Effects of Climate Change on Runoff Dynamics of Alpine Catchments

Master thesis (2020)

Authors

S. Hanus Civil Engineering & Geosciences

Contributors

M. Hrachowitz Water Resources - CEG (supervisor 1)
G.H.W. Schoups Water Resources - CEG (supervisor 2)
M. Vizcaino Physical and Space Geodesy - CEG (supervisor 2)
H. Zekollari Mathematical Geodesy and Positioning - CEG (supervisor 2)
Faculty
Civil Engineering & Geosciences
Copyright: © 2020 Sarah Hanus
Hydrology Climate change impact Hydrological Modelling Austria Runoff dynamics
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Published Date

27-10-2020

Language

English

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Faculty

Civil Engineering & Geosciences

Abstract

Hydrological regimes of alpine catchments are expected to be strongly influenced by climate change due to their dependence on snow dynamics. While seasonal changes have been studied extensively, studies on changes in the timing and magnitude of annual extremes remain rare. This study investigates the effects of climate change on runoff patterns in six alpine catchments in Austria by using a topography-driven semi-distributed hydrological model and 14 climate projections for both RCP 4.5 and RCP 8.5. The study catchments represent a range of alpine catchments, from pluvial-nival to nivo-glacial, as the study focuses on exploring the effects of climate change on catchments of different altitudes. Simulations of 1981-2010 were compared to projections of 2071-2100 and changes in timing and magnitude of annual maximum and minimum flows as well as monthly discharges and melt were examined. Our results indicate a substantial shift to earlier occurrences in annual maximum flows by 9 to 31 days and an extension of the potential flood season by 1 to 3 months for high elevation catchments. For lower elevation catchments, changes in timing of annual maximum flows are less pronounced. Magnitudes of annual maximum flows are likely to increase, with four catchments exhibiting larger increases under RCP 4.5 than RCP 8.5. The timing of minimum annual discharges shifts to earlier in the winter months for high elevation catchments, whereas for lower elevation catchments a shift from winter to autumn is observed. While all catchments show an increase in mean magnitude of minimum flows under RCP 4.5, this is only the case for four catchments under RCP 8.5. Our results suggest a relationship between the altitude of catchments and changes in timing of annual maximum and minimum flows and magnitude of low flows, whereas no relationship between altitude and magnitude of annual maximum flows could be distinguished. The degree of future change in timing and monthly discharges is larger under RCP 8.5, a change of up to twice as large in monthly discharges is found for RCP 8.5 compared to RCP 4.5.