Titlebook: Decadal Climate Variability; Dynamics and Predict David L. T. Anderson,Jürgen Willebrand Conference proceedings 1996 Springer-Verlag Berlin

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Oberfl?chenspannung und Kapillarit?t. Which mechanism operates implies the existence and range of possible predictability. These lectures, therefore, have two purposes: 1) to look at the evidence for the various proposed mechanisms and see if any can be chosen as most likely (or if any can be rejected and thereby eliminated from furth

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Ged?mpfte und erzwungene SchwingungenSea both contribute significantly to the production and export of North Atlantic Deep Water, thus helping to drive the global thermohaline circulation, while the formation and spreading of 18-degree water at shallow-to-intermediate depths off the US eastern seaboard is a major element in the circula

Obverse

Das Neue Physikalische GrundpraktikumOceans. A hierarchy of numerical models and observations are used to understand the fundamental dynamics of these decadal cycles. They are generated by large-scale ocean-atmosphere interactions in mid-latitudes and must be regarded as inherently coupled modes. The memory of the coupled system, howev

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Das Neue Physikalische Grundpraktikumy been carefully considered. The question is related to the accelerating increase in the so-called greenhouse gases, carbon dioxide, methane, nitrous oxide and CFCs and to what extent and how fast this increase is likely to lead to climate changes. It is indeed of considerable interest that a few ga

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Quo vadis Strategisches Management? on time scales of decades to centuries. Time scales extracted from high-resolution proxy records and observations indicate that the spectrum of climate variability exhibits significant power in the range of decades to centuries superimposed on a red-noise continuum. The classical view of climate va

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Das Neue Strategische Managementis not only the obvious geometrical similarity — the zonal unboundedness of a current reaching all around the earth —, there are also deeper dynamical correspondences. Though the forcing is different, the dynamical balance of the zonal atmospheric flow and the ACC resides substantially on the excita

CLASP

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1431-7125 theoretical conceptions of the physical mechanisms of climate change with observational evidence of these changes. The following key topics are included: Observed Climatic Variability, Predictability of the Atmosphere and Oceans from Days to Decades, and Mechanisms for Decadal to Centennial Climate

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Oberfl?chenspannung und Kapillarit?t wrong, the research is likely to get off on the wrong track. If they are lacking altogether, the course of the research may be determined by default, through ad-hoc choices, as in the maxim: “If all you have is a hammer, all you’ll see is nails”.