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Titlebook: Long and Short Term Variability of Climate; Heinz Wanner,Ulrich Siegenthaler Conference proceedings 1988 Springer-Verlag Berlin Heidelberg

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Variations in the spring-summer climate of central europe from the high middle ages to 1850,
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Causes and effects of natural CO2 variations during the glacial-interglacial cycles,
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Norwegian sea deep water variations over the last climatic cycle: Paleo-oceanographical implicationith the benthic record of Pacific core V 19–30 for glacial stages 2 and 3. The resulting record may be used to extract either the temperature signal present in benthic records from other oceanic basins or the variations in surface hydrology recorded by the oxygen isotope variations of planktonic for
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Causes of interannual global temperature variations over the period since 1861,rature. The effects are relatively short-lived. The duration of the maximum effect is of the order of 6 months and it occurs at some time within the two years immediately after the volcano or warm or cold event. These two factors are responsible for between 30 and 50% of the interannual, high freque
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Norwegian sea deep water variations over the last climatic cycle: Paleo-oceanographical implications an active area of deep water formation not only during full interglacial conditions (isotopic stages 1 and 5e) but also during the early part of the glaciation (isotope stages 4 and 5a–5d)..As sinking of surface water to the depth is linked to its cooling during winter, the Norwegian Sea deep wate
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punktes für eine stetige Abbildung einer kompakten konvexen Menge in einem lokal-konvexen topo-logischen Vektorraum auf die Berechnung eines Index im Hilbertraum zurückführen. Als Vorbereitung soll jedoch zunächst gezeigt werden, daß überhaupt für stetige Abbildungen von kompakten konvexen Mengen in
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