Available online at www.sciencedirect.com Physica A 330 (2003) 283–290 www.elsevier.com/locate/physa A stochastic model of river discharge uctuations V. Livina a ; ∗ , Y. Ashkenazy b; c , Z. Kizner d , V. Strygin e , A. Bunde f , S. Havlin d a Minerva Center, Bar-Ilan University, Ramat-Gan 52900, Israel b Department of Earth, Atmospheric and Planetary Sciences, Massachusetts Institute of Technology, Cambridge, MA 02139, USA c Department of Environmental Sciences, Weizmann Institute, Rehovot, Israel d Department of Physics, Bar-Ilan University, Ramat-Gan 52900, Israel e Department of Applied Mathematics and Mechanics, Voronezh State University, Universitetskaya pl. 1, Voronezh 394693, Russia f Institute f ur Theoretische Physik III, Justus-Liebig-Universit at Giessen, Heinrish-Bu-Ring 16, 35392 Giessen, Germany Abstract We study the daily river ow uctuations of 30 international rivers. Using the detrended uctu- ation analysis, we study the correlations in the magnitudes of river ow increments (volatilities), and nd power-law correlations in volatilities for time scales less than 1 year; these correlations almost disappear for time scales larger than 1 year. Using surrogate data test for nonlinearity, we show that correlations in the magnitudes of river ow uctuations are a measure for nonlinear- ity. We propose a simple nonlinear stochastic model for river ow uctuations that reproduces the main scaling properties of the river ow series as well as the correlations and periodicities in the magnitudes of river ow increments. According to our model, the source of nonlinear- ity observed in the data is an interaction between a long-term correlated process and the river discharge itself. c 2003 Elsevier B.V. All rights reserved. PACS: 92.40.Cy; 05.40.-a; 02.70.Hm Keywords: Scaling analysis; DFA; Periodic volatility; Long-term volatility; Nonlinearity; Stochastic modeling 1. Introduction The climate system often exhibits irregular and complex behavior. Although the climate system is driven by the well-dened seasonal periodicity, it is also a subject to * Corresponding author. E-mail address: livina@ory.ph.biu.ac.il (V. Livina). 0378-4371/$-see front matter c 2003 Elsevier B.V. All rights reserved. doi:10.1016/j.physa.2003.08.012