Emission ratios of trace gases and particles for Siberian forest fires on the basis of mobile ground observations

Boreal forest fires are currently recognized as a significant factor in climate change and air quality problems. Although emissions of biomass burning products are widely measured in many regions, there is still lack of information on the composition of wildfire emissions in Siberia, a region kn...

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Main Authors: A. Vasileva, K. Moiseenko, A. Skorokhod, I. Belikov, V. Kopeikin, O. Lavrova
Format: Article
Language:English
Published: Copernicus Publications 2017-10-01
Series:Atmospheric Chemistry and Physics
Online Access:https://www.atmos-chem-phys.net/17/12303/2017/acp-17-12303-2017.pdf
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spelling doaj-35fa0936a14e41a19bf9d64ab76626b82020-11-24T23:22:16ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242017-10-0117123031232510.5194/acp-17-12303-2017Emission ratios of trace gases and particles for Siberian forest fires on the basis of mobile ground observationsA. Vasileva0K. Moiseenko1A. Skorokhod2I. Belikov3V. Kopeikin4O. Lavrova5O. Lavrova6A.M. Obukhov Institute of Atmospheric Physics, Russian Academy of Sciences, Moscow, 119017, RussiaA.M. Obukhov Institute of Atmospheric Physics, Russian Academy of Sciences, Moscow, 119017, RussiaA.M. Obukhov Institute of Atmospheric Physics, Russian Academy of Sciences, Moscow, 119017, RussiaA.M. Obukhov Institute of Atmospheric Physics, Russian Academy of Sciences, Moscow, 119017, RussiaA.M. Obukhov Institute of Atmospheric Physics, Russian Academy of Sciences, Moscow, 119017, RussiaA.M. Obukhov Institute of Atmospheric Physics, Russian Academy of Sciences, Moscow, 119017, RussiaRussian Research Institute of Railway Transport, Moscow, 107996, RussiaBoreal forest fires are currently recognized as a significant factor in climate change and air quality problems. Although emissions of biomass burning products are widely measured in many regions, there is still lack of information on the composition of wildfire emissions in Siberia, a region known for its severe wildfire activity. Emission ratios (ERs) are important characteristics of wildfire emissions as they may be used to calculate the mass of species emitted into the atmosphere due to combustion of a known mass of biomass fuel. We analyze observations of carbon dioxide (CO<sub>2</sub>), carbon monoxide (CO), methane (CH<sub>4</sub>), total nonmethane hydrocarbons (NMHCs), nitrogen oxides NO<sub><i>x</i></sub> ( =  NO + NO<sub>2</sub>), particulate matter (PM<sub>3</sub>), and black carbon (BC) within two forest fire plume transects made by the moving railway observatory during TRanscontinental Observations Into the Chemistry of the Atmosphere (TROICA) expeditions. Slopes in linear regressions of excess levels of the pollutants are used to obtain ER<sub>CO ∕ CO<sub>2</sub></sub> = 10–15 %, ER<sub>CH<sub>4</sub> ∕ CO</sub> = 8–10 %, ER<sub>NMHC ∕ CO</sub> = 0.11–0.21 % ppmC ppmC<sup>−1</sup>, ER<sub>NO<sub><i>x</i></sub> ∕ CO</sub> = 1.5–3.0  ppb ppm<sup>−1</sup>, ER<sub>PM<sub>3</sub> ∕ CO</sub> = 320–385 ng m<sup>−3</sup> (µg m<sup>−3</sup>)<sup>−1</sup>, and ER<sub>BC ∕ CO</sub> =  6.1–6.3 µg m<sup>−3</sup> ppm<sup>−1</sup>, which fall within the range of uncertainty of the previous estimates, being at the higher edge for ER<sub>CH<sub>4</sub> ∕ CO</sub>, ER<sub>NMHC ∕ CO</sub>, and ER<sub>PM<sub>3</sub> ∕ CO</sub> and at the lower edge for ER<sub>NO<sub><i>x</i></sub> ∕ CO</sub>. The relative uncertainties comprise 5–15 % of the estimated ER<sub>CH<sub>4</sub> ∕ CO</sub>, ER<sub>NMHC ∕ CO</sub>, and ER<sub>PM ∕ CO</sub> and 10–20 % of ER<sub>NO<sub><i>x</i></sub> ∕ CO</sub>, ER<sub>CO ∕ CO<sub>2</sub></sub>, and ER<sub>BC ∕ CO</sub>. The uncertainties are lower than in many other similar studies and associated mainly with natural variability of wildfire emissions.https://www.atmos-chem-phys.net/17/12303/2017/acp-17-12303-2017.pdf
