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The IGAC Biomass Burning Experiment (BIBEX): Rationale and Evolution Contributed by: Meinrat O. Andreae, BIBEX Convener 1988-1998, Biogeochemistry Department, Max Planck Institute for Chemistry, Mainz, Germany
![]() Fire must have been around ever since land plants evolved some 300-400 million years ago. Before the advent of humans, fire was ignited naturally by lightning strikes in dry vegetated regions. Today, however, fire is almost exclusively the result of human activities, which include the burning of forested areas to facilitate land clearing, the burning of harvest debris, the extensive burning of natural grasslands and savannas to sustain nomadic agriculture, and the burning of biomass as fuel for cooking and heating. Fires and smoke in Indonesia, Florida, Brazil, and other regions have been all over the news recently. The general public, as well as the scientific community, is now aware that the emissions from biomass burning represent a large perturbation to global atmospheric chemistry, especially in the tropics. Satellite and airborne observations have revealed elevated levels of O3, CO, and other trace gases over vast areas of Africa, South America, the tropical Atlantic, the Indian Ocean, and the Pacific. Smoke aerosols from fires perturb regional, and probably global, radiation budgets by their light-scattering effects and by their influence on cloud microphysical processes. Fire also has both short- and long-term effects on trace gas emissions from affected ecosystems, which, for instance, in the case of CO2 and N2O, may be more significant than their immediate release during burning. Fire also alters the long term dynamics of the cycling and storage of elements within terrestrial ecosystems, thereby changing their potential as sources or sinks of various trace gases. Finally, deposition of compounds produced by biomass burning on pristine tropical ecosystems may affect their composition and dynamics. When, in November 1988, some 50 atmospheric scientists met at Dookie College, a small campus in the agricultural lands of Victoria (Australia) to map out the scientific goals of the International Global Atmospheric Chemistry (IGAC) Project, they were keenly aware of the prominent role that biomass burning plays in the tropics. Given the scarcity of available data at the time, they assigned high priority to the creation of the IGAC Biomass Burning Experiment (BIBEX) with the goals to
The first meeting of the BIBEX Coordinating Committee took
place in September 1990, in Chamrousse, France. Additional meetings
have been held approximately once per year, often in conjunction
with IGAC symposia or other appropriate scientific meetings.
The BIBEX community has also been involved in organizing several
workshops and symposia, which served as platforms to review existing
information, report on recent research, and plan future BIBEX
activities. Examples are the 1992 Dahlem conference on Fire in
the Environment (Crutzen and Goldammer, 1993), and the two Chapman
Conferences on Biomass Burning (Levine, 1991; Levine, 1996)
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