Titlebook: Biogeochemistry of Global Change; Radiatively Active T Ronald S. Oremland (Chairman) Book 1993 Chapman & Hall, Inc. 1993 Atmospheric chemis

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https://doi.org/10.1007/978-3-8349-9417-2s were 25 μg N.O-N m. h.. If this coniferous forest can be considered representative, we estimate a contribution of temperate coniferous forest soils to the global N.O budget of 1 Tg y.. For NO, mean annual fluxes from temperate coniferous forest soils were estimated to be in the range of 0.5–24 μg

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Gerhard Girmscheid,Christoph Motzkoogged, organic soil (Histosol) in the northern hardwood forest at the Hubbard Brook Experimental Forest in New Hampshire, USA, to determine the extent to which fluxes and processes varied between soil types. Field measurements were carried out between April and November 1990 and indicated that metha

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Die Kostengruppen der Kalkulation,rtilizer influences the flux rates of these gases in agroecosystems. Methane and nitrous oxide fluxes were measured periodically in an irrigated corn (. L.) field from time of fertilization to harvest. Fertilizer treatments included 0 and 218 kg urea-N ha., as well as applications of the nitrificati

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Biogeochemical Cycles of Carbon on a Hierarchy of Time Scalesc carbon dioxide on all time scales. Particular problems with restricted time scales can be analyzed in terms of a subset of the total system. Observations that illustrate interactions on different levels of the hierarchy include the seasonal change of carbon dioxide partial pressure, the glacial to

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Ice Core Records as a Key to Understanding the History of Atmospheric Trace Gasesated with global climatic changes showing strongly depleted concentrations (by up to about a factor of 2 in the case of CH.) during the full glacial conditions relative to interglacial periods. The gas records obtained from ice cores can be interpreted, at least qualitatively, in terms of flux chang

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Late Jurassic Paleoclimate of Pangea Based on Results from a General Circulation Modelfrom a simulation using 1120 ppm CO., four times the preindustrial level, produce a paleoclimate that fits the geologic record. Sea ice is restricted to the high latitudes, making landfall only in restricted areas. The trade winds bring heavy seasonal rainfall to eastern Gondwana and to the Tethys S

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Erythropoietin

A Time-Dependent Two-Dimensional-Model Study of the Trend in Atmospheric Methaneations of tropospheric OH, caused mostly by increasing abundances of CO, with the remaining 60% due to increasing emissions of CH.. However, our calculations only include the direct coupling between CO, CH., and OH. Uncertainties due to the impact of other factors, such as increases in tropospheric