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Glaciological Literature

Published online by Cambridge University Press:  30 January 2017

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Journal of Glaciology , Volume 5 , Issue 42 , 1965 , pp. 883 - 891
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Copyright © International Glaciological Society 1965

This is a selected list of glaciological literature on the scientific study of snow and ice and of their effects on the earth; for the literature on polar expeditions, and also on the “applied” aspects of glaciology, such as snow ploughs, readers should consult the bibliographies in each issue of the Polar Record. For Russian material the system of transliteration used is that agreed by the U.S. Board on Geographic Names and the Permanent Committee on Geographical Names for British Official Use in 1947. Readers can greatly assist by sending reprints of their publications to the Society, or by informing Dr. J. W. Glen of publications of glaciological interest. It should be noted that the Society does not necessarily hold copies of the items in this list, and also that the Society does not possess facilities for microfilming or photocopying.

References

General Glaciology

Crary, A. P. Recent U.S. scientific research in Antarctic– Part I. Activities and preliminary findings of field programs during austral summer 1963–64. Transactions. American Geophysical Union, Vol. 45, No. 4, 1964, p. 719–26; 1G Bulletin (Washington, D.C.), No. 88, 1964, p. 15–22. [Glaciological research by various U.S. bodies in Antarctica described, p. 725–26.]Google Scholar
Grötzbach, E. Hillebrandt, A. Von. Die rezente und eiszeitliche Vergletscherung im mittleren Khwāja Muhammad-Gebirge. (In Münchner Hindukvsch-Kundfahrt 1963. Verlatf, wissenschaftliche und bergsteigerische Ergebnisse. München, Akademischen Sektion München des Deutschen Alpenvereins, 1964, p. 26–31.) [General description, also periglacial phenomena of the recent and Ice Age glacierizations in the central Khwāja Muhammad ranges.]Google Scholar
Grosval’d, M. G. Sukhodrovskiy, V. L. Some results of glaciological investigations on the territory of the U.S.S.R. according to the I.G.ϒ. program. Translations of various articles appearing in Opisareiye ob’yektou glyatsiologicheskikkh rsledavaniy, provedennykh po programme Mezhdunarodnoga Geofizicheskago Goda na territorii Sovietskogo Soyuza (Description of subjects of glaciological investigations conducted on the territory of the Soviet Union under the I.G.Y. program), Moscow, 1938, p. 4–18, 19–41, 42–56, 139–160. Washington, D.C., U.S. Department of Commerce, 1960. 60 p.Google Scholar
Haefeli, R. Kommentar, Spezifikation und Ergänzungen zum generellen Arbeitsprogramm von 25. September 1963 für die 2. Expedition 1966. Bulletin de l’Association Internationale d’Hydrologie Scientifique, 9e An., No. 3, 1964, p. 5–11. [Aims, supplies, budget etc. and programme of work from 25 Sept. 1963 for 2nd international glaciological expedition to Greenland 1966.]Google Scholar
Hofmann, W. Richard Finsterwalder und die Alpenvereinskartographie. Jahrbuch des Österreichischen Alpenvereins, Bd. 89, 1964, p. 132–37. [Description of Finsterwalder’s many–sided interests and work in the mountains.]Google Scholar
Lorius, C. Contribution à la connaissance de l’Antarctique: glaciologie en Terre Adélie (1956–1959), Année Géophysique Internationale. Participation Française, Sér. 9, Fasc. 1, 1964, 101 p. [Analysis of glaciological observations in Terre Adélie 1956–59 during French I.G.Y. expeditions.]Google Scholar
SirPriestley, R. E., and others, ed. Antarctic research: a review of British scientific achievement in Antarctica. Edited by SirPriestley, R. [E.] Adie, R. J. Robin, G. de Q.. London, Butterworths, 1964. xii, 360 p. [Contents include: Sir R. [E.] Priestley, “The background”, p. 1–15; Sir V. [E.] Fuchs, “Polar travel”, p. 16–27; D. L. Linton, “Landscape evolution”, p. 85–99; G. de Q. Robin and R. J. Adie, “The ice cover”, p. 100–17; R. J. Adie, “Geological history”, p. 118–62; G. de Q. Robin, “International co–operation and geophysics”, p. 254–64; H. H. Lamb, “Circulation of the atmosphere”, p, 265–77; H. H, Lamb, “The climate”, p. 278–91; G. E. R. Deacon, “The Southern Ocean”, p. 292–307; J, A. Heap, “Pack ice”, p. 308–17.]Google Scholar
Roberts, B. B. Gazetteer of the British Antarctic Territory, South Georgia and the South Sandwich Islands. First supplement to first edition. London, H.M. Stationery Office, 1964. 4 p. [196 new names with alterations and corrections.]Google Scholar
Rutsch, R. F. Grindelwald, Wiege der experimentellen Gletscherforschung. Les Alpes. Revue du Club Alpin Suisse, 38e An., 1er Trimestre. 1962, p. 49–50.Google Scholar
Ya-Feng, Shih Tzu-Hsiu, Chi Scientists study Mount Shisha Pangma. China Reconstructs, Vol. 14, No. 3, 1965, p. 19–23. [One of the centres of present glaciation in the Himalaya.]Google Scholar
Troll, C. Richard Finsterwalders Lebenswerk und die geographische Hochgebirgsforschung. Allgemeine Vermessungsnachrichten, Jahrg. 71, Ht.11, 1964, p. 398–404. [Account of Richard Finsterwalder’s work and his geographical researches in the high mountains of the world.]Google Scholar
Yoshida, A. Suzuki, T. Map compilation for coastal region between 37° and 45° E. Antarctic Record (Tokyo), No. 23, 1964. p. 32–41. [Compilation of 8 colour maps scale 1:250,000 of “Lützow–Holm Bay” and “Prince Olav Coast”, Dronning Maud Land. In Japanese with English abstract and captions.]Google Scholar

