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Glaciological Literature

Published online by Cambridge University Press:  30 March 2017

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Abstract

Type
Research Article
Copyright
Copyright © International Glaciological Society 1955

This biannual 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

Ängeby, O. Recent, subglacial and lateroglacial pothole-erosion (evorsion). Kungl. Fysiografiska Sällskapets i Lund Handlingar, N.F., Bd. 63, Nr. 5, 1952, 53 p. [Potholes formed by glacial and non-glacial streams compared. Also published as Lunds Universitets Årsskrift, N.F., Avd. 2, Bd. 48, Nr. 5, 1952, and as Lund Studies in Geography, Ser. A, No. 3, 1952, p. 14–24.]Google Scholar
Akkuratov, V. Bluzhdayushchiye ostrova [Wandering islands]. Vokrug Sveta [Round the World], No. 6, 1954, p. 1.721. [Possible reasons for disappearance of arctic islands; “ice island“sighted 700 km. north of Ostrov Vrangelya in March 1946.]Google Scholar
Arakawa, K. Studies on the freezing of water. 2. Formation of disc crystals. Journal of the Faculty of Science, Hokkaidd University, Ser. 2, Vol. 4, No. 5, 1954, p. 31139. [Conditions which produce disc crystals; surface phenomena of growing crystals; mechanics of anchor ice formation.]Google Scholar
Artmann, K. Hybridisierung, Gleichgewichtswinkel and Normalschwingirilgen von H2O and verwandten Molekülen. Zeitschrift für Physik, Bd. 538, Ht. 5, 1954, p. 64057. [Theory of the position of the H atoms in H2O, H2S and H2Se.]CrossRefGoogle Scholar
Atwater, M. M. The relationship of precipitation intensity to avalanche occurrence. Proceedings. Western Snow Conference, 20th annual meeting, 21 and 22 April 1952.Fort Collins, Colorado, 1952, p. 1119. [Recent investigations at U.S. Forest Service experimental stations.]Google Scholar
Atwater, M. M., Avalanche research; a progress report, part I, by M. M. Atwater E. [R.] LaChapelle R. M. Stillman F. M. Foto. Appalachia, N.S. Vol. 20, No. 12, 1954, p. 20920. [Research by U.S. Forest Service on use of new snowfall intensity gauge, of snow collectors and of operations recorders; new electronic avalanche timing system.]Google Scholar
Avsyuk, G. A. Lednik Inylchek. (In Pobezhdennyye vershiny. Yezhegodnik sovetskogo al’pinizma. God 1952 [Conquered peaks. Yearbook of Soviet Mountaineering, 1952] (Moscow), 1952, p. 2790.) [Glacier in Tien Shan; description and history of exploration and study. Copy at Royal Geographical Society.]Google Scholar
Baird, P. D., Baffin Island expedition 1953: a preliminary field report. Arctic, Vol. 6, No. 4, 1953, p. 22651. [Expedition to Cumberland Peninsula area. Reports on glacier physics by W. H. Ward; seismic soundings by H. Röthlisberger; meteorology by S. Orvig and B. H. Bonnlander; geology by D. J. Kidd; geomorphology by H. R. Thompson; zoology by A. Watson; botany by F. H. Schwarzenbach; mountaineering and surveying by J. Marmet; photography by J. A. Thomson and J. R. Weber.]Google Scholar
Bauer, A. Glaciologie. Groenland. Vol. 2: le glacier de l’Eqe. Paris, Hermann, 1955. 120 p., 26 plates. (Actualités scientifiques et industrielles, 1225; Expéditions Polaires Françaises [travaux], 6.) [Ice streams in Ata Sund region, west Greenland; description of lower reaches of Eqip Sermia, velocity, regime. Bibliography. German and English summaries.]Google Scholar
Black, R. F. Precipitation at Barrow, Alaska, greater than recorded. Transactions. American Geophysical Union, Vol. 35, No. 2, 1954, p. 20307. [Data on depth and density of snow, winter 1949–50, show that wind affects accuracy of standard U.S. Weather Bureau 8-inch precipitation gauge. Discussion by W. T. Wilson, p. 206–07.]Google Scholar
Bowden, F. P. Recent studies of metallic friction. London, Institution of Mechanical Engineers, 1954. 12 p. (Hawksley Lecture.) [Includes section on friction in skiing and the development of some new fast-running ski.]Google Scholar
Bowden, F. P. Rowe, G. W. The friction and mechanical properties of solid krypton. Proceedings of the Royal Society, Ser. A, Vol. 228, No. 1172, 1955, p. 19. [Includes comparison between friction and hardness of krypton and those of ice.]Google Scholar
