Effects of Climate Change and Flow Regulation on the Flow Characteristics of a Low-Relief River within Southern Boreal Climate Area
We investigated how hydro-climatological changes would affect fluvial forces and inundated area during a typical high-flow situation (MHQ, mean high discharge), and how adaptive regulation could attenuate the climate change impacts in a low-relief river of the Southern Boreal climate area. We used h...
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doaj-5b3683308cae4efaaf942babaecc36fb2020-11-24T21:26:23ZengMDPI AGWater2073-44412019-09-01119182710.3390/w11091827w11091827Effects of Climate Change and Flow Regulation on the Flow Characteristics of a Low-Relief River within Southern Boreal Climate AreaElina Kasvi0Eliisa Lotsari1Miia Kumpumäki2Tanja Dubrovin3Noora Veijalainen4Department of Geography and Geology, University of Turku, 20014 Turun Yliopisto, FinlandDepartment of Geography and Geology, University of Turku, 20014 Turun Yliopisto, FinlandFinnish Environment Institute, Latokartanonkaari 11, 00790 Helsinki, FinlandFinnish Environment Institute, Latokartanonkaari 11, 00790 Helsinki, FinlandFinnish Environment Institute, Latokartanonkaari 11, 00790 Helsinki, FinlandWe investigated how hydro-climatological changes would affect fluvial forces and inundated area during a typical high-flow situation (MHQ, mean high discharge), and how adaptive regulation could attenuate the climate change impacts in a low-relief river of the Southern Boreal climate area. We used hydrologically modeled data as input for 2D hydraulic modeling. Our results show that, even though the MHQ will increase in the future (2050−2079), the erosional power of the flow will decrease on the study area. This can be attributed to the change of timing in floods from spring to autumn and winter, when the sea levels during flood peaks is higher, causing backwater effect. Even though the mean depth will not increase notably (from 1.14 m to 1.25 m) during MHQ, compared to the control period (1985−2014), the inundated area will expand by 15% due to the flat terrain. The increase in flooding may be restrained by adaptive regulations: strategies favoring ecologically sustainable and recreationally desirable lake water levels were modeled. The demands of environment, society, and hydropower are not necessarily contradictory in terms of climate change adaptation, and regulation could provide an adaptive practice in the areas of increased flooding.https://www.mdpi.com/2073-4441/11/9/1827climate changestream erosionflood riskhydraulic modelingregulated rivers |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Elina Kasvi Eliisa Lotsari Miia Kumpumäki Tanja Dubrovin Noora Veijalainen |
spellingShingle |
Elina Kasvi Eliisa Lotsari Miia Kumpumäki Tanja Dubrovin Noora Veijalainen Effects of Climate Change and Flow Regulation on the Flow Characteristics of a Low-Relief River within Southern Boreal Climate Area Water climate change stream erosion flood risk hydraulic modeling regulated rivers |
author_facet |
Elina Kasvi Eliisa Lotsari Miia Kumpumäki Tanja Dubrovin Noora Veijalainen |
author_sort |
Elina Kasvi |
title |
Effects of Climate Change and Flow Regulation on the Flow Characteristics of a Low-Relief River within Southern Boreal Climate Area |
title_short |
Effects of Climate Change and Flow Regulation on the Flow Characteristics of a Low-Relief River within Southern Boreal Climate Area |
title_full |
Effects of Climate Change and Flow Regulation on the Flow Characteristics of a Low-Relief River within Southern Boreal Climate Area |
title_fullStr |
Effects of Climate Change and Flow Regulation on the Flow Characteristics of a Low-Relief River within Southern Boreal Climate Area |
title_full_unstemmed |
Effects of Climate Change and Flow Regulation on the Flow Characteristics of a Low-Relief River within Southern Boreal Climate Area |
title_sort |
effects of climate change and flow regulation on the flow characteristics of a low-relief river within southern boreal climate area |
publisher |
MDPI AG |
series |
Water |
issn |
2073-4441 |
publishDate |
2019-09-01 |
description |
We investigated how hydro-climatological changes would affect fluvial forces and inundated area during a typical high-flow situation (MHQ, mean high discharge), and how adaptive regulation could attenuate the climate change impacts in a low-relief river of the Southern Boreal climate area. We used hydrologically modeled data as input for 2D hydraulic modeling. Our results show that, even though the MHQ will increase in the future (2050−2079), the erosional power of the flow will decrease on the study area. This can be attributed to the change of timing in floods from spring to autumn and winter, when the sea levels during flood peaks is higher, causing backwater effect. Even though the mean depth will not increase notably (from 1.14 m to 1.25 m) during MHQ, compared to the control period (1985−2014), the inundated area will expand by 15% due to the flat terrain. The increase in flooding may be restrained by adaptive regulations: strategies favoring ecologically sustainable and recreationally desirable lake water levels were modeled. The demands of environment, society, and hydropower are not necessarily contradictory in terms of climate change adaptation, and regulation could provide an adaptive practice in the areas of increased flooding. |
topic |
climate change stream erosion flood risk hydraulic modeling regulated rivers |
url |
https://www.mdpi.com/2073-4441/11/9/1827 |
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