Titlebook: Global Atmospheric-Biospheric Chemistry; Ronald G. Prinn Book 1994 Springer Science+Business Media New York 1994 Aerosol.Atmospheric chemi

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Atmospheric Chemistry of the East Asian Northwest Pacific Region,d to steer the APARE activity..The first intensive APARE field study was completed in September-October 1991, by the cooperative leadership of the U.S. National Aeronautics and Space Administration (NASA) and the Japanese National Institute of Environmental Studies (NIES). NASA’s initiative, named P

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Biomass Burning in the Global Environment: First Results from the IGAC/BIBEX Field Campaign STARE/T-scattering effects and 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 CO. and N.O, may be more significant than their immediate release during the fire. Fire also al

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Trace Gas Emissions from Rice Fields,ane emission. A part of the methane emitted from naturally flooded ricefields may not be considered anthropogenic. Because of the limited number and locations of comprehensive seasonal flux measurements, global extrapolations of emission rates from ricefields are still highly uncertain and tentative

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Polar Atmosphere and Snow Chemistry, blown dust or marine gases and particles. The pollution has an impact on both physical and chemical climatology. Anthropogenic Arctic haze aerosols of black carbon and sulphate have a net warming influence in the north in contrast to elsewhere on the globe where (with less black carbon) they tend t

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Global Measurements of Photochemically Active Compounds,we focus on measurement of nitrogen oxides, NO., in the troposphere. The oxides of nitrogen to a large extent control hydroxyl radical concentration and ozone production in the troposphere. Thus, accurate knowledge of the global NO. distribution is required for the understanding of tropospheric chem

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Global Emissions and Models of Photochemically Active Compounds,sequences of anthropogenic emissions. This paper compares IGAC recommended emissions inventories for reactive nitrogen and sulfur dioxide to those that have been in use previously. We also present results from the three-dimensional LLNL atmospheric chemistry model that show how emissions of anthropo