Breitner, H. J. Entmischung beim Gefrieren wässeriger Lösungen. Deutsche Hydrographische Zeitschrift, Bd. 6, Ht. 2, 1953, p. 8086. [Effect of concentration and cooling temperature of salt solutions on the structure of their ice. Salt content of sea ice at different temperatures discussed.]Google Scholar
Broida, H. P., and others. Optical spectroscopic determination of hydrogen isotopes in aqueous mixtures, by Broida, H. P. Morowitz, H. J. Selgin, M. Journal of Research of the National Bureau of Standards, Vol. 52, No. 6, 1954, p. 293301. [Methods of quick determination of deuterium oxide concentration using a small sample.]Google Scholar
Brothers, R. N. The relative Pleistocene chronology of the South Kaipara district, New Zealand. Transactions of the Royal Society of New Zealand, Vol. 82, Part 3, 1954, p. 67794. [Correlation of this district in western North Island (N.Z.) with European Pleistocene chronology.]Google Scholar
Carlson, H. Calculation of depth of freezing and thawing under pavements. U.S. Highway Research Board. Bulletin 71, 1953, p. 8598. [Theory compared with empirical results in Alaska. Discussion by H. P. Aldrich and H. M. Paynter, p. 95–98.]Google Scholar
Corbel, J. Sols polygonaux et “terrasses marines” du Spitzberg. Revue de Géographie de Lyon, Vol. 29, No. 1, 1954, p. 128. [In Spitsbergen practically all the great fields of polygons are found on limestones forming marine terraces.]CrossRefGoogle Scholar
Crary, A. P. A brief study of ice tremors. Bulletin of the Seismological Society of America, Vol. 45, No. 1, 1955, p. 19. [Seismic ice tremors in floating ice at Barter Island, Alaska, recorded and possible causes discussed.]CrossRefGoogle Scholar
Diamond, M. lowry, W. P. Correlation of density of new snow with 700-millibar temperature. Journal of Meteorology, Vol. 11, No. 6, 1954, p. 51213. [Correlation found with 700 mb. temperature but not with 500 mb. temperature.]Google Scholar
Dibner, V. D. O proiskhozhdenii plovuchikh ledyanykh ostrovov [Origin of floating ice islands]. Priroda [Nature], 1955, No. 3, p. 8992. [Origin from glacier tongues suggested; iceberg 12 km. long in fiord in Severnaya Zemlya quoted as example.]Google Scholar
Dobrowolski, A. B. Petrografia lodu a pojecie linii brzegowej lqdu polarnego [Petrography of ice and the coast line of polar lands]. Acta Geologica Polonica (Warsaw), Vol. 3, 1953, p. 19092. [Author proposed that land and sea ice should be regarded as crystalline rock; special reference is made to the problem of determining the coast line of glacier–covered land merging into ice shelf. Russian and French summaries, p. 599–62.]Google Scholar
Dole, M. The chemistry of the isotopes of oxygen. Chemical Reviews, Vol. 51, No. 2, 1952, p. 263300. [Includes discussion of isotopic separation in freezing. Bibliography.]Google Scholar
Dorywalski, M. Zastowowanie wskaánika zaokrqglenia do badań peryglacjalnych [Application of the smoothness index (indice d’émoussé) of pebbles to periglacial research], Biuletyn Peryglacjalny [Periglacial Bulletin], Nr. 1, 1954, p. 3538, 132–35. [Use of Cailleux’ index of smoothness in determining origin of sediments. French translation, p. 132–35.]Google Scholar
Dury, G. H. A glacial breach in the north western Highlands. Scottish Geographical Magazine, Vol. 69, No. 3, 1953, p. 10617. [Drainage development.]Google Scholar
Dylikowa, A. Olchowik, J. Zmarzlina—Pojçcia ogólne [Frozen ground—general terms]. Biuletyn Peryglacjalny [Periglacial Bulletin], Nr. 1, 1954, p. 3948, 136–41. [Survey of terms used to describe frozen ground in English, French, German, Russian and Polish, including the ice in it and the active layer. English translation, p. 536–45.]Google Scholar
Eythórsson, J. Report on sea ice off the Icelandic coasts in Jan.-Sept. 1953. Jökull, Ár 3, 1953, p. 4549. [Observations in area between Iceland and Greenland, lats. 65°–72° N.]Google Scholar
Flint, R. F. Rates of advance and retreat of the margin of the late-Wisconsin Ice Sheet. American Journal of Science, Vol. 253, No. 5, 1955, p. 24955. [Rates of advance and retreat from C14 dates of wood.]CrossRefGoogle Scholar
