Kolmogorov complexity based information measures applied to the analysis of different river flow regimes

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Abstract

We have used the Kolmogorov complexities and the Kolmogorov complexity spectrum to quantify the randomness degree in river flow time series of seven rivers with different regimes in Bosnia and Herzegovina, representing their different type of courses, for the period 1965-1986. In particular, we have examined: (i) the Neretva, Bosnia and the Drina (mountain and lowland parts), (ii) the Miljacka and the Una (mountain part) and the Vrbas and the Ukrina (lowland part) and then calculated the Kolmogorov complexity (KC) based on the Lempel-Ziv Algorithm (LZA) (lower-KCL and upper-KCU), Kolmogorov complexity spectrum highest value (KCM) and overall Kolmogorov complexity (KCO) values for each time series. The results indicate that the KCL, KCU, KCM and KCO values in seven rivers show some similarities regardless of the amplitude differences in their monthly flow rates. The KCL, KCU and KCM complexities as information measures do not "see" a difference between time series which have different amplitude variations but similar random components. However, it seems that the KCO information measures better takes into account both the amplitude and the place of the components in a time series.

Figures

  • Figure 1. Relief of Bosnia and Herzegovina with the location of the ten hydrological stations on seven rivers used in the study (the abbreviations for rivers and letters indicating the river regime are given in Table 1).
  • Table 1. Rivers in Bosnia and Herzegovina used in the study with the corresponding flow rates (FR—mean; FRmax—maximal; FRmin—minimal for the period 1965–1985) and their classification following a classification of typology for mountains and other relief classes by [27]: lowland (altitude < 200 m)—(L regime), platforms and hills (200 < altitude < 500 m)— (H regime) and mountains (500 < altitude < 6000 m)—(M regime).
  • Figure 2. Cont.
  • Figure 2. Ten river flow time series of seven rivers in Bosnia and Herzegovina for the period 1965–1986.
  • Table 2. Kolmogorov complexities (lower—KCL, upper—KCU, Kolmogorov complexity spectrum highest value—KCM) and overall Kolmogorov complexity information measure (KCO) values of the flow rate for ten time series of seven rivers in Bosnia and Herzegovina for the period 1965–1986.
  • Figure 3. The dependence of KCL and KCM complexities of river flow rate on altitude, for ten time series of the seven rivers in Bosnia and Herzegovina for the period 1965–1986. Closed contours indicate the river regime: L (blue), H (green) and M (red).
  • Figure 4. Cont.
  • Figure 4. The Kolmogorov complexity spectra for the normalized amplitude of the monthly flow rate time series of the seven rivers in Bosnia and Herzegovina for the period 1965–1986. The circles indicate the regime of river course: L (blue), H (green) and M (red).

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CITATION STYLE

APA

Mihailovic, D. T., Mimic, G., Dreškovic, N., & Arsenic, I. (2015). Kolmogorov complexity based information measures applied to the analysis of different river flow regimes. Entropy, 17(5), 2973–2987. https://doi.org/10.3390/e17052973

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