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Titlebook: Current Issues in Climate Research; Proceedings of the E A. Ghazi,R. Fantechi Conference proceedings 1986 Springer Science+Business Media D

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楼主: 弄混
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The Impact on Europe of Large-Scale Climatic Changes: The Onset of Glaciation and the Last Deglaciatundly modified: at the height of the last ice age, surface water temperatures in the neighbouring Atlantic Ocean were more than 10°C lower than those of the present day. A cold dry climate had led to the development of a polar desert in northern Europe and to steppe conditions further to the south..
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Modelling the Astronomical Theory of Paleoclimates in the Time and Frequency Domainural decrease of the atmospheric C0. would follow the present cooling trend..Spectral analyses and a paleoclimatic data bank have allowed to perceive the overall physical meaning of the isotopic spectra collected from deep-sea cores. The response of the climatic system to the astronomical forcing ca
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Paleoclimatic Reconstruction in Belgium and in Greece Based on Quaternary Lithostratigraphic Sequencveal long term periodicities which allow subdivision of the Pleistocene into four Maxi Cycles of each 600.000 yrs. The latter may be split up into Cryomeres of 250.000 yrs and Thermomeres of 350.000 yrs each comprising a number of cold-warm cycles at 100.000 yrs interval. So far the 413.000 yrs is n
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Evidence of Bimodality in the Statistics of Northern Hemisphere Circulations identified as a key mechanism to take into account in order to produce better agreement with observations. A new improved version of CDV is studied and its theoretical predictions concerning statistical properties of general circulation are verified by means of data analysis. Particular attention
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Simulation of European Climate with an Atmospheric General Circulation Model the earth’s climate system. This is being used in studies of the physical basis of climate and of its response to natural or man-induced perturbations. Such a model is potentially a powerful tool for climate research, but for it to be applicable to the real world it must be able to simulate the pre
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