P. J. Crutzen , E. Sanhueza , and C. A. M. Brenninkmeijer
Measurements of methane concentrations in the boundary layer in the northern part of the Guayana shield, Venezuela, during the wet season (October 1988), showed the presence of substantial methane surface emissions. The measuring site is within the savanna climate region, but is affected by emissions from savanna and forest vegetation. From day versus night concentration measurements, with higher concentrations during night, a methane source strength near the site of 3–7×1011 molecules/cm2 /s can be estimated, which includes emissions from small tracts of flooded soils, termites and especially tropical vegetation. Extrapolated to the entire savanna, this may imply a methane source of ~30–60 Tg yr−1 similar to the one calculated for tropical vegetation on the basis of recently published in vitro plant emission experiments by Keppler et al. (2006), which indicate emissions of ~30 Tg yr−1 for tropical savannas and grasslands and ~78 Tg yr−1 for tropical forests.
Received: 21 Mar 2006 – Discussion started: 13 Apr 2006
Publisher's note : Copernicus Publications remains neutral with regard to jurisdictional claims made in the text, published maps, institutional affiliations, or any other geographical representation in this paper. While Copernicus Publications makes every effort to include appropriate place names, the final responsibility lies with the authors. Views expressed in the text are those of the authors and do not necessarily reflect the views of the publisher.
P. J. Crutzen , E. Sanhueza , and C. A. M. Brenninkmeijer
Status: closed (peer review stopped)
Status: closed (peer review stopped)
AC : Author comment | RC : Referee comment | SC : Short comment | EC : Editor comment
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Status: closed (peer review stopped)
Status: closed (peer review stopped)
AC : Author comment | RC : Referee comment | SC : Short comment | EC : Editor comment
- Printer-friendly version
- Supplement
P. J. Crutzen , E. Sanhueza , and C. A. M. Brenninkmeijer
P. J. Crutzen , E. Sanhueza , and C. A. M. Brenninkmeijer
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