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Titlebook: Nonlinear Time Series Analysis in the Geosciences; Applications in Clim Reik V. Donner (Dr),Susana M. Barbosa (Dr) Book 2008 Springer-Verla

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发表于 2025-3-21 18:23:15 | 显示全部楼层 |阅读模式
书目名称Nonlinear Time Series Analysis in the Geosciences
副标题Applications in Clim
编辑Reik V. Donner (Dr),Susana M. Barbosa (Dr)
视频video
概述Includes supplementary material:
丛书名称Lecture Notes in Earth Sciences
图书封面Titlebook: Nonlinear Time Series Analysis in the Geosciences; Applications in Clim Reik V. Donner (Dr),Susana M. Barbosa (Dr) Book 2008 Springer-Verla
描述The enormous progress over the last decades in our understanding of the mechanisms behind the complex system “Earth” is to a large extent based on the availability of enlarged data sets and sophisticated methods for their analysis. Univariate as well as multivariate time series are a particular class of such data which are of special importance for studying the dynamical p- cesses in complex systems. Time series analysis theory and applications in geo- and astrophysics have always been mutually stimulating, starting with classical (linear) problems like the proper estimation of power spectra, which hasbeenputforwardbyUdnyYule(studyingthefeaturesofsunspotactivity) and, later, by John Tukey. In the second half of the 20th century, more and more evidence has been accumulated that most processes in nature are intrinsically non-linear and thus cannot be su?ciently studied by linear statistical methods. With mat- matical developments in the ?elds of dynamic system’s theory, exempli?ed by Edward Lorenz’s pioneering work, and fractal theory, starting with the early fractal concepts inferred by Harold Edwin Hurst from the analysis of geoph- ical time series,nonlinear methods became availabl
出版日期Book 2008
关键词Climatology; Deformation; Geosciences; Nonlinear time series analysis; Observational data; Scale; Simulati
版次1
doihttps://doi.org/10.1007/978-3-540-78938-3
isbn_softcover978-3-642-09769-0
isbn_ebook978-3-540-78938-3Series ISSN 0930-0317 Series E-ISSN 1613-2580
issn_series 0930-0317
copyrightSpringer-Verlag Berlin Heidelberg 2008
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发表于 2025-3-21 21:14:29 | 显示全部楼层
0930-0317 m “Earth” is to a large extent based on the availability of enlarged data sets and sophisticated methods for their analysis. Univariate as well as multivariate time series are a particular class of such data which are of special importance for studying the dynamical p- cesses in complex systems. Tim
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Prediction of Extreme Eventslly preceeding events. Theoretical considerations lead to the construction of schemes that are optimal with respect to several scoring rules. We discuss scenarios for which, in contrast to intuition, events with larger magnitude are better predictable than events with smaller magnitude.
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Crustal Deformation Models and Time-Frequency Analysis of GPS Data from Deception Island Volcano (Sont, whose deviation is reduced down to the deviation of the horizontal components before the denoising. An estimation of the displacements in the network for the period 2001/02 – 2005/06 is also included.
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Template Analysis of the Hide, Skeldon, Acheson Dynamonsition diagrams and generating unstable periodic orbits for the two chaotic examples. We now extend that analysis and use ideas from topology [3] and results from a corresponding analysis of the Lorenz attractor to identify a possible template for the HSA dynamo.
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Methods to Detect Solitons in Geophysical Signals: The Case of the Derivative Nonlinear Schrödinger ld rapidly drop when a signal is close to the .-soliton profile, has been used as a soliton detector. Application of this technique to numerically simulated signals shows that it is more efficient than the standard Fourier transform and can be used as a practical tool for the analysis of outputs from nonlinear systems.
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Detecting Oscillations Hidden in Noise: Common Cycles in Atmospheric, Geomagnetic and Solar Datainear way, so that dynamical modes are identified which are more regular, or better predictable than linearly filtered noise. A number of oscillatory modes are identified in data reflecting solar and geomagnetic activity and climate variability, some of them sharing common periods.
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