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Finally, a 100-yr return level map for the North Atlantic region is presented.
The m period return level of the residuals of spring discharge is obtained by using a generalized Pareto distribution (GPD).
The 95%% confidence interval of the 100-year return level was calculated using the delta method and the profile likelihood.
The mean expected amplitude of the geolectric field for a 100-year return level is 4.3 V/km.
The estimated return level values obtained by the ACER method are compared to the corresponding values obtained by the annual maxima method and the peaks-over-threshold method.
We thus acquired the spring discharge distribution of extreme values by combining the trend, periodicity and the return level of residuals.
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Return levels were calculated for several return periods and the confidence intervals were constructed for the return levels.
Estimating return levels of extreme wind speeds due to hurricanes presents both practical and analytical difficulties.
We evaluate the hydrological risk in predictions using the estimated return levels.
Scale invariance theory is employed for obtaining short duration return levels from daily data.
Figure 12 shows the return levels of the de-clustered −AL and AU data.
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