Fractal Analysis of the Long-Term Memory in Precipitation over Bénin (West Africa)

Figure 5

Absolute difference of Hurst exponents and as a function of (q) (where q) is the order of the fluctuation function), q = −3 : 0.5 : 3 at each synoptic station: (a) Cotonou station, (b) Bohicon station, (c) Savè station, (d) Parakou station, (e) Natitingou station, and (f) Kandi station.

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