng, Lamkaddam, Houssni, Lopez, Brandon, Makhmutov, Vladimir, Marten, Ruby, Mentler, Bernhard, Müller, Tatjana, Onnela, Antti, Philippov, Maxim, Piedehierro, Ana A., Rörup, Birte, Schervish, Meredith, Tian, Ping, Umo, Nsikanabasi S., Wang, Dongyu S., Wang, Mingyi, Weber, Stefan K., Welti, André, Wu, Yusheng, Zauner-Wieczorek, Marcel, Amorim, Antonio, Haddad, Imad, Kulmala, Markku, Lehtipalo, Katrianne, Petäjä, Tuukka, Tomé, António, Mirme, Sander, Manninen, Hanna E., Donahue, Neil M., Flagan, Richard C., Kürten, Andreas, Curtius, Joachim, and Kirkby, Jasper
Abstract: Aerosol particles have an important role in Earth's radiation balance and climate, both directly and indirectly through aerosol–cloud interactions. Most aerosol particles in the atmosphere are weakly charged, affecting both their collision rates with ions and neutral molecules, as well as the rates by which they are scavenged by other aerosol particles and cloud droplets. The rate coefficients between ions and aerosol particles are important since they determine the growth rates and lifetimes of ions and charged aerosol particles, and so they may influence cloud microphysics, dynamics, and aerosol processing. However, despite their importance, very few experimental measurements exist of charged aerosol collision rates under atmospheric conditions, where galactic cosmic rays in the lower troposphere give rise to ion pair concentrations of around 1000 cm−3. Here we present measurements in the CERN CLOUD chamber of the rate coefficients between ions and small ( nm) aerosol particles containing up to 9 elementary charges, e. We find the rate coefficient of a singly charged ion with an oppositely charged particle increases from 2.0 (0.4–4.4) × 10−6 cm3 s−1 to 30.6 (24.9–45.1) × 10−6 cm3 s−1 for particles with charges of 1 to 9 e, respectively, where the parentheses indicate the ±1σ uncertainty interval. Our measurements are compatible with theoretical predictions and show excellent agreement with the model of Gatti and Kortshagen (2008).
Published: 2023

25. NO at low concentration can enhance the formation of highly oxygenated biogenic molecules in the atmosphere

Author: Nie, Wei, Yan, Chao, Yang, Liwen, Roldin, Pontus, Liu, Yuliang, Vogel, Alexander L, Molteni, Ugo, Stolzenburg, Dominik, Finkenzeller, Henning, Amorim, Antonio, Bianchi, Federico, Curtius, Joachim, Dada, Lubna, Draper, Danielle C, Duplissy, Jonathan, Hansel, Armin, He, Xu-Cheng, Hofbauer, Victoria, Jokinen, Tuija, Kim, Changhyuk, Lehtipalo, Katrianne, Nichman, Leonid, Mauldin, Roy L, Makhmutov, Vladimir, Mentler, Bernhard, Mizelli-Ojdanic, Andrea, Petäjä, Tuukka, Quéléver, Lauriane L J, Schallhart, Simon, Simon, Mario, Tauber, Christian, Tomé, António, Volkamer, Rainer, Wagner, Andrea C, Wagner, Robert, Wang, Mingyi, Ye, Penglin, Li, Haiyan, Huang, Wei, Qi, Ximeng, Lou, Sijia, Liu, Tengyu, Chi, Xuguang, Dommen, Josef, Baltensperger, Urs, Haddad, Imad El, Kirkby, Jasper, Worsnop, Douglas, Kulmala, Markku, Donahue, Neil M, Ehn, Mikael, and Ding, Aijun
Subjects: Physics in General
Abstract: The interaction between nitrogen monoxide (NO) and organic peroxy radicals (RO$_{2}$) greatly impacts the formation of highly oxygenated organic molecules (HOM), the key precursors of secondary organic aerosols. It has been thought that HOM production can be significantly suppressed by NO even at low concentrations. Here, we perform dedicated experiments focusing on HOM formation from monoterpenes at low NO concentrations (0 – 82 pptv). We demonstrate that such low NO can enhance HOM production by modulating the RO$_{2}$ loss and favoring the formation of alkoxy radicals that can continue to autoxidize through isomerization. These insights suggest that HOM yields from typical boreal forest emissions can vary between 2.5%-6.5%, and HOM formation will not be completely inhibited even at high NO concentrations. Our findings challenge the notion that NO monotonically reduces HOM yields by extending the knowledge of RO$_{2}$-NO interactions to the low-NO regime. This represents a major advance towards an accurate assessment of HOM budgets, especially in low-NO environments, which prevails in the pre-industrial atmosphere, pristine areas, and the upper boundary layer.
Published: 2023

26. Nitrate radicals suppress biogenic new particle formation from monoterpene oxidation

Author: Li, Dandan, primary, Huang, Wei, additional, Wang, Dongyu, additional, Wang, Mingyi, additional, Thornton, Joel, additional, Caudillo, Lucía, additional, Rörup, Birte, additional, Marten, Ruby, additional, Scholz, Wiebke, additional, Finkenzeller, Henning, additional, Marie, Guillaume, additional, Bell, David, additional, Brasseur, Zoé, additional, Curtius, Joachim, additional, Dada, Lubna, additional, Duplissy, Jonathan, additional, Gong, Xianda, additional, Hansel, Armin, additional, He, Xu-cheng, additional, Hofbauer, Victoria, additional, Junninen, Heikki, additional, Krechmer, Jordan E., additional, Kurten, Andreas, additional, Lamkaddam, Houssni, additional, LEHTIPALO, Katrianne, additional, Lopez, Brandon, additional, Ma, Yingge, additional, Mahfouz, Naser, additional, Manninen, Hanna E., additional, Mentler, Bernhard, additional, Perrier, Sebastien, additional, Petäjä, Tuukka, additional, Pfeifer, Joschka, additional, Philippov, Maxim, additional, Schervish, Meredith, additional, Schobesberger, Siegfried, additional, Shen, Jiali, additional, Surdu, Mihnea, additional, Tomaz, Sophie, additional, Volkamer, Rainer, additional, Wang, Xinke, additional, Weber, Stefan, additional, Welti, André, additional, Worsnop, Douglas, additional, wu, yusheng, additional, Yan, Chao, additional, Zauner-Wieczorek, Marcel, additional, Kulmala, Markku, additional, Kirkby, Jasper, additional, Donahue, Neil, additional, George, Christian, additional, El-Haddad, Imad, additional, Bianchi, Federico, additional, and Riva, Matthieu, additional
Published: 2023
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27. Iodine oxoacids enhance nucleation of sulfuric acid particles in the atmosphere

