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Glaciological Literature

Published online by Cambridge University Press:  24 March 2017

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Journal of Glaciology , Volume 7 , Issue 50 , 1968 , pp. 355 - 360
Copyright
Copyright © International Glaciological Society 1968

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

Glaciological Instruments and Methods

Gitlin, S. N., and others. A calorimetric method for measuring water content of hailstones, by S. N. Gitlin, H. S. Fogler and G. G. Goyer. Journal of Applied Meteorology, Vol. 5, No. 5, 1966, p. 715–21.2.0.CO;2>CrossRefGoogle Scholar
Knight, C. A. Formation of crystallographic etch pits on ice, and its application to the study of hailstones. Journal of Applied Meteorology, Vol. 5, No. 5, 1966, p. 710–14. [New technique for etching ice described and applied to hailstones.]2.0.CO;2>CrossRefGoogle Scholar
Welch, R. A comparison of aerial films in the study of the Breidamerkur glacier area, Iceland. Photograrnrnetric Record, Vol. 5, No. 28, 1966, p. 289–306. [Colour, infrared, false colour and panchromatic film tried in experiments in 1965. Two latter considered superior.]CrossRefGoogle Scholar
Williams, R. J. Meryman, H. T. A calorimetric method for measuring ice in frozen solutions Cryobiology. Vol. 1, No. 5,1965 p. 317–23.CrossRefGoogle ScholarPubMed

