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Sea currents in atlantic

ATLANTIC OCEAN

Atlantic ocean

Gretz. Historian Herodotus, V v. BC e., zgadu sea Atlantis, ancient Rome. author Pliniy, I v., Atlantic Ocean (Oceanus Atlanticus) ... The name is tied with walnuts. myth about the titan Atlant, trimati on his shoulders the heavenly crypt, the place where the Greeks respected the extreme 3. (Niblingch to Atlanta) I will call it the Atlantic Ocean. A presentation about the Atlantic Ocean in yogo bitch rosumіnnі leached until the middle of the XVII v. Div. also Pivnichne sea.

Geographic name of the light: Toponymic vocabulary. - M: AST... Pospulov E.M. 2001.

ATLANTIC OCEAN

rozstashovany zdebіlshy in zap. pіvkulі, run out of pіvnochі on pіvday at 16000 km. Area 91.56 km2, middle glybin 3600 m, naybilsha - 8742 m.Omivaє Sivshi. i Pd. America, Antarctica, Africa, Europe. Widely tied with usima by the oceans. All in. The coastal line is strongly divided, 13 seas. Through the entire ocean, stretching the Mid-Atlantic ridge with a height of approx. 2000 km, with a rift valley up to 30 km wide. Before the rifts are dated to the events of the volcano. Iceland and Azores. The area of ​​the shelf is larger, lower in the Pacific Ocean. On the shelf of the Pivnichnaya Sea, in the Mexican, Guineyskiy, Biskayskiy, Venezuelan inflows - naphtha, in the United Kingdom and Florida - rossy tin, diamonds - in the Pivdenno-Zal. Africa, phosphorites - the coast of tropical Africa, the jelly-manganese concretion - in Florida and Newfoundland. Rosetting for all climatic belts... Nybilsh suvori pivd. r-no. Technical: Pivn. Pasatne, Golfstrom, North Atlantic (warm), Kanarska (cold) Pd. Pasatne, Brazilian (warm). Zap. Vєtrov, Benguela (cold). The zonality of water masses will be severely destroyed by leaks and overflowing land. The salinity of the fish, lower in the other oceans, so how to drink a vologue rush to the continents. temperature surface waters lower, lower in the Pacific Ocean, through the Arctic inflow. It does not freeze only in winter, but in other specific inflows and seas of Eurasia. A large number of icebergs and floating ice in the north and south are characteristic. organic light bednishim, lower in the Quiet. The shelf districts have a lot of bottom and bottom ribs, the resources of those from them are hanging.

Short geographic vocabulary... EdwART. 2008.

Atlantic ocean

the other is beyond the magnitude (from the Pacific Ocean) to the Earth. The name is tied to the ancient walnut myth about the titan Atlanta. Sowshi. boundary to Z. vid Greenland walk 70 ° Mon. Iceland and far to Faroeseі Shetland about-to you - at 61 ° Mon. to uzberezhzh Scandinavian p_vostrov ... On the west coast of the continent Sivsha. i Pd. America, in the east - to the Uzbeks of Europe and Africa to Misu Golkovy, far to the south of the south along the meridian of 20 ° of the western direction. NS. Pl. (To the level of the Atlantic sector of the Pivdenny Ocean), the road is 91.7 million km², the length (along the meridian 30 °) is approx. 12.5 yew Km, naib. width (parallel to 30 ° N) 6.7 yew. km. Max. depth of 8742 m (Puerto Riko trough), middle 3600 m. communicate to internal, most: Karibske, Middle ground, Pivnichne, chorne, Baltiyske... Most inflows: mexican, Biskaysky... The main islands (zagalnaya square 1070 thousand sq. Km) have been roasted off the mainland: Great Britain , Ireland , Newfoundland , Bol. і Small. Antilsk , Kanarski, green misu, Falklands... V into the ocean there are small islands of volcanic hiking ( Azorski, holy yleni, Tristan da Cunha ta in.). OK. 10% of the ocean is borrowed by a shelf with a width of dozens of decils up to 400 km or more (in the Pivnichny Sea). The mainland has grasped the slopes, sprinkled with sub-water canyons, in the middle of them the Hudson is the largest. In the middle. h. from the ocean from Iceland at winter to about. Bouvet in the south of the Mayzhe along the axis of the symmetry ocean stretches the Mid-Atlantic Ridge with dimples above it approx. 3000 m, which repeats the contours of the mainland shores.
V in the middle latitudes ah over A. o. panuyut app. vіtri, in tropical - skh. (Pasati). To the northwest. parts of sov. West Indian hurricanes. All in. h. іnu tighter heat Golfstrom , Yake trivaє Pivnichno-Atlantic Plin ... At the same time cold Kanarsky i warm Sowshi. Pasatnoi the leaks of the stench make up the sows. anticlonic cycle of ocean waters. Sowshi. the cyclonic circulation is stored from the warm flows of the Pivnichno-Atlantic, Irmingerі cold Labrador... Near the tropical zones of the ocean, ocean vikhori are not often found - a circuit of water with a diameter of 150-200 m, the stench of the water rises up to a glibine of 1.5 km.
Tim-ra drives on the surface in conjunction with 28 ° C at the ekvatorі to 6 ° C in the north, up to 26 and 10 ° C. Salinity 34-37.3 ‰. Max. pour into the hall. Fundi reach 18 m. seas and tributaries ( Baltiyske, Azovske, St. Lawrence ta in.); through the Greenland and Baffin Seas to A. about. to wine a lot of ice and icebergs from Sivsha. Freezing the ocean. Lead the ocean inhabited by approx. 2000 views of roslin and tvarin, 15 yew. View ribs, approx. 100 species of whales and pinnipeds. V tropical belt live jellyfish, crabs, flying ribs, sharks, sea turtles, sperm whales; in the middle and cold zones - crayfish and molluscs, sedge, tricky and flounder ribs, whales, pinnipeds and іn. There are few sea birds. A. about. yesє approx. 35% of the white ribby catch (Atlantic triska, capelin, oseledets, European anchovy, blue whiting).
Nafta and gas vidobuvayut on the shelf in Venezuelan, Mexican, Guineyskiy tributaries, in the Pivnichnoe and Seredzemny Seas. Bilya shores of Brazil and the United States - great births of ilmenite, zircon, monocyte, rutile; on the shelf pivdenno-zap. Africa - diamonds. Near the Mexican hall. there is a sub-water videotap of the sea, bilya shores of Newfoundland, Finland and Normandy - rail. ore, in the coastal waters of Canada and Great Britain - cam. vugillya. On a part of A. about. brought to 2/3 of the obsyagu of the light sea trade. Naybilsh zhvavi oceanskih highways pass between 35-40 and 55-60 ° Mon. Most important ports: Rotterdam , NY , H'uston , New orleans , Marseilles , Le Havre , Hamburg , Genoa , London , Buenos Aires , St. Petersburg , Novorosisk , Іllichivsk , Odessa .

