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Glaciological Literature

Published online by Cambridge University Press:  30 January 2017

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Copyright © International Glaciological Society 1955

This bi-annual list of glaciological literature aims to cover the scientific aspects of snow and ice in all parts of the world. Attention is drawn to the bibliographies in each number of the Polar Record (Cambridge), which aim to cover the significant work dealing with expeditions, research, equipment and conditions of living in the Polar regions. Both journals, however, deal with Polar literature having specific glaciological interest and with general matters of a practical nature such as snowcraft.

Readers will greatly assist the Editor by notifying him of their own, or any other, publication of glaciological interest.

References

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Jenness, J. L. Problem of glaciation in the western islands of arctic Canada. Bulletin of the Geological Society of America, Vol. 63, 1952, p. 93951. [Extent and character of former glaciation of islands west of approximately 95° W.]CrossRefGoogle Scholar
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Kahn, F. D. The formation of interstellar dust. Monthly Notices of the Royal Astronomical Society, Vol. 112, No. 5, 1952, p. 51826. [Calculations on the assumption that interstellar dust consists primarily of ice crystals. Includes calculation of tensile strength of polarized ice crystal.]CrossRefGoogle Scholar
Kasser, P. Ablation und Schwund am Grossen Aletschgletscher. Verhandlungen der Schweizerischen Naturforschenden Gesellschaft, 133 Sitzung, Lugano 1953, p. 7375. [Shows sinking of the glacier surface from 1926 to 1947.]Google Scholar
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Klæboe, H. The Hellstugu River: investigations concerning the run-off conditions. Norsk Geografrsk Tidsskrift, Bd. 14, Ht. 1–4, 1953, p. 14051. [Measurements on a glacier stream in Jotunheim, Norway, correlated with the processes of the glacier.]Google Scholar
Korff, S. A. Effect of the melting of polar ice on the length of the day. Physical Review, Ser. 2, Vol. 95, No. 1, 1954, p. 20697. [The length of the day would increase by 26 microseconds if 1000 cubic Km. of ice melted-e.g. if the surface of Antarctica dropped 3 cm.]Google Scholar
Kreeb, K. Die Schneeschmelze als phänologischer Factor. Meteorologische Rundschau, 7 Jahrg., Ht. 3–4, 1954, p. 4849. [Advocates use of maps of snow cover as well as of plant development as indication of climatic conditions during spring.]Google Scholar
Kuhn, W. Statistische Ergebnisse von Firnzuwachsmessungen. Verhandlungen der Schweizerischen Naturforschenden Gesellschaft, 133 Sitzung, Lugano 1953, p. 7173. [Correlation between firn accumulation and meteorological conditions.]Google Scholar
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Lauscher, F. Klimatologische Probleme des festen Niederschlags. Archiv für Meteorologie, Geophysik und Bioklimatologie, Serie B, Bd. 6, Ht. 1–2, 1954, p. 6065. [On basis of alpine, Norwegian and arctic observations, relation derived between percentage of precipitation in solid form and monthly and annual mean temperature. Different relation found in pack-ice zone.]CrossRefGoogle Scholar
Lauscher, F. Schneedichten in Norwegen. Wetter und Leben, Jahrg. 6, Ht. 3–4, 1954, p. 6061. [Density of snow cover in Norway during twentieth century.]Google Scholar
Liestøl, O. Et forsok ph mäling av breforandring i Antarktis. Norsk Geogïafisk Tidsskrift, Bd. 14, Ht. 1–4, 1953, p. 15257. [Air photographs used to estimate increase of glaciers in Dronning Maud Land and Australian Antarctic Territory.]Google Scholar
Lliboutry, L. Le Massif du Nevado Juncal (Andes de Santiago); ses pénitents et ses glaciers. Revue de Géographie Alpine, Tom. 42, Fasc. 3, 1954, p. 46595. [Cartography of the Nevado Juncal Massif, its climate especially with regard to penitente formation; the regime of the glaciers, and their recent fluctuations.]Google Scholar
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Martin, S. Observations sur le relief glaciaire en Irlande du sud. Chronique Géographique des Pays Celtes, An. 1953, p. 12532. [Of the two great Irish glaciations, the Eastern General and Midland General, the latter is only represented in the south by the independent local Cork-Kerry glacier.]Google Scholar
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Nakaya, U. Matsumoto, A. Evidence of the existence of a liquidlike film on ice surfaces. U.S. Snow, Ice and Permafrost Research Establishment. Research Paper 4, 1953, 6 p. [In regelation the surface of ice behaves as though it had a liquid surface film.]Google Scholar
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