The movement of water in the ocean is brief. The movement of water in the ocean - sea waves, tsunamis, ebbs and flows. Warm and cold currents

Dynamics of the waters of the World Ocean. Waves. General provisions

One of the fundamental characteristics of the World Ocean, as part of the hydrosphere, is the continuous movement and mixing of waters.

The movement of water masses occurs not only on the surface of the World Ocean, but also in its depths, up to the bottom layers. The dynamics of water is observed throughout its thickness, both in the horizontal and vertical directions. These processes support regular mixing of water masses, redistribution of heat, gases and salts, which ensures the constancy of chemical, salt, temperature and gas compositions. The forms of movement (dynamics) of water masses in the World Ocean include:

waves and swell;
waves of a spontaneous nature;
currents and tides;
convective currents, etc.

Waves is a phenomenon resulting from external forces of various nature (wind, sun and moon, earthquakes, etc.) and representing periodic systematic fluctuations of water particles. The main reason for the formation of waves on the surface of any water body, which includes the waters of the oceans, is wind and wind processes. Insignificant wind speed equal to about $0.2-0.3$ m/s in the process of air friction on the surface of water masses causes a system of insignificant uniform waves called ripples. The ripples appear with one-time gusts of wind and instantly die out in the absence of the influence of wind processes. If the wind speed is $1$ m/s or more, then in such cases wind waves are formed.

Formation of unrest in the waters of the oceans can be caused not only by the influence of wind processes, but also by a sharp change in atmospheric pressure, tidal forces (tidal waves), natural processes - earthquakes, volcanic eruptions (seismic waves - tsunamis). Ships, yachts, ferries, boats and other shipping engineering structures, in the course of their direct activity, when cutting the surface of the water mirror, they create special waves called ship waves.

Waves that are formed solely under the influence of external forces that cause them are forced waves. Waves that continue to exist for a certain amount of time after the force that causes them has ceased to operate are called free. Waves that are formed on the surface of the water mirror, as well as in the uppermost layer of the water masses of the World Ocean (up to $200$m) are surface waves.

Waves that originate in the deeper parts of the oceans and are not visually visible on the surface of the water are called internal waves.

The strength and size of wind waves directly depend on the speed of the wind, the time component of its impact on the surface of the water mirror, as well as the size and depth of the space of water masses covered by wind processes. The height of the waves, from the base to its crest, is usually no more than $5$ meters, waves with a height of $7$ to $12$ meters or more are much less common. The largest wind waves in size and strength are formed in the southern hemisphere of the Earth, this is due to the fact that in this part the ocean is continuous, there are no large land areas in the form of continents or islands, and strong and constant westerly winds influence the height of the waves. Waves in this region of the World Ocean can be up to $25 meters high and hundreds of meters long. There are much fewer waves in open and especially inland seas than in the open ocean. For example, in the Black Sea, the maximum recorded wave height is $12$ meters, in the Sea of Azov these figures are an order of magnitude lower - $4$ meters.

At the moment when wind activity stops in the ocean, long gentle waves are formed - swell. Swell is the most ideal and undistorted waveform. Since the swell is essentially a free wave, this wave propagates much faster than other waves. The length of such a wave in a swell state can be up to several hundred meters, and taking into account their low height, swell wave processes in the World Ocean, especially in its open areas, are practically imperceptible.

However, since waves propagate at a significant speed, they tend to fall on the coastal part of the land several hundred and even thousands of kilometers from the place of their initial formation. The movement of water masses actively decays with depth. At a depth equal to the wavelength, the waves practically stop.

Since the length of wind waves in many cases is not significant, even with the most active waves, at a depth of $50$ meters and deeper, these waves are practically not noticeable. Thus, the strength of the waves directly depends on its height, length and width of the crest. But the main role still belongs to her height.

Due to the volatility of the aquatic environment and regular dynamics and mixing, the layers of the water masses of the World Ocean have varying degrees of density, viscosity, speed, and salt composition. The most striking example is the areas of the World Ocean, where there are such phenomena as the melting of glaciers, icebergs, in places of intense precipitation and at the mouths of full-flowing rivers. AT this case the waters of the oceans are covered with a layer of fresh water, forming the necessary conditions for the formation of the so-called internal wave passing on the surface of the watershed of fresh and salty water masses.

Remark 1

On the basis of oceanological research, it was found that internal waves in the open World Ocean occur with the same frequency as surface waves. Quite often, the main mechanisms for the formation of internal waves are the processes of changes in atmospheric pressure, wind speed, earthquakes, tide-forming and other factors. Internal waves are characterized by a significant amplitude, but not a high propagation speed. The height of internal waves usually reaches $20–30$ m, but can be up to $200$ m. Waves with such a height are characterized as a rare and intermittent phenomenon, but still occur, for example, in southern Europe in the area of the Strait of Gibraltar.

Currents of the oceans

sea currents- one of the most important forms of movement in the oceans. Currents are called relatively regular periodic and constant deep and surface movements of the masses of the waters of the World Ocean in a horizontal direction. The main currents of the World Ocean are shown in Fig.1.

These movements of water masses play one of the primary roles both in the life of the World Ocean and its inhabitants, which include:

exchange of waters of the World Ocean;
creation of special climatic conditions;
relief-forming function (conversion coastline);
transfer of masses of ice;
creation of habitat conditions for the life of the biological resources of the oceans.

Also one of the leading roles ocean currents is the circulation of the atmosphere and the creation of certain climatic conditions in various parts of the planet.

A huge number of ocean currents can be divided into categories:

by origin;
on sustainability;
by depth of location;
by the nature of the movement;
on physical and chemical properties.

According to the origin of the current, in turn, are divided into: friction, gradient and tidal. Friction currents are formed under the influence of wind forces. Thus, frictional currents, which are caused by temporary winds, are called wind currents, and those caused by prevailing winds are called drift currents. Among the gradient currents, one can distinguish: barogradient, runoff, waste, density (convection), compensatory. Runoff currents are formed as a result of the tilt of the sea level, which is caused by the inflow of fresh river water into ocean water, precipitation or evaporation; wastewater is due to the slope of the sea level, which is characterized by the inflow of water from other areas of the sea under the influence of external forces.

Currents lead to a decrease in the volume of water in one part of the oceans, causing a decrease in the level, and an increase in another. The difference in levels between parts of the World Ocean instantly leads to the movement of neighboring parts, which seek to eliminate this difference. Thus, compensatory currents are born, that is, currents of a secondary nature that compensate for the outflow of water.

Tidal currents are created by the components of tide-forming forces. These currents have the highest speed in narrow straits (up to $22$ km/h), in the open ocean it does not exceed $1$ km/h. In the sea, currents are rarely observed due to only one of these factors or processes.

According to the stability of the flow, they are divided into constant, periodic and temporary flows. Permanent currents are currents that are always located in the same areas of the World Ocean and practically do not change their speed and direction for a particular season or calendar year. Striking examples of such currents include trade winds, such as the Gulf Stream and others. Periodic - these are currents, the direction and speed of which change based on the changes that caused them. Temporary - these are currents caused by random causes (gusts of wind).

According to the depth of the current, it can be divided into surface, deep and near-bottom ones. By the nature of the movement - meandering, rectilinear and curvilinear. According to physical and chemical properties - warm, cold and neutral, salty and desalinated. The nature of the currents is formed from the ratio of the temperature indicators or, respectively, the salinity of the water that form the current. If the temperature of the currents exceeds the temperature of the surrounding water masses, then the currents are called warm, and if lower, they are called cold. Similarly, salty and freshened currents are determined with this.

Seismic and tidal waves

Seismic waves (tsunami)

The main reason for the formation of seismic waves (tsunamis) is the transformation of the relief of the ocean floor, which occurs as a result of the movement of lithospheric plates, which result in earthquakes, landslides, dips, uplifts and other phenomena that are spontaneous and occur instantly in significant areas of the ocean floor. It should be noted that the mechanism of generation of seismic waves largely depends on the nature of the processes that transform the topography of the ocean floor. For example, during the formation of a tsunami in the open ocean in the process of the appearance of a dip or crack at the bottom of a section of the World Ocean, water instantly rushes to the center of the formed depression, first filling it, and then overflowing, forming a huge column of water on the surface of the ocean.

Remark 2

The formation of a tsunami in the open ocean and their collapse on the coast is usually preceded by a decrease in the water level. In just a few minutes, the water recedes hundreds of meters from the land, and in some cases even kilometers, after which tsunamis hit the coast. The first largest wave is usually followed by an average of $2$ to $5$ of smaller waves, with an interval of $15-20$ minutes to several hours.

The speed of propagation of tsunami waves is huge and amounts to $150-900$ km/h. Falling on the coasts and settlements located in the zone of influence of such waves, tsunamis can take human lives, destroy infrastructure, industrial buildings and social facilities. An example of the most devastating recent tsunami is the $2004 Indian Ocean tsunami, which killed more than $200,000 people and caused billions of dollars in damage.

The appearance of a tsunami, at the moment, can be predicted with a high coefficient of accuracy. The basis of such forecasts is the presence of seismic activity (shocks) under the water column of the World Ocean. As a rule, predictions are made by means of the following methods:

seismic monitoring;
monitoring with the help of tide gauges (above the surface of the World Ocean);
acoustic observations.

These methods allow developing and taking preventive measures aimed at ensuring life safety.

tidal waves

Remark 3

tidal waves- these are phenomena that occur under the influence of the forces of attraction of the Moon and the Sun and are characterized by periodic fluctuations in the level of the World Ocean. The active forces of attraction in the Earth-Moon system, as well as the centrifugal force, explain the formation of tidal waves, one of which occurs on the side that faces the Moon, and the other on the opposite side.