Freymann, M. Freymann, R. Spectre hertzien et structure des solides: II, absorption Debye de l’eau libre et de l’eau liée. Journal de Physique et le Radium, Sér. 8, Tom 55, No. 3, 1954, p. 16575. [Review article, including dielectric losses in ice.]Google Scholar
Fristrup, B. Istidens isfrie oaser. Grønland, Ht. 8, [1953], p. 29195. [Ice-free areas in Greenland and other arctic regions during Ice Age, as indicated by survival of plant and animal life.]Google Scholar
Fristrup, B. Permafrost. Grøniand, Ht. 9, [1953], p. 33136. [Effect on roads and buildings.]Google Scholar
Frödin, G. De sista skedena av Centraljämtlands glaciala historia. Geographica, No. 24, 1954, 251 p. [Last stages of glacial history of central Jämtland (Sweden). English summary.]Google Scholar
Garavel, L. Comportement glaciaire et fluctuations climatiques. Revue Forestière Française, No. 1, 1955, p. 926. [Study of the Glacier de Sarennes in relation to the local climatic conditions.]Google Scholar
Gerdel, R. W. The transmission of water through snow. Transactions. American Geophysical Union, Vol. 35, No. 3, 1954, p. 47585. [Instrument to detect water content of snow by measuring dielectric constant; its use to measure rate of water transmission in snow for different snow densities.]Google Scholar
Glen, J. W. The creep of polycrystalline ice. Proceedings of the Royal Society, Ser. A, Vol. 228, No. 1175, 1955, p. 51938. [Results of compression tests on polycrystalline blocks of ice in the laboratory.]Google Scholar
Goedecke, E. Über den Zusammenhang zwischen Eis- und Kältesumme sowie Oberflächentemperatur in der Elbe- und Wesermündung während der Winter 1903–1950. Annalen der Meteorologie, Jahrg. 6, Ht. 5/6, 1953/54, p. 15163. [Relation between number of days with ice and mean temperatures of air and of surface water of rivers.]Google Scholar
Gold, L. W. Power, B. A. Dependence of the forms of natural snow crystals on meteorological conditions. Journal of Meteorology, Vol. 11, No. 5, 1954, p. 3542. [Observations during a snowfall gave dependence with temperature in agreement with Nakaya’s laboratory tests.]2.0.CO;2>CrossRefGoogle Scholar
Gordiyenko, P. A. Izucheniye ledovogo rezhima v arkticheskikh moryakh i Severnom Ledovitom okeane [Study of ice behaviour in the arctic seas and the Arctic Ocean]. Morskoy Flot [Merchant Fleet], 1955, No. 3, p. 2528. [Drift of sea ice in Arctic Ocean, based largely on work of Soviet drifting stations, 1954–55.]Google Scholar
Gutenberg, B. Postglacial uplift in the Great Lakes region. Archiv für Meteorologie, Geophysik und Bioklimatologie, Serie A, Bd. 7, 1954, p. 24351. [Uplift data of North America similar to those for Fennoscandia.]Google Scholar
Haefeli, R. Creep problems in soils, snow and ice. Revised and supplemented version. Proceedings of the Third International Conference on Soil Mechanics and Foundation Engineering, Switzerland, 16th to 27th August 1953. Zürich, Berichthaus, Vol. 3, [1953 or 4], p. 23851. [Discussion on creep, shear and plasticity in snow, glaciers and soils.]Google Scholar
Haley, J. F. Cold-room studies of frost action in soils; a progress report. U.S. Highway Research Board. Bulletin 71, 1953, p. 118. [Factors influencing ice segregation in soils.]Google Scholar
Hasted, J. B. Etude des molécules d’eau par les radiofréquences. Journal de Chimie Physique, Tom. 50, Nos. 7–8, 1953, p. C35C39. [Review of the dielectric properties of water and ice. Also published as Colloque International du Centre National de la Recherche Scientifique, No. 53, 1953, p. C35–C39.]Google Scholar
Heuberger, J.–C. Glaciologie. Groenland. Vol. 1: forages sur l’inlandsis. Paris, Hermann, 1954. 68 p. (Actualités scientifiques et industrielles, 1214. Expéditions Polaires Françaises [travaux], 5.) [Drilling technique, specific gravity, temperature and electrical measurements. English and German summaries.]Google Scholar
Heusser, C. J. Nunatak flora of the Juneau Ice Field, Alaska. Bulletin of the Torrey Botanical Club, Vol. 81, No. 3, 1954, p. 23650. [Flora listed. No conclusive evidence that areas remained unglaciated during Mankato glaciation.]Google Scholar
