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246 Fundamentals of Ocean Renewable Energy
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0.8 0.6 0.4 0.2 −0.2 −0.4 −0.6 −0.8 −1 0.8 0.6 0.4 0.2 −0.2 −0.4 −0.6 −0.8 −1 from
1 0 1 0
2.1 2.1
x 10 4 x 10 4
2.08 2.08 (Reproduced
2.06 2.06
2.04 2.04 velocities.
2.02 2.02 east/west
2 Distance along channel (m) 2 Distance along channel (m) to
1.98 1.98 refers
1.96 1.96 sense
1.94 1.94 this
in
1.92 1.92
1.9 1.9 ‘Staggered’
4600 4400 4200 4000 3800 3600 3400 3200 3000 2800 4600 4400 4200 4000 3800 3600 3400 3200 3000 2800 Velocity deficit for staggered (A and B) and regular (C and D) array configurations at peak ebb (B and D) and flood (A and C) for a symmetrical headland
(B) Distance across channel (m) (D) Sound.
Distance across channel (m)
0.8 0.6 0.4 0.2 −0.2 −0.4 −0.6 −0.8 −1 0.8 0.6 0.4 0.2 −0.2 −0.4 −0.6 −0.8 −1 Roc, D. Greaves, K.M. Thyng, D.C. Conley, Tidal turbine representation in an ocean circulation model: towards realistic applications, Ocean Eng. 78 (2014) 95–111,
1 0 1 0 Puget
2.1 x 10 4 2.1 x 10 4 in
2.08 2.08 Inlet
2.06 2.06 Admiralty
2.04 2.04
Distance along channel (m) Distance along channel (m) an
2.02 2.02 idealized
2 2
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1.96 1.96 Elsevier.)
1.94 1.94 bathymetry,
1.92 1.92 from
1.9 1.9 constant
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(A) Distance across channel (m) (C) FIG. a with
Distance across channel (m)