Author: He, Xu-Cheng, Simon, Mario, Iyer, Siddharth, Xie, Hong-Bin, Rörup, Birte, Shen, Jiali, Finkenzeller, Henning, Stolzenburg, Dominik, Zhang, Rongjie, Baccarini, Andrea, Tham, Yee Jun, Wang, Mingyi, Amanatidis, Stavros, Piedehierro, Ana A., Amorim, Antonio, Baalbaki, Rima, Brasseur, Zoé, Caudillo, Lucía, Chu, Biwu, Dada, Lubna, Duplissy, Jonathan, El Haddad, Imad, Flagan, Richard C., Granzin, Manuel, Hansel, Armin, Heinritzi, Martin, Hofbauer, Victoria, Jokinen, Tuija, Kemppainen, Deniz, Kong, Weimeng, Krechmer, Jordan, Kürten, Andreas, Lamkaddam, Houssni, Lopez, Brandon, Ma, Fangfang, Mahfouz, Naser G. A., Makhmutov, Vladimir, Manninen, Hanna E., Marie, Guillaume, Marten, Ruby, Massabò, Dario, Mauldin, Roy L., Mentler, Bernhard, Onnela, Antti, Petäjä, Tuukka, Pfeifer, Joschka, Philippov, Maxim, Ranjithkumar, Ananth, Rissanen, Matti P., Schobesberger, Siegfried, Scholz, Wiebke, Schulze, Benjamin, Surdu, Mihnea, Thakur, Roseline C., Tomé, António, Wagner, Andrea C., Wang, Dongyu, Wang, Yonghong, Weber, Stefan K., Welti, André, Winkler, Paul M., Zauner-Wieczorek, Marcel, Baltensperger, Urs, Curtius, Joachim, Kurtén, Theo, Worsnop, Douglas R., Volkamer, Rainer, Lehtipalo, Katrianne, Kirkby, Jasper, Donahue, Neil M., Sipilä, Mikko, Kulmala, Markku, He, Xu-Cheng, Simon, Mario, Iyer, Siddharth, Xie, Hong-Bin, Rörup, Birte, Shen, Jiali, Finkenzeller, Henning, Stolzenburg, Dominik, Zhang, Rongjie, Baccarini, Andrea, Tham, Yee Jun, Wang, Mingyi, Amanatidis, Stavros, Piedehierro, Ana A., Amorim, Antonio, Baalbaki, Rima, Brasseur, Zoé, Caudillo, Lucía, Chu, Biwu, Dada, Lubna, Duplissy, Jonathan, El Haddad, Imad, Flagan, Richard C., Granzin, Manuel, Hansel, Armin, Heinritzi, Martin, Hofbauer, Victoria, Jokinen, Tuija, Kemppainen, Deniz, Kong, Weimeng, Krechmer, Jordan, Kürten, Andreas, Lamkaddam, Houssni, Lopez, Brandon, Ma, Fangfang, Mahfouz, Naser G. A., Makhmutov, Vladimir, Manninen, Hanna E., Marie, Guillaume, Marten, Ruby, Massabò, Dario, Mauldin, Roy L., Mentler, Bernhard, Onnela, Antti, Petäjä, Tuukka, Pfeifer, Joschka, Philippov, Maxim, Ranjithkumar, Ananth, Rissanen, Matti P., Schobesberger, Siegfried, Scholz, Wiebke, Schulze, Benjamin, Surdu, Mihnea, Thakur, Roseline C., Tomé, António, Wagner, Andrea C., Wang, Dongyu, Wang, Yonghong, Weber, Stefan K., Welti, André, Winkler, Paul M., Zauner-Wieczorek, Marcel, Baltensperger, Urs, Curtius, Joachim, Kurtén, Theo, Worsnop, Douglas R., Volkamer, Rainer, Lehtipalo, Katrianne, Kirkby, Jasper, Donahue, Neil M., Sipilä, Mikko, and Kulmala, Markku
Abstract: The main nucleating vapor in the atmosphere is thought to be sulfuric acid (H2SO4), stabilized by ammonia (NH3). However, in marine and polar regions, NH3 is generally low, and H2SO4 is frequently found together with iodine oxoacids [HIOx, i.e., iodic acid (HIO3) and iodous acid (HIO2)]. In experiments performed with the CERN CLOUD (Cosmics Leaving OUtdoor Droplets) chamber, we investigated the interplay of H2SO4 and HIOx during atmospheric particle nucleation. We found that HIOx greatly enhances H2SO4(-NH3) nucleation through two different interactions. First, HIO3 strongly binds with H2SO4 in charged clusters so they drive particle nucleation synergistically. Second, HIO2 substitutes for NH3, forming strongly bound H2SO4-HIO2 acid-base pairs in molecular clusters. Global observations imply that HIOx is enhancing H2SO4(-NH3) nucleation rates 10- to 10,000-fold in marine and polar regions.
Published: 2023

28. Reduced anthropogenic aerosol radiative forcing caused by biogenic new particle formation

Author: Gordon, Hamish, Sengupta, Kamalika, Rap, Alexandru, Duplissy, Jonathan, Frege, Carla, Williamson, Christina, Heinritzi, Martin, Simon, Mario, Yan, Chao, Almeida, João, Tröstl, Jasmin, Nieminen, Tuomo, Ortega, Ismael K., Wagner, Robert, Dunne, Eimear M., Adamov, Alexey, Amorim, Antonio, Bernhammer, Anne-Kathrin, Bianchi, Federico, Breitenlechner, Martin, Brilke, Sophia, Chen, Xuemeng, Craven, Jill S., Dias, Antonio, Ehrhart, Sebastian, Fischer, Lukas, Flagan, Richard C., Franchin, Alessandro, Fuchs, Claudia, Guida, Roberto, Hakala, Jani, Hoyle, Christopher R., Jokinen, Tuija, Junninen, Heikki, Kangasluoma, Juha, Kim, Jaeseok, Kirkby, Jasper, Krapf, Manuel, Kürten, Andreas, Laaksonen, Ari, Lehtipalo, Katrianne, Makhmutov, Vladimir, Mathot, Serge, Molteni, Ugo, Monks, Sarah A., Onnela, Antti, Peräkylä, Otso, Piel, Felix, Petäjä, Tuukka, Praplan, Arnaud P., Pringle, Kirsty J., Richards, Nigel A. D., Rissanen, Matti P., Rondo, Linda, Sarnela, Nina, Schobesberger, Siegfried, Scott, Catherine E., Seinfeld, John H., Sharma, Sangeeta, Sipilä, Mikko, Steiner, Gerhard, Stozhkov, Yuri, Stratmann, Frank, Tomé, Antonio, Virtanen, Annele, Vogel, Alexander Lucas, Wagner, Andrea C., Wagner, Paul E., Weingartner, Ernest, Wimmer, Daniela, Winkler, Paul M., Ye, Penglin, Zhang, Xuan, Hansel, Armin, Dommen, Josef, Donahue, Neil M., Worsnop, Douglas R., Baltensperger, Urs, Kulmala, Markku, Curtius, Joachim, and Carslaw, Kenneth S.
Published: 2016

