Pivdenno Atlantic current. Earth sciences

The Atlantic Ocean is the very creation and development of people from all oceans. For one hypothesis, I will name my wine after the name of the titan Atlanta (according to the Greek mythology, like a trim on my shoulders is the heavenly crypt). V early hour yogo was called in a simple way: "The Sea beyond the Heracles Stops", "Atlantik", "The Western Ocean", "The Sea of ​​Darkness" etc. The name "Atlantic Ocean" first appeared in 1507 on the Wald-Zemuller map, Quietly, the name was firmly established in geography.

Theme: Ocean Lands

Lesson: Atlantic Ocean

1. Christmas Day

About the peculiarities of nature and the ocean;

About victorious people and environmental problems.

2. Geographic location of the ocean

The Atlantic Ocean is another planet beyond the size of the ocean. Vin borrows an area of ​​92 million km. The Atlantic Ocean is located on the shores of five continents.

By the cordons of the Atlantic Ocean є Pivnichna America and Eurasia in the pivne part, and Pivdenna America, Africa and Antarctica - in Pivdenniy.

The Atlantic is seen from the Old Kremlin, from the New.

The Atlantic Ocean is overflowing with an ekvator and a zero meridian (div. Fig. 1). Yogo length - 13 thousand km. The ocean is wide (the greatest width is 6700 km) in the winter and early parts, it sounds in the equatorial latitudes up to 2900 km. At winter it will be in the Pivnichny Lydovitim ocean, and at winter it will be widely located in the Pacific and Indian oceans.

Small. 1. Physical map of the Atlantic Ocean

The Atlantic Ocean is the other one beyond the size of the middle of the oceans of the planet. The coastal line to the ocean in the winter season is strongly divided by the number of rivers and inflows. 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 this area (Div. Fig. 2).

Remember the names of the greatest of them.

Caribbean Sea - 1

Mexicanska zatoka -2

Sargasov Sea - 3

Baltic Sea - 4

Biskayska inflow - 5

Middle earth sea - 6

Chorne More - 7

Gvineyska inflow - 8

Mori Weddell - 9

Small. 2. Seas of the Atlantic Ocean

3. Relief of the bottom of the Atlantic Ocean

The Atlantic Ocean is younger than the Pacific Ocean, having established itself in the Mesozoic era, with the fall of the Gondwani mainland. Yogo bottom - the price of dilyanka decilkoh lithospheric plates... At the center of the Atlantic Ocean, from winter to day, the majestic Mid-Atlantic ridge is stretched, breaking through without transverse breaks.

The usual height of the ridge is about 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.

Itself here, in the central parts of the Mid-Atlantic Ridge, from the depths of the mantia, it appears on the surface of the young crust and step by step diverge to the turn and the west, the widening ocean. At the top of the Mid-Atlantic Ridge there are islands of Iceland - one of the most beautiful places on Earth (Div. Fig. 3).

Small. 3. Iceland

At the school western parts the ocean stretches vast ocean depressions, and at remote shoresє two small glide-water beetles- most of the ocean (div. Fig. 4).

Small. 4. Relief of the bottom of the Atlantic Ocean

4. Climate of the Atlantic Ocean

The Atlantic Ocean of the Mayzhe climatic belts, Krim one (see the name of the card). Virno, tse Arctic climatic belt.

The zonality of water masses in the oceans has been accelerated by the inflow of land and sea currents. Tse manifests itself in front of the temperature rise 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 the first, the temperature difference is up to 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 vaping from the aquatic environment does not turn 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, entangled 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.

At subtropical and tropical latitudes, it is dim past, but more forcefully and lighter in the Atlantic during the Wandering transfer. The stench is especially strong in outside latitudes Pivdennoy pivkuli.

The most severe storms and hurricanes regularly occur in the western part of the Atlantic, so they can unleash their ferocity on the Uzbek coast. Їх boo 10-20 per season. The meteorological service is being established.

