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在过去的650年中,南半球生物质燃烧的巨大变化

Z Wang1, J Chappellaz, K Park

  • 1Institute for Terrestrial and Planetary Atmospheres/School of Marine and Atmospheric Sciences, Stony Brook University, Stony Brook, NY 11794-5000, USA.

Science (New York, N.Y.)
|December 4, 2010
PubMed
概括

大气中的一氧化碳水平在650年内大幅波动,这是由于南半球生物质燃烧造成的. 冰芯数据揭示了燃烧活动的重大变化,影响了CO度和同位素比率.

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