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Glaciological Literature

Published online by Cambridge University Press:  30 January 2017

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Journal of Glaciology , Volume 2 , Issue 16 , 1954 , pp. 445 - 448
Copyright
Copyright © International Glaciological Society 1954

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

Arakawa, K. Higuchi, K. Studies on the freezing of water. (I.) Journal of the Faculty of Science, Hokkaido University, Ser. 2, Vol. 4, No. 3, 1952, p. 201–08. [Growth of stellar crystals from disc crystals.]Google Scholar
Auty, R. P. Cole, R. H. Dielectric properties of ice and solid D2O. Journal of Chemical Physics, Vol. 20, No. 8, 1952, p. 1309 –14. [Complex dielectric constants measured from melting point to –65° C. (H2O) and –35° C. (D2O).]Google Scholar
Avery, E. C. Grossweiner, L. I. Thermoluminescence of ice. Journal of Chemical Physics, Vol. 21, No. 2, 1953,. p. 372–73. [Ice, irradiated with X-rays at –183° C., glows when subsequently warmed.]Google Scholar
Bader, H., and others. Preliminary investigations of some physical properties of snow, by Bader, H. Hansen, B. L. Joseph, J. A. Sandgren, M. A.. U.S. S[now,] I [ce and] P[ermafrost] R[esearch] E[stablishment]. Report 7, 1951, viii, 48 p. [+14 sheets diagrs.] [Mechanics of snow compaction; description of instruments for its investigation.]Google Scholar
Barrére, P. Équilibre glaciaire actuel et quaternaire dans louest des Pyrénées centrales. Revue Géographique des Pyrénées et du Sud-Ouest, Tome 24, Fasc. 2, 1953, p. 116–34.Google Scholar
Berg, H. Temperaturmessungen in der schneenahen Luftschicht. Wetter und Leben, Jahrg. 5, Ht. 1/2, 1953, p. 34–35. [Temperature of air layer above snow.]Google Scholar
Berger, C. Saffer, C. M. Jr. The existence of “beta” ice. Science, Vol. 118, No. 3070, 1953, p. 52–22. [Seljakov’s report of rhombohedral ice formed by freezing supercooled water at ordinary pressure almost certainly fallacious.]Google Scholar
Biays, P. Les îles de glace arctiques. Annales de Géographie, 62 An., No. 333, 1953, p. 377–80. [Form, origin, movement.]CrossRefGoogle Scholar
Bigg, E. K. The supercooling of water. Proceedings of the Physical Society of London, Series B, Vol. 66, No. 404, 1953, p. 688–94. [Drops suspended at the interface of two insoluble liquids were used to find dependence of supercooling on volume and cooling rate.]Google Scholar
Blue, R. W. The librational heat capacity of ice and of heavy ice. Journal of Chemical Physics, Vol. 22, No. 2, 1954, p. 280–83. [Heat capacity of ice can be split into translational and rotational parts by studying the difference in heavy ice.]CrossRefGoogle Scholar
Bossolasco, M. Sulla micrometeorologia del manto nevoso. Geofisica e Meteorologia, Vol. 2, No. 1/2, 1954, p. 1–2. [Micro-climate of the snow cover.]Google Scholar
Bout, P. Études de géomorphologie dynamique en Islande. Paris, Hermann, 1953 219 p. (Actualités scientifiques et industrielles, 1197. Expéditions Polaires Françaises [travaux], III.) [Includes chapters on soil polygons and periglacial erosion.]Google Scholar
Brunner, T. Einige Beobachtungen über das Haften von Eis an Oberflächen. Zeitschrift für angewandte Mathematik und Physik, Vol. 3, Fasc. 6, 1952, p. 460–66. [Shear tests on adhesion of ice to clean and greased surfaces.]Google Scholar
Cailleux, A. Taylor, G. Cryopédologie:étude des sols gélés. Paris, Hermann, 1954 220 p. (Actualités scientifiques et industrielles, 1203. Expéditions Polaires Françaises [travaux], IV.) [Physical mechanisms; true soils; superficial formations; practical applications. Bibliography.]Google Scholar
