Drawing of the earth's atmosphere. Layers of the atmosphere - troposphere, stratosphere, mesosphere, thermosphere and exosphere
The role of the atmosphere in the life of the Earth
The atmosphere is the source of oxygen that people breathe. However, as you ascend to altitude, the total atmospheric pressure drops, resulting in a decrease in partial oxygen pressure.
The human lungs contain approximately three liters of alveolar air. If the atmospheric pressure is normal, then the partial oxygen pressure in the alveolar air will be 11 mm Hg. Art., pressure of carbon dioxide - 40 mm Hg. Art., and water vapor - 47 mm Hg. Art. With an increase in altitude, oxygen pressure decreases, and the pressure of water vapor and carbon dioxide in the lungs in total will remain constant - approximately 87 mm Hg. Art. When the air pressure equals this value, oxygen will stop flowing into the lungs.
Due to the decrease in atmospheric pressure at an altitude of 20 km, water and interstitial body fluid in the human body will boil here. If you do not use a pressurized cabin, at such a height a person will die almost instantly. Therefore, from the point of view physiological features human body, "cosmos" originates from a height of 20 km above sea level.
The role of the atmosphere in the life of the Earth is very great. So, for example, thanks to dense air layers - the troposphere and stratosphere, people are protected from radiation exposure. In space, in rarefied air, at an altitude of over 36 km, ionizing radiation acts. At an altitude of over 40 km - ultraviolet.
When rising above the Earth's surface to a height of over 90-100 km, there will be a gradual weakening, and then the complete disappearance of phenomena familiar to humans, observed in the lower atmospheric layer:
Sound does not propagate.
There is no aerodynamic force and drag.
Heat is not transferred by convection, etc.
The atmospheric layer protects the Earth and all living organisms from cosmic radiation, from meteorites, is responsible for regulating seasonal temperature fluctuations, balancing and equalizing daily ones. In the absence of an atmosphere on Earth, the daily temperature would fluctuate within +/-200С˚. The atmospheric layer is a life-giving "buffer" between the earth's surface and outer space, a carrier of moisture and heat; processes of photosynthesis and energy exchange take place in the atmosphere - the most important biospheric processes.
Layers of the atmosphere in order from the Earth's surface
The atmosphere is a layered structure, which is the following layers of the atmosphere in order from the surface of the Earth:
Troposphere.
Stratosphere.
Mesosphere.
Thermosphere.
Exosphere
Each layer does not have sharp boundaries between them, and their height is affected by latitude and seasons. This layered structure was formed as a result of temperature changes at different heights. It is thanks to the atmosphere that we see twinkling stars.
The structure of the Earth's atmosphere by layers:
What is the earth's atmosphere made of?
Each atmospheric layer differs in temperature, density and composition. The total thickness of the atmosphere is 1.5-2.0 thousand km. What is the earth's atmosphere made of? At present, it is a mixture of gases with various impurities.
Troposphere
The structure of the Earth's atmosphere begins with the troposphere, which is the lower part of the atmosphere about 10-15 km high. Here is the main part atmospheric air. Feature troposphere - a drop in temperature of 0.6 ˚C as you rise up for every 100 meters. The troposphere has concentrated in itself almost all atmospheric water vapor, and clouds are also formed here.
The height of the troposphere changes daily. In addition, her average value varies with latitude and season. The average height of the troposphere above the poles is 9 km, above the equator - about 17 km. The average annual air temperature over the equator is close to +26 ˚C, and over the North Pole -23 ˚C. The upper line of the boundary of the troposphere above the equator is the average annual temperature of about -70 ˚C, and above north pole in summer -45 ˚C and in winter -65 ˚C. Thus, the higher the altitude, the lower the temperature. The rays of the sun pass freely through the troposphere, heating the surface of the Earth. The heat radiated by the sun is retained by carbon dioxide, methane and water vapor.
Stratosphere
Above the layer of the troposphere is the stratosphere, which is 50-55 km in height. The peculiarity of this layer is the increase in temperature with height. Between the troposphere and stratosphere lies a transitional layer called the tropopause.
Approximately from a height of 25 kilometers, the temperature of the stratospheric layer begins to increase and, upon reaching a maximum height of 50 km, it acquires values from +10 to +30 ˚C.
