Ozone depletion
Stratospheric phenomena of Earth
Nº Q183140 ★★★
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Ozone depletion
Stratospheric phenomena of Earth
Ozone depletion in the stratosphere (the ozone layer) consists of two related phenomena observed since the late 1970s: a lowered total amount of ozone in Earth's upper stratosphere, and a much larger springtime decrease in around Earth's polar regions. The latter phenomenon over the south pole is referred to as the ozone hole.
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From Wikipedia
Ozone depletion in the stratosphere (the ozone layer) consists of two related phenomena observed since the late 1970s: a lowered total amount of ozone in Earth's upper stratosphere, and a much larger springtime decrease in around Earth's polar regions. The latter phenomenon over the south pole is referred to as the ozone hole. There are also springtime polar tropospheric ozone depletion events in addition to these stratospheric events. The main causes of ozone depletion and the ozone hole are manufactured chemicals, especially manufactured halocarbon refrigerants, solvents, propellants, and foam-blowing agents (chlorofluorocarbons (CFCs), HCFCs, halons), referred to as ozone-depleting substances (ODS). These compounds are transported into the stratosphere by turbulent mixing after being emitted from the surface, mixing much faster than the molecules can settle. Once in the stratosphere, they release atoms from the halogen group through photodissociation, which catalyze the breakdown of ozone (O3) into oxygen (O2). Ozone depletion in both the upper and lower stratosphere were observed to increase as emissions of halocarbons increased. Ozone depletion and the ozone hole have generated worldwide concern over increased cancer risks and other negative effects. The ozone layer prevents harmful wavelengths of ultraviolet (UVB) light from passing through the Earth's atmosphere. These wavelengths cause skin cancer, sunburn, permanent blindness, and cataracts, which were projected to increase dramatically as a result of thinning ozone, as well as harming plants and animals. These concerns led to the adoption of the Montreal Protocol in 1987, which bans the production of CFCs, halons, and other ozone-depleting chemicals. Over time, scientists have developed new refrigerants with lower global warming potential (GWP) to replace older ones. For example, in new automobiles, R-1234yf systems are now common, being chosen over refrigerants with much higher GWP such as R-134a and R-12. The controls on ozone-depleting substances came into effect in...
Text: Wikipédia, CC BY-SA 4.0. · Image: NASA (Public domain) ·