Synergistic HNO3–H2SO4–NH3 upper tropospheric particle formation
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Stefan K. Weber | J. Lelieveld | A. Pozzer | I. Riipinen | T. Petäjä | P. Winkler | R. Volkamer | D. Worsnop | R. Flagan | R. Guida | J. Kirkby | M. Kulmala | Y. Stozhkov | U. Baltensperger | A. Ekman | A. Onnela | A. Hansel | L. Dada | A. Welti | K. Korhonen | O. Möhler | M. Sipilä | H. Gordon | N. Donahue | I. El-Haddad | V. Makhmutov | K. Lehtipalo | S. Schobesberger | J. Curtius | Theodoros Christoudias | J. Krechmer | F. Vogel | R. Wagner | R. Mauldin | Guillaume Marie | M. Granzin | S. Mathot | A. A. Piedehierro | Jiali Shen | J. Duplissy | M. Philippov | Mingyi Wang | Brandon Lopez | Naser G. A. Mahfouz | K. Höhler | Dongyu S. Wang | M. Xiao | A. Kürten | A. Tomé | M. Heinritzi | M. Simon | A. Amorim | H. Lamkaddam | B. Bertozzi | V. Hofbauer | Xucheng He | B. Rörup | B. Schulze | R. Bardakov | W. Scholz | R. Marten | Rima Baalbaki | Hanna E. Manninen | Farnoush Ataei | Pia Bogert | Zoé Brasseur | L. Caudillo | L. De Menezes | H. Finkenzeller | L. Carracedo | Dario Massabò | B. Mentler | Tatjana Müller | A. Ranjithkumar | Meredith Schervish | N. Umo | Yusheng Wu | Marcel Zauner-Wieczorek | Manuel Granzin | Houssni Lamkaddam | Henning Finkenzeller
[1] L. Ahonen,et al. The driving factors of new particle formation and growth in the polluted boundary layer , 2021, Atmospheric Chemistry and Physics.
[2] M. Chin,et al. Chemical transport models often underestimate inorganic aerosol acidity in remote regions of the atmosphere , 2021, Communications Earth & Environment.
[3] Stefan K. Weber,et al. Role of iodine oxoacids in atmospheric aerosol nucleation , 2021, Science.
[4] J. Peischl,et al. Supplementary material to "Large hemispheric difference in ultrafine aerosol concentrations in the lowermost stratosphere at mid and high latitudes" , 2021 .
[5] I. Riipinen,et al. Transport and chemistry of isoprene and its oxidation products in deep convective clouds , 2021, Tellus B: Chemical and Physical Meteorology.
[6] Jian Wang,et al. High concentration of ultrafine particles in the Amazon free troposphere produced by organic new particle formation , 2020, Proceedings of the National Academy of Sciences.
[7] Stefan K. Weber,et al. Molecular understanding of new-particle formation from α-pinene between −50 and +25 °C , 2020 .
[8] Stefan K. Weber,et al. Rapid growth of new atmospheric particles by nitric acid and ammonia condensation , 2020, Nature.
[9] I. Riipinen,et al. A Novel Framework to Study Trace Gas Transport in Deep Convective Clouds , 2020, Journal of Advances in Modeling Earth Systems.
[10] T. Leisner,et al. Solid Ammonium Nitrate Aerosols as Efficient Ice Nucleating Particles at Cirrus Temperatures , 2020, Journal of Geophysical Research: Atmospheres.
[11] U. Pöschl,et al. Particle production in the upper troposphere over the Amazon Basin , 2020 .
[12] K. Lehtinen,et al. Formation and growth of sub-3-nm aerosol particles in experimental chambers , 2020, Nature Protocols.
[13] Stefan K. Weber,et al. Enhanced growth rate of atmospheric particles from sulfuric acid , 2019, Atmospheric Chemistry and Physics.
[14] E. Ray,et al. A large source of cloud condensation nuclei from new particle formation in the tropics , 2019, Nature.
[15] T. Leisner,et al. Ammonium nitrate particles formed in upper troposphere from ground ammonia sources during Asian monsoons , 2019, Nature Geoscience.
[16] A. Kürten. New particle formation from sulfuric acid and ammonia: nucleation and growth model based on thermodynamics derived from CLOUD measurements for a wide range of conditions , 2019, Atmospheric Chemistry and Physics.
[17] J. Lelieveld,et al. Two new submodels for the Modular Earth Submodel System (MESSy): New Aerosol Nucleation (NAN) and small ions (IONS) version 1.0 , 2018, Geoscientific Model Development.
[18] I. Riipinen,et al. Multicomponent new particle formation from sulfuric acid, ammonia, and biogenic vapors , 2018, Science Advances.
[19] R. Flagan,et al. Scanning DMA Data Analysis I. Classification Transfer Function , 2018, Aerosol Science and Technology.
[20] J. Seinfeld,et al. Scanning DMA data analysis II. Integrated DMA-CPC instrument response and data inversion , 2018, Aerosol Science and Technology.
[21] J. Lelieveld,et al. Two new submodels for the Modular Earth Submodel System (MESSy): New Aerosol Nucleation (NAN) and small ions (IONS) version 1.0 , 2018 .
