Titlebook: Non-CO2 Greenhouse Gases: Why and How to Control?; Proceedings of an In J. Ham,L. J. H. M. Janssen,R. J. Swart Conference proceedings 1994

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Biosphere Atmosphere Exchanges: Ozone and Aerosol Dry Deposition Velocities Over a Pine Forest correlation method. Low frequency fluctuations in the variations of scalars can introduce erroneous values of vertical fluxes for ozone and aerosol particles but also, in some cases of low wind, for momentum and heat. The dry deposition velocity variations are similar for ozone and aerosol, althoug

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Kornelis Blok,David De Jagerst, though, the general idea of a warranted argument is put forward. A ‘warranted’ argument has components that can be parsed and have been checked for coherence. Merely verifying something by giving evidence for it is not enough to ensure valid, new knowledge. In addition the argument put forward s

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I. B. Obioh,A. F. Oluwole,F. A. Akeredoluretation stage, as opposed to commenting on mere associations of variables. Regression and other techniques are used to discern findings about mechanisms that are causal or which supply explanatory context. Sometimes we may want to know what conditions are necessary or sufficient for outcomes. Thus,

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