29. Temperature, humidity, and ionisation effect of iodine oxoacid nucleation

Author: Rörup, Birte, He, Xu-Cheng, Shen, Jiali, Baalbaki, Rima, Dada, Lubna, Sipilä, Mikko, Kirkby, Jasper, Kulmala, Markku, Amorim, Antonio, Baccarini, Andrea, Bell, David M., Caudillo-Plath, Lucía, Duplissy, Jonathan, Finkenzeller, Henning, Kürten, Andreas, Lamkaddam, Houssni, Lee, Chuan Ping, Makhmutov, Vladimir, Manninen, Hanna E., Marie, Guillaume, Marten, Ruby, Mentler, Bernhard, Onnela, Antti, Philippov, Maxim, Scholz, Carolin Wiebke, Simon, Mario, Stolzenburg, Dominik, Tham, Yee Jun, Tomé, António, Wagner, Andrea C., Wang, Mingyi, Wang, Dongyu, Wang, Yonghong, Weber, Stefan K., Zauner-Wieczorek, Marcel, Baltensperger, Urs, Curtius, Joachim, Donahue, Neil M., El Haddad, Imad, Flagan, Richard C., Hansel, Armin, Möhler, Ottmar, Petäjä, Tuukka, Volkamer, Rainer, Worsnop, Douglas, and Lehtipalo, Katrianne
Abstract: Iodine oxoacids are recognised for their significant contribution to the formation of new particles in marine and polar atmospheres. Nevertheless, to incorporate the iodine oxoacid nucleation mechanism into global simulations, it is essential to comprehend how this mechanism varies under various atmospheric conditions. In this study, we combined measurements from the CLOUD (Cosmic Leaving OUtdoor Droplets) chamber at CERN and simulations with a kinetic model to investigate the impact of temperature, ionisation, and humidity on iodine oxoacid nucleation. Our findings reveal that ion-induced particle formation rates remain largely unaffected by changes in temperature. However, neutral particle formation rates experience a significant increase when the temperature drops from +10 °C to −10 °C. Running the kinetic model with varying ionisation rates demonstrates that the particle formation rate only increases with a higher ionisation rate when the iodic acid concentration exceeds 1.5 × 107cm−3, a concentration rarely reached in pristine marine atmospheres. Consequently, our simulations suggest that, despite higher ionisation rates, the charged cluster nucleation pathway of iodic acid is unlikely to be enhanced in the upper troposphere by higher ionisation rates. Instead, the neutral nucleation channel is likely to be the dominant channel in that region. Notably, the iodine oxoacid nucleation mechanism remains unaffected by changes in relative humidity from 2% to 80%. However, under unrealistically dry conditions (below 0.008% RH at +10 °C), iodine oxides (I2O4and I2O5) significantly enhance formation rates. Therefore, we conclude that iodine oxoacid nucleation is the dominant nucleation mechanism for iodine nucleation in the marine and polar boundary layer atmosphere.
Published: 2024
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30. Interactions of peroxy radicals from monoterpene and isoprene oxidation simulated in the radical volatility basis setElectronic supplementary information (ESI) available. See DOI: https://doi.org/10.1039/d4ea00056k

Author: Schervish, Meredith, Heinritzi, Martin, Stolzenburg, Dominik, Dada, Lubna, Wang, Mingyi, Ye, Qing, Hofbauer, Victoria, DeVivo, Jenna, Bianchi, Federico, Brilke, Sophia, Duplissy, Jonathan, El Haddad, Imad, Finkenzeller, Henning, He, Xu-Cheng, Kvashnin, Aleksander, Kim, Changhyuk, Kirkby, Jasper, Kulmala, Markku, Lehtipalo, Katrianne, Lopez, Brandon, Makhmutov, Vladimir, Mentler, Bernhard, Molteni, Ugo, Nie, Wei, Petäjä, Tuuka, Quéléver, Lauriane, Volkamer, Rainer, Wagner, Andrea C., Winkler, Paul, Yan, Chao, and Donahue, Neil M.
Abstract: Isoprene affects new particle formation rates in environments and experiments also containing monoterpenes. For the most part, isoprene reduces particle formation rates, but the reason is debated. It is proposed that due to its fast reaction with OH, isoprene may compete with larger monoterpenes for oxidants. However, by forming a large amount of peroxy-radicals (RO2), isoprene may also interfere with the formation of the nucleating species compared to a purely monoterpene system. We explore the RO2cross reactions between monoterpene and isoprene oxidation products using the radical Volatility Basis Set (radical-VBS), a simplified reaction mechanism, comparing with observations from the CLOUD experiment at CERN. We find that isoprene interferes with covalently bound C20dimers formed in the pure monoterpene system and consequently reduces the yields of the lowest volatility (Ultra Low Volatility Organic Carbon, ULVOC) VBS products. This in turn reduces nucleation rates, while having less of an effect on subsequent growth rates.
Published: 2024
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31. Molecular Understanding of the Enhancement in Organic Aerosol Mass at High Relative Humidity

Author: Surdu, Mihnea, primary, Lamkaddam, Houssni, additional, Wang, Dongyu S., additional, Bell, David M., additional, Xiao, Mao, additional, Lee, Chuan Ping, additional, Li, Dandan, additional, Caudillo, Lucía, additional, Marie, Guillaume, additional, Scholz, Wiebke, additional, Wang, Mingyi, additional, Lopez, Brandon, additional, Piedehierro, Ana A., additional, Ataei, Farnoush, additional, Baalbaki, Rima, additional, Bertozzi, Barbara, additional, Bogert, Pia, additional, Brasseur, Zoé, additional, Dada, Lubna, additional, Duplissy, Jonathan, additional, Finkenzeller, Henning, additional, He, Xu-Cheng, additional, Höhler, Kristina, additional, Korhonen, Kimmo, additional, Krechmer, Jordan E., additional, Lehtipalo, Katrianne, additional, Mahfouz, Naser G. A., additional, Manninen, Hanna E., additional, Marten, Ruby, additional, Massabò, Dario, additional, Mauldin, Roy, additional, Petäjä, Tuukka, additional, Pfeifer, Joschka, additional, Philippov, Maxim, additional, Rörup, Birte, additional, Simon, Mario, additional, Shen, Jiali, additional, Umo, Nsikanabasi Silas, additional, Vogel, Franziska, additional, Weber, Stefan K., additional, Zauner-Wieczorek, Marcel, additional, Volkamer, Rainer, additional, Saathoff, Harald, additional, Möhler, Ottmar, additional, Kirkby, Jasper, additional, Worsnop, Douglas R., additional, Kulmala, Markku, additional, Stratmann, Frank, additional, Hansel, Armin, additional, Curtius, Joachim, additional, Welti, André, additional, Riva, Matthieu, additional, Donahue, Neil M., additional, Baltensperger, Urs, additional, and El Haddad, Imad, additional
Published: 2023
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32. Supplementary material to "Measurement of the rate coefficients between atmospheric ions and multiply charged aerosol particles in the CERN CLOUD chamber"

