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Identification of CO plumes from MOPITT data: Application to the August 2000 Idaho‐Montana forest fires

Identifieur interne : 000B38 ( Istex/Corpus ); précédent : 000B37; suivant : 000B39

Identification of CO plumes from MOPITT data: Application to the August 2000 Idaho‐Montana forest fires

Auteurs : J. Lamarque ; D. P. Edwards ; L. K. Emmons ; J. C. Gille ; O. Wilhelmi ; C. Gerbig ; D. Prevedel ; M. N. Deeter ; J. Warner ; D. C. Ziskin ; B. Khattatov ; G. L. Francis ; V. Yudin ; S. Ho ; D. Mao ; J. Chen ; J. R. Drummond

Source :

RBID : ISTEX:2EF1A0909347B8C0E04A3BA1917FF821C2EDE18B

Abstract

This study focuses on the identification of carbon monoxide (CO) released during the forest fires that took place primarily in Montana and Idaho during the summer of 2000. We focus our analysis on the most intense period of the fires during the second half of August. During that period, the MOPITT instrument onboard the EOS‐Terra platform collected extensive measurements of CO. A simulation of the dispersal of the CO from the fires, constrained by the AVHRR observations of fire location and extent, clearly identifies the affected regions. The model results are compared with the CO observations from the COBRA experiment flight on August 19. Using these various data, we are able to identify the transport of the CO plume originating from the fires. In particular, it is shown that the CO travels eastward from the fires, reaching as far as the East coast and the Gulf of Mexico in a few days. Although the distribution of CO over the U.S. is clearly a combination of a variety of sources it is found that wildfires are a strong component of the summer tropospheric CO.

Url:
DOI: 10.1029/2003GL017503

Links to Exploration step

ISTEX:2EF1A0909347B8C0E04A3BA1917FF821C2EDE18B

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<div type="abstract">This study focuses on the identification of carbon monoxide (CO) released during the forest fires that took place primarily in Montana and Idaho during the summer of 2000. We focus our analysis on the most intense period of the fires during the second half of August. During that period, the MOPITT instrument onboard the EOS‐Terra platform collected extensive measurements of CO. A simulation of the dispersal of the CO from the fires, constrained by the AVHRR observations of fire location and extent, clearly identifies the affected regions. The model results are compared with the CO observations from the COBRA experiment flight on August 19. Using these various data, we are able to identify the transport of the CO plume originating from the fires. In particular, it is shown that the CO travels eastward from the fires, reaching as far as the East coast and the Gulf of Mexico in a few days. Although the distribution of CO over the U.S. is clearly a combination of a variety of sources it is found that wildfires are a strong component of the summer tropospheric CO.</div>
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<dateValid encoding="w3cdtf">2003-05-29</dateValid>
<edition>Lamarque, J.‐F., et al. (2003), Identification of CO plumes from MOPITT data: Application to the August 2000 Idaho‐Montana forest fires, Geophys. Res. Lett., 30, 1688, doi:10.1029/2003GL017503, 13.</edition>
<copyrightDate encoding="w3cdtf">2003</copyrightDate>
</originInfo>
<language>
<languageTerm type="code" authority="rfc3066">en</languageTerm>
<languageTerm type="code" authority="iso639-2b">eng</languageTerm>
</language>
<physicalDescription>
<internetMediaType>text/html</internetMediaType>
<extent unit="figures">4</extent>
</physicalDescription>
<abstract>This study focuses on the identification of carbon monoxide (CO) released during the forest fires that took place primarily in Montana and Idaho during the summer of 2000. We focus our analysis on the most intense period of the fires during the second half of August. During that period, the MOPITT instrument onboard the EOS‐Terra platform collected extensive measurements of CO. A simulation of the dispersal of the CO from the fires, constrained by the AVHRR observations of fire location and extent, clearly identifies the affected regions. The model results are compared with the CO observations from the COBRA experiment flight on August 19. Using these various data, we are able to identify the transport of the CO plume originating from the fires. In particular, it is shown that the CO travels eastward from the fires, reaching as far as the East coast and the Gulf of Mexico in a few days. Although the distribution of CO over the U.S. is clearly a combination of a variety of sources it is found that wildfires are a strong component of the summer tropospheric CO.</abstract>
<relatedItem type="host">
<titleInfo>
<title>Geophysical Research Letters</title>
</titleInfo>
<titleInfo type="abbreviated">
<title>Geophys. Res. Lett.</title>
</titleInfo>
<subject>
<genre>Index Terms</genre>
<topic authorityURI="http://psi.agu.org/taxonomy5/0300">ATMOSPHERIC COMPOSITION AND STRUCTURE</topic>
<topic authorityURI="http://psi.agu.org/taxonomy5/0322">Constituent sources and sinks</topic>
<topic authorityURI="http://psi.agu.org/taxonomy5/0345">Pollution: urban and regional</topic>
<topic authorityURI="http://psi.agu.org/taxonomy5/0368">Troposphere: constituent transport and chemistry</topic>
<topic authorityURI="http://psi.agu.org/taxonomy5/0305">Aerosols and particles</topic>
<topic authorityURI="http://psi.agu.org/taxonomy5/0400">BIOGEOSCIENCES</topic>
<topic authorityURI="http://psi.agu.org/taxonomy5/0478">Pollution: urban, regional and global</topic>
<topic authorityURI="http://psi.agu.org/taxonomy5/4200">OCEANOGRAPHY: GENERAL</topic>
<topic authorityURI="http://psi.agu.org/taxonomy5/4251">Marine pollution</topic>
<topic authorityURI="http://psi.agu.org/taxonomy5/4300">NATURAL HAZARDS</topic>
<topic authorityURI="http://psi.agu.org/taxonomy5/4325">Megacities and urban environment</topic>
</subject>
<identifier type="ISSN">0094-8276</identifier>
<identifier type="eISSN">1944-8007</identifier>
<identifier type="DOI">10.1002/(ISSN)1944-8007</identifier>
<identifier type="CODEN">GPRLAJ</identifier>
<identifier type="PublisherID">GRL</identifier>
<part>
<date>2003</date>
<detail type="volume">
<caption>vol.</caption>
<number>30</number>
</detail>
<detail type="issue">
<caption>no.</caption>
<number>13</number>
</detail>
<extent unit="pages">
<start>n/a</start>
<end>n/a</end>
<total>4</total>
</extent>
</part>
</relatedItem>
<identifier type="istex">2EF1A0909347B8C0E04A3BA1917FF821C2EDE18B</identifier>
<identifier type="DOI">10.1029/2003GL017503</identifier>
<identifier type="ArticleID">2003GL017503</identifier>
<accessCondition type="use and reproduction" contentType="copyright">Copyright 2003 by the American Geophysical Union.</accessCondition>
<recordInfo>
<recordContentSource>WILEY</recordContentSource>
</recordInfo>
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</metadata>
<serie></serie>
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