mercredi 26 février 2014

SEAS AND OCEANS



seas and oceans

The seas and the oceans are  stretches of water salted, unlike wide and soft rivers such as the lakes, the rivers and the rivers.
The seas and the oceans cover  71 % with the surface of the Earth  and play an essential role in the climatic balance of the environment.
In the Northern hemisphere, the seas and the oceans represent 61 % of surface, against 81 % in the Southern hemisphere (also called "marine" hemisphere).

SEAS

The seas are smaller than the oceans. There are 3 types of seas: closed seas, inland seas and seas of the Mediterranean type.
The closed seas are the Caspian Sea and the sea of Aral (in Asia) and the Dead Sea (in the Middle East). These seas, which do not communicate with any other sea nor any ocean, are fed only by rivers. It is in fact of immense salted lakes; salt is there besides in quantity more significant than in the other seas and oceans.
The inland seas open on other seas. It is the case of the Black Sea or North Sea (which gives on the Baltic) (which communicates with the Mediterranean by the Bosphorus in Turkey). These seas are low depth.
Lastly, the seas of the Mediterranean type  are the largest seas and communicate with oceans, as the Mediterranean (which gives on the Atlantic Ocean), the sea of the Philippines (Pacific Ocean), the Caribbean Sea (Atlantic Ocean) or the sea of Arabia (Indian Ocean).

OCEANS

The oceans have for principal characteristics to be of a surface quite higher than that of the seas and to be delimited by several continents.
The Pacific Ocean is largest of all the oceans (165 million km² approximately, is 300 times the size of France) and deepest (more than 11 000 m to the pit of Mariannes). It is delimited in the east by the American continent and the west by Asia and Oceania.
Second by its surface (more than 80 million km²), the Atlantic Ocean  is delimited in the east by Europe and Africa and in the west by the American continent (North America, Central America and South America).
Lastly, the Indian Ocean  (more than 70 million km²) is almost entirely located in the Southern hemisphere. It is bordered in the east by Oceania and Indonesia, in north by India and the west by Africa.
To these three oceans are added the Arctic Ocean  (also called sea Arctic Glaciale because of its dimensions, "small" for an ocean) and the ocean Glacial the Antarctic  (or Antarctic Ocean).
The principal points of passage  between these oceans are:
the Bering Strait: located between Alaska (in the United States) and Russia, it connects the Pacific Ocean to the Arctic Ocean, in the Northern hemisphere;
the Magellan Strait,  Cape Horn  and  the Drake passage: located at the southern point and Chile, they connect the Pacific Ocean to the Atlantic Ocean, in the Southern hemisphere;
the strait of Bass: located at the south of Australia, it connects the Indian Ocean to the Pacific Ocean, in the Southern hemisphere;
the strait of Torres: located between New Guinea-News-Guinea and Australia, it connects the Indian Ocean to the Pacific Ocean, in the Southern hemisphere;
the course of the Needles: located at the southern point of South Africa, it marks the limit between the Indian Ocean and the Atlantic Ocean, in the Southern hemisphere.

MARINE WATER

The water of the seas and the oceans  is naturally salted. The average content salt (35 grams per liter) varies according to the fresh water arrival: the more there is fresh water, the less there is salt, and conversely.
The temperature of the water of the seas and the oceans varies according to  the depth of water,  the latitude  (position compared to the equator) and of the sun contribution , but also of the importance of  the marine currents. The sea waters of the Caribbean, for example, can reach a temperature of 30 °C, while in the Arctic Oceans and the Antarctic, the surface water is below 0 °C all the year.
The tides are a phenomenon which appears by  the rise  (flow) of water on the coasts then their  descent  (the backward flow). This movement is the consequence of the attraction of the Moon and the Sun  on the Earth. The tides function according to  a periodic rate/rhythm  (one or two tides per day). The amplitude  of the tides is more or less significant (the coefficient goes from 20 to 120) and depends on the seas (of 10 cm at sea the Mediterranean with nearly 20 m in the Atlantic Ocean).
The waves are undulatory movements on the surface of marine water, due to the winds. The waves are littoral when they arrive to the coast. If not, they are oceanic waves: one speaks then about  swell, left bearing of surface water on the open sea. More the spacing between two waves and their rate of travel are significant, more the swell is strong. The highest waves can measure up to 30 m (in the Pacific Ocean).
The marine currents are constant or periodic movements marine water: they are due to the winds or are produced by the descent and the rise of water (indeed, the difference of salinity, temperature and density of water causes this type of movements, in-depth). The importance of the currents is capital for the climatic balance of certain areas of the Earth.
The Gulf Stream, for example, is a current heat: it is born on the coasts from the Gulf of Mexico and goes up the North Atlantic at broad coasts of the North-American continent, under the blast pressure of south-west. Then, it deviates towards the east and joined Western Europe (France in particular) to which it brings soft and wet winters; without this marine current, this part of Europe would have the same climate as Canada.

LIFE AND RESOURCES OF THE SEAS AND THE OCEANS

The marine ecosystem particularly rich and is varied. Indeed, water of the seas and the oceans abounds in life, at the same time vegetable (the vegetable plankton and algae) and animal (the animal plankton, of many invertebrates, the fish, marine mammals). They have  considerable, but also energy resources  living  (the energy of the waves and tides for example, used to produce electricity) and  mineral  (oil and the gas).
For a long time, the man largely exploits these resources: they are for example the activities of  fishing  (become industrial to  the xx E century), of  intensive  trade or exploitation of  oil reservoirs  (at sea of North in particular), etc.
However, this exploitation is not without  dangers:  many fish species are threatened, are in process of extinction or disappeared from the seas and the oceans, and  the marine  water pollution became at certain places of planet a true plague.




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