ozone layer by mahesh joshi

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The ozone layer Depletion MAHESH DIGAMBER JOSHI M.Sc First Semester presentation Antarctic and Arctic ozone hole formation

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Page 1: Ozone Layer by Mahesh Joshi

The ozone layerDepletion

MAHESH DIGAMBER JOSHIM.Sc First Semester presentation

Antarctic and Arctic ozone hole formation

Page 2: Ozone Layer by Mahesh Joshi

What is the ozone layer?

The ozone layer or ozone shield refers to a region of Earth's stratosphere thatabsorbs most of the Sun's UV radiation. It contains high concentrations of ozone (O3)relative to other parts of the atmosphere, although it is still very small relative toother gases in the stratosphere. The ozone layer contains less than ten parts permillion of ozone, while the average ozone concentration in Earth's atmosphere as awhole is only about 0.3 parts per million. The ozone layer is mainly found in thelower portion of the stratosphere, from approximately 20 to 30 kilometres (12 to19 mi) above Earth, though the thickness varies seasonally and geographically

The ozone layer is the part of the upper atmosphere where ozone is found in the highest concentrations.

It is a deep layer in the stratosphere, encircling the Earth, that has large amounts of ozone in it

Page 3: Ozone Layer by Mahesh Joshi

Discoverey of Ozone LayerThe ozone layer was discovered in 1913 by the French physicists Charles Fabry and Henri Buisson. Its properties were explored in detail by the British meteorologist G. M. B. Dobson, who developed a simple spectrophotometer (the Dobsonmeter) that could be used to measure stratospheric ozone from the ground. Between 1928 and 1958 Dobson established a worldwide network of ozone monitoring stations, which continue to operate to this day. The "Dobson unit", a convenient measure of the amount of ozone overhead, is named in his honor.The ozone layer absorbs 97–99% of the Sun's medium-frequency ultraviolet light (from about 200 nm to 315 nm wavelength), which otherwise would potentially damage exposed life forms near the surface.

-Near the end of the last century, scientists discovered that ozone levels over the Antarctic were reduced. This discovery was unexpected. Chemists knew that reactive chlorine atoms could destroy ozone. They also knew that chemicals called chlorofluorocarbons - CFCs - break down in ultraviolet light to release reactive chlorine atoms. Scientists used these ideas to explain the low ozone levels.-CFCs were once used widely in insulating foam and aerosol spray-cans. Once released, they gradually spread through the atmosphere, eventually reaching the ozone layer. Once there, they destroy ozone. CFCs have now been almost completely replaced by chemicals that do not cause this damage.-An international treaty was signed in 1973 called the Montreal Protocol, and the manufacture of these chemicals was greatly reduced.

Page 4: Ozone Layer by Mahesh Joshi

Ozone is a special form of oxygen, made up of three oxygen atoms rather than the usual two oxygen atoms. It usually forms when some type of radiation or electrical discharge separates the two atoms in an oxygen molecule (O2), which can then individually recombine with other oxygen molecules to form ozone (O3).

The photochemical mechanisms that give rise to the ozone layer were discovered by the British physicist Sydney Chapman in 1930.

Formation of Ozone Layer

Ozone in the Earth's stratosphere is created by ultraviolet light striking oxygen molecules containing two oxygen atoms (O2), splitting them into individual oxygen atoms (atomic oxygen); the atomic oxygen then combines with unbroken O2 to create ozone, O3. The ozone molecule is unstable (although, in the stratosphere, long-lived) and when ultraviolet light hits ozone it splits into a molecule of O2 and an atom of atomic oxygen, a continuing process called the ozone-oxygen cycle.

Page 5: Ozone Layer by Mahesh Joshi

Formation of Ozone Layer

About 90% of the ozone in our atmosphere is contained in the stratosphere. Ozone concentrations are greatest between about 20 and 40 kilometres (66,000 and 131,000 ft), where they range from about 2 to 8 parts per million. If all of the ozone were compressed to the pressure of the air at sea level, it would be only 3 millimeters thick.

Chemically, this can be described as:

O2 + νℎ uv → 2O

O + O2 ↔ O3

Page 6: Ozone Layer by Mahesh Joshi

Necessity of Ozone LayerThe layer shields the entire Earth from much of the harmful ultraviolet radiation that comes from the sun.

United Nations General Assembly has designated September 16 as the International Day for the Preservation of the Ozone Layer.

The ozone there absorbs ultraviolet radiation, preventing most of it from reaching the ground. This is important because ultraviolet radiation can lead to skin cancer.

While stratospheric ozone which protects us from the sun is good, there is also ozone produced near the ground from sunlight interacting with atmospheric pollution in cities that is bad for human health. It causes breathing problems for some people, and usually occurs in the summertime when the pollution over a city builds up during stagnant air conditions associated with high pressure areas.

Page 7: Ozone Layer by Mahesh Joshi

Crisis on Ozone Layer