The most powerful current in the world's oceans. Which current in the Zusha River is fast or slow Antarctic Circumpolar Current

The average speed of ocean currents is 5 km. at one o'clock. But there are also those that significantly exceed this speed and carry with them a huge amount of water. What are the strongest currents you can find in the ocean?

Gulf Stream

This is the most powerful warm current in the World Ocean. It begins in the Sargasso Sea, then flows along the coast of the United States to California. Here the Gulf Stream turns towards Europe. The speed of the water flow is 2.5 meters per second. The maximum width of the Gulf Stream reaches 200 kilometers, and its depth is 800 meters.

Rice. 1. Gulf Stream

The water temperature in the Gulf Stream ranges from 24 degrees Celsius in winter to 28 in summer. The warm influence of the Gulf Stream softens the climate European countries on the Atlantic coast.

Antarctic Circumpolar Current

This flow is also called flow Western winds. It is located in Southern Hemisphere, around Antarctica.

The current of the Western Winds crosses as many as three oceans.

Its power is three times greater than the power of the Gulf Stream, so it can rightfully be considered the most powerful current in the World Ocean. The length of the flow of the Western Winds reaches 30 thousand kilometers, and the maximum width is 2500 kilometers. The water speed is approximately 58 meters per second. In a second, the ACC carries about 200 million tons of water - this is more than the volume of rivers on the globe.

TOP 1 articlewho are reading along with this

Rice. 2. Antarctic Circumpolar Current

El Niño

This beautiful name translated from Spanish as baby, child. However, the El Niño current is very treacherous and destructive for coastal countries. This is the warmest current in the Pacific Ocean. Its water temperature is 9 degrees Celsius higher than that of environment. This leads to the formation of hurricane-force winds in the coastal zone.

As a result, long rainfalls, droughts, and fires occur on the coast. El Niño affects millions of people and causes enormous damage to the global economy.

Rice. 3. The destructive El Niño current

North Atlantic

This current passes through the eastern part of the Atlantic Ocean. Its speed reaches 2 km. at one o'clock. The current carries about 40 million cubic meters of water per second. Due to its proximity to the mainland, coastal countries enjoy a warm climate.

Kuroshio

This is a powerful warm current Pacific Ocean. Its width is 170 km, and its depth reaches 700 m. In terms of power, this current is slightly weaker than the Gulf Stream. It passes by Japan and Kuril Islands. In the north it merges with the waters of the North Pacific Current, reaching Alaska.

To the question whether the current of the Volga is fast or slow, asked by the author Adelina Kuasheva the best answer is The nature of the Volga flow

Features of lowland rivers

2. Low flow speed
3. Wide shallow valley
Current direction





The place where the Akhtuba branch separates is sometimes taken as the beginning of the Volga delta. It is more correct, however, to count the beginning of the delta from the place where the Buzan branch separated. From here the Volga is divided into a dense network of branches and channels. The Volga delta is one of the largest deltas in our country. Numerous branches, channels, islands, lakes (called here ilmens and hollows) and sand ridges (Berovsky hillocks) occupy a total space of over 13,000 km2.

Answer from Neurologist[guru]
When we go up it's slow, but when we go down it's fast

Answer from Alexandra Gurgaeva[newbie]
The current on the Volga is slow

Answer from Put down[guru]
The average current speed is low - from 2 to 6 km/h.

Answer from Staff[guru]
The Volga is a flat river, the current is slow.

Answer from Marina Loginova[newbie]
The Volga is flat.
so the current is slow

Answer from Vika Balandina[newbie]
slow

Answer from Elizaveta Viktorovna[newbie]
average

Answer from Olga Afanasyeva[newbie]
gne54ennekuapavyvacuv45

Answer from Ksunchic Richkova[newbie]
The Volga is a flat river, which means it has slow current.