Capello, C. Gli apparati morenici di diversione. Bollettino del Comitato Glaciologico Italiano, 2 Ser., No. 3, 1952, p. 25–44. [Effect of morainic obstructions on flow of the Macunaga and Miage glaciers.]Google Scholar
Chalmers, J. A. Electric charges from ice friction. Journal of Atmospheric and Terrestrial Physics, Vol. 2, No. 6, 1952, p. 337–39. [Experiments showing that when ice is rubbed the large fragments carry a negative charge.]CrossRefGoogle Scholar
Cumming, W. A. The dielectric properties of ice and snow at 32 cm. Journal of Applied Physics, Vol. 23, No. 7, 1952, p. 768–72. [Data of use in studying radar echoes from snow-covered terrain and snowstorms.]Google Scholar
Dessens, H. Sur la microstructure et la précipitation artificielle dun brouillard surfondu. Comptes Rendus Hebdomadaires des Séances de l’Académie des Sciences, Tome 235, No. 25, 1952, p. 1675–78. [Examination of a supercooled town fog with ultramicroscope showed presence of rare, asymmetric ice crystals.]Google Scholar
Diamond, M. Lowry, W. P. Correlation of density of new snow with 700 mb temperature. U.S. Snow, Ice and Permafrost Research Establishment. Research Paper 1, 1953, 3 p.Google Scholar
Dibner, V. D. Nekotoryye osobennosti zamerzaniya rek i ozer v zapolyarye [Some features of the freezing of rivers and lakes in the polar regions]. Priroda [Nature] (Moscow), 1953, No. 10, p. 119–20. [Characteristics of new freshwater ice.]Google Scholar
Dreimanis, A. Studies of friction cracks along shores of Cirrus Lake and Kasakokwog Lake, Ontario. American, Journal of Science, Vol. 251, No. 11, 1953, p. 769–83. [Friction cracks do not always dip in direction of ice flow.]Google Scholar
Epstein, S. Mayeda, T. Variation of O18 content of waters from natural sources. Geochimica et Cosmochimica Acta, Vol. 4, No. 5, 1953, p 213–24. [Low O18:O16 ratios obtained from marine waters contaminated with melt water from ice fields.]Google Scholar
Finsterwalder, R. Die zahlenmässige Erfassung des Gletscherrückgangs an Ostalpengletschem. Zeitschrift für Gletscherkunde und Glazialgeologie, Bd. 2, Ht. 2, 1953, p. 189–239. [Data on glacier retreat for eight glaciers in the Eastern Alps.]Google Scholar
Flohn, H. Studien über die atmosphärische Zirkulation in der letzten Eiszeit. Erdkunde, Bd. 7, Ht. 4, 1953, p. 266–75 [Climate during last glacial period and speculation on cause of ice ages.]CrossRefGoogle Scholar
Friedman, I. Deuterium content of natural waters and other substances. Geochimica et Cosmochimica Acta, Vol. 4, Nos. 1/2, 1953, p. 89–103. [Accurate method using a mass spectrometer. Includes results in Bering Sea and off coast of Greenland.]Google Scholar
Friedrich, W. Die Ursachen der Lawinenkatastrophen im Jänner 1951. Anzeiger der Österreichischen Akademie der Wissenschaften. Mathematisch-naturwissenschaftliche Klasse, Jahrg. 88, Nr. 6, 1951, p. 117–25. [Analysis of the causes of the Austrian avalanches, January 1951.]Google Scholar
Friedrich, W. Schneerollen. Wetter und Leben, Jahrg. 5, Ht. 1/2, 1953, p. 82–83. [“Snow rollers.”)Google Scholar
Fuchs, Alfred. Die Scherfestigkeit von Schnee und Eis in Abhängigkeit von der Temperatur. Veröffentlichungen des Museum Ferdinandeum (Innsbruck), Bd. 26/29, Jahrg. 1946/49,[pub.] 1949, p. 101–05. [Shear strength of snow and ice in relation to temperature.]Google Scholar
Fuchs, Alfred. Raümliche Abbildungen von Schneegefügen als Dauerpräparate. Zeitschrift für Gletscherkunde und Glazialgeologie, Bd. 2, Ht. 2, 1953, p. 299–301. [New method of making permanent snow replicas.]Google Scholar
Fuchs, Alfred. Über eine Verbesserung des Rotations-Zerreissapparates für Schneeproben. Zeitschrift für Gletscherkunde und Glazialgeologie, Bd. 2, Ht. 2, 1953, p. 302–03. [Improved “tearing” apparatus for testing strength of snow samples.]Google Scholar
