Sea flows of the Pacific Ocean. Complex physical and geographical characteristics of the Pacific Ocean

16.11.2007 13:52

The current is called the transfer of particles of water from one ocean and sea to the other.

The current hunt for the majestic masses of the ocean waters, widening with a wide swamp, lie on the surface of the ocean and the ball of water is thirsty for this glibini. On larger depths and at the bottom, there is more and more movement of particles of water, more often than not, directly from surface leaks, to become a part of the outbound circulation of the waters of the Svitovoy Ocean.

Basic strength, wiklikayut sea ​​flows These are both hydrometeorological and astronomical factors.

Until the first time zarahuvati:

1) a strong force and a ruin the force of currents, causing the difference in power through the unevenness of changes in temperature and salinity of sea water

2) hesitated the sea level, wicked over too little or too little water near the same region, as well as on the coastal runoff or wind surges and waves

3) nahil the sea level atmospheric vice, so the lowering of the sea level in the area of ​​an increased atmospheric pressure and an increase in the level of the lower pressure of the sea

4) rubbing the wind on the surface of the sea waters and grip the wind on the top of the water.

To others to be introduced flushing power Misyatsya and Sontsya, so that it continuously fluctuates in conjunction with the periodic changes in the intermittent growth of the Sontsya, Earth and Mysyatsya and expands horizontally during the flow of water in excess

Immediately after the detection of a leak, victorious by the same number of forces due to the significant forces, second forces are recognized, as they infuse leaks. As soon as a leak occurs, the stench doesn’t make it look like it’s a leak.

To such forces are admitted:

1) the strength of the Coriolis, which is seen in the winter season, every little bit, when it collapses to the right, and in the new season it goes straight to its own hand, so it’s possible to lay it down in the breadth of the world and often

2) the power of rubbing

3) center force.

Sea flows follow the following signs:

1. For walking, tobto. behind the factors, scho їх viklikayut - a) gustinnі (gradієntnі) leaks; b) drifts and winds; c) basic leakage; d) baroperative; e) tidal; f) compensation for leaks, such as a lot of more incompressibility of water (irregularities), through the need to remember the drop in water, for example, from the rise of water in the middle of the current flow.

2. Behind the districts.

3. For triviality or for style: a) permanent leakage, how to go rik at rik in the same straight line with deyakoi shvidkistu; b) time-lapse leaks, which can be affected by time-based reasons and change in their own right and liquidity in fallowness every hour of every day of the magnitude of the established force; c) Periodic flow, which changes directly and quickly, up to the period of the magnitude of the fuel-creating forces.

4. For physical and chemical characteristics, for example, warm and cold. Moreover absolute value the temperature for the characteristics of the overrun is not significant; the temperature of the waters of warm leaks is the temperature of the waters, which are blown by the sinks, the temperature of the waters of the cold streams is lower.

The main flows in the Pacific Ocean, which are injected into the Primor'ya climate

Kurosio (Kuro-Sio) The Kurosio system is divided into three parts: a) vasne Kurosio, b) drift of Kurosio and c) Pivnichno-Tioheanska current. Vlasne Kurosio is called a warm flow in the western half of the Pacific Ocean and the island of Taiwan at 35 ° Mon., 142 ° N.

Serve as a corn of Kurosio in the winter season Philippines Islands... Near the island of Taiwan, Kurosio has a width of about 185 km and a width of 0.8-1.0 m / s. Far away to see the right-hander and pass through remote shores The Ryukyu Island Ridge, moreover, the speed of growth for an hour is up to 1.5-1.8 m / s. Increase the number of items Kurosio vidbuvatsya vlіtka vіtku at the passing vіtrah lіtnі pіvdenno-skіdny monsoon.