Glossary of current geographical names. - Yekaterinburg: U-Factoria. Under the editorship of Acad. V. M. Kotlyakova. 2006 .

Atlantic ocean

the other is beyond the magnitude (from the Pacific Ocean) to the Earth. Yogo sіvshi. the border in Greenland pass at 70 ° N. sh., and on the way out of it - from Misu Brewster to Iceland and far to the Faroese and Shetland Islands at 61 ° N. NS. to the Uzbek coast of Norway, from the other to the Norwegian and Greenland seas of Sivsha. Freezing the ocean. To the west, the Atlantic Ocean is surrounded by the Sivsha shores. i Pd. America, in the east - to the Uzbeks of Europe and Africa to Misu Golkovy, far to the south of the yogo between slid along the meridian of 20 ° sk. e. In the south to be angry with the waters of the Pivdenny Ocean; a clearing boundary between them to serve as a ruhoma zone pivd. subtropical convergence, passing approximately parallel to 40 ° S. NS.
Ancient Greek. Historian Herodotus in the 5th century BC That is, behind the Atlantis sea, the ancient writer of Pliniy in the 1st century. n. e. - Atlantic Ocean (Oceanus Atlanticus). The name is tied with the myth about the titan Atlanta, trimati on his shoulders the heavenly crypt, - behind him stretching the ocean, a part of which, closest to Atlantis, I named the Atlantic Ocean.
The area of ​​the Atlantic Ocean with the urahuvannya of the Atlantic sector of the Pivdenny Ocean is 91.7 million km2, length (along the meridian 30 °) approx. 12.5 yew Km, best lat. (Parallel 30 °) 6.7 yew. Km, naymensha - 2.8 yew. Km. Max. glib. 8742 m (Puerto-Rico jolob), time. glib. 3600 m.
Most of the seas of the Atlantic Ocean are carried to the inland. most seas and inflows: Karibske, Seredzemne, Mexicanska inflow, Pivnichne, Chorne, Baltiyske, Biskayska inflow. Main the islands of the mainland coastlines: Great Britain, Ireland, Newfoundland, Great and Small Antilles, Canarsky, Green Misu Islands, Falklands (Malvinsky). In the open part of the ocean, there are small islands of volcanic hiking: Azorsk, Svyatoi Eleni, Tristan da Cunya і іn., And also corals, for example. Bahamas Islands. Zagalna square islands 1070 yew. km².
OK. 10% of the Atlantic Ocean loan shelf lat. from dozens of decils up to 300 (in the arm of the Amazon) and 400 km (from the Argentine Uzbek). Shelf zones near Scandinavia and in the Pivnichny Sea stretch for hundreds of kilometers. The mainland has grasped the slopes, sprinkled with sub-water canyons, in the middle of them the Hudson is the largest. ON WEDNESDAY. parts of the ocean from Iceland (in the north) to about. Bouvet (in the south), the S-shaped Mid-Atlantic Ridge stretches along the symmetry axis of the ocean. with glibines above it approx. 3000 m, which repeats the contours of the mainland shores.
Above the Atlantic Ocean, two centers of the atmosphere have developed - the Icelandic minimum and the Pivnichno-Atlantic maximum; two similar centers in the Atlantic sector of the European Ocean. In the middle latitudes over the ocean, there is a strong pang. vіtri, and in subtropical latitudes - pіvnіchno-schіdnі. і pіvdenno-cx. vіtri ( passati). Most dim in the middle latitudes of the Pd. pіvkulі, I will call it "stormy forties". All in. tropical latitudes of the so-called. West Indian hurricanes.
All in. parts of the Atlantic Ocean, the system of warm leaks is tight Golfstrom, The contours of how constantly change. The Gulfstrom system at once to its progress - the Pivnichno-Atlantic Plin - approved by the West. and sіvshi. the periphery of the sows. anti-cyclonic circulation. Cx. the periphery of the cycle becomes a cold Canary current, the pivdenna - a warm Pivnich Pasatnoy current. Sowshi. the cyclonic circulation is stored with warm leaks - Pivnichno-Atlantic and Irminger and cold Labrador. In the tropical zones of the ocean, it is not easy to find ocean vichoris - a circuit of water diam. 150-200 m, the stench will burst into the water from the surface to the slope. 1.5 km.
Timing of water on the surface is charged from 28 ° C at the equator to 6 ° C at 60 ° C. sh., up to 26 and 10 ° C. Salinity 34-37.3 ‰. Max. float in the zatotsi fundi reach 18 m. parts of the ocean sea ​​ice zustr_chayutsya at the ext. seas (Baltiyske, Pivnichne and іn.), across the Greenland and Baffin Seas into the Atlantic Ocean to wine a lot of ice and icebergs from Sivshi. Freezing the ocean.
The Atlantic Ocean is inhabited by approx. 2000 views of roslin and tvarin, 15 yew. View ribs, approx. 100 species of whales and pinnipeds. Jellyfish, crabs, flying ribs, sharks, sea turtles, sperm whales live near the tropical zone of the ocean; in the middle and cold zones - crayfish and molluscs, sedge, tricky and flounder ribs, whales, pinnipeds and іn. There are few sea birds. Atlantic Ocean yesє approx. 35% of the catch is ribe, mainly Atlantic triska, capelin, oseledets, European anchovy, blue whiting, shrimp, oysters, honey.
Nafta and gas are produced on the shelf in the Venezuelan, Mexican, Guinean inflows, in the Pivnichny and Middle-earth seas. Bilya shores of Brazil and the USA (Peninsula Florida) - great genera of ilmenite, zircon, monocyte, rutile, in the northwest. Afritsy shoot diamonds. The Mexican plant has a double-sided videotape of the waters of Newfoundland, Finland and Normandy - gold ore, In the coastal waters of Canada and Great Britain - Kam'yanovy Vugilla.
On a part of the Atlantic Ocean attackє to 2 / 3 obsyagu svitovoy sea trade. Naygustish and zhvava of the ocean nobles pass between 35-40 and 55-60 ° N. NS. Most important ports: Rotterdam, Amsterdam (Netherlands), Antwerp (Belgium), New York, H'uston, New Orleans (USA), Marseille, Le Havre (France), Hamburg, Bremen (Nimechchina), Genoa (Italy), London ( Great Britain), Bergen (Norway), Buenos Aires (Argentina), Novorossiysk, St. Petersburg (Russia), Illichivsk, Odessa (Ukraine).