[22] J. Lelieveld,et al. The South Asian monsoon—pollution pump and purifier , 2018, Science.
[23] Andreas Peckhaus,et al. The Fifth International Workshop on Ice Nucleation phase 2 (FIN-02): laboratory intercomparison of ice nucleation measurements , 2018, Atmospheric Measurement Techniques.
[24] Jun Wang,et al. A molecular perspective for global modeling of upper atmospheric NH3 from freezing clouds , 2018, Proceedings of the National Academy of Sciences.
[25] J. Kirkby,et al. Temperature uniformity in the CERN CLOUD chamber , 2017 .
[26] A. Hansel,et al. PTR3: An Instrument for Studying the Lifecycle of Reactive Organic Carbon in the Atmosphere. , 2017, Analytical chemistry.
[27] J. Seinfeld,et al. Design, simulation, and characterization of a radial opposed migration ion and aerosol classifier (ROMIAC) , 2017 .
[28] J. Warner,et al. Increased atmospheric ammonia over the world's major agricultural areas detected from space , 2017, Geophysical research letters.
[29] Harald Saathoff,et al. A New Ice Nucleation Active Site Parameterization for Desert Dust and Soot , 2017 .
[30] G. Mann,et al. Global atmospheric particle formation from CERN CLOUD measurements , 2016, Science.
[31] T. Clarmann,et al. First detection of ammonia (NH 3 ) in the Asian summer monsoon upper troposphere , 2016 .
[32] G. Mann,et al. Size-resolved simulations of the aerosol inorganic composition with the new hybrid dissolution solver HyDiS-1.0: description, evaluation and first global modelling results , 2016 .
[33] T. Petäjä,et al. Experimental particle formation rates spanning tropospheric sulfuric acid and ammonia abundances, ion production rates, and temperatures , 2016 .
[34] J. Curtius,et al. Observation of new particle formation and measurement of sulfuric acid,ammonia, amines and highly oxidized organic molecules at a rural site incentral Germany , 2016 .
[35] G. Pfister,et al. The CU mobile Solar Occultation Flux instrument: structure functions and emission rates of NH 3 , NO 2 and C 2 H 6 , 2016 .
[36] M. Chipperfield,et al. The TOMCAT global chemical transport model v1.6: description of chemical mechanism and model evaluation , 2016 .
[37] D. Worsnop,et al. Reactions of Atmospheric Particulate Stabilized Criegee Intermediates Lead to High-Molecular-Weight Aerosol Components. , 2016, Environmental science & technology.
[38] I. Riipinen,et al. The role of low-volatility organic compounds in initial particle growth in the atmosphere , 2016, Nature.
[39] J. Seinfeld,et al. Ion-induced nucleation of pure biogenic particles , 2016, Nature.
[40] D. Brus,et al. Effect of ions on sulfuric acid‐water binary particle formation: 2. Experimental data and comparison with QC‐normalized classical nucleation theory , 2016 .
[41] John B. Nowak,et al. The global tropospheric ammonia distribution as seen in the 13-year AIRS measurement record , 2015 .
[42] U. Baltensperger,et al. Fast and precise measurement in the sub-20nm size range using a Scanning Mobility Particle Sizer , 2015 .
[43] D. Jacob,et al. Active and widespread halogen chemistry in the tropical and subtropical free troposphere , 2015, Proceedings of the National Academy of Sciences.
[44] J. Seinfeld,et al. Neutral molecular cluster formation of sulfuric acid–dimethylamine observed in real time under atmospheric conditions , 2014, Proceedings of the National Academy of Sciences.
[45] Richard A. Cox,et al. Compilation and evaluation of gas phase diffusion coefficients of reactive trace gases in the atmosphere: volume 1. Inorganic compounds , 2014 .
[46] A. Ekman,et al. Technical note: Introduction to MIMICA, a large‐eddy simulation solver for cloudy planetary boundary layers , 2014 .
[47] J. Seinfeld,et al. Oxidation Products of Biogenic Emissions Contribute to Nucleation of Atmospheric Particles , 2014, Science.
[48] J. Curtius,et al. submitter : Influence of aerosol lifetime on the interpretation of nucleation experiments with respect to the first nucleation theorem , 2013 .
[49] M. Hallquist,et al. A novel method for online analysis of gas and particle composition: description and evaluation of a Filter Inlet for Gases and AEROsols (FIGAERO) , 2013 .
[50] T. Petäjä,et al. Molecular understanding of atmospheric particle formation from sulfuric acid and large oxidized organic molecules , 2013, Proceedings of the National Academy of Sciences.
[51] S. Haider,et al. Characterisation of organic contaminants in the CLOUD chamber at CERN , 2013 .
[52] T. Petäjä,et al. Performance of diethylene glycol-based particle counters in the sub-3 nm size range , 2013 .
[53] H. Schlager,et al. Aerosol observations and growth rates downwind of the anvil of a deep tropical thunderstorm , 2012 .
[54] T. Petäjä,et al. Atmospheric sulphuric acid and neutral cluster measurements using CI-APi-TOF , 2011 .