Garcia-sáinz, L. Los glaciares cuaternarios de la Sierra de la Estrella. Boletim da Sociedade de Geografia de Lisboa, Sér. 71, Nos. 4–6, 1953, p. 170–71. [Reconstruction of Quaternary glaciers on the Sierra de Estrella (Portugal).]Google Scholar
Garrigue, H. Observations sur les impuretés dans lair libre. Comptes Rendus Hebdomadaires des Séances de l’Académie des Sciences, Tome 236, No. 24, 1953, p. 2309 –11. [Radioactivity in snow probably of distant origin, e.g. atomic bombs; the dust and soot are of local origin.]Google Scholar
Gill, E. W. B. Electrification by freezing. British Journal of Applied Physics. Supplement No. 2, 1953, p. S16–S19. [Potentials of order 100 volts found when ice formed from dilute solutions. A theory is suggested.]Google Scholar
Gourley, Mary G. Crozier, W. D. Persistent residues from ice particles. Physical Review, Ser. 2, Vol. 92, No. 2, 1953, p. 526. [Ice particles formed and evaporated at –75° C. leave residue capable of nucleating further ice particles.]Google Scholar
Grunow, J. Kritische Nebelfroststudien: nach Beobachtungen auf dem Hohenpeissenberg. Archiv für Meteorologie, Geophysik und Bioklimatologie, Ser. B, Bd. 4, Ht. 4, 1953, p. 389–419. [Fog deposit, frequency of occurrence and meteorological conditions.]Google Scholar
Haefeli, R. Kriechprobleme im Boden, Schnee und Eis. Wasser und Energiewirtschaft, 1954, Nr. 3, 19 p. [Problems of creep in soils, snow and ice; includes sections on creep in causing avalanches, apparent viscosity and extrusion flow in glaciers.]Google Scholar
Hast, N. Observations regarding resistant surface films of crystals. Arkiv for Fysik, Bd. 4, Ht. 6, 1952, p. 535–39. [Ice from distilled water leaves surface film as a veil-like structure visible in electron microscope.]Google Scholar
Hawice, E. L. Bonacina, L. C. W. The Snow Survey of Great Britain. Quarterly Journal of the Royal Meteorological Society, Vol. 79, No. 339, 1953, p. 168–71. [Correspondence on a review of the 1949–50 and 1950–51 Snow Survey, ibid., Vol. 78, together with reply by reviewer.]Google Scholar
Heaps, H. S. An analysis of downpunching. Transactions of the Royal Society of Canada, Third Ser., Vol. 47, Section 4, 1953, p. 17–21. [Mathematical discussion of stress pattern in crust of the Earth due to surface load of an ice sheet.]Google Scholar
Heinsheimer, G. J. Schwund der Staubschichten in einem Gletscher; nach Beobachtungen am Glaciar Derecho in der Cordillera von San Juan (Argentinien). Zeitschrift für Gletscherkunde und Glazialgeologie, ***Bd. z, Ht. z, 1953, p. 183–88. [Suggests mechanism by which one side of the glacier is dirt-laden, other side dirt-free.]Google Scholar
Helk, J. V. Dunbar, Moira. Ice islands: evidence from north Greenland. Arctic, Vol. 6, No. 4, 1953, p. 263–71. [Photographs of only areas in north Greenland where ice of this nature is found.]Google Scholar
Heusser, C. J. Palynology of the Taku Glacier snow cover, Alaska, and its significance in the determination of glacier regimen. American Journal of Science, Vol. 252, No. 5, 1954, p. 291–308. [Investigation of the pollen and spore stratigraphy of the glacier as a help in determining its regime.]Google Scholar
Heusser, C. J., and others. Geobotanical studies on the Taku Glacier anomaly, by Heusser, C. J. Schuster, R. L. Gilkey, A. K.. Geographical Review, Vol. 44, No. 2, 1954, p. 224–39. [Botanical evidence on why this glacier is advancing.]Google Scholar
Higucm, K. A method for observation of falling snow particles. Journal of the Meteorological Society of Japan, Ser. 2, Vol. 32, No. 3, 1954, p. 19–24. [Shadow photography of snow crystals to obtain shape, size and mass.]Google Scholar