On the way to the western edge of the island of Kyushu, there is a current flow to two branches: the headway to pass through the Van Diemen channel to the Pacific Ocean (Vlasne Kurosio), and іnsha gіlka directly to Korean duct(Tsusimska current). Vlasne Kurosio when we walk to the side of the island of Honshu - Misu Nazima (35 ° Mon, 140 ° N) - turn to turn, being seen from the coast cold Kuril current.

At points with coordinates 35 ° mon. Lat., 142 ° n. From Kurosio there are two heads: one is direct for the private day, and one is for the private meeting. The time for the remainder of the gilka penetrates far into the pivnich. With a wine-and-dividing bottle, you can be promoted right up to Commander Islands.

The drift of Kurosio is called a heat leak between 142 and 160 ° N, the Pivnichno-Tikhookeanska leak is still to be repaired.

Naybіlsh stіykim from all three warehouse system Kurosio є by stretching out Kurosio, I want to win schilny until the great seasonal collection; So at the chest, at the period of the greatest development of the winter mouson, when the house is from the winter or on the first call, there, dear to start, Kurosio starts to grow, the ships often see leaks, direct for the winter. It is worth noting about the great accumulation of the current from the monastic winds, how the great power of that steel may be from the ancient shores of Asia.

Kurosio inflow to the climate of coastal regions of Eastern Asia Also, the warming of waters in the region of Kurosio wiklikє will collect the warming up of the winter monsoons.

... Kurilskaya leak

The Kuril current, which is called Oya-Sio, is a cold current. It will emerge from the Bering Sea and flow from a spate for every day by name Kamchatka current along the western shores of Kamchatka, and then along the western shores of the Kuril ridge.

Have winter hour through the ducts Kuril ridge(Especially through the small canals) from the Sea of ​​Okhotsk to the Pacific Ocean, a lot of cold water flows, and some and some ice, which is a significant world Kurilskaya leak... The rate of increase in the rate of the Kuril current fluctuates close to 0.5-1.0 m / s, while the flow rate is often 0.25-0.35 m / s.

Cold Kuril current is anywhere on the surface, penetrating on the first day of the Trohi Dal Misu Nodzima - the north-western edge of the island of Honshu. The width of the Kuril current for misu Nozima will become close to 55.5 km. Unsatisfactory p_d surface water the ocean and continue for 370 km at the bottom of the water leak.

Main trends in the Sea of ​​Japan

The Japanese sea is roasted in the winter-western part of the Pacific Ocean along the mainland coast of Asia. Japanese islandsі Sakhalin Island v geographic coordinates 34 ° 26 "-51 ° 41" Mon. W, 127 ° 20 "-142 ° 15" W For its physical and geographical position, it is possible to be referred to the outskirts of the oceanic seas and to the city from the sumy basins by water barriers.

At the winter and winter descent, the Sea of ​​Japan is connected to the Sea of ​​Okhotsk by the channels of the Nevelskoy and La Perouse (Soya), at the descent - By the Pacific Ocean Sangarsky (Tsugaru) by the channel, on private - from Central Chinese Sea Korean (Tsusimskoy) channel. Finding a duct from them- Nevelskoy maє maximum glybin 10 m, and the greatest Sangarsky- Close to 200 m.

The most inflow to the hydraulic regime the pool may have subtropical waters, Korean duct from the Skhidno-China Sea. The rook of waters near the Sea of ​​Japan will form as a result of the global growth of the atmospheric pressure, wind fields, heat flows and water. From the Pacific Ocean to the Asian continent, there are nahil of the isobaric surfaces with the transported waters. At the Sea of ​​Japan, from the Pacific Ocean, it passes through the western part of the warm Kurosio, and passes through the South China Sea and before the water.

