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- W26222614 abstract "ABSTRACT Excluding the slow processes of conversion of, natural vegetation into arable land and pastures (lasting since the neolithic revolution 6-8000 years ago) all other anthropogenic processes within the climatic system contribute to global warming. These processes are the release of CO2 and other trace gases absorbing in the infrared window (e.g. N2O), air pollution by particles (with some exceptions) and direct input of energy (heat and water vapour). Since sensible heat (enthalpy) and tropospheric particles remain only a few days within the atmosphere, in contrast to many years in the case of CO2 and the trace gases, it is possible to concentrate on the so-called greenhouse effect of the latter. To include the role of trace gases, a “Combined Greenhouse Effect” is proposed, expressed in units of virtual CO2 content. Using the Augustsson-Ramanathan model, representative data for global warming can be related to given virtual CO2 levels. Estimates of the time-scale are derived from the Zimen model, using logistic functions for different CO2 growth rate." @default.
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- W26222614 date "1979-01-01" @default.
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- W26222614 title "Can Climate History Repeat Itself? Possible Climatic Warming and the Case of Paleoclimatic Warm Phases" @default.
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- W26222614 doi "https://doi.org/10.1016/b978-0-444-41766-4.50009-6" @default.
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