collection DOAJ
language English
format Article
sources DOAJ
author A. Vasileva
K. Moiseenko
A. Skorokhod
I. Belikov
V. Kopeikin
O. Lavrova
O. Lavrova
spellingShingle A. Vasileva
K. Moiseenko
A. Skorokhod
I. Belikov
V. Kopeikin
O. Lavrova
O. Lavrova
Emission ratios of trace gases and particles for Siberian forest fires on the basis of mobile ground observations
Atmospheric Chemistry and Physics
author_facet A. Vasileva
K. Moiseenko
A. Skorokhod
I. Belikov
V. Kopeikin
O. Lavrova
O. Lavrova
author_sort A. Vasileva
title Emission ratios of trace gases and particles for Siberian forest fires on the basis of mobile ground observations
title_short Emission ratios of trace gases and particles for Siberian forest fires on the basis of mobile ground observations
title_full Emission ratios of trace gases and particles for Siberian forest fires on the basis of mobile ground observations
title_fullStr Emission ratios of trace gases and particles for Siberian forest fires on the basis of mobile ground observations
title_full_unstemmed Emission ratios of trace gases and particles for Siberian forest fires on the basis of mobile ground observations
title_sort emission ratios of trace gases and particles for siberian forest fires on the basis of mobile ground observations
publisher Copernicus Publications
series Atmospheric Chemistry and Physics
issn 1680-7316
1680-7324
publishDate 2017-10-01
description Boreal forest fires are currently recognized as a significant factor in climate change and air quality problems. Although emissions of biomass burning products are widely measured in many regions, there is still lack of information on the composition of wildfire emissions in Siberia, a region known for its severe wildfire activity. Emission ratios (ERs) are important characteristics of wildfire emissions as they may be used to calculate the mass of species emitted into the atmosphere due to combustion of a known mass of biomass fuel. We analyze observations of carbon dioxide (CO<sub>2</sub>), carbon monoxide (CO), methane (CH<sub>4</sub>), total nonmethane hydrocarbons (NMHCs), nitrogen oxides NO<sub><i>x</i></sub> ( =  NO + NO<sub>2</sub>), particulate matter (PM<sub>3</sub>), and black carbon (BC) within two forest fire plume transects made by the moving railway observatory during TRanscontinental Observations Into the Chemistry of the Atmosphere (TROICA) expeditions. Slopes in linear regressions of excess levels of the pollutants are used to obtain ER<sub>CO ∕ CO<sub>2</sub></sub> = 10–15 %, ER<sub>CH<sub>4</sub> ∕ CO</sub> = 8–10 %, ER<sub>NMHC ∕ CO</sub> = 0.11–0.21 % ppmC ppmC<sup>−1</sup>, ER<sub>NO<sub><i>x</i></sub> ∕ CO</sub> = 1.5–3.0  ppb ppm<sup>−1</sup>, ER<sub>PM<sub>3</sub> ∕ CO</sub> = 320–385 ng m<sup>−3</sup> (µg m<sup>−3</sup>)<sup>−1</sup>, and ER<sub>BC ∕ CO</sub> =  6.1–6.3 µg m<sup>−3</sup> ppm<sup>−1</sup>, which fall within the range of uncertainty of the previous estimates, being at the higher edge for ER<sub>CH<sub>4</sub> ∕ CO</sub>, ER<sub>NMHC ∕ CO</sub>, and ER<sub>PM<sub>3</sub> ∕ CO</sub> and at the lower edge for ER<sub>NO<sub><i>x</i></sub> ∕ CO</sub>. The relative uncertainties comprise 5–15 % of the estimated ER<sub>CH<sub>4</sub> ∕ CO</sub>, ER<sub>NMHC ∕ CO</sub>, and ER<sub>PM ∕ CO</sub> and 10–20 % of ER<sub>NO<sub><i>x</i></sub> ∕ CO</sub>, ER<sub>CO ∕ CO<sub>2</sub></sub>, and ER<sub>BC ∕ CO</sub>. The uncertainties are lower than in many other similar studies and associated mainly with natural variability of wildfire emissions.
url https://www.atmos-chem-phys.net/17/12303/2017/acp-17-12303-2017.pdf
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