Through the low water of the channel near the Sea of ​​Japan, there is no more surface water. Shchorichno through the Korean watering near the Sea of ​​Japan to rise from 55 to 60 yew. km3 of warm water. The stream of water near the viglyad Tsusimsky current zmіnyutsya stretching out to rock. There is a lot of intensiveness, for example a lita - a corncob of autumn, if it’s overflowing with a dripping monsoon, it’s getting better at the backwaters of Kurosio and the water near Skhidno-Chinese sea... At tsei hour, the inflow of waters increases up to 8 yew. km3 per month. For example, in winter, the inflow of waters near the Sea of ​​Japan through the Korean irrigation changes to 1.5 yew. km3 per month. During the passage of the Tsusim current of the western shores of the Japanese islands, the sea level here appears in the middle mountain 20 cm, below the Pacific Ocean, of the western shores of Japan. Intensive flow of waters into the Pacific Ocean is already flown into the first path of the waters of the current flow of the Sangarskoy channel.

Approximately 62% of the Tsusim flow passes through the channel, after which it has become greatly weakened. Still close to 24% of the water flow, which comes from the Korean channel, flows through the La Perouse channel, and even more, the flow of warm waters becomes insignificant, but still the part of the waters is insignificant. Tsusimsky current penetration into Tatarska duct... At a new level, through the nebagato recess of the Nevelskoy canal, a large number of cykh waters are turned for pivden. In the world of the flow of water flowing near the Tsusimskiy current, for the first time before it, water flows and flows out of the stream are turned on. The wake of the strumen, when they go out to the west in front of the Tatar channel, get angry with the waters, when they go out, they shape those that go with a small speed for the day Primorska leak.

For the first day from the inflow of Peter the Great, the current flows on two springs: Korean duct, and the downward strum seeks to turn and end up with the Tsusim current. I will save the bottle and call it Pivnichno-Korean current.

The entire system of leaks is re-insured, creating a cyclonic circulation for the sea, at which circuit periphery it is stored from the heat, and from the cold.

The rise in temperature and fluidity on the surface of the Sea of ​​Japan is presented according to the data of the electronic Atlas of Oceanography of Beringov, Okhotsk and Japan Sea (TOI FEB RAS) for the day, birch, grass, linden, heather, jovten.

The fluidity of the currents is near the half of the sea of ​​the sea, below the half of the sea. Calculated by the dynamic method of stench at the top 25 meter ball Tsusimsky current falling out 70 cm / s Korean prototypes up to approximately 29 cm / s at the latitude of the La Perouse channel and less than 10 cm / s Tatar prototypes... Shvidkist cold current sutta mensha. You will be able to increase for a day by a few centimeters for a second at a break of up to 10 cm in a private part of the sea.

In addition to persistent flows, drifting and winding flows are not frequently spared, so that the floods of water flow. There are drops, if there are any total leaks, warehouses are also from late, drift and tidal-long leaks, which are straightened along a straight cut to the coast or out of the coast. The first vipadku stench is called “cuddly”, the other “vidzhimny”. The fluidity of the slack does not change 0.25 m / s.

Water exchange through the ducts is a dominant inflow into the hydraulic regime of the winter and skid half of the Sea of ​​Japan. Ti, go through Korean duct The subtropical waters of the Kurosio river, stretching out to the sea, warm the northern regions of the sea, and the waters that lie down to the Uzbek coast of the Japanese islands right up to the La Perouse channel, after all the waters of the lower part of the sea, beyond the warmth.

Literature: 1. Doronin Yu. P. Regional Oceanology. - L .: Gidrometeozdat, 1986 p.

2. Stoshin I. V. Oceanology. - L .: Gidrometeozdat, 1953 p.

3. The sailing of the Sea of ​​Japan. Part 1, 2. - L .: Kartfabrika VMF, 1972

4. Atlas of oceanography of Beringov, Okhotsk and Japanese seas (TOI FEB RAS). - Vladivostok, 2002 p.

Head of UGMM
Yushkina K.A.

