Abstract
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.
Highlights
Climate change is one of the greatest threats to human existence, economic activity, ecosystems, and civil infrastructure (Kim and Choi, 2012)
The simulation results of the climate and hydrological models were further analyzed to quantify the changes in the hydroclimatic variables
The results show that there will be an increase in the mean annual flow for the future period (2070–2100)
Summary
Climate change is one of the greatest threats to human existence, economic activity, ecosystems, and civil infrastructure (Kim and Choi, 2012). Changes in temperature and precipitation and the shift in winter precipitation from snow to rain play an important role in studying impacts of climate change on the hydrology of a catchment. These changes influence the hydrological regime of a stream, and the most serious and widespread potential impact of the changes is flooding (Baltas, 2007; Richardson, 2002; Thornes, 2002).
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