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Titlebook: Climatic Variations and Variability: Facts and Theories; NATO Advanced Study A. Berger Book 1981 D. Reidel Publishing Company, Dordrecht,

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Glacial to Interglacial Changes in Ocean and Atmosphere Chemistryce water and the atmosphere. Evidence in support of this hypothesis is obtained from the .C results for benthic and planktonic foraminifera. Changes in the difference between warm surface water and mean oceanic .C values reflect changes in the oceanic PO. to ΣCO. ratio.
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https://doi.org/10.1007/978-3-642-41048-2reenland seesaw”. The injection of volcanic aerosol by the eruption of Mt. Agung in March 1963 into the stratosphere gives rise to temperature increases of up to 5°C in the stratosphere and cooling of 1°C in the troposphere. The third major climatic signal in the recent record—the so called “Biennial oscillation”is also briefly reviewed.
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Rechtliche Aspekte von Kunstfehlern,sonal temperatures and salinity. When applied to samples from a chronostratigraphic horizon, transfer functions yield synoptic charts of past climates. In this form paleontological data are readily interpretable by meteorologists and physical oceanographers, and can be entered as boundary conditions into numerical models of climate.
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Climatic Changes and Variations: A Geophysical Problemreenland seesaw”. The injection of volcanic aerosol by the eruption of Mt. Agung in March 1963 into the stratosphere gives rise to temperature increases of up to 5°C in the stratosphere and cooling of 1°C in the troposphere. The third major climatic signal in the recent record—the so called “Biennial oscillation”is also briefly reviewed.
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