There is very little water vapor in the stratosphere. Sometimes at an altitude of about 25 km you can find quite thin clouds, which are called "mother-of-pearl". In the daytime, they are not noticeable, but at night they glow due to the illumination of the sun, which is below the horizon. The composition of mother-of-pearl clouds is supercooled water droplets. The stratosphere is made up mostly of ozone.
Mesosphere
The height of the mesosphere layer is approximately 80 km. Here, as it rises upwards, the temperature decreases and at the uppermost boundary it reaches values several tens of C˚ below zero. In the mesosphere, clouds can also be observed, which are presumably formed from ice crystals. These clouds are called "silvery". The mesosphere is characterized by the coldest temperature in the atmosphere: from -2 to -138 ˚C.
Thermosphere
This atmospheric layer got its name from high temperatures. The thermosphere is made up of:
Ionosphere.
exospheres.
The ionosphere is characterized by rarefied air, each centimeter of which at an altitude of 300 km consists of 1 billion atoms and molecules, and at an altitude of 600 km - more than 100 million.
The ionosphere is also characterized by high air ionization. These ions are composed of charged oxygen atoms, charged molecules of nitrogen atoms and free electrons.
Exosphere
From a height of 800-1000 km, the exospheric layer begins. Gas particles, especially light ones, move here at great speed, overcoming the force of gravity. Such particles, due to their rapid movement, fly out of the atmosphere into outer space and disperse. Therefore, the exosphere is called the sphere of scattering. It is predominantly hydrogen atoms that fly into space, which make up the highest layers of the exosphere. Thanks to particles in the upper atmosphere and particles of the solar wind, we can observe the northern lights.
Satellites and geophysical rockets made it possible to establish the presence in the upper atmosphere of the planet's radiation belt, which consists of electrically charged particles - electrons and protons.
The surrounding world is formed from three very different parts: land, water and air. Each of them is unique and interesting in its own way. Now we will talk only about the last of them. What is atmosphere? How did it come about? What is it made of and what parts is it divided into? All these questions are extremely interesting.
The very name "atmosphere" is formed from two words of Greek origin, translated into Russian they mean "steam" and "ball". And if you look at the exact definition, you can read the following: "The atmosphere is the air shell of the planet Earth, which rushes along with it in outer space." It developed in parallel with the geological and geochemical processes that took place on the planet. And today all the processes occurring in living organisms depend on it. Without an atmosphere, the planet would become a lifeless desert like the moon.
What does it consist of?
The question of what is the atmosphere and what elements are included in it has interested people for a long time. The main components of this shell were already known in 1774. They were installed by Antoine Lavoisier. He discovered that the composition of the atmosphere for the most part formed from nitrogen and oxygen. Over time, its components have been refined. And now we know that it contains many more gases, as well as water and dust.
Let us consider in more detail what the Earth's atmosphere near its surface consists of. The most common gas is nitrogen. It contains a little more than 78 percent. But, despite such a large amount, nitrogen in the air is practically not active.
The next largest and most important element is oxygen. This gas contains almost 21%, and it just shows very high activity. Its specific function is to oxidize dead organic matter, which decomposes as a result of this reaction.
Low but important gases
The third gas that is part of the atmosphere is argon. Its slightly less than one percent. It is followed by carbon dioxide with neon, helium with methane, krypton with hydrogen, xenon, ozone and even ammonia. But they are contained so little that the percentage of such components is equal to hundredths, thousandths and millionths. Of these, only carbon dioxide plays essential role, since it is a building material that plants need for photosynthesis. Its other important function is to keep out radiation and absorb part of the sun's heat.
Another rare but important gas, ozone, exists to trap ultraviolet radiation coming from the sun. Thanks to this property, all life on the planet is reliably protected. On the other hand, ozone affects the temperature of the stratosphere. Due to the fact that it absorbs this radiation, the air is heated.
permanence quantitative composition atmosphere is maintained by constant mixing. Its layers move both horizontally and vertically. So anywhere the globe enough oxygen and no excess carbon dioxide.
What else is in the air?
It should be noted that in airspace steam and dust can be detected. The latter consists of pollen and soil particles, in the city they are joined by impurities of particulate emissions from exhaust gases.
But there is a lot of water in the atmosphere. Under certain conditions, it condenses, and clouds and fog appear. In fact, this is the same thing, only the first ones appear high above the surface of the Earth, and the last one spreads along it. Clouds take on a variety of shapes. This process depends on the height above the Earth.