Answer from Maxim Goncharov[active]
The nature of the Volga flow
The Volga is a typical lowland river.
Features of lowland rivers
1. Small difference in height between mouth and source
2. Low flow speed
3. Wide shallow valley
Current direction
The main direction of the Volga flow is to the south.
Flowing within the East European Plain, the Volga is a classic example of a lowland river. Its longitudinal profile is close to the so-called equilibrium profile. The average slope is only 0.06°/oo. The drop is especially small in the lower reaches, where it does not exceed 0.02°/oo. According to the size and nature of the current, the Volga is usually divided into three parts: the upper current (Upper Volga) - from the source to the city of Shcherbakov, the middle current (Middle Volga) - from the city of Shcherbakov to the mouth of the Kama and the lower current ( Lower Volga) - from the confluence of the Kama to the mouth.
IN upper reaches, within the Valdai Upland, the Volga passes through the chain of Upper Volga lakes - Verkhit, Sterzh, Vselug, Peno and Volgo. At the source of the lake. In the Volga River, in the middle of the last century (1843), a dam was built - the Upper Volga Beishlot - designed to enhance the river's nutrition during low water periods and maintain navigable depths. Major tributaries Upper Volga - Selizharovka, Tverda, Mologa and Sheksna. During the years of Stalin's five-year plans, the Upper Volga was reconstructed, that is, radically reorganized. Three powerful hydroelectric power stations were built here: Ivankovskaya, Uglichskaya and Shcherbakovskaya. The dams of these hydroelectric power plants turned the Upper Volga into a chain of lakes and reservoirs, among which the Rybinsk Reservoir is the largest in the world. Waters: this reservoir was flooded by the lower reaches of pp. Mologa and Scheksny and the entire Mologo-Sheksna interfluve.
In the middle reaches, below the town of Shcherbakov, the river becomes even more full-flowing; here a number of large tributaries flow into it, the most important of which are the Oka, Unzha, Vetluga and Sura. The regime of the river's middle flow has changed significantly and is highly dependent on releases from the Rybinsk Reservoir. Below the confluence of the Kama, which in its water content is almost as good as the Volga itself, the latter becomes especially full-flowing. The width of the valley reaches 20-30 km. In the area of ​​the city of Kuibyshev, the Volga, bending around the Zhiguli Mountains, forms a giant bend - the Samara Luka, where the valley narrows to 2-3 km. The asymmetrical structure of the valley is characteristic: the right bank is high and steep everywhere, and the left bank is flat and low. The valley expands especially strongly below Stalingrad. Here the Volga on the left separates the first branch - the river. Akhtuba, which then flows as an independent stream parallel to the main channel of the Volga.
The vast space between the Volga and Akhtuba, cut by numerous channels and old rivers, is called the Volga-Akhtuba floodplain. Spills within the Volga-Akhtuba floodplain reach 20-30 km. The Lower Volga receives only relatively small tributaries: Samara, Bolshoi Irgiz and Eruslan.
The place where the Akhtuba branch separates is sometimes taken as the beginning of the Volga delta. It is more correct, however, to count the beginning of the delta from the place where the Buzan branch separated. From here the Volga is divided into a dense network of branches and channels. The Volga delta is one of the largest deltas in our country. Numerous branches, channels, islands, lakes (called here ilmens and hollows) and sand ridges (Berovsky hillocks) occupy a total space of over 13,000 km2.

Complete group work assignments.

1) Make a list water bodies your region.

There are up to 2,000 rivers and streams, of which 323 are more than 10 km long. The rivers of the Moscow region belong entirely to the Volga basin.

The largest rivers in the Moscow region are the Oka and Moskva with their tributaries. The third major river of the Klyazma region.

Rivers: Moscow, Yauza, Klyazma, Setun, Skhodnya, Khimka.
Lakes: Beloe, Kosinskie lakes, Svyatoe (lake, Moscow), Trostenskoye, Nerskoye, Krugloye
Swamps: Black, Great, Holy, Oak

2) Fill out the tables.

Table 1. Description of the river.

Table 2. Description of Moscow - rivers

Use your textbook to create a diagram.

The importance of water resources in nature and human life

Using the diagram, talk about the importance of water resources.

Think about what environmental problems are expressed by these signs. Formulate and write down.

Suggest conservation measures for class discussion that would help solve these problems.

The Question Ant and the Wise Turtle ask you to write a letter to your peers from other cities and villages, urging you to take care of water resources. In your letter, try to prove that water resources in every corner of the country need protection.

Boys and girls! All water resources(rivers, lakes, seas, oceans, streams) are the most important wealth of our planet. Clean drinking water necessary for the life of people, animals and plants. Life is not possible without water! The water is home to many fish and other animals that participate in a variety of activities. food chains. In addition, people have learned to use water resources in their economic activities. Protect water resources: keep the water clean, clear springs and streams, protect plants and animals. Save water!

Much in the world depends on the majority. The climate on the planet as well. Almost 70% of the surface globe takes up water. It determines the fate of humanity

Cross-sectional area of ​​the ACC (5)(the only one that crosses all the longitudes of the world) is huge: the depth is up to 4000 m, and the width is up to 2000 km. But it does not flow quickly - the speed does not exceed 0.7 km/h.

