Emissions relationships in western forest fire plumes – Part 1: Reducing the effect of mixing errors on emission factors

<p>Studies of emission factors from biomass burning using aircraft data complement the results of lab studies and extend them to conditions of immense hot conflagrations. A new theoretical development of plume theory for multiple tracers is developed after examining aircraft samples. We illust...

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Main Authors: R. B. Chatfield, M. O. Andreae, ARCTAS Science Team
Format: Article
Language:English
Published: Copernicus Publications 2020-12-01
Series:Atmospheric Measurement Techniques
Online Access:https://amt.copernicus.org/articles/13/7069/2020/amt-13-7069-2020.pdf
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language English
format Article
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author R. B. Chatfield
M. O. Andreae
M. O. Andreae
ARCTAS Science Team
spellingShingle R. B. Chatfield
M. O. Andreae
M. O. Andreae
ARCTAS Science Team
Emissions relationships in western forest fire plumes – Part 1: Reducing the effect of mixing errors on emission factors
Atmospheric Measurement Techniques
author_facet R. B. Chatfield
M. O. Andreae
M. O. Andreae
ARCTAS Science Team
author_sort R. B. Chatfield
title Emissions relationships in western forest fire plumes – Part 1: Reducing the effect of mixing errors on emission factors
title_short Emissions relationships in western forest fire plumes – Part 1: Reducing the effect of mixing errors on emission factors
title_full Emissions relationships in western forest fire plumes – Part 1: Reducing the effect of mixing errors on emission factors
title_fullStr Emissions relationships in western forest fire plumes – Part 1: Reducing the effect of mixing errors on emission factors
title_full_unstemmed Emissions relationships in western forest fire plumes – Part 1: Reducing the effect of mixing errors on emission factors
title_sort emissions relationships in western forest fire plumes – part 1: reducing the effect of mixing errors on emission factors
publisher Copernicus Publications
series Atmospheric Measurement Techniques
issn 1867-1381
1867-8548
publishDate 2020-12-01
description <p>Studies of emission factors from biomass burning using aircraft data complement the results of lab studies and extend them to conditions of immense hot conflagrations. A new theoretical development of plume theory for multiple tracers is developed after examining aircraft samples. We illustrate and discuss emissions relationships for 422 individual samples from many forest fire plumes in the Western USA. Samples are from two NASA investigations: ARCTAS (Arctic Research of the Composition of the Troposphere from Aircraft and Satellites) and SEAC4RS (Studies of Emissions and Atmospheric Composition, Clouds and Climate Coupling by Regional Surveys). This work provides sample-by-sample enhancement ratios (EnRs) for 23 gases and particulate properties. Many EnRs provide candidates for emission ratios (ERs, corresponding to the EnR at the source) when the origin and degree of transformation is understood. From these, emission factors (EFs) can be estimated, provided the fuel dry mass consumed is known or can be estimated using the carbon mass budget approach. This analysis requires understanding the interplay of mixing of the plume with surrounding air. Some initial examples emphasize that measured <span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M1" display="inline" overflow="scroll" dspmath="mathml"><mrow><msub><mi>C</mi><mi mathvariant="normal">tot</mi></msub><mo>=</mo><mrow class="chem"><msub><mi mathvariant="normal">CO</mi><mn mathvariant="normal">2</mn></msub></mrow><mo>+</mo><mrow class="chem"><mi mathvariant="normal">CO</mi></mrow></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="81pt" height="13pt" class="svg-formula" dspmath="mathimg" md5hash="84305589fa4e90cbb65d6f0136852b6c"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="amt-13-7069-2020-ie00001.svg" width="81pt" height="13pt" src="amt-13-7069-2020-ie00001.png"/></svg:svg></span></span> in a fire plume does not necessarily describe the emissions of the total carbon liberated in the flames, <span class="inline-formula"><i>C</i><sub>burn</sub></span>. Rather, it represents <span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M3" display="inline" overflow="scroll" dspmath="mathml"><mrow><msub><mi>C</mi><mi mathvariant="normal">tot</mi></msub><mo>=</mo><msub><mi>C</mi><mi mathvariant="normal">burn</mi></msub><mo>+</mo><msub><mi>C</mi><mi mathvariant="normal">bkgd</mi></msub></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="92pt" height="14pt" class="svg-formula" dspmath="mathimg" md5hash="d7b80c67dccc42d28c3657949673d67e"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="amt-13-7069-2020-ie00002.svg" width="92pt" height="14pt" src="amt-13-7069-2020-ie00002.png"/></svg:svg></span></span>, which includes possibly varying background concentrations for entrained air. Consequently, we present a simple theoretical description for plume entrainment for multiple tracers from the flame tops to hundreds of kilometers downwind and illustrate some intrinsic linear behaviors. The analysis suggests a mixed-effects regression emission technique (MERET), which can eliminate occasional strong biases associated with the commonly used normalized excess mixing ratio (NEMR) method. MERET splits <span class="inline-formula"><i>C</i><sub>tot</sub></span> to reveal <span class="inline-formula"><i>C</i><sub>burn</sub></span> by exploiting the fact that <span class="inline-formula"><i>C</i><sub>burn</sub></span> and all tracers respond linearly to dilution, while each tracer has consistent EnR behavior (slope of tracer concentration with respect to <span class="inline-formula"><i>C</i><sub>burn</sub></span>). The two effects are separable. Two or three or preferably more emission indicators are required as a minimum; here we used eight. In summary, MERET allows a fine spatial resolution (EnRs for individual observations) and comparison of similar plumes that are distant in time and space. Alkene ratios provide us with an approximate photochemical timescale. This allows discrimination and definition, by fire situation, of ERs, allowing us to estimate emission factors.</p>