The formation of tidal activity is due not only to the participation of the Moon, but also to the influence of the Sun, however, due to the much greater distance of the Sun from the Earth, solar tides are more than $2$ times less than lunar ones. The key influence on the tides is the shape of the coastline, the presence of islands, and so on. This reason explains how tidal fluctuations in the level of the World Ocean at the same latitude vary over a wide range. Minor tides are observed near the islands. In the open waters of the World Ocean, the rise of water during high tide can reach no more than $1$ meter. The tides reach much greater values in the mouths of rivers, straits and in bays with winding shores.

There are only four of them. Wind waves, tsunamis, ebbs and flows, currents.

The waters of the oceans are constantly in motion. There are two types of water movement: 1) oscillatory - excitement; 2) progressive - currents. The main reason for the formation of waves is the wind, the average height of wind waves is 4-6 m, off the coast of some countries, the wave height reaches 20 m or more, and the wave length is more than 250 m. High waves are an opportunity to organize world-class surfing. When the wind subsides, long gentle waves of swell remain for a long time, on which it is so pleasant to swing in the warm sea. Near the shore, due to friction on the bottom, the waves overturn, forming surf. Off the coast with strong surf, swimming in the sea is almost impossible. In seismically active areas of the ocean floor, as a result of earthquakes or volcanic eruptions, huge waves arise - tsunamis, causing catastrophic destruction. Areas where they visit quite often are unfavorable for tourism. Another type of unrest is tidal movement. The reason for their occurrence is the influence of the attraction of the Moon and the Sun. In the narrow bays of a number of countries, the height of the tides is so high that this phenomenon has become an important condition that attracts many tourists. Currents are horizontal movements of water in the seas and oceans, a kind of "river in the ocean". They are characterized by a certain temperature, direction and speed. The influence of currents on climate has already been discussed, and in this section we will consider sea and ocean currents directly as a condition for the development of tourism. Of course, if a powerful current passes near the coast, this worsens the tourist opportunities of the territory, especially if it is a cold current, since people swimming in the sea or even small ships can be carried far from the coast.

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The global ocean is in constant motion. In addition to the waves of the world, the waters also interfere with currents, tides and tides. All these are different types water traffic in the global ocean.

It is difficult to imagine a perfectly peaceful ocean surface. Quiet - full world and the absence of waves on the surface is a rarity. Even in calm and clear weather, you can notice waves on the surface of the water.

And this corrugation and disgusting foam shafts are born from the force of the wind.

The stronger the wind, the larger the waves, and the speed of their movement is higher. Waves can travel thousands of miles from where they originated. Waves contribute to the mixing of sea water and enrich them with oxygen.

The largest waves are observed between 40° and 50°C.

where the strongest winds blow. These latitudes are called assault sailors or rhythmic latitudes. Areas of high waves are also found off the US coast near San Francisco and Tierra del Fuego. Storm waves destroy coastal structures.

tsunami

The highest and most destructive tsunami waves. The reason for their formation are underwater earthquakes. In the open ocean, tsunamis are invisible. On the coast, the wavelength decreases, the height rises and can exceed 30 meters.

These waves cause accidents in coastal areas.

sea currents

The oceans have strong water currents. Constant winds cause surface winds. Some flows (compensation) compensate for the loss of water moving from areas of its relative abundance.

A stream whose water temperature is higher than the temperature of the surrounding waters is called hot, if it is lower - cold.

Warm currents carry warmer waters from the equator to half, cold currents carry cold water in the opposite direction. Thus, the flows redistribute heat between geographical latitudes in the ocean and have a significant impact on the climate of the coastal areas where they carry their waters.

One of the strongest ocean currents is the Gulf Stream. The speed of this flow reaches 10 kilometers per hour and is 25 million cubic meters of water per second.

Ebb and flow

The rhythmic rise and roll of water in the oceans is called periphery and flow.

The reason for their occurrence is the action of the gravitational force of the moon on the surface of the earth. Twice a day, under the rises, it covers part of the ground and comes out twice, exposing the coastal bottom. Tidal wave energy that people have learned to use to generate electricity in tidal power plants.

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. Water. oceans are in constant motion. Among the types of water movement, waves and currents are distinguished. According to the reasons for the occurrence of waves, they are divided into wind, tsunami and forced-flow

The cause of wind waves is the wind that leads the vertical oscillating motion water surface. The height of the waves depends more on the strength of the wind. Waves can reach a height of 18-20 m. If in the open ocean and the water is subject to vertical movements, then near the coast it makes a forward movement, forming a surf.

The degree of wind waves is evaluated on a 9-point scale.

. Tsunami- These are giant waves that occur during underwater earthquakes, the hypocenters of which are located under the ocean floor.

The waves caused by tremors propagate at a tremendous speed - up to 800 km / h. In the open ocean, the height is negligible, so they do not pose a danger. However, such waves, running into shallow water, grow, reaching a height of 20-30 m, and fall on the coast, causing great destruction.

The tidal waves are associated with the attraction of water masses. World Ocean. Moon and. Sun.

The height of the tides depends on the geographical location and the dissection and configuration of the coastline. M. The maximum height of the tides (18 m) is observed in the bay. Fandi.

Currents are horizontal movements of water in the oceans and seas in certain constant ways; they are kind of rivers in the ocean, the length of which

reaches several thousand kilometers, width - up to hundreds of kilometers, and depth - hundreds of meters

According to the depth of location in the water column, surface, deep and near-bottom currents are distinguished.

According to the temperature characteristics, the currents are divided into warm and cold. The affiliation of a particular current in warm or cold is determined not by their own temperature, but by the temperature of the surrounding waters. A current is called warm, the waters of which are warmer than the surrounding waters, and cold - cold ones.

The main reasons for the occurrence surface currents are the winds and the difference in water levels in different parts of the ocean. Among the currents caused by the wind, drift (caused by constant winds) and wind and (arise under the influence of seasonal winds) are distinguished.

The general circulation of the atmosphere has a decisive influence on the formation of a system of currents in the ocean.

Scheme of currents in. The northern hemisphere forms two rings. The trade winds cause trade wind currents directed to equatorial latitudes. There they collect east direction and move to the western part of the oceans, raising the water level there.

This leads to the formation of sewage currents moving along the eastern coasts of the South (Gulf Stream,. Kuro-Sio,. Brazilian,. Mozambique, Madagascar,. East-Australian). In temperate latitudes, these currents are picked up by the prevailing westerly winds and directed to the eastern part of the oceans.

water in the form of compensatory currents moves up to 30 latitudes, from where the trade winds drove out the water (California,.

Canarian), closing the southern ring. The bulk of the water displaced by westerly winds moves along the western coasts of the continents to high subpolar latitudes (North Atlantic, mid-Pacific). From there, water in the form of sewage currents, which are picked up by northeast winds, is directed along the eastern coasts of the continents to temperate latitudes (Labrador, Kamchatka), closing the northern ring.

In the southern hemisphere, only one ring is formed in the equatorial and tropical latitudes.

The main reason for its existence is also the trade winds. To the south (in temperate latitudes), since there are no continents in the way of the waters, picked up by the western winds, a circular current is formed. Western winds.

Between the trade wind currents of both hemispheres along the equator, an interpasatia countercurrent is formed.

In the northern part. Indian Ocean monsoonal circulation generates seasonal wind currents

geography The movement of water in the ocean

The oceans are in constant motion. There are two types of movement: enthusiasm and flows.

Excitement. The main cause of waves is the wind. Wind waves - is only an oscillatory motion of the surface of the water. It is compared to the area of "bread", along which the waves flow from the wind.

The stronger and longer the wind and the larger the water area, the larger the waves. Waves up to 18-20 m and more were observed several times. Away from the coast, the water translates forward motion, and due to the higher speed of the water particles from above, where there is less friction, the waves are thrown back, surf is formed. A 9-point scale is used to assess the degree of wind waves in the sea: the greater the excitement, the higher the result. Waves affect the well-being of people, they destroy the coast, strong enthusiasm is dangerous for ships.

At the same time, the waves are mixed. water, contribute to the enrichment of the water column with oxygen and heat and the removal of nutrients to the surface. All of these support the life of organisms.

In addition to wind waves, waves from another source tsunami. These are giant waves caused by underwater and coastal earthquakes, as well as volcanic eruptions that propagate at high speeds - up to 800 km / h.

In the open ocean, they are low, and in tsunamis, tsunamis reach 20-30 m, they have tremendous energy and, in this regard, cause great devastation on the coast.

tidal waves cause oscillations on the surface of the World Ocean relative to its average level, combined with the attractiveness of the Earth along the Moon and the Sun.

Given the dependence of the industry and the configuration of the coast, the tide is very different. The highest elevation (18 m) is visible in the Bay of Fundy, near Newfoundland; in Russia, in Shelikhov Bay

12 m. On a lunar day, which is 50 minutes longer than sunlight, there are two tides and two layers on Earth.

A tidal wave with it and sea vessels turns into a tithe and tens of kilometers.

Sea currents. These are horizontal movements of water in the oceans and seas, characterized by a certain direction and speed. Their length reaches thousands of kilometers, width - tens, hundreds of kilometers, depth - hundreds of meters. The extended comparison between river and river is not very successful.

First, in rivers, water moves along the slope, and sea currents can move due to the influence of the wind, despite the slope of the surface. Second, sea currents have lower flow velocities, averaging 1-3 km/h. Third, the flows are multiple and multi-layered, and there are eddy systems on both sides of the core.