Heybrock, W. Eiszeitliche Gletscherspuren und heutige Schneeverhältnisse im Zentralgebiet des Hohen Atlas. Zeitschrift für Gletscherkunde und Glazialgeologie, Bd. 2, Ht. 2, 1953, p. 31720. [Pleistocene glaciers and present snow conditions in the Atlas mountains.]Google Scholar
Hoinkes, H. Über glazial–meteorologische Arbeiten im Sommer 1952. Anzeiger der Österreichische Akademie der Wissenschaften. Mathernatisch-naturwissenschaftliche Klasse, Jahrg. 91, Nr. 15, 1954, p. 21925. [Continuation of programme on radiation, ablation, wind and heat balance on the Vernagtferner (Otztaler Alps).]Google Scholar
Huetz de Lemps, A. Le relief de la Nouvelle-Zélande. Revue de Géographie Alpine, Tom 43, Fasc. 1, 1955 p. 596. [Geomorphological study including glaciation and glacierization.]Google Scholar
Humbel, F., and others. Le comportement diélectrique et les modules d’élasticité de monocristaux de glace, par F. Humbel, F. Jona et P. Scherrer. Journal de Chimie Physique, Tom 50, Nos. 7–8, 1953, p. C40C43. [Growth of large single crystals of ice and the determination of the dielectric and elastic constants. Also published as Colloque International du Centre National de la Recherche Scientifique, No. 53, 1953, p. C40–C431Google Scholar
Johnsson, G. Deglaciation of the highland of south Sweden; some aspects. Kungl. Fysiografiska Sällskapets i Lund Handlingar, N.F., Bd. 63, Nr. 7, 1952, 14 p. [Also published as Lunds Universitets Arsskrift, N.F., Avd. 2, Bd. 48, Nr. 7, 1952, and as Lund Studies in Geography, Ser. A, No. 3, 5952, p. 1–13.]Google Scholar
King, C. A. M. The University of Nottingham South-East Iceland Expedition, 1953. Part 3. Geomorphological and glaciological observations made in north-west Uraefi. Weather, Vol. 9, No. 52, 1954, p. 37479 CrossRefGoogle Scholar
King, R. F. Tabor, D. The strength properties and frictional behaviour of brittle solids. Proceedings of the Royal Society of London, Ser. A, Vol. 223, No. 1153, 1954 p. 22538. [Includes results for the shear strength of ice measured from friction grooves.]Google Scholar
Kirshenbaum, I. Physical properties and analysis of heavy water, edited by Urey, H. C. Murphy, G. M.. New York, McGraw-Hill, 1951. xvi, 438 p. [Includes chapters on the physical properties of D2O, isotopic analysis of water, and the natural abundance of hydrogen and oxygen isotopes. Bibliography.]Google Scholar
Kobayashi, T. Studies on small ice crystals. I. The ice crystals of rectangular plane form. Contributions from the Institute of Low Temperature Science, No. 5, 1954, p. 15. [Rectangular crystals apparently belonging to the cubic system in artificially precipitated snow.]Google Scholar
Kobayashi, T. Studies on small ice crystals. II. On the ice crystals formed on hydrophobic substances; a general survey. Contributions from the Institute of Low Temperature Science, No. 6, 1954, p. 718.Google Scholar
Kurtyka, J. C. Precipitation measurements study. Urbana, Illinois, Department of Registration and Education, State Water Survey Division, 1953. viii, 178 p. (Report of investigation no. 20.) [Review of past and present methods and instruments for measuring rain and snow. Well illustrated. Bibliography.]Google Scholar
Lecomte, J. Le spectre infrarouge et l’étude de l’eau dans les solides; 1: Introduction générale et position de la question. Journal de Chimie Physique, Tom. 50, No. 9, 1953, p. C53C64. [Review of work on infra-red absorption in ice, water and steam. Also published as Colloque International du Centre National de la Recherche Scientifique, No. 53, 1953 p. C53–C64]Google Scholar
Lecomte, J., and others. Dosage isotopique de l’eau par mesure d’absorption dans l’infrarouge, par J. Lecomte, M. Ceccaldi et E. Roth. Journal de Physique et le Radium, Sér. 8, Tom 15, No. 6, 1954, p. 54344. [A method of determining the D2O content of water by infrared absorption measurements.]Google Scholar
Liljequist, G. H. Radiation, and wind and temperature profiles over an antarctic snow-field-a preliminary note. Proceedings of the Toronto Meteorological Conference 1953. London, Royal Meteorological Society, 1954, p. 7887.Google Scholar
Lister, H. Report on glaciology at Breidamerkuryikull 1951. Jökull, Ár 3, 1953, p. 2331. [Investigations by Durham University Expedition to Iceland, 1951. Effect of rock debris on ablation.]Google Scholar
