The Ozone Layer and Climate Change

Since the beginning of the Industrial Revolution in the early 19th century, our ability to change the world around us became very deep. At first, the impact on the Earth is hardly noticeable, but as the quantity and skill increases, this influence will increase. Recently, the impact of the increase in our activities has begun to appear in various subtle, slightly subtle ways. We are thinning the ozone layer and are beginning to change the dependence on the earth of the climate system of us and all other lives.

In some studies, the ozone layer is related to climate change, but this is another phenomenon. Ozone is a layer of gas located in the upper part of the atmosphere (the stratosphere) and is located at approximately 20 to 48 km above sea level. It contains various forms of oxygen (oxygen allotropes) that react continuously in the presence of ultraviolet light to pass harmless ultraviolet light. Since this layer contains reactive gases, these gases are inherently highly artificial and chemically stable in the atmosphere but they are detrimental if they drift into the upper stratosphere and the ozone layer It consumes.

Stratospheric ozone layer: The stratosphere contains the layer with the highest ozone concentration, the so-called ozone layer. This layer ranges from about 12 to 40 kilometers. Chlorine and bromine compounds released from the human body are exhausting this layer. Every year in the spring of the Southern Hemisphere, extremely strong ozone depletion occurs in Antarctica. This is caused by artificial chlorine and bromine compounds and the weather conditions in the area. Ozone hole

Since ozone itself is a greenhouse gas and contributes to global warming together with other ozone-depleting substances such as bromine (Br) and chlorine (Cl), climate change and destruction of the ozone layer are interrelated I will. Therefore, changes in atmospheric concentrations and ozone distribution have a major impact on the global climate system. The release of these (ODS) substances including carbon dioxide and chlorofluorocarbon brings about a cooling effect in the stratosphere. This cooling effect promotes the chemical reaction of chlorine and bromine, which leads to the formation of polar stratospheric clouds (PSC), which is a condition leading to destruction of the ozone layer.