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Other Aspects of Ocean Renewable Energy Chapter | 10 275























































             FIG. 10.3  S2 cotidal chart for the northwest European shelf seas (compare with M2 cotidal
             chart—Fig. 9.12). At locations where the S2 phase equals 0 degrees (thick dashed contours), MHWS
             will always occur at noon and midnight. (Reproduced from S.P. Neill, J.D. Scourse, K. Uehara,
             Evolution of bed shear stress distribution over the northwest European shelf seas during the last
             12,000 years, Ocean Dyn. 60 (5) (2010) 1139–1156, with permission from Springer.)
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