Sea currents are sorted according to the nature of the characteristics. By duration constant streams (for example, north and south trade winds), repeated(summer and winter monsoons in the north of the Indian Ocean or tides in the coastal regions of the World Ocean) and temporarily(episodic).

In the position of depth in the water column, surfaces differ, deep currents near the bottom.

Based on temperature, warm and cold currents.

This classification is not based on absolute temperature, but on relative water temperature. Warm currents have a water temperature higher than the surrounding water, cold currents - on the contrary. Warm, usually directed from the equator to the poles, cold - from the drug to the equator.

By origin between surface currents:

Drift caused by constant winds; Wind that occurs under the influence of seasonal winds; Waste water flowing from excess water areas, and hoping to level the surface of the water; compensatory compensatory water losses in any part of the ocean. Most threads are called joint work many factors.

It's installed today specific system of ocean currents, mainly due to the general circulation of the atmosphere (Fig.

12). Their scheme is as follows. On each hemisphere, on both sides of the equator, there are large streams of currents around permanent subtropical high pressure: clockwise in the northern hemisphere, counterclockwise in the southern hemisphere. Among them found equatorial arch from east to east. In temperate subpolar latitudes of the northern hemisphere Small annular rings are observed around the minimum pressure in the opposite direction from the clock, in the southern hemisphere - from west to east around Antarctica.

The most stable currents are north and south trade wind(Equatorial) streams on both sides of the equator in the Pacific, Atlantic and southern hemispheres of the Indian Ocean, pumping water from east to west.

The eastern coasts of the continents in tropical latitudes are characterized by Warm wastewater streams: Gulfstream, Kuroshivo. Brazil, Mozambique, Madagascar, East African Republic. These analog currents are not only in the source, but also in the physical and chemical properties of water.

In moderate width, under the influence of constant westerly winds, there are warm currents in the North Atlantic and North Pacific in the northern hemisphere and cold(and it would be more correct to say neutral) the course of the westerly winds, or Western drain, - South.

This strong current forms a ring in three oceans around Antarctica.

Close big cycles cold compensation currents analogs along the western coast of the continents in tropical latitudes:

12. World Ocean:

1 - warm currents, 2 - cold currents

California, Canary Islands, Peru, Benguela, Western Australia.

In Ljubljana small current rings It should be noted warm and cold labrador In the Atlantic around the periphery of the Icelandic low and the like Alaska and Kuril-Kamchatskaya - in the Pacific Ocean at the edge of the Aleutian Low.

In the northern Indian Ocean, monsoonal circulation creates seasonal winds of wind: from east to west, from west to east.

It's still very well expressed here. Somali stream - the only cold current from the equator.

It is associated with the southwest monsoon, unloading water off the African coast from the Somali peninsula and thereby causing cold deep water to rise.

In the Northern Arctic Ocean the main direction of water and ice movement from east to west, from the Novosibirsk Islands to the Greenland Sea. There it is that the research stations" North Pole"(SP) complement their existence, starting with SP-1 - the heroic four papans (1937-1938).

Arctic augmented Atlantic waters in the shape of North Cape, Murmansk, Svalbard and New land currents whose waters are saltier and therefore denser, submerged under the ice.

The importance of sea currents for the climate and nature of the earth in general and especially coastal areas is excellent.

Sea currents, together with air masses, transfer heat and carry frost between latitudes. Warm and cold currents in all climatic zones maintain the temperature difference in the western and eastern coasts of the continents and disrupt the territorial distribution of temperature. For example, without the icy Murmansk harbor across the Arctic Circle and on the North American coast north of ᴦ.

Negative winter temperatures in New York. The currents affect the amount of precipitation. Warm currents contribute to the development of convection and precipitation. The astronauts point to the characteristic shapes of the clouds that accompany the warm streams along their entire length.

Cold currents, which weaken the vertical exchange of air masses, reduce the likelihood of precipitation. For this reason, the territories are washed by warm currents and, under the influence of air currents on their side, the climate is humid and the territories that are washed by cold currents are dry.

Sea currents also promote water mixing and carry nutrients and gas exchange, and aid in the migration of plants and animals.

Natural resources of the ocean, its protection

Organic (biological) ocean resources.Οʜᴎ are the highest values, especially fish.

The share of fish is up to 90% of all resources of the organic ocean. First of all in the world, fishing is a footprint - almost a third of the sun? his catch is cod and produces a lot of flakes. The wealth of the ocean is salmon and especially shard. The main fish catch falls on the shelf zone. Fish is used not only as food. This is fodder flour (sardoni, etc.), technical fat, for fertilizers.

Bird hunting (sailors, seals, furs) and whaling is now restricted.

In the countries of Southeast Asia and some other warmer coastal countries, bivalves (oysters, mussels, scallops, squid, octopus, etc.) and echinoderms - sea cucumbers are often found. An important natural source of the ocean is algae used for cooking, iodine, as a fertilizer for feed, and for making paper, glue, textiles, and so on. D. While the oceans are large, it is important to protect them from depletion from destruction due to pollution of water bodies in order to ensure natural renewal in order to move from widespread use and free hunting to cultural holding - marine animal farming and algae cultivation.

Chemical and mineral resources. It, first of all, dissolves its chemical elements in water, as well as minerals lying on the bottom and in the ground.

Due to distillation, millions of cubic meters of fresh water are produced every year from sea water. There are more than 100 medical plants in the world in the "thirst" regions (Kuwait, Western USA, the city of Shevchenko in the Caspian Sea, etc.).

At the same time, the price of such fresh water is still high. Salt, magnesium, bromine, potassium are extracted from sea water.

The main minerals mined in the sea on the shelf are oil and gas (the Persian and Mexican Gulfs, the North Sea, oil stones in the Caspian and other areas).

Their production continues to grow rapidly, and in the coming years it is expected that half of all oil and gas resources will be produced from offshore fields. Thus, only in the North Sea in 1987, 165 million tons of oil and 83 billion km3 of gas were produced, although the first fountains first appeared in 1964.

Now there are 300 drilling machines owned by different countries, and over 6,000 km of pipelines and pipelines on the seabed. The coal industry began (England, Japan), des ?? eznoy rude (in Newfoundland), tin (Malaysia) and others. Esomanganese nodules, large reserves of phosphate rock, and building materials are covered with sediments at the bottom of the ocean. Along the coast of South Africa, diamond mining is taken from rivers off the ground.

Energy resources of the oceans.Οʜᴎ are huge.

There are already (France) and declared power plants operating on the energy flow (PES). In the hot belt, hydrothermal stations operate with differences in hot surface temperatures and cold deep waters. Sea waters contain deuterium (heavy water) - the future fuel of nuclear reactors.

If they learn to use wave energy (there are projects), humanity will receive an inexhaustible source of energy.

The great importance of the ocean in terms of traffic.

Protection of the oceans. This is a necessary international problem. During the scientific and technological revolution, the flow of pollutants into the ocean increased significantly: industrial waste, oil, domestic sewage, fertilizers, pesticides, etc.

This causes disruptions in natural interactions and dynamic balance. Due to its mobility, the ocean proved to be light over large areas. Especially harmful to the sun??? its pollution is daily oil, and according to scientists, there are now about 10 million in the ocean. A ton of oil and oil products during their production, washing tanks, their accidents. Film oil destroys moisture and gas exchange, including oxygen, destroys plankton, fish and even the Sun? those. living organisms that are concentrated mainly in the surface layer of water.

To understand the nature and mysteries of the oceans, we need a variety of scientific research.

Today they are often implemented in many countries and coordinated by UNESCO (United Nations Educational, Scientific and Cultural Organization). The study of the global ocean, which belongs to all mankind, has become a prime example of international cooperation.

An unusual new method is to study the ocean from space. From space, ocean water dynamics, interaction with the atmosphere, ice observation, especially along the paths of the North Sea, dangerous natural disasters (tsunamis, storms, underwater volcanic activity), assessment and forecasting of food supplies, especially fish, shelf exploration for minerals, monitoring water pollution, analysis of the consequences of environmental pollution and much more.

They organize special international conferences, which, based on the latest scientific data, determine the rational use of the resources of the World Ocean and the protection of its waters.

Questions and tasks:

What is the global ocean and what are its parts? Why is it conditional?

2. Specify the conditions: sea, bay, strait, peninsula, island.

3. Tell us about the classification of the seas by location. Give examples.

4. What is the correct distribution of surface water temperature in the World Ocean? What are the reasons for this?

5. What is the composition of salt in the oceans?

Its medium salty? How and why does the salinity of surface ocean waters change from the equator to the poles?

What movements of water do you know in the oceans? Specify the types of waves.

7. What are sea currents? How are they sorted?

8. Condition and note the maximum sea currents. Tell us about the source of the currents, their temperature.

What are the natural resources of the ocean?

10. Why does the World Ocean need protection? Tell us about the most important environmental issues ocean at the current stage?

Sushi water

On the origin of the earth's waters. Why are these waters mostly fresh? Why are they unevenly distributed on the surface of the continents? What is the provision of a particular land dependent on water?

ground water

Groundwater is the water that is found in the soil and rocks of the upper earth's crust. Fill loose rock pores and hard rock cracks.

They are found in all three states of aggregation: liquid, solid and gaseous. Groundwater is produced mainly by penetration into the depths of precipitation during rain or snow and melting ice.

