Articles | Volume 23, issue 16
https://doi.org/10.5194/acp-23-9023-2023
© Author(s) 2023. 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-23-9023-2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Nighttime NO emissions strongly suppress chlorine and nitrate radical formation during the winter in Delhi
Sophie L. Haslett
CORRESPONDING AUTHOR
Department of Environmental Science, Stockholm University, Stockholm, Sweden
Bolin Centre for Climate Research, Stockholm University, Stockholm, Sweden
David M. Bell
Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232
Villigen PSI, Switzerland
Varun Kumar
Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232
Villigen PSI, Switzerland
now at: Institut National de l'Environnement Industriel et des
Risques (INERIS), Parc Technologique ALATA, 60550 Vemeuil-en-Halatte, France
Jay G. Slowik
Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232
Villigen PSI, Switzerland
Dongyu S. Wang
Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232
Villigen PSI, Switzerland
Suneeti Mishra
Department of Civil Engineering, Indian Institute of Technology
Kanpur, Kanpur, India
Neeraj Rastogi
Geosciences Division, Physical Research Laboratory, Ahmedabad, India
Atinderpal Singh
Geosciences Division, Physical Research Laboratory, Ahmedabad, India
now at: Department of Environmental Studies, University of Delhi,
Delhi 110007, India
Dilip Ganguly
Centre for Atmospheric Sciences, Indian Institute of Technology Delhi, New Delhi, India
Joel Thornton
Department of Atmospheric Sciences, University of Washington, Seattle, WA, USA
Feixue Zheng
Aerosol and Haze Laboratory, Beijing Advanced Innovation Centre for
Soft Matter Science and Engineering, Beijing University of Chemical Technology, Beijing 100029, China
Yuanyuan Li
Joint International Research Laboratory of Atmospheric and Earth
System Sciences, School of Atmospheric Sciences, Nanjing University, Nanjing 210023, China
Wei Nie
Joint International Research Laboratory of Atmospheric and Earth
System Sciences, School of Atmospheric Sciences, Nanjing University, Nanjing 210023, China
Yongchun Liu
Aerosol and Haze Laboratory, Beijing Advanced Innovation Centre for
Soft Matter Science and Engineering, Beijing University of Chemical Technology, Beijing 100029, China
Wei Ma
Aerosol and Haze Laboratory, Beijing Advanced Innovation Centre for
Soft Matter Science and Engineering, Beijing University of Chemical Technology, Beijing 100029, China
Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, Helsinki, Finland
Markku Kulmala
Aerosol and Haze Laboratory, Beijing Advanced Innovation Centre for
Soft Matter Science and Engineering, Beijing University of Chemical Technology, Beijing 100029, China
Joint International Research Laboratory of Atmospheric and Earth
System Sciences, School of Atmospheric Sciences, Nanjing University, Nanjing 210023, China
Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, Helsinki, Finland
Kaspar R. Daellenbach
Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, Helsinki, Finland
David Hadden
Department of Environmental Science, Stockholm University, Stockholm, Sweden
Bolin Centre for Climate Research, Stockholm University, Stockholm, Sweden
Urs Baltensperger
Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232
Villigen PSI, Switzerland
Andre S. H. Prevot
Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232
Villigen PSI, Switzerland
Sachchida N. Tripathi
CORRESPONDING AUTHOR
Department of Civil Engineering, Indian Institute of Technology
Kanpur, Kanpur, India
Department of Sustainable Energy Engineering, Indian Institute of Technology Kanpur, Kanpur, India
Department of Environmental Science, Stockholm University, Stockholm, Sweden
Bolin Centre for Climate Research, Stockholm University, Stockholm, Sweden
now at: Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232 Villigen PSI, Switzerland
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Cited
6 citations as recorded by crossref.
- Variation in chemical composition and volatility of oxygenated organic aerosol in different rural, urban, and mountain environments W. Huang et al. 10.5194/acp-24-2607-2024
- Significant chlorine emissions from biomass burning affect the long-term atmospheric chemistry in Asia D. Chang et al. 10.1093/nsr/nwae285
- Diurnal emission variation of ozone precursors: Impacts on ozone formation during Sep. 2019 Y. Tang et al. 10.1016/j.scitotenv.2024.172591
- Changing optical properties of black carbon and brown carbon aerosols during long-range transport from the Indo-Gangetic Plain to the equatorial Indian Ocean K. Budhavant et al. 10.5194/acp-24-11911-2024
- Comprehensive multiphase chlorine chemistry in the box model CAABA/MECCA: implications for atmospheric oxidative capacity M. Soni et al. 10.5194/acp-23-15165-2023
- Extreme Concentrations of Nitric Oxide Control Daytime Oxidation and Quench Nocturnal Oxidation Chemistry in Delhi during Highly Polluted Episodes B. Nelson et al. 10.1021/acs.estlett.3c00171
5 citations as recorded by crossref.
- Variation in chemical composition and volatility of oxygenated organic aerosol in different rural, urban, and mountain environments W. Huang et al. 10.5194/acp-24-2607-2024
- Significant chlorine emissions from biomass burning affect the long-term atmospheric chemistry in Asia D. Chang et al. 10.1093/nsr/nwae285
- Diurnal emission variation of ozone precursors: Impacts on ozone formation during Sep. 2019 Y. Tang et al. 10.1016/j.scitotenv.2024.172591
- Changing optical properties of black carbon and brown carbon aerosols during long-range transport from the Indo-Gangetic Plain to the equatorial Indian Ocean K. Budhavant et al. 10.5194/acp-24-11911-2024
- Comprehensive multiphase chlorine chemistry in the box model CAABA/MECCA: implications for atmospheric oxidative capacity M. Soni et al. 10.5194/acp-23-15165-2023
Latest update: 20 Nov 2024
Short summary
In Delhi, some aspects of daytime and nighttime atmospheric chemistry are inverted, and parodoxically, vehicle emissions may be limiting other forms of particle production. This is because the nighttime emissions of nitrogen oxide (NO) by traffic and biomass burning prevent some chemical processes that would otherwise create even more particles and worsen the urban haze.
In Delhi, some aspects of daytime and nighttime atmospheric chemistry are inverted, and...
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