Author: Pfeifer, Joschka, primary, Mahfouz, Naser G., additional, Schulze, Ben, additional, Mathot, Serge, additional, Stolzenburg, Dominik, additional, Baalbaki, Rima, additional, Brasseur, Zoé, additional, Caudillo, Lucia, additional, Dada, Lubna, additional, Granzin, Manuel, additional, He, Xu-Cheng, additional, Lamkaddam, Houssni, additional, Lopez, Brandon, additional, Makhmutov, Vladimir, additional, Marten, Ruby, additional, Mentler, Bernhard, additional, Müller, Tatjana, additional, Onnela, Antti, additional, Philippov, Maxim, additional, Piedehierro, Ana A., additional, Rörup, Birte, additional, Schervish, Meredith, additional, Tian, Ping, additional, Umo, Nsikanabasi S., additional, Wang, Dongyu S., additional, Wang, Mingyi, additional, Weber, Stefan K., additional, Welti, André, additional, Wu, Yusheng, additional, Zauner-Wieczorek, Marcel, additional, Amorim, Antonio, additional, El Haddad, Imad, additional, Kulmala, Markku, additional, Lehtipalo, Katrianne, additional, Petäjä, Tuukka, additional, Tomé, António, additional, Mirme, Sander, additional, Manninen, Hanna E., additional, Donahue, Neil M., additional, Flagan, Richard C., additional, Kürten, Andreas, additional, Curtius, Joachim, additional, and Kirkby, Jasper, additional
Published: 2022
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33. Measurement of the rate coefficients between atmospheric ions and multiply charged aerosol particles in the CERN CLOUD chamber

Author: Pfeifer, Joschka, primary, Mahfouz, Naser G., additional, Schulze, Ben, additional, Mathot, Serge, additional, Stolzenburg, Dominik, additional, Baalbaki, Rima, additional, Brasseur, Zoé, additional, Caudillo, Lucia, additional, Dada, Lubna, additional, Granzin, Manuel, additional, He, Xu-Cheng, additional, Lamkaddam, Houssni, additional, Lopez, Brandon, additional, Makhmutov, Vladimir, additional, Marten, Ruby, additional, Mentler, Bernhard, additional, Müller, Tatjana, additional, Onnela, Antti, additional, Philippov, Maxim, additional, Piedehierro, Ana A., additional, Rörup, Birte, additional, Schervish, Meredith, additional, Tian, Ping, additional, Umo, Nsikanabasi S., additional, Wang, Dongyu S., additional, Wang, Mingyi, additional, Weber, Stefan K., additional, Welti, André, additional, Wu, Yusheng, additional, Zauner-Wieczorek, Marcel, additional, Amorim, Antonio, additional, El Haddad, Imad, additional, Kulmala, Markku, additional, Lehtipalo, Katrianne, additional, Petäjä, Tuukka, additional, Tomé, António, additional, Mirme, Sander, additional, Manninen, Hanna E., additional, Donahue, Neil M., additional, Flagan, Richard C., additional, Kürten, Andreas, additional, Curtius, Joachim, additional, and Kirkby, Jasper, additional
Published: 2022
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34. The gas-phase formation mechanism of iodic acid as an atmospheric aerosol source

Author: Finkenzeller, Henning, primary, Iyer, Siddharth, additional, He, Xu-Cheng, additional, Simon, Mario, additional, Koenig, Theodore K., additional, Lee, Christopher F., additional, Valiev, Rashid, additional, Hofbauer, Victoria, additional, Amorim, Antonio, additional, Baalbaki, Rima, additional, Baccarini, Andrea, additional, Beck, Lisa, additional, Bell, David M., additional, Caudillo, Lucía, additional, Chen, Dexian, additional, Chiu, Randall, additional, Chu, Biwu, additional, Dada, Lubna, additional, Duplissy, Jonathan, additional, Heinritzi, Martin, additional, Kemppainen, Deniz, additional, Kim, Changhyuk, additional, Krechmer, Jordan, additional, Kürten, Andreas, additional, Kvashnin, Alexandr, additional, Lamkaddam, Houssni, additional, Lee, Chuan Ping, additional, Lehtipalo, Katrianne, additional, Li, Zijun, additional, Makhmutov, Vladimir, additional, Manninen, Hanna E., additional, Marie, Guillaume, additional, Marten, Ruby, additional, Mauldin, Roy L., additional, Mentler, Bernhard, additional, Müller, Tatjana, additional, Petäjä, Tuukka, additional, Philippov, Maxim, additional, Ranjithkumar, Ananth, additional, Rörup, Birte, additional, Shen, Jiali, additional, Stolzenburg, Dominik, additional, Tauber, Christian, additional, Tham, Yee Jun, additional, Tomé, António, additional, Vazquez-Pufleau, Miguel, additional, Wagner, Andrea C., additional, Wang, Dongyu S., additional, Wang, Mingyi, additional, Wang, Yonghong, additional, Weber, Stefan K., additional, Nie, Wei, additional, Wu, Yusheng, additional, Xiao, Mao, additional, Ye, Qing, additional, Zauner-Wieczorek, Marcel, additional, Hansel, Armin, additional, Baltensperger, Urs, additional, Brioude, Jérome, additional, Curtius, Joachim, additional, Donahue, Neil M., additional, Haddad, Imad El, additional, Flagan, Richard C., additional, Kulmala, Markku, additional, Kirkby, Jasper, additional, Sipilä, Mikko, additional, Worsnop, Douglas R., additional, Kurten, Theo, additional, Rissanen, Matti, additional, and Volkamer, Rainer, additional
Published: 2022
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35. High Gas-Phase Methanesulfonic Acid Production in the OH-Initiated Oxidation of Dimethyl Sulfide at Low Temperatures

Author: Shen, Jiali, primary, Scholz, Wiebke, additional, He, Xu-Cheng, additional, Zhou, Putian, additional, Marie, Guillaume, additional, Wang, Mingyi, additional, Marten, Ruby, additional, Surdu, Mihnea, additional, Rörup, Birte, additional, Baalbaki, Rima, additional, Amorim, Antonio, additional, Ataei, Farnoush, additional, Bell, David M., additional, Bertozzi, Barbara, additional, Brasseur, Zoé, additional, Caudillo, Lucía, additional, Chen, Dexian, additional, Chu, Biwu, additional, Dada, Lubna, additional, Duplissy, Jonathan, additional, Finkenzeller, Henning, additional, Granzin, Manuel, additional, Guida, Roberto, additional, Heinritzi, Martin, additional, Hofbauer, Victoria, additional, Iyer, Siddharth, additional, Kemppainen, Deniz, additional, Kong, Weimeng, additional, Krechmer, Jordan E., additional, Kürten, Andreas, additional, Lamkaddam, Houssni, additional, Lee, Chuan Ping, additional, Lopez, Brandon, additional, Mahfouz, Naser G. A., additional, Manninen, Hanna E., additional, Massabò, Dario, additional, Mauldin, Roy L., additional, Mentler, Bernhard, additional, Müller, Tatjana, additional, Pfeifer, Joschka, additional, Philippov, Maxim, additional, Piedehierro, Ana A., additional, Roldin, Pontus, additional, Schobesberger, Siegfried, additional, Simon, Mario, additional, Stolzenburg, Dominik, additional, Tham, Yee Jun, additional, Tomé, António, additional, Umo, Nsikanabasi Silas, additional, Wang, Dongyu, additional, Wang, Yonghong, additional, Weber, Stefan K., additional, Welti, André, additional, Wollesen de Jonge, Robin, additional, Wu, Yusheng, additional, Zauner-Wieczorek, Marcel, additional, Zust, Felix, additional, Baltensperger, Urs, additional, Curtius, Joachim, additional, Flagan, Richard C., additional, Hansel, Armin, additional, Möhler, Ottmar, additional, Petäjä, Tuukka, additional, Volkamer, Rainer, additional, Kulmala, Markku, additional, Lehtipalo, Katrianne, additional, Rissanen, Matti, additional, Kirkby, Jasper, additional, El-Haddad, Imad, additional, Bianchi, Federico, additional, Sipilä, Mikko, additional, Donahue, Neil M., additional, and Worsnop, Douglas R., additional
Published: 2022
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36. Critical Role of Iodous Acid in Neutral Iodine Oxoacid Nucleation