If they formed 2 km above land, then they are called layered. It is from them that rain falls on the ground or snow falls. Cumulus clouds form above them up to a height of 8 km. They are always the most beautiful and picturesque. It is they who are examined and wondered what they look like. If such formations appear in the next 10 km, they will be very light and airy. Their name is cirrus.
What are the layers of the atmosphere?
Although they have very different temperatures from each other, it is very difficult to say at what particular height one layer begins and another ends. This division is very conditional and is approximate. However, the layers of the atmosphere still exist and perform their functions.
The lowest part of the air shell is called the troposphere. Its thickness increases when moving from the poles to the equator from 8 to 18 km. This is the warmest part of the atmosphere, because the air in it is heated from earth's surface. Most of the water vapor is concentrated in the troposphere, so clouds form in it, precipitation falls, thunderstorms rumble and winds blow.
The next layer is about 40 km thick and is called the stratosphere. If the observer moves to this part of the air, he will find that the sky has become purple. This is due to the low density of the substance, which practically does not scatter the sun's rays. It is in this layer that they fly jet aircraft. For them, all open spaces are open there, since there are practically no clouds. Inside the stratosphere there is a layer consisting of a large amount of ozone.
It is followed by the stratopause and the mesosphere. The latter has a thickness of about 30 km. It is characterized by a sharp decrease in air density and temperature. The sky appears black to the observer. Here you can even watch the stars during the day.
Layers with little to no air
The structure of the atmosphere continues with a layer called the thermosphere - the longest of all the others, its thickness reaches 400 km. This layer is characterized by a huge temperature, which can reach 1700 ° C.
The last two spheres are often combined into one and called it the ionosphere. This is due to the fact that reactions occur in them with the release of ions. It is these layers that allow you to observe such a natural phenomenon as the northern lights.
The next 50 km from the Earth are reserved for the exosphere. This is the outer shell of the atmosphere. In it, air particles are scattered into space. Weather satellites usually move in this layer.
The Earth's atmosphere ends with a magnetosphere. It was she who sheltered most artificial satellites planets.
After all that has been said, there should be no question about what the atmosphere is. If there are doubts about its necessity, then it is easy to dispel them.
The value of the atmosphere
The main function of the atmosphere is to protect the surface of the planet from overheating during the day and excessive cooling at night. The next importance of this shell, which no one will dispute, is to supply oxygen to all living beings. Without it, they would suffocate.
Most meteorites burn up in the upper layers, never reaching the Earth's surface. And people can admire the flying lights, mistaking them for shooting stars. Without an atmosphere, the entire Earth would be littered with craters. And about protection from solar radiation has already been mentioned above.
How does a person affect the atmosphere?
Very negative. This is due to the growing activity of people. The main share of all the negative aspects falls on industry and transport. By the way, it is cars that emit almost 60% of all pollutants that penetrate the atmosphere. The remaining forty are divided between energy and industry, as well as industries for the destruction of waste.
The list of harmful substances that replenish the composition of the air every day is very long. Because of the transport in the atmosphere are: nitrogen and sulfur, carbon, blue and soot, as well as a strong carcinogen that causes skin cancer - benzopyrene.
The industry accounts for chemical elements: sulfur dioxide, hydrocarbon and hydrogen sulfide, ammonia and phenol, chlorine and fluorine. If the process continues, then soon the answers to the questions: “What is the atmosphere? What does it consist of? will be completely different.
The atmosphere is one of the most important components of our planet. It is she who "shelters" people from the harsh conditions of outer space, such as solar radiation and space debris. However, many facts about the atmosphere are unknown to most people.
1. The true color of the sky
Although it's hard to believe, the sky is actually purple. When light enters the atmosphere, air and water particles absorb the light, scattering it. At the same time, the most scattered purple That's why people see blue skies.
2. An exclusive element in the Earth's atmosphere
As many remember from school, the Earth's atmosphere consists of approximately 78% nitrogen, 21% oxygen, and small impurities of argon, carbon dioxide and other gases. But few people know that our atmosphere is the only one so far discovered by scientists (besides comet 67P) that has free oxygen. Because oxygen is a highly reactive gas, it often reacts with other chemicals in space. Its pure form on Earth makes the planet habitable.
3. White stripe in the sky
Surely, some sometimes wondered why a white stripe remains in the sky behind a jet plane. These white trails, known as contrails, form when hot, moist exhaust gases from an aircraft engine mix with colder outside air. Water vapor from exhaust gases freezes and becomes visible.
