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      <ref-type name="Journal Article">17</ref-type>
      <work-type>ACL : Articles dans des revues avec comité de lecture répertoriées par l'AERES</work-type>
      <contributors>
        <authors>
          <author>
            <style face="bold" font="default" size="100%">Mouillot, F.</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Narasimha, A.</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Balkanski, Y.</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Lamarque, J. F.</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Field, C. B.</style>
          </author>
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      <titles>
        <title>Global carbon emissions from biomass burning in the 20th century</title>
        <secondary-title>Geophysical Research Letters</secondary-title>
      </titles>
      <pages>art. L01801 [4 ]</pages>
      <dates>
        <year>2006</year>
      </dates>
      <call-num>fdi:010065884</call-num>
      <language>ENG</language>
      <periodical>
        <full-title>Geophysical Research Letters</full-title>
      </periodical>
      <isbn>0094-8276</isbn>
      <accession-num>ISI:000234509100003</accession-num>
      <number>1</number>
      <electronic-resource-num>10.1029/2005GL024707</electronic-resource-num>
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      <volume>33</volume>
      <remote-database-provider>Horizon (IRD)</remote-database-provider>
      <abstract>We used a new, 100-year, 1 x 1 degrees global fire map and a carbon cycle model (CASA) to provide a yearly gridded estimate of the temporal trend in carbon emissions due to wildfires through the 20th century. 2700 - 3325 Tg C y(-1) burn at the end of the 20th century, compared to 1500 2700 Tg C y(-1) at the beginning, with increasing uncertainty moving backward in time. There have been major changes in the regional distribution of emissions from fires, as a consequence of i) increased burning in tropical savannas and ii) a switch of emissions from temperate and boreal forests towards the tropics. The frequently- used assumption that pre-industrial emissions were 10% of present biomass burning is clearly inadequate, in terms of both the total amount and the spatial distribution of combustion.</abstract>
      <custom6>021 ; 082 ; 112</custom6>
      <custom1>UR060</custom1>
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