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  2. Water cycle - Wikipedia

    en.wikipedia.org/wiki/Water_cycle

    The water cycle is powered from the energy emitted by the sun. This energy heats water in the ocean and seas. Water evaporates as water vapor into the air. Some ice and snow sublimates directly into water vapor. Evapotranspiration is water transpired from plants and evaporated from the soil. The water molecule H

  3. Marine biogeochemical cycles - Wikipedia

    en.wikipedia.org/wiki/Marine_biogeochemical_cycles

    This process is known as thermohaline circulation. In the Earth's polar regions ocean water gets very cold, forming sea ice. As a consequence the surrounding seawater gets saltier, because when sea ice forms, the salt is left behind. As the seawater gets saltier, its density increases, and it starts to sink.

  4. Southern Ocean overturning circulation - Wikipedia

    en.wikipedia.org/wiki/Southern_Ocean_overturning...

    The formation of sea-ice is accompanied by brine rejection, resulting in water with a higher salinity and density and therefore buoyancy loss. When ice melts there is a freshwater flow and exposure to the atmosphere. If water turns into ice, there is more salt in the water and less exposure to the atmosphere.

  5. Brinicle - Wikipedia

    en.wikipedia.org/wiki/Brinicle

    A brinicle (brine icicle, also known as an ice stalactite) is a downward-growing hollow tube of ice enclosing a plume of descending brine that is formed beneath developing sea ice. As seawater freezes in the polar ocean, salt brine concentrates are expelled from the sea ice, creating a downward flow of dense, extremely cold, saline water , with ...

  6. Atlantic meridional overturning circulation - Wikipedia

    en.wikipedia.org/wiki/Atlantic_meridional...

    Normally, relatively warm, less-saline water stays on the ocean's surface while deep layers are colder, denser and more-saline, in what is known as ocean stratification. [19] Deep water eventually gains heat and/or loses salinity in an exchange with the mixed ocean layer, and becomes less dense and rises towards the surface.

  7. New phase of water, known as "superionic ice," discovered ...

    www.aol.com/news/phase-water-known-superionic...

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  8. Sea ice - Wikipedia

    en.wikipedia.org/wiki/Sea_ice

    Air volume fraction during ice growth period is typically around 1–2 %, but may substantially increase upon ice warming. [18] Air volume of sea ice in can be as high as 15 % in summer [19] and 4 % in autumn. [20] Both brine and air volumes influence sea-ice density values, which are typically around 840–910 kg/m 3 for first-year ice. Sea ...

  9. EXPLAINER: Water Cube where Phelps ruled turns into Ice ... - AOL

    www.aol.com/news/explainer-water-cube-where...

    Somewhere under the four sheets of curling ice being used for the Beijing Olympics is the swimming pool where Michael Phelps splashed his way to history in the 2008 Summer Games. At first glance ...

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