Hoinkes, H. Wärmeumsatz und Ablation auf Alpengletschem. II. Hornkees (Zillertaler Alpen), September 1951. Geografiska Annaler, Arg. 35, Ht. 2, 1953, p. 116–40. [Studies of ablation on alpine glaciers, 1950–51]Google Scholar
Hoinkes, H. Zur Frage der Schutzbänder auf den Gletscherzungen. Zeitschrift für Gletscherkunde und Glazialgeologie, Bd. 2, Ht. 2, 1953 p. 177–84. [Suggests cause of non-sedimentary “dirt-bands” (ogives) to be as proposed by Tyndall.]Google Scholar
Hoinkes, H. Zur Mikrometeorologie der eisnahen Luftschicht. Wetter und Leben, Jahrg. 5, Ht. 1/2, 1953, p. 33–34. [Micrometeorology of air layer above ice.]Google Scholar
Hoppe, G. Nägra iakttagelser vid isländska jöklar sommaren 1952. Ymer, Arg. 73, Ht. 4, 1953, p. 241–65. [Observations of 12 of Vatnajökull’s lobes and tongues. Superficial moraines uncommon on Icelandic glaciers. English summary.]Google Scholar
Hoppe, G. Schytt, V. Some observations on fluted moraine surfaces. Geografiska Annaler, Arg. 35, Ht. 2, 1953, p. 105–15. [Ground moraine surfaces recently exposed by retreating ice are often strikingly “fluted”, the ridges consisting of fine material.]Google Scholar
Howell, W. E. Some measurements of ablation, melting and solar absorption on a glacief in Peru. Transactions. American Geophysical Union, Vol. 34, No. 6, 1953, p. 883–88.Google Scholar
Humbel, F., and others. Anisotropie der Dielektrizitätskonstante des Eises, von F. Humbel, F. Jona und P. Scherrer. Helvetica Physica Acta, Vol. 26, Fasc. 1, 1953, p. 17–32. [Measurement of the dielectric constant of ice for various orientations of a single crystal at temperatures from –5° to –40° C.]Google Scholar
Imbert, B. Sondages séismiques en Terre Adélie: rapports scientifiques des Expéditions Polaires Françaises S. III. 2. Annales de Géophysique, Tome 9, No. 1, 1953, p. 85–92. [Results of 4 series of observations made south of Port-Martin, Dec. 1951 and Jan. 1952.]Google Scholar
Itoo, K. Mass, size and cristallizing [sic] velocity of skeleton-shaped depth hoar. Papers in Meteorology and Geophysics (Tokyo), Vol.2, No. 2, 1951, p. 189–90. [Description and growth of depth hoar.]Google Scholar
Itoo, K. Forms of ice crystals in the air: on small ice crystals (II). Papers in Meteorology and Geophysics (Tokyo), Vol. 3, No. 3, 1953, p. 207–16.Google Scholar
Itoo, K. Size, mass and some other properties of ice crystals in the air: on small ice crystals (III). Papers in Meteorology and Geophysics (Tokyo), Vol. 3, No. 4, 1953, p. 297–306.Google Scholar
Ivanov, K. YE Lavrov, V. V. Ob odnoy osobennosti mekhanizma plasticheskoy deformatsii lda [A peculiarity in the mechanism of plastic deformation of ice]. Zhurnal Tekhnicheskoy Fiziki [Journal of Technical Physics], Tom 20, Vyp. 2, 1950, p. 230–31. [Plastic deformation curve of ice is stepped, like that of some metals. English translation by J. A. Bender, U.S. S[now,] I[ce and] P[ermafrost] R[esearch] Ejstablishment]. Translation 10.]Google Scholar
Ivanovskiy, A. D. Snegovoy rezhim tsentralnoy lesostepi [Snow regime in the central forest-steppe region]. Gidrotekhnika i Melioratsiya [Hydraulic Engineering and Reclamation] (Moscow), No. 12, 1952, p. 13–22. [Effect of variation of relief and shelter-belts on snow fall, melting and runoff.]Google Scholar
Jaeger, F. Der Rückgang der Gletscher des Kilimandjaro. Zeitschrfft für Gletscherkunde und Glazialgeologie, Bd. 2, Ht. 2, 1953, p. 306–11. [Retreat of Kilimanjaro glaciers.]Google Scholar
Jobert, N. Dispersion des ondes de Rayleigh en milieu hétérogène; application au névé du Groenland. Annales de Géophysique, Tome 9, Fasc. 1, 1953, p. 28–32. [Theoretical study.]Google Scholar
