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Titlebook: Stochastic Climate Models; Peter Imkeller,Jin-Song Storch Conference proceedings 2001 Springer Basel AG 2001 Differentialgleichungen.Scale

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楼主: foresight
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A gallery of simple models from climate physicse to train the physical intuition of the behavior of the system and guide the interpretation of the results of numerical models. Simple models may be stand-alone models of subsystems, such stand-alone general circulation models of the ocean or the atmosphere or coupled models, with reduced degrees o
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Dynamical systems with time scale separation: averaging, stochastic modelling, and central limit therecent rigorous results on Central Limit Theorems and the way how deterministic chaotic dynamical systems can approach a (stochastic) Langevin process in the limit of infinitely separated time scales. Again, the numerical example indicates their relevance also under less idealized conditions.
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Hasselmann’s stochastic climate model viewed from a statistical mechanics perspectivees in position and momentum space. The theory of the climate system is less developed. There exists a gallery rather than a hierarchy of models. Hasselmann’s stochastic climate model is a mesoscopic description. It ignores the details of the weather fluctuations. In its original version, it is a cog
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Conference proceedings 2001ic expertise, from mathematicians concerned with the derivation of stochastic models from first principles, to app­ lied climate modellers trying to understand the dynamics of the complex climate system. Following the first burst of stochastic modelling papers in the decade from the mid-seventies to
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Stochastic Climate Models978-3-0348-8287-3Series ISSN 1050-6977 Series E-ISSN 2297-0428
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Averaging and climate modelsIt is natural to view climate as a slow motion governed by a set of equations depending on weather considered as a fast motion governed by another set of equations. This leads to the averaging setup which is discussed in this paper.
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Progress in Probabilityhttp://image.papertrans.cn/s/image/877879.jpg
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https://doi.org/10.1007/978-3-0348-8287-3Differentialgleichungen; Scale; climate modelling; digital elevation model; globale Analysis; random dyna
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Some mathematical aspects of the GCMsze a number of results concerning the well-posedness of the associated boundary and initial value problems, and concerning the long time behavior of the solutions (attractors and dynamical systems points of views).
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