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Glaciological Literature

Published online by Cambridge University Press:  30 January 2017

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Journal of Glaciology , Volume 7 , Issue 49 , 1968 , pp. 135 - 145
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Copyright © International Glaciological Society 1968

This is a selected list of glaciological literature ou 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

Bull, C. [B. B.] Antarctic glaciology. Geotimes, Vol. 11, No. 4, 1966, p. 22–23. [Review of progress since beginning of I.G.Y.]Google Scholar
[Conferences.] Proceedings of the, first international symposium on water desalination. Washington, D.C. October 3–9, 1965. Washington, D.C., U.S. Department of the Interior. Office of Saline Water, [c 1967]. 3 vols.: 632 p., 830 p., 792 p. $3.25. [Full text of papers with summaries in French, Russian and Spanish. Includes the following papers: C. Jaccard. “Electrical properties of ice”, Vol. 1, p. 224–39; V. A. Klyachko, “Research in the field of water desalination”, Vol. 1, p. 331–38; A. J. Barduhn, “The freezing process for water conversion in the United States”, Vol. 2, p. 641–58; G. Bozza, G. Dassù [and] G. Giambclli, “On the freezing process”, Vol. 2, p. 751–67; A. Peled, “Operation of the freeze desalination plant at Eilat, Israel”, Vol. 3. p. 1–10; J. W. Pike, “The direct contact controlled crystal desalination process”, Vol. 3, p. 173–88; D. J. Sandell, Jr., and C. A. Johnson, “Direct freeze-wash separation process”, Vol. 3, p. 625–50.1Google Scholar
[Glaciology Arctic.] Glaciology in the Arctic, [by] Glaciology Panel, Committee on Polar Research, . Transactions. American Geophysical Union, Vol. 48, No. 2, 1967, p. 759–67. [Includes reports on sea ice (volume. condition and dynamics), glaciers, seasonal snow cover, frozen ground and Quaternary chronology.]CrossRefGoogle Scholar
Jaworowski, Z. Temporal and geographical distribution of radium D (lead-210). Nature, Vol. 212, No. 5065, 1966, p. 886–89. [Concentration in snow and ice fluctuates and is greater in Arctic than temperate regions.]CrossRefGoogle ScholarPubMed
McLeod, I. R. Glaciological observations in Enderby, Kemp, and Mac.Robertson [sic] Lands, Antarctica. ANARE Interim Reports. Series A (IV). Glaciology. Publication No. 90, 1967, 48p. [Snow and ice features, and topography of the ice sheet in 1958, 1959 and 1961 are described, also sea ice formation in 1958 and 1959.]Google Scholar
Meier, M. F. Why study glaciers? In the context of water resources. Transactions. American Geophysical Union, Vol. 48, No. 2, 1967, p. 798–802. [Major problems in an understanding of the hydrology of snow and ice.]Google Scholar
O’Leary, B. T. The presence of ice in the Venus atmosphere as inferred from a halo effect. Astrophysical Journal, Vol. 146, No. 3, 1966, p. 754–66. [Evidence for existence of ice crystals at top of clouds in Venus atmosphere.]CrossRefGoogle Scholar
O’Leary, B. T. Rea, D. G. Mars: influence of topography on formation of temporary bright patches. Science, Vol. 155, No. 3760, 1967, p. 317–19. [Bright patches may be CO2 in depressions rather than ice on mountains.]CrossRefGoogle ScholarPubMed
Oulianoff, N. De quelques termes employés dans la littérature glaciologique. Actes de la Société Helvétique des Sciences Naturelles, 1966, p. 137–39.Google Scholar
Ragle, R. H. Icefield Ranges Research Project, St. Elias Mountains, Yukon, 1966. Arctic, Vol. 20, No. 1, 1967, p. 49–53. [Study of Kaskawulsh Glacier medial moraine; morphological analysis of streams on a glacier; rock glacier studies; cation content of snow and ice in the area of the divide station; snow and ice sampling for analysis of 120Pb; and Steele Glacier observations.]CrossRefGoogle Scholar
Sekyra, J. Glacial geology and cryogeology of the Dronning Maud Land-East Antarctica (the Schirmacher Oasis-the Wohlthat Massif). Casopis pro Mineralogii a Geologii (Prague), [Vol.] 11, No. 2, 1966, F. 209–16.Google Scholar
Tolstikov, Ye. I., ed. Atlas Antarkliki . Moscow. Leningrad, Glavnoye Upravleniye Geodezii i Kartografii, 1966. xxiii, 225 p., maps. 60 cm. [Distribution of natural phenomena over whole area, and by regions.]Google Scholar
Vendrov, S. L., and others. Grigoriy Aleksandrovich Avsyuk (k 60-lctno so dnya rozhdeniya) , [by] S. L. Vendrov [and 13 others]. Izvestiya Akademii Nauk SSSR. Seriya Geograficheskaya , 1967, No. 2, p. 152–53. [Tribute and biography.]Google Scholar
Wilhelm, F. Hydrologie, Claziologie. Braunschweig, Georg Westermann Verlag, [c 1966]. 144 p. (Das Geographische Seminar.) [Includes sections on underground water, springs, rivers and seas, chemical properties of water, and glaciers (description, behaviour, and properties).]Google Scholar

