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2. Opinion - It’s time to ride the marine energy wave - AOL

   www.aol.com/opinion-time-ride-marine-energy...

   The United States is investing in marine energy technology to help meet clean energy goals, with the Marine Energy Technologies Acceleration Act providing $1 billion for research, demonstration ...

3. Direct deep-sea carbon dioxide injection - Wikipedia

   en.wikipedia.org/wiki/Direct_deep-sea_carbon...

   The ocean could potentially hold over a thousand billion tons of CO 2. However, the interest in this avenue of carbon storage has much reduced since about 2001 because of concerns about the unknown impacts on marine life, high costs and concerns about its stability or permanence. [1]

4. Oceanic carbon cycle - Wikipedia

   en.wikipedia.org/wiki/Oceanic_carbon_cycle

   DIC circulates throughout the whole ocean by Thermohaline circulation, which facilitates the tremendous DIC storage capacity of the ocean. [17] The chemical equations below show the reactions that CO 2 undergoes after it enters the ocean and transforms into its aqueous form.

5. Offshore aquaculture - Wikipedia

   en.wikipedia.org/wiki/Offshore_aquaculture

   According to proponents of offshore aquaculture, the wastes from aquafarms that have been moved offshore tend to be swept away and diluted into the open ocean. Moving aquaculture offshore also provides more ecological space where production yields can expand to meet the increasing market demands for fish. Offshore facilities also avoid many of ...

6. Marine energy - Wikipedia

   en.wikipedia.org/wiki/Marine_energy

   Marine energy or marine power (also sometimes referred to as ocean energy, ocean power, or marine and hydrokinetic energy) refers to the energy carried by ocean waves, tides, salinity, and ocean temperature differences. The movement of water in the world's oceans creates a vast store of kinetic energy, or energy in motion.

7. Marine biogeochemical cycles - Wikipedia

   en.wikipedia.org/wiki/Marine_biogeochemical_cycles

   Because of conservation of potential vorticity caused by the poleward-moving winds on the subtropical ridge's western periphery and the increased relative vorticity of poleward moving water, transport is balanced by a narrow, accelerating poleward current, which flows along the western boundary of the ocean basin, outweighing the effects of ...