Geography. The encyclopedia is now well illustrated. - M .: Rosmen. Edited by prof. A. P. Gorkina. 2006 .

Atlantic ocean

part of the Svitovoy ocean, surrounded by Europe and Africa from the outset and the Old and New America from the sunset. Its name is imovirno to resemble from the Atlantean mountains to the mountains of Africa, or from the mythical bending continent of Atlantis.
The Atlantic Ocean is sacrificing for the size of the Pacific; of this area to become approximately 91.56 million km2. From the other oceans of the second generation, the coastal line is very rugged, which confirms the number of seas and inflows, especially in the private part. In addition, the total area of ​​the basin is a rychok, which flows into the whole ocean of either the edge of the sea, significantly more, below the rychok, which flows into what might be the ocean. In the same view of the Atlantic Ocean, there is an altogether small number of islands and foldable bottom relief, as well as on the submarine ridges and uplifts that create a lifeless environment.
PIVNICHNA CHASTINA ATLANTIC OCEANU
Between that coastal line. The Atlantic Ocean extends into private and private parts, and between them is cleverly defined according to the rules. From the oceanographic point of view, however, until the first part of the ocean, there was an ekvatorialny prototype, but it was rosted at 5-8 ° C. Mysciami tsya between them is designated by sub-water ridges.
Near the Pivnichniy Pivkul, the Atlantic Ocean is heavily crumbling along the coastline. Yogo shodo vuzka pivnichna chastina z'unnuetsya s pivnichny Freezing ocean trioma with narrow ducts. On the pivnichny descent of the Devis channel, 360 km wide (at the latitude of the Pivnichny Polar Stake), across the Buffin Sea, it lies to the Pivnichny Ice Ocean. Near the central part, between Greenland and Iceland, there is a Danish channel with a width of 287 km in the sea. Nareshty, on the winter descent, between Iceland and Norway, grows into the Norwegian sea with a width of bl. 1220 km. At the descent of the Atlantic Ocean, two are cut off into the land of the aquatorium. Most of them are to be repaired by the Pivnich Sea, as they cross at the Baltic Sea to the Botnian and Finnish inlets. Півdenніше є system of internal continental seas - Seredzemny and Chornoye - beyond the bl. 4000 km The Gibraltarskiy prototypes, which have an ocean with the Middle-Earth Sea, є one after two other proto-straightened leaks. More low position of the loan Midland Sea in the Atlantic Ocean, some of the Middle Sea waters and more intensive vaping from the surface are characterized by greater salinity, and also more brilliant.
At the tropical belt, at the beginning of the Winter Atlantic, the Caribbean Sea and the Mexican inflow, where the Florida canal is located, across the ocean. uzberezhzha Wine of America porizan of small inflows (Pamliko, Barnegat, Chesapikska, Delaware and the Long Island channel); on the first visit there are inflows of Fund and St. Lawrence, Bell Isle Channel, Hudson Channel and Hudson Channel.
Islands. Naybilshi islands in the private part of the ocean; Central British Islands, Iceland, Newfoundland, Cuba, Haiti (Espanyola) and Puerto Rico. There are several groups of small islands - Azorski, Kanarski, Zelenyi Misu on the outskirts of the Atlantic Ocean. More groups in the western part of the ocean. Yak butt can be used in the Bahamsk Islands, Florida Kis and Mali Antilski. The archipelagos of the Great and Malikh of the Antilles are setting up an island arc, now a part of the Caribbean Sea. In the Pacific Ocean, some sharp arcs are typical for areas of deformation earth measles... Glybokovodnі zholobi grow out of the lumpy side of the arc.
Bottom relief. The west of the Atlantic Ocean will be provided with a shelf, the width of which will vary. Shelf rises through gorges - t.v. underwater canyoni. Їх podrodzhennya dosi wiklikє supercircuits. It is one theory that the canyoni boules are sprinkled with small rivulets, since the ocean is just lower than the current one. Іnsha theory po'vyazu їх formulation with the range of punctuated leaks. The drooped float, which turbidity leaks, is the main agent, which is the main agent of the deposition of sediments on the bottom of the ocean and that the stench itself breaks through underwater canyons.
The bottom of the private part of the Atlantic Ocean can be easily reconfigured for relief, statements on sub-water ridges, visochin, valleys and gorges. A large part of the oceanic bottom, from the depths of approximately 60 m and up to decilkokh kilometers, is covered with thin mulisty inserts of a dark blue or blakite green color. An altogether small area is occupied by skelny outlets and dilens of gravel-pebble and pebbled clays, as well as glide-water worm clays.
On the shelf in the private part of the Atlantic Ocean, telephone and telegraph cables have been laid to connect Pivnichnaya America with Pivnichno-Western Europe. Immediately to the area of ​​the Indian-Atlantic shelf, confined to the areas of industrial ribalism, it is possible to be referred to the number of the most productive in the world.
At the central part of the Atlantic Ocean pass, mayzhe repetitive lines of coastal lines, majestic underwater girskiy lantsyug dovzhinoy bl. 16 yew. Km, see the name of the Mid-Atlantic Ridge. The whole ridge stretches the ocean for two approximately equal parts. A large part of the peaks of the tsi sub-water ridge does not reach the surface of the ocean and is at a depth of at least 1.5 km. Some of the most high peaks rise above the ocean and set up islands - Azores in the Pivnichniy Atlantic and Tristan da Cunya - in Pivdenniy. On the half of the ridge of the Uzbek coast of Africa and on the way to the winter in the Indian Ocean.
