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JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 112, D10S43, doi:10.1029/2006JD007563, 2007

Forest fire plumes over the North Atlantic: p-TOMCAT model simulations with aircraft and satellite measurements from the ITOP/ICARTT campaign

Peter A. Cook

Centre for Atmospheric Science, Department of Chemistry, University of Cambridge, Cambridge, UK


Nicholas H. Savage

Centre for Atmospheric Science, Department of Chemistry, University of Cambridge, Cambridge, UK
Atmospheric Chemistry Modelling Support Unit, National Environment Research Council Centres for Atmospheric Sciences, University of Cambridge, Cambridge, UK


Solène Turquety

Atmospheric Chemistry Modeling Group, Harvard University, Cambridge, Massachusetts, USA


Glenn D. Carver

Centre for Atmospheric Science, Department of Chemistry, University of Cambridge, Cambridge, UK
Atmospheric Chemistry Modelling Support Unit, National Environment Research Council Centres for Atmospheric Sciences, University of Cambridge, Cambridge, UK


Fiona M. O'Connor

Centre for Atmospheric Science, Department of Chemistry, University of Cambridge, Cambridge, UK


Andreas Heckel

Institute of Environmental Physics, University of Bremen, Bremen, Germany


David Stewart

School of Environmental Sciences, University of East Anglia, Norwich, UK


Lisa K. Whalley

School of Chemistry, University of Leeds, Leeds, UK


Alex E. Parker

Department of Chemistry, University of Leicester, Leicester, UK


Hans Schlager

Institut fuer Physik der Atmosphaere, Deutsches Zentrum fuer Luft- und Raumfahrt, Oberpfaffenhofen, Germany


Hanwant B. Singh

NASA Ames Research Center, Moffett Field, California, USA


Melody A. Avery

NASA Langley Research Center, Hampton, Virginia, USA


Glen W. Sachse

NASA Langley Research Center, Hampton, Virginia, USA


William Brune

Department of Meteorology, Pennsylvania State University, University Park, Pennsylvania, USA


Andreas Richter

Institute of Environmental Physics, University of Bremen, Bremen, Germany


John P. Burrows

Institute of Environmental Physics, University of Bremen, Bremen, Germany


Ruth Purvis

Facility of Airborne Atmospheric Measurements, Cranfield, UK


Alastair C. Lewis

Department of Chemistry, University of York, York, UK


Claire E. Reeves

School of Environmental Sciences, University of East Anglia, Norwich, UK


Paul S. Monks

Department of Chemistry, University of Leicester, Leicester, UK


James G. Levine

Centre for Atmospheric Science, Department of Chemistry, University of Cambridge, Cambridge, UK


John A. Pyle

Centre for Atmospheric Science, Department of Chemistry, University of Cambridge, Cambridge, UK
Atmospheric Chemistry Modelling Support Unit, National Environment Research Council Centres for Atmospheric Sciences, University of Cambridge, Cambridge, UK


Abstract

Intercontinental Transport of Ozone and Precursors (ITOP) (part of International Consortium for Atmospheric Research on Transport and Transformation (ICARTT)) was an intense research effort to measure long-range transport of pollution across the North Atlantic and its impact on O3 production. During the aircraft campaign plumes were encountered containing large concentrations of CO plus other tracers and aerosols from forest fires in Alaska and Canada. A chemical transport model, p-TOMCAT, and new biomass burning emissions inventories are used to study the emissions long-range transport and their impact on the troposphere O3 budget. The fire plume structure is modeled well over long distances until it encounters convection over Europe. The CO values within the simulated plumes closely match aircraft measurements near North America and over the Atlantic and have good agreement with MOPITT CO data. O3 and NOx values were initially too great in the model plumes. However, by including additional vertical mixing of O3 above the fires, and using a lower NO2/CO emission ratio (0.008) for boreal fires, O3 concentrations are reduced closer to aircraft measurements, with NO2 closer to SCIAMACHY data. Too little PAN is produced within the simulated plumes, and our VOC scheme's simplicity may be another reason for O3 and NOx model-data discrepancies. In the p-TOMCAT simulations the fire emissions lead to increased tropospheric O3 over North America, the north Atlantic and western Europe from photochemical production and transport. The increased O3 over the Northern Hemisphere in the simulations reaches a peak in July 2004 in the range 2.0 to 6.2 Tg over a baseline of about 150 Tg.

Received 26 May 2006; accepted 13 December 2006; published 25 April 2007.

Keywords: long-range transport; forest fires; ozone.

Index Terms: 0345 Atmospheric Composition and Structure: Pollution: urban and regional (0305, 0478, 4251); 0368 Atmospheric Composition and Structure: Troposphere: constituent transport and chemistry; 0365 Atmospheric Composition and Structure: Troposphere: composition and chemistry.


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Citation: Cook, P. A., et al. (2007), Forest fire plumes over the North Atlantic: p-TOMCAT model simulations with aircraft and satellite measurements from the ITOP/ICARTT campaign, J. Geophys. Res., 112, D10S43, doi:10.1029/2006JD007563.