what layer of the atmosphere receives enough energy from the sun to break apart molecules and atoms
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- Answer is Ionosphere. The ionosphere is a layer of ionized air in the atmosphere extending from almost 80 km above the Earth's surface altitudes of 600 km and more. Technically, the ionosphere is not another atmospheric layer. [ It occupies the same region of the upper atmosphere as the thermosphere. In this region of the atmosphere the Sun's energy is so strong that it breaks apart molecules. and atoms of air, leaving ions (atoms with missing electrons) and free-floating electrons. The ionosphere is the region of the atmosphere where the aurorae occur.
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Which two layers of the atmosphere are responsible for the majority of solar radiation absorption? 2015-07-16T04:15:28-04:00. I am gonna go with B since the stratosphere has to deal with hot temp and the ozone layer radiation thus the thermosphere is the thinest layer also being the hottest layers in the atmosphere that have much solar radiation observation. Report.
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Atmosphere of the Sun: Photosphere, Chromosphere & Corona It's in these outer layers that the sun's energy, which has bubbled up from the sun's interior layers, is detected as sunlight. The lowest layer of the sun's atmosphere is the photosphere. It is about 300 miles (500 kilometers) thick. This layer is where the sun's energy is released as light.
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- Ozone forms readily in the stratosphere as incoming ultraviolet radiation breaks molecular oxygen (two atoms) into atomic oxygen (a single atom). In that process, oxygen absorbs much of the ultraviolet radiation and prevents it from reaching the Earth’s surface where we live.In the language of a simplified chemical formula, When an electrically excited free oxygen atom encounters an oxygen molecule, they may bond to form ozone.Destruction of ozone in the stratosphere takes place as quickly as formation of ozone, because the chemical is so reactive. Sunlight can readily split ozone into an oxygen molecule and an individual oxygen atom.zone forms readily in the stratosphere as incoming ultraviolet radiation breaks molecular oxygen (two atoms) into atomic oxygen (a single atom). In that process, oxygen absorbs much of the ultraviolet radiation and prevents it from reaching the Earth’s surface where we live.
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- When an electronically excited oxygen atom encounters an ozone molecule, they may combine to form two molecules of oxygen. The ozone formation-destruction process in the stratosphere occurs rapidly and constantly, maintaining an ozone layer.zone forms readily in the stratosphere as incoming ultraviolet radiation breaks molecular oxygen (two atoms) into atomic oxygen (a single atom). In that process, oxygen absorbs much of the ultraviolet radiation and prevents it from reaching the Earth’s surface where we live.
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Introduction to the Atmosphere Energy Heat Transfer. Practically all of the energy that reaches the earth comes from the sun. Intercepted first by the atmosphere, a small part is directly absorbed, particularly by certain gases such as ozone and water vapor. Some energy is also reflected back to space by clouds and the earth's surface.
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How bad is the Ozone layer depletion today? When CFCs reach the stratosphere, the ultraviolet radiation from the sun causes them to break apart and release chlorine atoms, which react with ozone, starting chemical cycles of ozone destruction that deplete the ozone layer. One chlorine atom can break apart more than 100,000 ozone molecules.bout 90% of the planet's ozone is in the ozone layer. The layer of the Earth's atmosphere that surrounds us is called the troposphere. The stratosphere, the next higher layer, extends about 10–50 kilometers above the Earth's surface.
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- Ozone forms readily in the stratosphere as incoming ultraviolet radiation breaks molecular oxygen (two atoms) into atomic oxygen (a single atom). In that process, oxygen absorbs much of the ultraviolet radiation and prevents it from reaching the Earth’s surface where we live.hen an electrically excited free oxygen atom encounters an oxygen molecule, they may bond to form ozone. Destruction of ozone in the stratosphere takes place as quickly as formation of ozone, because the chemical is so reactive. Sunlight can readily split ozone into an oxygen molecule and an individual oxygen atom.
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- Average hvac technician salaries can vary greatly due to company, location, industry, experience and benefits. This salary was calculated using the average salary for all jobs with the term hvac technician anywhere in the job listing.
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Layers of the Sun Compared to the amount of time it takes to get through the radiative zone, energy is transported very quickly through the outer convective zone. The Sun’s visible surface the photosphere is “only” about 5,800 K (10,000 degrees F). Just above the photosphere is a thin layer called the chromosphere.The name chromosphere is derived from the word chromos, the Greek word for color.It can be detected in red hydrogen-alpha light meaning that it appears bright red.he Sun’s visible surface the photosphere is “only” about 5,800 K (10,000 degrees F). Just above the photosphere is a thin layer called the chromosphere. The name chromosphere is derived from the word chromos, the Greek word for color. It can be detected in red hydrogen-alpha light meaning that it appears bright red.
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Thermosphere From Earth's surface to the top of the stratosphere (50 kilometres (31 mi)) is just under 1% of Earth's radius. The thermosphere is the layer of the Earth's atmosphere directly above the mesosphere and directly below the exosphere.ithin this layer, ultraviolet radiation causes photoionization /photodissociation of molecules present. Called from the Greek θερμός (pronounced thermos) meaning heat, the thermosphere begins about 85 kilometres (53 mi) above the Earth.
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Ozone Depletion Photograph by Stephen G. St. John. The ozone layer is a belt of naturally occurring ozone gas that sits 9.3 to 18.6 miles (15 to 30 kilometers) above Earth and serves as a shield from the harmful ultraviolet B radiation emitted by the sun.Ozone is a highly reactive molecule that contains three oxygen atoms.It is constantly being formed and broken down in the high atmosphere, 6.2 to 31 miles (10 to 50 kilometers) above Earth, in the region called the stratosphere.zone is a highly reactive molecule that contains three oxygen atoms. It is constantly being formed and broken down in the high atmosphere, 6.2 to 31 miles (10 to 50 kilometers) above Earth, in the region called the stratosphere.