Part of the groundwater comes from water vapor condensate that enters the earth's crust from the atmosphere or is released from magma. On plains formed by sedimentary rocks, layers with different water permeability usually change. Some of them can easily tolerate water (sand, pebbles, gravel) and are named in this regard. permeable Others have water (clay, crystal jars) and are called waterproof, or waterproof. On impervious rocks, water is retained, filling the gap between permeable permeable rock particles and forms aquifer. There can be several such horizons in the same area, sometimes up to 10-15.

The water of deep aquifers in most cases is formed during the formation of sedimentary rocks in which they are embedded. Under conditions of presence, groundwater is divided into soils, soil and intermediate waters.

ground water, as the name suggests, they are closed in the ground. They usually do not fill all the spaces between soil particles.

The floor of water is like free (gravity), movement under the influence of gravity and related, maintained by molecular forces.

Groundwater that forms an aquifer on the first surface of the impermeable layer is called Earth. Aquifers covered, sealed between waterproof layers interplastični. Due to the shallow surface of the water table, it experiences significant seasonal fluctuations: it increases even more when precipitation falls or snow melts during the dry season.

During harsh winters, groundwater can freeze. These waters are more susceptible to pollution.

The depth of groundwater in different natural areas varies.

This is primarily determined by climatic conditions: in the degrees of the desert and desert provinces, groundwater lies much deeper than in forest and tundra landscapes.

The degree of disintegration of the territory becomes a significant influence on the depth of groundwater occurrence. Deeper and deeper fragments of the terrain with rivers, ramparts and ravines, deeper groundwater.

Unlike groundwater, interstitial water levels are more constant but less variable.

Interplastic water is cleaner than groundwater. If meploplastic water completely fills the aquifer and is under pressure, they are called pressure. All water has a spiral,

In layers that lie in concave tectonic structures. The openings of the orifices lift these waters upwards and pour them out to the surface or flow at a sufficient height of the head.

Such waters are called artesian(Fig. 13).

Groundwater moves slowly along the slope of the aquifer. In river valleys, you can open beams, ravines, layers (usually groundwater), their natural sources are formed on the surface of the earth - resources or springs. Special source - geysers, which regularly releases hot water and steam at a height of up to 60 m.

Οʜᴎ are formed mainly in areas of modern volcanism, where light magma is near the surface. Geysers are found in the United States, the USSR (in Kamchatka), Iceland, New Zealand.

Groundwater differs in chemical composition and temperature.

Upper groundwater horizons are usually fresh (up to 1 g/l) or weakly mineralized, deeply buried horizons are often significantly mined (up to 35 g/l or more). They are frozen at temperatures up to +20 "C) and thermal (from +20 to +100 ° C). Thermal water usually has a high content of various salts, acids, metals, radioactive and rare earth elements.

Groundwater is very important in nature and human economic activity.

It is the most important food source for rivers and lakes, with the formation of karst groundwater and landslide landforms.

Rice. 13. The structure of the arteve basin:

1 - meploplastic water in sand, 2 - waterproof rocks, (clay), 3 — Spring, 4 — interstitial water pressure level, 5- oil gusher

they supply plants with moisture and dissolve nutrients in them.

With surface appearance, groundwater can cause waterlogging processes. Man is widely used for domestic, industrial and agricultural purposes. * A large number of different chemical substances(iodine, Glauber's salt, boric acid, various metals) are obtained from thermal waters.

The thermal energy of groundwater is used to heat buildings, greenhouses, generate electricity, and at the end of groundwater is used for treatment various diseases person.

Education

How are ocean currents different from waves? The nature and possibilities of these phenomena

Do you know how ocean waters move? How are ocean currents different from waves?

Are these processes connected and what benefits does a person derive from them? Let's try to answer these questions...

ocean waters

The ocean acts as a single organism that never stands still. This is the largest water body on the planet.

The world ocean is divided into four regions (sometimes five) - Pacific, Atlantic, Indian and Arctic, based on its differences and characteristics in different regions.

It develops and interacts with the earth's crust and atmosphere. The ocean does not stand still, it is constantly in motion, the result of which are tides, waves, currents.

Numerous processes contribute to the emergence of these phenomena. Some events are regular, while others occur suddenly.

The movement of ocean waters largely depends on the movement of air, and its temperature affects the formation certain properties water.

At the same time, there is also an opposite effect, when the ocean influences the course of atmospheric processes.

How are ocean currents different from waves?

The appearance of waves, currents, tides is facilitated by the constant circulation of the atmosphere, the occurrence of winds.

Their formation is influenced by solar energy and the attraction of the moon. The factors influencing the strength, nature and power of water flows are the topography of the bottom and the movement of the Earth.

To determine how ocean currents differ from waves, consider both phenomena in detail. In short, we can say that waves are formed temporarily, most often this is facilitated by wind currents over the surface of the water.

Sometimes earthquakes become the cause, then not just waves, but tsunamis appear.

Currents, on the contrary, are longer-term phenomena. Their main difference from waves is that they do not necessarily form on the surface of the water, they can also be present in its thickness.

They do not always depend on the wind and often have the opposite direction with it.

sea currents

We roughly figured out how ocean currents differ from waves. Now let's talk about this in more detail. Currents are the horizontal water flows of the oceans and seas, which have a constant path and direction.

It's like rivers in the midst of other waters.

Depending on the depth, they are superficial, near-bottom and deep. By temperature, they are divided into cold, warm and neutral, based on the difference compared to the surrounding waters. Currents are also classified according to the nature of their occurrence, the nature of the movement, according to physical and chemical features.

The cause of their occurrence, like waves, can be wind.

Only in this case, the wind must be constant (in certain areas) or seasonal, that is, appearing at certain times of the year. An excess of water can create a current (for example, during the melting of glaciers), or seiche fluctuations in its level.

The main reason for the formation of currents is the atmosphere.

Uneven heating of air in different latitudes creates its circulation, which contributes to the formation of ocean currents. Warm, as a rule, carry their waters from the equator, cold - to the equator.

The nature of the waves

Waves familiar to us are usually formed by wind currents over the water surface, which blow at a variable speed. This phenomenon is spontaneous, so their power and size depends on the strength of the wind. In the open sea, the wave height sometimes reaches 30 meters.

As the waves move, they gradually lose their strength.

Their speed is proportional to their length. Very often they merge, for example, when the longer ones overtake the shorter ones, which either breaks up or strengthens the waves.

The movements of the earth's crust can cause waves of extremely large sizes - tsunamis. They pick up speed up to 800 kilometers per hour. Their destructive power becomes more dangerous as they get closer to the coast, when they reach great heights, crashing onto the coast.

In the open sea, the height of the tsunami is small.

Tidal waves are a separate type. They are governed by the forces of attraction. celestial bodies. The height of such waves is strongly influenced by the geographical position, the terrain, and especially the ruggedness of the coastline. Some scientists talk about the connection between tidal waves and ocean currents, suggesting that lunar tides cause some of the currents in the ocean.

Impact and dangers of water movement

Most permanent consequences have sea currents.

They carry cold and warm masses of water, affecting the climate of the continents. Warm currents make it wet, bring precipitation, cold ones contribute to dry weather.

Prolonged exposure to cold currents can form deserts such as the Atacama in South America.

During strong waves, rip currents, or ripples, often form. This is a narrow stream of water moving perpendicular to the shore, rushing away from it. The danger of a reverse flow into the ocean lies in the fact that the surface water jet literally drags everything into the open sea.

If the current is gaining high speed, then it is quite difficult to get out of it, although it is quite possible.

To do this, it is worth rowing not to the shore, but to the side. To prevent vacationers from falling into rips, special signs or red flags are often placed at the places of their occurrence.

ocean wave energy

The old way of generating electricity using nuclear power plants no longer suits the world community. It is being replaced by alternative methods. One of them is getting energy from ocean waves. The potential for this exists in Australia, the countries of South Africa, Western Europe, North and South America on the Pacific coast.

Waves can also be used to desalinate water.

However, this method is too costly salty water corrodes everything, so keeping the equipment in working condition is not easy.

Currently, the possibility of exploiting ocean waters is only being developed.

In addition to waves, scientists plan to use the power of tides, currents, biomass energy.

The waters of the oceans are in constant motion. There are two types of movement: waves and currents.

Excitement. The main cause of waves is the wind. Wind waves - it is only the oscillatory movement of the water surface. It can be compared to a "bread" field, along which waves from the wind run. The stronger and longer the wind and the larger the water area, the higher the waves. Waves up to 18-20 m and even more were repeatedly observed. Only near the shore, the water receives translational motion, and due to the greater speed of the water particles at the top, where there is less friction, the waves overturn, and surf is formed. To assess the degree of wind waves in the sea, a 9-point scale is used: the stronger the waves, the higher the score. Waves affect the well-being of people, destroy the coast, strong waves are dangerous for ships. At the same time the waves are stirring. water, contribute to the enrichment of the water column with oxygen and heat, as well as the removal of nutrients to the surface. All this favors the vital activity of organisms.

In addition to wind waves, there are waves of other origin, for example tsunami. These are gigantic waves caused by underwater and coastal earthquakes, as well as volcanic eruptions, propagating at a tremendous speed - up to 800 km / h. In the open ocean, they are not high, but in shallow water tsunamis reach 20-30 m, they have tremendous energy, therefore they produce huge devastation on the coast.

tidal waves cause fluctuations in the surface of the World Ocean relative to its average level due to the attraction of the Earth by the Moon and the Sun. Depending on the dissection and configuration of the coastline, the height of the tides is very different. The maximum height (18 m) is observed in the Bay of Fundy, near Newfoundland; in Russia, in Shelikhov Bay, they reach

12 m. During a lunar day, which is 50 minutes longer than a solar day, two high tides and two low tides are observed on Earth. The tidal wave, and with it the ocean-going ships, enter the rivers for tens and hundreds of kilometers.

