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Chapter 3





             Tidal Energy







             Tidal energy is presently one of the more favoured forms of marine renewable
             energy because, due to its origins in (astronomical) tide generating forces, it
             is predictable. This is in contrast to other more stochastic renewable energy
             sources such as wind and wave and, in part, solar. However, regardless of its
             predictability, tidal energy shares a key feature with the majority of renewable
             energy sources—it is intermittent, from diurnal (once per day) and semidiurnal
             (twice daily), to fortnightly (spring-neap) timescales. In this chapter, we explain
             the origin of the tides, and how tides evolve as they propagate over shelf
             sea regions. It covers methods of analysing and predicting the tides, and how
             tides can be used to generate electricity through arrays of tidal stream devices,
             and tidal range schemes (lagoons). The primary objective of this chapter is to
             equip those working within or researching marine renewable energy with an
             understanding of the fundamentals of tidal energy from both oceanographic and
             engineering perspectives.


             3.1 TIDE GENERATING FORCES
             Newton’s Law of Universal Gravitation explains how every object in the uni-
             verse attracts every other object with a force that is proportional to the product
             of their masses, and inversely proportional to the square of their distance apart
                                             m 1 m 2
                                       F = G                            (3.1)
                                              r 2
             where F is the force between two masses m 1 and m 2 , G is the gravitational
                                            2
                                    3
             constant (6.674 × 10 −11  m /kg per s ), and r is the distance between the
             centres of the masses (Fig. 3.1).
                In the case of the Earth-Moon system, the Earth and Moon orbit each other
             about their common centre of gravity, and so the gravitational attraction is
                                                     1
             balanced by the outward directed centrifugal force (Fig. 3.2). Because the mass
             of the Earth is two orders of magnitude greater than the mass of the Moon,



             1. The outward directed centrifugal force is an apparent force, whilst centripetal force, the
               component of force acting on a body in curvilinear motion that is directed towards the centre
               of the axis of rotation, is an actual force.
             Fundamentals of Ocean Renewable Energy. https://doi.org/10.1016/B978-0-12-810448-4.00003-3
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