Glaciological Instruments and Methods

Bogorodskiy, V. V. Sovremennyye fizicheskiye sposoby izmereniya tolshchiny morskikh l’dov . Okeanologiya [Oceanography], Tom 3, Vyp. 4, 1963, p. 720–30. [Electric, ultrasonic and electromagnetic close-contact methods; seismic-acoustic and electromagnetic remote methods discussed and compared.]Google Scholar
Buck, B. M. Ice drilling in Fletcher’s Ice Island (T–3) with a portable mechanical drill. Arctic, Vol. 18, No. 1, 1965, p. 51–54.CrossRefGoogle Scholar
Cheremnykh, G. D. Novoye v izmerenii skorostey dvizheniya l’da v poverkhnostnykh chastyakh lednikov po materialam aeros”yemki . Geodeziya i Aerofotos”yemka, No. 5, 1962, p. 111–15. [Discussion of techniques and accuracy. English translation, Geodesy and Aerophotography, No. 5, 1962 [pub. 1963], p. 342–44.]Google Scholar
Konovalov, V. G. A method of measuring ablation of a glacier. Soviet Hydrology. Selected Papers, 1963, No. 2, p. 201–04. [Method based on collecting melt water from sample area.]Google Scholar
Langway, C. C. jr., and others. Sampling Polar ice for radiocarbon dating, [by] C. C. Langway, Jr., Hans Oeschger, Bernhard Alder [and] André Renaud., Nature, Vol. 206, No. 4983, 1965, p. 500–01. [Letter. Joint research by U.S. Cold Regions Research and Engineering Laboratory, Swiss Gletscherkommission and Universität Bern, using a highly sensitive low-level counting device.]Google Scholar
McLerran, J. H. Airborne crevasse detection. Proceedings of the third symposium on remote sensing of environment, 14, 15, 16 October 1964 (Ann Arbor, University of Michigan. Institute of Science and Technology), 1965, p. 801–02. [Feasibility of aerial detection of snow-bridged crevasses by infrared sensing.]Google Scholar
McLerran, J. H. Infrared sea ice reconnaissance. Proceedings of the third symposium on remote sensing of environment, 14, 15, 16 October 1964 (Ann Arbor, University of Michigan. Institute of Science and Technology), 1965, p. 789–99. [Interpretation of illustrations of infra-red images of sea ice; applications and limitations discussed briefly.]Google Scholar
Nezami, M., and others. Mesure du taux d’accumulation de la neige au bord du continent antarctique par la méthode du plomb 210, par M. Nezami, G. Lambert, C. Lorius et J. Labeyrie. Comptes Rendus Hebdomadaires des Séances de l’Académie des Sciences (Paris), Tom. 259, No. 19, 1964, p. 3319–22. [Measurement of rate of accumulation of snow in Terre Adélie by means of 210Pb.]Google Scholar
Rinker, J. N. Radio echo sounding and strain rate measurement in the ice sheet of north-west Greenland: 1964. Polar Record, Vol. 12, No. 79, 1965, p. 403–05. [Results of measurements briefly reported. Future use of ice depth determination by radar discussed.]Google Scholar
Savel’yev, B. A. Rukovodstvo po izucheniyu suoystv l’da [Handbook on study of ice properties]. Moscow, Izdatel’stvo Moskovskoga Universiteta [Publishing House of Moscow University], 1963. 198 p. [Properties of ice and how to determine them in laboratory and field.]Google Scholar
Shvayshteyn, Z. I. Poluprovnikovyy solemer dlya izmereniya solenosti morskogo l’da . Problemy Arktiki i Antarktiki [Problems of the Arctic and Antarctic], Vyp. 15, 1964, p. 85–87.Google Scholar