Sea currents. These are horizontal movements of water in the oceans and seas, characterized by a certain direction and speed. Their length reaches several thousand kilometers, width - tens, hundreds of kilometers, depth - hundreds of meters. The widespread comparison of currents with rivers is not entirely apt. First, in rivers, water moves along a slope, and sea currents under the influence of winds can move in spite of the slope of the surface. Secondly, sea currents have a lower current speed, on average 1-3 km / h. Thirdly, the flows are multi-jet and multilayer, and on both sides of the axial zone they represent a system of vortices.

Sea currents are classified according to a number of criteria. By duration, there are constant currents(for example, North and South trade winds), periodical(summer and winter monsoonal in the north of the Indian Ocean or tidal in the coastal parts of the oceans) and temporary(episodic).

According to the depth of location in the water column, surface, deep, and bottom currents are distinguished.

On the basis of temperature - warm and cold currents. This classification is based not on the absolute, but on the relative temperature of the water. Warm currents have a water temperature higher than the surrounding water, cold ones do the opposite. Warm, as a rule, are directed from the equator to the poles, cold - from the poles to the equator.

By origin, among the surface currents are:

drift, caused by constant winds; wind, arising under the influence of seasonal winds; sewage flowing from areas of excess water and seeking to level the surface of the water; compensatory, compensating for the loss of water in any region of the ocean. Most currents are caused by the combined action of a number of factors.

Currently installed certain system of ocean currents, primarily due to the general circulation of the atmosphere (Fig. 12). Their scheme is as follows. In each hemisphere, on both sides of the equator, there are large circulations of currents around permanent subtropical baric maxima: clockwise in the northern hemisphere, counterclockwise in the southern. Between them revealed equatorial countercurrent from west to east. In temperate - subpolar latitudes of the northern hemisphere small rings of currents are observed around baric lows counterclockwise, in the southern hemisphere - the current from west to east around Antarctica.

The most stable currents are Northern and southern trade winds(equatorial) currents on both sides of the equator in the Pacific, Atlantic and southern hemispheres of the Indian Oceans, "pumping" water from east to west. Off the eastern coasts of the continents in tropical latitudes, warm waste streams: Gulf Stream, Kuroshivo. Brazilian, Mozambique, Madagascar, East Australian. These currents are analogues not only in origin, but also in the physicochemical properties of waters.

In temperate latitudes, under the influence of constant westerly winds, there are warm North Atlantic and North Pacific currents - in the northern hemisphere and cold(it would be more correct to say neutral) the course of the West winds, or Western drift, - in the south. This powerful current forms a ring in the three oceans around Antarctica.

Close big circles cold compensation currents-analogues along the western coasts of the continents in tropical latitudes:

Rice. 12. Scheme of currents of the World Ocean:

1 - warm currents, 2 - cold currents

Californian, Canarian, Peruvian, Benguela, Western Australian.

AT small rings of currents It should be noted warm Norwegian and cold labrador current in the Atlantic along the periphery of the Icelandic low and similar Alaskan and Kuril-Kamchatskoe - in the Pacific Ocean along the periphery of the Aleutian Low.

In the northern part of the Indian Ocean, the monsoon circulation generates seasonal wind currents: in winter from east to west, in summer from west to east. In summer it is still well expressed Somali current - the only cold current from the equator. It is associated with the southwest monsoon, which drives water away from the coast of Africa near the Somali peninsula and thereby causes the rise of cold deep waters.

In the Arctic Ocean, the main direction of water movement and ice drift is from east to west, from the New Siberian Islands to the Greenland Sea. It is there that the research stations "North Pole" (SP) end their existence, starting with SP-1 - the heroic four of the Papanins (1937-1938). The Arctic is replenished with waters from the Atlantic in the form North Cape, Murmansk, Svalbard and Novaya Zemlya currents, the waters of which are more salty and therefore more dense sink under the ice.

The importance of sea currents for the climate and nature of the Earth as a whole and especially coastal areas is great. Sea currents, along with air masses, carry out the transfer of heat and cold between latitudes. Warm and cold currents in all climatic zones maintain temperature differences on the western and eastern coasts of the continents and disrupt the zonal temperature distribution. For example, the ice-free port of Murmansk is beyond the Arctic Circle, and on the coast North America freezing winter temperatures north of New York City. Currents also affect the amount of precipitation. Warm currents contribute to the development of convection and precipitation. Astronauts note characteristic cloud formations that accompany warm currents along their entire length.

Cold currents, weakening the vertical exchange air masses reduce the possibility of precipitation. Therefore, areas washed by warm currents and influenced by air currents from their side have a humid climate, and areas washed by cold currents are dry. Sea currents also contribute to the mixing of water and carry out the transport of nutrients and gas exchange, with their help, the migration of plants and animals is carried out.

Natural resources of the ocean, its protection

Organic (biological) resources of the ocean. They are of the greatest value, especially fish. Fish account for up to 90% of all organic resources in the ocean. In the first place in the world fishery are herrings - almost a third of the total catch, a lot of cod and flounder are caught. The wealth of the ocean is salmon and especially sturgeon. The main fish catch falls on the shelf zone. Fish is used not only as a food product. It goes to fodder flour (anchovy, etc.), technical fat, and fertilizers.

St. John's hunting (walruses, seals, fur seals) and whaling are now limited. In the countries of Southeast Asia and some other warm coastal countries, mollusks (oysters, mussels, scallops, squids, octopuses, etc.) are widely eaten, and trepangs are among echinoderms. An important natural resource of the ocean is algae, which is used for food preparation, for iodine production, as fertilizer, for livestock feed and for the manufacture of paper, glue, fabrics, etc. Although the organic resources of the ocean are large, it is necessary to protect them from depletion, from death due to pollution of water areas, ensure natural regeneration, switch from extensive use and free hunting to cultural economy - breeding of marine animals and cultivation of algae.

Chemical and mineral resources. This is, first of all, the water itself, the chemical elements dissolved in it, as well as the minerals that occur at the bottom and in the soil. Millions of cubic meters of fresh water are annually extracted from sea water as a result of distillation. More than 100 desalination plants are already operating in the world in “areas of thirst” (Kuwait, the western United States, the city of Shevchenko in the Caspian Sea, etc.). However, the cost of such fresh water is still high. Salt, magnesium, bromine, potassium are extracted from sea water.

The main minerals extracted from the sea on the shelf are oil and gas (the Persian and Mexican Gulfs, the North Sea, "Oil Rocks" in the Caspian and other areas). Their production continues to grow rapidly, and in the coming years it is planned to extract half of all oil and gas from offshore fields. So, only in the North Sea in 1987, 165 million tons of oil and 83 billion km 3 of gas were produced, although the first wells appeared recently - in 1964. Now there are 300 drilling platforms belonging to different countries, and more than 6000 km of oil and gas pipelines. The extraction of coal (England, Japan), iron ore (near the Newfoundland peninsula), tin (Malaysia), etc. has begun. The ocean floor is covered with sedimentary ferromanganese nodules, large reserves of phosphorites and building materials. Off the coast of South Africa, diamonds are being mined, carried by rivers from land.

Energy resources of the oceans. They are huge. Tidal power plants (TEPs) are already in operation (France) and are being designed. Hydrothermal stations operate in the hot zone, using the temperature difference between warm surface and cold deep waters. Sea water contains deuterium (heavy water) - the future fuel of nuclear reactors. If they learn to use the energy of waves (there are projects), then humanity will receive an inexhaustible source of energy.

The importance of the ocean in terms of transport is enormous.

Conservation of nature of the World Ocean. This is an urgent problem of international scale. In the age of the scientific and technological revolution, the flow of pollutants into the ocean has sharply increased: industrial waste, oil, domestic wastewater, fertilizers, pesticides, etc. This leads to a violation of natural relationships and dynamic balance. The ocean turned out to be easily vulnerable immediately over large spaces due to its mobility. Oil pollution is especially detrimental to all living things, and according to scientists, about 10 million tons of oil and oil products enter the ocean every year during its extraction, tanker washing, and their accidents. The oil film disrupts moisture and gas exchange, including oxygen exchange, destroys plankton, fish and, in general, all living organisms that are concentrated mainly in the surface layer of water.

To understand the nature and mysteries of the World Ocean, versatile scientific research is needed. They are now widely held in many countries and coordinated by UNESCO (United Nations Educational, Scientific and Cultural Organization). The study of the World Ocean, which belongs to all mankind, has become a vivid example of international cooperation.

Fundamentally new method- exploration of the ocean from space. From space orbits, the study of the dynamics of ocean waters, its interaction with the atmosphere, observation of the ice situation, especially along the Northern Sea Route, dangerous natural phenomena (tsunamis, typhoons, underwater volcanic activity), assessment and forecast of food reserves, in particular fish, study shelf in order to search for minerals, water pollution control, analysis environmental impact caused by pollution, and much more.

Special international conferences are held, which, based on the latest scientific data, make decisions on the rational use of the resources of the World Ocean and the protection of its waters.

Questions and tasks:

1. What is the World Ocean, and what parts is it divided into? Why is this division conditional?

2. Define the concepts: sea, bay, strait, peninsula, island.

3. Tell us about the classification of the seas by location. Give examples.

4. What pattern has been established in the distribution of the temperature of the surface waters of the World Ocean? What are the reasons for it?

5. What is the composition of the salts of the oceans? Its average salinity? How and why does the salinity of the surface waters of the ocean change from the equator to the poles?

