Download Advances in Energy Systems and Technology. Volume 4 by Peter Auer and David Douglas (Eds.) PDF

By Peter Auer and David Douglas (Eds.)

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The form used is: dNldt = aN(l - Ν/Αγ 30 R. M. , (1 - NIA). This procedure has the advantage of projecting over a longer time span while maintaining what is intuitively the proper shape for fuel use during the fossil fuel era. By adjusting α, γ, and A, the fossil fuel use pattern can be made to ap­ proach almost any pattern one can conceive for the future, including the shorter range "forecasts" of energy models. The atmospheric C0 2 concentrations in Fig. 3 are computed by a carbon cycle model which attempts to systematically increment the reservoirs in the global carbon cycle on a year-by-year basis.

A new look at atmospheric carbon dioxide. , op. , pp. 19-29. 34 R. M. Rotty Holdridge, L. , Grenke, W. C , Hathaway, W. , and Tosi, J. , Jr. (1971). " Pergamon, Oxford. Houghton, R. , Hobbie, J. , Melitto, J. , Peterson, B. , Shaver, G. , and Woodwell, G. M. (1983). Changes in the carbon content of terrestrial biota and soils between 1860 and 1980: A net release of C0 2 to the atmosphere. Ecol. Monogr. (in press). Keeling, C D . (1973). Industrial production of carbon dioxide from fossil fuels and limestone.

S. Brown and A. E. ). Final Report, Septem­ ber 15, 1978-September 14, 1980. , and Stouffer, R. J. (1980). Sensitivity of a global climate A Current View of Atmospheric C02 35 model to an increase of C0 2 concentration in the atmosphere. J. Geophys. Res. 85(C10), 5529-5554. , and Wetherald, R. T. (1975). The effects of doubling the C0 2 concentration on the climate of a general circulation model. J. Atmos. Sei. 32(1), 3-15. , and Wetherald, R. T. (1980). On the distribution of climate change resulting from an increase in C0 2 content of the atmo­ sphere.

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