Glaciological Instruments and Methods

Bauer, A. Utilisation de la photographie aérienne en glaciologie. (In Chevallier, R., ed. Phodographie aérienne. panorama intertechnique. Paris, Gauthier-Villars, 1965, p. 65–68.) [Review of use of aerial photographs in glaciology.]Google Scholar
Beaumont, R. T. Mt. Hood pressure pillow snow gage. Proceedings of the Western Snow Conference, 33rd annual meeting, 1965, p. 29–35. [Description of device for measuring water equivalent.]Google Scholar
Bertle, F. A. Snow compaction method for the analysis of runoff from rain on snow. Proceedings of the Western Snow Conference, 33rd annual meeting, 1965, p. 11–18. [Method of computation described.]Google Scholar
Bogorodskiy, V. V. Fedorov, B. A. Radiolokatsiya lednikov . Zhurnal Tekhnicheskoy Fiziki , Torn 37, Vyp. 4, 1967, p. 781–88. [Use during Soviet Antarctic Expedition near Mirny. English translation in Soviet Physics-Technical Physics, Vol. 12, No. 4. 1967, p. 561–66.]Google Scholar
Bonneval, M. Mesure de la direction et de la vitesse d’écoulement d’un glacier par photogrammetrie. (In Chevallier, R., ed. Photographie aérienne, panorama intertechnique. Paris, Gauthier-Villars, 1965, p. 69–72.) [Description of method of determining glacier velocity by aerial photogrammetry.]Google Scholar
Bugayev, Yu. G. Opyt rabot s radiodal’nomerami v Antarktide . Geodeziya i Kartografiya , No. 4, 1966, p. 10–14. [Use of this instrument under extreme conditions without loss of accuracy.]Google Scholar
Clough, J. W. Bentley, C. R. Electromagnetic sounding of glacial and shelf ice. Antarctic journal of the U.S., Vol. 2, No. 4, 1967, p. 119–20. [Soundings of ice thickness in five areas in Antarctica during the 1966–67 field season. Two complete systems were used.]Google Scholar
Crozaz, G., and others. Artificial radioactivity reference horizons in Greenland firn, by G. Crozaz, C. C. Langway. Jr., and E. Picciotto. Earth and Planetary Science Letters, Vol. 1, No. 1, 1966, p. 42–48. [Object was to investigate total a-activity in firn layers and to determine whether artificial nuclide variations exist which could be used to measure snow accumulation rates.]CrossRefGoogle Scholar
Dansgaard, W., and others. The Si32 fallout in Scandinavia: a new method for ice dating, by W. Dansgaard, H. B. Clausen and A. Aarkrog. Tellus, Vol. 18, Nos. 2–3, 1966, p. 187–91. [Measurements on snow and old glacier ice in Jotunheimen, Norway, in 1962 show 32Si as usable element for dating ice up to 2 000–3 000 years old.]CrossRefGoogle Scholar
Grant, L. O., and others. Application of radar to snow surveying, by L. O. Grant, J. D. Marwitz and C. W. Thompson. Proceedings of the Western Snow Conference, 33rd annual meeting, 1965, p. 42–48. [Discussion of methods of using radar to study falling snow.]Google Scholar
