Trend assessment: applications for hydrology and climate research

The assessment of trends in climatology and hydrology still is a matter of debate. Capturing typical properties of time series, like trends, is highly relevant for the discussion of potential impacts of global warming or flood occurrences. It provides indicators for the separation of anthropoge...

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Main Authors: M. Kallache, H. W. Rust, J. Kropp
Format: Article
Language:English
Published: Copernicus Publications 2005-01-01
Series:Nonlinear Processes in Geophysics
Online Access:http://www.nonlin-processes-geophys.net/12/201/2005/npg-12-201-2005.pdf
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spelling doaj-379731ba3a4c4fa98b516fe09dc819592020-11-24T21:15:27ZengCopernicus PublicationsNonlinear Processes in Geophysics1023-58091607-79462005-01-01122201210Trend assessment: applications for hydrology and climate researchM. KallacheH. W. RustJ. KroppThe assessment of trends in climatology and hydrology still is a matter of debate. Capturing typical properties of time series, like trends, is highly relevant for the discussion of potential impacts of global warming or flood occurrences. It provides indicators for the separation of anthropogenic signals and natural forcing factors by distinguishing between deterministic trends and stochastic variability. In this contribution river run-off data from gauges in Southern Germany are analysed regarding their trend behaviour by combining a deterministic trend component and a stochastic model part in a semi-parametric approach. In this way the trade-off between trend and autocorrelation structure can be considered explicitly. A test for a significant trend is introduced via three steps: First, a stochastic fractional ARIMA model, which is able to reproduce short-term as well as long-term correlations, is fitted to the empirical data. In a second step, wavelet analysis is used to separate the variability of small and large time-scales assuming that the trend component is part of the latter. Finally, a comparison of the overall variability to that restricted to small scales results in a test for a trend. The extraction of the large-scale behaviour by wavelet analysis provides a clue concerning the shape of the trend.http://www.nonlin-processes-geophys.net/12/201/2005/npg-12-201-2005.pdf
collection DOAJ
language English
format Article
sources DOAJ
author M. Kallache
H. W. Rust
J. Kropp
spellingShingle M. Kallache
H. W. Rust
J. Kropp
Trend assessment: applications for hydrology and climate research
Nonlinear Processes in Geophysics
author_facet M. Kallache
H. W. Rust
J. Kropp
author_sort M. Kallache
title Trend assessment: applications for hydrology and climate research
title_short Trend assessment: applications for hydrology and climate research
title_full Trend assessment: applications for hydrology and climate research
title_fullStr Trend assessment: applications for hydrology and climate research
title_full_unstemmed Trend assessment: applications for hydrology and climate research
title_sort trend assessment: applications for hydrology and climate research
publisher Copernicus Publications
series Nonlinear Processes in Geophysics
issn 1023-5809
1607-7946
publishDate 2005-01-01
description The assessment of trends in climatology and hydrology still is a matter of debate. Capturing typical properties of time series, like trends, is highly relevant for the discussion of potential impacts of global warming or flood occurrences. It provides indicators for the separation of anthropogenic signals and natural forcing factors by distinguishing between deterministic trends and stochastic variability. In this contribution river run-off data from gauges in Southern Germany are analysed regarding their trend behaviour by combining a deterministic trend component and a stochastic model part in a semi-parametric approach. In this way the trade-off between trend and autocorrelation structure can be considered explicitly. A test for a significant trend is introduced via three steps: First, a stochastic fractional ARIMA model, which is able to reproduce short-term as well as long-term correlations, is fitted to the empirical data. In a second step, wavelet analysis is used to separate the variability of small and large time-scales assuming that the trend component is part of the latter. Finally, a comparison of the overall variability to that restricted to small scales results in a test for a trend. The extraction of the large-scale behaviour by wavelet analysis provides a clue concerning the shape of the trend.
url http://www.nonlin-processes-geophys.net/12/201/2005/npg-12-201-2005.pdf
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