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  2. Cyclic salt - Wikipedia

    en.wikipedia.org/wiki/Cyclic_salt

    Use of the term "cyclic" refers to the cycle in which the salt moves from sea to land and is then washed by rainwater back to the sea. The salt (and other solid matter) cannot evaporate as water does. Instead it leaves the ocean surface in fine droplets of drop impacts or bubble bursts. Wave-crests and other turbulence form foam.

  3. Marine biogeochemical cycles - Wikipedia

    en.wikipedia.org/wiki/Marine_biogeochemical_cycles

    Many physical processes over ocean surface generate sea salt aerosols. One common cause is the bursting of air bubbles, which are entrained by the wind stress during the whitecap formation. Another is tearing of drops from wave tops. [19] The total sea salt flux from the ocean to the atmosphere is about 3300 Tg (3.3 billion tonnes) per year. [20]

  4. Water cycle - Wikipedia

    en.wikipedia.org/wiki/Water_cycle

    The ocean plays a key role in the water cycle as it is the source of 86% of global evaporation. [2] The water cycle involves the exchange of energy, which leads to temperature changes. When water evaporates, it takes up energy from its surroundings and cools the environment. When it condenses, it releases energy and warms the environment.

  5. The Earth Is Getting Salty - AOL

    www.aol.com/lifestyle/earth-getting-salty...

    The planet’s natural “salt cycle” is speeding up—and new research shows that we are to blame. Skip to main content. Sign in. Mail. 24/7 Help. For premium support please call: ...

  6. Thermohaline circulation - Wikipedia

    en.wikipedia.org/wiki/Thermohaline_circulation

    NADW is formed because North Atlantic is a rare place in the ocean where precipitation, which adds fresh water to the ocean and so reduces its salinity, is outweighed by evaporation, in part due to high windiness. When water evaporates, it leaves salt behind, and so the surface waters of the North Atlantic are particularly salty.

  7. Changes in the Atlantic Ocean Cycle Are Threatening Climate - AOL

    www.aol.com/news/changes-atlantic-ocean-cycle...

    When it flows into the North Atlantic Ocean it is less dense because of the lack of salt. This causes the new water to float and not sink to the bottom, which disrupts the AMOC cycle.

  8. Seawater - Wikipedia

    en.wikipedia.org/wiki/Seawater

    Upon reaching the ocean, these salts concentrated as more salt arrived over time (see Hydrologic cycle). Halley noted that most lakes that do not have ocean outlets (such as the Dead Sea and the Caspian Sea, see endorheic basin), have high salt content. Halley termed this process "continental weathering".

  9. Portal:Oceans - Wikipedia

    en.wikipedia.org/wiki/Portal:Oceans

    The ocean contains 97% of Earth's water and is the primary component of Earth's hydrosphere and is thereby essential to life on Earth. The ocean influences climate and weather patterns, the carbon cycle, and the water cycle by acting as a huge heat reservoir. (Full article...) Waves in Pacifica, California. A sea is a large body of salt water.