Current

The Pacific Ocean reaches a lot of winds from the approach of the Shid and from the new one to overcome the latitudinal streams of water. In the ocean, there are two majestic rings of water: the wine and the air. The private cycle includes Alaska, Kurilsk, Kurosio, Pivnichno-Tikhookeanska, Californian and Pivnichnu passatnu leaks. Pivdenno-Pasatna, Skhidno-Australiska, Pivdenno-Tikhookeanska, Peruvian and Antarctic circumpolar leaks (Fig. 5). Today, they are pouring into the overflow of heat in the ocean and on the nature of the adjacent continents. Thus, the flow of warm water flows from the remote tropical coasts of the mainland to the lower ones, also at low latitudes. Zakhidna chastina the ocean is a little warmer than the last one. In the middle high latitudes - navpaki, the middle part of the ocean warmer beyond the western one.

Small. 5. Pacific Ocean

Alaska current - heat flow in the winter-skidny part of the Pacific Ocean, the pivnichnaya gilka of the Pivnichno-Pacific current.

In the meantime, enter Alaska outflow from the beginning of the day, pass at the beginning and end, at the top of the inflow, turn to the beginning; after the turn is meaningful. Through the skidny channels of the Aleutian Islands it penetrates the Bering Sea. Expand to great glibini, to the bottom, it's easy to keep an eye out for the current, wicked by the irregularities of the bottom. The speed of the overrun in the intervals from 0.2 to 0.5 m / s. If you move around, you will be affected by the change in temperature, on the surface it will be 2 to 7 ° C at a fierce level, and from 10 to 15 ° C at the serpentine. Salinity of water - 32.5 ‰.

Kuril current, or Oyasio - a cold current at the winter entry of the Pacific Ocean, as it shores its cob near the waters of the Pivnichny The icy ocean... On a weekday to reach shidny uzberezhzh Japan, while staying with the warm flow of Kurosio, has had to be forced to settle for the Pivnichna Pacific current. Kurilskie is holding out in a serious manner in a flood ghet klimat Dalekoy Skhodu, especially Kamchatka and Chukotka, deeper between the widening of the number of destructions for the day, below the analogous latitudes of Siberia. Against the backdrop of Kamchatka, the Kuril Islands and the Japanese islands. The speed of the Kuril current varies from 0.25-0.35 m / s up to 0.5-1.0 m / s. The width of the Kuril current on the island of Honshu becomes close to 55.5 km.

Kurosio, Inodi Japanese Current - the heat of the current from the early and western shores of Japan in the Pacific Ocean. Kurosio transfer heat salt water Pivdenno-Chinese and Shidno-Chinese seas at the winter latitude, meaningfully helping the climes. If the main stream of Kurosio does not enter the Sea of ​​Japan, three yogo gilki (Skidno-Korean current, Tsusimska current that is unchangeable between them) penetrate the yo aquatorium through the Tsusimske channel, and some distant sea Warm currents of Kurosio penetrate at mid to 40 ° Mon. NS. і dalі for pіvnіch. Flow rate approx. 6 km / year Pivden, up to 1-2 km / year pivnich. The water temperature at the crescent on the outside is 28 ° C to 25 ° C at the night, at the fierce one from 18 ° C to 12 ° C.

In general, there is a lower edge of the current of fewer values, lower than that of the past. On the western edge, there is a rise in surface temperatures during the transition from the current to the west, probably to the "cold weather" near Gulfstrom, I want a different world. Techia Kurosio is rich in chomu podibna to Golfstrom. The current is significantly infused into the climate of the islands of Shikoku, Honshu and Kyushu.

Pivnichno-Pacific current - heat of the oceanic flow in the private part of the Pacific Ocean. The continuation of the current Kurosio on the way from Japan is called the Kurosio Drift, and later - the Pivnichno-Pacific Current. Rukhak from approaching the highway near the coast Wine of America from shvidkistu 25-50 cm / s.