Physics of Ice

Adamson, A. W., and others. Physical adsorption of vapors on ice. I. Nitrogen [by] A. W. Adamson, L. M. Dormant and M. Orem. Journal of Colloid and Interface Science, Vol. 25, No. 2, 1967, p. 206–17. [Ice powder at 77°K gives adsorption isotherms which suggests surface is not highly polar.]CrossRefGoogle Scholar
Akitt, J. W. Lilley, T. H. The nature of hydrogen bonding in ice and water: ‘H nuclear magnetic resonance data on ice. Chemical Communications, 1967, No. 7, p. 323–24. [Narrow line observed inconsistent with usual view of hydrogen bonding in ice.]Google Scholar
Anantha, N. G. Chalmers, B. Electrical phenomena occurring during freezing of dilute aqueous solutions. Journal of Applied Physics, Vol. 38, No. 11, 1967, p. 4416–20. [Study of potential developed at surface during freezing of NH4OH and NH4Cl solutions. Explanation of effect.]CrossRefGoogle Scholar
Anderson, D. M. Ice nucleation and the substrate-ice interface. Nature, Vol. 216, No. 5115, 1967, p. 563–66. [Discussion of the theory of heterogeneous nucleation of ice.]CrossRefGoogle Scholar
Anderson, D. M. The interface between ice and silicate surfaces. Journal of Colloid and Interface Science, Vol. 25, No. 2, 1967, p.174–91. [Evidence for liquid-like layer.]CrossRefGoogle Scholar
Angell, C. A., and others. Concentrated electrolyte solution transport theory: directly measured glass temperatures and vitreous ice, [by] C. A. Angell, E. J. Sare [and] R. D. Bressel. Journal of Physical Chemistry, Vol. 71, No. 8, 1967, p. 2759–61. [Letter. Measurements of glass transition in concentrated solutions of Ca(NO3)2 in H2O gives curve which extrapolates to pure vitreous ice transition temperature.]CrossRefGoogle Scholar
Bailey, I. H. Macklin, W. C. The effect of impurities on the mechanical strength of accreted ice. Journal of the Atmospheric Sciences, Vol. 24, No. 6, 1967, p. 707–10. [Experiments with a number of organic impurities.]2.0.CO;2>CrossRefGoogle Scholar
Boger, D. V. Westwater, J. W. Effect of buoyancy on the melting and freezing process. Transactions of the American Society of Mechanical Engineering, Vol. 89, No. 1, 1967, p. 81–89. [Measurements of freezing rates with and without convection.]Google Scholar
Brivati, J. A., and others. Electron spin resonance studies of the hydroxyl radical in y-irradiated ice. by J. A. Brivati, M. C. R. Symons, D. J. A. Tinling, H. W. Wardale and D. O. Williams. Transactions of the Faraday Society, Vol. 63, No. 9, 1967, p. 2112–16. [Study of electron spin resonance spectra of H2O and D2O irradiated at 77° K shows lack of axial symmetry of OH radical.]CrossRefGoogle Scholar
Brownscombe, J. L. Hallett, J. Experimental and field studies of precipitation particles formed by the freezing of supercooled water. Quarterly Journal of the Royal Meteorological Society, Vol. 93, No. 398, 1967. p. 455–73. [Physical basis for interpreting shape, bubble and crystal structure of accreted ice.]CrossRefGoogle Scholar
Bryant, G. W. Thermoelectric power of single crystals of ice containing HF or NH3 . Philosophical Magazine. Eighth Ser., Vol. 16, No. 141, 1967, p. 495–504. [Measurements in agreement with Jaccard’s theory.]CrossRefGoogle Scholar
Clifford, J. Proton magnetic resonance data on ice. Chemical Communications, 1967, No. 17, p. 880–81. [Width of resonance line implies a proton spin-spin relaxation time of 5–10 μs. A narrow line is also observed and its origin is discussed in terms of liquid water or non-hydrogen-bonded water molecules.]Google Scholar
Cross, J. D. The electret effect in ice. Journal of the Electrochemical Society, Vol. 115, No. 1, 1968, p. 42–45. [Measurement of behaviour of ice single crystals and polycrystalline ice at −70°C.]CrossRefGoogle Scholar
Dibdin, G. H. E. S. R. of γ-irradiated single crystals of ice at 77°K. Identification of the hydroxyl radical and its trapping site. Transactions of the Faraday Society, Vol. 63. No. 9, 1967, p. 2098–111. [Trapping sites identified as 24 sites differing only in orientation. Annealing of radicals studied.]CrossRefGoogle Scholar
Drost-Hansen, W. The water-ice interface as seen from the liquid side. Journal of Colloid and Interface Science. Vol. 25. No. 2, 1967, p. 131–60. [Review of properties of ice and of what happens on molecular scale in freezing process.]CrossRefGoogle Scholar
Durand, M., and others. Bulk conductivity of ice between −25 and −100°C with ion exchange membranes, [by] M. Durand, M. Deleplanque and A. Kahane. Solid State Communications, Vol. 5, No. 9, 1967, p. 759–60. [Activation energy found to be about 9 kcal/mol to −70°C and about 13 kcal/mol below.]CrossRefGoogle Scholar
Evans, L. F. Ice nucleation under pressure and in salt solution. Transactions of the Faraday Society, Vol. 63, No. 12, 1967, p. 3060–71. [Organic compounds which nucleate ice do so better under pressure or with dissolved salt.]CrossRefGoogle Scholar
Evans, L. F. Selective nucleation of the high-pressure ices. Journal of Applied Physics, Vol. 38, No. 12, 1967, p. 4930–32. [Use of selective nucleators to produce any required polymorph of ice from liquid at high pressure except ice II or VII.]CrossRefGoogle Scholar