The Uzdovzh axis of the Mid-Atlantic Ridge stretches across the rift zone.
Tech. The top flows in the private part of the Atlantic Ocean collapse behind the year's arrow. The main elements of the great system є are direct to pivnich heat leak Golfstrom, as well as Pivnichno-Atlantichny, Kanarska and Pivnichne pasatni (Equatorial) flows. Golfstrom slid from the Florida Channel and Cuba Island in the northwestern corner of the Uzbek coast of the United States at approximately 40 ° N latitude. go to the pivnichny skid, I will call it the pivnichno-Atlantic stretch. The current flow is distributed on two heads, one of which goes to the winter circuit of the coastlines of Norway and distant to the Icelandic Ocean. The founders of the Norwegian climate and all of the European and Eastern European countries are much warmer, less can be found in latitudes similar to the region, which will drag on from the New Scotland to the Summer. Another gilka turned for a week and a distance to the western end of the coast of Africa, the Kanarska current is still cold. The current flow collapses into the wintertime and goes down to the Pivnichnyy Passatnoy current, like direct to the west near the West Indies, de and get angry with the Golfstrom. At the beginning of the Pivnichny Passate Current there is an area of ​​stagnant waters, abundant in algae and in the name of the Sargasso Sea. The frontier of the Pivnichno-Atlantic Uzbek coast of Pivnichnaya America for the first time passes the cold Labradorska in a stretch, viplivay from the Buffin outlets and the Labrador Sea and the cold-water coast of the New England.
PIVDENNA PART OF THE ATLANTIC OCEAN
Between that coastal line. Deyakі fakhіvtsі carry to the Atlantic Ocean on the whole water expanse up to the Antarctic ice cover; They take a clear line for the new Atlantic cordon, which is how they got Ms. Horn in Pivdenniy America with the Mes of Good Nadia in Africa. The coastal line in the first part of the Atlantic Ocean is significantly less porous, lower at the winter, here there are also internal seas, beyond which the ocean could penetrate into the continent of Africa and Of America... Let's share a great flow on the African Uzbek є Guineyska. There are also innumerable inflows on the Uzbek coast of America. The very first edge of the tsiy continent - Vognyana Zemlya - grows along the coastline, lined with numerous other islands.
Islands. There are no great islands in the early part of the Atlantic Ocean, however, there are some isolated islands, such as Fernando de Noronia, Voznesinnya, Sao Paulo, St. , Pivdenny Sandvichev, Pivdenny Orkney, Falkland Islands.
Bottom relief. Across the Mid-Atlantic Ridge, in the Pivdenniy Atlantic, there are two main sub-water girders. The whale ridge stretches across the ancient-western edge of Angola to about. Tristan da Cunya, de vin z'єnutsya s Mid-Atlantic. The Rio de Janeiro ridge stretches from the islands of Tristan da Cunha to the place of Rio de Janeiro and is a group of submarines.
Tech. The main systems of leaks in the early part of the Atlantic Ocean collapse against the old days. Pivdenna Pasatna is directed towards the west. Have a whistupu shidny uzberezhzh Brazil won’t be able to go on two flights: it’s on the winds of the western coast of America to the Caribbean, and in winter, it is warmer Brazilian stretching, to fall on the winds of the Antarctic coast to pіvnіchny skіd. A part of this cold current is coming to the end and not all of your lead to the pivnich of the African Uzbeks, making the cold Benguela stretch; We will stay at the end of the day to come to the Pivdenny Passatna leak. Warmly Guinea's stretch collapses on the first day of the coasts of Pivnichno-Western Africa in Guineyska Zatoka.
LITERATURE
Atlas of oceans. T. 2. Atlantic and Indian oceans... L., 1977
Geography of the Holy Ocean: Atlantic Ocean... L., 1984

Encyclopedia Krugosvet. 2008 .

Atlantic Ocean map

The area of ​​the ocean is 91.6 million square kilometers;
The maximum depth is Puerto Rico, 8742 m;
Number of seas - 16;
sami great seas- Sargasov Sea, Karibske Sea, Seredzemne Sea;
The most inflow - Mexican inflow;
The most popular islands - Great Britain, Iceland, Ireland;
Strongest trends:
- warm - Golfstrom, Brazilian, Pivnichne Pasatne, Pivdenna Pasatna;
- cold - Bengal, Labradorskoe, Kanarska, Zakhidnykh Vіtriv.
The Atlantic Ocean covers the entire area from subarctic latitudes to Antarctica. At the first entry of the wine between the Pacific Ocean, at the first exit from the Indian and at the winter - with the Pivnichny Ldovitim. In the winter season, the coastline of the continent, which is washed by the waters of the Ice Ocean, is heavily porous. There is a lot internal seas, Especially at the gathering.
The Atlantic Ocean is embraced by a remarkably young ocean. The mid-Atlantic ridge, which stretches across the mayzhe strictly along the meridian, extends the ocean bed into two approximately the same parts. On a snowy day near the top of the ridge, float above the water at the viglyad volcanic islands, Most of Iceland.
The shelf part of the Atlantic Ocean is not large - 7%. Naybilsha shelf width, 200 - 400 km, in the area of ​​the Pivnichniy and the Baltic Sea.