Lombard, A. Observations sur la morphologie du massif du Mt. Everest. Bulletin de l’Académie Royale de Belgique (Classe des Sciences), 5e Sér., Tom 40, 1954, p. 32031. [Brief description of geomorphology of Mt. Everest and its glaciers.]Google Scholar
Lougee, R. J. The role of upwarping in the post-glacial history of Canada. Revue Canadienne de Géographie, Vol. 7, No. 1–2, 1953, p. 314; Vol. 8, No. 1–2, 1954, p. 3–52. [Retreat of ice associated with glacial Lake Madawaska.]Google Scholar
McCall, J. G. Glacier tunnelling and related observations. Polar Record, Vol. 7, No. 48, 1954 p. 12036. [Methods used on Vesl-Skautbreen, Jotunheimen, Norway, 1951 and 1952.]Google Scholar
Mackay, J. R. Fissures and mud circles on Cornwallis Island, N.W.T. Canadian Geographer, No. 3, 1953, p. 3137. [Patterned ground; large fissures, forming outlines of polygons. Mud circles also occur on raised beaches.]Google Scholar
Manley, G. A climatological study of the retreat of the Laurentide Ice Sheet. American Journal of Science, Vol. 253, No. 5, 1955, p. 25673. [Estimation of climatic conditions since the Wisconsin maximum.]Google Scholar
Mason, B. J. On the generation of charge associated with graupel formation in thunderstorms. Quarterly Journal of the Royal Meteorological Society, Vol. 79, No. 342, 1953, p. 50109. [Theory of thunderstorm electricity based on charge developed by rime deposit.]Google Scholar
Mason, B. J. McDonald, J. E. Homogeneous nucleation of supercooled droplets. Journal of Meteorology, Vol. 11, No. 6, 1954, p. 5 1416. [Criticism by Mason of paper by McDonald, ibid, Vol. Io, No. 6, 1953, p. 416–33, with reply by McDonald.]Google Scholar
Mathieu, J.-P. L’effet Raman dans les cristaux hydratés. Journal de Chimie Physique, Tom. 50, No. 9, 1953, p. C79C88. [Experiments on the Raman spectrum of ice and of hydrated salts. Also published as Colloque International du Centre National de la Recherche Scientifique, No. 53, 1953, p. C79–C88.]CrossRefGoogle Scholar
Matznetter, J. Über die Lawinentätigkeit an der Arlbergbahn. Wetter und Leben, Jahrg. 6, Ht. 1–2, 1954, p. 2125. [Report of experience of avalanches on the Arlberg railway since 1888.]Google Scholar
Meier, M. F., and others. Preliminary data from Saskatchewan Glacier, Alberta, Canada, by M. F. Meier G. P. Rigsby R. P. Sharp. Arctic, Vol. 7, No. 1, 1954, p. 326. [Results of comprehensive field studies in summer 1952 and 1953.]Google Scholar
Miller, R., and others. Stone stripes and other surface features of Tinto Hill, by R. Miller R. Common and R. W. Galloway. Geographical Journal, Vol. 120, Pt. 2, 1954, p. 21619. [Stone stripes of Tinto Hill, upper Lanarkshire, attributed to frost heaving and water drainage.]Google Scholar
Milthers, K. Er Grenland stadig midt i en istid? Grgnland, Ht. 5, [1953], p. 16166. [Occurrence of ice ages and significance of Greenland ice.]Google Scholar
Milthers, K. Inlandsisens oprindelse. Gritnland, Ht. 6, [1953], p. 22530. [Origins of Greenland ice sheet.] MILTHERS, K. Inlandsisens “produktion”. Grtsnland, Ht. 9, [1953], p. 343–47. [Melting, melt water streams, icebergs from Greenland ice sheet.]Google Scholar
Möller, F. Zur Erklärung des Eisblinks. Polarforschung, Bd. 3, Jahrg. 23, Ht. 1–2, 1943, p. 236. [Explanation of ice-blink.]Google Scholar
Mossop, S. C. Bigg, E. K. The freezing of cloud droplets. Quarterly Journal of the Royal Meteorological Society, Vol. 80, No. 345, 1954, p. 45557. [Comments on Bigg’s work, with reply by Bigg and some new measurements.]Google Scholar
Nichols, R. L. Geomorphology of Marguerite Bay, Palmer Peninsula, Antarctica ; compiled by Ronne Antarctic Research Expedition under contract with Geophysics Branch, Earth Sciences Division.… Washington, D.C., Office of Naval Research, [1953]. vi, 151 p. 26 cm. (Ronne Antarctic Research Expedition. Technical Report No. 12.)Google Scholar
Nielsen, L. E. Regimen and flow of ice in equilibrium glaciers. Bulletin of the Geological Society of America, Vol. 66, No. 1, 1935, p. 18. [Theory of the equilibrium of a stationary glacier.]Google Scholar
