Climatic Change

, Volume 2, Issue 3, pp 207–247

Estimates of gross and net fluxes of carbon between the biosphere and the atmosphere from biomass burning

  • Wolfgang Seiler
  • Paul J. Crutzen
Article

DOI: 10.1007/BF00137988

Cite this article as:
Seiler, W. & Crutzen, P.J. Climatic Change (1980) 2: 207. doi:10.1007/BF00137988

Abstract

In order to estimate the production of charcoal and the atmospheric emissions of trace gases volatilized by burning we have estimated the global amounts of biomass which are affected by fires. We have roughly calculated annual gross burning rates ranging between about 5 Pg and 9 Pg (1 Pg = 1015 g) of dry matter (2–4 Pg C). In comparison, about 9–17 Pg of above-ground dry matter (4–8 Pg C) is exposed to fires, indicating a worldwide average burning efficiency of about 50%. The production of dead below-ground dry matter varies between 6–9 Pg per year. We have tentatively indicated the possibility of a large production of elemental carbon (0.5–1.7 Pg C/yr) due to the incomplete combustion of biomass to charcoal. This provides a sink for atmospheric CO2, which would have been particularly important during the past centuries. From meager statistical information and often ill-documented statements in the literature, it is extremely difficult to calculate the net carbon release rates to the atmosphere from the biomass changes which take place, especially in the tropics. All together, we calculate an overall effect lof the biosphere on the atmospheric carbon dioxide budget which may range between the possibilities of a net uptake or a net release of about 2 Pg C/yr. The release of CO2 to the atmosphere by deforestation projects may well be balanced by reforestation and by the production of charcoal. Better information is needed, however, to make these estimates more reliable.

Copyright information

© D. Reidel Publishing Company 1980

Authors and Affiliations

  • Wolfgang Seiler
    • 1
  • Paul J. Crutzen
    • 1
  1. 1.National Center for Atmospheric ResearchBoulderU.S.A.