url https://amt.copernicus.org/articles/13/7069/2020/amt-13-7069-2020.pdf
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spelling doaj-ab662f3832a3473498267c4dfe7494492020-12-23T12:21:43ZengCopernicus PublicationsAtmospheric Measurement Techniques1867-13811867-85482020-12-01137069709610.5194/amt-13-7069-2020Emissions relationships in western forest fire plumes – Part 1: Reducing the effect of mixing errors on emission factorsR. B. Chatfield0M. O. Andreae1M. O. Andreae2ARCTAS Science TeamNASA Ames Research Center, Moffett Field, CA 94035, USAMax Planck Institute for Chemistry, P.O. Box 3060, 55020 Mainz, GermanyScripps Institution of Oceanography, UCSD, La Jolla, CA 92093, USA<p>Studies of emission factors from biomass burning using aircraft data complement the results of lab studies and extend them to conditions of immense hot conflagrations. A new theoretical development of plume theory for multiple tracers is developed after examining aircraft samples. We illustrate and discuss emissions relationships for 422 individual samples from many forest fire plumes in the Western USA. Samples are from two NASA investigations: ARCTAS (Arctic Research of the Composition of the Troposphere from Aircraft and Satellites) and SEAC4RS (Studies of Emissions and Atmospheric Composition, Clouds and Climate Coupling by Regional Surveys). This work provides sample-by-sample enhancement ratios (EnRs) for 23 gases and particulate properties. Many EnRs provide candidates for emission ratios (ERs, corresponding to the EnR at the source) when the origin and degree of transformation is understood. From these, emission factors (EFs) can be estimated, provided the fuel dry mass consumed is known or can be estimated using the carbon mass budget approach. This analysis requires understanding the interplay of mixing of the plume with surrounding air. Some initial examples emphasize that measured <span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M1" display="inline" overflow="scroll" dspmath="mathml"><mrow><msub><mi>C</mi><mi mathvariant="normal">tot</mi></msub><mo>=</mo><mrow class="chem"><msub><mi mathvariant="normal">CO</mi><mn mathvariant="normal">2</mn></msub></mrow><mo>+</mo><mrow class="chem"><mi mathvariant="normal">CO</mi></mrow></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="81pt" height="13pt" class="svg-formula" dspmath="mathimg" md5hash="84305589fa4e90cbb65d6f0136852b6c"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="amt-13-7069-2020-ie00001.svg" width="81pt" height="13pt" src="amt-13-7069-2020-ie00001.png"/></svg:svg></span></span> in a fire plume does not necessarily describe the emissions of the total carbon liberated in the flames, <span class="inline-formula"><i>C</i><sub>burn</sub></span>. Rather, it represents <span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M3" display="inline" overflow="scroll" dspmath="mathml"><mrow><msub><mi>C</mi><mi mathvariant="normal">tot</mi></msub><mo>=</mo><msub><mi>C</mi><mi mathvariant="normal">burn</mi></msub><mo>+</mo><msub><mi>C</mi><mi mathvariant="normal">bkgd</mi></msub></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="92pt" height="14pt" class="svg-formula" dspmath="mathimg" md5hash="d7b80c67dccc42d28c3657949673d67e"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="amt-13-7069-2020-ie00002.svg" width="92pt" height="14pt" src="amt-13-7069-2020-ie00002.png"/></svg:svg></span></span>, which includes possibly varying background concentrations for entrained air. Consequently, we present a simple theoretical description for plume entrainment for multiple tracers from the flame tops to hundreds of kilometers downwind and illustrate some intrinsic linear behaviors. The analysis suggests a mixed-effects regression emission technique (MERET), which can eliminate occasional strong biases associated with the commonly used normalized excess mixing ratio (NEMR) method. MERET splits <span class="inline-formula"><i>C</i><sub>tot</sub></span> to reveal <span class="inline-formula"><i>C</i><sub>burn</sub></span> by exploiting the fact that <span class="inline-formula"><i>C</i><sub>burn</sub></span> and all tracers respond linearly to dilution, while each tracer has consistent EnR behavior (slope of tracer concentration with respect to <span class="inline-formula"><i>C</i><sub>burn</sub></span>). The two effects are separable. Two or three or preferably more emission indicators are required as a minimum; here we used eight. In summary, MERET allows a fine spatial resolution (EnRs for individual observations) and comparison of similar plumes that are distant in time and space. Alkene ratios provide us with an approximate photochemical timescale. This allows discrimination and definition, by fire situation, of ERs, allowing us to estimate emission factors.</p>https://amt.copernicus.org/articles/13/7069/2020/amt-13-7069-2020.pdf