Kampe, H. J. Aufm and others. The influence of temperature on the shape of ice crystals growing at water saturation, by Kampe, H. J. Aufm Weickmann, H. K. Kelly, J. J.. Journal of Meteorology, Vol. 8, No. 3, 1951, p. 168–74. [Laboratory experiments on crystals formed at various temperatures.]Google Scholar
Kampe, H. J. Aufm and others. Remarks on “Electron-microscope study of snow-crystal nuclei”, by Kampe, H. J. Aufm Weickmann, H. K. Aufm Kedesdy, H. H.. Journal of Meteorology, Vol. 9, No. 5, 1952, p. 374–75. [Criticism of paper by M. Kumai, ibid., Vol. 8, No. 3, 1951, p. 151–56, with reply by Kumai, ibid., p. 375–76.]Google Scholar
Kautsky, G. Eine von einem Gletscher gefurchte Moräne. Geologiska Föreningens i Stockholm Förhandlingar, Bd. 75, Ht. 4, 1953, p. 490–92. [Moraine furrowed by glacier.]Google Scholar
Keller, J. B. Weitz, M. Reflection and transmission coefficients for waves entering or leaving an icefield . Communications on Pure and Applied Mathematics, Vol. 6, No. 3, 1953, P- 415–17.: Equations for the reflection and transmission of water waves are derived.]Google Scholar
Klebelsberg, R. Von. Ergebnisse der Gletschermessungen des Österreichischen Alpenvereins in den Österreichischen Alpen 1951 und 5952. Zeitschrift für Gletscherkunde und Glazialgeologie, Bd. 2, Ht. 2, 1953, p. 333–43. [Detailed account of glacier fluctuation in Austrian Alps.]Google Scholar
Klebelsberg, R. Von. Die Gletscher der Österreichischen Alpen 1952–53. Mittelungen des Österreichischen Alpenvereins, Jahrg. 9 (79), Ht. 1/2, 1954, p. 5–7. [55 of the principal Austrian glaciers in retreat in 1953, 2 in advance.]Google Scholar
Kramers, H. Stemerding, S. The sublimation of ice in vacuum. Applied Scientific Research, Vol. A3, No 1, 1951, p. 73–82. [Results show gas kinetic accommodation is nearly unity from –40° to –60° C. and confirm theory.]Google Scholar
Kumai, M. Itagaki, K. Cinematographic study of ice crystal formation in water. Journal of the Faculty of Science, Hokkaidô University, Ser. 2, Vol. 4, No. 4, 1953, p. 235–46. [Disc crystals are formed at higher temperature and grow more slowly than needle crystals.]Google Scholar
Kumm, A. Über die Entstehung von elektrischen Ladungen bei Vorgängen in der kristallinen Eisphase. Archiv für Meteorologie, Geophysik und Bioklimatologie, Ser. A, Bd. 3, Ht. 5, 1951, p. 382–401. [Charges are found on crystals broken from a hoar layer.]Google Scholar
Lachapelle, E. R. Snow studies on the Juneau Ice Field. New York, American Geographical Society, 1954, 31, +1. (J.I.R.P. report no. 9.) [Experimental results of 1952 summer season; includes descriptions and methods of using instruments.]Google Scholar
Langleben, M. P. The terminal velocity of snowflakes. Quarterly Journal of the Royal Meteorological Society, Vol. 80, No. 344, 1954, p.174–81. [Photographic measurements.]Google Scholar
Lawrence, D. W. Elson, J. A. Periodicity of deglaciation in North America since the late Wisconsin maximum. Geografiskh Annaler, Arg. 35, Ht. 2, 1953, p. 83–104. [The first part on Alaskan glaciers by Lawrence, the second on late Wisconsin recession by Elson.]Google Scholar
Lied, Herta. Der Abfluss des Glogau-Baruth-Hamburger Urstromtals während des Brandenburger Stadiums der Weichsel-Eiszeit. Petermann Geographische Mitteilungen, Jahrg. 97, 2 Quartalsheft, 1953, p. 89–96. [Summer ablation amounted to 80–90% of annual ablation.]Google Scholar
Lipscomb, W. N. Residual entropy of the polar structure of ice. Journal of Chemical Physics, Vol. 22, No. 2, 1954, p. 344. [Discussion of paper by Rundle, ibid., Vol. 21, 1953, p. 1311, pointing out an error.]Google Scholar