5. The current Atlantic Ocean

Panіvnі vіtrіvnі form head leaks in the oceans. Ale Atlantic Ocean is very strong from winter to evening, that and the head of the ocean is in a meridional straight line (Div. Fig. 5).

In the Atlantic Ocean, as in the Pacific Ocean, there are two rings of surface leaks.

Quote the atlas behind the cards and you will easily know these flows of the Atlantic Ocean.

At the winter season, the Pivnichne Passatne stretch, the Golfstrum, the Atlantic-Atlantic and the Canarian current set up the rush of waters behind the year's line.

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 a new world in the greater world of development of the meridional streams of water, lower latitude.

Small. 5. Map of flows of the Atlantic Ocean

6. The organic light of the Atlantic

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, in the vast ocean of organisms, it is 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.).

7. Exploration of the Atlantic Ocean

The Atlantic Ocean has been conquered by people for hours and hours. At the same time, I have a great role in the life of people: through the new, a thick hedge of the most important transport nobles has spread, so that Europe and America and the regions of the Persian inflow can be brought together.

On the shelf of the Pivnichnaya Sea and the Mexican tributaries, naphtha is seen, in the paved part of the ocean, reserves of gallium-manganese concretes have been discovered.

In the Atlantic Ocean, there are the main regions and ribalism and the most popular resorts in the world.

The biological resources of the ocean have long and intensively been growing. However, a number of valuable industrial species of ribs were caught at the the rest of the rock The Atlantic is being sold to the Pacific Ocean for a package of ribbons 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 twilight, the change in the stocks of industrial species of ribs), as well as on the Uzbeks.

I see the growth of the natural environment of the Atlantic Ocean, and the change in the existing environment of the Atlantic Ocean scientific recommendations and pollagayut international please on rational victoriannya resources in the ocean.

Home zavdannya

Read § 18. Practical robot.

Follow the patterns of current flow in the Atlantic Ocean and flow into the climate of the coastal territories.

List of Literature

The mainI am

1. Geography. Earth and people. Grade 7: Pidruchnik for general education. uch. / A.P. Kuznetsov, L. Є. Savel'va, V. P. Dronov, "Sphere" series. - M .: Education, 2011 rock.

2. Geography. Earth and people. Class 7: atlas, "Sphere" series.

Dodatkova

1. N. A. Maksimov. Behind the sides of the handler of geography. - M .: Education.

Literature for training before DPA and ZNO

Seafarers learned about by sea currents a long time ago. Columbus, who poured to America in the stream of the Pivnichny Equatorial Current, when he turned around, said that he would "collapse in the western direction right away from the sky" in the ocean. In 1513, the Spanish Ponce de Leon, who was a Vyishov in the sea on the trick of the mythical "Happy Islands", having drunk in the flow of the Florida current, like it was so strong, that sailing ships did not appear in the snake fighting against him. In the other half of the XVIII century. American merchant sailors already knew about the discovery of GolfStrum. On the way from America to England, the stinks went to the yogi structure, and on the ringing way they laid the course of the road towards it. The breeders of this stink came from Falmouth (England) to America for two large shipment packets, which were controlled by the English captains, who did not know from the interruption. Tse bulo will be announced soon. Roz'yasniti the riddle was handed over to V. Franklin, who took over the post of the post director of the United States of America. Having fed the sailors, they sklav the card to GolfStrum, on yaky tug Atlantic current It is depicted at a viglyad rychka, flowing in the middle of the ocean.

Directly, the speed of ocean currents began with the drift of the vessels, which were related to the current in the course of the course. According to the patterns of the suffered ships, which have been held out to the navigators more than once, it is possible to judge the direction of the leaks.

