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Overview of Game To survive you need to be playing your best game. 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. Both the depth and the distance from shore strongly influence the biodiversity of the plants and animals present in each region.
In addition, many land animals have adapted to living a major part of their life on the oceans. For instance, seabirds are a diverse group of birds that have adapted to a life mainly on the oceans.
They feed on marine animals and spend most of their lifetime on water, many only going on land for breeding. Other birds that have adapted to oceans as their living space are penguins , seagulls and pelicans.
Seven species of turtles, the sea turtles , also spend most of their time in the oceans. A zone of rapid salinity increase with depth is called a halocline.
The temperature of maximum density of seawater decreases as its salt content increases. Freezing temperature of water decreases with salinity, and boiling temperature of water increases with salinity.
If evaporation exceeds precipitation, as is the case in tropical regions, salinity will be higher.
Thus, oceanic waters in polar regions have lower salinity content than oceanic waters in temperate and tropical regions.
Salinity can be calculated using the chlorinity, which is a measure of the total mass of halogen ions includes fluorine, chlorine, bromine, and iodine in seawater.
By international agreement, the following formula is used to determine salinity:. The average chlorinity is about Many of the world's goods are moved by ship between the world's seaports.
Some of the major harvests are shrimp , fish , crabs , and lobster. The motions of the ocean surface, known as undulations or waves , are the partial and alternate rising and falling of the ocean surface.
The series of mechanical waves that propagate along the interface between water and air is called swell.
Although Earth is the only known planet with large stable bodies of liquid water on its surface and the only one in the Solar System , other celestial bodies are thought to have large oceans.
The gas giants , Jupiter and Saturn , are thought to lack surfaces and instead have a stratum of liquid hydrogen ; however their planetary geology is not well understood.
The possibility of the ice giants Uranus and Neptune having hot, highly compressed, supercritical water under their thick atmospheres has been hypothesised.