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Titlebook: Global Atmospheric Chemical Change; C. N. Hewitt,W. T. Sturges Book 1994 Springer Science+Business Media Dordrecht 1994 air pollution.clim

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發(fā)表于 2025-3-21 19:47:05 | 只看該作者 |倒序瀏覽 |閱讀模式
書目名稱Global Atmospheric Chemical Change
編輯C. N. Hewitt,W. T. Sturges
視頻videohttp://file.papertrans.cn/387/386033/386033.mp4
叢書名稱Environmental Management Series
圖書封面Titlebook: Global Atmospheric Chemical Change;  C. N. Hewitt,W. T. Sturges Book 1994 Springer Science+Business Media Dordrecht 1994 air pollution.clim
描述Air pollution has historically been viewed as a local or regional scale problem with attention focused on acute episodes such as the sulphur dioxide and smoke smogs of London in the 1950s and 1960s and the photochemical smogs of southern California first recognized by Haagen- Smit in the early 1950s. In recent years, however, it has become apparent that human activity has, and still is, changing the chemical composition of the atmosphere on a global scale. The composition of the atmosphere has seen enormous changes due to natural processes since the formation of the planet. Data obtained from air bubbles trapped in polar ice are beginning to reveal information about these changes over the last tens of thousands of years and geochemical models of the evolution of the Earth give us insights into the changes over much longer periods of time. Perhaps the crucial differences between 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 emission
出版日期Book 1994
關鍵詞air pollution; climate; climate change; environment; environmental management; ozone; pollution
版次1
doihttps://doi.org/10.1007/978-94-015-3714-8
isbn_softcover978-94-015-3716-2
isbn_ebook978-94-015-3714-8
copyrightSpringer Science+Business Media Dordrecht 1994
The information of publication is updating

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https://doi.org/10.1007/978-4-431-56535-2stics, 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 climate is our subject—comprises the revelant subsystems: the atmosphere, the hydrosphere, the cryosphe
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Alyssa Rumsey,Christopher A. Le Dantecle it is possible that the next decade will see a shift of research interest towards problems such as long-term climate change, acid rain will present a practical challenge for a considerable time. Acid rain has many meanings: for some it is simply rainfall with pH < 5·0, but definitions can be so b
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Humanbiologie für Lehramtsstudierendely greater detail and with greater precision than ever before possible. This is particularly true for studies of the organic chemical composition of the atmosphere. Measurements of organic chemicals have been made in a variety of atmospheric environments around the globe: from urban and rural sites
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https://doi.org/10.1007/978-3-662-45368-1tive. In1900, Wilson. investigated the electrical conductivity of air and showed that it could be explained by low level ionisation of the air, and two years later Elster and Geitel. showed that a negatively charged wire exposed in the atmosphere became radioactive. The same authors. showed that soi
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Wolfgang Clauss,Cornelia Clauss has been repeated in other areas of environmental concern (e.g. water, endangered species, marine resources), culminating in what has been referred to as the ‘internationalization of environmental regulation.’. This chapter addresses major local, national and international milestones in the regulat
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Chemical Changes of the Atmosphere on Geological and Recent Time Scales,urs Venus and Mars have atmospheres containing carbon dioxide as the major constituent, whereas the more massive outer planets, starting with Jupiter, have atmospheres dominated by hydrogen, with smaller contributions of helium, methane and ammonia. Earth also is the only planet endowed with an ocea
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