From 1887 to 1909, 157 great ships were named in the oceans, which became aware of the ship's accident. In 1891, the sailing ship "Fanny Wal-Stogin" was flooded by a storm after the storm was filled with abandonment by the command not far from Mis Gatteras (Pivnichna America). Stretching three coming rock_v yogo backed in the small parts of the Atlantic Ocean 46 times. Tsikaviy vipadok with the ship "Fred Taylor", yak in 1892, the storm broke before the hour. One part, covered with water, flooded for a drink, and it drifted down to Boston; On the afternoon of the day it drifted into the Delaware backwater for the afternoon. Once, in the 30s of our capital, from the Japanese shores to the inflow of Juan de Fuca on the western birch Wine of America the Japanese ship "Reyosi Maru" nailed with the corpses of the commander, the yaka was starved to death.

Being careful to drift with shmats of pumice, wikipedia in the presence of volcanoes, allowed the development of the middle class and just some ocean currents. For the drift of the pumice, the drift of the Krakatau volcano in 1883 was established, that the speed of the backward current in the Indian Ocean reached the middle 9.3 miles per day. In 1952, the head of the Barsen volcano was raised on the island. San Benedetto Beachfront Central America... Pumice was known to Vikinut pumice on the Hawaiian Islands after 264 days, on the Wake Islands - after 562 days. The average rate of the Pivne Equatorial Current in the Pacific Ocean was numbered 9.8 miles per day. The rate of increase in the turn of radioactive contamination in the ocean from atomic vibuchs at the Bikin atoll is 9.3 miles per dob. Behind the caution of the Japanese chemist-oceanographer Miyake, the core of the contaminated water approached the shores of Asia almost across the river, and then it began to grow for the first time with the waters of the Kurosio current.

Chi not satisfied with vypadkovyh objects, scho to pour on hvilyah, in the sea wikidati began to cork up the dances with a post card inserted into them. Knowing this dance by lowering the card into the post screen, having told the m_sce, de vin know the dance.

In 1868, when seamen were led in dances, they called it "dance shit". The tsei method of "mail order" has been practiced for a long time. In 1560, a young man of the know, a dance was sealed on the birch of England. Being unwritten, he delivered the sorceress to the judge. At the dancers, there is a secret information about those who wanted to establish the Russian Arctic island Nova Earth... The English queen lizaveta fell asleep to the position of the "dance uncorker". For the rosette known on the birch and in the sea of ​​dancing without the participation of a sovereign official, the bully was sentenced to death by hanging. The posad of the "dance uncorker" was made in England for a long time and the ball was cut off only under the king George III(1760-1820 pp.).

In the Atlantic Ocean, Pivnichne Equatorial, stretching out water in the Caribbean Sea and the Mexican inflow, calls out through the high Florida channel, and yes an ear of goodness to all the Gulfstream. In the Pacific Ocean, the current of Kurosio, the people of the Pivnich Equatorial Plin, has to repent in exactly the same order. Lead Pivdennye Equatorial flows turn on pivday and live the Power of the Last Weeks, without bounds enveloping Antarctica.

Golfstrom, carrying warm water to the beach, expanding, reaching the shores of Europe and flowing into a kintsev bag in the Barents Sea and Pivnichny Ice ocean The water will turn for the afternoon at the sight of the cold Greenland current. Part of your water is taken by the Golfstrom on the way. Tsya water, looking to the right, established a circular current in the Pivnichniy Atlantic. Mayzhe also has a picture of sposterіgaєmo in the Pacific Oceanі. But here Kurosio is not in the snake to penetrate into the Icelandic ocean through those that are close to Asia and America. To that, by stretching to the right on the skid, close the circle of water masses on the pivnich from the ekvoryuly. Nazustrich Kurosio, also adopting the "rules of the ruch", set up the wraps of the Earth for the winter season, that is. At the Holy Week from the Antarctic Circular Current off the back coast of the mainland, there are cold currents - Peruvian near the coast Of America, Benguela Bilya of African shores and Western Australia. The flow carries cold water into the biker of adequateness and the life of the equatorial flow, ruined by the wind.

If you speak warmly or the flow is cold, then do not expect the need for intelligence literally. For example, the water temperature of the Benguela current is about 20 ° C, the water is “cold” in a stretch, while the North Cape stretch (one of the Gulfstrom's springs), which carries water at a temperature of “4 to 6”. Call such leaks, as the stench will ruin the normal latitude of the temperature of the water in the ocean, as the water, as the stench carries with it, is warmer or colder than the ocean water.