Lliboutry, L. Les Andes de Santiago, leurs pénitents et leurs glaciers. Bulletin de la Société Scientifique du Dauphiné, Tome 69, No. 2, 1954, p. 7–11. [Description of penitentes, theory of formation, general description of glaciers near Santiago, which exhibit large advances and retreats.]Google Scholar
Lovell, C. W. jr. Herrin, M. Review of certain properties and problems of frozen ground, including permafrost. U.S. S[now,] I[ce and] P[ermafrost] R[esearch] E[stablishment]. Report 9, 19531 ×, 124 p. [Includes chapter on terminology, definition and classification.]Google Scholar
Mcdonald, J. E. Homogeneous nucleation of supercooled water drops. Journal of Meteorology, Vol. 10, No. 6, 1953, p. 416–33. [Theory of supercooling of water drops.]Google Scholar
Magono, C. On the fall velocity of snowflakes. Journal of Meteorology, Vol. 8, No. 3, 1951, p. 199–200. [Fall velocity as function of maximum diameter.]Google Scholar
Mantis, H. T., ed. Review of the properties of snow and ice, with reports by Bader, H. Benson, C. S. Bey, P. P. Doherty, R. H. Goldstein, R. J. Joseph, J. A. Rasmussen, S. W. Schiavone, D. C.. U.S. S[now,] I[ce and] P[ermafrost] R[esearch] E[stablishment]. Report 4, 1951 × 156 p. [Physical properties, chiefly mechanical; reviews, bibliographies, abstracts.]Google Scholar
Martin-chavannes, J. Les débäcles au vallon de Ferpècle. Die Alpen, 29 Jahrg., No. 1, 1953, p. 26–29. [The flood of 4 August 1952 in the valley of Ferpècle attributed to the Mont Mini glacier.]Google Scholar
Mason, B. J. Progress in cloud physics research: a progress report on recent investigations at Imperial College, London. Archiv für Meteorologie, Geophysik und Bioklimatologie, Ser. A, Bd. 6, Ht. 1, 1953, p. 1–52. [Includes review of laboratory and theoretical studies on supercooling and freezing of water and on growth of ice crystals from the vapour. Bibliography.]Google Scholar
Melcher, D. Experimentelle Untersuchung von Vereisungserscheinungen. Zeitschrift für angewandte Mathematik und Physik, Vol. 2, Fase. 6, 1951, p. 421–43; Vol. 5, Fasc. 1, 1954, p. 89. [Experiments to determine factors influencing growth of rime in laboratory and the field.]Google Scholar
Murphy, E. J. Surface migration of water molecules in ice. Journal of Chemical Physics, Vol. 21, No. 10, 1953, p. 1831–35. [Activation energy for surface migration is 52 Kcal/mole.]Google Scholar
Nakaya, U. Formation of snow crystals. U.S. Snow, Ice and Permafrost Research Establishment. Research Paper 3, 1954, 12 p. [Ice crystals form either from supercooled droplets, from seeding, or by condensation of vapour on to solid nuclei; snow crystals develop from these ice crystal “germs”.]Google Scholar
Nordnes, S. Sund, T. lsaysmeltningen pá Saltfjellet. Norsk Geografisk Tidsskrift, Bd. 54, Nr. 1–4, 1953, p. 165– 204. [Glacial geology of Saltfjellet and Nordre Bjellävatn district, north Norway. English summaries.]Google Scholar
Norinder, H. Siksna, R. Experiments concerning electrification of snow. Arkiv for Geofysik, Bd. 2, Ht. 1, Nr. 3, 1954, p. 59–89. [Experiments on the electrification of snow when it is poured, blown through a nozzle, etc.]Google Scholar
Nussbaum, F. Gygax, F. La glaciación cuaternaria en la Cordillera cantabrica. Estudios Geograficos,/Año 14, No. 51, 1953, p. 261–70.Google Scholar
Obenland, E. Obenland, Lisa. Zum Entwicklungsgang der Schneedecke. Berichte des Deutschen Wetterdienstes in der US-Zone, Bd. 7, Nr. 42, 1952, p. 186–90. [Depth of snow in relation to the weather situation.]Google Scholar
Owston, P. G. Diffuse scattering of X-rays by ice. Acta Crystallographica, Vol. 2, Pt. 4, 1949, p. 222–28. [Diffuse scattering is due to thermal vibrations, whose amplitude is 04 A at –5° C. The streaks may be due to H atom interchange.]Google Scholar