The Atlantic Ocean is located in more climatic belts, and a larger part - in tropical and peaceful latitudes. Klimatichnі think here vіtchayut passati and vіdnі vіtri. Most of them can be reached in the lower latitudes of the Atlantic Ocean. Near the region of the island of Iceland there is the center of the origin of cyclones, which significantly infuse the whole Pivnichnoe period into the nature.
The average temperature of surface waters in the Atlantic Ocean is significantly lower, lower in the Pacific. The price is explained by the inflow of cold waters and ice, as it comes from the Pivnichny Ice Ocean and Antarctica. At high latitudes, there are abundant icebergs and drifting slopes. At winter, icebergs are brought from Greenland, and at winter - from Antarctica. In our days behind the collapse of icebergs to run from space piece companions of the earth.
The current in the Atlantic Ocean may be meridian directly and is characterized by a strong movement of water masses from some latitudes in the region.
The organic light of the Atlantic Ocean behind a large warehouse, below the Pacific Ocean. Explain the geological youth and the cooler ones clever minds... Ale, unaffected by the price, stocks of ribs and other sea creatures and roselin in the ocean reach the value. The organic light is large in the middle latitudes. More friendly minds for the living of the bagatech species of ribs were laid in the private and old parts of the ocean, less streams of warm and cold currents. here promise value Mayut: triska, oseledets, sea bass, mackerel, capelin.
free to see natural complexes Outside the sea and the inflow of the Atlantic Ocean, especially the inner seas: Seredzemny, Chorny, Pivnichniy and Baltiyskiy. Near the winter subtropical belt of Roztashovana, unique for its nature, the Sargasovo Sea. Giant sargasovs of water growth, on the rich sea, they broke up.
There are important sea routes across the Atlantic Ocean, which will bring Novy Svit to the lands of Europe and Africa. On the Uzbek and Atlantic islands there are all kinds of regions and for tourism.
The Atlantic Ocean has begun to be conquered since ancient times. Recovering from the 15th century, the Atlantic Ocean has become the main waterway of the people and does not consume its significance and the present. The first period reached the ocean until the middle of the 18th century. Vin is characterized by the growth of the ocean waters and the establishment between the ocean. The complex nature of the Atlantic has gone from end of XIX stolittya.
The nature of the ocean in our hour is more than 40 scientific ships from the Russian lands. Oceanologists are reliably listening to the ocean and atmosphere, keeping up with the Gulfstream and other leaks, beyond the icebergs. The Atlantic Ocean is no longer in the snake of its own biological resources. Preservation of the current nature is international on the right.
Vibrate in one of the unique places of the Atlantic Ocean and at the same time go to Google maps to get more expensive.
About the rest, they have appeared on the site of an independent mission of the planet, you can learn, change

Atlantic Ocean - warehouse of the Svitovoy ocean with forced flow povitryan mas... For a borrowed territory, you will be in another place. Aquatoria roztashovana in small climatic belts. Sensitive, as the mass of water streams represent warm and cold. And about the reasons for this particularity. Otzhe, zhenemno knowledge of the majestic water element.

flows of the Atlantic

The Atlantic Ocean (you can clearly see it on the map) is practically all over the continent. Naturally, the aquatoria was given the form of klimatic specialties on the cich dilyankas of the land. And what about the axle? I play a great role in the formation of the climate not only but the current. Warm in oceans overcame cold ones. Stay for a few days to eat all 5.

The currents of the Atlantic Ocean have a special feature: the stench collapses behind the year-old arrow, setting up the straining circulation to the flow of water and changing warm and cold waters. There are two such cycles in the aquatorium: in Pivnichny and Pivdenniy pivkuli.

Yake of the Atlantic Yak they said before, the greats see all 5:

  1. Labrador.
  2. Kanarska.
  3. Benguela.
  4. Falklands.
  5. Techіya Zakhіdnykh vіtrіv.


Techіya Zakhіdnykh vіtrіv

At the Pivdennii pivkuli of the Atlantic Ocean, it is especially swept by the stretch of the Western Winds. Another name is Antarctic circumpolar. Vono get involved in the most straining and great flow of the entire Svitovoy ocean, so pass through all the meridians of the Earth. There are many waters not only in the Atlantic Ocean, but rather in the Indian and Pacific. The length of this current is 30 thousand. Sq. km, width - up to 1 yew. km. The temperature of the surface waters in this period rises from + 2 ° С in the interior regions to + 12 ° С - in the winter ones.

The tensely cold current of the Atlantic Ocean has been victorious as a result of the Winter Winds that are overwhelming here. The main stench is on the territory of the peace belt in the area from 35 ° S. NS. up to 65 ° S NS. Three dims right from the entrance to the skid, the stronger the charge, the weaker - the more. They blow over the meat of the Pivnichny and Pivdenny Pivkuly. But in the end, there is a push to develop through those that are less dry here on the crossroads at the winds. The region, in yakiy dіє stretching Wandering winds, often sees like the outskirts of the Pivdenny Ocean. The fluidity of the given water flow in the surface sphere reaches 9 m / s, in glib balls it changes up to 4 m / s. It is given with a stretch to live by two cold compasses: Benguela and Falkland.

Malvinsky stretch

Falklands (Malvinsky) - cold flow of the Atlantic Ocean. Introducing the Antarctic Circumpolar Current. Go to the area extreme point O. On its way out, burning the shores of the American-American continent and Patagonia, opposite the Falkland Islands, end up in the area of ​​La Platskoy inlet. Distant flow into the warm waters of the Brazilian current. A bit of angry two streams of water, which is clearly visible from the sky, as well as the Atlantic Ocean on the map. On the right, in the one where the cold flows are of the green color, and the warm ones are blakytny.

Falklands potik is not very high speed - up to 1 m / s. The water temperature in the middle is from + 4 ° С to + 15 ° С. It is tied with a tse z tim, scho over the course of time he will repair his icebergs, which step by step.