To judge about the pressure of ocean currents, to finish it, 400 yews will come from the Atlantic to the Arctic Basin. Km 3 vodi, Gulfstrom for rik to carry close to 750 yew. Km 3, mіzh tim yak rіchny stіk all rіchok earthly coo warehouseє total 37 yew. km 3. Through the crossing between the northern edges of Africa and the coast of Antarctica, 6 million km 3 waterways. There is nothing of its own in the Techiya Zakhidnykh vіtrіv, which is often called the plate of the Zakhidnykh vіtriv. We already know that I will close the circle near Antarctica.

Behind the radians' pre-sluggish stretches, taken by the late and strong backward winds, blowing between 40 and 60 ° S. sh., zavdyak of one-way salinity and temperature, I am hunting all the water to the bottom. Radiansky oceanologist V. G. Kort pidrakhuvav, so the water exchange between the oceans is 48 million km 3, or 3.5% of the vast amount of ocean water on the planet. If the figure is not exactly accurate, then, at any time, it will be of an order of magnitude and allow judging about the swiftness of the exchange of water masses between the oceans at a time. Vaughn talk about those who the whole Svitovy ocean is located in uninterrupted Russia.

For example, Golfstrum often breaks on the edge of the stream, the act of the stream goes to the side, making a majestic whirlwind, as at the same time it appears in the main stream. Richny transferred by water leaks do not become permanent and change in wider fringes, but it is useful to be recognized in the weather and, especially, on the behavior of ribi. Pulsations of GolfStrum and Kurosio to lie down, completely imovirno, as a result of the change atmospheric circulation i, zokrema, pasativ. Along with the wiklicane, he moved on to the edge of the structure, changing the cutting of the current and the illumination of the eddies, to become obscure. It may be, in which there is manifested in the inflow of the wrapping of the Earth, forcefully rubbing, forcefully energetic, perhaps, in fact, playing an important role in Russian water. Mіzh іnshim, geophysicist I. V. Maksimov to direct the proof of the inflow of the hard times of the earth's axis on the periodic changes of the ocean currents. In a word, strained ocean currents are dynamic rivals in the ocean, alley rivulets pulsing and bluish in their wilder and crumbling shores.

The top currents in the ocean will flood the balls in a few hundred meters. And yak carry water in clay balls to the ocean? For a long time, we thought that it’s great and especially the bottom of the ocean water and how it’s nerdy. Ale axis has appeared new technology vimіryuvannya leaks, and a statement about the dynamics clay waters absolutely changing. At the depths of the ocean, there have been leaks of changeable strains and liquids from a centimeter to tens of centimeters per second. Near the Pacific Ocean, there is an Equatorial Plin on the sea level in the middle 100 m, there is a tight leak, it is not straight to the skid. Perebіg is called іm'am of the th first glimpse of Cromwell, and it was clear that it was baked, thrown into the water, dropped into the water much more, no more extravagantly. There is also a top leak in equatorial zone and are also direct to the meeting of the equatorial current as seen by the criterion and reported in the Atlantic Ocean by the Radian oceanographers. Wono is named after Lomonosov. The width is 200 miles, the maximum speed is at a depth of 100 m, the maximum speed is set at a depth of 56 miles for the trip, the transfer of the transport half of the transfer of the Gulf Stream and the Kurosio. The maximum speed of such a subsurface equatorial flow in the Pacific Ocean is 70 miles, in the Indian Ocean - 28 miles to go.