Jaccard, C. Four-point method for measuring the volume and surface conductivities of a thin sample.,Zeitschrifl für angewandte Mathcrnalik and Physik, Vol. 17, Fase. 6, 1966, p. 657–63. [Details of method suitable for application to ice.]CrossRefGoogle Scholar
Lambert, G., and others. Possibilities of using lead 210 as an atmospheric tracer, by G. Lambert, B. Ardouin, M. Nezami and G. Polian. Tellus, Vol. 18, Nos. 2–3, 1966, p. 421–26. [Use to date seasonal layers in snow.]CrossRefGoogle Scholar
Lorius, C., and others. Sur une méthode gravimétrique simplifiée de détermination de l’épaisseur de glace en bordure de l’Antarctique. [par] C. Lorius, G. Rouillon et F. Helly. Comptes Rendus Hebdomadaires des Séances de l’Académie des Sciences (Paris), Sér. B, Tom. 264, No. 3, 1967, p. 266–69. [Description of simple gravimetric method for determining ice thickness at edge of ice sheet and comparison of depths so found with depths found by drilling at Cap André Prudhomme, Terre Adélie.]Google Scholar
Meier, M. F., and others. Multispectral sensing tests at South Cascade Glacier, Washington, by M. F. Meier, R. H. Alexander and W. J. Campbell. Proceedings of the fourth symposium on remote sensing of environment… 1966… University of Michigan (Ann Arbor, Willow Run Laboratories, Institute of Science and Technology, University of Michigan), 1966, p. 145–59. [Correlative meteorological and photometric measurements were made on the ground; detailed glaciological information was available from past studies.]Google Scholar
Penton, V. E. Robertson, A. C. Experience with the pressure pillow as a snow measuring device. Water Resources Research, Vol. 3, No. 2, 1967, p. 405–08. [Useful for seasonal measurements; unreliable for short time-period variations.]CrossRefGoogle Scholar
Pettengill, D. Ice auger. U.S. Geological Survey. Water Supply Paper No. 1822, 1966, p. 53–54. [Description of powered auger suitable for drilling holes through river ice up to 0.5 m thick.]Google Scholar
Rinker, J. N., and others. Radio ice-sounding techniques, by J. N. Rinker, S. Evans and G. de Q. Robin. Proceedings of the fourth symposium on remote sensing of environment… 1966… University of Michigan (Ann Arbor. Willow Run Iaboratories, Institute of Science and Technology, University of Michigan), 1966, p. 793–800. [Evaluation of two VHF-band radar systems for measuring ice thickness and contouring bedrock profile of ice-rock interface, Greenland ice sheet, 1964.]Google Scholar
Shannon, W. G. Electronic methods of snow surveying. Soil Conservation, Vol. 23, No. 5, 1966, p. 107–09. [Continuous recording of snowfall, air temperature and water equivalent.]Google Scholar

