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The Ozone Layer

The ozone layer contains high ozone concentrations (O3), and we can describe it as a layer in the earth’s atmosphere. The layer is essential because it helps absorb 97-99% of the sun’s ultraviolet light, potentially dangerous to human, animal, and plant life. On earth, you will find over 90% of the ozone layer. The thickness of the ozone layer varies on the season and geography of the earth’s surface. The ozone layer is on the lowest part of the stratosphere, which is 15km to 35km above the earth’s surface. Scientists, who specialize in the measurement of the ozone layer, use the Dobson unit, which is 0.01mm thick at the Standard Temperature and Pressure (STP).

We often describe the ozone layer thickness in the form of Dobson units. The units measure the physical thickness of the ozone layer when compressed into the earth’s atmosphere. When we measure the thickness in those terms, we often find the layer quite thin. The standard ozone layer thickness is 300 to 500 Dobson units, equivalent to two pennies stacked together. When discussing the measurement of the ozone layer while in space, it is not recommendable that we think about it as a separate entity, which is measurable. However, scientists recommend that we view it as parts per million concentrations found in the stratosphere, mainly the layer found six to thirty miles above the earth’s surface. The Dobson unit used in the measurement of the thickness of the ozone layer is a discovery of the scientist, G.M.B. Dobson, who was the first scientist to research the earth’s atmosphere.

The gradual thinning out of the ozone layer puts a significant risk to human, plant, and animal life. For human beings, the destruction of this layer makes us prone to skin cancer and eye cataracts, and the most significant threat is to children. That’s why it is essential to have an ozone generator at home. For other forms of life on earth, destroying the ozone layer leads to biodiversity. The increase in the UV-B rays causes a reduction in plankton levels, which you can find in the oceans. These rays also decrease the fish levels in the water bodies. For plant growth, the increase in the UV-B rays harms plants’ growth, negatively affecting agriculture. These rays also harm other materials because they reduce their lifespan. The first incidence of ozone layer depletion in the Antarctic happened in the early 1980s.

This incident led to the adoption of the international response to the Montreal Protocol. Currently, over 190 countries are campaigning for the adoption of this protocol. The Montreal Contract is one of the best and most successful Multinational Environment agreements to be made and approved by countries. This protocol has helped reduce ozone-depleting substances, which helps eradicate climate change because the ozone-depleting elements are potent greenhouse gases.

A brief history of the ozone layer

In the beginning, the ozone layer formed in 600,000,000 B.C. In 1839, Christian Schöenbein was the first to discover the ozone layer while working in the laboratory. In 1845, two scientists, Auguste de la Rive and Jean-Charles de Marignac, suggested that an ozone layer is a form of oxygen, and Thomas Andrews confirmed this theory in 1856. Andrei Houzeau later discovered that the ozone layer was available in natural air in 1958 before Jean-Louis Soret proved that the ozone was O3 in 1865. In the mid-1900s, John William Strut showed that absorption could not happen in the lower atmosphere. In 1919, Charles Fabry made the first spectrometric measurements, which showed the thickness of the ozone layer. In 1930, Sydney Chapman came up with the theory describing the existence of the ozone layer. In 1934, the balloon measurements established that the ozone concentration was up to 12 miles up. In the 1930s, G.M. developed the application for CFC, and in the 1950s, these CFC markets.

In 1987, the Montreal Protocol was formed on substances that deplete the ozone layer. In 1988, DuPont agreed on the CFC production phase-out, and in 1991, DuPont decided on the phase-out of the CFC production by 1996. In the late 1980s, ten years of satellite data began to show the depletion of the ozone layer. In 1992, there was an abnormal observation of low ozone globally. In 1996, there was a total decrease in CFC production in the U.S. and Europe. Shortly after, in 2000, there was an increase in the total amounts of CFCs in the atmosphere.

Future of the Ozone Layer

In 2010, the production of CFC phased out across the globe. By the end of 2030, the HCFC alternatives, otherwise known as Hydrochlorofluorocarbon, will no longer exist, and by 2040, the production of HCFC products will cease across the globe. In 2050, the Springtime Antarctic ozone hole will disappear.