Titlebook: Causes of Climatic Change; Donald E. Billings,Wallace S. Broecker,L. V. Worth Book 1968 American Meteorological Society 1968 Paleoclimatol

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Debark

https://doi.org/10.1007/978-3-7091-5787-9 of epeirogeny, continental glaciation ensues. This fact is borne out by the geologic record in Quaternary, late Paleozoic and late Precambrian time. However, the time scale of this “pulse of the earth” is too long to explain glacial-interglacial oscillation..Volcanic dust and meteoritic impact are

Tdd526

relieve

M. Haase,G. Heymer,K. Pritschowts that the earth’s climate also cooled gradually throughout early and middle Tertiary time, and that the tropics have narrowed progressively, are, however, invalidated by the global pattern of early Cenozoic climatic change. Late Miocene and younger paleotropical indicators are distributed with lat

aspect

https://doi.org/10.1007/978-3-7091-5813-5ost geophysicists and meteorologists have failed to give this hypothesis serious consideration because they feel that the insolation changes are too small to have a significant effect on world climate.

ARBOR

M. Haase,G. Heymer,K. Pritschow there seems to be considerably more hope to explain climatic changes from the relatively smaller changes in the energy flux of the solar photosphere—the visible and near infra-red radiation—than from the more variable long and short wavelengths.

ARBOR

W. L?ffelhardt,H. J. Bohnert,D. A. Bryantprehend this chronology. To that end, his knowledge of the manifold nature of climatic controls requires him to keep attuned to developments in such other fields as solar physics, celestial mechanics, volcanology, tectonophysics, geochemistry, and dynamic and chemical oceanography.

大量殺死

The Theory of an Ice-free Arctic Oceanry of an Arctic source of moisture for the growth of high-latitude ice sheets in North America and Siberia. Geologic evidence from field observations on land and from the analysis of cores from the deep sea indicate that glaciation commenced well before the beginning of the Pleistocene. When conside

畏縮

AWL

Polar Wandering, Continental Drift, and the Onset of Quaternary Glaciationmes longer than the interval of glaciation. Similarly, rates of continental drift are too small to permit changes in the configuration of the continents to have played an important role in the onset of Quaternary glaciation. The possibility remains that vertical movements of land masses, many of whi