Palmer, L. S., and others. Dielectric constant of water films, by Palmer, L. S. Cunliffe, A. Hough, J. M.. Nature, Vol. 170, No. 4332, 1952, p. 796. [Dielectric constant of thin water films is more like that of ice than of the bulk liquid.]Google Scholar
Paschinger, H. Fünf Jahre Pasterzenmessungen 1947–1951. Mitteilungen des Naturwissenschaftlichen Vereines für Kärnten, Jahrg. 142, Ht. 2, 1953, p. 7–15. [Summary of annual recessions and ablation on Pasterzenkees, Eastern Alps, 1947–51–]Google Scholar
Peterson, S. W. Levy, H. A. A single crystal neutron diffraction study of heavy ice. Bulletin of the American Physical Society, Vol. 28, No. 5, 1953, p. 10. [Data in full agreement with the Pauling model of the structure of ice. Reprinted in Physical Review, Ser. 2, Vol. 92, No. 4, 1953, p. 1082.]Google Scholar
Press, F. Ewing, M. Propagation of elastic waves in a floating ice sheet. Transactions. American Geophysical Union, Vol. 32, No. 5, 1951, p. 673–78. [Derivation of characteristic equation and discussion.]Google Scholar
Press, F. Ewing, M. Theory of air-coupled flexural waves. Journal of Applied Physics, Vol. 22, No. 7, 1951, p. 892–99. [Theory of these waves in a floating ice sheet is derived for the case of an impulsive point source in either air or water.]CrossRefGoogle Scholar
Proudfoot, V. B. The glaciation of the Dingle Peninsula. Irish Geography, Vol. 3, No. 1, 1954, p. 36–38. [No evidence that an ice sheet covered the area during any stage of the local glaciations.]Google Scholar
Pugh, H. L. D. Price, W. I. J. Snow drifting and the use of snow fences. Polar Record, Vol. 7, No. 47, 1954, p. 4–23.Google Scholar
Quervain, M. De. Strength properties of a snow cover and its measurement, translated by Gottschalk, Charles M.. U.S. S[now,] I[ce and] P[ermafrost] R[esearch] E[stablishment]. Translation 9, 1951, [i], 8 leaves +2 plates. [Translated from Geofisica Pura e Applicata, Vol. 18, 1950, p. 179–91.]Google Scholar
Rasmussen, W. C. Periglacial frost-thaw basins in New Jersey. Journal of Geology, Vol. 61, No. 5, 1953, p. 473–74 [Disputes view that basins of interior drainage in Atlantic Coastal Plain of New Jersey can be entirely explained by periglacial action.]Google Scholar
Rau, W. Über den Einfluss des Tropfenvolumens auf die Unterkühlbarkeit von Wassertropfen und die Bedeutung des Gefrier spektrums. Zeitschrift für Naturforschung, Bd. 8a, Ht. 2/3, 1953, p. 197–204. [Amount of supercooling of water drops as a function of their volume.]Google Scholar
Richardson, W. E. Dirt polygons. Weather, Vol. 9, No. 4, 1954, p 117–21. [Mode of formation of snow-surface polygons on Cross Fell.]Google Scholar
Richmond, G. M. Modification of the glacial chronology of the San Juan Mountains, Colorado. Science, Vol. 119, No. 3096, 1954, p. 614–15. [Identification of tills, including some recent deposits up to 1860.]Google Scholar
Ritchie, A. S. A contribution to the geology and glaciology of the Snowy Mountains. Journal and Proceedings of the Royal Society of New South Wales, Vol. 86, Pt. 4, 1952, p. 88–93. [Glaciation and nivation in mountains of New South Wales.]Google Scholar
Rode, K. Zum Problem der Aetna-Vergletscherung. Zeitschrift der Deutschen Geologischen Gesellschaft, Bd. 104, Teil 1, 1952, p. 10–14. [Was Etna glaciated ?]Google Scholar
Rohrer, E. Staublawinen-ja oder nein ? Die Alpen, 30 Jahrg., No. 3, 1954, p. 62–88. [The term Staublawinen should be used for avalanches with turbulent motion; reply by M. de Quervain, ibid., No. 6, Pt. 11, 1954, p. 97.]Google Scholar
Roller, Maria. Über die Auswirkung mikroklimatischer Faktoren auf das Abschmelzen der Winterschneedecke.Wetter und Leben, Jahrg. 5, Ht. 1/2, 1953, p. 31–33. [Micrometeorological factors in snow melting.]Google Scholar