Physics of Ice

Barnes, G. T., and others. Ice forming activity and the surface properties of nucleating materials, [by] G. T. Barnes, U. Katz and R. Sänger., Zeitschrift für angewandte Mathematik and Physik, Vol. 13, Fasc. 1, 1962, p. 76–80. [Theoretical study of physics of nucleation.]Google Scholar
Bennett, J. E., and others. Electron spin resonance spectra of hydrated electrons prepared by reaction of atomic sodium with ice at 77° K, [by] J. E. Bennett, B. Mile [and] A. Thomas., Nature, Vol. 201, No. 4922, 1964, p. 919–20. [Letter. Results allow state of this defect in ice to be analysed.]Google Scholar
Bertie, J. E. Whalley, E. Infrared spectra of ices Ih and Ic in the range 4000 to 350 cm–1’. Journal of Chemical Physics, Vol. 40, No. 6, 1964, p. 1637–45. [Observations and discussion. No detectable difference between hexagonal and cubic ice.]Google Scholar
Bertie, J. E. Whalley, E. Infrared spectra of ices II, III and V in the. range 4000 to 350 cm–1’. Journal of Chemical Physics, Vol. 40, No. 6, 1964, p. 1646–59. [Observations and interpretation in terms of structure.]Google Scholar
Bertie, J. E., and others. Transformations of ice II, ice III, and ice V at atmospheric pressure, [by] J. E. Bertie, L. D. Calvert and E. Whalley. Journal of Chemical Physics, Vol. 38, No. 4, 1963, p, 840–46. [All these high-pressure phases transform first to cubic ice on heating from liquid nitrogen temperature.]Google Scholar
Bigg, E. K. Miles, G. T. The results of large-scale measurements of natural ice nuclei. Journal of the Atmospheric Sciences, Vol. 21, No. 4, 1964, p. 396–403. [Australian data used to show probable extra-terrestrial source of many nuclei.]Google Scholar
Blicks, H., and others. Zur Verteilung von Fremdsubstanzen in Eis-Einkristallen, von H. Blicks, H. Egger and N. Riehl. Physik der kondensierten Materie, Bd. 2, Ht. 5, 1964, p. 419–22. [Study of radial distribution of HF and NH4F in ice grown from dilute solutions.]Google Scholar
Camp, P. R. Barter, C. F. An electrical effect un the growth of ice crystals. Nature. Vol. 200, No. 4904, 1963, p. 350–51. [Letter. Presence of electric field affects grain size and shape of ice frozen from water.]Google Scholar
Camp, P. R. Barter, C. F. Rate of growth of ice at an aluminium-water interface. Nature, Vol. 206, No. 4983, 1965, p. 495–97. [Letter. At least two different modes of growth occurred depending on the amount of supercooling and the manner of nucleation.]Google Scholar
Child, W. C. jr. Thermodynamic functions for metastable ice structures I and II. Journal of Physical Chemistry, Vol. 68, No. 7, 1964, p. 1834–38. [Reanalysis of data on free energies.]Google Scholar
Dean, J. W. Timmerhaus, K. D. Thermal conductivity of solid H2O and D2O at low temperatures. Advances in Cryogenic Engineering, Vol. 8, 1962, p. 263–67. [Measurements at liquid hydrogen and liquid nitrogen temperatures.]Google Scholar
Dengel, O. Riehl, N. Diffusion von Protonen (Tritonen) in Eiskristallen. Physik der kondensierten Materie, Bd. 1, Ht. 3, 1963, p. 191–96. [Diffusion of 3H in ice measured. Activation energy consistent with that for dielectric and mechanical relaxation.]Google Scholar
Dengel, O., and others. Ferroelectric behaviour of ice, [by] O. Dengel, U. Eckener, H. Plitz and N. Riehl. Physics Letters, Vol. 9, No. 4, 1964, p. 291–94. [Ferroelectricity observed below 100°K. provided water from which ice was made was not extremely pure.]CrossRefGoogle Scholar
DiMarzio, E. A. Stillinger, F. H. jr. Residual entropy of ice. Journal of Chemical Physics, Vol. 40, No. 6, 1964, p. 1577–81. [Calculation.]Google Scholar
Dinger, J. E. Electrification accompanying melting of ice and snow. Quarterly Journal of the Royal Meteorological Society, Vol. 90, No. 384, 1964, p. 208–09. [Correspondence relating to use of artificially made snow arising out of article by J. B. Matthews and B. J. Mason, ibid., Vol. 89, No. 381, 1963, p. 376–80. Reply by Mason and Matthews, p. 208–09.]Google Scholar
Dooley, D. Observations on the deformation of ice at low stresses. Ohio State University Institute of Polar Studies. Report No. 12, 1964, [ii, 16] p. [Single crystals and polycrystalline ice.]Google Scholar