Noth, H. Vom Schneefall bei Temperaturen über null Grad. Zeitschrift für Meteorologie, Bd. 8, Ht. 6, 1954, p. 18283. [Snow flakes do not melt in unsaturated air just above 0° C. because of the hypsometric effect.]Google Scholar
Nusser, F. Die Eisverhältnisse des südlichen Atlantischen Ozeans. (In Handbuch des Atlantischen Ozeans. Hamburg, Deutsches Hydrographisches Institut, Bd. 2, 1954, p. 4247.) [Ice conditions in the South Atlantic; maps.]Google Scholar
Okko, V. Periglasiaalisesta morfologiasta Suomessa. Terra, Årg. 66, No. 2, 1954, p. 5457. [Periglacial morphology in Finland. “Palsa-bogs”, solifluction phenomena, fossil dunes, and their distribution. English summary.]Google Scholar
Olyunin, V. N. K istorii oledeneniya yugo–vostoka gornoy chasti Kabardinskoy ASSR [On the history of the glaciation of the south-east of the mountainous part of Kabardinskaya A.S.S.R.]. Trudy Instituta Geografli [Transactions of the Institute of Geography], Tom 58, 1953, p. 90178. [Fluctuations of several glaciers in this part of Caucasus.]Google Scholar
Oouchi, K. A study of the freezing process of supercooled water. Journal of the Meteorological Society of Japan, Ser. 2, Vol. 32, No. 5–6, 1954, p. 11928. [In Japanese with English summary. Theory of freezing of a supercooled drop.]Google Scholar
Oulianoff, N. Ecroulements de glaces et avalanches de neige. Bulletin des Laboratoires de Géologie, Minéralogie, Géophysique et du Musée Géologique de l’Université de Lausanne, No. 110, 1954, 7 p. [Retreat of glaciers favours the release of more ice avalanches.]Google Scholar
Owston, P. G. La position des atomes d’hydrogène dans la glace. Journal de Chimie Physique, Tom. 50, Nos. 7–8, 1953, p. C13C18. [Discussion of the structure of ice. Also published as Colloque International du Centre National de la Recherche Scientifique, No. 53, 1953, p. C13–C18.]Google Scholar
Péwé, T. L. The geological approach to dating archaeological sites. American Antiquity, Vol. 20, No. 1, 1954, p. 5161. [Includes sections on pollen analysis, glacial deposits, and frost action, and connects archaeological and Quaternary investigation.]Google Scholar
Picca, R. Etudes sur la surfusion de gouttelettes d’eau. Bulletin de l’Observatoire du Puy de Dôme, 1954, No. 2, p. 3342. [Experiments on the supercooling of droplets on spiders’ webs.]Google Scholar
Pople, J. A. The electronic structure and polarity of the water molecule. Journal of Chemical Physics, Vol. 21, No. 12, 1953, p. 223435. [Calculation of the dipole moment of the H2O molecule.]Google Scholar
Pound, G. M., and others. Critical supercooling of pure water droplets by a new microscopic technique, [by] G. M. Pound L. A. Madonna S. L. Peake. Journal of Colloid Science, Vol. 8, No. 2, 1953, p. 18793. [Critical supercooling measured for droplets of 10–15μ diameter to be —40±2°C.]Google Scholar
Rathjens, C. Das Schlernstadium und der Klimaablauf der Späteiszeit im nordlichen Alpenraum. Eiszeitalter und Gegenwart, Bd. 4/5, 1954, p. 18188. [Evolution of climate in the late glacial period in the northern Alps.]Google Scholar
Rau, W. Nachweis der allgemeinen Gültigkeit des Gefrierkernspektrums. Geofisica Pura e Applicata, Vol. 26, 1953, p. 7587. [The freezing point of water drops has same distribution for water of all origins.]Google Scholar
Rau, W. Die Unterkuhlbarkeit wässeriger Lösungen und ihre Bedeutung für die atmosphärische Eisbildung. Zeitschrift für Naturforschung, Bd. 9a, Ht. 11, 1954, p. 93944. [NaC1 and other solutes depress the temperature to which water will supercool.]Google Scholar
Rommel, C. Les dommages causés en Suisse par les avalanches et leur indemnisation. Revue pour l’Étude des Calamités, Tom. 13, No. 30–31, 1952–53 p. 8188. [Translation from Schweizerischer Versicherungs-Kurier, No. 1, 1952, p. 3–12; also published in La Réassurance, Tom 35, Nos. 410–11, 1952. Statistics of damage done by avalanches in Switzerland, 16–20 January 1951, insurance coverage, action taken by federal government, and problems involved in avalanche insurance.]Google Scholar
Rouch, J. Les îles flottantes. Archiv für Meteorologie, Geophysik und Bioklimatologie, Ser. A, Bd. 7, 1954, p. 52832. [General discussion of floating “islands” of all sorts, including icebergs, “ice islands”, etc., and their use in oceanography and ecology.]Google Scholar