The last hour of the proclamation of the wondrous currents streaming in your ocean water, the dumb at the pipe with the crying stinks, has become a mystery. Tsіkave explained proponuvav for them in the special event at the 2nd International Congress Radiansky oceanologist NK Khanaichenko. Near the zone of straining surface leakage, current at the ekvor from the descent to the west, along the western shores of the continents, they pour in from the second day and during the winter. surface leaks... You will also be able to move from the coast to the surface of the water. If not, it appears, inadequately, to compensate for the waters from the distant shores of the continent. The first axis, not enough water, at the cob of pasty leaks, will close the equatorial leaks, and at the same time, the upper leaks. The stench is sufficient to replenish the leaks, if they are weak in the fallowness, because of the weakening or weakening of the passages and equatorial leaks. The system of ocean currents can serve as a butt of self-regulating physical processes on a planetary scale.

Instrumental water leaks have been accumulated for a long time. However, it is enough to prove that the water in the ocean is in post-rus... However, the pattern is far from divisive. Riznі thoughts vyslovlyuyuyutsya, for example, about those who penetrate the stream of the GolfStrum to the bottom, or nazustrіch їm for a deyakіy glybinі for a sensible leak? Some allowances, for each glide is close to 1000-1500 m in the ocean, "zero surface", de the water is unruly, so as the surface serves as a cordon for detecting leaks. It’s impossible to keep up, such a zero surface is dumb, as all the water is covered by leaks, including the horizons, as you want to take the zero surface during theoretical leakages. I will tell you more about it on the butt of the wine half The Pacific played at the 2nd International Congress 3. F. Gurikova. In a word, before the rejection of the recurrence of the folding roach, the water in the ocean is even more robotic. One day will be for the whole theoretical models, Basics on mathematical designs, іnsі go by the way іnstrumental tricks and quilting to the water mass.

In the ocean, there is still one force that can bring water into the fold. The price of the difference in the water content, as it lays in the temperature, salinity, and at great depths it is infused with a hydrostatic grip. The changes in the ocean water are insignificant, the stench is vimiryuyutsya hundreds of parts of one. Ale the strength, born of zimi zmіnami, to finish it is great, to bring it into the ruins of the waters and navigate the ocean without any participation wіth wіth. One of the wonders of geophysics. Until now, there have not yet been extinguished super-streams about those who have a leading role in the circulation of oceanic water masses - in the form of a difference in the power of water.

In an atmosphere of darkness from districts to high barometric grip, T.E. To the great turnin, in the area with a low grip - to the low turner. The water on the surface of the ocean flows from areas with a smaller area to areas with a greater area. So, progrіtі tropіchnі, less thirsty water, and poke into the polar pools, then get cold, grow shіlіnіyu, more importantly, zanyuruyuyutsya to the bottom and flow at the fast-paced right up to the depths of the ocean. The ocean is a gigantic thermal machine, which will be brought into the hands of the Sontsya power plant. Without interruption of the robot, the whole machine will transfer water exchange between the surface and the clay balls to the ocean, supplying the water with water from the sour water and the great inflow into the climate and the weather.

There, as two ocean currents converge (convergence), the drainage of the green waters is seen; in times, de-flow, diverge (divergence), water and ocean float to the surface. A slow sweat, like a fan, pumped the surface water into the ocean, a bagat for kissen, and for an hour I will flood the bags of the surface balls into the mouth for those who are in the zone of the high vise. The downward flow, nemov lift, pіdnіmaє from glybin to the living salts of phosphorus and nitrogen and to the written development of the willow and food life in the surface balls to the ocean.

From the boreal waters, from the inflowing leaks, it is also drawn along the cuttings from the water cans. It’s a phenomenon that springs up on the cliffs of the mainland mile, as it’s muddy from the coast to the bottom of the coastline. surface water; Today, cold waters, rich in living salts, are used for glybin. Areas of the ocean, de-vidbuvaetsya under the waters of the sea or the frontal zone, including the bagati on the riba.

