strike-slip records, when compared to European and North-American events of similar sizes
and source depths, on normal and oblique faults. This might point to a reason for why the
foreign models fail to describe the PGA of our reference events. Ólafsson’s and
Sigurbjörnsson’s model is also the one that fits best, within the one standard deviation region of
our model D.
Table 1 shows
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be the best way to counterbalance the estimated negative effects of climate change.
In Lake Pielinen the results of this study are already being used in an ongoing
investigation of the possibilities to change the current regulation permit (Verta
et al. 2007). Together with the recent mild winters, the results have already had
some influence on this process and the proposed new regulation scheme
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catchments
are shown in Figure 9; all the others are available in Appendix II (Figures II.1 – 11). In each
plot, the solid blue line shows the evolution of the total snow-fraction over the study period,
while the dashed blue line shows the regression that fits the data best. At the top of each plot,
a percentage change over the 39 years is indicated, calculated as the difference between the
snow
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