Articles | Volume 15, issue 11
https://doi.org/10.5194/acp-15-6047-2015
© Author(s) 2015. 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-15-6047-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Biomass burning influence on high-latitude tropospheric ozone and reactive nitrogen in summer 2008: a multi-model analysis based on POLMIP simulations
Institute for Climate and Atmospheric Science, School of Earth & Environment, University of Leeds, UK
L. K. Emmons
Atmospheric Chemistry Division, NCAR, Boulder, CO, USA
S. A. Monks
Institute for Climate and Atmospheric Science, School of Earth & Environment, University of Leeds, UK
K. S. Law
UPMC Univ. Paris 06, Université Versailles St-Quentin; CNRS/INSU, UMR 8190, Paris, France
D. A. Ridley
Department of Civil and Environmental Engineering, Massachusetts Institute of Technology, Cambridge, MA, USA
S. Turquety
Laboratoire de Météorologie Dynamique, IPSL, CNRS, UMR8539, 91128 Palaiseau CEDEX, France
S. Tilmes
Atmospheric Chemistry Division, NCAR, Boulder, CO, USA
J. L. Thomas
UPMC Univ. Paris 06, Université Versailles St-Quentin; CNRS/INSU, UMR 8190, Paris, France
I. Bouarar
UPMC Univ. Paris 06, Université Versailles St-Quentin; CNRS/INSU, UMR 8190, Paris, France
J. Flemming
ECMWF, Reading, UK
V. Huijnen
Royal Netherlands Meteorological Institute (KNMI), De Bilt, the Netherlands
Program in Atmospheric and Oceanic Sciences, Princeton University and Geophysical Fluid Dynamics Laboratory/National Oceanic and Atmospheric Administration, Princeton, NJ, USA
B. N. Duncan
NASA Goddard Space Flight Center, Greenbelt, MD, USA
S. Steenrod
NASA Goddard Space Flight Center, Greenbelt, MD, USA
Y. Yoshida
NASA Goddard Space Flight Center, Greenbelt, MD, USA
J. Langner
Swedish Meteorological and Hydrological Institute, 60176 Norrköping, Sweden
Y. Long
Laboratoire de Météorologie Dynamique, IPSL, CNRS, UMR8539, 91128 Palaiseau CEDEX, France
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Short summary
The extent to which forest fires produce the air pollutant and greenhouse gas ozone (O3) in the atmosphere at high latitudes in not well understood. We have compared how fire emissions produce O3 and its precursors in several models of atmospheric chemistry. We find enhancements in O3 in air dominated by fires in all models, which increase on average as fire emissions age. We also find that in situ O3 production in the Arctic is sensitive to details of organic chemistry and vertical lifting.
The extent to which forest fires produce the air pollutant and greenhouse gas ozone (O3) in the...
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