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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https://doi.org/10.1007/978-3-642-99600-9g of chemical species (Barnola et al., 1987; Dansgaard et al., 1989; Mayewski et al., 1990; Taylor et al., 1993). This information has been obtained by noting variations in chemical concentrations and in ice properties with depth in ice sheets worldwide (Delmas and Legrand, 1989). Virtually all of t

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P,s Theorie des Wasserstoffatomsis directly applicable to ice cores, occurrence of certain processes are inferred from the results of lower temperature studies carried out to understand polar stratospheric clouds (PSCs). It is suggested that strong acids will be efficiently taken up. Easily-hydrolyzable species such as .... and ..

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P,s Theorie des Wasserstoffatomsf processes in dry snow and polar firn shows feedback mechanisms exist between microstructure changes and energy and mass transfer coefficients. Differences between the predominant processes in the short polar summer and the winter cause sharp textural discontinuities in the stratigraphic columns at

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https://doi.org/10.1007/978-3-642-99600-9 These chemical constituents have been subjected to a series of physical and chemical processes at each step on their journey from the remote paleo-atmosphere into the ice (see Neftel, this volume; Waddington, this volume). Current research in polar snow chemistry focuses on the . the chemical and p

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https://doi.org/10.1007/978-3-642-99600-9rpretation of glacial phenomena:.Following Peary’s reasoning, the blowing snow phenomenon was studied intensively in the Antarctic several decades ago (Lister, 1960; Mellor and Radok, 1960; Dingle and Radok, 1961; Budd et al, 1966) with more recent studies by Kobayashi (1978), Takahashi (1985) and M

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Nato ASI Subseries I:http://image.papertrans.cn/c/image/224338.jpg

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