Eisenberg, D. Coulson, C. A. Energy of formation of D-defects in ice. Nature, Vol. 199, No. 4891, 1963, p. 368–69. [Comparison of total energies of formation of D- and X-defects.]Google Scholar
Giguère, P. A. Arraudeau, J. P. Spectres d’absorption de trois formes allotropiques de la glace dans l’infrarouge lointain. Comptes Rendus Hebdomadaires des Séances de l’Académie des Sciences (Paris), Tom. 257, No. 10, 1963, p. 1692–94. [Similarities in far infrared absorption spectra of vitreous, cubic and hexagonal ice.]Google Scholar
Gränicher, C. Properties and lattice imperfections of ice crystals and the behaviour of H2O–HF solid solutions. Physik der kondensierten Materie, Bd. 1, Ht. 1, 1963, p. 1–12. [A review article dealing with electrical, acoustic and nuclear magnetic resonance properties of ice and their interpretation.]Google Scholar
Haas, C. On diffusion, relaxation and defects in ice. Physics Letters, Vol. 3, No. 3, 1962, p. 126–28. [Suggests mechanism for electrical and mechanical relaxation and diffusion of oxygen in ice.]Google Scholar
Harrison, J. D. Solute transpiration pores in ice. Journal of Applied Physics, Vol. 36, No. 1, 1965, p. 326–27. [Letter. Observation of pores developed when freezing solutions and theory of their formation.]Google Scholar
Hayes, C. E. Webb, W. W. Dislocations in ice. Science, Vol. 147, No. 3653, 1965, p. 44–45. [X-ray diffraction topography shows Burgers vectors of slip dislocations to have <1120>directions.]Google Scholar
Heinmets, F. Blum, R. Conductivity measurements on pure ice. Transactions of the Faraday Society, Vol. 59, No. 5, 1963, p. 1141–46. [Results give activation energy of 24.2 kcal. for proton transfer.]Google Scholar
Higashi, A., and others. Plastic yielding in ice single crystals, [by] A. Higashi, S. Koinuma and S. Mae. Japanese Journal of Applied Physics, Vol. 3, No. 10, 1964. p. 610–16. [Constant strain-rate tests. No work hardening found. Activation energy consistent with Johnston’s dislocation theory.]Google Scholar
Hollins, G. T. Configurational statistics and the dielectric constant of ice. Proceedings of the Physical Society, Vol. 84, Pt. 6, 1964, p. 1001–16. [Theoretical study.]Google Scholar
Itagaki, K. SeIf-diffusion in single crystals of ice. journal of the Physical Society ofjapan, Vol. 19, No. 6, 1964, p. 1081. [Measurements of activation energy and of D 0. Time variation found and discussed. No anisotropy observed.]Google Scholar
Jaccard, C. Thermodynamics of irreversible processes applied to ice. Physik der kondensierten Materie, Bd. 3, Ht. 2, 1964, p. 99–118. [Calculation of entropy production and resulting thermoelectric effects.]Google Scholar
Jaccard, C. Thermoelectric effects in ice crystals. I. Theory of the steady state. Physik der kondensierten Materie, Bd. 1, Ht. 2, 1963, p. 143–51. [Theory starting from equations for ice defects.]Google Scholar
Jackson, J. A. Rabideau, S. W. Deuteron magnetic resonance in polycrystalline heavy ice (D2O). Journal of Chemical Physics, Vol. 41. No.12, 1964, p. 4008. [Letter. Measurements reported and discussed.]Google Scholar
Joss, J. List, R. Zur Radarrückstrahlung von Eis-Wasser-Germischen. Zeitschrift für angewandte Mathematik und Physik, Vol. 14, Fasc. 4, 1963, p. 377–80. [Radar experiments on back-scattering of spherical ice particle.]Google Scholar
Kamb, W. B. Ice II: a proton-ordered form of ice. Acta C.ryslallographica, Vol. 17, Pt, 11, 1964, p. 1437–49. [X-ray structure determination and discussion.]Google Scholar
Kamb, W. B. Davis, B. L. Ice VII, the densest form of ice. Proceedings of the National Academy of Sciences of the United States of America, Vol. 52, No. 6, 1964, p. 1433–39. X-ray structure determination shows ice VII to have body–centred cubic structure.]Google Scholar
Kevan, L., and others. Formation of electrons and of atomic hydrogen in y-irradiated ice, by L. Kevan, P. N. Moorthy and J. J. Weiss. Nature, Vol. 199, No. 4894, 1963, p. 689–90.Google Scholar
Larsson, K. E. Dahlborg, U. Some vibrational properties of solid and liquid H2O and D2O derived from differential cross-section measurements. Journal of Nuclear Energy, Parts A and B, Vol. 16, No. 2, 1962, p. 81–89. [Neutron measurements used to deduce phonon frequency spectra.]Google Scholar
