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

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Modelling the Ocean Circulationaffect the solution: the system of coordinates, the grid, the numerical algorithms… The impact of physical choices is then presented. Present capacity of numerical modelling is discussed on two examples: a high resolution model of the tropical Pacific and a global circulation model.

Counteract

Precession, Eccentricity, Obliquity, Insolation and Paleoclimatesrequency domain. The annual mean energy received by the whole Earth is varying in time according to the variations of the mean distance from the Earth to the Sun, i.e. as a function of (1 − ..).. The so-called 100 ka period of the eccentricity (and the other periods as well) are originating from a c

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Biosphere Modeling for Climate Studiesses. First, since vegetation is sensitive and slowly adjusting to climate fluctuations, its composition and diversity reflect the interplay of the laws of succession under the constraints of climatic and environmental stress. This interaction can be studied with the help of dynamic gap forest models

忘川河

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

接合

RENAL

Organic Compounds as Proxy-Indicators of Sea Surface Palaeotemperature: The Uk 37 Indexkenones) which are commonly found in Quaternary marine sediments. These compounds are biosynthesized by some species of algae of the Class Prymnesiophyceae, which includes the coccolithophorids. U.. stratigraphy in ocean cores can provide time series records of local SST in the photic zone. Despite

Spinal-Fusion

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