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Quality & Definitions, we provide a table of ODS and their respective ‘ozone depleting potential’ . ODP measures the relative impact on ozone depletion per tonne of gas. An ODP of 10, for example, is ten times as effective in depleting ozone per tonne, than an ODP of The emission of ozone-depleting gases impacted the earth’s ozone layer – a layer that absorbs most of the Sun’s ultraviolet radiation. Emissions were increasing rapidly until the 1980s. Higher air temperatures are increasing the surface water temperatures of numerous lakes and oceans, with many large lakes warming at twice the rate of air temperatures in some regions. Species composition and distribution of many marine ecosystems may change with warmer oceans. For others, such as corals, the warming may alter their tolerance to other stressors. This warming can also shift the thermal niche of organisms towards the pole and causes changes in community structure. Such a balance may be difficult to achieve in practice as the recommended time outdoors will differ between individuals, depending on personal factors such as skin colour, age, and clothing as well as on environmental factors such as location, time of day, and season of year. Current uncertainties centre on defining an optimal level of vitamin D and the amount and pattern of sun exposure required to achieve the optimum in different individuals. Thus, devising appropriate health messages for the public at the present time is not straightforward. Vitamin D is critical in maintaining blood calcium levels and is required for strong bones. People vary in how efficiently their skin makes vitamin D from sun exposure and perhaps in their physiological needs for this vitamin. Vitamin D deficiency might increase the risk of an array of diseases such as cancers, autoimmune diseases and infections. At present it is not clear if the low level of vitamin D is a cause of these diseases, occurs as a consequence of them, or is a marker of other factors that predispose to ill-health. Increases in UV-B irradiance 280–15 nm ranging from 5 to 10% per decade have been reported for several northern mid-latitude sites, caused predominantly by reductions in cloudiness and aerosols. However, at some northern high latitude sites, UV-B irradiance has decreased during that period mainly due to reduction in snow- or ice-cover. Because of the large natural variability, any responses of UV-B irradiance to stabilisation of the concentrations of stratospheric ozone and possible beginning of a recovery are not yet detectable in the measurements. Chlorine is able to destroy so much of the ozone because it acts as a catalyst. Chlorine initiates the breakdown of ozone and combines with a freed oxygen to create two oxygen molecules. After each reaction, chlorine begins the destructive cycle again with another ozone molecule. One chlorine atom can thereby destroy thousands of ozone molecules. Because ozone molecules are being broken down they are unable to absorb any ultraviolet light so we experience

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