Ocean energy is an important and promising renewable energy for the future. Even though extensive technology development and demonstrations have occurred in the areas of ocean thermal energy, wave energy and tidal energy over the last 40 years, commercial plants based on these technologies are very slow in coming up because of the high capital costs. In recent years, due to increase in the fossil fuel costs, renewable energies such as solar photo voltaic systems and wind energy systems have become cost competitive. Ocean energy systems are likely to become cost competitive in a decade or so, especially for remote islands and coastal areas. This chapter presents the highlights of developments in the areas of ocean thermal energy, wave energy and tidal energy.
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Ocean EnergyOcean energy, which is an indirect form of solar energy, is a very large resource. The development and demonstration of ocean energy technology has been suffering all along because of high cost of plant structures and offshore infrastructure. The sharp increase in the oil prices has highlighted, once again, the need to develop large-scale renewable energies including ocean energy.The three forms of ocean energy conversion systems which have reached already a ''technology demonstration'' or ''pre-commercial'' phase are:Ocean thermal energy conversion (OTEC)ii. Wave energy conversion (WEC)iii. Tidal energy conversion (TEC)The highest priority of ocean technologists today is to reassess the techno-economic viability of ocean energy plants vs fossil fuel plants, in the context of high oil price and the available carbon credit.The potential of ocean energy in different regions depends on their geographical location with respect to the equator. Countries closer to the equator having tropical seas around them have good potential for OTEC and countries in northern and southern latitudes have a good potential for wave energy. Tidal energy, caused by gravitational pull of moon and sun on the ocean mass of water, is high only in estuaries and bays where the tidal oscillations are amplified.
Ocean Thermal Energy Conversion
Regional Availability and Current StatusOTEC utilizes the temperature-difference between warm surface sea water of around 27-29 o C in tropical waters and the cold deep sea water of around 5-7 o C, which is available at a depth of 800 to 1000 m, to run a heat engine under Rankine cycle. This temperature differential worldwide and typical temperature depth profiles are shown in Fig. 1 (Ravindran, 2010).The warm surface water exchanges energy with low temperature boiling fluids such as ammonia and