Climacogram versus autocovariance and power spectrum in stochastic modelling for Markovian and Hurst–Kolmogorov processes
详细信息    查看全文
  • 作者:Panayiotis Dimitriadis…
  • 关键词:Stochastic modelling ; Climacogram ; Autocovariance ; Power spectrum ; Uncertainty ; Bias ; Turbulence
  • 刊名:Stochastic Environmental Research and Risk Assessment (SERRA)
  • 出版年:2015
  • 出版时间:August 2015
  • 年:2015
  • 卷:29
  • 期:6
  • 页码:1649-1669
  • 全文大小:12,567 KB
  • 参考文献:Chen Y, Sun R, Zhou A (2010) An improved hurst parameter estimator based on fractional Fourier transform. Telecommun Syst 43(3/4):197-06View Article
    Dimitriadis P, Koutsoyiannis D, Markonis Y (2012) Spectrum vs climacogram, European Geosciences Union General Assembly 2012, Geophysical Research Abstracts, Vienna, Session HS7.5/NP8.3: Hydroclimatic stochastics, EGU2012-993
    Fleming SW (2008) Approximate record length constraints for experimental identification of dynamical fractals. Ann Phys (Berlin) 17(12):955-69View Article
    Fourier J (1822) Théorie analytique de la chaleur. Firmin Didot Père et Fils, Paris
    Gilgen HJ (2006) Univariate time series in geosciences: theory and examples. Springer, Berlin
    Hassani H (2010) A note on the sum of the sample autocorrelation function. Phys A 389:1601-606View Article
    Hassani H (2012) The sample autocorrelation function and the detection of long-memory processes. Phys A 391:6367-379View Article
    Hurst HE (1951) Long term storage capacities of reservoirs. Trans. Am. Soc. Civil Engrs. 116, 776-08
    Kang HS, Chester S, Meneveau C (2003) Decaying turbulence in an active-grid-generated flow and comparisons with large-eddy simulation. J Fluid Mech 480:129-60View Article
    Khintchine A (1934) Korrelationstheorie der station?ren stochastischen Prozesse. Math Ann 109(1):604-15View Article
    Kolmogorov AN (1941) Dissipation energy in locally isotropic turbulence, Dokl. Akad. Nauk. SSSR 32:16-8
    Koutsoyiannis D (2002) The Hurst phenomenon and fractional Gaussian noise made easy. Hydrol Sci J 47(4):573-95View Article
    Koutsoyiannis D (2003) Climate change, the Hurst phenomenon, and hydrological statistics. Hydrol Sci J 48(1):3-4View Article
    Koutsoyiannis D (2010) A random walk on water. Hydrol Earth Syst Sci 14:585-01View Article
    Koutsoyiannis D (2012) Re-establishing the link of hydrology with engineering, Invited lecture at the National Institute of Agronomy of Tunis (INAT), Tunis
    Koutsoyiannis D (2013a) Encolpion of stochastics: fundamentals of stochastic processes, p 12, Department of Water Resources and Environmental Engineering—National Technical University of Athens, Athens
    Koutsoyiannis D (2013b) Climacogram-based pseudospectrum: a simple tool to assess scaling properties, European Geosciences Union General Assembly 2013, Geophysical Research Abstracts, Vol 15, Vienna, EGU2013-4209, European Geosciences Union
    Lombardo F, Volpi E, Koutsoyiannis D (2013) Effect of time discretization and finite record length on continuous-time stochastic properties, IAHS-em class="EmphasisTypeItalic">IAPSO-em class="EmphasisTypeItalic">IASPEI Joint Assembly, Gothenburg, Sweden, International Association of Hydrological Sciences, International Association for the Physical Sciences of the Oceans, International Association of Seismology and Physics of the Earth’s Interior
    Lombardo F, Volpi E, Papalexiou S, Koutsoyiannis D (2014) Just two moments! A cautionary note against use of high-order moments in multifractal models in hydrology. Hydrol Earth Syst Sci 18:243-55View Article
    Mandelbrot BB (1977) The fractal geometry of nature. Freeman, New York
    Papalexiou SM, Koutsoyiannis D, Makropoulos C (2013) How extreme is extreme? An assessment of daily rainfall distribution tails. Hydrol Earth Syst Sci 17:851-62View Article
    Papoulis A (1991) Probability, random variables and stochastic processes, 3rd edn. McGraw Hill, New York
    Press WH, Teukolsky SA, Vetterling WT, Flannery BP (2007) Numerical recipes: the art of scientific computing, 3rd edn. Cambridge University Press, New York
    Pope SB (2000) Turbulent Flows. Cambridge University Press
    Stoica P, Moses R (2004) Spectral analysis of samples. Prentice Hall, Upper Saddle River
    Tyralis H, Koutsoyiannis D (2011) Simultaneous estimation of the parameters of the Hurst-Kolmogorov stochastic process. Stoch Environ Res Risk Assess 25(1):21-3View Article
    Wiener N (1930) Generalized harmonic analysis. Acta Math 55:117-58View Article
  • 作者单位:Panayiotis Dimitriadis (1)
    Demetris Koutsoyiannis (1)

    1. Department of Water Resources and Environmental Engineering, School of Civil Engineering, National Technical University of Athens, Heroon Polytechneiou 5, 158 80, Zographou, Greece
  • 刊物类别:Earth and Environmental Science
  • 刊物主题:Environment
    Mathematical Applications in Environmental Science
    Mathematical Applications in Geosciences
    Probability Theory and Stochastic Processes
    Statistics for Engineering, Physics, Computer Science, Chemistry and Geosciences
    Numerical and Computational Methods in Engineering
    Waste Water Technology, Water Pollution Control, Water Management and Aquatic Pollution
  • 出版者:Springer Berlin / Heidelberg
  • ISSN:1436-3259
文摘
Three common stochastic tools, the climacogram i.e. variance of the time averaged process over averaging time scale, the autocovariance function and the power spectrum are compared to each other to assess each one’s advantages and disadvantages in stochastic modelling and statistical inference. Although in theory, all three are equivalent to each other (transformations one another expressing second order stochastic properties), in practical application their ability to characterize a geophysical process and their utility as statistical estimators may vary. In the analysis both Markovian and non Markovian stochastic processes, which have exponential and power-type autocovariances, respectively, are used. It is shown that, due to high bias in autocovariance estimation, as well as effects of process discretization and finite sample size, the power spectrum is also prone to bias and discretization errors as well as high uncertainty, which may misrepresent the process behaviour (e.g. Hurst phenomenon) if not taken into account. Moreover, it is shown that the classical climacogram estimator has small error as well as an expected value always positive, well-behaved and close to its mode (most probable value), all of which are important advantages in stochastic model building. In contrast, the power spectrum and the autocovariance do not have some of these properties. Therefore, when building a stochastic model, it seems beneficial to start from the climacogram, rather than the power spectrum or the autocovariance. The results are illustrated by a real world application based on the analysis of a long time series of high-frequency turbulent flow measurements.

© 2004-2018 中国地质图书馆版权所有 京ICP备05064691号 京公网安备11010802017129号

地址:北京市海淀区学院路29号 邮编:100083

电话:办公室:(+86 10)66554848;文献借阅、咨询服务、科技查新:66554700