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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Methoden der operativen Frakturenbehandlung,od the mean salinity of the oceans was 35.7‰, one part per thousand more saline than it is now. The evolution and eventual dissipation of the Wisconsin bottom water mass is discussed together with the possible effect of this water mass on pelagic sediments.

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Osmotischer Wert, Saugkraft, Turgor,n the mean temperature of the earth. It is emphasized that the simple black-body radiation model frequently used to relate terrestrial mean temperature changes to solar radiation changes is not necessarily valid. Alternative models, based on information regarding the seasonal variation of the earth’

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Osmotischer Wert, Saugkraft, Turgor,overed ocean and for an ice-free ocean. The annual patterns of atmospheric heat loss for both conditions are obtained as residuals; the relation of these patterns to general atmospheric circulation and glacier accumulation is discussed..It is shown that atmospheric cooling in the Arctic is closely r

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Protoplasmatologia‘ Cell Biology Monographss been modified. According to the revision, the importance of the ice-free Arctic Ocean is in the initiating of high-latitude glaciation followed by glacial growth to lower latitudes in those regions where an adequate moisture supply is present. The Arctic Ocean surface would freeze once a good-size

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https://doi.org/10.1007/978-3-7091-5787-9ologic evidence is thus at least permissive that polar continentality is a necessary condition for glaciation. However, continents also occupied the polar regions during most of the Paleozoic, Mesozoic and Cenozoic eras at times when glaciation did not occur, so that clearly polar continentality is

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https://doi.org/10.1007/978-3-7091-5813-5tory were caused by variations in summer insolation in the Northern Hemisphere resulting from the earth’s precession and variations in its tilt. Curves for the tilt variation (period ~40,000 yr) and for the precessional variation (period ~22,000 yr) are reproduced in Fig. 1. From these Milankovitch