Bengalska stretching

Bengelskoe is another bit of the cold stream given to the ocean, separating from the crossing of the Western Winds. I keep a small ear of goodness at the place of Good Hope and, straight for the winter, end up in the Namib area (in Afritsi). Dal, beastly on the west, pour into Pivdenno-Pasatna with a stretch, and by ourselves end the circulation of circulating masses in Pivdenniy pivkuli. The water temperature of the Bengal current does not depend on the temperature of the water in the ocean, but does not decrease by 3-4 °. Denmark is still close to go to the western outskirts of the African continent. Directly to the current, ask the old ones on the very cob and on the first step, pass them on.

Labrador broach

You can see the cold flow of the Atlantic Ocean - Labrador. tsey potik sea ​​waters I will repair my way through the Baffin Sea, straight to Fr. Newfoundland. Pass through Canada and Greenland. Rukhayuchis from pivnichi for the day, in the end of the way to build up with warm Golfstrom. Vitisnyayuchi yogo vodi, directing to the skid. Seemingly, the very heat of the leak will give me a lot of problems friendly climate across Europe. You can say that the Labrador spriya is the same.

Closeness to the Pivnichniy Ice Ocean and ice-cold waters, but the water salinity is low, up to 32%. Through the Labrador Current, on the first day of the Atlantic, there are numerous icebergs, which will quickly go to shipfaring in the cich regions. All the synonymous Titanic hitting the iceberg, like a blast into the ocean by itself.

Kanarska leak

Kanarska - cold flow of the Atlantic Ocean. maє change type... On the ear of his own ruch (at pivnichno remote shores Africa and the Canary Islands) the current is not cold water. Dal, collapsing on the west, change the temperature of the water from the cold to the heat and in the end bag to pour into Pivnichno-Pasatna.

The very name of the Atlantic Ocean became something of the Atlantean Mountains in the winter of Africa, or something of the legendary continent of Atlantis, which has been in the old days and was bent as a result of the terrible flood. With the drive of the Atlantis mystery, the superheets and the jokes go to the tsikh pir.
The Atlantic is filled with a lot of myths, retelling and riddles of history. For example, one of those who found geographic descriptions- about the floating of the Greek Pytheas from Massilia (Ninishniy Marseilles) in the IV century. BC That is, on the pivnich of the Atlantic, Tula is de nibito, the land of the legendary cold and fog. Until now, more precisely, the time of the growth of Tuli, like Atlantis, is not significant.
The Egyptians, the Egyptians, the Greeks, the old fleet of Oleksandr the Great, the Arabian sailors, the Temples of the Atlantic, and so on. On the other hand, the persistence of Scandinavian seafarers in America is absolutely complete. Archaeological excavations showed that vіkіngi in the X century. They didn’t go only to Greenland, but only a few of the capital lived for some time, and they also made it to the Uzbek coast of the mainland. On the eastern edge of Newfoundland boules, there are many small villages.
Ale navazhliv_shim ocean for all people The Atlantic Ocean became in the era of the Great geographic views, In the XV-XVII centuries, If the European civilization across the Atlantic has seen for itself, our great saint is so great. The Atlantic Ocean was first transformed into the mainstream of European ships, and practical information provided by expedited ships, as well as new technologies, as well as being easy to maintain.
However, if the people were viral, they had already reached the fullness in the edgy elements, the Atlantic Ocean had given a lesson.
On April 14, 1912, the largest passenger liner in the world, Titanik, hitting an iceberg, sank in its first swim. 1502 people disappeared, for the whole world the tragedy was a shock. The Atlantic thirsted for a serious challenge to itself, and the lesson was forgotten for a while. The end of "Titanic" has become a legend;
Comply with those who, if not, people, we will be organized in the Atlantic, like in our kitchen, not varsity. To navigate in the XXI century, Volodyuchi kudi with more sophisticated technologies, not even in an hour "Titanic", until the captains of the whole family will be afraid to be afraid of a bag of fame in the ocean, they have earned some ill-fame. Chogo one Bermuda tricycle, De still prodovzhuyut people and sea vessels.

Geography of the Atlantic Ocean

Through the Atlantic Ocean to pass as much as all the climatic belts of the Earth, and to become close to 20,000 km. In the middle of the Bagatio Sea, which lies overlooking the Atlantic Ocean, the Sargas Sea is especially visible. To the fact that there is one sea in the world, not just continental shores, but the waters of the Sargassah (sea weeds of a brown color).
Atlantic Ocean behind the form of nagaduє latin letter S... Win a trip from Greenland at winter to Antarctica at winter. From a large part of the land, water flows into a magnificent water basin.

Another for the size in the light of the Pacific Ocean, the Atlantic Ocean has its own characteristic features... The yogo coastline is characterized by great ruggedness, in the new one there is an altogether small number of islands, rivulets that flow into the Atlantic Ocean, or at the end of the sea, may the most area basins.
The Atlantic Ocean also grows with the folding of the bottom relief. The Mid-Atlantic Ridge extends over the ocean bed to a height of 2 km. Near the top the ridge constitutes the islands, the largest of them is Iceland. In a whole area, the volcanic activity and parts of the earthquake do not fall.
Another feature of the Atlantic is icebergs - the majestic mountains of the mountains, floating on the surface of the ocean. The stench is periodically seen from the crooked surface of Greenland and Antarctica. Ci beautiful ocean blue dos - a great threat to sea vessels.
For Europeans, the understanding of the Atlantic is mintly tied with a plate, to show the most serious inflow into the weather of the continent. The gulfstrom leaders themselves, who carry their waters out of the Bahamas (de Florida stretch out from the Antilski Plins, set up the Gulfstrom), the land of Europe, lay down to the Atlantic Ocean, we can enjoy the cold weather at the same latitude, ale in the distance towards the Gulfstream. To deliver the tales that the heat demand of the Golfstrom for the demand of the millions of atomic power stations. In the ocean, the Gulfstream collapses from the speed of 6-10 km / year, the area of ​​the stream is 700-800 m.
The Atlantic Ocean is the most intensely vicious ocean of humans, and the very much the most difficult and anthropogenic (due to the participation of people) injected. To deliver the tales that the velov ribi in Atlantitsa regularly becomes the subject of controversy between small lands- Duzhe neatly home about quotas. Overfishing should be regularly carried out to the fast-growing populations and the need for new ones. the manifestation of powerlessness great placesі rozvinenikh lands on the Uzbek coast of the Atlantic Ocean, it will lead to the skidding in the waters of the great number of foreign rivers.
Vvazhaє, about 200 million rubles to that in the Atlantic Ocean has not yet been built. But the majestic continent of Pangea, which is 160-180 million rocky in that, I know approximately (in paleogeography exact dates mayzhe does not start), breaks up. Other rozcoli and rozcoli lithospheric plates The earth was brought up before, close to 5-10 million rocky in that Atlantic Ocean, adding a lot of bitchy viglyad. Bagato in the best schools in the respect of the Atlantic Ocean for the youngest of the oceans on Earth.