Physics of Ice

Adamson, A. W. Surface of very cold ice is nonpolar. Chemical and Engineering News, Vol. 44, No. 18, 1966, p. 50. [Adsorption of Na at 78°K implies ice is non-polar at surface.]Google Scholar
Al-Naimy, B. S., and others. An electron spin resonance study of the radiolysis and the photolysis of frozen ammonia-water systems, by B. S. Al-Naimy, P. N. Moorthy and J. J. Weiss. Journal of Physical Chemistry, Vol. 70, No. 11, 1966, p. 3654–60. [Identification of NH2 radical as formed by γ-irradiation. Study of its production.]CrossRefGoogle Scholar
Arias, D., and others. Electrical properties of ice doped with NH3, [by] D. Arias, L. Levi and L. Lubart. Transactions of the Faraday Society, Vol. 62, No. 523, 1966, p. 1955–62. [Dielectric constant and conductivity as function of temperature and NH3 concentration.]CrossRefGoogle Scholar
Barnaal, D. E. Lowe, I. J. Experimental free-induction-decay shapes and theoretical second moments for hydrogen in hexagonal ice. Journal of Chemical Physics, Vol. 46, No. 12, 1967, p. 4800–09. [Good agreement with model of nuclear magnetic resonance line shape which assumes that high-frequency proton tunnelling does not take place along the hydrogen bonds.]CrossRefGoogle Scholar
Berendsen, H. J. C. Water structure in biological systems. Federation Proceedings. Federation of American Societies for Experimental Biology, Vol. 25, No. 3, Pt. 1, 1966, p. 971–76. [Discussion of structure of H2O in biomolecular systems. Includes suggestion about ice nucleating ability of many steroid hormones.]Google ScholarPubMed
Blinc, R. Hadži, D. Deuteron quadrupole coupling and hydrogen bonding in crystals. Nature, Vol. 212, No. 5068, 1966, p. 1307–09. [Use of deuteron magnetic resonance to study hydrogen bonds in, among other things. ice.]CrossRefGoogle Scholar
Bogorodskiy, V. V. Khokhlov, G. P. Akusticheskiyc kharakteristiki l’da, nakhodyashchegosya pod staticheskim davleniyem . Akusticheskiy.Zhurnal , Tom 13, Vyp. 1, 1967, p. 18–22. [Velocity of sound in columnar polycrystalline ice up to 500 bar. Main effect attributed to recrystallization of ice. English translation in Soviet Physics—Acoustics, Vol. 13, No. 1, 1967, p. 14–17.]Google Scholar
Brill, R. Tippe, A. Gitterparameter von Eis I bei tiefen Temperaturen. Acta Crystallographiea, Vol. 23, No. 3, 1967, p. 343–45. [Accurate determination of lattice parameters of hexagonal ice, 15°-200°K. English summary.]CrossRefGoogle Scholar
Campbell, E. S., and others. Interpretation of the energy of hydrogen bonding; permanent multiple contribution to the energy of ice as a function of the arrangement of hydrogens, [by] E. S. Campbell, G. Gelertner, H. Heinen and V. R. G. Moorti. Journal of Chemical Physics, Vol. 46, No. 7, 1967, p. 2690–707, [Review of present knowledge of hydrogen bond and of hydrogen positions in ice and calculation of energy variation for different hydrogen arrangements.]CrossRefGoogle Scholar
De Micheli, S. M. de Licenblat, A. R. Ice whiskers grown in subsaturated atmospheres. Journal of the Atmospheric Sciences, Vol. 24, No. 3, 1967, p. 312–15. [Appearance of whiskers during evaporation of ice crystals.]2.0.CO;2>CrossRefGoogle Scholar
Grant, N. H. The biological role of ice. Discovery, Vol. 27, No. 8, 1966, p. 26–30. [Implications of discovery that some biochemical reactions are faster in ice.]Google Scholar
Grant, N. H. Alburn, H. E. Acceleration of enzyme reactions in ice. Nature, Vol. 212, No. 5058, 1966, p. 194. [Reactions faster in ice at −23°C than in water at +1°C.]CrossRefGoogle ScholarPubMed
