Space-based observations of fire NO<sub>x</sub> emission coefficients: a global biome-scale comparison

Biomass burning represents both a significant and highly variable source of NO<sub>x</sub> to the atmosphere. This variability stems from both the episodic nature of fires, and from fire conditions such as the modified combustion efficiency of the fire, the nitrogen content of the fuel a...

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Main Authors: A. K. Mebust, R. C. Cohen
Format: Article
Language:English
Published: Copernicus Publications 2014-03-01
Series:Atmospheric Chemistry and Physics
Online Access:http://www.atmos-chem-phys.net/14/2509/2014/acp-14-2509-2014.pdf
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spelling doaj-5fd1c9611bcf4ff1a94ddcb07b2d12032020-11-24T22:38:49ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242014-03-011452509252410.5194/acp-14-2509-2014Space-based observations of fire NO<sub>x</sub> emission coefficients: a global biome-scale comparisonA. K. Mebust0R. C. Cohen1Department of Chemistry, University of California at Berkeley, Berkeley, California, USADepartment of Chemistry, University of California at Berkeley, Berkeley, California, USABiomass burning represents both a significant and highly variable source of NO<sub>x</sub> to the atmosphere. This variability stems from both the episodic nature of fires, and from fire conditions such as the modified combustion efficiency of the fire, the nitrogen content of the fuel and possibly other factors that have not been identified or evaluated by comparison with observations. Satellite instruments offer an opportunity to observe emissions from wildfires, providing a large suite of measurements which allow us to study mean behavior and variability on the regional scale in a statistically rigorous manner. Here we use space-based measurements of fire radiative power from the Moderate Resolution Imaging Spectroradiometer in combination with NO<sub>2</sub> tropospheric column densities from the Ozone Monitoring Instrument to measure mean emission coefficients (ECs in g NO MJ<sup>&minus;1</sup>) from fires for global biomes, and across a wide range of smaller-scale ecoregions, defined as spatially-distinct clusters of fires with similar fuel type. Mean ECs for all biomes fall between 0.250–0.362 g NO MJ<sup>−1</sup>, a range that is smaller than found in previous studies of biome-scale emission factors. The majority of ecoregion ECs fall within or near this range, implying that under most conditions, mean fire emissions of NO<sub>x</sub> per unit energy are similar between different regions regardless of fuel type or spatial variability. In contrast to these similarities, we find that about 24% of individual ecoregion ECs deviate significantly (with 95% confidence) from the mean EC for the associated biome, and a similar number of ecoregion ECs falls outside the range of all mean biome ECs, implying that there are some regions where fuel type-specific global emission parameterizations fail to capture local fire NO<sub>x</sub> emissions.http://www.atmos-chem-phys.net/14/2509/2014/acp-14-2509-2014.pdf
collection DOAJ
language English
format Article
sources DOAJ
author A. K. Mebust
R. C. Cohen
spellingShingle A. K. Mebust
R. C. Cohen
Space-based observations of fire NO<sub>x</sub> emission coefficients: a global biome-scale comparison
Atmospheric Chemistry and Physics
author_facet A. K. Mebust
R. C. Cohen
author_sort A. K. Mebust
title Space-based observations of fire NO<sub>x</sub> emission coefficients: a global biome-scale comparison
title_short Space-based observations of fire NO<sub>x</sub> emission coefficients: a global biome-scale comparison
title_full Space-based observations of fire NO<sub>x</sub> emission coefficients: a global biome-scale comparison
title_fullStr Space-based observations of fire NO<sub>x</sub> emission coefficients: a global biome-scale comparison
title_full_unstemmed Space-based observations of fire NO<sub>x</sub> emission coefficients: a global biome-scale comparison
title_sort space-based observations of fire no<sub>x</sub> emission coefficients: a global biome-scale comparison
publisher Copernicus Publications
series Atmospheric Chemistry and Physics
issn 1680-7316
1680-7324
publishDate 2014-03-01
description Biomass burning represents both a significant and highly variable source of NO<sub>x</sub> to the atmosphere. This variability stems from both the episodic nature of fires, and from fire conditions such as the modified combustion efficiency of the fire, the nitrogen content of the fuel and possibly other factors that have not been identified or evaluated by comparison with observations. Satellite instruments offer an opportunity to observe emissions from wildfires, providing a large suite of measurements which allow us to study mean behavior and variability on the regional scale in a statistically rigorous manner. Here we use space-based measurements of fire radiative power from the Moderate Resolution Imaging Spectroradiometer in combination with NO<sub>2</sub> tropospheric column densities from the Ozone Monitoring Instrument to measure mean emission coefficients (ECs in g NO MJ<sup>&minus;1</sup>) from fires for global biomes, and across a wide range of smaller-scale ecoregions, defined as spatially-distinct clusters of fires with similar fuel type. Mean ECs for all biomes fall between 0.250–0.362 g NO MJ<sup>−1</sup>, a range that is smaller than found in previous studies of biome-scale emission factors. The majority of ecoregion ECs fall within or near this range, implying that under most conditions, mean fire emissions of NO<sub>x</sub> per unit energy are similar between different regions regardless of fuel type or spatial variability. In contrast to these similarities, we find that about 24% of individual ecoregion ECs deviate significantly (with 95% confidence) from the mean EC for the associated biome, and a similar number of ecoregion ECs falls outside the range of all mean biome ECs, implying that there are some regions where fuel type-specific global emission parameterizations fail to capture local fire NO<sub>x</sub> emissions.
url http://www.atmos-chem-phys.net/14/2509/2014/acp-14-2509-2014.pdf
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