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  2. Meeting of Waters - Wikipedia

    en.wikipedia.org/wiki/Meeting_of_Waters

    This phenomenon is due to the differences in temperature, speed, and amount of dissolved sediments in the waters of the two rivers. The Rio Negro flows at near 2 km/h (1.2 mph) at a temperature of 28 °C (82 °F), while the Rio Solimões flows between 4 and 6 km/h (2.5–3.7 mph) at a temperature of 22 °C (72 °F). [ 1 ]

  3. Parting of the Waters - Wikipedia

    en.wikipedia.org/wiki/Parting_of_the_Waters

    Parting of the Waters is an unusual hydrologic site at Two Ocean Pass on the Great Divide, within the Teton Wilderness area of Bridger-Teton National Forest, Wyoming, USA. Two Ocean Pass separates the headwaters of Pacific Creek, which flows west to the Pacific Ocean, and Atlantic Creek, which flows east to the Atlantic Ocean.

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  5. List of countries bordering on two or more oceans - Wikipedia

    en.wikipedia.org/wiki/List_of_countries...

    World map of the five-ocean model with approximate boundaries This list of countries which border two or more oceans includes both sovereign states and dependencies , provided the same contiguous territory borders on more than one of the five named oceans , the Pacific , Atlantic , Indian , Southern , and Arctic . [ 1 ]

  6. Open ocean convection - Wikipedia

    en.wikipedia.org/wiki/Open_ocean_convection

    Open ocean convection is a process in which the mesoscale ocean circulation and large, strong winds mix layers of water at different depths. Fresher water lying over the saltier or warmer over the colder leads to the stratification of water, or its separation into layers. Strong winds cause evaporation, so the ocean surface cools, weakening the ...

  7. 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 ...

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  9. Convective mixing - Wikipedia

    en.wikipedia.org/wiki/Convective_mixing

    In fluid dynamics, convective mixing is the vertical transport of a fluid and its properties. In many important ocean and atmospheric phenomena, convection is driven by density differences in the fluid, e.g. the sinking of cold, dense water in polar regions of the world's oceans; and the rising of warm, less-dense air during the formation of cumulonimbus clouds and hurricanes.

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