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Sustainability 2016, 8, 1300                                                        8 of 21


                                                        P(kW)
                                                                                                     (8)
                Sustainability 2016, 8, 1300      c=     e          [ ]m                            8 of 21
                                                   w
                                                       P(kW / m)
                                                        w
                    The performances of AquaBuoy, Pelamis, AWS and Wave Dragon were evaluated in the most
                     The performances of AquaBuoy, Pelamis, AWS and Wave Dragon were evaluated in the most
                energetic points on the 50 m water depth between those selected in this work and compared with
                energetic points on the 50 m water depth between those selected in this work and compared with
                seven EU oceanic offshore locations whose scatter matrix were available in the open literature. These
                seven EU oceanic offshore locations whose scatter matrix were available in the open literature.
                locations are: São Jorge in Azores Island [59], Madeira Island [29], Nazarè-Peniche and Sines-Aljezur in
                These locations are: São Jorge in Azores Island [59], Madeira Island [29], Nazarè-Peniche and
                Portugal [42], Belmullet in Ireland [60], Ile d’Yeu in France [61], and Cornish Coast in United Kingdom
                Sines-Aljezur in Portugal [42], Belmullet in Ireland [60], Ile d’Yeu in France [61], and Cornish Coast in
                [62].
                United Kingdom [62].
                    The performances of the Oyster and Wave Star were evaluated in the four nearshore hotspots
                     The performances of the Oyster and Wave Star were evaluated in the four nearshore hotspots and
                and compared with the nearshore location at Madeira Island [29].
                compared with the nearshore location at Madeira Island [29].
                4. Wave Energy Assessments
                4. Wave Energy Assessments
                    The spatial distribution of the offshore wave power for the whole Mediterranean Sea is shown
                     The spatial distribution of the offshore wave power for the whole Mediterranean Sea is shown in
                in Figure 3 (mean values related to the used hindcasting period). The higher values (above 10 kW/m)
                Figure 3 (mean values related to the used hindcasting period). The higher values (above 10 kW/m) are
                are  located  in the Central Mediterranean and the  maximum value, which reaches  16.4 kW/m, is
                located in the Central Mediterranean and the maximum value, which reaches 16.4 kW/m, is located
                located between Corsica Island,  Sardinia Island and the Balearic Islands. In the  Eastern
                between Corsica Island, Sardinia Island and the Balearic Islands. In the Eastern Mediterranean Sea,
                Mediterranean Sea, the wave power values are between 6 and 9 kW/m. The lower values are located
                the wave power values are between 6 and 9 kW/m. The lower values are located in the Adriatic Sea
                in the Adriatic Sea (below 2 kW/m).
                (below 2 kW/m).











                   Figure 3. Yearly mean wave power spatial distributions (kW/m) during the analyzed hindcasted period.
                     Figure 3. Yearly mean wave power spatial distributions (kW/m) during the analyzed hindcasted period.
                    Similar analyses, still based on numerical wave hindcasting as done in the present study, have
                     Similar analyses, still based on numerical wave hindcasting as done in the present study, have been
                been conducted by Liberti et al. [17] and Besio et al. [19]. It is worth noting that, although the length
                conducted by Liberti et al. [17] and Besio et al. [19]. It is worth noting that, although the length of the
                of the hindcasted periods used are very different, the results in terms of the spatial distribution and
                hindcasted periods used are very different, the results in terms of the spatial distribution and local
                local magnitudes of the yearly mean wave power are almost identical among all the three studies.
                magnitudes of the yearly mean wave power are almost identical among all the three studies.
                    The spatial distribution of the nearshore wave power at the four studied areas are depicted in
                     The spatial distribution of the nearshore wave power at the four studied areas are depicted
                Figures 4b, 5b, 6b and 7b, while Figures 4a, 5a, 6a and 7a show the location of the points (Pi) used as
                in Figures 4b, 5b, 6b and 7b, while Figures 4a, 5a, 6a and 7a show the location of the points (Pi)
                offshore boundary conditions and the location of points, on water depths of 50 m and 15 m, where the
                used as offshore boundary conditions and the location of points, on water depths of 50 m and 15 m,
                wave powers are plotted as wave roses and the maximum values are summarized in Table 2. Following
                where the wave powers are plotted as wave roses and the maximum values are summarized in Table 2.
                Cornett [6], the coefficients that aim to describe the temporal fluctuation of the wave power were
                Following Cornett [6], the coefficients that aim to describe the temporal fluctuation of the wave power
                also computed (COV Equation (3), SV Equation (4) and MV Equation (5)).
                were also computed (COV Equation (3), SV Equation (4) and MV Equation (5)).
                    In the case of the Tuscany (Figure 4), the wave power decreases during the propagation toward
                     In the case of the Tuscany (Figure 4), the wave power decreases during the propagation toward the
                the coastal waters except at a location in front of Livorno where it reaches values higher than those
                coastal waters except at a location in front of Livorno where it reaches values higher than those along
                along the offshore boundary (Figure 4b). This is clearly related to wave focusing due to refraction
                the offshore boundary (Figure 4b). This is clearly related to wave focusing due to refraction processes
                processes that are triggered by the presence of the Meloria shoals (Figure 4a). This hotspot is located
                that are triggered by the presence of the Meloria shoals (Figure 4a). This hotspot is located in 10 m of
                in 10 m of water depth (Table 2) about 1400 m shoreward of point 9. The mean wave power reaches
                water depth (Table 2) about 1400 m shoreward of point 9. The mean wave power reaches 4.7 kW/m,
                4.7 kW/m, a value about 25% larger than the value at the closer offshore boundary points P4 (3.6
                a value about 25% larger than the value at the closer offshore boundary points P4 (3.6 kW/m) and
                kW/m) and P5 (3.9 kW/m). It is worth noting that at a distance of 1.5 km around this hotspot the
                P5 (3.9 kW/m). It is worth noting that at a distance of 1.5 km around this hotspot the wave power
                wave power  potentials dramatically decrease. This result motivates the necessity of high spatial
                potentials dramatically decrease. This result motivates the necessity of high spatial resolution for the
                resolution for the assessment of wave energy potentials in order to locate the most promising site for
                assessment of wave energy potentials in order to locate the most promising site for wave energy pilot
                wave energy pilot plants. The COV values everywhere are lower than 1.7, the SV values everywhere
                plants. The COV values everywhere are lower than 1.7, the SV values everywhere are below 1 and the
                are below 1 and the MV values are lower than 1.8 on water depths below 20 m.
                MV values are lower than 1.8 on water depths below 20 m.
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