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WATER RESOURCES RESEARCH,
VOL. 42,
W01419,
doi:10.1029/2004WR003772,
2006
Identification of periodic autoregressive moving average models and their application to the modeling of river flows
Yonas Gebeyehu Tesfaye
Graduate Program of Hydrologic Sciences, University of Nevada, Reno, Nevada, USA
Mark M. Meerschaert
Department of Mathematics and Statistics, University of Otago, Dunedin, New Zealand
Paul L. Anderson
Department of Mathematics and Computer Science, Albion College, Albion, Michigan, USA
Abstract
The generation of synthetic river flow samples that can reproduce the essential statistical features of historical river flows
is useful for the planning, design, and operation of water resource systems. Most river flow series are periodically stationary;
that is, their mean and covariance functions are periodic with respect to time. This article develops model identification
and simulation techniques based on a periodic autoregressive moving average (PARMA) model to capture the seasonal variations
in river flow statistics. The innovations algorithm is used to obtain parameter estimates. An application to monthly flow
data for the Fraser River in British Columbia is included. A careful statistical analysis of the PARMA model residuals, including
a truncated Pareto model for the extreme tails, produces a realistic simulation of these river flows.
Received 28
October
2004;
accepted 18
October
2005;
published 31
January
2006.
Keywords: innovation algorithm;
model identification;
parameter estimation;
PARMA model;
river flows;
simulation study.
Index Terms: 1869 Hydrology: Stochastic hydrology; 1860 Hydrology: Streamflow; 1817 Hydrology: Extreme events; 1872 Hydrology: Time series analysis (3270, 4277, 4475).
Read Full Article (file size: 936831 bytes) Cited by
Citation: Tesfaye, Y. G., M. M. Meerschaert, and P. L. Anderson
(2006),
Identification of periodic autoregressive moving average models and their application to the modeling of river flows,
Water Resour. Res.,
42,
W01419,
doi:10.1029/2004WR003772.
Copyright 2006 by the American Geophysical Union.
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