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Ocean Energy Overview

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Tidal Barrage

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A dam-like structure that captures the potential energy generated by the height difference between high and low tides.

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Dynamic Tidal Power (DTP)

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A theoretical concept where a long dam (or series of dams) is built perpendicular to the coast, with the potential to capture energy from tidal currents on a grand scale.

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Marine Current Power

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Energy derived from the kinetic energy of marine currents, which are driven by tides and wind.

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Tidal Power

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The harnessing of energy from the natural rise and fall of ocean tides to generate electricity.

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Thermocline

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A layer in a body of water where temperature changes more rapidly with depth than it does in the layers above or below.

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Pelamis Wave Energy Converter

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A wave power generation technology that uses the motion of floating, articulated structures to generate electricity.

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Tidal Stream Generator

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A machine that extracts energy from the kinetic flow of tidal waters, similar functionally to a wind turbine.

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Wave Period

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The time it takes for two successive wave crests or troughs to pass a fixed point.

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Wave Height

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The vertical distance between the crest (the highest point of the wave) and the trough (the lowest point).

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Pressure Retarded Osmosis (PRO)

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A method of generating electricity by using the osmotic pressure difference between fresh water and salt water to produce a pressure that can drive a turbine.

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Wave Frequency

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The number of waves passing a fixed point per unit time, usually measured in hertz (Hz).

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Wave Energy

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Energy captured from surface waves or from pressure fluctuations below the surface.

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Ocean Thermal Energy Conversion (OTEC)

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A process that leverages the temperature difference between cooler deep and warmer shallow or surface seawaters to generate electricity.

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Salinity Gradient Energy

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Power generated from the differential in salt concentration between fresh water and sea water, often using osmosis.

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Reverse Electrodialysis (RED)

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An energy generation process that harnesses the voltage potential across a membrane due to the salinity gradient between saltwater and freshwater.

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