6. What movements of water in the oceans do you know? Name the types of waves.

7. What are sea currents? How are they classified?

8. Name and describe the largest sea currents. Tell us about the origin of currents, about their temperature.

9. What natural resources does the ocean have?

10. Why does the ocean need to be protected? Tell us about the most important environmental problems of the ocean at the present stage?

Land waters

Remember! On the origin of land waters. Why are these waters mostly fresh? Why are they unevenly distributed on the surface of the continents? What determines the supply of water to a particular land area?

The groundwater

Groundwater is water found in soils and rocks in the upper part of the earth's crust. They fill the pores of loose rocks and cracks in hard rocks. They can be in all three aggregate states: liquid, solid and gaseous. Groundwater is formed mainly due to infiltration into the depths of precipitation during rains or melting snow and ice. Part of groundwater arises from the condensation of water vapor that enters the earth's crust from the atmosphere or is released from magma. On plains composed of sedimentary rocks, layers with different water permeability usually alternate. Some of them easily pass water (sands, pebbles, gravel) and are called therefore permeable, others retain water (clay, schist) and are called waterproof, or waterproof. On water-resistant rocks, water seeping down is retained, fills the gaps between the particles of the overlying water-permeable rock and forms aquifer. There can be several such horizons in the same area, sometimes up to 10-15. The water of deep aquifers in most cases was formed during the formation of those sedimentary rocks in which they are enclosed. According to the conditions of occurrence, groundwater is divided into soil, ground and interstratal.

ground water, as their name indicates, they are enclosed in soils. Usually they do not fill all the gaps between the soil particles. Ground water can be free (gravitational), moving under the influence of gravity, and related, held by molecular forces. Groundwater that forms an aquifer on the first water-resistant layer from the surface is called ground. The underlying aquifers enclosed between two impermeable layers are called interstratal. Due to the shallow occurrence from the surface, the groundwater level experiences significant fluctuations according to the seasons of the year: it either rises after precipitation or snow melts, or decreases during dry periods. In harsh winters, groundwater can freeze. These waters are more susceptible to pollution.

The depth of groundwater occurrence in different natural areas is different. It is primarily determined by climatic conditions: in steppe, semi-desert and desert landscapes, groundwater occurs much deeper than in forest and tundra landscapes. The degree of dismemberment of the territory has a great influence on the depth of groundwater. The stronger and deeper the dissection of the terrain by rivers, beams and ravines, the deeper the groundwater is.

Unlike the ground level, the level of interstratal waters is more constant, it changes less over time. Interstratal waters are cleaner than groundwater. If the interstratal waters completely fill the aquifer and are under pressure, they are called pressure. All waters have pressure, concluded

nye in layers occurring in concave tectonic structures. Opened by wells, these waters rise up and, with a sufficient pressure height, pour out to the surface or gush. Such waters are called artesian(Fig. 13).

Groundwater moves slowly along the slope of the aquifer. In river valleys, gullies, ravines, layers can open (usually groundwater), their natural outlets to the earth's surface are formed - sources, or springs. A peculiar type of sources - geysers, periodically ejecting hot water and steam to a height of up to 60 m. They are formed mainly in areas of modern volcanism, where hot magma lies close to the surface. Geysers are found in the USA, the USSR (on Kamchatka), in Iceland, New Zealand.

Groundwater varies in chemical composition and temperature. The upper horizons of groundwater are usually fresh (up to 1 g/l) or slightly mineralized, deep-immersed horizons are often significantly mineralized (up to 35 g/l or more). By temperature, they are divided into cold (up to +20 "C) and thermal (from +20 to + 100 °C). Thermal waters usually have a high content of various salts, acids, metals, radioactive and rare earth elements.

Groundwater has great importance in nature and human activities. This is the most important source of nutrition for rivers and lakes, with the participation of groundwater, karst and landslide landforms are formed, they

Rice. 13. Scheme of the structure of the artesian basin:

1 - interstratal waters in sands, 2 - waterproof rocks, (clays), 3 - spring, 4 - level of pressure interstratal waters, 5- flowing well

supply plants with moisture and nutrients dissolved in them. With a close occurrence from the surface, groundwater can cause waterlogging processes. They are widely used by man for household, industrial and agricultural purposes. * A large number of various chemicals (iodine, Glauber's salt, boric acid, various metals) are obtained from thermal waters. The thermal energy of groundwater is used to heat buildings, greenhouses, generate electricity, and finally, groundwater is used to treat a number of human diseases.

The movement of the waters of the World Ocean………………………………………………3

Western border currents - Gulf Stream and Kuroshio……….6

Equatorial currents……………………………………………...8

Circulation of polar waters………………………………………………10

Waves and tides……………………………………………………...11

Tsunami……………………………………………………………………12

Tides………………………………………………………………..12

Bibliographic list ....………………………………………………13

The movement of the waters of the oceans

According to its physical state, water is a very mobile medium, therefore in nature it is in continuous motion. This movement is caused by various reasons, primarily the wind. Influencing the waters of the ocean, it excites surface currents that carry huge masses of water from one region of the ocean to another. The energy of the translational movement of surface water due to internal friction is transferred to the underlying layers, which are also involved in the movement. However, the direct influence of the wind extends over a relatively small (up to 300 m) distance from the surface. Below in the water column and in the near-bottom horizons, the movement occurs slowly and has directions associated with the bottom topography.

Surface currents form two large gyres separated by a countercurrent near the equator. The whirlpool of the northern hemisphere rotates clockwise, and the southern hemisphere - counterclockwise. When comparing this scheme with the currents of the real ocean, one can see a significant similarity between them for the Atlantic and Pacific oceans. At the same time, it is impossible not to notice that the real ocean has a more complex system of countercurrents near the boundaries of the continents, where, for example, the Labrador Current (North Atlantic) and the Alaska Return Current (Pacific Ocean) are located. In addition, the currents near the western margins of the oceans are characterized by higher speeds of water movement than those of the eastern ones. The winds apply a couple of forces to the surface of the ocean, rotating the water in the northern hemisphere clockwise, and in the southern hemisphere - against it. Large eddies of ocean currents result from this pair of rotating forces. It is important to emphasize that winds and currents are not one-to-one. For example, the presence of the fast Gulf Stream off the western shores of the North Atlantic does not mean that particularly strong winds blow in this area. The balance between the rotating pair of forces of the mean wind field and the resulting currents is formed over the area of the entire ocean. In addition, currents accumulate a huge amount of energy. Therefore, a shift in the mean wind field does not automatically lead to a shift in large oceanic eddies.

Whirlpools driven by the wind are superimposed by another circulation, thermohaline ("halina" - salinity). Together, temperature and salinity determine the density of water. The ocean transports heat from tropical to polar latitudes. This transport is carried out with the participation of such large currents as the Gulf Stream, but there is also a return flow of cold water towards the tropics. It occurs mainly at depths below the layer of wind-driven whirlpools. Wind and thermohaline circulations are components of the general circulation of the ocean and interact with each other. So, if thermohaline conditions explain mainly the convective movements of water (the sinking of cold heavy water in the polar regions and its subsequent runoff to the tropics), then it is the winds that cause the divergence (divergence) of surface waters and actually “pump out” cold water back to the surface, completing the cycle .

Ideas about thermohaline circulation are less complete than about wind circulation, but some features of this process are more or less known. It is believed that education sea ice in the Weddell Sea and in the Norwegian Sea is important for the formation of cold dense water that spreads near the bottom in the South and North Atlantic. Both areas receive water of increased salinity, which cools down to freezing in winter. When water freezes, a significant part of the salts contained in it is not included in the newly formed ice. As a result, the salinity and density of the remaining unfrozen water increase. This heavy water sinks to the bottom. It is commonly referred to as Antarctic bottom water and North Atlantic deep water, respectively.

Another important feature of the thermohaline circulation is related to the density stratification of the ocean and its effect on mixing. The density of water in the ocean increases with depth and the lines of constant density are almost horizontal. Water with different characteristics is much easier to mix in the direction of lines of constant density than across them.

Thermohaline circulation is difficult to characterize with certainty. In fact, both horizontal advection (transport of water by sea currents) and diffusion must play important role in thermohaline circulation. Determining the relative importance of these two processes in any area or situation is an important task.

The main features of the surface circulation of the waters of the world ocean are determined by wind currents. It is important to note that the movement of water masses in the Atlantic and Pacific oceans is very similar. In both oceans, there are two huge anticyclonic circular currents separated by the equatorial countercurrent. In both oceans, there are, in addition, powerful western (in the northern hemisphere) boundary currents (Gulf Stream in the Atlantic and Kuroshio in the Pacific) and similar in nature, but weaker eastern currents (in the southern hemisphere) - Brazilian and East Australian. Along their western coasts, cold currents can be traced - Oyashio in the Pacific Ocean, Labrador and Greenland currents in the North Atlantic. In addition, a smaller-scale cyclonic gyre has been found in the eastern part of each basin north of the main gyre.

Some of the differences between the oceans are due to differences in the outlines of their basins. The Atlantic, Indian and Pacific Oceans are all different shapes. But some of the differences are determined by the features of the wind field, as, for example, in the Indian Ocean. The circulation in the southern part of the Indian Ocean is basically similar to the circulation in the southern basins of the Atlantic and Pacific oceans. But in the northern part of the Indian Ocean, it is clearly subject to monsoon winds, where during the summer and winter monsoons the circulation pattern changes completely.

For a number of reasons, as one approaches the coast, deviations from the general circulation pattern become more and more significant. As a result of the interaction of the main climatic characteristics of the currents with the same characteristics of the coasts, stable or quasi-stable eddies often arise. Noticeable deviations from the average circulation pattern can also cause local winds near the coasts. In some areas, the disturbing factors of the circulation regime are river runoff and tides.

