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Titlebook: Global Atmospheric Chemical Change; C. N. Hewitt,W. T. Sturges Book 1993 Elsevier Science Publishers Ltd. 1993 air pollution.atmosphere.cl

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Joseph Thachil George,Meghna Joseph Georgegeochemical coupling between the continents and the oceans. For example, throughout geological times, aeolian mineral particles originating from arid and semi-arid regions have probably been — major source of particulate and dissolved materials found in many areas of the open ocean. It is now believ
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Book 1993ural changes and those now being induced by man are their rel­ ative rates of change. The magnitude of present day fluxes of some com­ pounds released as air pollutants is in some cases much larger than those arising naturally. In other cases, for example carbon dioxide, the an­ thropogenic emission
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these natural changes and those now being induced by man are their rel­ ative rates of change. The magnitude of present day fluxes of some com­ pounds released as air pollutants is in some cases much larger than those arising naturally. In other cases, for example carbon dioxide, the an­ thropogenic emission978-94-011-1864-4
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Global Change in Atmospheric Metal Cycles,geochemical coupling between the continents and the oceans. For example, throughout geological times, aeolian mineral particles originating from arid and semi-arid regions have probably been — major source of particulate and dissolved materials found in many areas of the open ocean. It is now believ
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Global Climate Change due to Radiatively Active Gases,the potential changes to climate that may be occurring due to growing atmospheric concentrations of gases that absorb terrestrial infrared radiation, termed greenhouse gases. Much of this concern has centeredaround carbon dioxide (CO.) because of its importance as — greenhouse gas and also because o
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Global Climate Change due to Aerosols,ics, and an effect, the impact of climate. This list is not exhaustive. More, and quite different categories have been used for defining climate.’ The climate system of the Earth-and this global climateis our subject-comprises the revelant subsystems: the atmosphere, thehydrosphere, the cryosphere,
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