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Future evolution and uncertainty of river flow regime change in a deglaciating river basin

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Figure

Figure 1. Location of the Virkisá river basin in Iceland withand detailed topographical map of the basin including major landsurface types as well as meteorological and stream gauging sta-tionsglaciated areas highlighted in grey (a), location of Öræfajökull (b), (c).
Figure 3. Example of the advanced delta-change approach when applied to near-surface air temperature data based on the RCP8.5 projectionsusing the CNRM-CM5 GCM and CCLM4-8-17 RCM
Table 1.calibration and evaluation procedure.
Figure 4. Capture ratio projected onto observed river dischargeFDCdashed black line. Also shown are the range of acceptability scoresfor each of the available river discharge signatures over the evalu-ation perioddata during evaluation period for 2015 (a),
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