The waterless forces of the cosmic and the earth are pouring into the water in the Svitovoy oceans: heating by water and sleepy interchanges, different in the lower latitudes, heavy heavenly lights, rubbing against the surface of the water, growing in the depth of water, etc. The collapse develops in a heterogeneous stratified mass of water on a turning and also a heterogeneous spherical surface of the earth, poorani by wisps, folds, islands and continents. Rivnyannya to the ruku in the ocean is not to be seen, and this hour of the nobility is not less important for the oceanologist, but for the meteorologist of the nobility is to rule the ruk povitryan mas... The role of leaks in the life of the ocean is great. Rukh water oils are injected into the climate and the weather, onto the ribs. Figuratively, the manifestation of flows is the whole of life, the visibility is death and death. A short walk until the rise of ocean currents and pulsations is the organization of a great number of stations in the ocean, which are used by meteorologists on land.

The roc of water masses in the oceans was put at the service of people. At first, I would like to be in the same world, in which the movement of the overwhelming masses over the surface of the planet will be allowed to transfer the weather.

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 imovinous to resemble from the Atlantean mountains to the mountains of Africa, or from the mythical 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 falls into the whole ocean anyway outskirts of the sea Much more, lower at the rychok, so they fall into whatever 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, creating a lifeless environment.

Atlas of oceans. T. 2. Atlantic and Indian oceans... L., 1977
Geography of the Holy Ocean: Atlantic Ocean... L., 1984

Flowing flows into the climates of the Pacific Uzbeks

Injection of leaks into the climate Atlantic Uzbeks

The flows of the Svitovoy ocean flow into the climate and the height of the mainland.

The warm and cold currents of the Atlantic Ocean are pouring into the climate of the coastal territories. Try to viparovannya in the area of ​​Gulfstream, so go to the pivnichno-Atlantic, to bring to the approval of the badness and a great climate of the Pivnichno-American Uzbek. Yogo warming inflow is known in the climates of all Europe. It is colder Labrodorskoe with a stretch of lining bolsh suvoriy klimat pvostrova Labrador in the same latitudes in Europe. Cold Canarska and Bengal currents to curb the hanging inflow on the climate of the western Uzbek coast of Africa in tropical latitudes, de-roasted empty spaces.

The current flows into the climate of the Uzbek Pacific Ocean. Climates of ancient and modern territories, which are located approximately at the same latitude, but they do not see much in the influx of recent currents. So, the Pacific Uzbek coast of Canada, is surrounded by a warm Pivnich Pacific stretch, there is more dense growth, lower than the Uzbek coast of Kamchatka, with a cold Kuril plin. Skhidni grasped the Great Water Ridge in Australia, surrounded by the warm Skidno-Australian Plin, sometimes covered with fools, and at the sunset of the Great America there is the dry Atacama heathland itself, so the Uzbeks will be washed by the cold, cold Peru. Shelter landscapes can be seen on the Uzbek coast, washed by the waters of the cold Californian current.

Cold currents, (Californian, Peruvian, Bengelskoe and Kanarska) pass along the remote Uzbek continents in tropical latitudes, cross over to the ocean from the surface, and soak up the empty space by ourselves.

Flowing leaks to the klimat uzberezh Indian Ocean .

Musoni flowing from the private part of the Indian Ocean may have a great inflow into the climate. The flow of the currents flies through the rock, through the monstrous winds. Samalijskoe with a stretch of lita is cold and flowing in the bik of the Indies, and the charge is navpaki.

So the very majestic flow into the climate rob the cold current of the old winds to pass through all the oceans. The current flow does not allow the snowflakes of Antarctica.

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 direction of the Uzbek coast of the United States, at about 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 the distance to the Icelandic Ocean. Another gilka turned for a week and a distance to the western end of the coastlines of Africa, the Kanarska current is still cold. The current flow collapses on the New Years and ends up with the Pivnichny Passatnoye Current, €€ as straight to the west side of 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 day passes the cold Labradorska in a stretch, boiling from the Buffin outlets and the Sea of ​​Labrador and the chilled-out coast of the New England.

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 skhіd. A part of this cold current is coming to a place and not all of your lead to the party of the African Uzbek, making a cold Benguela stretch; We will stay at the end of the day to come to the Pivdenny Passatna leak. Warmly Guinea's reach collapses on the first day of the coasts of Pivnichno-Western Africa in Guineyska Zatoka.