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Titlebook: Glacier Fluctuations and Climatic Change; Proceedings of the S Johannes Oerlemans Conference proceedings 1989 Springer Science+Business Med

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Calculation of Glacier Ablation from Air Temperature, West Greenland,of positive temperature sums. The relation has already been used for the simulation of runoff from glacier-covered basins but might also be suitable for calculating ablation under alternative climates..The degree-day factor, linking ice ablation to positive temperature sums, shows no distinct season
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On the Blowing Snow in Adelie Land, Eastern Antarctica, The instrument photo-electrically measures the number and size of the snow particles. The logarithm of the mass fluxes were found to vary with the wind speed, a result previously reported..We know the annual wind speed from an automatic weather station (AWS), which reports over satellite year round
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Karl Volger,Erhard Laasch,Erhard Laasch to assist in refining the glacial chronology and in reconstructing palaeoclimate. Topographic position of deposits, weathering features, degree of soil development, and radiocarbon assist in assigning ages to Quaternary deposits in the Afroalpine and bamboo forest-Hagenia woodland zones. AD and RD
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https://doi.org/10.1007/978-3-8348-9900-2 sections up to 11 m deep, and containing up to 78 tephra layers, were logged to a resolution of 0.25 cm. The chronological framework was completed with 15 radiocarbon dates, and by examining the association of the tephra stratigraphy with moraines representing former ice margins, a chronology of Ho
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Die Domestikation der einzelnen Arten standardized glacier information. The data basis is briefly described and illustrated. It includes observations on changes in length and, since World War II, also in mass, as well as recent glacier inventories. By far the highest information density is found for the Alps and Scandinavia..About 90 y
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