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Prominent contributors include dissolved organic matter and chlorophyll. In , scientists announced that for the first time, they had obtained photographic evidence of this glow.
Oceanographers divide the ocean into different vertical zones defined by physical and biological conditions. The pelagic zone includes all open ocean regions, and can be divided into further regions categorized by depth and light abundance.
Because plants require photosynthesis , life found deeper than the photic zone must either rely on material sinking from above see marine snow or find another energy source.
The pelagic part of the photic zone is known as the epipelagic. The pelagic part of the aphotic zone can be further divided into vertical regions according to temperature.
The mesopelagic is the uppermost region. The last zone includes the deep oceanic trench , and is known as the hadalpelagic. The benthic zones are aphotic and correspond to the three deepest zones of the deep-sea.
Lastly, the hadal zone corresponds to the hadalpelagic zone, which is found in oceanic trenches. The pelagic zone can be further subdivided into two subregions: the neritic zone and the oceanic zone.
The neritic zone encompasses the water mass directly above the continental shelves whereas the oceanic zone includes all the completely open water.
In contrast, the littoral zone covers the region between low and high tide and represents the transitional area between marine and terrestrial conditions.
It is also known as the intertidal zone because it is the area where tide level affects the conditions of the region. If a zone undergoes dramatic changes in temperature with depth, it contains a thermocline.
The tropical thermocline is typically deeper than the thermocline at higher latitudes. Polar waters, which receive relatively little solar energy, are not stratified by temperature and generally lack a thermocline because surface water at polar latitudes are nearly as cold as water at greater depths.
Because this deep and cold layer contains the bulk of ocean water, the average temperature of the world ocean is 3.
If a zone undergoes a strong, vertical chemistry gradient with depth, it contains a chemocline. The halocline often coincides with the thermocline, and the combination produces a pronounced pycnocline.
The British naval vessel Challenger II surveyed the trench in and named the deepest part of the trench the " Challenger Deep ".
In , the Trieste successfully reached the bottom of the trench, manned by a crew of two men. Oceanic maritime currents have different origins.
Tidal currents are in phase with the tide , hence are quasiperiodic ; they may form various knots in certain places, [ clarification needed ] most notably around headlands.
Non-periodic currents have for origin the waves, wind and different densities. These currents can decompose in one quasi-permanent current which varies within the hourly scale and one movement of Stokes drift under the effect of rapid waves movement at the echelon of a couple of seconds.
This acceleration of the current takes place in the direction of waves and dominant wind. Accordingly, when the sea depth increases, the rotation of the earth changes the direction of currents in proportion with the increase of depth, while friction lowers their speed.
At a certain sea depth, the current changes direction and is seen inverted in the opposite direction with current speed becoming null: known as the Ekman spiral.
The influence of these currents is mainly experienced at the mixed layer of the ocean surface, often from to meters of maximum depth.
These currents can considerably alter, change and are dependent on the various yearly seasons. If the mixed layer is less thick 10 to 20 meters , the quasi-permanent current at the surface adopts an extreme oblique direction in relation to the direction of the wind, becoming virtually homogeneous, until the Thermocline.
In the deep however, maritime currents are caused by the temperature gradients and the salinity between water density masses.
In littoral zones , breaking waves are so intense and the depth measurement so low, that maritime currents reach often 1 to 2 knots. Ocean currents greatly affect Earth's climate by transferring heat from the tropics to the polar regions.
Transferring warm or cold air and precipitation to coastal regions, winds may carry them inland. Surface heat and freshwater fluxes create global density gradients that drive the thermohaline circulation part of large-scale ocean circulation.
It plays an important role in supplying heat to the polar regions, and thus in sea ice regulation. Changes in the thermohaline circulation are thought to have significant impacts on Earth's energy budget.
In so far as the thermohaline circulation governs the rate at which deep waters reach the surface, it may also significantly influence atmospheric carbon dioxide concentrations.
For a discussion of the possibilities of changes to the thermohaline circulation under global warming , see shutdown of thermohaline circulation.
The Antarctic Circumpolar Current encircles that continent, influencing the area's climate and connecting currents in several oceans.
One of the most dramatic forms of weather occurs over the oceans: tropical cyclones also called "typhoons" and "hurricanes" depending upon where the system forms.
The ocean has a significant effect on the biosphere. Oceanic evaporation , as a phase of the water cycle , is the source of most rainfall, and ocean temperatures determine climate and wind patterns that affect life on land.
Life within the ocean evolved 3 billion years prior to life on land. Apr 12, Well, Yeah a good site. But you can get arrested Jan 21, This website www.
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This game was developed by the developers named as Ubisoft Montreal and released by Ubisoft as well. This game was published in the year and challenges the players to explore the unknown fierce world.
In Far cry 3, the players are let out to explore the Rook island, the whole game revolves around battle and fights.
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