4. The main layers of the atmosphere
The atmosphere of the Earth consists of five main layers, which make life possible on the planet. The first of these, the troposphere, extends from sea level to an altitude of about 17 km to the equator. Most of the weather events occur in it.
5. Ozone layer
The next layer of the atmosphere, the stratosphere, reaches a height of about 50 km at the equator. It contains the ozone layer, which protects people from dangerous ultraviolet rays. Even though this layer is above the troposphere, it may actually be warmer due to the energy it absorbs from the sun's rays. Most jet planes and weather balloons fly in the stratosphere. Planes can fly faster in it because they are less affected by gravity and friction. Weather balloons can get a better idea of storms, most of which occur lower in the troposphere.6. Mesosphere
The mesosphere is the middle layer, extending to a height of 85 km above the surface of the planet. Its temperature fluctuates around -120°C. Most of the meteors that enter the Earth's atmosphere burn up in the mesosphere. The last two layers that pass into space are the thermosphere and the exosphere.
7. The disappearance of the atmosphere
The Earth has most likely lost its atmosphere several times. When the planet was covered in oceans of magma, massive interstellar objects crashed into it. These impacts, which also formed the Moon, may have formed the planet's atmosphere for the first time.
8. If there were no atmospheric gases...
Without various gases in the atmosphere, the Earth would be too cold for human existence. Water vapor, carbon dioxide, and other atmospheric gases absorb heat from the sun and "distribute" it over the planet's surface, helping to create a habitable climate.
9. Formation of the ozone layer
The notorious (and importantly necessary) ozone layer was created when oxygen atoms reacted with ultraviolet light from the sun to form ozone. It is ozone that absorbs most of the harmful radiation from the sun. Despite its importance, the ozone layer was formed relatively recently after enough life arose in the oceans to release into the atmosphere the amount of oxygen needed to create a minimum concentration of ozone.
10. Ionosphere
The ionosphere is so named because high-energy particles from space and from the sun help form ions, creating an "electric layer" around the planet. When there were no satellites, this layer helped reflect radio waves.
11. Acid rain
Acid rain, which destroys entire forests and devastates aquatic ecosystems, forms in the atmosphere when sulfur dioxide or nitrogen oxide particles mix with water vapor and fall to the ground as rain. These chemical compounds are also found in nature: sulfur dioxide is produced during volcanic eruptions, and nitric oxide - during lightning strikes.
12. Lightning Power
Lightning is so powerful that just a single discharge can heat the surrounding air up to 30,000 °C. The rapid heating causes an explosive expansion of the nearby air, which is heard in the form of a sound wave called thunder.
Aurora Borealis and Aurora Australis (Northern and Southern Aurora) are caused by ion reactions taking place in the fourth level of the atmosphere, the thermosphere. When highly charged solar wind particles collide with air molecules over the planet's magnetic poles, they glow and create magnificent light shows.
14. Sunsets
Sunsets often look like a burning sky as small atmospheric particles scatter light, reflecting it in orange and yellow hues. The same principle underlies the formation of rainbows.
In 2013, scientists discovered that tiny microbes can survive many kilometers above the Earth's surface. At an altitude of 8-15 km above the planet, microbes were found that destroy organic chemical substances, which float in the atmosphere, "feeding" on them.
Adherents of the theory of the apocalypse and various other horror stories will be interested to learn about.
The atmosphere is the gaseous shell of our planet that rotates with the Earth. The gas in the atmosphere is called air. The atmosphere is in contact with the hydrosphere and partially covers the lithosphere. But it is difficult to determine the upper bounds. Conventionally, it is assumed that the atmosphere extends upwards for about three thousand kilometers. There it flows smoothly into the airless space.
The chemical composition of the Earth's atmosphere
Formation chemical composition atmosphere began about four billion years ago. Initially, the atmosphere consisted only of light gases - helium and hydrogen. According to scientists, the initial prerequisites for the creation of a gas shell around the Earth were volcanic eruptions, which, together with lava, threw out great amount gases. Subsequently, gas exchange began with water spaces, with living organisms, with the products of their activity. The composition of the air gradually changed and in its present form was fixed several million years ago.
The main components of the atmosphere are nitrogen (about 79%) and oxygen (20%). The remaining percentage (1%) is accounted for by the following gases: argon, neon, helium, methane, carbon dioxide, hydrogen, krypton, xenon, ozone, ammonia, sulfur dioxide and nitrogen, nitrous oxide and carbon monoxide, included in this one percent.