Gunter, T. E. Electron paramagnetic resonance studies of the radiolysis of H2O in the solid state. Journal of Chemical Physics, Vol. 46, No. 10, 1967, p. 3818–29. [Study of OH radical in ice after electron irradiation at 77°K.]CrossRefGoogle Scholar
Hall, P. G. Tompkins, F. C. Dielectric relaxation in water adsorbed on ionic crystals. Journal of the Chemical Society, Sect. A, 1966, No. 1, p. 36–40. [Study of dielectric loss of ILO adsorbed on CaF2, MgO, KCl and Ag1. Discussion of extent to which adsorbed layers are ordered and ice-like.]CrossRefGoogle Scholar
James, D. W. Solidification kinetics of ice determined by the thermal wave technique. (In Peiser, H. S., ed. Crystal growth. Proceedings of an international conference on crystal growth, Boston, 20–24 June 1966. Oxford, etc., Pergamon Press, [1967], p. 767–73.) [Application to ice of method of determining kinetics of freezing normal to basal plane.]Google Scholar
Jones, S. J. Softening of ice crystals by dissolved fluoride ions. Physics Letters, Vol 25A, No. 5, 1967, p. 366–67. [At c. −70°C small amounts of HF considerably reduce stress in constant strain-rate tests and increase the creep rate.]CrossRefGoogle Scholar
Kikuchi, K. On the positive electrification of snow crystals in the process of their melting (III).-(IV). Journal of the Meteorological Society of Japan, Ser. 2, Vol. 43, No. 6, 1965, p. 343–50; p. 351–58. [(III): relation between bubble concentration in ice and charge generation during melting confirmed experimentally. (IV): during melting of bubbly ice, droplets seen to burst from surface carried negative charge.]Google Scholar
Kim, D.-Y. Schmidt, V. H. Semiclassical theory of proton transport in ice. Canadian Journal of Physics, Vol. 45, No. 4, 1967, p. 1507–16. [Calculation of mobility of protons in ice which agrees well with electrical conductivity experiments.]CrossRefGoogle Scholar
Koros, R. M., and others. The sticking probability of water on ice, [by] R. M. Koros, J. M. Deckers, R. P. Andreas and M. Boudart. Chemical Engineering Science, Vol. 21, No. 10, 1966, p. 941–50. [Beam of water vapour molecules impinges on ice target and number sticking found.]CrossRefGoogle Scholar
Krausz, A. S., and others. Tubular ice crystals, by A. S. Krauss, B. Harron and G. G. Litvan. Nature, Vol. 215, No. 5098, 1967, p. 271–73.CrossRefGoogle Scholar
Kröger, F. A. The chemistry of imperfect crystals. Amsterdam, North-Holland Publishing Co., 1964. xvi, 1039 p. [Ch. 18, “Special cases of disorder”, has section 18.2, p. 750–67, devoted to ice.]Google Scholar
Levi, L. Kobayashi, T. Ice filaments grown in a gradient of vapour pressure. Journal of the Meteorological Society ofjapan, Ser. 2, Vol. 45, No. 4, 1967. p. 315–25. [Study of the filaments which form when ice crystals, nucleated on fine threads, grow upwards and sublimate underneath, leaving a Filament between crystals and thread.]CrossRefGoogle Scholar
Levi, L. Milman, O. Freezing potential of electrolytic solutions. Journal of the Atmospheric Sciences, Vol. 23. No. 2, 1966, p. 182–86. [Experimental study for NH3 and NaCI solutions.]2.0.CO;2>CrossRefGoogle Scholar
Lieb, E. H. Exact solution of the F model of an antiferroelectric. Physical Review Letters, Vol. 18, No. 24, 1967. p. 1046–48. [Exact solution of phase transition and electrical properties of antiferroelectric structure similar to that of ice.]CrossRefGoogle Scholar
Lieb, E. H. Exact solution of the problem of the entropy of two-dimensional ice. Physical Review Letters, Vol. 18, No. 17, 1967, p. 692–94. [Entropy of two-dimensional square lattice obeying Bernal-Fowler rules found to be k In (4/3)3/1 per molecule.]CrossRefGoogle Scholar
