Articles | Volume 15, issue 6
https://doi.org/10.5194/acp-15-3575-2015
© 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-15-3575-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
31 Mar 2015
Research article |
| 31 Mar 2015
Multi-model study of chemical and physical controls on transport of anthropogenic and biomass burning pollution to the Arctic
Institute for Climate and Atmospheric Science, School of Earth and Environment, University of Leeds, Leeds, UK
now at: Cooperative Institute for Research in Environmental Sciences, University of Colorado Boulder, Boulder, Colorado, USA
now at: Chemical Sciences Division, NOAA Earth System Research Laboratory, Boulder, Colorado, USA
S. R. Arnold
Institute for Climate and Atmospheric Science, School of Earth and Environment, University of Leeds, Leeds, UK
L. K. Emmons
National Center for Atmospheric Research, Boulder, Colorado, USA
K. S. Law
Sorbonne Universités, UPMC Univ. Paris 06, Université Versailles St-Quentin, CNRS/INSU, LATMOS-IPSL, Paris, France
S. Turquety
Laboratoire de Météorologie Dynamique, IPSL, CNRS, UMR8539, 91128 Palaiseau CEDEX, France
B. N. Duncan
NASA Goddard Space Flight Center, Greenbelt, USA
J. Flemming
European Centre for Medium range Weather Forecasting, Reading, UK
V. Huijnen
Royal Netherlands Meteorological Institute (KNMI), De Bilt, the Netherlands
S. Tilmes
National Center for Atmospheric Research, Boulder, Colorado, USA
J. Langner
Swedish Meteorological and Hydrological Institute, 60176 Norrköping, Sweden
Program in Atmospheric and Oceanic Sciences, Princeton University and Geophysical Fluid Dynamics Laboratory/National Oceanic and Atmospheric Administration, Princeton, New Jersey, USA
Y. Long
Laboratoire de Météorologie Dynamique, IPSL, CNRS, UMR8539, 91128 Palaiseau CEDEX, France
J. L. Thomas
Sorbonne Universités, UPMC Univ. Paris 06, Université Versailles St-Quentin, CNRS/INSU, LATMOS-IPSL, Paris, France
S. D. Steenrod
NASA Goddard Space Flight Center, Greenbelt, USA
J. C. Raut
Sorbonne Universités, UPMC Univ. Paris 06, Université Versailles St-Quentin, CNRS/INSU, LATMOS-IPSL, Paris, France
C. Wilson
Institute for Climate and Atmospheric Science, School of Earth and Environment, University of Leeds, Leeds, UK
M. P. Chipperfield
Institute for Climate and Atmospheric Science, School of Earth and Environment, University of Leeds, Leeds, UK
G. S. Diskin
Chemistry and Dynamics Branch, NASA Langley Research Center, Hampton, VA, USA
A. Weinheimer
National Center for Atmospheric Research, Boulder, Colorado, USA
H. Schlager
Deutsches Zentrum für Luft- und Raumfahrt (DLR), Institute of Atmospheric Physics, Oberpfaffenhofen, Germany
G. Ancellet
Sorbonne Universités, UPMC Univ. Paris 06, Université Versailles St-Quentin, CNRS/INSU, LATMOS-IPSL, Paris, France
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Short summary
Multi-model simulations of Arctic CO, O3 and OH are evaluated using observations. Models show highly variable concentrations but the relative importance of emission regions and types is robust across the models, demonstrating the importance of biomass burning as a source. Idealised tracer experiments suggest that some of the model spread is due to variations in simulated transport from Europe in winter and from Asia throughout the year.
Multi-model simulations of Arctic CO, O3 and OH are evaluated using observations. Models show...
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