Author: Zhang, Rongjie, primary, Xie, Hong-Bin, additional, Ma, Fangfang, additional, Chen, Jingwen, additional, Iyer, Siddharth, additional, Simon, Mario, additional, Heinritzi, Martin, additional, Shen, Jiali, additional, Tham, Yee Jun, additional, Kurtén, Theo, additional, Worsnop, Douglas R., additional, Kirkby, Jasper, additional, Curtius, Joachim, additional, Sipilä, Mikko, additional, Kulmala, Markku, additional, and He, Xu-Cheng, additional
Published: 2022
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37. Neutral molecular cluster formation of sulfuric acid-dimethylamine observed in real time under atmospheric conditions

Author: Kürten, Andreas, Jokinen, Tuija, Simon, Mario, Sipilä, Mikko, Sarnela, Nina, Junninen, Heikki, Adamov, Alexey, Almeida, João, Amorim, Antonio, Bianchi, Federico, Breitenlechner, Martin, Dommen, Josef, Donahue, Neil M., Duplissy, Jonathan, Ehrhart, Sebastian, Flagan, Richard C., Franchin, Alessandro, Hakala, Jani, Hansel, Armin, Heinritzi, Martin, Hutterli, Manuel, Kangasluoma, Juha, Kirkby, Jasper, Laaksonen, Ari, Lehtipalo, Katrianne, Leiminger, Markus, Makhmutov, Vladimir, Mathot, Serge, Onnela, Antti, Petäjä, Tuukka, Praplan, Arnaud P., Riccobono, Francesco, Rissanen, Matti P., Rondo, Linda, Schobesberger, Siegfried, Seinfeld, John H., Steiner, Gerhard, Tomé, António, Tröstl, Jasmin, Winkler, Paul M., Williamson, Christina, Wimmer, Daniela, Ye, Penglin, Baltensperger, Urs, Carslaw, Kenneth S., Kulmala, Markku, Worsnop, Douglas R., and Curtius, Joachim
Published: 2014

38. Oxidation Products of Biogenic Emissions Contribute to Nucleation of Atmospheric Particles

Author: Riccobono, Francesco, Schobesberger, Siegfried, Scott, Catherine E., Dommen, Josef, Ortega, Ismael K., Rondo, Linda, Almeida, João, Amorim, Antonio, Bianchi, Federico, Breitenlechner, Martin, David, André, Downard, Andrew, Dunne, Eimear M., Duplissy, Jonathan, Ehrhart, Sebastian, Flagan, Richard C., Franchin, Alessandro, Hansel, Armin, Junninen, Heikki, Kajos, Maija, Keskinen, Helmi, Kupc, Agnieszka, Kürten, Andreas, Kvashin, Alexander N., Laaksonen, Ari, Lehtipalo, Katrianne, Makhmutov, Vladimir, Mathot, Serge, Nieminen, Tuomo, Onnela, Antti, Petäjä, Tuukka, Praplan, Arnaud P., Santos, Filipe D., Schallhart, Simon, Seinfeld, John H., Sipilä, Mikko, Spracklen, Dominick V., Stozhkov, Yuri, Stratmann, Frank, Tomé, Antonio, Tsagkogeorgas, Georgios, Vaattovaara, Petri, Viisanen, Yrjö, Vrtala, Aron, Wagner, Paul E., Weingartner, Ernest, Wex, Heike, Wimmer, Daniela, Carslaw, Kenneth S., Curtius, Joachim, Donahue, Neil M., Kirkby, Jasper, Kulmala, Markku, Worsnop, Douglas R., and Baltensperger, Urs
Published: 2014

39. Ammonium CI-Orbitrap: a tool for characterizing the reactivity of oxygenated organic molecules.

Author: Dandan Li, Dongyu Wang, Caudillo, Lucia, Scholz, Wiebke, Mingyi Wang, Tomaz, Sophie, Marie, Guillaume, Surdu, Mihnea, Eccli, Elias, Xianda Gong, Gonzalez-Carracedo, Loic, Granzin, Manuel, Pfeifer, Joschka, Rörup, Birte, Schulze, Benjamin, Rantala, Pekka, Perrier, Sébastien, Hansel, Armin, Curtius, Joachim, and Kirkby, Jasper
Subjects: CHEMICAL ionization mass spectrometry, MASS spectrometry, TIME-of-flight mass spectrometers, MASS spectrometers, ATMOSPHERIC aerosols, PINENE, NUCLEAR research
Abstract: Oxygenated organic molecules (OOMs) play an important role in the formation of atmospheric aerosols. Due to various analytical challenges in measuring organic vapors, uncertainties remain in the formation and fate of OOMs. The chemical ionization Orbitrap mass spectrometer (CI-Orbitrap) has recently been shown to be a powerful technique able to accurately identify gaseous organic compounds due to its great mass resolving power. Here we present the ammonium ion (NH4+) based CI-Orbitrap as a technique capable of measuring a wide range of gaseous OOMs. The performance of the CI-(NH4+)-Orbitrap was compared with that of state-of-the-art mass spectrometers, including a nitrate ion (NO3-) based CI coupled to an atmospheric pressure interfaced to long time-of-flight mass spectrometer (APi-LTOF), a new generation of proton transfer reaction-TOF mass spectrometer (PTR3-TOF), and an iodide (I-) based CI-TOF mass spectrometer equipped with a Filter Inlet for Gases and AEROsols (FIGAERO-CIMS). The instruments were deployed simultaneously in the Cosmic Leaving OUtdoors Droplets (CLOUD) chamber at the European Organization for Nuclear Research (CERN) during the CLOUD14 campaign in 2019. Products generated from α-pinene ozonolysis across multiple experimental conditions were simultaneously measured by the mass spectrometers. NH4+-Orbitrap was able to identify the widest range of OOMs (i.e., O = 2), from low oxidized species to highly oxygenated volatile organic compounds (HOM). Excellent agreements were found between the NH4+-Orbitrap and the NO3--LTOF for characterizing HOMs and with the PTR3- TOF for the less oxidized monomeric species. A semi-quantitative information was retrieved for OOMs measured by NH4+-Orbitrap using calibration factors derived from this side-by-side comparison. As other mass spectrometry techniques used during this campaign, the detection sensitivity of NH4+-Orbitrap to OOMs is greatly affected by relative humidity, which may be related to changes in ionization efficiency and/or multiphase chemistry. Overall, this study shows that NH4+ ion46 based chemistry associated with the high mass resolving power of the Orbitrap mass analyzer can measure almost all-inclusive compounds. As a result, it is now possible to cover the entire range of compounds, which can lead to a better understanding of the oxidation processes. [ABSTRACT FROM AUTHOR]
Published: 2023
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40. Ion-induced nucleation of pure biogenic particles

