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Chapter 6





             Other Forms of Ocean Energy







             Although the focus of this book is tidal, offshore wind, and wave energy, and
             those topics have been covered in detail in the preceding three chapters, we
             also recognize that there are other forms of ocean energy. These are primarily
             ocean currents (specifically western boundary currents), ocean thermal energy
             conversion (OTEC), and salinity gradient energy. These forms of ocean energy
             are introduced and discussed in limited detail in this chapter, in which we
             outline the main principles, technology types, commercial progress, potential
             environmental impacts, and challenges.


             6.1 INTRODUCTION
             In addition to the forms of ocean energy that were discussed in detail in the
             previous three chapters (tidal, offshore wind, and wave), there are three other
             main types of ocean energy:
             ●  Ocean currents
             ●  Ocean thermal energy conversion (OTEC)
             ●  Salinity gradients
                Although these forms of ocean energy conversion are each limited to
             particular environments (e.g. OTEC is limited to the tropics; see Section 6.3),
             they all have significant potential for electricity generation.



             6.2 OCEAN CURRENTS
             Ocean current energy is the kinetic energy that resides in large-scale open-ocean
             geostrophic surface currents. These currents transfer heat from tropical to polar
             regions, influence weather and climate, distribute nutrients, and disperse marine
             organisms [1]. Because these currents are largely driven by the winds, they
                                                1
             are actually indirect forms of solar energy. The Ocean Energy Council has
             estimated that ocean currents have a globally extractable potential of 450 GW,


             1. Because winds are driven by gradients in air pressure which are a result of variations in solar
               energy received at the surface of the Earth.
             Fundamentals of Ocean Renewable Energy. https://doi.org/10.1016/B978-0-12-810448-4.00006-9
             © 2018 Elsevier Ltd. All rights reserved.                   141
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