[55] J. M. Reeves,et al. In situ observations of new particle formation in the tropical upper troposphere: the role of clouds and the nucleation mechanism , 2011 .
[56] Jorge Lima,et al. Role of sulphuric acid, ammonia and galactic cosmic rays in atmospheric aerosol nucleation , 2011, Nature.
[57] Z. Jurányi,et al. A 17 month climatology of the cloud condensation nuclei number concentration at the high alpine site Jungfraujoch , 2011 .
[58] Patrick Jöckel,et al. Development cycle 2 of the Modular Earth Submodel System (MESSy2) , 2010 .
[59] J. Curtius,et al. Performance of a corona ion source for measurement of sulfuric acid by chemical ionization mass spectrometry , 2010 .
[60] Martyn P. Chipperfield,et al. Description and evaluation of GLOMAP-mode: a modal global aerosol microphysics model for the UKCA composition-climate model , 2010 .
[61] U. Rohner,et al. A high-resolution mass spectrometer to measure atmospheric ion composition , 2010 .
[62] D. Fahey,et al. Stratospheric correlation between nitric acid and ozone , 2009 .
[63] W. Winiwarter,et al. How a century of ammonia synthesis changed the world , 2008 .
[64] P. Schouten,et al. Utilising polyphenylene oxide for high exposure solar UVA dosimetry , 2008 .
[65] C. Clerbaux,et al. First global distributions of nitric acid in the troposphere and the stratosphere derived from infrared satellite measurements , 2007 .
[66] R. Martin,et al. Space‐based constraints on the production of nitric oxide by lightning , 2007 .
[67] Katrin Fuhrer,et al. Field-deployable, high-resolution, time-of-flight aerosol mass spectrometer. , 2006, Analytical chemistry.
[68] Luis Kornblueh,et al. Sensitivity of Simulated Climate to Horizontal and Vertical Resolution in the ECHAM5 Atmosphere Model , 2006 .
[69] M. Chipperfield,et al. New version of the TOMCAT/SLIMCAT off‐line chemical transport model: Intercomparison of stratospheric tracer experiments , 2006 .
[70] S. Martin,et al. Crystallization pathways of sulfate-nitrate-ammonium aerosol particles. , 2005, The journal of physical chemistry. A.
[71] J. M. Reeves,et al. Particle Formation by Ion Nucleation in the Upper Troposphere and Lower Stratosphere , 2003, Science.
[72] A. Weinheimer,et al. Deep convection as a source of new particles in the midlatitude upper troposphere , 2002 .
[73] M. Molina,et al. Heterogeneous Freezing of Aqueous Particles Induced by Crystallized (NH4)2SO4, Ice, and Letovicite , 2001 .
[74] Scot T. Martin,et al. Phase Transitions of Aqueous Atmospheric Particles. , 2000, Chemical reviews.
[75] B. Luo,et al. Water activity as the determinant for homogeneous ice nucleation in aqueous solutions , 2000, Nature.
[76] Kenneth A. Smith,et al. Development of an Aerosol Mass Spectrometer for Size and Composition Analysis of Submicron Particles , 2000 .
[77] J. Abbatt,et al. Infrared Observations of the Response of NaCl, MgCl2, NH4HSO4, and NH4NO3 Aerosols to Changes in Relative Humidity from 298 to 238 K , 2000 .
[78] A. Clarke,et al. Nucleation in the equatorial free troposphere: Favorable environments during PEM‐Tropics , 1999 .
[79] James M. Hoell,et al. Pacific Exploratory Mission in the tropical Pacific: PEM-Tropics A, August-September 1996 , 1999 .
[80] Barry J. Huebert,et al. International Global Atmospheric Chemistry (IGAC) Project's First Aerosol Characterization Experiment (ACE 1): Overview , 1998 .
[81] D. Oxtoby,et al. A general relation between the nucleation work and the size of the nucleus in multicomponent nucleation , 1994 .
[82] Frank Arnold,et al. Gaseous Sulfuric Acid and Sulfur Dioxide Measurements in the Arctic Troposphere and Lower Stratosphere: Implications for Hydroxyl Radical Abundances , 1992 .
[83] D. Rogers. Development of a continuous flow thermal gradient diffusion chamber for ice nucleation studies , 1988 .
[84] P. Mcmurry,et al. Gas and aerosol wall losses in Teflon film smog chambers. , 1985, Environmental science & technology.
[85] P. Winkler,et al. JournalofGeophysicalResearch : Atmospheres Causes and importance of new particle formation in the present-day and preindustrial atmospheres , 2017 .
[86] T. Schiebel. Ice Nucleation Activity of Soil Dust Aerosols , 2017 .
[87] T. Tuch,et al. Mobility particle size spectrometers : harmonization of technical standards and data structure to facilitate high quality long-term observations of atmospheric particle number size distributions , 2012 .
[88] Atmospheric Chemistry and Physics Atmospheric ions and nucleation: a review of observations , 2011 .
[89] J. Williams,et al. Application of the variability-size relationship to atmospheric aerosol studies: estimating aerosol lifetimes and ages , 2002 .