Articles | Volume 16, issue 12
https://doi.org/10.5194/acp-16-7623-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/acp-16-7623-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
The lifetime of nitrogen oxides in an isoprene-dominated forest
Paul S. Romer
Department of Chemistry, University of California at Berkeley, Berkeley, CA, USA
Kaitlin C. Duffey
Department of Chemistry, University of California at Berkeley, Berkeley, CA, USA
Paul J. Wooldridge
Department of Chemistry, University of California at Berkeley, Berkeley, CA, USA
Hannah M. Allen
Department of Chemistry, Reed College, Portland, OR, USA
Division of Chemistry and Chemical Engineering, California Institute of Technology, Pasadena, CA, USA
Benjamin R. Ayres
Department of Chemistry, Reed College, Portland, OR, USA
Steven S. Brown
Chemical Sciences Division, Earth System Research Laboratory, National Oceanic and Atmospheric Administration, Boulder, CO, USA
William H. Brune
Department of Meteorology, Pennsylvania State University, University Park, PA, USA
John D. Crounse
Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, CA, USA
Joost de Gouw
Chemical Sciences Division, Earth System Research Laboratory, National Oceanic and Atmospheric Administration, Boulder, CO, USA
Cooperative Institute for Research in Environmental Sciences, University of Colorado, Boulder, CO, USA
Danielle C. Draper
Department of Chemistry, Reed College, Portland, OR, USA
Department of Chemistry, University of California, Irvine, CA, USA
Philip A. Feiner
Department of Meteorology, Pennsylvania State University, University Park, PA, USA
Juliane L. Fry
Department of Chemistry, Reed College, Portland, OR, USA
Allen H. Goldstein
Department of Civil and Environmental Engineering, University of California at Berkeley, Berkeley, CA, USA
Department of Environmental Science, Policy and Management, University of California at Berkeley, Berkeley, CA, USA
Abigail Koss
Chemical Sciences Division, Earth System Research Laboratory, National Oceanic and Atmospheric Administration, Boulder, CO, USA
Cooperative Institute for Research in Environmental Sciences, University of Colorado, Boulder, CO, USA
Pawel K. Misztal
Department of Environmental Science, Policy and Management, University of California at Berkeley, Berkeley, CA, USA
Tran B. Nguyen
Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, CA, USA
Department of Environmental Toxicology, University of California, Davis, CA, USA
Kevin Olson
Department of Environmental Science, Policy and Management, University of California at Berkeley, Berkeley, CA, USA
Alex P. Teng
Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, CA, USA
Paul O. Wennberg
Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, CA, USA
Division of Engineering and Applied Science, California Institute of Technology, Pasadena, CA, USA
Robert J. Wild
Chemical Sciences Division, Earth System Research Laboratory, National Oceanic and Atmospheric Administration, Boulder, CO, USA
Cooperative Institute for Research in Environmental Sciences, University of Colorado, Boulder, CO, USA
Li Zhang
Department of Meteorology, Pennsylvania State University, University Park, PA, USA
Department of Chemistry, University of California at Berkeley, Berkeley, CA, USA
Department of Earth and Planetary Sciences, University of California at Berkeley, Berkeley, CA, USA
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Short summary
The lifetime of nitrogen oxides (NOx) is evaluated by analysis of field measurements from the southeastern United States. At warm temperatures in the daytime boundary layer, NOx interconverts rapidly with both PAN and alkyl and multifunctional nitrates (RONO2), and the relevant lifetime is the combined lifetime of these three classes. We find that the production of RONO2, followed by hydrolysis to produce nitric acid, is the dominant pathway for NOx removal in an isoprene dominated forest.
The lifetime of nitrogen oxides (NOx) is evaluated by analysis of field measurements from the...
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