Author: Kirkby, Jasper, Duplissy, Jonathan, Sengupta, Kamalika, Frege, Carla, Gordon, Hamish, Williamson, Christina, Heinritzi, Martin, Simon, Mario, Yan, Chao, Almeida, Joao, Amorim, Antonio, Bernhammer, Anne-Kathrin, Bianchi, Federico, Breitenlechner, Martin, Brilke, Sophia, and Chen, Xuemeng
Subjects: Vapors -- Chemical properties, Nucleation -- Research, Aerosols -- Chemical properties, Ions -- Chemical properties, Environmental issues, Science and technology, Zoology and wildlife conservation
Abstract: Aerosol particles can form in the atmosphere by nucleation of highly oxidized biogenic vapours in the absence of sulfuric acid, with ions from Galactic cosmic rays increasing the nucleation rate by one to two orders of magnitude compared with neutral nucleation. Aerosol particles can form in the atmosphere by nucleation of highly oxidized biogenic vapours in the absence of sulfuric acid, with ions from Galactic cosmic rays increasing the nucleation rate by one to two orders of magnitude compared with neutral nucleation. Aerosol particle formation in clean air The effect of atmospheric aerosols on clouds and the radiative forcing of the climate system remains poorly understood. It is thought that nucleation of aerosol particles from atmospheric vapours rarely proceeds in the absence of sulfuric acid. Now two papers in this week's Nature point to a previously unappreciated role for highly oxygenated molecules (HOMs) in promoting new particle formation and growth, essentially a mechanism that produces aerosols in the absence of pollution. Jasper Kirkby et al. show that aerosol particles can form as a result of ion-induced nucleation of HOMs in the absence of sulfuric acid under conditions relevant to the atmosphere in the CLOUD chamber at CERN. Jasmin Tröstl et al. examined the role of organic vapours in the initial growth of nucleated organic particles in the absence of sulfuric acid in the CERN CLOUD chamber under atmospheric conditions. They find that the organic vapours driving initial growth have extremely low volatilities. With increasing particle size, subsequent growth is primarily due to more abundant organic vapours of slightly higher volatility. Atmospheric aerosols and their effect on clouds are thought to be important for anthropogenic radiative forcing of the climate, yet remain poorly understood.sup.1. Globally, around half of cloud condensation nuclei originate from nucleation of atmospheric vapours.sup.2. It is thought that sulfuric acid is essential to initiate most particle formation in the atmosphere.sup.3,4, and that ions have a relatively minor role.sup.5. Some laboratory studies, however, have reported organic particle formation without the intentional addition of sulfuric acid, although contamination could not be excluded.sup.6,7. Here we present evidence for the formation of aerosol particles from highly oxidized biogenic vapours in the absence of sulfuric acid in a large chamber under atmospheric conditions. The highly oxygenated molecules (HOMs) are produced by ozonolysis of [alpha]-pinene. We find that ions from Galactic cosmic rays increase the nucleation rate by one to two orders of magnitude compared with neutral nucleation. Our experimental findings are supported by quantum chemical calculations of the cluster binding energies of representative HOMs. Ion-induced nucleation of pure organic particles constitutes a potentially widespread source of aerosol particles in terrestrial environments with low sulfuric acid pollution., Author(s): Jasper Kirkby [sup.1] [sup.2] , Jonathan Duplissy [sup.3] [sup.4] , Kamalika Sengupta [sup.5] , Carla Frege [sup.6] , Hamish Gordon [sup.2] , Christina Williamson [sup.1] [sup.24] , Martin Heinritzi [...]
Published: 2016
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41. Variations of Galactic Cosmic Rays and the Earth's Climate

Author: Kirkby, Jasper, Carslaw, Kenneth S., and Frisch, Priscilla C., editor
Published: 2006
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42. An intercomparison study of four different techniques for measuring the chemical composition of nanoparticles

Author: Caudillo, Lucía, primary, Surdu, Mihnea, additional, Lopez, Brandon, additional, Wang, Mingyi, additional, Thoma, Markus, additional, Bräkling, Steffen, additional, Buchholz, Angela, additional, Simon, Mario, additional, Wagner, Andrea C., additional, Müller, Tatjana, additional, Granzin, Manuel, additional, Heinritzi, Martin, additional, Amorim, Antonio, additional, Bell, David M., additional, Brasseur, Zoé, additional, Dada, Lubna, additional, Duplissy, Jonathan, additional, Finkenzeller, Henning, additional, He, Xu-Cheng, additional, Lamkaddam, Houssni, additional, Mahfouz, Naser G. A., additional, Makhmutov, Vladimir, additional, Manninen, Hanna E., additional, Marie, Guillaume, additional, Marten, Ruby, additional, Mauldin, Roy L., additional, Mentler, Bernhard, additional, Onnela, Antti, additional, Petäjä, Tuukka, additional, Pfeifer, Joschka, additional, Philippov, Maxim, additional, Piedehierro, Ana A., additional, Rörup, Birte, additional, Scholz, Wiebke, additional, Shen, Jiali, additional, Stolzenburg, Dominik, additional, Tauber, Christian, additional, Tian, Ping, additional, Tomé, António, additional, Umo, Nsikanabasi Silas, additional, Wang, Dongyu S., additional, Wang, Yonghong, additional, Weber, Stefan K., additional, Welti, André, additional, Zauner-Wieczorek, Marcel, additional, Baltensperger, Urs, additional, Flagan, Richard C., additional, Hansel, Armin, additional, Kirkby, Jasper, additional, Kulmala, Markku, additional, Lehtipalo, Katrianne, additional, Worsnop, Douglas R., additional, Haddad, Imad El, additional, Donahue, Neil M., additional, Vogel, Alexander L., additional, Kürten, Andreas, additional, and Curtius, Joachim, additional
Published: 2022
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43. Supplementary material to "An intercomparison study of four different techniques for measuring the chemical composition of nanoparticles"

