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Titlebook: Nonstationarities in Hydrologic and Environmental Time Series; A. Ramachandra Rao,Khaled H. Hamed,Huey-Long Chen Book 2003 Springer Scienc

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發(fā)表于 2025-3-21 18:05:01 | 只看該作者 |倒序瀏覽 |閱讀模式
書目名稱Nonstationarities in Hydrologic and Environmental Time Series
編輯A. Ramachandra Rao,Khaled H. Hamed,Huey-Long Chen
視頻videohttp://file.papertrans.cn/668/667905/667905.mp4
叢書名稱Water Science and Technology Library
圖書封面Titlebook: Nonstationarities in Hydrologic and Environmental Time Series;  A. Ramachandra Rao,Khaled H. Hamed,Huey-Long Chen Book 2003 Springer Scienc
描述Conventionally, time series have been studied either in the time domain or the frequency domain. The representation of a signal in the time domain is localized in time, i.e . the value of the signal at each instant in time is well defined . However, the time representation of a signal is poorly localized in frequency , i.e. little information about the frequency content of the signal at a certain frequency can be known by looking at the signal in the time domain . On the other hand, the representation of a signal in the frequency domain is well localized in frequency, but is poorly localized in time, and as a consequence it is impossible to tell when certain events occurred in time. In studying stationary or conditionally stationary processes with mixed spectra , the separate use of time domain and frequency domain analyses is sufficient to reveal the structure of the process . Results discussed in the previous chapters suggest that the time series analyzed in this book are conditionally stationary processes with mixed spectra. Additionally, there is some indication of nonstationarity, especially in longer time series.
出版日期Book 2003
關(guān)鍵詞Curve fitting; Fitting; Time series; Wavelet; algorithm; algorithms; calculus; entropy; linearity; marine; mod
版次1
doihttps://doi.org/10.1007/978-94-010-0117-5
isbn_softcover978-94-010-3979-6
isbn_ebook978-94-010-0117-5Series ISSN 0921-092X Series E-ISSN 1872-4663
issn_series 0921-092X
copyrightSpringer Science+Business Media Dordrecht 2003
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沙發(fā)
發(fā)表于 2025-3-21 22:54:25 | 只看該作者
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發(fā)表于 2025-3-22 02:44:42 | 只看該作者
Frequency Domain Analysis,can be identified. The shape of the spectrum also reveals features of the process that are useful in selecting the types of models which are suitable for analyzing the observed data (Jenkins and Watts, 1968).
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發(fā)表于 2025-3-22 06:33:39 | 只看該作者
Time-Scale Analysis,volves a tradeoff. On the one hand a short time window will capture high frequency components and allow for more time localization. On the other hand, a longer window is required to precisely capture low frequency information. Accordingly, a more effective method of analysis would require a variablesize window to be applied to the data.
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發(fā)表于 2025-3-22 09:29:50 | 只看該作者
Data Used in the Book, also taken from Earth Info (1993) database. Tree-ring data are obtained from the National Oceanic and Atmospheric Administration database (NOAA, 1997). The PDSI data are obtained from National Climatic Data Center, NOAA.
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Segmentation of Non-Stationary Time Series,utoregressive (AR) models. It is assumed in these techniques that statistical properties described by a set of AR parameters remain the same in each segment. If these algorithms yield a single series — the original series — then the series is stationary.
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發(fā)表于 2025-3-22 21:26:47 | 只看該作者
Estimation of Turbulent Kinetic Energy Dissipation,e key intrinsic fluid flow parameters is the kinetic energy dissipation rate ε This parameter provides an estimate for the smallest length and time scales relevant to interaction among small scale fluid motion, biological, and chemical particles.
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