Latham, J. The electrification of freezing water drops. Quarterly Journal of the Royal Meteorological Society, Vol, 90, No. 384, 1964, p. 209–11. [Correspondence arising out of article by D. G. Evans and W. C. A. Hutchinson, ibid., Vol. 89, No. 381, 1963, p. 370–75. Reply by W. C. A. Hutchinson, p. 211.]Google Scholar
Levi, L., and others. Electrical conductivity and dissociation constants in ice doped with HF and NH, in different ratios, by L. Levi, O. Milman and E. Suraski. Transactions of the Faraday Society, Vol. 59, No. 9, 1963, p. 2064–75. [Measurements suggest lower conductivity and ion mobilities in purr ice than previously assumed.]Google Scholar
Levi, L., and others. Thermal etching on ice crystals, by L. Levi, S. M. de De Michcli and L. Lubart. Physica Status Solidi, Vol. 4, No. 1, 1964, p. 63–70. [Facets found in pure ice but not ice doped with NaCI.]CrossRefGoogle Scholar
McMillan, J. A. Los, S. C. Vitreous ice: irreversible transformations during warm-up. Nature, Vol. 206, No. 4986, 1965, p. 807–07. [Observation of glass transformation and of change to cubic and finally hexagonal ice and measurement of heats of transformation.]Google Scholar
Magnan, D. Kahane, A. Conductivité de la glace aux basses températures. Comptes Rendus Hebdomadaires des Séances de l’Académie des Sciences (Paris), Tom. 256, No. 26, 1963, p. 5539–41. [Electrical conductivity measurements at −80° to −120°C. and high fields indicate a space-charge-limited proton current.]Google Scholar
Onsager, L. Runnels, L. K. Mechanism for self-diffusion in ice. Proceedings of the National Academy of Sciences of the United States of America, Vol. 50, No. 2, 1963, p. 208–10. [Evidence for interstitial molecule mechanism.]Google Scholar
Pascalar, H. G. Sakamoto, R. T. Microwave radiometric measurements of ice and water. Proceedings of the third symposium on remote sensing of environment, 14, 15, 16 October 1964 (Ann Arbor, University of Michigan. Institute of Science and Technology), 1965, p. 803–11. [Description of an experiment of ice measurements with a passive microwave radiometer, equipment used and data obtained. Possible utility of microwave radiometry in various ice applications is indicated.]Google Scholar
Pistorius, C. W. T., and others. Melting curve of ice VII to 200 kbar, [by] C. W. T. Pistorius, M. C. Pistorius, J. P. Blakey and L. J. Admiraal. Journal of Chemical Physics, Vol. 38, No. 3, 1963, p. 600–02. [Follows melting curve up to 442°C.]Google Scholar
Rabideau, S. W. Jackson, J. A. Low temperature observation of oxygen–17 NMR in H2O, D2O, and eutectic solutions. Journal of Chemical Physics, Vol. 41, No. 11, 1964, p. 3405–07. [No signals observed in pure solids.]CrossRefGoogle Scholar
Sano, I., and others. Adsorption studies on the mechanism of ice nucleation, [by] I Sano, N. Fukuta, Y. Kojima [and] T. Murai. Journal of the Meteorological Society of japan, Ser. 2, Vol. 41, No. 4, 1963, p. 189–96. [Relation between adsorption measurements and nucleation.]Google Scholar
Sitharamarao, D. N. Duncan, J. F. Molecular excitation of water by y-irradiation. journal of Physical Chemistry, Vol. 67, No. 10, 1963, p. 2126–32. [Study of thermoluminescence and fluorescence of y-irradiated ice.]Google Scholar
Taylor, M. J. Whalley, E. Raman spectra of ices Ih, Ic, II, III, and V. Journal of Chemical Physics, Vol. 40, No. 6, 1964, p. 1660–64. [Observations and discussion.]Google Scholar
Townsend, A. A. Natural convection in water over an ice surface. Quarterly Journal of the Royal Meteorological Society, Vol. 90, No. 385, 1964, p. 248–59; Vol. 91, No. 388, 1965, p. 243–45. [Laboratory observation of motions set up in water with upper surface at 25°C. and bottom surface of ice. Discussion printed in later issue.]Google Scholar
Waldstein, P., and others. Nuclear magnetic resonance of single crystals of D2O ice, by P. Waldstein, S. W. Rabideau and J. A. Jackson. Journal of Chemical Physics, Vol. 41, No. 11, 1964, p. 3407–11. [Measurements of deuteron magnetic resonance used to estimate hydrogen-bond energies.]CrossRefGoogle Scholar

