Stochastic Climate Theory: Models and Applications

Author:   Serguei G. Dobrovolski
Publisher:   Springer-Verlag Berlin and Heidelberg GmbH & Co. KG
Edition:   Softcover reprint of hardcover 1st ed. 2000
ISBN:  

9783642085581


Pages:   282
Publication Date:   01 December 2010
Format:   Paperback
Availability:   In Print   Availability explained
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Stochastic Climate Theory: Models and Applications


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Overview

The author describes the stochastic (probabilistic) approach to the study of changes in the climate system. Climatic data and theoretical considerations suggest that a large part of climatic variation/variability has a random nature and can be analyzed using the theory of stochastic processes. This work summarizes the results of processing existing records of climatic parameters as well as appropriate theories: from the theory of random processes (based on the results of Kolmogorov and Yaglom) and Hasselmann's ""stochastic climate model theory"" to recently obtained results.

Full Product Details

Author:   Serguei G. Dobrovolski
Publisher:   Springer-Verlag Berlin and Heidelberg GmbH & Co. KG
Imprint:   Springer-Verlag Berlin and Heidelberg GmbH & Co. K
Edition:   Softcover reprint of hardcover 1st ed. 2000
Dimensions:   Width: 15.50cm , Height: 1.50cm , Length: 23.50cm
Weight:   0.462kg
ISBN:  

9783642085581


ISBN 10:   364208558
Pages:   282
Publication Date:   01 December 2010
Audience:   Professional and scholarly ,  Professional and scholarly ,  Professional & Vocational ,  Postgraduate, Research & Scholarly
Format:   Paperback
Publisher's Status:   Active
Availability:   In Print   Availability explained
This item will be ordered in for you from one of our suppliers. Upon receipt, we will promptly dispatch it out to you. For in store availability, please contact us.

Table of Contents

Climatic System: Data, Processes, Scales, and Deterministic Models.- Theoretical Foundations of the Stochastic Approach to Climate Variability Studies.- Stochastic Models of Recent Climatic Changes.- Stochastic Models for Glacial Cycles.- Conclusion.

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