Rudberg, S. Västerbottens berggrundsmorfologi: ett försök till rekonstruktion av preglaciala erosionsgenerationer i Sverige. Geographica, No. 25, 1954, 457 p. [Geomorphology of Västerbottens län, north Sweden; attempt at reconstruction of cycles of preglacial erosion in Sweden. Review of theories on geomorphology of Sweden. English summary, p. 413–29.]Google Scholar
Rundle, R. E. The deuterium effect on hydrogen bond distances in crystals. Journal of Chemical Physics, Vol. 21, No. 5, 1953, p. 93738. [Evidence from Megaw’s data on ice supports Nordman and Lipscomb’s theory of this effect.]Google Scholar
Ryder, T. Compilation and study of ice thicknesses in the northern hemisphere, 1952–53. New York, American Geographical Society, [1954?]. 3 vols. [in 2]. [Mimeographed. Data on thickness of river and lake ice at 53 places in North America. Bibliography.]Google Scholar
Sager, R. C. Aerial photoanalysis of permanently frozen ground. Canadian Surveyor, Vol. Ix, No. 5, 1954, p. 31115. [Chief characteristics.]Google Scholar
Sanuki, M., and others. The final test of the anti-freezing combination wind vane and anenometer on the summit of Mt. Fuji, by M. Sanuki, S. Kimura and S. Toyama. Papers in Meteorology and Geophysics, Vol. 5, No. 2, 1954, p. 18285. [Apparatus with electrical heater works satisfactorily down to —12.7° C.]Google Scholar
Schell, I. I. Arctic ice and weather relationships. Quarterly Journal of the Royal Meteorological Society, Vol. 81, No. 347,1955, p. 9697. [Comment on relation between North Atlantic arctic ice and weather in north Europe.]Google Scholar
Schenk, E. Solifluktion. Zeitschrift der Deutschen Geologischen Gesellschaft, Bd. 105, Teil 2, 1953 [pub. 1954], p. 197202. [Description and theory of solifluction.]Google Scholar
Shidei, T. Studies on the damages on forest tree [sic] by snow pressures. Bulletin of the Government Forest Experiment Station (Tokyo), No. 73, 1954, p. I89. [Nature of damage under different conditions and measures of avoidance. English summary, p. 83–891Google Scholar
Shimada, H. Electrical resistance of snow [Sekisetsu no denki teikō]. U.S. Snow, Ice and Permafrost Research Establishment. Translation 31, 1954, 4 p. [Measurement of electrical resistance between two electrodes immersed in snow. Translation of article in Seppyō, Vol. 3, 1941, p. 503–06.]Google Scholar
Simpson, F. A. New Zealand Antarctica. New Zealand Geographer, Vol. 10, No. 1, 1954, p. 124. [Includes brief notes on ice shelves, ice cap and glaciations.]Google Scholar
[Snow Cover: Northern Hemisphere.] Depth of snow cover in the northern hemsiphere. Boston, Mass., Arctic Construction and Frost Effects Laboratory, Corps of Engineers, U.S. Army, 1954. [ii, 18] leaves, 38 plates. (Investigation of construction and maintenance of aerodromes on ice, fiscal year 1954.) [Includes maps, graphs and tables analysing snow cover data for some 511 stations. Covers a period of twenty years or less.]Google Scholar
[Snow Surveys.] Snow survey of Great Britain, season 1953–54. Meteorological Magazine, Vol. 83, No. 990, 1954, P 35359. [Report.]Google Scholar
Steinbach, A. Beobachtungen und Messungen an Eishöhlen im Westerwald und in der Eifel. Jahrbücher des Nassauischen Vereinsfür Naturkunde, Bd. 91, 1954, p. 836. [Ice caves in the mountains of the Westerwald and the Eifel described. Microclimatological studies reported.]Google Scholar
Stock, C. S. d’Este. The figure skate. Folkestone, privately printed, 1954. 32 p. [Tests of experimental skates of varying shapes.]Google Scholar
Sweeting, M. M. Recent trends of glacier fluctuations in the North Atlantic area, Nature, Vol. 175, No, 4448, 1955, p. 18890. [Report of meeting of British Glaciological Society at Oxford, 19 November 1954. Speakers: C. W. M. Swithinbank, C. A. M. King, M. M. Sweeting, M. F. W. Holland, H. Lister, and G. Manley.]Google Scholar
Swithinbank, C. W. M. Ice shelves. Geographical Journal, Vol. 121, Pt. 1, 1955, p. 6476. [Morphology, regime and movement of ice shelves of western Dronning Maud Land.]Google Scholar
