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• W1978214119 abstract "SummaryTo model climate in the distant geological past, we assume that the physical processes involved are the same as those built into models of present-day climate, but that certain of the boundary conditions were different. As regards the Mesozoic, the major changes in boundary condition would be to continental positions, mountain elevations, and sea level; these change only on timescales of the order 106 years. However, during the past million years, with today’s boundary conditions, climate has undergone enormous and rapid fluctuations. The examination of these more recent changes gives us very considerable insight into the myriad interactions whereby oceanic and atmospheric chemical composition, the marine and continental biosphere, the surface albedo as well as temperate-latitude ice vohrtne and low-latitude aridity have all fluctuated in response to rather subtle changes in the latitudinal and seasonal redistribution of solar energy. At present we can only construct a general circulation model of the climate of today, or of the last ice age, by specifying many of the components of the global climate system that ought to be treated as unknown variables. The models constructed by Gallée et al. (1991, 1992, 1993) point to the characteristics required to simulate a glacial-interglacial cycle. Despite this, we are a long way from actually understanding how climate actually changes on this timescale. In particular, it is difficult to understand how the climate system was able to build ice sheets as quickly as they appear to have formed (Rind et al. 1989)." @default.
• W1978214119 created "2016-06-24" @default.
• W1978214119 creator A5026246029 @default.
• W1978214119 date "1994-01-01" @default.
• W1978214119 modified "2023-09-27" @default.
• W1978214119 title "The climate system in the recent geological past" @default.
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• W1978214119 doi "https://doi.org/10.1007/978-94-011-1254-3_1" @default.
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