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Climate impact on floods: changes in high flows in Sweden in the past and the future (1911–2100)

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Figure

Figure 1. Maps showing (a) the four climate regions in Sweden and (b) the locations of the 69 gauges with long-term records from unregu-lated rivers.
Figure 3. Observed versus predicted annual high flow from the S-HYPE model for (a) the calibration period (1999–2008) and (b) thevalidation period (1988–1998)
Table 1. Deviation (%) in relation to the mean for the reference period (1961–1990) and trends (slope in percent per decade) for annualanomalies in high flows at the 69 river gauges, using observed discharge from gauges and S-HYPE modeled discharge, the lat
Figure 5. Modeled deviation (%) in annual regional estimates(1961–2100) versus the reference period (1961–1990) using S-HYPE for annual mean temperature and precipitation, maximumdaily precipitation, annual daily high flow, and number of gaugesexceeding the
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