In the midst of the Pacific Ocean, the Pivnichno-Pacific current during the first half of the 40th parallel syagaє 170 ° Mon. sh., de galluzhuєt in the warmth of Alaska, which is straight to the shores of Pivdennaya Alaska for the winter, and part of the waters are consumed by the Bering Sea, and another went by the name of the Californian to flow for the last time

Californian current is a cold surface current in the private part of the Pacific Ocean. Collapse from winter to winter time of the Kalifornyi as well as of the winter-Pacific current, so that during the winter it goes over to the Friday Passatna leak. Shvidk_st is close to 1-2 km / year., Width 550-650 km., Water temperature from 15 to 26 ° C. Salinity at night is 33-34 ‰.

The winter season as a result of the passage of the Californian current and against the 10 ° and 20 ° winter latitude in the western direction until a quiet winter, leaving before the winter warms of the Philippines is not going to go

Equatorial (mіzhpasatna) prototypes - are forced to prototypes in the midst of the winter passate current and the new passate current, which should be promoted in the equatorial Atlantean region of the Earth, in all the quiet Indian oceans.

The upper mid-range protrudes in the Atlantic, Pacific and Indian oceans from the 19th century. The given leaks are directing the circuit against the overburdened air and against the main surface leaks. Intermittent problems are affected by the transverse unevenness of overburdened vitreous (passages), that is, the fluidity and vitrate are significantly affected, even to the point of being determined, largely due to strength and deterioration.

Pivdenna Passatna Leak (Pivdenna Equatorial Leakage) - named after all the winds in the region - passats, which dim from the west - heat flows in the Holy Ocean, which pass through the northern tropical latitudes.

Near the Pacific Ocean Of America- approximately in the areas of the Galapagos Islands, and on the way to the shores of New Guinea and Australia. The winter cordon of the current rises from 1 ^ ° of the winter latitude up to 3 ^ ° paternal latitude charge. Bilya of the western Uzbek coast of the Pacific Ocean, the current flows to the head - part of the current zgorta to the circuit, pouring into the Equatorial prototype. Another great current is the current Australian current, to fix the Australian coastline. The fluidity of the flow ranges from 24 to 80 miles for additional. Average performance indicator is close to 40 miles for extra. Water temperature -? 32? ^ ° С.

Shidno-Australian current - a heat leak in the Pacific Ocean, which is seen from the European Passage current, seen on the first day of the winds of Australia. The price of the most oceanic current of the Australian coastline is within reach of the maximum flexibility in any number of times. little glibini vdovzh of the Australian continental shelf. Taking a cob off the tropical Coral Sea, passing through the Tasman Sea, between Australia and New Zealand.

The economical-Australian trend is to rob the climate of New Zealand and the declining Uzbek economy of Australia is more warm and natural, tropical is replaced by the subtropical; a wider range of tropical marine fauna in the subtropical region of the north-eastern Uzbek coast of Australia. There are 7 universities, but it is more important to establish 2-3 universities. The water temperature is around 25 ° C.

The Peruvian Current (Humboldt Protrusion) is a cold surface current in the Pacific Ocean, which is a neck of the Antarctic circumpolar current. Collapse for a week on a private island between 45 and 4 centuries old latitudes along the western shores of Peru and Chile. The speed is close to 0.9 km / year, the water vitrate is 15-20 million m / s, the water temperature is 15 to 20 ° C.

Deyakі prelіdniki see at the Peruvian current I will coast that ocean current, between which pass the Pivdenna Peruvian-Chileyska protitech At 4 ° Pivdennoy latitude Peruvian current go to the west and get angry with the Pivdennaya Passatnoy current.

Antarctic circumpolar (or by stretching Zakhidnykh Vіtriv) - the whole earthly kulu mіzh 40 ° і 50 ° F The speed is 04-09 km / year, temperature is 12-15 ° С. Qiu current is often called "re-sounding forties", which is why there are fierce storms. Peruvian current appears in the Pacific Ocean.

