Articles | Volume 24, issue 19
https://doi.org/10.5194/acp-24-11365-2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/acp-24-11365-2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Global modeling of aerosol nucleation with a semi-explicit chemical mechanism for highly oxygenated organic molecules (HOMs)
Xinyue Shao
School of Atmospheric Science, Nanjing University, Nanjing, 210023, China
Joint International Research Laboratory of Atmospheric and Earth System Sciences & Institute for Climate and Global Change Research, Nanjing University, Nanjing, 210023, China
School of Atmospheric Science, Nanjing University, Nanjing, 210023, China
Joint International Research Laboratory of Atmospheric and Earth System Sciences & Institute for Climate and Global Change Research, Nanjing University, Nanjing, 210023, China
School of Atmospheric Science, Nanjing University, Nanjing, 210023, China
Joint International Research Laboratory of Atmospheric and Earth System Sciences & Institute for Climate and Global Change Research, Nanjing University, Nanjing, 210023, China
Frontiers Science Center for Critical Earth Material Cycling, Nanjing University, Nanjing, China
Yaman Liu
School of Atmospheric Science, Nanjing University, Nanjing, 210023, China
Zhejiang Institute of Meteorological Sciences, Hangzhou, 310008, China
Wenxiang Shen
School of Atmospheric Science, Nanjing University, Nanjing, 210023, China
Joint International Research Laboratory of Atmospheric and Earth System Sciences & Institute for Climate and Global Change Research, Nanjing University, Nanjing, 210023, China
Stephen R. Arnold
Institute for Climate and Atmospheric Science, School of Earth and Environment, University of Leeds, Leeds, LS2 9JT, UK
Leighton A. Regayre
Institute for Climate and Atmospheric Science, School of Earth and Environment, University of Leeds, Leeds, LS2 9JT, UK
Met Office Hadley Centre, Exeter, Fitzroy Road, Exeter, Devon, EX1 3PB, UK
Centre for Environmental Modelling and Computation, School of Earth and Environment, University of Leeds, Leeds, LS2 9JT, UK
Meinrat O. Andreae
Max Planck Institute for Chemistry, 55020 Mainz, Germany
Scripps Institution of Oceanography, University of California, San Diego, La Jolla, CA, USA
Mira L. Pöhlker
Max Planck Institute for Chemistry, 55020 Mainz, Germany
Leipzig Institute for Meteorology, Universität Leipzig, 04103 Leipzig, Germany
Experimental Aerosol and Cloud Microphysics Department, Leibniz Institute for Tropospheric Research, 04318 Leipzig, Germany
Duseong S. Jo
Atmospheric Chemistry Observations and Modeling Laboratory, National Center for Atmospheric Research, Boulder, CO 80103, USA
now at: Department of Earth System Science Education, Seoul National University, Seoul, 999 007, South Korea
School of Atmospheric Science, Nanjing University, Nanjing, 210023, China
Zhejiang Institute of Meteorological Sciences, Hangzhou, 310008, China
Ken S. Carslaw
Institute for Climate and Atmospheric Science, School of Earth and Environment, University of Leeds, Leeds, LS2 9JT, UK
Data sets
Particle number concentrations measured by CPC and UHSAS during the ACRIDICON-CHUVA campaign in 2014 Meinrat O. Andreae https://halo-db.pa.op.dlr.de/mission/5
Short summary
Highly oxygenated organic molecules (HOMs) play an important role in atmospheric new particle formation (NPF). By semi-explicitly coupling the chemical mechanism of HOMs and a comprehensive nucleation scheme in a global climate model, the updated model shows better agreement with measurements of nucleation rate, growth rate, and NPF event frequency. Our results reveal that HOM-driven NPF leads to a considerable increase in particle and cloud condensation nuclei burden globally.
Highly oxygenated organic molecules (HOMs) play an important role in atmospheric new particle...
Altmetrics
Final-revised paper
Preprint