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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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 |
work_keys_str_mv |
AT avasileva emissionratiosoftracegasesandparticlesforsiberianforestfiresonthebasisofmobilegroundobservations AT kmoiseenko emissionratiosoftracegasesandparticlesforsiberianforestfiresonthebasisofmobilegroundobservations AT askorokhod emissionratiosoftracegasesandparticlesforsiberianforestfiresonthebasisofmobilegroundobservations AT ibelikov emissionratiosoftracegasesandparticlesforsiberianforestfiresonthebasisofmobilegroundobservations AT vkopeikin emissionratiosoftracegasesandparticlesforsiberianforestfiresonthebasisofmobilegroundobservations AT olavrova emissionratiosoftracegasesandparticlesforsiberianforestfiresonthebasisofmobilegroundobservations AT olavrova emissionratiosoftracegasesandparticlesforsiberianforestfiresonthebasisofmobilegroundobservations |
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