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The scenarios referred to above depend mainly on future concentrations of certain trace gases, called greenhouse gases, that have been injected into the lower atmosphere in increasing amounts through the burning of fossil fuels for industry, transportation, and residential uses.
One approach to predict future concentrations is to use a detailed atmospheric diffusion model.
All of the simulations assumed that future concentrations of greenhouse gases would rise from today's 392 parts per million to 520 ppm by 2050.
Present study was designed to assess the impact of ambient (present) and elevated (future) concentrations of O3 on two cultivars of Indian rice (Oryza sativa L. cvs Malviya dhan 36 and Shivani).
This paper introduces four approaches to adjust for model bias and errors in order to provide greater confidence for their use in estimating future concentrations as well as using modeled pollutant concentrations in exposure assessments.
We review how climate change could affect future concentrations of tropospheric ozone and particulate matter (PM), and what changing concentrations could mean for population health.
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The only variable contributing significantly towards rising yields is atmospheric CO2; therefore, its actual future concentration will be crucial for maize yields.
However, in the past plans of Budapest transport development (S-Bahn Concept, 2007; Budapest Transport System Development Plan – BKRFT, 2009), only one version of the future concentration of living and working zones was examined as a base for different network proposals.
and the future concentration of gases in atmosphere.
Finally, we want to see, in the present preparation, whether a measure of global population activity may be enough to compare different drugs and open the path to perform, in the future, concentration-response functions.
Some disagreement was noted between the observed and modeled results, suggesting that only limited confidence can be placed in the estimates of the present RF of tropospheric O3 derived from modeled historic concentration changes and in the prediction of future O3 concentrations.
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