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Titlebook: Chemical Exchange Between the Atmosphere and Polar Snow; Eric W. Wolff,Roger C. Bales Conference proceedings 1996 Springer-Verlag Berlin H

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书目名称Chemical Exchange Between the Atmosphere and Polar Snow
编辑Eric W. Wolff,Roger C. Bales
视频videohttp://file.papertrans.cn/225/224338/224338.mp4
丛书名称Nato ASI Subseries I:
图书封面Titlebook: Chemical Exchange Between the Atmosphere and Polar Snow;  Eric W. Wolff,Roger C. Bales Conference proceedings 1996 Springer-Verlag Berlin H
描述Polar ice cores have provided tremendous advances in our knowledge of past climate change. They also contain an archive of geochemical data, which can certainly delineate some of the forcing factors that govern climate change. However, our ability to interpret these data is severely curtailed by lack of knowledge of the processes governing the transfer of chemical species from the air to the snow. This book outlines the potential and problems of ice core chemistry and discusses the processes involved in air-snow transfer. It gives the state of current knowledge and an agenda for future research.
出版日期Conference proceedings 1996
关键词Antarktis; Atmosphäre; Eisbohrkerne; Greenland; Grönland; Ice cores; Klimaveränderung; Schnee; Snow; antarcti
版次1
doihttps://doi.org/10.1007/978-3-642-61171-1
isbn_softcover978-3-642-64730-7
isbn_ebook978-3-642-61171-1Series ISSN 1431-7125
issn_series 1431-7125
copyrightSpringer-Verlag Berlin Heidelberg 1996
The information of publication is updating

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Central Antarctica: Atmospheric Chemical Composition and Atmospheric Transport,n on earth. It is a true pristine background environment in the most fundamental sense. Indeed, it may be the . true pristine background environment. Yet, airborne materials of anthropogenic origin are detected there, albeit at very small concentrations, thanks to long-range transport and mixing pro
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Chemical Reactions in the Polar Troposhere Relevant to C, S, and N Compounds,e is attenuated by scattering and absorption processes in the upper layers of the atmosphere. In polar regions, the path to the troposphere is longer than at other parts of the globe, and hence less radiation is available for photochemical processes. In fact, during the winter months the lower parts
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Overview Of Field Data on the Deposition Of Aerosol-Associated Species to the Surface Snow Of Polariers and the composition of aerosols in the overlying atmosphere. The limited data exisiting prior to the late 1980s indicated that aerosol removal processes should cause fractionation between the composition of aerosols and snow. Uncertainties regarding the relative importance of ice-nucleation sca
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