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  2. Ocean acidification - Wikipedia

    en.wikipedia.org/wiki/Ocean_acidification

    The rate at which ocean acidification will occur may be influenced by the rate of surface ocean warming, because warm waters will not absorb as much CO 2. [53] Therefore, greater seawater warming could limit CO 2 absorption and lead to a smaller change in pH for a given increase in CO 2. [53]

  3. Effects of climate change on oceans - Wikipedia

    en.wikipedia.org/wiki/Effects_of_climate_change...

    The majority of ocean heat gain occurs in the Southern Ocean. For example, between the 1950s and the 1980s, the temperature of the Antarctic Southern Ocean rose by 0.17 °C (0.31 °F), nearly twice the rate of the global ocean. [15] The warming rate varies with depth. The upper ocean (above 700 m) is warming the fastest.

  4. Oceanic carbon cycle - Wikipedia

    en.wikipedia.org/wiki/Oceanic_carbon_cycle

    By doing so, the ocean has acted as a buffer, somewhat slowing the rise in atmospheric CO 2 levels. However, this absorption of anthropogenic CO 2 has also caused acidification of the oceans. [8] [10] Climate change, a result of this excess CO 2 in the atmosphere, has increased the temperature of the ocean and atmosphere. [11]

  5. Ocean heat record smashed amid ‘hot tub’ temperatures: ‘The ...

    www.aol.com/ocean-heat-record-smashed-amid...

    Global ocean temperatures have reached a record high, prompting warnings of serious consequences for the Earth’s climate. Reaching an average of 20.96C, according to the EU’s climate change ...

  6. Over a year of astonishing ocean heat has given way to the ...

    www.aol.com/news/over-astonishing-ocean-heat...

    A bleached coral is not dead, but ocean temperatures need to cool off for any hope of recovery. At least 14% of the world’s remaining corals were estimated to have died in the previous two ...

  7. Human impact on marine life - Wikipedia

    en.wikipedia.org/wiki/Human_impact_on_marine_life

    The anthropogenic perturbation occurs on top of an active carbon cycle, with fluxes and stocks represented in the background [123] for all numbers, with the ocean gross fluxes updated to 90 GtC yr−1 to account for the increase in atmospheric CO2 since publication. The carbon stocks in coasts are from a literature review of coastal marine ...

  8. Marine biogeochemical cycles - Wikipedia

    en.wikipedia.org/wiki/Marine_biogeochemical_cycles

    Winds drive ocean currents in the upper 100 meters of the ocean's surface. However, ocean currents also flow thousands of meters below the surface. These deep-ocean currents are driven by differences in the water's density, which is controlled by temperature (thermo) and salinity (haline). This process is known as thermohaline circulation.

  9. A system of ocean currents that transports heat northward across the North Atlantic could collapse by mid-century, according to a new study, and scientists have said before that such a collapse ...