In addition, the air contains water vapor and particulate matter (plant pollen, dust, salt crystals, aerosol impurities).
AT recent times scientists note not a qualitative, but a quantitative change in some air ingredients. And the reason for this is the person and his activity. Only in the last 100 years, the content of carbon dioxide has increased significantly! This is fraught with many problems, the most global of which is climate change.
Formation of weather and climate
The atmosphere is playing essential role in the formation of climate and weather on Earth. A lot depends on the amount of sunlight, on the nature of the underlying surface and atmospheric circulation.
Let's look at the factors in order.
1. The atmosphere transmits the heat of the sun's rays and absorbs harmful radiation. The ancient Greeks knew that the rays of the Sun fall on different parts of the Earth at different angles. The very word "climate" in translation from ancient Greek means "slope". So, at the equator, the sun's rays fall almost vertically, because it is very hot here. The closer to the poles, the greater the angle of inclination. And the temperature is dropping.
2. Due to the uneven heating of the Earth, air currents are formed in the atmosphere. They are classified according to their size. The smallest (tens and hundreds of meters) are local winds. This is followed by monsoons and trade winds, cyclones and anticyclones, planetary frontal zones.
All these air masses are constantly moving. Some of them are quite static. For example, the trade winds that blow from the subtropics towards the equator. The movement of others is largely dependent on atmospheric pressure.
3. Atmospheric pressure is another factor influencing climate formation. This is the air pressure on the earth's surface. As you know, air masses move from an area with high atmospheric pressure towards an area where this pressure is lower.
There are 7 zones in total. The equator is a low pressure zone. Further, on both sides of the equator up to the thirtieth latitudes - the region high pressure. From 30° to 60° - again low pressure. And from 60° to the poles - a zone of high pressure. Air masses circulate between these zones. Those that go from the sea to land bring rain and bad weather, and those that blow from the continents bring clear and dry weather. In places where air currents collide, atmospheric front zones are formed, which are characterized by precipitation and inclement, windy weather.
Scientists have proven that even a person's well-being depends on atmospheric pressure. According to international standards, normal atmospheric pressure is 760 mm Hg. column at 0°C. This figure is calculated for those areas of land that are almost flush with sea level. The pressure decreases with altitude. Therefore, for example, for St. Petersburg 760 mm Hg. - is the norm. But for Moscow, which is located higher, the normal pressure is 748 mm Hg.
The pressure changes not only vertically, but also horizontally. This is especially felt during the passage of cyclones.
The structure of the atmosphere
The atmosphere is like a layer cake. And each layer has its own characteristics.
. Troposphere is the layer closest to the Earth. The "thickness" of this layer changes as you move away from the equator. Above the equator, the layer extends upwards for 16-18 km, in temperate zones - for 10-12 km, at the poles - for 8-10 km.
It is here that 80% of the total mass of air and 90% of water vapor are contained. Clouds form here, cyclones and anticyclones arise. The air temperature depends on the altitude of the area. On average, it drops by 0.65°C for every 100 meters.
. tropopause- transitional layer of the atmosphere. Its height is from several hundred meters to 1-2 km. The air temperature in summer is higher than in winter. So, for example, over the poles in winter -65 ° C. And over the equator at any time of the year it is -70 ° C.
. Stratosphere- this is a layer, the upper boundary of which runs at an altitude of 50-55 kilometers. Turbulence is low here, water vapor content in the air is negligible. But a lot of ozone. Its maximum concentration is at an altitude of 20-25 km. In the stratosphere, the air temperature begins to rise and reaches +0.8 ° C. This is due to the fact that the ozone layer interacts with ultraviolet radiation.
. Stratopause- a low intermediate layer between the stratosphere and the mesosphere following it.
. Mesosphere- the upper boundary of this layer is 80-85 kilometers. Here complex photochemical processes involving free radicals take place. It is they who provide that gentle blue glow of our planet, which is seen from space.
Most comets and meteorites burn up in the mesosphere.
. Mesopause- the next intermediate layer, the air temperature in which is at least -90 °.
. Thermosphere- the lower boundary begins at an altitude of 80 - 90 km, and the upper boundary of the layer passes approximately at the mark of 800 km. The air temperature is rising. It can vary from +500° C to +1000° C. During the day, temperature fluctuations amount to hundreds of degrees! But the air here is so rarefied that the understanding of the term "temperature" as we imagine it is not appropriate here.
