A long range dependent model with nonlinear innovations for simulating daily river flows

We present the analysis aimed at the estimation of flood risks of Tisza River in Hungary on the basis of daily river discharge data registered in the last 100 years. The deseasonalised series has skewed and leptokurtic distribution and various methods suggest that it possesses substantial long memor...

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Main Authors: P. Elek, L. Márkus
Format: Article
Language:English
Published: Copernicus Publications 2004-01-01
Series:Natural Hazards and Earth System Sciences
Online Access:http://www.nat-hazards-earth-syst-sci.net/4/277/2004/nhess-4-277-2004.pdf
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spelling doaj-2d01890ae0e24c6cb45230fc746ae3062020-11-24T22:08:16ZengCopernicus PublicationsNatural Hazards and Earth System Sciences1561-86331684-99812004-01-0142277283A long range dependent model with nonlinear innovations for simulating daily river flowsP. ElekL. MárkusWe present the analysis aimed at the estimation of flood risks of Tisza River in Hungary on the basis of daily river discharge data registered in the last 100 years. The deseasonalised series has skewed and leptokurtic distribution and various methods suggest that it possesses substantial long memory. This motivates the attempt to fit a fractional ARIMA model with non-Gaussian innovations as a first step. Synthetic streamflow series can then be generated from the bootstrapped innovations. However, there remains a significant difference between the empirical and the synthetic density functions as well as the quantiles. This brings attention to the fact that the innovations are not independent, both their squares and absolute values are autocorrelated. Furthermore, the innovations display non-seasonal periods of high and low variances. This behaviour is characteristic to generalised autoregressive conditional heteroscedastic (GARCH) models. However, when innovations are simulated as GARCH processes, the quantiles and extremes of the discharge series are heavily overestimated. Therefore we suggest to fit a smooth transition GARCH-process to the innovations. In a standard GARCH model the dependence of the variance on the lagged innovation is quadratic whereas in our proposed model it is a bounded function. While preserving long memory and eliminating the correlation from both the generating noise and from its square, the new model is superior to the previously mentioned ones in approximating the probability density, the high quantiles and the extremal behaviour of the empirical river flows.http://www.nat-hazards-earth-syst-sci.net/4/277/2004/nhess-4-277-2004.pdf
collection DOAJ
language English
format Article
sources DOAJ
author P. Elek
L. Márkus
spellingShingle P. Elek
L. Márkus
A long range dependent model with nonlinear innovations for simulating daily river flows
Natural Hazards and Earth System Sciences
author_facet P. Elek
L. Márkus
author_sort P. Elek
title A long range dependent model with nonlinear innovations for simulating daily river flows
title_short A long range dependent model with nonlinear innovations for simulating daily river flows
title_full A long range dependent model with nonlinear innovations for simulating daily river flows
title_fullStr A long range dependent model with nonlinear innovations for simulating daily river flows
title_full_unstemmed A long range dependent model with nonlinear innovations for simulating daily river flows
title_sort long range dependent model with nonlinear innovations for simulating daily river flows
publisher Copernicus Publications
series Natural Hazards and Earth System Sciences
issn 1561-8633
1684-9981
publishDate 2004-01-01
description We present the analysis aimed at the estimation of flood risks of Tisza River in Hungary on the basis of daily river discharge data registered in the last 100 years. The deseasonalised series has skewed and leptokurtic distribution and various methods suggest that it possesses substantial long memory. This motivates the attempt to fit a fractional ARIMA model with non-Gaussian innovations as a first step. Synthetic streamflow series can then be generated from the bootstrapped innovations. However, there remains a significant difference between the empirical and the synthetic density functions as well as the quantiles. This brings attention to the fact that the innovations are not independent, both their squares and absolute values are autocorrelated. Furthermore, the innovations display non-seasonal periods of high and low variances. This behaviour is characteristic to generalised autoregressive conditional heteroscedastic (GARCH) models. However, when innovations are simulated as GARCH processes, the quantiles and extremes of the discharge series are heavily overestimated. Therefore we suggest to fit a smooth transition GARCH-process to the innovations. In a standard GARCH model the dependence of the variance on the lagged innovation is quadratic whereas in our proposed model it is a bounded function. While preserving long memory and eliminating the correlation from both the generating noise and from its square, the new model is superior to the previously mentioned ones in approximating the probability density, the high quantiles and the extremal behaviour of the empirical river flows.
url http://www.nat-hazards-earth-syst-sci.net/4/277/2004/nhess-4-277-2004.pdf
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