Rossmann, F. Polare Kristallform und elektrische Erregung des Eises. Experientia, Vol. 6, No. 5, 1950, p. 182. [Ice has piezoelectric effect ten times that of tourmaline; it is masked by twinning.]Google Scholar
Rothé, J. P., and others. Sondages séismiques au Groenland 1949, 1950, 1951: rapports scientifiques des Expéditions Polaires Françaises N III 2. Annales de Géophysique, Tome 9, Fasc. 4, 1953, p. 329–57. [Introduction by J. P. Rothé, “Étude des vitesses de propagation des ondes séismiques sur linlandsis du Groenland” by A. Joset and J.-J. Holtzscherer; “Dispersion des ondes de surface dans la couche superficielle du glacier du Groenland” by Mme. N. Jobert.]Google Scholar
Rundle, R. E. The structure and residual entropy of ice. Journal of Chemical Physics, Vol. 11, No. 7, 1953, p. 1311. [The entropy anomaly can be explained without Pauling’s assumption on the basis of the bond angle in the water molecule.]Google Scholar
Rundle, R. E. Polar versus nonpolar ice. Journal of Chemical Physics, Vol. 22, No. 2, 1954, p. 344–45. [Discussion of residual entropy of ice and possible crystal structures of ice.]Google Scholar
Sandström, A. E. On the concentration of heavy water in glacier ice. Arkiv för Fysik, Bd. 3, Nr. 35, 1951, p. 549–56. [Accurate density measurements show that ice from glaciers has up to 05°% heavy water (D2O), i.e., three times normal content.]Google Scholar
Sauberer, F. Dirmhirn, Inge. Untersuchungen über die Strahlungsverhältnisse auf den Alpengletschern. Archiv für Meteorologie, Geophysik und Bioklimatologie, Ser. B, Bd. 3, 1951, p. 256–69. [Experiments on incoming and outgoing radiation on the Hohen Sonnblick. Albedo of glacier very variable.]Google Scholar
Schwarzacher, W. Untersteiner, N. Zum Problem der Bänderung des, Gletschereises. Sitzungsberichte der Österreichischen Akademie der Wissenschaften. Mathematisch-naturwissenschaftliche Klasse, Abt., 2a, Bd. 162, Ht. 1 bis 4, 1953, p. 111–45. [Preferred orientation of crystals in glacier bands on Pasterzenkees, and explained in terms of the Nye theory. Air content of ice studied.]Google Scholar
[Sea Ice: Terminology.] World Meteorological Organization, Commission for Maritime Meteorology: abridged final report of the first session, London, 14th–29th July, 1952. Geneva, Secretariat of the World Meteorological Organization, [1952 ?]. 108 p., 28 cm. (WMO-No. 10. RP. 2.) [Mimeographed. International sea ice nomenclature recommended, with definition of terms.]Google Scholar
Shakhov, A. A. Fizicheskiye protsessy v snegovom pokrove [Physical processes in snow cover]. Izve.:tiya Akademii Nauk SSSR. Seriya Geograficheskaya i Geofizicheskaya [News of the Academy of Sciences of the USSR. Geographical and Geophysical series] (Moscow), Tom is, No. 3, 1948, p.239–18 [Effect of sublimation on snow cover; methods. of promoting sublimation in order to harden surface. English translation by Peter P. Kapusta, U.S. S[now,] I[ce and] P[ermafrost] R[esearch] E[stablishment]. Translation 15.]Google Scholar
Shapiro, A. Simpson, L. S. The effect of a broken icefield on water waves. Transactions. American Geophysical Union, Vol. 34, No. 1, 1953, p. 36–42. [Technique of forecasting sea and swell in pack ice.]Google Scholar
Thompson, H. R. Geology and geomorphology in southern Nordaustlandet (North-East Land), Spitsbergen. Proceedings of the Geo:ogists’ Association, Vol. 64, Part 4, 1953, p. 293–312. [Includes glaciology.]Google Scholar
Wright, J. K. The open Polar Sea, Geographical Review, Vol. 43, No. 3, 1953, p. 338–65. [Refers to the early belief in an ice-free Arctic Ocean.]Google Scholar