The scheme of the circulation of water in the Pacific Ocean may be more accurate repeating the scheme of circulation in the Atlantic: here we do not only know two counts of leaks on the sides of the body - one from the falling of water behind the year's arrow, and the one that flows from the ringing bell, but the analogue Kuro-Sio.

Due to the fact that the oceans are often built up to the details.

Pivdenna Passatna current flow to be repaired in the Galapagosky islands near the viglyadi decilkoh teplikh (from 25 to 28 °) strumeniv. Tech_ya, a straight line from the start to the west, the most beautifully turned around 5 ° pd. NS. ta 3 ° n. NS. In addition to its names, I have the greatest flexibility at this part of the city, as I lie on the first step of the square (between 0 ° and 3 ° Mon. lat.). At all times of the current flow, go over the ekvator to a private leak, to start at the time of his weakening, pushing for a personal leak.

At sunset, in Oceania, Pivdenna Pasatna flows through the islands and is often weak. Approximately in the New Guinea area, we see left, then descend for the afternoon at the sight of the Eastern Australian current along the coast of Australia, more than once we have seen a turn around the Earth New Zealand, Straighten back to the skid across the ocean, catching the smogs between 40 and 45 parallels. Having reached the western Uzbek coast of the Holy America, the water masses will fix the cold Peruvian current here, so that we can go to a private island for a weekend. Secha (38 ° 3 ′ long lat.) To Misu Blanco (4 ° 27 ′ long lat.).

Pivnichna Passatna flow is direct to the west, spreading in the main in smoothies at 10 and 20 ° N. NS. Pivnichne that Pivdenna leak distribution of equatorial prototypes (from the approach to the route from the island of Mindanao to the Panama inlet). Yak and all prototypes, here it is, compensation.

Between the Philippines and the Carolinian Islands, the waters of the Winter Passage Current are seen in the winter and give the ear of the Kuro-Sio current. On the vidminu of the GolfStrum, far from all equatorial waters are taken here directly; a part of them penetrates into the Chinese sea, between the Philippines and Taiwan, a part in the Zhovta sea and the Koreyska channel; Also, there is a head leak, as soon as it is possible for a private drive, it is unimportant for its speed from 90 to 100 km on the way, so that it can go up to 35 ° N. sh., mensh virazno, nіzh Floridska leak. It’s important to set up the main points of the Kuro-Sio: once you remember the entire space between the Ryu-Kyu and Bonin islands, then it’s not viral in the whole zone. Vlіtku Kuro-Sіo expands to the distance, not narrow, protein nikols do not go (close to Japan) to the beginning of the 40th parallel. The water is warm, ale and cold streams, but nicholas have not been spared by the Florida current. Shorter than it seems, Kuro-Сіo is the price of a small flow.

From the shores of Japan, there is a turn and an irregular drift (Pivnichno-Tikhookeanske stretch) up to 145 ° W. d., de і distribute: more weak zagortaє on the pivnich, collapsing against the year old shoots, - tse Alaska leak; іnsha gilka turned on the evening of the banks of the Californian coast and accepted the cold Californian current. Remaining angry with the Pivnichnaya Passatnoy current.

(In the winter part of the Pacific Ocean, along the shores of Kamchatka and the Kuril Islands, on the cold day of the Kamchatka current, to form at the sight of a large number of songs on the island,

Yaksho vi knew the mercy, be weasel, see a fragment of the text and natisnit Ctrl + Enter.

It is not uncommon to call it Great because it is tied for low reasons. According to him, this is the reason why they wash between five continents. At the entrance to the new one they adjoin the shores of Eurasia and Australia, at the descent - the Uzbek continents of the Pivnichnaya and Pivdennaya America, and at the end of the day - the cordon of Antarctica. As it seems, the ocean is stretched out from both sides of the adequate. In other words, close to half of the area of ​​the St. Thirdly, the ocean is the greatest and the most awesome. Take an ear of giant winds and tropical hurricanes from yogo mountains, which will take an hour to make. ruin_vni diy... I, nareshty, the bottom of the Pacific Ocean has a great potential, from sub-water ridges, girskih lantsyugiv. There are most of the islands on the surface of the ocean.