In the central regions of the oceans, the average characteristics of the currents are calculated from a small amount of accurate data and are therefore especially unreliable.

Western Boundary Currents - Gulf Stream and Kuroshio

It is known that the western boundary currents in the northern hemisphere (Gulf Stream and Kuroshio) are better developed than their counterparts in the southern hemisphere.

If the Gulf Stream is considered part of a circular anticyclonic eddy, then it is hardly possible to accurately determine its beginning and end. It is known that between Mexico and Cuba, a strong current rushes through the Yucatan Strait, which usually describes a loop in the Gulf of Mexico and only then exits into the ocean from the Florida Strait. For about 1200 km, from Key West in Florida to Cape Hatteras in North Carolina, the Gulf Stream stubbornly follows the coast of America, only occasionally slightly deviating from it. However, having passed the Hatteras, the Gulf Stream, as it were, begins to scour. South of the Great Newfoundland Bank, it crosses the North Atlantic. On this winding section of its path, the Gulf Stream forms huge undulating meanders. One of them was found at 45 degrees. west, about 2500 km from Cape Hatteras. Somewhere along the path between the southeastern edge of the Newfoundland Rise and the Mid-Atlantic Ridge, the Gulf Stream ceases to be traced as a single current.

The width of the Gulf Stream on the surface ranges from 125 to 175 km. The left, if you look downstream, edge of the Gulf Stream is easy to detect by the horizontal temperature gradient, which becomes noticeable starting from a depth of several tens of meters, and countercurrent. It is difficult to detect the right edge by temperature, but quite a noticeable countercurrent is often noted there. The speed of the Gulf Stream on the surface can reach 250 cm/s, i.e. exceed 5 knots.

Thinking in general terms about the circulation of oceanic waters as a system of extensive anticyclonic eddies, it should be noted that the currents, which together form the gyres, are very different in their different parts. The western border currents, such as the Gulf Stream and the Kuroshio, are narrow, fast, deep streams with fairly well-defined boundaries. Currents directed to the equator on the other side of the ocean basins, such as the California, Peru and Bengal, on the contrary, are wide, weak and shallow flows with vague boundaries, some researchers even believe that it makes sense to draw these boundaries on the seaward side of currents of this type.

The California current is considered the most studied of them. The depth of this flow is limited mainly by the upper 500-meter layer. It consists of a series of large eddies superimposed on a weak but wide flow of water directed towards the equator. The speeds and directions of water movement measured in the California Current zone at any given moment may be completely different from the average values. The same picture, apparently, is characteristic of other eastern boundary currents.

The coastal flow of water is usually very complex, and when describing it, it is often distinguished from the wider system of alongshore currents, assigning it a different name.

In the zone of many eastern boundary currents, upwelling is the main factor determining the distribution of temperature, salinity, and chemical characteristics of water on the surface. Upwelling is of great biological importance, because thanks to it, deep waters carry nutrients to the upper layers of the water and thus contribute to an increase in the productivity of phytoplankton. Upwelling zones are biologically the most productive areas in the world.

equatorial currents

The currents of the tropical zone are closely connected with the system of trade winds. Northeast trade winds blow in most of the Atlantic and Pacific Oceans in the northern hemisphere, and southeast trade winds play their role in the southern hemisphere. These two systems of trade winds are separated by an area of intratropical convergence characterized by weak winds of unstable directions. It is often called the equatorial calm zone. Since it separates the wind systems of the two hemispheres, it can be considered a kind of climatic equator. Usually it is located between 3 degrees. NL and 10 deg. NL

The main oceanic currents of the tropical zone, as it were, reflect the features of the wind system of these places. Thus, the North and South equatorial currents of the western direction, which form part of the main anticyclonic circulations of the currents of the northern and southern hemispheres, are "controlled" by the trade winds. Between these two wide streams there is a relatively narrow (300 - 500 km wide) Equatorial countercurrent directed to the east. Near the coasts, both the field of trade winds and the system of equatorial currents become more complicated.

The oceanic waters of the tropical zone are characterized by well-mixed warm surface layer, which is separated by a powerful thermocline from the cold water of the depths. The thermocline also serves as a kind of barrier between oxygen-rich, but poor in phosphate and nitrate, surface waters and deep waters with low oxygen content and relatively high nutrient content. Equatorial currents are confined mainly to the thermocline region. This equatorial subsurface current in the Pacific Ocean is commonly referred to as the Cromwell current. Resembling in the vastness of the ocean a ribbon only 200 m thick and 300 km wide, it moves at a speed of up to 150 cm per second. The current core usually coincides with the thermocline and is located at or near the equator. Sometimes it rises to the surface, but this rarely happens.

Circulation of polar waters

The circulation of the waters of the World Ocean in the polar regions of the northern and southern hemispheres is completely different. The Arctic Ocean is hidden under the cover of drifting ice. Existing information about the currents in the Arctic Ocean indicates the presence of a slow transfer of water in a counterclockwise direction. The free mixing of the deep cold waters of the Arctic with the deep waters of the Atlantic and Pacific oceans is hindered by two fairly shallow sills between the continents. The depth of the shallow threshold in the Bering Strait, which separates Chukotka and Alaska, does not even reach 100 m, but it strongly impedes water exchange between the Atlantic and Pacific Oceans through the Arctic Ocean.

Things look different in the southern hemisphere. The wide (300 miles) and deep (3000 m) Drake Passage - between South America and Antarctica - provides unhindered water exchange between the Atlantic and Pacific oceans. Due to this, the Antarctic Circumpolar Current, directed to the east, extends to the bottom and, with the calculated amount of water discharge, turns out to be the greatest current in the World Ocean.

The Antarctic Circumpolar Current is driven by prevailing westerly winds, and its average speed and water flow are determined by the balance between the tangential wind force on the surface and the friction force on the bottom. It has been established that the current deviates to the south over the bottom depressions, and to the north over the uplifts, which indicates the undoubted influence of the bottom topography on the direction of this current.

The most well-pronounced advective water flows in the deep-sea region of the oceans are noted along the western boundaries of the basins.

Waves and tides

Waves are regular and have some common characteristics - length, amplitude and period. The speed of wave propagation is also noted.

The wavelength is the distance between the peaks or bottoms of the waves, the height of the wave is the vertical distance from the bottom to the top, it is equal to twice the amplitude, the period is equal to the time between the moments of the passage of two successive tops (or bottoms) through the same point.

The height of the ripple is measured in about a centimeter, and the period is about one second or less. Surf waves reach several meters in height at periods of 4 to 12 s.

Ocean waves have different outlines and shapes.

Waves caused by local wind are called wind waves. Another type of waves are swells, which slowly rock the ship even in calm weather. Swells form waves that persist after they leave the wind area.

At any wind speed, a certain equilibrium state is reached, which is expressed in the phenomenon of fully developed waves, when the energy transmitted by the wind to the waves equals the energy transmitted by the wind to the waves, equals the energy lost during the destruction of the waves. But in order to form a fully developed wave, the wind must blow for a long time and over a large area. The space exposed to the wind is called the fetch region.

Tsunami

Tsunamis propagate in waves from the epicenter of underwater earthquakes. The area affected by tsunami waves is huge.

Tsunamis are directly related to the movements of the earth's crust. A shallow-focus earthquake, which causes significant displacements of the crust at the bottom of the oceans, will also cause a tsunami. But an equally strong earthquake, not accompanied by any noticeable movements of the crust, will not cause a tsunami.

A tsunami occurs as a single impulse, the leading edge of which propagates at the speed of a shallow wave. The initial impulse does not always ensure the concentric propagation of energy, and with it the waves.

tides

Tides are the slow rise and fall of the water level and the movement of its edge. Tidal forces are the result of the attraction of the Sun and Moon. When the Sun and Moon are approximately in line with the Earth, that is, during the periods of the full moon and new moon, the tides are greatest. Because the planes of revolution of the sun and moon are not parallel, the action of the forces of the moon and the sun changes with the seasons, and also depending on the phase of the moon. The tidal force of the Moon is about twice that of the Sun. Large differences in the amplitude of the tides in different parts of the coast are determined mainly by the shape of the ocean basins.

Bibliographic list

Big series of knowledge. Planet Earth/Comp. A.M. Berlyant. - M .: LLC "TD" Publishing House "World of Books", 2006. Publishing House "Modern Pedagogy", 2006. - 128 pp.: ill.

FEDERAL AGENCY FOR EDUCATION

STATE EDUCATIONAL INSTITUTION OF HIGHER PROFESSIONAL EDUCATION "SHUI STATE PEDAGOGICAL UNIVERSITY"

Department of Geography and Teaching Methods

MOVEMENT OF WATERS OF THE WORLD OCEAN

The work was completed by: Ermakov Dmitry Yuryevich, student of the 2nd year of the 1st group of the day department of the Faculty of Natural Geography Specialty -050102.65 Biology with an additional specialty 050103.65 Geography

Supervisor: Associate Professor of Geographical Sciences, Senior Lecturer Markov Dmitry Sergeevich

ocean

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Pollution problem world ocean (2)
Abstract >> Ecology
The natural processes that take place in world ocean - motion, temperature regime waters- are inexhaustible energy ... as a result of the cycle water all in nature water World ocean is being updated. Chapter II. Pollution World ocean like a global...
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Abstract >> Customs system
... world ocean; 2. oil pollution world ocean: - oil and oil products; - liability for oil spills; 3. Pollution control waters world ocean...) islands, harbors, lagoons and estuaries. Motion water depends on the ebb and flow, complex ...

