A major regional air pollution event in the northeastern United States caused by extensive forest fires in Quebec, Canada

[1] During early July 2002, wildfires burned ∼1 × 106 ha of forest in Quebec, Canada. The resultant smoke plume was seen in satellite images blanketing the U.S. east coast. Concurrently, extremely high CO mixing ratios were observed at the Atmospheric Investigation, Regional Modeling, Analysis and Prediction (AIRMAP) network sites in New Hampshire and at the Harvard Forest Environmental Measurement Site (HFEMS) in Massachusetts. The CO enhancements were on the order of 525–1025 ppbv above low mixing ratio conditions on surrounding days. A biomass burning source for the event was confirmed by concomitant enhancements in aerosol K+, NH4+, NO3−, and C2O42− mixing ratios at the AIRMAP sites. Additional data for aerosol K, organic carbon, and elemental carbon from the Interagency Monitoring of Protected Visual Environments network and CO data from Environmental Protection Agency sites indicated that the smoke plume impacted much of the U.S. east coast, from Maine to Virginia. CO mixing ratios and K concentrations at stations with 10-year or longer records suggested that this was the largest biomass burning plume to impact the U.S. east coast in over a decade. Furthermore, CO mixing ratios and aerosol particles with diameters <2.5 μm (PM2.5) mass and scattering coefficients from the AIRMAP network and HFEMS indicated that this event was comparable to the large anthropogenic combustion and haze events which intermittently impact rural New England. The degree of enhancement of O3, NOy, NO3−, NH4+, and SO42− in the biomass plume showed significant variation with elevation and latitude that is attributed to variations in transport and surface depositional processes.

[1]  Zhanqing Li,et al.  Smoke over haze: Aircraft observations of chemical and optical properties and the effects on heating rates and stability , 2004 .

[2]  J. Dibb,et al.  Relationships between surface and column aerosol radiative properties and air mass transport at a rural New England site , 2004 .

[3]  J. Dibb,et al.  Asian dust storm events of spring 2001 and associated pollutants observed in New England by the Atmospheric Investigation, Regional Modeling, Analysis and Prediction (AIRMAP) monitoring network , 2004 .

[4]  X. Lee,et al.  Emission and long-range transport of gaseous mercury from a large-scale Canadian boreal forest fire. , 2003, Environmental science & technology.

[5]  P. Pilewskie,et al.  Evolution of gases and particles from a savanna fire in South Africa , 2003 .

[6]  P. Buseck,et al.  Individual aerosol particles from biomass burning in southern Africa: 2, Compositions and aging of inorganic particles , 2003 .

[7]  P. Formenti,et al.  The mean physical and optical properties of regional haze dominated by biomass burning aerosol measured from the C-130 aircraft during SAFARI 2000 , 2003 .

[8]  M. Khalil,et al.  Tracers of Wood Smoke , 2003 .

[9]  Gerhard Wotawa,et al.  Ozone production from Canadian wildfires during June and July of 1995 , 2002 .

[10]  J. Houghton,et al.  Climate change 2001 : the scientific basis , 2001 .

[11]  M. Andreae,et al.  Emission of trace gases and aerosols from biomass burning , 2001 .

[12]  O. Cooper,et al.  PROPHET 1998 meteorological overview and air‐mass classification , 2001 .

[13]  Ulla Wandinger,et al.  Transport of boreal forest fire emissions from Canada , 2001 .

[14]  W. Hao,et al.  Measurements of excess O3, CO2, CO, CH4, C2H4, C2H2, HCN, NO, NH3, HCOOH, CH3COOH, HCHO, and CH3OH in 1997 Alaskan biomass burning plumes by airborne Fourier transform infrared spectroscopy (AFTIR) , 2000 .

[15]  J. Lelieveld,et al.  Photochemistry of the African troposphere: Influence of biomass‐burning emissions , 2000 .

[16]  J. Cafmeyer,et al.  Biomass Burning in Southern Africa: Individual Particle Characterization of Atmospheric Aerosols and Savanna Fire Samples , 2000 .

[17]  Trainer,et al.  The influence of canadian forest fires on pollutant concentrations in the united states , 2000, Science.

