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  2. Solubility pump - Wikipedia

    en.wikipedia.org/wiki/Solubility_pump

    The solubility pump is driven by the coincidence of two processes in the ocean : The solubility of carbon dioxide is a strong inverse function of seawater temperature (i.e. solubility is greater in cooler water) The thermohaline circulation is driven by the formation of deep water at high latitudes where seawater is usually cooler and denser

  3. Continental shelf pump - Wikipedia

    en.wikipedia.org/wiki/Continental_shelf_pump

    the cooler waters promote the solubility pump and lead to an increased storage of dissolved inorganic carbon; this extra carbon storage is augmented by the increased biological production characteristic of shelves [2] the dense, carbon-rich shelf waters sink to the shelf floor and enter the sub-surface layer of the open ocean via isopycnal mixing

  4. Biological pump - Wikipedia

    en.wikipedia.org/wiki/Biological_pump

    These three pumps are: (1) the solubility pump, (2) the carbonate pump, and (3) the biological pump. The total active pool of carbon at the Earth's surface for durations of less than 10,000 years is roughly 40,000 gigatons C (Gt C, a gigaton is one billion tons, or the weight of approximately 6 million blue whales ), and about 95% (~38,000 Gt C ...

  5. European Multidisciplinary Seafloor and water column ...

    en.wikipedia.org/wiki/European_Multidisciplinary...

    Biogeochemistry: ocean acidification and the solubility pump, the biological pump, hypoxia, continental shelf exchange, deep-ocean biogeochemical fluxes. Marine Ecology : climate forcing of ecosystems, molecules to microbes, fisheries, marine noise, deep biosphere , chemosynthetic ecology.

  6. Ocean fertilization - Wikipedia

    en.wikipedia.org/wiki/Ocean_fertilization

    Oceanic carbon naturally cycles between the surface and the deep via two "pumps" of similar scale. The "solubility" pump is driven by ocean circulation and the solubility of CO 2 in seawater. The "biological" pump is driven by phytoplankton and subsequent settling of detrital particles or dispersion of dissolved organic carbon.

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  8. Oceanic carbon cycle - Wikipedia

    en.wikipedia.org/wiki/Oceanic_carbon_cycle

    These three pumps are: (1) the solubility pump, (2) the carbonate pump, and (3) the biological pump. The total active pool of carbon at the Earth's surface for durations of less than 10,000 years is roughly 40,000 gigatons C (Gt C, a gigaton is one billion tons, or the weight of approximately 6 million blue whales ), and about 95% (~38,000 Gt C ...

  9. Marine biogeochemical cycles - Wikipedia

    en.wikipedia.org/wiki/Marine_biogeochemical_cycles

    These three pumps are: (1) the solubility pump, (2) the carbonate pump, and (3) the biological pump. The total active pool of carbon at the Earth's surface for durations of less than 10,000 years is roughly 40,000 gigatons C (Gt C, a gigaton is one billion tons, or the weight of approximately 6 million blue whales ), and about 95% (~38,000 Gt C ...