The most powerful currents of the World Ocean(water consumption* in m 3 /s)

* Consumption - the volume of water flowing per unit of time through cross section flow

(5) Antarctic circumpolar current 150,000,000 m 3 /s
(3) Gulf Stream 100,000,000 m 3 /s
(2) Kuroshio 80,000,000 m 3 /s

Global Ocean Conveyor connects the upper (in depth) part of the ocean water column with the lower. The length of the conveyor path is 40 thousand kilometers.

Deep water travels this path in 1.5–2 thousand years.

Solar energy reaches the Earth's surface unevenly: the maximum is at the equator, the minimum is at the poles. Thanks to the conveyor belt, ocean currents transfer heat from where there is more of it to where there is less of it, that is, from the equator to the poles.

If there were no oceans, average temperature the Earth's surface would be 36 °C lower than today and would be only –21 °C

Fastest currents**

(1) SOMALIAN SUMMER 75 CM/S
(2) KUROSHIO 50 CM/S
(3) GULF STREAM 40 CM/S
(4) AGULYASSKOE 34 CM/S
(5) ACC 28 CM/S

** Dana average speed currents

Gulf Stream flow, according to some estimates, 40 times more than the flow of all the world's rivers combined

Currents are divided into warm and cold. But the division is relative. Thus, in the “warm” North Cape Current in the Barents Sea, the water temperature in summer is up to 8 °C, and in the “cold” Canary Current in the Atlantic - all year round from 12 to 26 °C

Average wave height V Atlantic Ocean V Lately increases by about a centimeter per year. This indicates widespread climate change

The Oryol region has a well-developed river network. However most of Oryol rivers are either the sources large rivers, or their small tributaries. In the territory Oryol region are the sources of the largest rivers in the European part of Russia - the Oka, Don and Dnieper. Therefore, the Oryol region is a geographical center of nutrition for the most important river systems European part of Russia. On its territory, the surface runoff of the rivers of the Volga basin is formed. The river catchments are separated by two watershed areas. The first runs from the city of Maloarkhangelsk north to the village of Alekseevka, then northeast to the Verkhovye station and to the village of Pankovo. This hilly area is the watershed between the Oka and Zusha rivers with its tributary Neruch and the Sosnaya River with its tributary Trudy River. In the central part of the region there are elevated hills representing the watershed of the Oka and Zushi rivers, which in its southern part in the Maloarkhangelsk region connects with the watersheds of the Oka and Sosna, Oka and Desna. The second watershed between the basins of the Oka and Desna rivers is located in the southwestern part. The Oka basin occupies 60% of the region's territory and includes 1,377 rivers and streams. The Don basin includes 529 watercourses, the Dnieper - 195. The region's water fund has over 2,100 watercourses with a total length of 9,154 km, including about 180 watercourses with a length of 10 kilometers or more and with a total length of over 4,000 km. Large rivers of the Oryol region - Oka and Zusha are used to generate electricity. On the river In Oka there is a hydroelectric power station Shakhovskaya with a capacity of 510 kW, on the Zusha River - Novosilskaya (210 kW) and Lykovskaya (760 kW). The construction of the dams of these power plants significantly affected the ecology of some fish species living in Oka and Zush. The longest and most abundant rivers in the region are: r. Oka (average annual flow on the border with the Tula region is 2058 million m3); R. Zusha (tributary of the Oka, average annual flow - 988.6 million m3); R. Sosna (tributary of the Don, average annual flow on the border with Lipetsk region- 687.0 million m3). In the south-eastern part of the region there are basins of the Navli and Nerussa rivers, flowing into the Desna (a tributary of the Dnieper River), with a total annual flow of 210 million m3. The terrain provides a slow, calm flow of rivers. The rivers Zusha, Sosna and a number of other smaller rivers, due to the significant difference in elevation, have a fairly fast flow. The amount of surface runoff of the Oryol rivers is influenced by climatic factors- quantity atmospheric precipitation, seasonal air temperature and humidity. In addition, the amount of runoff is somewhat influenced by the terrain, geological structure underlying rocks, swampiness of catchment areas and the presence forest areas. Great importance in the formation of surface runoff has economic activity human and technogenic load on landscapes [Natural Resources, 2002]. The regional water fund is replenished through the creation of reservoirs and ponds that accumulate the runoff of spring floods. The water quality of many ponds is improved by numerous springs that feed the ponds, preventing them from drying out and improving flow. In total, there are more than 1,730 ponds in the region with a total area of ​​2,800-3,000 hectares. [Blinnikov V.I. et al., 1989; Fedorov A.V., 1960]. Of these, as of September 1, 2005, the Administration of the Oryol Region approved a list of fishing grounds. This list includes 608 reservoirs with a total area of ​​5105.6 hectares. Table 1 shows the distribution of reservoirs intended for fish farming needs by district of the region.