Warm and cold currents of the Pacific Ocean

The comrades of the Pacific Ocean are setting themselves up for a leak. Tse vіtrami, as to sweep over the water surface waters in a vise. The stench swirls so much that you can make two completed colas at the wine and drink. Near the depths of the ocean, there are a number of warm leaks, which are called so, so that the temperature is higher, lower than the temperature indicators of the waters. Superficial leaks The Pacific Ocean is also present, albeit in the minority. The stench is seen through the inflow of the old and pasatny povitryan mas on the surface of the ocean.

Japanese, Alaskin and Skhidno-Australian current

Kurosio abo the Japanese current on the fringes of Japan from the beginning of the day. This is the name of the flow of nabula through the dark blakitny vidtinok of its waters. Vono to set up for a show of growth at the level of the waters of the Chinese Sea and the part of the ocean. Described heat leak The Pacific Ocean redirects the flows of water from the Pivdenno-Chinese and Shidno-Chinese Seas, which are warm and salty, at the winter latitude, by the very timid climes of the sea.

Already, in the old-fashioned part of the given ocean, the Alaskan current is taking place. From the beginning of the day, it will flow into the Alaska inflow, directly at the beginning of the day and turn towards the beginning of the day. Then, passing, flow into the Bering Sea.

Skhidno-Australian heat flow of the Pacific Ocean non-drop-wise I will name it. Even more water flows to some of the best shores in New Zealand and the western shores of Australia. Through the flow of water, the climate on the Uzbeks is tropical. Tobto is overwhelmed by the warmth of the weather.

Pivnichna Tikhookeanska and Pivdenna Equatorial current

Krym perakhovanih vishche, warm currents of the Pacific Ocean є Pivnichne Pacific and Pivdenne Equatorialne.

Pivnichna Pacific current in the midst of the pivne shores of the aquatorium. Look at the results of the meeting of Kurilskiy. Tsia vodna masa to say goodbye from cordons to Uzbek Pivnichnaya America.
Pivdenna Pasatna or Pivdenna Equatorial heat flow of the Pacific Ocean is called so through the approval of the current flow. And the male water stream, scho circulating, winykah through vіtri-pasati, scho dim from the outset to the west. Nowadays the coastal cordon of the Indian American coastline is closer to the end of the New Guinea and Australian cordon. Let's get away with it. On one drive, turn to the skid. The heat flow of the Pacific Ocean from another part of its go to the Schedule-Australian leak.

Californian and Peruvian current

In addition to warm flows near the nadra of the Pacific Ocean, there is also a cool circulation of waters.

Californian current, which is not only cold, but above the surface, expands into the private part of the ocean. Vono Omivan uzberezhzha Kalifornia right from the weekend for the winter.

The Peruvian Pacific Ocean is also called Humboldt's name. Wono is also superficial and non-glib. There is a flow close to the remote part of the Holy America in the region of Peru and Chile.

Techia Cromwell and Oyasio

At the Pacific Ocean, the Cromwell current is still cold. Vono vvazhaєtsya pіdpoverkhnevim, і renamed my names to the American oceanographer, which was a current in one of its expeditions.

Kuril current or Oyasio shores its ear at the nadra of the Pivnichny Ice Ocean and the Pacific Ocean from the pivnichny call. Tsey vodniy potik zoomovlyuє climatic mind Kamchatka and Chukotka. The current is to stretch across the shores of Kamchatka, the Kuriles and the Japanese islands. Yogo bring a bagat of ribbons and other seafood.

In such a rank, rich in that because of the fact that the order with the shores of the continents, is laid down in such a class and natural versatility. Some stinks can be transferred from cold and warm water, and by themselves it is infused into the temperature on the continents and a number of fallen goods.