Titlebook: Long-Term Climatic Variations; Data and Modelling Jean-Claude Duplessy,Marie-Thérèse Spyridakis Conference proceedings 1994 Springer-Verlag

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Effects of Short and Long Term Climatic Changes on Permafrost - Sedimentological Datawo consecutive winters and intervening summer’ (Brown and Kupsch 1974). It currently underlies approximately one fifth of the earth’s terrestrial surface. During the cold stages of the Quaternary, permafrost extended equatorwards and developed in areas which currently enjoy relatively temperate clim

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Mid-Latitude Ice Sheets through the Last Glacial Cycle : Glaciological and Geological Reconstruction of the system by interactions across their upper, basal and marine boundaries. Numerical models of ice sheet behaviour require a description of the physics of time dependent thermo-mechanically coupled flow, specification of the boundary conditions and an appropriate time dependent climatic forcing function. The basis of such a model is described.

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Precession, Eccentricity, Obliquity, Insolation and Paleoclimates periods and combination tones between eccentricity and precession. Over the Quaternary, the latitudes of the polar and the tropical circles, varying with obliquity, are situated respectively between 65.5. and 68. and between 22. and 24.5.. Their present-day motion towards north is estimated to be 1

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Biosphere Modeling for Climate StudiesDendroclimatology has traditionally resorted to empirical correlations between tree-ring characteristics and climate in the recent past, and extrapolated such relations beyond the period of instrumental records. An explicit modeling approach provides a powerful and flexible tool, but its application

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nen Objektes, wenn gleichzeitig mit der Objektinformation eine nicht zu dem Objekt passende Farbe dargeboten wurde. In anderen Untersuchungen konnte kein statistisch signifikanter Einfluss von Farbinformationen auf das Erkennen und Benennen von Objekten gefunden werden (Ostergaard & Davidoff, 1985;

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