The world ocean is the main part of the hydrosphere, which is characterized by certain features of the biological, salt and temperature composition.

The main characteristic of the World Ocean, as a component of the hydrosphere, is the constant movement and mixing of waters. Water moves not only on the surface of the ocean, but also at depth, even in its bottom layers. The dynamics of water can be observed throughout its thickness in the vertical and horizontal directions. These processes strongly support the regular mixing of the water mass, the redistribution of salts, gases and heat, which makes it possible to maintain a constant gas, temperature, salt and chemical composition. The types of movement of water mass in the oceans are:

convective currents;
swell and waves;
tides and currents;
spontaneous waves.

Waves are a phenomenon that is formed due to the action of external forces of a different nature (earthquakes, the Moon, wind or the Sun) and they are periodic oscillations of water particles. The main reason why waves are formed is wind processes. Even a small wind speed, which is equal to 0.2 - 0.3 m / s, with air friction on the surface, can cause a system of small uniform waves, which are called ripples. Most often, it appears during simultaneous wind gusts and immediately disappears after the wind processes calm down. At a wind speed of 1 m/s or more, wind waves begin to form.

The excitement of the waters in the World Ocean begins to form not only from the impact of wind processes on them, but also from a sharp change in pressure in the atmosphere, from tide-forming forces, various natural processes - volcanic eruptions, earthquakes. Boats, ferries, yachts, ships and other navigable vehicles, during their movement, cutting through the surface of the water create waves, which are called ship waves.

Waves that are formed only from the influence of external forces that cause them are called forced, and waves that continue to exist for a certain period of time after the cessation of the force that caused them are called free. Waves that form on the water surface and in the upper layers of the water mass are called surface waves, and waves that occur at a depth of more than 200 m and are visually imperceptible on the water surface are called internal waves.

The size and strength of wind waves depend on what the wind speed is, as well as on the depth and size of the water mass that is covered by the wind process. The height of the wave, from its beginning to the very crest, most often does not exceed 5 meters. It is very rare to find waves with a height of 7 - 12 meters or more. The largest wind waves are formed on the territory of the southern hemisphere of the Earth, since in this part of the planet the ocean has no interruptions due to the absence of large land areas. Waves in this region sometimes reach a height of 25 meters, and they stretch for several hundred meters in length. Waves in inland seas are much smaller, for example, in the Black Sea, the highest recorded wave height was 12 meters, and in the Sea of \u200b\u200bAzov this figure is generally 4 meters.

After the cessation of wind activity in the ocean, gentle long waves begin to form, called swell. Swell is the most undistorted, ideal waveform. Since swell is a free wave, such waves propagate much faster when compared with other types of waves. Wavelengths during swells can spread over a couple of hundred meters, and if we take into account their small height, then the wave processes of swells on the surface of the oceans remain almost invisible.

However, because the waves travel at such high speeds, they often hit the coast hundreds and sometimes even thousands of kilometers from where they originated. The movement of the water mass with depth abruptly stops. at a depth that is equal to the wavelength, the waves are almost completely attenuated.

Given that the length of wind waves in most cases is insignificant, then even during the most active waves, at a depth of more than 50 meters, these waves are almost not felt. Therefore, the strength of the waves directly depends on their length, height and how wide the crest is. However, the main role still belongs to the height of the wave.

Due to the variability of the aquatic environment, as well as systematic dynamics and mixing, the water layers in the World Ocean have different levels of density, salt composition, movement speed and viscosity. One of the most striking examples are areas in the world's oceans in which such a phenomenon as the melting of icebergs is observed, as well as in places where precipitation is intense. In these cases, the water layer of the World Ocean begins to be covered fresh water, creating favorable conditions for the creation of the so-called. internal wave that passes through the watershed of salt and fresh water masses.

Based on oceanographic research, scientists have found that in the open ocean, internal waves can be encountered with the same regularity as surface waves. Quite often, internal waves are caused by changes in pressure in the atmosphere, earthquakes, wind speed, tides, and some other factors. Internal waves are characterized by a significant amplitude, however, a low propagation velocity. In height, internal waves usually reach up to 30 meters, in rare cases, the height can reach up to 200 meters. Such waves sometimes occur near the Strait of Gibraltar in Southern Europe.

Currents in the oceans

Sea currents are the most important form of movement of the World Ocean. A current is a relatively regular, constant and periodic surface and deep movement of water masses in the World Ocean in a horizontal direction.

Such movements of the water mass are very important both for the life of the World Ocean itself and for its inhabitants. These processes are accompanied by:

full exchange of waters in the World Ocean;
transfer of masses of ice;
creation of special climate conditions;
perform a relief-forming function;
create favorable living conditions for the functioning of the biological resources of the ocean.

A large number of currents in the oceans can be divided into groups:

on sustainability;
by origin;
by the nature of the movement;
by depth of location;
by physical and chemical composition.

According to the stability of the flow are divided into temporary, periodic and permanent.

Constant currents are those that are always in the same region of the ocean and almost never change their direction and speed. An example is the Gulf Stream, trade winds and others. Periodic is a flow that can change speed and direction based on the changes that provoked their causes. Temporary are those currents that are formed due to causes of a random nature (wind).

According to the depth, the currents are divided into near-bottom, deep and surface.

By the nature of the movement - into curvilinear, rectilinear and meandering. According to the physico-chemical composition - into freshened, salty, neutral, cold and warm. The nature of the currents is formed on the ratio of temperature indicators or water salinity, which form the current. Provided that the flow temperature is higher than the temperature of the surrounding water mass, then such a flow is warm, if lower - warm. By the same principle, freshened and salty currents are determined.

By origin, the currents are divided into: tidal, gradient and frictional.

The latter are formed due to the impact of wind forces on the water masses. Friction currents that appear from the influence of temporary winds are called wind currents, and those that appear from the influence of prevailing winds are called drift currents. Gradient currents are divided into: compensation, density, waste, runoff and barogradient. Runoff currents are formed due to the tilt of the sea level, provoked by the inflow of fresh water from rivers into the oceans, large precipitation from the atmosphere, or their large-scale evaporation. Waste currents are formed due to the tilt of the sea level, which occurs due to the inflow of water from other parts of the sea during the action of some external force.

Currents cause a decrease in the volume of water in one part of the oceans, causing at the same time an increase in another part of it. The difference in levels between different parts of the ocean immediately activates the neighboring parts, which take an active part in eliminating this difference. So, there are compensatory currents. They are currents of a secondary nature and compensate for the outflow of water.

Currents, which are called tidal currents, appear due to the tidal force. The highest speed of such currents appears in narrow straits and sometimes it can reach 22 km / h, but within the open ocean it rarely exceeds the speed of 1 km / h. In the ocean, it is very rare to observe a current that is due to only one of the above processes or factors.

Tidal and seismic waves

tidal waves

Tidal waves are called phenomena arising from the influence of the forces of attraction of the Sun and the Moon and causing periodic characteristic fluctuations in the level of water masses in the oceans. Tidal activity begins to form from the influence of the Moon and the Sun, but, due to the greater remoteness of the Sun, the tides provoked by it do not happen as often as because of the Moon (there are half of them). The main influence on tidal activity is the islands and the outlines of the coastline. This reason can explain how the oscillations of the World Ocean during tides at the same latitude change over a wider range. Near the islands, the tides are not at all significant, but in open waters, the water rises to 1 meter. Tides can reach much higher values in bays with winding coasts, straits and river mouths.

seismic waves

The reason why seismic waves (tsunamis) begin to form is a change in the relief on the seabed, which occurs due to the movement of lithospheric plates, as a result of which uplifts, dips, landslides or earthquakes can appear. It should be emphasized that the mechanism by which seismic waves are generated is directly dependent on the nature of the processes that transform the relief on the ocean floor. For example, during the formation of a tsunami in the waters of the open ocean, when a crack or dip appears on the bottom, water immediately tends to get into the center of the depression that has appeared, first filling it, and then overflowing, forming a giant water column on the surface of the oceans.

Before the process of tsunami formation and their collapse on the coastline begins, a serious drop in the water level usually precedes. In just a couple of minutes, the water begins to recede from the coast for several hundred meters, and in rare cases for kilometers, after which a tsunami begins to collapse on the coastline. Immediately after the first, largest and most destructive wave, another 2-5 small waves come.

The speed of movement of tsunami waves is very high and can reach 150 - 900 km/h. When they hit cities and towns located on the coastline in the zone of their impact, they can cause serious damage and can take lives. One of the most devastating tsunamis occurred in 2004 in the Indian Ocean, killing more than 200,000 people and causing billions of dollars in damage.

Nowadays, the appearance of a tsunami can be predicted with the highest possible accuracy factor. These forecasts are based on observations and control of seismic activity under the water masses of the World Ocean. Typically, forecasts are made based on observations such as:

acoustic observation;
monitoring with tide gauges;
seismic monitoring.

These methods make it possible to develop and take certain measures that are aimed at ensuring security.

The movement of water in the ocean is brief. The movement of water in the ocean - sea waves, tsunamis, ebbs and flows. Warm and cold currents

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Currents in the oceans

According to the stability of the flow are divided into temporary, periodic and permanent.

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Tidal and seismic waves

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The movement of water in the ocean is brief. The movement of water in the ocean - sea waves, tsunamis, ebbs and flows. Warm and cold currents

Currents of the oceans

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geography The movement of water in the ocean

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By origin, the currents are divided into: tidal, gradient and frictional.

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tidal waves

seismic waves

sea currents

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