Hydrology and water resources management in a changing world
In: In focus - special book series
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In: In focus - special book series
Alterations in hydrological and thermal regimes can potentially affect salmonid early life stages development and survival. The dewatering of salmon spawning redds due to hydropeaking can lead to mortality in early life stages, with higher impact on the alevins as they have lower tolerance to dewatering than the eggs. Flow-related mitigation measures can reduce early life stage mortality. We present a set of modelling tools to assess impacts and mitigation options to minimise the risk of mortality in early life stages in hydropeaking rivers. We successfully modelled long-term hydrological and thermal alterations and consequences for development rates. We estimated the risk of early life stages mortality and assessed the cost-effectiveness of implementing three release-related mitigation options (A,B,C). The economic cost of mitigation was low and ranged between 0.7% and 2.6% of the annual hydropower production. Options reducing the flow during spawning (B and C) in addition to only release minimum flows during development (A) were considered more effective for egg and alevin survival. Options B and C were however constraint by water availability in the system for certain years, and therefore only option A was always feasible. The set of modelling tools used in this study were satisfactory and their applications can be useful especially in systems where little field data is available. Targeted measures built on well-informed modelling tools can be tested on their effectiveness to mitigate dewatering effects vs. the hydropower system capacity to release or conserve water for power production. Environmental flow releases targeting specific ecological objectives can provide better cost-effective options than conventional operational rules complying with general legislation. ; acceptedVersion ; © 2016. This is the authors' accepted and refereed manuscript to the article. Locked until 5.10.2018 due to copyright restrictions. This manuscript version is made available under the CC-BY-NC-ND 4.0 license http://creativecommons.org/licenses/by-nc-nd/4.0/
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In: Natural hazards and earth system sciences: NHESS, Band 20, Heft 8, S. 2133-2155
ISSN: 1684-9981
Abstract. Climate change is one of the greatest threats currently facing the
world's environment. In Norway, a change in climate will strongly affect the
pattern, frequency, and magnitudes of stream flows. However, it is
challenging to quantify to what extent the change will affect the flow
patterns and floods from small rural catchments due to the unavailability
or inadequacy of hydro-meteorological data for the calibration of
hydrological models and due to the tailoring of methods to a small-scale level. To
provide meaningful climate impact studies at the level of small catchments,
it is therefore beneficial to use high-spatial- and high-temporal-resolution
climate projections as input to a high-resolution hydrological model. In
this study, we used such a model chain to assess the impacts of climate
change on the flow patterns and frequency of floods in small ungauged rural
catchments in western Norway. We used a new high-resolution regional climate
projection, with improved performance regarding the precipitation
distribution, and a regionalized hydrological model (distance distribution
dynamics) between a reference period (1981–2011) and a future period (2070–2100). The flow-duration curves for all study catchments show more wet periods in the future than during the reference period. The results also show that in the future period, the mean annual flow increases by 16 % to 33 %. The mean annual maximum floods increase by 29 % to 38 %, and floods of 2- to 200-year return periods increase by 16 % to 43 %. The results are based on the RCP8.5 scenario from a single climate model simulation tailored to the Bergen region in western Norway, and the results should be interpreted in this context. The results should therefore be seen in consideration of other scenarios for the region to address the
uncertainty. Nevertheless, the study increases our knowledge and understanding of the hydrological impacts of climate change on small
catchments in the Bergen area in the western part of Norway.
In: STOTEN-D-22-00071
SSRN
Floods are among the most damaging of natural disasters, and flood events are expected to increase in magnitude and frequency with the effects of climate change and changes in land use. As a consequence, much focus has been placed on the engineering of structural flood mitigation measures in rivers. Traditional flood protection measures, such as levees and dredging of the river channel, threaten floodplains and river ecosystems, but during the last decade, sustainable reconciliation of freshwater ecosystems has increased. However, we still find many areas where these traditional measures are proposed, and it is challenging to find tools for evaluation of different measures and quantification of the possible impacts. In this paper, we focus on the river Lærdal in Norway to (i) present the dilemma between traditional flood measures and maintaining river ecosystems and (ii) quantify the efficiency and impact of different solutions based on 2D hydraulic models, remote sensing data, economics, and landscape metrics. Our results show that flood measures may be in serious conflict with environmental protection and legislation to preserve biodiversity and key nature types. ; publishedVersion ; This is an open access article distributed under the Creative Commons Attribution License which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.
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