Author: Caudillo, Lucía, primary, Surdu, Mihnea, additional, Lopez, Brandon, additional, Wang, Mingyi, additional, Thoma, Markus, additional, Bräkling, Steffen, additional, Buchholz, Angela, additional, Simon, Mario, additional, Wagner, Andrea C., additional, Müller, Tatjana, additional, Granzin, Manuel, additional, Heinritzi, Martin, additional, Amorim, Antonio, additional, Bell, David M., additional, Brasseur, Zoé, additional, Dada, Lubna, additional, Duplissy, Jonathan, additional, Finkenzeller, Henning, additional, He, Xu-Cheng, additional, Lamkaddam, Houssni, additional, Mahfouz, Naser G. A., additional, Makhmutov, Vladimir, additional, Manninen, Hanna E., additional, Marie, Guillaume, additional, Marten, Ruby, additional, Mauldin, Roy L., additional, Mentler, Bernhard, additional, Onnela, Antti, additional, Petäjä, Tuukka, additional, Pfeifer, Joschka, additional, Philippov, Maxim, additional, Piedehierro, Ana A., additional, Rörup, Birte, additional, Scholz, Wiebke, additional, Shen, Jiali, additional, Stolzenburg, Dominik, additional, Tauber, Christian, additional, Tian, Ping, additional, Tomé, António, additional, Umo, Nsikanabasi Silas, additional, Wang, Dongyu S., additional, Wang, Yonghong, additional, Weber, Stefan K., additional, Welti, André, additional, Zauner-Wieczorek, Marcel, additional, Baltensperger, Urs, additional, Flagan, Richard C., additional, Hansel, Armin, additional, Kirkby, Jasper, additional, Kulmala, Markku, additional, Lehtipalo, Katrianne, additional, Worsnop, Douglas R., additional, Haddad, Imad El, additional, Donahue, Neil M., additional, Vogel, Alexander L., additional, Kürten, Andreas, additional, and Curtius, Joachim, additional
Published: 2022
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44. Molecular understanding of atmospheric particle formation from sulfuric acid and large oxidized organic molecules

Author: Schobesberger, Siegfried, Junninen, Heikki, Bianchi, Federico, Lönn, Gustaf, Ehn, Mikael, Lehtipalo, Katrianne, Dommen, Josef, Ehrhart, Sebastian, Ortega, Ismael K., Franchin, Alessandro, Nieminen, Tuomo, Riccobono, Francesco, Hutterli, Manuel, Duplissy, Jonathan, Almeida, João, Amorim, Antonio, Breitenlechner, Martin, Downard, Andrew J., Dunne, Eimear M., Flagan, Richard C., Kajos, Maija, Keskinen, Helmi, Kirkby, Jasper, Kupc, Agnieszka, Kürten, Andreas, Kurtén, Theo, Laaksonen, Ari, Mathot, Serge, Onnela, Antti, Praplan, Arnaud P., Rondo, Linda, Santos, Filipe D., Schallhart, Simon, Schnitzhofer, Ralf, Sipilä, Mikko, Tomé, António, Tsagkogeorgas, Georgios, Vehkamäki, Hanna, Wimmer, Daniela, Baltensperger, Urs, Carslaw, Kenneth S., Curtius, Joachim, Hansel, Armin, Petäjä, Tuukka, Kulmala, Markku, Donahue, Neil M., and Worsnop, Douglas R.
Published: 2013

45. Modelling the gas–particle partitioning and water uptake of isoprene-derived secondary organic aerosol at high and low relative humidity

Author: Amaladhasan, Dalrin Ampritta, primary, Heyn, Claudia, additional, Hoyle, Christopher R., additional, El Haddad, Imad, additional, Elser, Miriam, additional, Pieber, Simone M., additional, Slowik, Jay G., additional, Amorim, Antonio, additional, Duplissy, Jonathan, additional, Ehrhart, Sebastian, additional, Makhmutov, Vladimir, additional, Molteni, Ugo, additional, Rissanen, Matti, additional, Stozhkov, Yuri, additional, Wagner, Robert, additional, Hansel, Armin, additional, Kirkby, Jasper, additional, Donahue, Neil M., additional, Volkamer, Rainer, additional, Baltensperger, Urs, additional, Gysel-Beer, Martin, additional, and Zuend, Andreas, additional
Published: 2022
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46. Survival of newly formed particles in haze conditions

Author: Marten, Ruby, primary, Xiao, Mao, additional, Rörup, Birte, additional, Wang, Mingyi, additional, Kong, Weimeng, additional, He, Xu-Cheng, additional, Stolzenburg, Dominik, additional, Pfeifer, Joschka, additional, Marie, Guillaume, additional, Wang, Dongyu S., additional, Scholz, Wiebke, additional, Baccarini, Andrea, additional, Lee, Chuan Ping, additional, Amorim, Antonio, additional, Baalbaki, Rima, additional, Bell, David M., additional, Bertozzi, Barbara, additional, Caudillo, Lucía, additional, Chu, Biwu, additional, Dada, Lubna, additional, Duplissy, Jonathan, additional, Finkenzeller, Henning, additional, Carracedo, Loïc Gonzalez, additional, Granzin, Manuel, additional, Hansel, Armin, additional, Heinritzi, Martin, additional, Hofbauer, Victoria, additional, Kemppainen, Deniz, additional, Kürten, Andreas, additional, Lampimäki, Markus, additional, Lehtipalo, Katrianne, additional, Makhmutov, Vladimir, additional, Manninen, Hanna E., additional, Mentler, Bernhard, additional, Petäjä, Tuukka, additional, Philippov, Maxim, additional, Shen, Jiali, additional, Simon, Mario, additional, Stozhkov, Yuri, additional, Tomé, António, additional, Wagner, Andrea C., additional, Wang, Yonghong, additional, Weber, Stefan K., additional, Wu, Yusheng, additional, Zauner-Wieczorek, Marcel, additional, Curtius, Joachim, additional, Kulmala, Markku, additional, Möhler, Ottmar, additional, Volkamer, Rainer, additional, Winkler, Paul M., additional, Worsnop, Douglas R., additional, Dommen, Josef, additional, Flagan, Richard C., additional, Kirkby, Jasper, additional, Donahue, Neil M., additional, Lamkaddam, Houssni, additional, Baltensperger, Urs, additional, and El Haddad, Imad, additional
Published: 2022
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47. Detectors for ø, τ-charm and B Factories

Author: Kirkby, Jasper, Beiglböck, W., editor, Dienes, M., editor, Month, M., editor, Strasser, B., editor, and Turner, S., editor
Published: 1994
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48. Chemical composition of nanoparticles from <i>α</i>-pinene nucleation and the influence of isoprene and relative humidity at low temperature