Lieb, E. H. Exact solution of the two-dimensional Slater KDP model of a ferroelectric. Physical Review Letters, Vol. 19, No. 3, 1967, p. 508–10. [Exact solution of phase transition and electrical properties of ferroelectric structure similar to that of ice.]CrossRefGoogle Scholar
Lindenmeyer, C. S. Chalmers, B. Growth rate of ice dendrites in aqueous solutions. Journal of Chemical Physics, Vol. 45, No. 8, 1966, p. 2807–08. [Measurement of free and substrate growth rates as function of supercooling and solute concentration.]CrossRefGoogle Scholar
Lindenmeyer, C. S. Chalmers, B. Morphology of ice dendrites. Journal of Chemical Physics, Vol. 45, No. 8, 1966, p. 2804–06. [Direction of dendrites growing in supercooled pure water, aqueous solution and on substrates.]CrossRefGoogle Scholar
Maybank, J. Barthakur, N. N. The growth and destruction of ice filaments in an electric field. Nature. Vol. 216, No. 5110, 1967, p. 50–52. [Letter. Study of filament-like ice crystals growing near a freezing water drop and their modification by an electric field.]CrossRefGoogle Scholar
Morachevskiy, B. G. Ob aktivnosti chastits Ag J v kachestve l’doobrazuyushchikh yader . Izvestiya Akademii.Nauk SSSR. Atmosfery I Okeana , Tom 3, No. 1, 1967, p. 105–07. [If the isotope 131I is used in the Ag1 it does not act as nucleus. English translation in Izvestiya. Academy of Sciences, U.S.S.R. Atmospheric and Oceanic Physics, Vol. 3, No. 1, 1967, p. 59–60.]Google Scholar
Parungo, F. P. Lodge, J. P. jr. Amino acids as ice nucleators. Journal of the Atmospheric Sciences, Vol. 24. No. 3, 1967, p. 274–77. [Difference between optically active and inactive forms. Thermodynamic explanation.]2.0.CO;2>CrossRefGoogle Scholar
Parungo, F. P. Lodge, J. P. jr. Molecular structure and ice nucleation of some organics. Journal of the Atmospheric Sciences, Vol. 22, No. 3, 1965, p. 309–13. [Nucleating ability found to vary with potential strength of hydrogen bond between hydroxyl or carboxyl group and H2O molecule.]2.0.CO;2>CrossRefGoogle Scholar
Pinatti, D. Mascarenhas, S. Electrical currents produced during the solidification of water (Costa Ribeiro effect). Journal of Applied Physics, Vol. 38, No. 6, 1967, p. 2648–52. [Description of apparatus in which freezing or melting rate can be controlled and associated current measured. Results quoted. Importance for thunderstorm electricity discussed.]CrossRefGoogle Scholar
Pruppacher, H. R. On the growth of ice in aqueous solutions contained in capillaries. eitschriftfür.Nataforschung, Bd. 22A, Ht. 6, 1967, p. 895–901. [Observations of variation of dendritic growth rate with various dissolved monovalent ions.]Google Scholar
Qureshi, M. M. Maybank, J. Further tests on the ice nucleation potential of meteoritic material. Nature, Vol. 211, No. 5048, 1966, p. 508–09. [Laboratory tests.]CrossRefGoogle Scholar
Ramseier, R. O. Self-diffusion of tritium in natural and synthetic ice monocrystals. Journal of Applied Physics, Vol. 38, No. 6, 1967, p. 553–56. [Measurement both parallel and perpendicular to c-axis from −2.5° to −35.9°C. Interpretation as due to vacancy diffusion of H2O molecules.]CrossRefGoogle Scholar
Riehl, N. Protonic mobility and its importance for biological systems. Transactions of the New rork Academy of Sciences, Ser. 2, Vol. 27, No. 7, 1965, p. 772–81. [Discussion of proton motion along hydrogen bonds, particularly in ice. Also published in Phillips, G. O., ed. Energy transfer in radiation processes. Chemical, physical and biological aspects. Proceedings of the international symposium held at Cardiff, January, 1965. Amsterdam, Elsevier, 1966, p. 95–104.]CrossRefGoogle Scholar
