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  2. Marine biogeochemical cycles - Wikipedia

    en.wikipedia.org/wiki/Marine_biogeochemical_cycles

    Water carried into the mantle eventually returns to the surface in eruptions at mid-ocean ridges and hotspots. [131]: 646 Estimates of the amount of water in the mantle range from 1 ⁄ 4 to 4 times the water in the ocean. [131]: 630–634 The deep carbon cycle is the movement of carbon through the Earth's mantle and core.

  3. Human impact on marine life - Wikipedia

    en.wikipedia.org/wiki/Human_impact_on_marine_life

    The surface salinity of the ocean is a key variable in the climate system when studying the global water cycle, ocean–atmosphere exchanges and ocean circulation, all vital components transporting heat, momentum, carbon and nutrients around the world. [84] Cold water is more dense than warm water and salty water is more dense than freshwater.

  4. Ocean stratification - Wikipedia

    en.wikipedia.org/wiki/Ocean_stratification

    The stratified configuration of the ocean can act as a barrier to water mixing, which impacts the efficiency of vertical exchanges of heat, carbon, oxygen, and other constituents. Thus, stratification is a central element of Earth's climate system. Global upper-ocean stratification continued its increasing trend in 2022 and was among the top ...

  5. The Ocean Can Remember for 20 Years, Study Says - AOL

    www.aol.com/lifestyle/ocean-remember-20-years...

    The results of the team’s various models showed that temperature anomalies in the ocean persisted for a full 10 to 20 years before fully dissipating, though the team notes that variability can ...

  6. Effects of climate change on oceans - Wikipedia

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

    The sinking and bacterial decomposition of some organic matter in deep ocean water, at depths where the waters are out of contact with the atmosphere, leads to a reduction in oxygen concentrations and increase in carbon dioxide, carbonate and bicarbonate. [51] This cycling of carbon dioxide in oceans is an important part of the global carbon cycle.

  7. Ocean heat content - Wikipedia

    en.wikipedia.org/wiki/Ocean_heat_content

    The ocean heat content (OHC) has been increasing for decades as the ocean has been absorbing most of the excess heat resulting from greenhouse gas emissions from human activities. [1] The graph shows OHC calculated to a water depth of 700 and to 2000 meters. Ocean heat content (OHC) or ocean heat uptake (OHU) is the energy absorbed and stored ...

  8. Ocean levels are rising faster than ever -- and we're to blame

    www.aol.com/2016-02-25-ocean-levels-are-rising...

    A new study reports that global sea levels could rise more than 4 feet by 2100, thanks to human-induced climate change Ocean levels are rising faster than ever -- and we're to blame Skip to main ...

  9. This Is How to Tell When Your Olive Oil Is Bad

    www.aol.com/tell-olive-oil-bad-201500454.html

    Extra virgin olive oil can go bad a little sooner, after around 12 to 18 months. To know how long your olive oil has been sealed, the most important date to look for on the bottle is the harvest date.