6-5 The Impact of Climate Change on Physical Instream Habitats and Its Response to River Morphology

Christoph Hauer , Department for Water – Atmosphere – Environment, Christian Doppler Laboratory for Advanced Methods in River Monitoring, Institute for Water Management, Hydrology and Hydraulic, Vienna, Austria
Günther Unfer , Institut for Hydrobiology and Aquatic Management, Vienna, Austria
Hubert Holzmann , Department for Water – Atmosphere – Environment, IWHW - Institute for Water Management, Hydrology and Hydraulic Engineering, Vienna, Austria
S. Schmutz , Department of Water, Atmosphere & Environment, University of Natural Resources & Life Sciences (BOKU), Vienna, Austria
Helmut Habersack , Christian Doppler Laboratory for Advanced Methods in River Monitoring, Modelling and Engineering, Institute of Water Management, Hydrology and Hydraulic Engineering, University of Natural Resources and Life Sciences, Vienna, Austria
The impact of climate-induced run-off change based on 1951 – 2008 time series was investigated within the crystalline catchment of the Grosse Mühl River in Northern Austria. A significant trend change of aerial temperature, based on Mann-Whitney statistical testing, was recorded for spring 1989 (P = 98.9 %) and summer 1990 (P = 99.9 %). This led to a pronounced increase in summer drought periods. Hydrodynamic-numerical (one-dimensional / two-dimensional) modelling was applied to simulate the changing habitat characteristics due to decreasing run-off in relation to various morphological patterns (riffle-pool / plane-bed reaches). Using bathymetric data, which were sampled on cross sectional measurements, we clearly determined that plane-bed reaches (featureless bed forms) are sensitive to climate-related, reduced run-off, whereas riffle-pool reaches continued to exhibit suitable physical fish habitats even under extreme low-flow conditions. The impact of the decreased summer run-off on instream habitats was especially strong for subadult and adult grayling (target fish species). In situ measurements in microhabitats (velocity / depth) revealed habitat suitabilities. These values were taken as biotic input for habitat evaluation on the micro scale. The findings clearly show that river morphology is a decisive parameter in terms of habitat preservation and restoration in the context of the future impacts of climate change (decreased run-off).