Introduced flow variability and its propagation downstream of hydropower stations in Sweden

Hydropower regulations may increase flow variability when compared with the natural hydrological regime, with detrimental impacts on river habitats. Attenuation of the variability improves ecological status at some distance downstream of the introduced variability, and being able to accurately estim...

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Main Authors: Maria Teres Elenius, Göran Lindström
Format: Article
Language:English
Published: IWA Publishing 2022-11-01
Series:Hydrology Research
Subjects:
Online Access:http://hr.iwaponline.com/content/53/11/1321
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author Maria Teres Elenius
Göran Lindström
author_facet Maria Teres Elenius
Göran Lindström
author_sort Maria Teres Elenius
collection DOAJ
description Hydropower regulations may increase flow variability when compared with the natural hydrological regime, with detrimental impacts on river habitats. Attenuation of the variability improves ecological status at some distance downstream of the introduced variability, and being able to accurately estimate this distance is critical for the evaluation of ecological status. The attenuation has only been studied previously for specific rivers, and the dominant mechanisms have not been analyzed in detail. In this work, the attenuation and its important drivers are studied for regulated rivers in all of Sweden by comparing Fourier components and their attenuation based on hydrological and hydraulic models and observations, with comparisons also to lake attenuation. In many rivers, weekly flow variability is dominant among periods up to 1 month, and variability with periodicity days to months attenuates with an exponential rate that is largest for short periods. This is mainly driven by instream processes. Furthermore, regulated systems often resemble cascades with low-gradient river stretches between the dams. The associated attenuation can be described by hydrological models using a linear channel and linear reservoir. In contrast, the sometimes-used diffusion wave equation is often unable to replicate the observed attenuation here. Lakes may contribute significantly to attenuation. HIGHLIGHTS Exponential river attenuation rates are presented.; Attenuation of variability introduced by hydropower is more efficient than what the diffusion wave equation predicts and can be described by a combined linear channel and linear reservoir.; Undisturbed river stretches are nevertheless often not long enough for substantial attenuation.; Lakes have a larger attenuation potential than rivers, especially at low flows.;
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spelling doaj.art-80e59e26813741189918cbb41cd143ea2022-12-22T04:40:00ZengIWA PublishingHydrology Research1998-95632224-79552022-11-0153111321133910.2166/nh.2022.138138Introduced flow variability and its propagation downstream of hydropower stations in SwedenMaria Teres Elenius0Göran Lindström1 Department of Research and Development – Hydrology, Swedish Meteorological and Hydrological Institute, Folkborgsvägen 17, 601 76 Norrköping, Sweden Department of Research and Development – Hydrology, Swedish Meteorological and Hydrological Institute, Folkborgsvägen 17, 601 76 Norrköping, Sweden Hydropower regulations may increase flow variability when compared with the natural hydrological regime, with detrimental impacts on river habitats. Attenuation of the variability improves ecological status at some distance downstream of the introduced variability, and being able to accurately estimate this distance is critical for the evaluation of ecological status. The attenuation has only been studied previously for specific rivers, and the dominant mechanisms have not been analyzed in detail. In this work, the attenuation and its important drivers are studied for regulated rivers in all of Sweden by comparing Fourier components and their attenuation based on hydrological and hydraulic models and observations, with comparisons also to lake attenuation. In many rivers, weekly flow variability is dominant among periods up to 1 month, and variability with periodicity days to months attenuates with an exponential rate that is largest for short periods. This is mainly driven by instream processes. Furthermore, regulated systems often resemble cascades with low-gradient river stretches between the dams. The associated attenuation can be described by hydrological models using a linear channel and linear reservoir. In contrast, the sometimes-used diffusion wave equation is often unable to replicate the observed attenuation here. Lakes may contribute significantly to attenuation. HIGHLIGHTS Exponential river attenuation rates are presented.; Attenuation of variability introduced by hydropower is more efficient than what the diffusion wave equation predicts and can be described by a combined linear channel and linear reservoir.; Undisturbed river stretches are nevertheless often not long enough for substantial attenuation.; Lakes have a larger attenuation potential than rivers, especially at low flows.;http://hr.iwaponline.com/content/53/11/1321hydropowerriver and lake attenuationspectral analysis
spellingShingle Maria Teres Elenius
Göran Lindström
Introduced flow variability and its propagation downstream of hydropower stations in Sweden
Hydrology Research
hydropower
river and lake attenuation
spectral analysis
title Introduced flow variability and its propagation downstream of hydropower stations in Sweden
title_full Introduced flow variability and its propagation downstream of hydropower stations in Sweden
title_fullStr Introduced flow variability and its propagation downstream of hydropower stations in Sweden
title_full_unstemmed Introduced flow variability and its propagation downstream of hydropower stations in Sweden
title_short Introduced flow variability and its propagation downstream of hydropower stations in Sweden
title_sort introduced flow variability and its propagation downstream of hydropower stations in sweden
topic hydropower
river and lake attenuation
spectral analysis
url http://hr.iwaponline.com/content/53/11/1321
work_keys_str_mv AT mariatereselenius introducedflowvariabilityanditspropagationdownstreamofhydropowerstationsinsweden
AT goranlindstrom introducedflowvariabilityanditspropagationdownstreamofhydropowerstationsinsweden