Global information of ATLANTIC

International Hydrographic Organization has set the boundaries of the Atlantic Ocean: at winter - between the Labrador Sea (Atlantic) from the Davis Channel (), the Atlantic Ocean from the (Icelandic Ocean) and the Norwegian Sea (Icelandic Ocean) and the Icelandic Sea (Atlantic) from the Norwegian Sea (Iceland); on private - from by the ocean(Navkolishnim Antarctica); at the first entry - from the Pacific Ocean along the Magellanic Channel (to the pacific); on the paved descent - from the Indian Ocean.

Greater sea: more Weddell.

Most of the rivers that flow into the Atlantic Ocean: Amazon, Nil, Congo, Niger, Misisipi, La Plata.

Find out more: Golfstrom, Pivnichno-Atlantic, Kanarska, Pivnichne passatna, Labradorskoe, Pivdenna passatna, Brazilian, Antarctic circumpolar, Bengal, Guianske, Falklands Ekvatorialne prototypes.

digits

Length (from nights to weekdays): close to 20,000 km.
Nimensha width (from start to finish): 2800 km

Nybilsha width: 13 500 km.

Area: 91.4 million km 2 (including all the middle continental seas).

itself great glybin: 8742 m - Puerto Rico jolob.

Average Glybin: 3600 m.

Obsyag: 329.7 million km 3.

Average salinity of waters: 35%.

Economics

The main significance is the transport, private part of the Atlantic - the most important part of the Atlantic Morskiy Shlyakh... Pidvodny vidobutok naphtha and gas, rich in coastal genera of cinnamon copalins.
Victory of biological resources - more than half of the light video of trisky, tuna, settling, etc. D.

Climat and weather

All klimatic belts are presented.

There is a large part of the Atlantic Ocean - at 40º c. NS. at 42º S NS. - located in the equatorial, subquatorial, tropical and subtropical zones, de tsiliy rik plus temperature. At tropical latitudes, the average temperature is + 20 ° C with clear litter. In subquatorial areas - from + 10 ° C to + 20 ° C overflow, fall over the same time. Often the phenomenon is tropical hurricanes. In subtropics, the temperature of the coldest month in rotsi drops to + 10 ° C, for winter it is typical for the fall. Near the latitudes, at a half-hour from 40º s. NS. and for half a day from 42º S. sh., fall off with a stretch of rock, vipadayut most frequently (in the boundaries of 1000 mm), reaching the maximum in the autumn-winter period. Characterized by strong storms, temperature - from +10 ... 15 ° С during up to -10 charge. Naybilsh Suvoriy Klimat - in the northernmost part of the Atlantic, in the sub-Antarctic and Antarctic latitudes. Вім, Atlantic Ocean in subarctic i arctic latitudes you can vvazhati "more warm" deprived of intelligence.

memorials

■ Beautiful beaches on the shores of more continents such as the Atlantic Ocean;
■ Island Madeira;
■ Azores Islands;
■ Islands of Green Misu;
■ Canary and Antilles Islands.
■ Bermuda Islands.

tsikavi facts

■ American salesman Charles Lindberg first made a non-stop flight across the Atlantic Ocean in 1927
■ The most distant islands in the world are the islands of Bouvet in the Pivdenniy Atlantic, located 1600 km from the city of Good Nadiya. And the greatest island in the world is Greenland in the private part of the Atlantic Ocean.
■ Engage in bringing oil reserves to the Mexican market to reach 4 billion tons.
■ At the center of the Mid-Atlantic Ridge, which passes in the central part of the bottom of the Atlantic Ocean, there is a volcanic process. Wikidi melted kam'yan breed - magmi - emboss on the face of earthly measles. As a result, America and Europe will grow one inch by one per 2 cm.

Geographic location.The Atlantic Ocean stretched from winter to 16 yew. Km from subarctic to antarctic latitudes... The ocean is wide in the winter and winter parts, it sounds in the equatorial latitudes up to 2900 km. At the weekend, get to the Pivnichny Ice Ocean, and at the weekend, it is wide to go to the Quiet and Indian oceans... Bordered by the shores of Pivnichnaya and Pivdennoy America - at sunset, Europe and Africa - at the descent and Antarctica - at winter.

Atlantic Ocean - the other beyond the size of the middle of the oceans of the planet... The coastal line to the ocean in the first season is strongly divided by the number of birds and outflows. Close to the mainland, many islands, internal and outskirts of the sea... There are 13 seas to enter the Atlantic warehouse, which occupy 11% of the area.

Bottom relief. Through the entire ocean (approximately on the edge of the mainland from the Uzbek continent) Mid-Atlantic Ridge... The typical height of the ridge is close to 2 km. Transverse breaks and breaks apart on the edge of the segment. In the axial part of the Roztashov ridge, a giant rift valley is 6 to 30 km wide and up to 2 km wide. Before the Rift and the breaks of the Mid-Atlantic Ridge, there are both sub-water volcanoes, as well as the volcanoes of Iceland and the Azores. Along the offensive sides of the ridge, lie the slopes with an altogether flat bottom, divided by uplifts. The area of ​​the shelf in the Atlantic Ocean is larger, lower in the Pacific.

