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and carbon tetrachloride) in chemistry labs Roughly 84% of stratospheric chlorine comes from human-made sources, while only 16% comes from natural sources Unfortunately, these compounds don t just break down in the atmosphere and disappear They linger and are carried by winds into the stratosphere to destroy ozone faster than it is naturally created CFCs break down only by exposure to strong UV radiation When that happens, CFC releases chlorine, which damages the ozone layer Scientists have found that 1 atom of chlorine can destroy over 100,000 ozone molecules In the 1950s, a hole or thinning of the ozone layer over Antarctica was first reported This annual event of extremely low ozone levels showed drops of over 60% during bad years Further research found ozone also thinned over North America, Europe, Asia, Australia, South America, and Africa In fact, since the first reports, Earth observation satellites, such as the European Space Agency s Envisat, track the yearly arrival and shape of the ozone hole Scientific outcry over ozone depletion led to a 1978 ban on aerosol CFCs in several countries, including the United States In 1985, the Vienna Convention was tasked to gather international cooperation in reducing CFC levels by half The good news is that atmospheric chlorine stopped rising in 1997-98, and if this trend continues, natural ozone recovery should occur in about 50 years The ozone layer will recover over time, but other problem gases (eg, sulfur hexafluoride) are released during aluminum smelting, electricity production, magnesium processing, and semiconductor manufacturing and need to be addressed as well

Green plants use the sun s energy and carbon dioxide from the air for photosynthesis This is a good thing, because they soak up carbon dioxide in the process Plants are considered to be carbon dioxide storehouses During the photosynthetic cycle, they form carbohydrates, which make up the foundation of the food chain Forests absorb carbon dioxide in a big way Over time, forests build up a significant supply of stored carbon in their tree trunks, roots, stems, and leaves Then, when the land is cleared, this stored carbon is converted back to carbon dioxide by burning or decomposition The oceans are another big player in this process of carbon dioxide absorption They also absorb carbon dioxide from the atmosphere and act as a moderating influence on temperature ranges

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Ozone reduction is a global issue since it makes the Earth vulnerable to solar radiation When the protective ozone layer is thin or absent, the sun s harmful UV radiation is able to get through the atmosphere and reach the Earth s surface Ozone depletion is strongly affected by chlorofluorocarbons and halons that made their way into the stratosphere However, excessive ozone is also an atmospheric pollutant, especially in urban areas Urban ozone is a major conponent of smog and forms when volatile organic compounds and nitrogen oxides react in sunlight These reactants come from vehicle, construction, industrial and residential (lawn and garden) equipment exhaust as well as some paints and cleaners Ozone pollution is believed to cause planetwide heating in addition to its bad health effects To slow ozone s contribution to global warming, exceptional international cooperation is crucial

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Climate change includes temperature increases, rising sea levels, rainfall changes, and more extreme weather events Scientific data discussed at the 2002 World Summit on Sustainable Development and the 2004 United Nations Convention on Biological Diversity suggest global

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warming is causing shifts in species habitat and migrations by an average of 61 kilometers per decade toward the poles This shift, predicted by climate change models, notes that spring arrives 23 days earlier per decade, on average, in temperate latitudes Entire boreal and polar ecosystems are also showing the effects of global warming Climate change describes the difference in either the average state of the climate, or its variability, taking place over an extended period of time

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