Abstract

Abstract. Biomass burning emission inventories serve as critical input for atmospheric chemical transport models that are used to understand the role of biomass fires in the chemical composition of the atmosphere, air quality, and the climate system. Significant progress has been achieved in the development of regional and global biomass burning emission inventories over the past decade using satellite remote sensing technology for fire detection and burned area mapping. However, agreement among biomass burning emission inventories is frequently poor. Furthermore, the uncertainties of the emission estimates are typically not well characterized, particularly at the spatio-temporal scales pertinent to regional air quality modeling. We present the Wildland Fire Emission Inventory (WFEI), a high resolution model for non-agricultural open biomass burning (hereafter referred to as wildland fires, WF) in the contiguous United States (CONUS). The model combines observations from the MODerate Resolution Imaging Spectroradiometer (MODIS) sensors on the Terra and Aqua satellites, meteorological analyses, fuel loading maps, an emission factor database, and fuel condition and fuel consumption models to estimate emissions from WF. WFEI was used to estimate emissions of CO (ECO) and PM2.5 (EPM2.5) for the western United States from 2003–2008. The uncertainties in the inventory estimates of ECO and EPM2.5 (uECO and uEPM2.5, respectively) have been explored across spatial and temporal scales relevant to regional and global modeling applications. In order to evaluate the uncertainty in our emission estimates across multiple scales we used a figure of merit, the half mass uncertainty, ũEX (where X = CO or PM2.5), defined such that for a given aggregation level 50% of total emissions occurred from elements with uEX ũEX. The sensitivity of the WFEI estimates of ECO and EPM2.5 to uncertainties in mapped fuel loading, fuel consumption, burned area and emission factors have also been examined. The estimated annual, domain wide ECO ranged from 436 Gg yr−1 in 2004 to 3107 Gg yr−1 in 2007. The extremes in estimated annual, domain wide EPM2.5 were 65 Gg yr−1 in 2004 and 454 Gg yr−1 in 2007. Annual WF emissions were a significant share of total emissions from non-WF sources (agriculture, dust, non-WF fire, fuel combustion, industrial processes, transportation, solvent, and miscellaneous) in the western United States as estimated in a national emission inventory. In the peak fire year of 2007, WF emissions were ~20% of total (WF + non-WF) CO emissions and ~39% of total PM2.5 emissions. During the months with the greatest fire activity, WF accounted for the majority of total CO and PM2.5 emitted across the study region. Uncertainties in annual, domain wide emissions was 28% to 51% for CO and 40% to 65% for PM2.5. Sensitivity of ũECO and ũEPM2.5 to the emission model components depended on scale. At scales relevant to regional modeling applications (Δx = 10 km, Δt = 1 day) WFEI estimates 50% of total ECO with an uncertainty <133% and half of total EPM2.5 with an uncertainty <146%. ũECO and ũEPM2.5 are reduced by more than half at the scale of global modeling applications (Δ x = 100 km, Δ t = 30 day) where 50% of total emissions are estimated with an uncertainty <50% for CO and <64% for PM2.5. Uncertainties in the estimates of burned area drives the emission uncertainties at regional scales. At global scales ũECO is most sensitive to uncertainties in the fuel load consumed while the uncertainty in the emission factor for PM2.5 plays the dominant role in ũEPM2.5. Our analysis indicates that the large scale aggregate uncertainties (e.g. the uncertainty in annual CO emitted for CONUS) typically reported for biomass burning emission inventories may not be appropriate for evaluating and interpreting results of regional scale modeling applications that employ the emission estimates. When feasible, biomass burning emission inventories should be evaluated and reported across the scales for which they are intended to be used.

Highlights

  • Biomass burning (BB; defined here as open biomass burning which includes wildfires and managed fires in forests, savannas, grasslands, and shrublands, and agricultural fire such the burning of crop residue) is a significant source of global trace gases and particles

  • Our analysis indicates that the large scale aggregate uncertainties typically reported for biomass burning emission inventories may not be appropriate for evaluating and interpreting results of regional

  • The air quality impacts occur through the emission of primary pollutants and production of secondary pollutants (e.g. O3 and secondary organic aerosol) when nonmethane organic compounds (NMOC) and nitrogen oxides released by biomass fires undergo photochemical processing

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Summary

Introduction

Biomass burning (BB; defined here as open biomass burning which includes wildfires and managed fires in forests, savannas, grasslands, and shrublands, and agricultural fire such the burning of crop residue) is a significant source of global trace gases and particles (van der Werf et al, 2010; Michel et al, 2005; Ito and Penner, 2004). Biomass fire emissions comprise a substantial component of the total global source of carbon monoxide (40 %), carbonaceous aerosol (35 %), and nitrogen oxides (20 %) (Langmann et al, 2009). Other primary BB emissions include greenhouse gases (CO2, CH4, N2O) and a vast array of photochemically reactive nonmethane organic compounds (NMOC; Akagi et al, 2011) that contribute to the production of ozone (O3) and secondary organic aerosol (Alvarado et al, 2009; Pfister et al, 2008; Sudo and Akimoto, 2007). The air quality impacts occur through the emission of primary pollutants (e.g. fine particulate matter; PM2.5) and production of secondary pollutants (e.g. O3 and secondary organic aerosol) when NMOC and nitrogen oxides released by biomass fires undergo photochemical processing. Air quality can be impacted by the transport and transformation of BB emissions on local (Muhle et al, 2007; Phuleria et al, 2005), regional (Spracklen et al, 2007; Sapkota et al, 2005; DeBell et al, 2004), and continental (Morris et al, 2006) scales

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