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<article xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:xlink="http://www.w3.org/1999/xlink" article-type="research-article" dtd-version="3.0" xml:lang="en">
<front>
<journal-meta>
<journal-id journal-id-type="publisher">ACP</journal-id>
<journal-title-group>
<journal-title>Atmospheric Chemistry and Physics</journal-title>
<abbrev-journal-title abbrev-type="publisher">ACP</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1680-7324</issn>
<publisher><publisher-name>Copernicus GmbH</publisher-name>
<publisher-loc>GÃ¶ttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/acp-11-12973-2011</article-id>
<title-group>
<article-title>The wildland fire emission inventory: western United States emission estimates and an evaluation of uncertainty</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Urbanski</surname>
<given-names>S. P.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Hao</surname>
<given-names>W. M.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Nordgren</surname>
<given-names>B.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Missoula Fire Sciences Laboratory, Rocky Mountain Research Station, United States Forest Service, Missoula, Montana, USA</addr-line>
</aff>
<pub-date pub-type="epub">
<day>20</day>
<month>12</month>
<year>2011</year>
</pub-date>
<volume>11</volume>
<issue>24</issue>
<fpage>12973</fpage>
<lpage>13000</lpage>
<permissions>
<license xlink:type="simple">
<license-p>This is an open-access article ditributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.</license-p>
</license>
</permissions>
<self-uri xlink:href="http://www.atmos-chem-phys.net/11/12973/2011/acp-11-12973-2011.html">This article is available from http://www.atmos-chem-phys.net/11/12973/2011/acp-11-12973-2011.html</self-uri>
<self-uri xlink:href="http://www.atmos-chem-phys.net/11/12973/2011/acp-11-12973-2011.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys.net/11/12973/2011/acp-11-12973-2011.pdf</self-uri>
<abstract>
<p>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.
&lt;br&gt;&lt;/br&gt;
WFEI was used to estimate emissions of CO (ECO) and PM&lt;sub&gt;2.5&lt;/sub&gt; (EPM&lt;sub&gt;2.5&lt;/sub&gt;)
for the western United States from 2003â€“2008. The uncertainties in the
inventory estimates of ECO and EPM&lt;sub&gt;2.5&lt;/sub&gt; (&lt;i&gt;u&lt;/i&gt;&lt;sub&gt;ECO&lt;/sub&gt; and &lt;i&gt;u&lt;/i&gt;&lt;sub&gt;EPM&lt;sub&gt;2.5&lt;/sub&gt;&lt;/sub&gt;, 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, &lt;i&gt;Å©&lt;/i&gt;&lt;sub&gt;EX&lt;/sub&gt;
(where X = CO or PM&lt;sub&gt;2.5&lt;/sub&gt;), defined such that for a given aggregation
level 50% of total emissions occurred from elements with &lt;i&gt;u&lt;/i&gt;&lt;sub&gt;EX&lt;/sub&gt;
&lt;i&gt;Å©&lt;/i&gt;&lt;sub&gt;EX&lt;/sub&gt;. The sensitivity of the WFEI estimates of ECO and
EPM&lt;sub&gt;2.5&lt;/sub&gt; to uncertainties in mapped fuel loading, fuel consumption, burned
area and emission factors have also been examined.
&lt;br&gt;&lt;/br&gt;
The estimated annual, domain wide ECO ranged from 436 Gg yr&lt;sup&gt;âˆ’1&lt;/sup&gt; in 2004
to 3107 Gg yr&lt;sup&gt;âˆ’1&lt;/sup&gt; in 2007. The extremes in estimated annual, domain wide
EPM&lt;sub&gt;2.5&lt;/sub&gt; were 65 Gg yr&lt;sup&gt;âˆ’1&lt;/sup&gt; in 2004 and 454 Gg yr&lt;sup&gt;âˆ’1&lt;/sup&gt; 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 PM&lt;sub&gt;2.5&lt;/sub&gt; emissions. During the months
with the greatest fire activity, WF accounted for the majority of total CO
and PM&lt;sub&gt;2.5&lt;/sub&gt; emitted across the study region. Uncertainties in annual,
domain wide emissions was 28% to 51% for CO and 40% to
65% for PM&lt;sub&gt;2.5&lt;/sub&gt;. Sensitivity of &lt;i&gt;Å©&lt;/i&gt;&lt;sub&gt;ECO&lt;/sub&gt; and
&lt;i&gt;Å©&lt;/i&gt;&lt;sub&gt;EPM&lt;sub&gt;2.5&lt;/sub&gt;&lt;/sub&gt; to the emission model components depended on
scale. At scales relevant to regional modeling applications (&amp;Delta;&lt;i&gt;x&lt;/i&gt; = 10 km, &amp;Delta;&lt;i&gt;t&lt;/i&gt; = 1 day) WFEI estimates 50% of total ECO with
an uncertainty &lt;133% and half of total EPM&lt;sub&gt;2.5&lt;/sub&gt; with an uncertainty
&lt;146%. &lt;i&gt;Å©&lt;/i&gt;&lt;sub&gt;ECO&lt;/sub&gt; and &lt;i&gt;Å©&lt;/i&gt;&lt;sub&gt;EPM&lt;sub&gt;2.5&lt;/sub&gt;&lt;/sub&gt; are
reduced by more than half at the scale of global modeling applications
(&amp;Delta;&lt;i&gt; x&lt;/i&gt; = 100 km, &amp;Delta;&lt;i&gt; t&lt;/i&gt; = 30 day) where 50% of total emissions
are estimated with an uncertainty &lt;50%
 for CO and &lt;64% for PM&lt;sub&gt;2.5&lt;/sub&gt;. Uncertainties in the estimates of
burned area drives the emission uncertainties at regional scales. At global
scales &lt;i&gt;Å©&lt;/i&gt;&lt;sub&gt;ECO&lt;/sub&gt; is most sensitive to uncertainties in the fuel
load consumed while the uncertainty in the emission factor for PM&lt;sub&gt;2.5&lt;/sub&gt;
plays the dominant role in &lt;i&gt;Å©&lt;/i&gt;&lt;sub&gt;EPM&lt;sub&gt;2.5&lt;/sub&gt;&lt;/sub&gt;. 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.</p>
</abstract>
<counts><page-count count="28"/></counts>
</article-meta>
</front>
<body/>
<back>
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