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The spatial structure of European wind storms as characterized by bivariate extreme-value Copulas

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Figure

Fig. 1. Analysis domain is formed by 15 European countries. Eachcresta.org) defined with respect to the distribution of population andcountries is further divided in regions known as CRESTA (www.buildings
Fig. 2. Map of 3 s peak gusts [m s−1] at the variable resolutiongrid (VRG) for storm Daria on 25 January 1990
Fig. 3. Pickands functions and scatter plots of [3]s peak gust from historical reconstruction footprints for location pairs London-Amsterdamand London-Paris.
Fig. 4.Tail dependence χ as a function of distance betweenCRESTA centroids and orientation
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