Land ice. Glaciers. Ice shelves

Aitkenhead, N. Ice calderas. British Antarctic Survey Bulletin, Vol. 1, No. 5, 1965, p. 63–64. [Letter. Suggestions regarding nomenclature; see also Stokes, J., below.]Google Scholar
Aliverti, G. Glaciologia. Bollettino del Comitato Glaciologico Italiano, 2 Ser., No. 11, Pt. 1, 1962, [pub.] 1964, supplement, 50 p. [Account of glaciers, their structure and flow, and of current theories.]Google Scholar
Andrews, J. T. Webber, P. J. A lichenometrical study of the northwestern margin of the Barnes Ice Cap: a geomorphological technique. Geographical Bulletin (Ottawa), No. 22, 1964, p. 80–104. [Use to date moraines back to 1680.]Google Scholar
Angino, E. E., and others. Ionic content of Antarctic ice samples, by E. E. Angino, K. B. Armitage and J. C. Tash. Polar Record, Vol. 12, No. 79, 1965, p. 407–09. [Results of analysis of chemical composition of samples of glacier ice, melt water and lake water.]Google Scholar
Ardus, D. A. Morphology and regime of the Brunt Ice Shelf and the adjacent inland ice, 1960–61. British Antarctic Survey Bulletin, No. 5, 1965, p. 13–42. [At present the glacierization of the area appears to be in equilibrium. Precipitation is discussed.]Google Scholar
Astori, V. Togliatti, G. II rilievo areofotogrammetrico del Ghiacciaio Pian di Neve. Bollettino del Comitato Glaciologico Italiano, 2 Ser., No. 11, Pt. 1, 1962, [pub.] 1964, p. 33–50. [Survey, plotting and drawing of map, scale 1:5,000, of Ghiacciaio Pian di Neve in the massif of Adamello.]Google Scholar
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Black, R. F., and others. Saline discharge from Taylor Glacier, Victoria Land, Antarctica, [by] R. F. Black, M. L. Jackson and T. E. Berg. Journal of Geology, Vol. 73, No. 1, 1965, p. 175–81. [Analysis and discussion of origin.]Google Scholar
Buynitskiy, V. Kh. Dvizhenlye i balans massy shel’fovykh l’dov Antarktiki . Vestnik Leningradskogo Universiteta [Messenger of Leningrad University], 1964, No. 6, p. 57–70.Google Scholar
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Chuchkalov, B. S. The causes for movements of the Medvezhiy glacier. Soviet Hydrology. Selected Papers, 1963, No. 5, p. 522–24. [Report of sudden advance and its explanation.]Google Scholar
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Icebergs. Sea, river and lake ice