Roedder, E. Metastable superheated ice in liquid-water inclusions under high negative pressure. Science, Vol. 155, No. 3768, 1967, p. 1413–57. [Retention of ice up to +6.5°C in liquid inclusions in minerals with negative pressure of c. 1000 bar.]CrossRefGoogle ScholarPubMed
Roulleau, M. Poc, M.-M. Electrocongelation des brouillards surfondus. Comptes Rendas Hebdomadaires des Séances de l’Académie des Sciences (Paris), Sér. B, Tom. 264, No. 21, 1967, p. 1480–83. [Strong electric field causes freezing of supercooled mist droplets.]Google Scholar
Shreve, R. L. Migration of air bubbles, vapor figures and brine pockets in ice under a temperature gradient. Journal of Geophysical Research, Vol. 72, No. 16, 1967, p. 4093–100. [Theory, and comparison with reported experiments.]CrossRefGoogle Scholar
Soules, J. A. Improved sophomore experiment to measure latent heat of fusion. American Journal of Physics, Vol. 35, No. 1, 1967, p. 23–26. [Two forms of teaching experiment to determine latent heat of fusion of ice.]CrossRefGoogle Scholar
Starr, J. R. Mason, B. J. The melting of small ice spheres and cones. Quarterly Journal of the Royal Meteorological Society, Vol. 92, No. 394, 1966, p. 500–09. [Times of complete melting in airstreams of controlled temperature, humidity and velocity measured and compared with theory.]Google Scholar
Sutherland, Bill. Exact solution of a two-dimensional model for hydrogen-bonded crystals. Physical Review Letters, Vol. 19, No. 3, 1967, p. 103–04. [Solution of two-dimensional ice lattice in electric field.]CrossRefGoogle Scholar
Tippe, A. Zum Piezoeffekte bei Eis I. Naturwissenschaften, 54. Jahrg., Ht. 3, 1967, p. 68–69. [Explanation of effect observed by A. Deubner, R. Heise and K. Wenzel, ibid., 47. Jahrg., Ht. 24, 1960, p. 600–01, as not due to piezoelectricity.]CrossRefGoogle Scholar
Weissmann, M., and others. On the hydrogen bond in an ice-like structure, [by] M. Weissmann, L. Blum and N. V. Cohan. Chemical Physics Letters, Vol. 1, No. 3, 1967, p. 95–98. [Comparison of various methods of calculating hydrogen-bond energy between water molecules in ice.]CrossRefGoogle Scholar
Williamson, R. B. Chalmers, B. Morphology of ice solidified in undercooled water. (In Peiser, H. S., ed. Crystal growth. Proceedings of an international conference on crystal growth, Boston, 20–24 June 1966. Oxford, etc. Pergamon Press, [c 1967], p. 739–43.) [Study of shapes of crystals formed at different supercooling and explanation.]Google Scholar
Yosida, Z. Kōri no kesshō no hyómen kōzō. I. Kesshō teimen no kōzō, keiri no kesshō no heikōkei . Teion-kagaku , Ser. A, Vol. 24, 1966, p. 1–18. [Theory of equilibrium form of ice surface. English extended summary p. 14–18.]Google Scholar
Zhitnikov, R. A. Kolesnikov, N. V. Teoreticheskoye rassmotreniye matrichnykh sdvigov rasshchepleniy sverkhtonkoy struktury dlya atomov Cu, Ag i Au, stabilizirovannykh v polyarnoy matritse (ILO) . Fizika Tverdogo Tela , Tom 9, Vyp. 1, 1967, p. 162–66. [Results for Ag and Au in good agreement with theory. English translation in Soviet Physics-Solid State, Vol. 9, No. 1, 1967, p. 121–24]Google Scholar
Zimbrick, J. Kevan, L. Evidence for trapped dielectrons in ice. Journal of the American Chemical Society, Vol. 89, No. 10, 1967, p. 2483–84. [Letter. After high y-irradiation electron resonance studies suggest two electrons can be trapped in the same OH− vacancy.]CrossRefGoogle Scholar

