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Open AccessJournal ArticleDOI

Emission of trace gases and aerosols from biomass burning

Meinrat O. Andreae, +1 more
- 01 Dec 2001 - 
- Vol. 15, Iss: 4, pp 955-966
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TLDR
In this article, the authors present a set of emission factors for a large variety of species emitted from biomass fires, where data were not available, they have proposed estimates based on appropriate extrapolation techniques.
Abstract
A large body of information on emissions from the various types of biomass burning has been accumulated over the past decade, to a large extent as a result of International Geosphere-Biosphere Programme/International Global Atmospheric Chemistry research activities. Yet this information has not been readily accessible to the atmospheric chemistry community because it was scattered over a large number of publications and reported in numerous different units and reference systems. We have critically evaluated the presently available data and integrated these into a consistent format. On the basis of this analysis we present a set of emission factors for a large variety of species emitted from biomass fires. Where data were not available, we have proposed estimates based on appropriate extrapolation techniques. We have derived global estimates of pyrogenic emissions for important species emitted by the various types of biomass burning and compared our estimates with results from inverse modeling studies.

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Citations
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Journal ArticleDOI

Characterizing the aging of biomass burning organic aerosol by use of mixing ratios: a meta-analysis of four regions.

TL;DR: Variability in ERs close to source is shown to substantially exceed the magnitude of any changes between fresh and aged OA, emphasizing the importance of fuel and combustion conditions in determining OA loadings from biomass burning.
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One-year observations of carbonaceous and nitrogenous components and major ions in the aerosols from subtropical Okinawa Island, an outflow region of Asian dusts

TL;DR: In this paper, the formation and transformation of East Asian aerosols during long-range atmospheric transport were analyzed for organic carbon (OC), elemental carbon (EC), water-soluble organic carbon, WSOC, water soluble total nitrogen (WSTN), water solubility organic nitrogen, and major ions, and the results indicated that NH4+ and Ca2+ play major role in neutralization of acidic aerosols forming NH4HSO4, (NH4)2SO4 and CaSO4.
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Chemical composition of fine particles in fresh smoke plumes from boreal wild-land fires in Europe.

TL;DR: Satellite observations employing MODIS sensor on board of NASA EOS Terra satellite with the dispersion model SILAM and the Fire Assimilation System were used for evaluation of the emission fluxes from wildfires and showed that the major growth in PM concentration was caused by submicrometer particles consisting mainly of particulate organic matter (POM).
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Organic trace gas measurements by PTR-MS during INDOEX 1999

TL;DR: In this paper, the authors present an overview of the distribution of acetonitrile, methanol, acetone, and acetaldehyde over a broad spatial extent of the Indian Ocean (19°N−13°S, 67°E−75°E).
References
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Journal ArticleDOI

Biomass Burning in the Tropics: Impact on Atmospheric Chemistry and Biogeochemical Cycles

TL;DR: Widespread burning of biomass serves to clear land for shifting cultivation, to convert forests to agricultural and pastoral lands, and to remove dry vegetation in order to promote agricultural productivity and the growth of higher yield grasses, but it may also disturb biogeochemical cycles, especially that of nitrogen.
Journal ArticleDOI

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

TL;DR: In this paper, the authors estimated the global amounts of biomass which are affected by fires, and estimated 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.
Journal ArticleDOI

Biomass burning as a source of atmospheric gases CO, H 2 , N 2 O, NO, CH 3 Cl and COS

TL;DR: In this article, it was shown that most biomass burning takes place in the tropics in the dry season and is caused by man's activities, which can contribute extensively to the budgets of several gases which are important in atmospheric chemistry.
Journal ArticleDOI

Soot Carbon and Excess Fine Potassium: Long-Range Transport of Combustion-Derived Aerosols

TL;DR: During a cruise from Hamburg to Montevideo, aerosol samples representing air masses from Europe, the Sahara, tropical Africa, South America, and open oceanic regions were collected and the ratio of soot carbon to fine carbon suggests that most of the particulate organic carbon over the Atlantic is of continental origin.

Global biomass burning: atmospheric, climatic, and biospheric implications.

TL;DR: The 1990 American Geophysical Union's Conference on Biochemical burning as discussed by the authors was attended by more than 175 participants representing 19 countries and discussed remote sensing data concerning biomass burning, gaseous and particle emissions resulting from BB in the tropics, BB in temperate and boreal ecosystems, the historic and prehistoric perspectives on BB, BB and global budgets for carbon, nitrogen, and oxygen, and the BB and the greenhouse effect.
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