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Glacial Geology

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Frost action on rocks and soil. Frozen ground. Permafrost

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Brown, R. J. E. Some observations on the influence of climatic and terrain features on permafrost at Norman Wells, N.W.T., Canada. Canadian Journal of Earth Sciences, Vol. 2, February 1965, p. 15–31.Google Scholar
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Grötzbach, E. Beobachtungen an Blockströmen im afghanischen Hindukusch und in den Ostalpen. Mitteilungen der Geographischen Gesellschaft München, Bd. 50, 1965, p. 175–201. [Differentiation between rock tongues as remnants of active ice glaciers and rock glaciers which originated as independent accumulations of rocks and debris interspersed by recent ice.]Google Scholar
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Rathjens, C. Ein Beitrag zur Frage der Solifluktionsgrcnzc in den Cebirgen Vorderasiens. Zeitschrift für Geomorphologie, Neue Folge, Bd. 9, Ht. 1, 1965, p. 35–49. [Researches in the Afghan Hindu Kush indicate that the region influenced by solifluction is broader in a dry climate.]Google Scholar
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Vel’mina, N. A. Vtyurin, B. I., ed. Geokriologicheskiye usloviya zapadnoy Sibiri, ϒakutii i Chukotki [Geocryological conditions in western Siberia, rakuliya and Chukotka]. Moscow, Izdatel’stvo “Nauka” [Publishing House “Nauka”], 1964. 140 p. [Papers on frozen ground and associated phenomena.]Google Scholar
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Meteorological and Climatological Glaciology

Arnold, K. C. MacKay, D. K. Different methods of calculating mean daily temperatures, their effects on degree-day totals in the high Arctic and their significance to glaciology. Geographical Bulletin (Ottawa), No. 21, 1964, p. 123–29.Google Scholar
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Fliri, F. Zur Witterungsklimatologie sommerlicher Schneefälle in den Alpen. Wetter und Leben, Jahrg. 16, Ht. 1–2, 1964, p. 1–11. [Based on observations of precipitation on the Säntis. It is shown that summer snowfalls are caused by meridional circulation in connection with disturbances travelling west to east.]Google Scholar
Havens, J. M. Climatological notes from Axel Heiberg Island, N.W.T., Canada. Arctic, Vol. 17, No. 4, 1964, p. 261–63. [Includes the cooling effect of a glacier terminus on the lower atmosphere.]Google Scholar
Jiusto, J. E. Rogers, R. R. Seeding whiteouts in Greenland. Research Trends, Cornell Aeronautical Laboratory, Vol. 9, No. 1, 1961, p. 5–7.Google Scholar
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McVehil, G. E. Wind and temperature profiles near the ground in stable stratification. Quarterly Journal of the Royal Meteorological Society, Vol. 90, No. 384, 1964, p. 136–46. [Antarctic and U.S.A. data compared. Surface stress and heat flux deduced.]Google Scholar

Snow

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Bergen, J. D. Swanson, R. H. Evaporation from a winter snow cover in the Rocky Mountain forest zone. Proceedings of the Western Snow Conference, 32nd annual meeting, 1964, [pub.] 1964, p. 52–57. [Quantitative results.]Google Scholar
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[France: Institutions.] Institut Français pour l’Étude de la Neige au Parc national de la Vanoise. Les Alpes. Revue du Club Alpin Suisse, 40e An., 3e Trimestre, 1964, p. 74–75. [Institute for study of snow in all aspects in course of construction in Parc national de la Vanoise.]Google Scholar
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