Land Ice Glaciers. Ice shelves

Adamson, R. G. Cavaney, R. J. Volcanic debris-layers near Mount Melbourne, northern Victoria Land, Antarctica. New Zealand Journal of Geology and Geophysics, Vol. 10, No. 2, 1967, p. 418–21. [Description of layers in Campbell Glacier.]CrossRefGoogle Scholar
Bayrock, L. A. Catastrophic advance of the Steele Glacier, Yukon, Canada. Alberta University. Boreal Institute. Occasional Publication No. 3, 1967, 35 p. [Report of survey, 20–23 August 1966. Maximum rate of flow was 46 ft (14 m) per 24 h mainly by slipping at the base. At the toe, most of the motion could be accounted for by shearing along the base.]Google Scholar
Behrendt, J. C., and others. Geophysical reconnaissance in the Pensacola Mountains, by J. C. Behrendt, J. R. Henderson and L. J. Meister. Antarctic Journal of the U.S., Vol. 1, No. 4, 1966, p. 125–26. [Helicopter survey made during 1965–66 austral summer included seismic reflection. gravity and aeromagnetic studies.]Google Scholar
Beitzel, J. E. Bentley, C. R. Geophysical investigations in Marie Byrd Land. Antarctic Journal of the U.S., Vol. 2, No. 4, 1967, p. 95–97. [Measurements of ice thickness, required for reduction of gravity data as well as for glaciological purposes.]Google Scholar
Bowman, G. C. Directional characteristics of ionosende interference patterns from the Filchner Ice Shelf. AVCO Corporation, AVCO Space Sÿslems Division, Wilmington, Mass., Contract NSF-C403, Antarctic Research and Data Analysis, Scientific Report 24, AVSSD-0224–66-CR, 1966, 34 p. [Use of apparatus intended to study ionosphere to find depth of ice shelf and dielectric constant of its ice.]Google Scholar
Brecher, H. H. Measurements of ice-surface movement by aerial triangulation. Antarctic Journal of the U.S., Vol. 2, No. 4, 1967, p. 123. [Variation of accumulation along line of markers was strikingly similar during two time intcrvals]Google Scholar
Browne-Cooper, P. J., and others. Probable local seismicity at Wilkes, Antarctica, [by] P. J. Browne-Cooper, G. R. Small and R. Whitworth. New Zealand Journal of Geology and Geophysics, Vol. 10, No. 2, 1967, p. 443–45. [Includes seismic records attributed to “ice-quakes”.]CrossRefGoogle Scholar
Crozaz, G. Langway, C. C. jr. Dating Greenland firn-ice cores with Ph-210. Earth and Planetary Science Letters, Vol. 1, No. 4, 1966, p. 194–96. [Method applied to depth profile of North Greenland ice sheet.]CrossRefGoogle Scholar
Einarsson, E. H. Sudurbrún Mÿrdalsjökuls viò Gvendarfell. Breytingar sioustu 100 ár 0. fl. Jökull, [Vol.] 3, Ár 16, 1966, p. 216–18. [Variations of the southern margin of Mÿrdalsjökull at Gvendarfell. Between about 1870 and about 189n the glacier margin advanced, but from then until 1966 it was on the whole retreating.]CrossRefGoogle Scholar
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Icebergs. Sea, River and Lake Ice

Adams, W. P. Shaw, J. B. Studies of ice cover on Knob Lake, New Quebec. Cahiers de Géographie de Québec, 11e An., No. 2, 1967, p. 88–96. [Systematic observations of lake ice cover in the vicinity of Schefferville, Quebec.]CrossRefGoogle Scholar
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Glacial Geology

Brown, M. J. F., and others. A new radiocarbon date for Wales, by M. J. F. Brown, L D. Ellis-Gruffydd, H. D. Foster, D. J. Unwin. Nature, Vol. 213, No. 5082, 1967, p. 1220–21. [Results in new views on southern limit of Würm ice in Irish Sea basin.]CrossRefGoogle Scholar
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Frost Action on Rocks and Soil. Frozen Ground. Permafrost

Anderson, D. W., and others. Frost phenomena on Mars, by D. W. Anderson, E. S. Gaffney and P. F. Low. Science, Vol. 155, No. 3760, 1967, p. 319–22. [Suggests frost phenomena are not to be expected on Mars without strongly deliquescent soils.]CrossRefGoogle Scholar
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Dylik, J. Traces fossiles de l’évolution descendante des polygones des fentes de gel. Tijdschrift van het koninklijk Nederlandsch Aardrijkskundig Genootschap, Deel 83, No. 3, 1966, p. 227–37. [Discussion of what can be learnt by studying fossil frost-wedge polygons.]Google Scholar
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[Frozen Ground: Canada.] Permafrost in Canada. Canada. Geological Survey. Dept. of Energy, Mines and Resources. Map 1246A, 1967. [Scale 1: 7 603 200.] 50 c. [Shows extent of continuous and discontinuous permafrost zones and occurrence of permafrost at high elevations, with other data. Explanatory notes on definition of permafrost, distribution and occurrence, physical factors influencing permafrost and a bibliography of source information are printed on the map.]Google Scholar
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Meteorological and Climatological Glaciology

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Snow

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