[18]  G. Carmichael,et al.  Impacts of biomass burning on tropospheric CO, NOx, and O3 , 2000 .

[19]  Paulo Artaxo,et al.  Chemical composition of aerosol particles from direct emissions of vegetation fires in the Amazon Basin: water-soluble species and trace elements , 2000 .

[20]  J. Lacaux,et al.  Airborne aerosols over central Africa during the Experiment for Regional Sources and Sinks of Oxidants (EXPRESSO) , 1999 .

[21]  D. Blake,et al.  Emission factors of hydrocarbons, halocarbons, trace gases and particles from biomass burning in Brazil , 1998 .

[22]  W. Elbert,et al.  Airborne studies of aerosol emissions from savanna fires in , 1998 .

[23]  V. W. J. H. Kirchhoff,et al.  An internally consistent set of globally distributed atmospheric carbon monoxide mixing ratios developed using results from an intercomparison of measurements , 1998 .

[24]  J. Bradshaw,et al.  An update on reactive odd-nitrogen measurements made during recent NASA Global Tropospheric Experiment programs , 1998 .

[25]  Janet Nichol,et al.  Smoke haze in Southeast Asia. A predictable recurrence , 1998 .

[26]  John S. Holloway,et al.  Relationships between ozone and carbon monoxide at surface sites in the North Atlantic region , 1998 .

[27]  Susan G. Conard,et al.  Wildfire in Russian Boreal Forests—Potential Impacts of Fire Regime Characteristics on Emissions and Global Carbon Balance Estimates , 1997 .

[28]  Harold J. Annegarn,et al.  Regional atmospheric aerosol composition and sources in the eastern Transvaal, South Africa, and impact of biomass burning , 1996 .

[29]  W. Malm,et al.  Examining the relationship among atmospheric aerosols and light scattering and extinction in the Grand Canyon area , 1996 .

[30]  K. E. Moore,et al.  Atmospheric deposition of reactive nitrogen oxides and ozone in a temperate deciduous forest and a subarctic woodland , 1996 .

[31]  D. Jacob,et al.  Origin of tropospheric ozone at remote high northern latitudes in summer , 1996 .

[32]  J. McConnell,et al.  BIOMASS BURNING SIGNATURES IN THE ATMOSPHERE AND SNOW AT SUMMIT, GREENLAND: AN EVENT ON 5 AUGUST 1994 , 1996 .

[33]  P. Artaxo,et al.  Trace elements in tropical African savanna biomass burning aerosols , 1995 .

[34]  F. Fehsenfeld,et al.  Routine, continuous measurement of carbon monoxide with parts per billion precision. , 1994, Environmental science & technology.

[35]  M. Chin,et al.  Relationship of ozone and carbon monoxide over North America , 1994 .

[36]  W. Malm,et al.  Spatial and seasonal trends in particle concentration and optical extinction in the United States , 1994 .

[37]  L. Barrie,et al.  Chemical composition of the atmospheric aerosol in the troposphere over the Hudson Bay lowlands and Quebec-Labrador regions of Canada , 1994 .

[38]  D. Blake,et al.  Enhancement of acidic gases in biomass burning impacted air masses over Canada , 1994 .

[39]  W. Grant,et al.  Ozone and aerosol distributions in the summertime troposphere over Canada , 1994 .

[40]  D. Ward,et al.  Airborne measurements of gases and particles from an Alaskan wildfire , 1993 .

[41]  J. Martins,et al.  Case study of atmospheric measurements in Brazil : aerosol emissions from Amazon Basin fires , 1993 .

[42]  D. Jacob,et al.  Summertime photochemistry of the troposphere at high northern latitudes , 1992 .

[43]  Edward V. Browell,et al.  Atmospheric chemistry in the Arctic and subarctic: Influence of natural fires, industrial emissions, and stratospheric inputs , 1992 .

[44]  P. Crutzen,et al.  Biomass Burning in the Tropics: Impact on Atmospheric Chemistry and Biogeochemical Cycles , 1990, Science.

[45]  M. Andreae Soot Carbon and Excess Fine Potassium: Long-Range Transport of Combustion-Derived Aerosols , 1983, Science.