. Ionosphere- unites mesosphere, mesopause and thermosphere. The air here consists mainly of oxygen and nitrogen molecules, as well as quasi-neutral plasma. The sun's rays, falling into the ionosphere, strongly ionize air molecules. In the lower layer (up to 90 km), the degree of ionization is low. The higher, the more ionization. So, at an altitude of 100-110 km, electrons are concentrated. This contributes to the reflection of short and medium radio waves.
The most important layer of the ionosphere is the upper one, which is located at an altitude of 150-400 km. Its peculiarity is that it reflects radio waves, and this contributes to the transmission of radio signals over long distances.
It is in the ionosphere that such a phenomenon as aurora occurs.
. Exosphere- consists of oxygen, helium and hydrogen atoms. The gas in this layer is very rarefied, and often hydrogen atoms escape into outer space. Therefore, this layer is called the "scattering zone".
The first scientist who suggested that our atmosphere has weight was the Italian E. Torricelli. Ostap Bender, for example, in the novel "The Golden Calf" lamented that each person was pressed by an air column weighing 14 kg! But the great strategist was a little mistaken. An adult person experiences pressure of 13-15 tons! But we do not feel this heaviness, because atmospheric pressure is balanced by the internal pressure of a person. The weight of our atmosphere is 5,300,000,000,000,000 tons. The figure is colossal, although it is only a millionth of the weight of our planet.
- the air shell of the globe that rotates with the Earth. The upper boundary of the atmosphere is conventionally carried out at altitudes of 150-200 km. The lower boundary is the surface of the Earth.
Atmospheric air is a mixture of gases. Most of its volume in the surface air layer is nitrogen (78%) and oxygen (21%). In addition, the air contains inert gases (argon, helium, neon, etc.), carbon dioxide (0.03), water vapor, and various solid particles (dust, soot, salt crystals).
The air is colorless, and the color of the sky is explained by the peculiarities of the scattering of light waves.
The atmosphere consists of several layers: troposphere, stratosphere, mesosphere and thermosphere.
The bottom layer of air is called troposphere. At different latitudes, its power is not the same. The troposphere repeats the shape of the planet and participates together with the Earth in axial rotation. At the equator, the thickness of the atmosphere varies from 10 to 20 km. At the equator it is greater, and at the poles it is less. The troposphere is characterized by the maximum density of air, 4/5 of the mass of the entire atmosphere is concentrated in it. The troposphere determines weather conditions: various air masses form here, clouds and precipitation form, and intense horizontal and vertical air movement occurs.
Above the troposphere, up to an altitude of 50 km, is located stratosphere. It is characterized by a lower density of air, there is no water vapor in it. In the lower part of the stratosphere at altitudes of about 25 km. there is an "ozone screen" - a layer of the atmosphere with a high concentration of ozone, which absorbs ultraviolet radiation, which is fatal to organisms.
At an altitude of 50 to 80-90 km extends mesosphere. As the altitude increases, the temperature decreases with an average vertical gradient of (0.25-0.3)° / 100 m, and the air density decreases. The main energy process is radiant heat transfer. The glow of the atmosphere is due to complex photochemical processes involving radicals, vibrationally excited molecules.
Thermosphere located at an altitude of 80-90 to 800 km. The air density here is minimal, the degree of air ionization is very high. The temperature changes depending on the activity of the Sun. Due to the large number of charged particles, auroras and magnetic storms are observed here.
The atmosphere has great value for the nature of the earth. Without oxygen, living organisms cannot breathe. Its ozone layer protects all living things from harmful ultraviolet rays. The atmosphere smooths out temperature fluctuations: the Earth's surface does not get supercooled at night and does not overheat during the day. In dense layers of atmospheric air, not reaching the surface of the planet, meteorites burn out from thorns.
The atmosphere interacts with all the shells of the earth. With its help, the exchange of heat and moisture between the ocean and land. Without the atmosphere there would be no clouds, precipitation, winds.
Significant adverse effect on the atmosphere economic activity person. Air pollution occurs, which leads to an increase in the concentration of carbon monoxide (CO 2). And this contributes to global warming and enhances the "greenhouse effect". Ozone layer The land is being destroyed due to industrial waste and transport.
The atmosphere needs to be protected. In developed countries, a set of measures is being taken to protect atmospheric air from pollution.
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