Mineral resources. Stocks of oil and gas have emerged on the shelf of the Pivnichnaya Sea, in the Mexican, Guinea and Biskaysk inlets. Pokladi phosphoritiv vіdkritі in the regionі pіdyomu clay waters bilya uzberezhzha Pivnichnoi in Africa in tropical latitudes. Roseypic genera of tin near the shores of Great Britain and Florida, as well as diamonds - along the shores of Pivdenno-Western Africa, appeared on the shelf in the sediments of ancient and recent rivers. Zalizomanganese concretions are known in the valleys of the bottom of the coast of Florida and Newfoundland.

Climat.The Atlantic Ocean of rippling along all the climatic belts of the Earth... The main part of the aquatic ocean is located at 40 ° Mon. і 42 ° N - to be located in subtropical, tropical, subquatorial and equatorial climatic belts. There is a round ric of high positive temperatures. Naybilsh suvoriy klimat may be subantarctic and antarctic latitudes, in the lesser world - polar and northern latitudes.

Tech.In the Atlantic, like in the Pacific Ocean, there are two rings surface leaks ... In the winter season, the Pivnichne Passatne stretch, the Golfstrom, the Atlantic-Atlantic and the Canarian flows set the water down behind the year-old river. At the Pivdennii Pivkuly Pivdenna Pasatna, Brazil, with a stretch of the Western Winds and the Benguela, there is the collapse of the waters of the Antiquity Strelka. Through the significant extent of the Atlantic Ocean, from winter to winter, in the greater world of development of the meridional streams of water, lower latitude.

The power of the waters. The zonality of water masses in the oceans has been accelerated by the inflow of land and sea ​​flows... Tse manifests itself in front of the rise in temperatures of surface waters. In some areas of the ocean, there is an oceanic coastline, and the coastline rises sharply towards the latitudinal direction.

Half of the ocean is warmer than half of the ocean, the temperature difference reaches 6 ° C. Average temperature surface waters (16.5 ° C) trocha lower, lower in the Pacific Ocean. Cooling inflow is used to pump water and ice in the Arctic and Antarctic. Salinity of surface waters in the Atlantic Ocean... One of the reasons for the increase in the salinity of the field is that the part of the brewery does not turn back into the ocean again, but is transferred to the continents (through the common ocean).

A number of great rivers flow into the Atlantic Ocean and the Third Sea: the Amazon, Congo, Mississip, Nil, Danube, La Plata and other. The stench to wine into the ocean of the majestic mass of fresh waters, filled with material and foreign words. In certain tributaries and seas of subpolar and inland latitudes, ice is set off from the remote shores of the ocean. Numerous icebergs and floating sea ice will be used by ships in the private part of the Atlantic Ocean.

organic light... Atlantic Ocean with many species in the warehouses of flora and fauna, below the Pacific. For one reason, the geological youth and the colder temperatures in the quarterly period before the hour of icy are noteworthy pіvnіchnoі pіvkulі. However, the ocean is rich in organisms - the most productive in one area... The perch is tied behind everything with a wide development of shelves and milky water cans, on some bags of rich bottom and bottom ribs (triska, flounder, perch, etc.). biological resources The Atlantic Ocean in the most important regions of the world. A piece of the ocean in the city of Ribals the rest of the rock significantly decreased.

Natural complexes.All zonal complexes are visible in the Atlantic Ocean - natural belts, Крім pіvnіchnoi polar... drive pіvnіchny subpolar belt Bagati lives. Vona is especially rooted on the shelves off the Uzbeks of Iceland, Greenland and Pivostrov Labrador. pomirny belt characterized by an intensive interaction of cold and warm waters, the most productive areas of the Atlantic. Great expanse of warm waters dvoh subtropical, two tropical and equatorial belt less productive, less water and a pivnichnogo pomirny belt.

In the wine subtropical belt you see special natural aquatic complex of the Sargas Sea... It is characterized by a change in the salinity of the waters (up to 37.5 ppm) and a low bioproductivity. At the glimpse of water, pure blue color to grow water growth - sargassi, They gave the name aquatoria.

V to the pomirny belt pіvdennoї pіvkulі, Yak and in pivnichnoe, natural complex of rich living in areas where water is depleted and with a high temperature and brilliant waters. Subantarctic i Antarctic belts Characteristic is the manifestation of seasonal and post-ice ice phenomena, which can be found in fauna warehouses (krill, whale-like, notothenic ribs).

Gospodarske vikoristannya. In the Atlantic Ocean, all kinds of state-owned people on the sea water are represented. Among them, the most significant may be sea transport, sometimes - a sub-water vid of oil and gas, and only a little more - forks and licenses of biological resources.

On the shores of the Atlantic there are 70 coastal regions with populations of 1.3 billion Cholovik. There are many transoceanic routes across the ocean with great vantage and passenger transportation. On Uzbek oceans and on the th sea, the most important values ​​for the return of the light.

already developed mineral resources to the ocean - meaning (put the point on). However, in the Danish hour, naftogaz production on the shelf of the Pivnichniy and Caribbean Seas, in the Biskayskiy Zatotsi is being intensively developed. Bagato region, before, there were not a few significant reserves of cich species of mineral water, they see at once an economical trip for a rakhunok of this vidbutku (England, Norway, Netherlands, Mexico, etc.).

biological resources the ocean has long been intensively growing. However, a number of valuable industrial species of ribs were caught at the close, and in the rest of the Atlantic, the Pacific Ocean was transferred from a species of ribs and seafood.

Intensive government activity of people on the Atlantic Ocean and the first sea natural center- yak in the oceans (the hardening of the waters, the food, the change in the reserves of industrial species of ribs), as well as on the Uzbeks. Wake up on the shores of the ocean. I see the growth of the natural environment of the Atlantic Ocean, and the change of the existing environment scientific recommendations and internationally please rational vikorystannya resources in the ocean.

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