Thomas, M. K. Climatological atlas of Canada; a joint publication of the Division of Building Research, National Research Council, and the Meteorological Division, Department of Transport, Canada. Ottawa, National Research Council, 1953. 256 p. (N.R.C. no. 3551. D.B.R. no. 41.) [Includes charts of snowfall, snow cover and limit of permafrost.]Google Scholar
Thorarinsson, S. The Grimsvötn expedition June–July 1953: travel account and report of scientific results. Jökull, Ár 3, 1953, p. 622.Google Scholar
Thorarinsson, S. Anchored stone polygons at low levels within the Iceland basalt regions . Jökull, Ár 3, 1953, p. 3738.Google Scholar
Thorarinsson, S. Svigdur á Svinafellsjökli i Orwfum. Jökull, Ár 3, 1953, p. 3940. [Chevrons (Forbes bands) on Svinafellsjökull, Iceland. English summary.]Google Scholar
Thornbury, W. D. Principles of geomorphology. New York, John Wiley; London, Chapman and Hall, 1954. ix, 618 p. 23 cm. 64s. [Chapters on types and characteristics of glaciers; mountain glaciation; ice caps and their topographic effects. Reviewed by G. Manley in Nature, Vol. 175, No. 4449, 1955, p. 226–27.]Google Scholar
Timashev, Ye. V. Otstupaniye kontsa lednika Devlokhan za 35 let [Retreat of Devlokhan glacier over 35 years]. Izvestiya Vsesoyuznogo Geograficheskogo Obshchestva [News of the All-Union Geographical Society], Tom 86, No. 1, 1954, p. 9395. [Measurements of glacier in Pamirs, 1913–48.]Google Scholar
Todtmann, E. M. Am Rand des Eyjabakkagletschers, Sommer 1953. Jökull, Ár 3, 1953, p. 3437. [Investigations on periphery of Eyjabakkajökull, Iceland.]Google Scholar
Tryggvason, E. Lambárdalsjökull: jökulis under grjdturd. Jökull, Ár 3, 1953, p. 4344. [Lambárdalsjökull, Iceland; glacier buried under scree.]Google Scholar
Walsh, A. D. The electronic orbitals, shapes and spectra of polyatomic molecules; 1 : AH2 molecules. Journal of the Chemical Society, 1953, Part 3, August, p. 226066. [Theory of shape and spectra of molecules such as H2O.]Google Scholar
Wiche, K. Pleistozäne Klimazeugen in den Alpen und im Hohen Atlas. Mitteilungen der Geographischen Gesellschaft Wien, Bd. 95, Ht. 7–52, 1953, p. 14360. [A morphological comparison with reference to climatic differences between two mountain systems in the Ice Age.]Google Scholar
Winchester, J. W. A study of the movement of arctic sea ice in the Canadian Arctic in relation to meteorological, geographical and oceanographic parameters. Bulletin of the American Meteorological Society, Vol. 35, No. 9, 1954, p. 41727. [Examples of wind and tide affecting sea ice movement.]Google Scholar
Woldstedt, P Die Klimakurve des Tertiärs und Quartärs in Mitteleuropa. Eiszeitalter und Gegenwart, Bd. 4/5, 1954, p. 59. [Large temperature fluctuations in central Europe during the Ice Age due to increase in continental height and fluctuation of solar energy.]Google Scholar
Woldstedt, P. Saaleeiszeit, Warthestadium und Weichseleiszeit in Norddeutschland. Eiszeitalter und Gegenwart, Bd. 4/5, 1954, p. 3448. [Climatic conditions and extent of ice during the Saale and Weichsel advances and the interglacial period.]Google Scholar
Wordie, J. M. Ice in Greenland. Geographical Magazine, Vol. 29, No. 12, 1955, p. 61320. [Glaciers and icebergs in Greenland.]Google Scholar
Yosida, Z. Iwai, H. Measurement of the thermal conductivity of snow cover [Sekisetsu no netsu dendo-ritsu no sokutei]. U.S. Snow, Ice and Permafrost Research Establishment. Translation 30, 1954, 7 p. [Method and results. Translation of article in Seppyō, Vol. 8, 1946, p. 48–531Google Scholar
Young, R. A. Some notes on the formation of medial moraines. Jökull, Ár 3, 1953, p. 3233. [Illustrated by examples from Breidamerkurjökull, Iceland.]CrossRefGoogle Scholar
Zeuner, F. E. Riss or Würm? Eiszeitalter und Gegenwart, Bd. 4/5, 1954, p. 98105. [Author’s view of what should be regarded as “Riss” and what as “Würm” in the Alpine area.]Google Scholar
[Zeuner, F. E., and others.] Changes in world glaciation. Observatory, Vol. 74, No. 881, 1954, p. 14448. [Report of discussion at joint meeting of Royal Astronomical Society and British Glaciological Society. Chairman: G. Seligman. Speakers: F. E. Zeuner, J. D. H. Wiseman, G. Manley and F. Hoyle.]Google Scholar