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  2. Ocean thermal energy conversion - Wikipedia

    en.wikipedia.org/wiki/Ocean_thermal_energy...

    Ocean thermal energy conversion (OTEC) is a renewable energy technology that harnesses the temperature difference between the warm surface waters of the ocean and the cold depths to run a heat engine to produce electricity. It is a unique form of clean energy generation that has the potential to provide a consistent and sustainable source of power.

  3. Marine energy - Wikipedia

    en.wikipedia.org/wiki/Marine_energy

    Marine energy, also known as ocean energy, ocean power, or marine and hydrokinetic energy, refers to energy harnessed from waves, tides, salinity gradients, and temperature differences in the ocean. The movement of water in the world's oceans stores vast amounts of kinetic energy , which can be converted into electricity to power homes ...

  4. Sulfate-methane transition zone - Wikipedia

    en.wikipedia.org/wiki/Sulfate-methane_transition...

    The SMTZ is a major sink for methane because AOM consumes mostly all of the methane produced by methanogens. [7] It has been shown that AOM takes up over 90 percent of all the methane produced in the ocean. [12] Since methane is a prominent greenhouse gas, AOM is especially vital to controlling the amount of greenhouse gases in the atmosphere. [13]

  5. Atmospheric carbon cycle - Wikipedia

    en.wikipedia.org/wiki/Atmospheric_carbon_cycle

    Methane (CH 4) is one of the more potent greenhouse gases and is mainly produced by the digestion or decay of biological organisms. It is considered the second most important greenhouse gas, [10] yet the methane cycle in the atmosphere is currently only poorly understood. [11] The amount of methane produced and absorbed yearly varies widely. [10]

  6. Oceanic carbon cycle - Wikipedia

    en.wikipedia.org/wiki/Oceanic_carbon_cycle

    Sedimentation is a long-term sink for carbon in the ocean, as well as the largest loss of carbon from the oceanic system. [43] Deep marine sediments and geologic formations are important since they provide a thorough record of life on Earth and an important source of fossil fuel. [ 43 ]

  7. Biological pump - Wikipedia

    en.wikipedia.org/wiki/Biological_pump

    Once this carbon is fixed into soft or hard tissue, the organisms either stay in the euphotic zone to be recycled as part of the regenerative nutrient cycle or once they die, continue to the second phase of the biological pump and begin to sink to the ocean floor. The sinking particles will often form aggregates as they sink, which greatly ...

  8. Methane chimney - Wikipedia

    en.wikipedia.org/wiki/Methane_chimney

    Frozen methane bubbles from thawing permafrost. Large deposits of frozen methane, when thawing, release gas into the environment. [3] In cases of sub-sea permafrost, the methane gas may be dissolved in the seawater before reaching the surface; however, in a number of sites around the world, these methane chimneys release the gas directly into the atmosphere, contributing to global warming. [4]

  9. Cold seep - Wikipedia

    en.wikipedia.org/wiki/Cold_seep

    The benthic filter cannot affect methane that is not traveling through the sediment. Methane can bypass the benthic filter if it bubbles to the surface or travels through cracks and fissures in the sediment. [7] These organisms are the only biological sink of methane in the ocean. [8]