Author: Caudillo, Lucía, primary, Rörup, Birte, additional, Heinritzi, Martin, additional, Marie, Guillaume, additional, Simon, Mario, additional, Wagner, Andrea C., additional, Müller, Tatjana, additional, Granzin, Manuel, additional, Amorim, Antonio, additional, Ataei, Farnoush, additional, Baalbaki, Rima, additional, Bertozzi, Barbara, additional, Brasseur, Zoé, additional, Chiu, Randall, additional, Chu, Biwu, additional, Dada, Lubna, additional, Duplissy, Jonathan, additional, Finkenzeller, Henning, additional, Gonzalez Carracedo, Loïc, additional, He, Xu-Cheng, additional, Hofbauer, Victoria, additional, Kong, Weimeng, additional, Lamkaddam, Houssni, additional, Lee, Chuan P., additional, Lopez, Brandon, additional, Mahfouz, Naser G. A., additional, Makhmutov, Vladimir, additional, Manninen, Hanna E., additional, Marten, Ruby, additional, Massabò, Dario, additional, Mauldin, Roy L., additional, Mentler, Bernhard, additional, Molteni, Ugo, additional, Onnela, Antti, additional, Pfeifer, Joschka, additional, Philippov, Maxim, additional, Piedehierro, Ana A., additional, Schervish, Meredith, additional, Scholz, Wiebke, additional, Schulze, Benjamin, additional, Shen, Jiali, additional, Stolzenburg, Dominik, additional, Stozhkov, Yuri, additional, Surdu, Mihnea, additional, Tauber, Christian, additional, Tham, Yee Jun, additional, Tian, Ping, additional, Tomé, António, additional, Vogt, Steffen, additional, Wang, Mingyi, additional, Wang, Dongyu S., additional, Weber, Stefan K., additional, Welti, André, additional, Yonghong, Wang, additional, Yusheng, Wu, additional, Zauner-Wieczorek, Marcel, additional, Baltensperger, Urs, additional, El Haddad, Imad, additional, Flagan, Richard C., additional, Hansel, Armin, additional, Höhler, Kristina, additional, Kirkby, Jasper, additional, Kulmala, Markku, additional, Lehtipalo, Katrianne, additional, Möhler, Ottmar, additional, Saathoff, Harald, additional, Volkamer, Rainer, additional, Winkler, Paul M., additional, Donahue, Neil M., additional, Kürten, Andreas, additional, and Curtius, Joachim, additional
Published: 2021
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49. The driving factors of new particle formation and growth in the polluted boundary layer

Author: Xiao, Mao, primary, Hoyle, Christopher R., additional, Dada, Lubna, additional, Stolzenburg, Dominik, additional, Kürten, Andreas, additional, Wang, Mingyi, additional, Lamkaddam, Houssni, additional, Garmash, Olga, additional, Mentler, Bernhard, additional, Molteni, Ugo, additional, Baccarini, Andrea, additional, Simon, Mario, additional, He, Xu-Cheng, additional, Lehtipalo, Katrianne, additional, Ahonen, Lauri R., additional, Baalbaki, Rima, additional, Bauer, Paulus S., additional, Beck, Lisa, additional, Bell, David, additional, Bianchi, Federico, additional, Brilke, Sophia, additional, Chen, Dexian, additional, Chiu, Randall, additional, Dias, António, additional, Duplissy, Jonathan, additional, Finkenzeller, Henning, additional, Gordon, Hamish, additional, Hofbauer, Victoria, additional, Kim, Changhyuk, additional, Koenig, Theodore K., additional, Lampilahti, Janne, additional, Lee, Chuan Ping, additional, Li, Zijun, additional, Mai, Huajun, additional, Makhmutov, Vladimir, additional, Manninen, Hanna E., additional, Marten, Ruby, additional, Mathot, Serge, additional, Mauldin, Roy L., additional, Nie, Wei, additional, Onnela, Antti, additional, Partoll, Eva, additional, Petäjä, Tuukka, additional, Pfeifer, Joschka, additional, Pospisilova, Veronika, additional, Quéléver, Lauriane L. J., additional, Rissanen, Matti, additional, Schobesberger, Siegfried, additional, Schuchmann, Simone, additional, Stozhkov, Yuri, additional, Tauber, Christian, additional, Tham, Yee Jun, additional, Tomé, António, additional, Vazquez-Pufleau, Miguel, additional, Wagner, Andrea C., additional, Wagner, Robert, additional, Wang, Yonghong, additional, Weitz, Lena, additional, Wimmer, Daniela, additional, Wu, Yusheng, additional, Yan, Chao, additional, Ye, Penglin, additional, Ye, Qing, additional, Zha, Qiaozhi, additional, Zhou, Xueqin, additional, Amorim, Antonio, additional, Carslaw, Ken, additional, Curtius, Joachim, additional, Hansel, Armin, additional, Volkamer, Rainer, additional, Winkler, Paul M., additional, Flagan, Richard C., additional, Kulmala, Markku, additional, Worsnop, Douglas R., additional, Kirkby, Jasper, additional, Donahue, Neil M., additional, Baltensperger, Urs, additional, El Haddad, Imad, additional, and Dommen, Josef, additional
Published: 2021
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50. Molecular understanding of sulphuric acid–amine particle nucleation in the atmosphere

Author: Almeida, João, Schobesberger, Siegfried, Kürten, Andreas, Ortega, Ismael K., Kupiainen-Määttä, Oona, Praplan, Arnaud P., Adamov, Alexey, Amorim, Antonio, Bianchi, Federico, Breitenlechner, Martin, David, André, Dommen, Josef, Donahue, Neil M., Downard, Andrew, Dunne, Eimear, Duplissy, Jonathan, Ehrhart, Sebastian, Flagan, Richard C., Franchin, Alessandro, Guida, Roberto, Hakala, Jani, Hansel, Armin, Heinritzi, Martin, Henschel, Henning, Jokinen, Tuija, Junninen, Heikki, Kajos, Maija, Kangasluoma, Juha, Keskinen, Helmi, Kupc, Agnieszka, Kurtén, Theo, Kvashin, Alexander N., Laaksonen, Ari, Lehtipalo, Katrianne, Leiminger, Markus, Leppä, Johannes, Loukonen, Ville, Makhmutov, Vladimir, Mathot, Serge, McGrath, Matthew J., Nieminen, Tuomo, Olenius, Tinja, Onnela, Antti, Petäjä, Tuukka, Riccobono, Francesco, Riipinen, Ilona, Rissanen, Matti, Rondo, Linda, Ruuskanen, Taina, Santos, Filipe D., Sarnela, Nina, Schallhart, Simon, Schnitzhofer, Ralf, Seinfeld, John H., Simon, Mario, Sipilä, Mikko, Stozhkov, Yuri, Stratmann, Frank, Tomé, Antonio, Tröstl, Jasmin, Tsagkogeorgas, Georgios, Vaattovaara, Petri, Viisanen, Yrjo, Virtanen, Annele, Vrtala, Aron, Wagner, Paul E., Weingartner, Ernest, Wex, Heike, Williamson, Christina, Wimmer, Daniela, Ye, Penglin, Yli-Juuti, Taina, Carslaw, Kenneth S., Kulmala, Markku, Curtius, Joachim, Baltensperger, Urs, Worsnop, Douglas R., Vehkamäki, Hanna, and Kirkby, Jasper
Published: 2013
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