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Earth's Atmosphere: Composition, Climate & Weather Atmosphere layers. Earth's atmosphere is divided into five main layers, the exosphere, the thermosphere, the mesosphere, the stratosphere and the troposphere. The atmosphere thins out in each higher layer until the gases dissipate in space.early all of the water vapor and dust in the atmosphere are in this layer and that is why clouds are found here. The stratosphere is the second layer. It starts above the troposphere and ends about 31 miles (50 km) above ground.
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- For nearly a billion years, ozone molecules in the atmosphere have protected life on Earth from the effects of ultraviolet rays. The ozone layer resides in the stratosphere and surrounds the entire Earth. UV-B radiation (280- to 315- nanometer (nm) wavelength) from the Sun is partially absorbed in this layer.
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- The stratospheric ozone layer, centered at about 20 km above the surface of the Earth (Figure 10-1), protects life on Earth by absorbing UV radiation from the Sun. In this chapter we examine the mechanisms controlling the abundance of ozone in the stratosphere and the effect of human influence.
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Atmosphere of the Sun: Photosphere, Chromosphere & Corona The atmosphere of the sun is composed of several layers, mainly the photosphere, the chromosphere and the corona. It's in these outer layers that the sun's energy, which has bubbled up from the sun's interior layers, is detected as sunlight. The lowest layer of the sun's atmosphere is the photosphere. It is about 300 miles (500 kilometers) thick. This layer is where the sun's energy is released as light. Because of the distance from the sun to Earth, light reaches our planet in about eight minutes.
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- The ozone layer is a layer of gas molecules which is bombarded with rays from the sun. These are harmful UV rays and this ozone layer in present in the stratosphere.he photosphere is the visible part of the Sun's atmosphere. The parts of the sun's atmosphere from the surface outward are the photosphere, the chromosphere, the corona, and the outer layers of the corona called the solar wind.
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- The troposphere is the atmosphere layer that is farthest from the  sun. This layer extends about 10 to 15 kilometers above the surface  of the Earth.he lithosphere is the solid part of the earth consisting of the crust and outer mantle. In other words, it is physically part of this planet. The atmosphere is not a solid no … r an object, and is not a geological part of our Earth.
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Ozone layer The ozone molecule is unstable (although, in the stratosphere, long-lived) and when ultraviolet light hits ozone it splits into a molecule of O 2 and an individual atom of oxygen, a continuing process called the ozone-oxygen cycle.
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- Ozone is constantly being formed in the earth's atmosphere by the action of the sun's ultraviolet radiation on oxygen molecules. Ultraviolet light splits the molecules apart by breaking the bonds between the atoms. A highly reactive free oxygen atom then collides with another oxygen molecule to form an ozone molecule.he other 10% of the ozone in the earth's atmosphere is found in the troposphere, which is the portion of the atmosphere from the earth's surface to about 12 km or 7 miles up.
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Layers of Earth's Atmosphere Thermosphere. The layer of very rare air above the mesosphere is called the thermosphere. High-energy X-rays and UV radiation from the Sun are absorbed in the thermosphere, raising its temperature to hundreds or at times thousands of degrees. However, the air in this layer is so thin that it would feel freezing cold to us!
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- In the language of a simplified chemical formula, When an electrically excited free oxygen atom encounters an oxygen molecule, they may bond to form ozone. Destruction of ozone in the stratosphere takes place as quickly as formation of ozone, because the chemical is so reactive.Sunlight can readily split ozone into an oxygen molecule and an individual oxygen atom.hen an electrically excited free oxygen atom encounters an oxygen molecule, they may bond to form ozone. Destruction of ozone in the stratosphere takes place as quickly as formation of ozone, because the chemical is so reactive. Sunlight can readily split ozone into an oxygen molecule and an individual oxygen atom.
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- The thermosphere and exosphere are together called the ionosphere because there is so much UV radiation from the sun that gases split apart into charged particles during ionization. The temperature in the ionosphere is extremely hot unlike the colder temperatures of lower atmosphere levels due to the low concentration of gases and high amount of energy in UV and X-rays from the sun.
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Atmosphere of the Sun: Photosphere, Chromosphere & Corona The atmosphere of the sun is composed of several layers, mainly the photosphere, the chromosphere and the corona. It's in these outer layers that the sun's energy, which has bubbled up from the sun's interior layers, is detected as sunlight.The lowest layer of the sun's atmosphere is the photosphere.It is about 300 miles (500 kilometers) thick. This layer is where the sun's energy is released as light. Because of the distance from the sun to Earth, light reaches our planet in about eight minutes.t's in these outer layers that the sun's energy, which has bubbled up from the sun's interior layers, is detected as sunlight. The lowest layer of the sun's atmosphere is the photosphere. It is about 300 miles (500 kilometers) thick. This layer is where the sun's energy is released as light.
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- The next layer up is called the stratosphere. In the stratosphere, temperature increases with altitude. This is because of ozone. When the ozone in this layer absorbs UV light from the sun, it increases in temperature. In the mesosphere, ozone concentration decreases. This means there is less absorption of UV light in this layer of atmosphere.
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- The stratosphere /ˈstraetɵsfɪər/ ˈstrætɵsfɪər is the second major layer Of'earth s, atmosphere just above the, troposphere and below the. Mesosphere it is stratified in, temperature with warmer layers higher up and cooler layers farther. downhe stratosphere is layered in temperature because ozone (O 3) here absorbs high energy ultraviolet (UVB and UVC) radiation from the Sun and is broken down into the allotropes of atomic oxygen (O 1) and common molecular oxygen (O 2).