Faure, P. Kahane, A. Interprétation des spectres optiques de basse fréquence de la glace à l’aide d’un modéle dynamique du réseau cristallin. Journal de Physique, Tom. 28, No. 11–12, 1967, p. 944–50. [Interpretation of low-frequency infrared and Raman spectra of ice in terms of dynamical model of the lattice. English abstract.]CrossRefGoogle Scholar
Frank, F. C. Regelation: a supplementary note. Philosophical Magazine, Eighth Ser., Vol. 16, No. 144, 1967, p. 1267–74. [Discussion of stability of ice-water interface in front of and behind a wire or other body moving through ice.]CrossRefGoogle Scholar
Glen, J. W. The effect of hydrogen disorder on dislocation movement and plastic deformation of ice. Physik der kondensierten Materie, Bd. 7, Ht. 1, 1968, p. 43–51. [Because of H disorder, dislocations can only move through ice if electrical point defects move and reverse H-bonds. French and German abstracts.]Google Scholar
Gross, G. W. Ion distribution and phase boundary potentials during the freezing of very dilute ionic solutions at uniform rates. Journal of Colloid and Interface Science, Vol. 25, No. 2, 1967, p. 270–79. [Experiments and theoretical interpretation.]Google Scholar
Hobbs, P. V. Scott, W. D. Surface diffusion at the ice-air interface. Journal of Colloid and Interface Science, Vol. 25, No. 2, 1967, p. 228–30. [Theory of surface diffusion which explains apparent anomaly between theory and experiment.]CrossRefGoogle Scholar
Hoekstra, P. Miller, R. D. On the mobility of water molecules in the transition layer between ice and a solid surface. Journal of Colloid and Interface Science, Vol. 25, No. 2, 1967, p. 166–73. [Experiments on migration of water along transition layer under electrical and temperature gradients.]CrossRefGoogle Scholar
Itagaki, K. Some surface phenomena of ice. Journal of Colloid and Interface Science, Vol. 25, No. 2, 1967, p. 218–27. [Neck formation between ice sphere and plane close to it. Particle migration on a subliming ice surface.]CrossRefGoogle Scholar
Jellinek, H. H. G. Liquid-like (transition) layer on ice. Journal of Colloid and Interface Science, Vol. 25, No. 2, 1967, p. 192–205. [Survey of ideas on and evidence for liquid-like layer.]CrossRefGoogle Scholar
Jellinek, H. H. G. Ibrahim, S. H. Sintering of powdered ice. Journal of Colloid and Interface Science, Vol. 25, No. 2, 1967, p. 245–54. [Rate of decrease of surface area of 0.5 μm ice spheres measured. Main cause is thought to be plastic flow under surface forces.]CrossRefGoogle Scholar
Ketcham, W. M. Hobbs, P. V. The preferred orientation in the growth of ice from the melt. Journal of Crystal Growth, Vol. 1, No. 5, 1967, p. 263–70. [Experimental study of criteria by which one grain wedges out another.]CrossRefGoogle Scholar
Knight, C. A. The contact angle of water on ice. Journal of Colloid and Interface Science, Vol. 25, No. 2, 1967, p. 280–84. [Observation of angle of surfaces of thin layer of water freezing on a copper plate used to deduce information about surface energies.]CrossRefGoogle Scholar
Knight, C. A. Spiral air bubbles in ice. Nature, Vol. 214, No. 95, 1967, p. 1324–25. [Discussion of origin of spiral bubbles formed in freezing 0.1% NaCl solution.]CrossRefGoogle Scholar
Kopp, M. Processes on the surface of ice. Surface Science, Vol 7, No. 3, 1967, p. 302–08. [Survey of surface phenomena and calculation of activation energies for release and mobility on freshly crystallized and on annealed ice basal planes.]CrossRefGoogle Scholar
Krausz, A. S. Gold, L. W. Surface features observed during thermal etching of ice. Journal of Colloid and Interface Science, Vol. 25, No. 2, 1967, p. 255–62. [Description of etching of grain boundaries and linear and hillock-like features.]CrossRefGoogle Scholar
Kuhns, I. E. Mason, B. J. The supercooling and freezing of small water droplets falling in air and other gases. Proceedings of the Royal Society, Ser. A, Vol. 302, No. 1471, 1968, p. 437–52. [Study of temperature of freezing, interpretation on homogeneous nucleation theory.]Google Scholar
Landy, M. Freiburger, A. Studies of ice adhesion. I. Adhesion of ice to plastics. Journal of Colloid and Interface Science, Vol. 25, No. 2, 1967, p. 231–44. [Measurement for 29 rigid plastics. Correlation with type of chemical bond and flexural modulus.]CrossRefGoogle Scholar
Latham, J. Stow, C. D. Charge transfer associated with the evaporation of ice in electric fields. Journal of the Meteorological Society of Japan, Vol. 44, No. 5, 1966, p. 286–90. [Experiments described.]Google Scholar
Lavrov, V. V. Koeffitsiyent Puassona l’da pri staticheskoy nagruzke . Problemy Arktiki i Antarktiki , Vyp. 26, 1967, p. 49–52.Google Scholar
LeFebre, V. The freezing potential effect. Journal of Colloid and Interface Science, Vol. 25, No. 2, 1967, p. 263–69. [The potential developed on freezing dilute ionic solutions is explained in terms of a model of the ice-solution interface.]CrossRefGoogle Scholar
Lieb, E. H. Residual entropy of square ice. Physical Review, Ser. 2, Vol. 162, No. 1, 1967, p. 162–72. [Exact calculation of residual entropy of two-dimensional analogue of ice.]CrossRefGoogle Scholar
Nozik, A. J. Kaplan, M. Mössbauer resonance studies of ferrous ions in ice. Journal of Chemical Physics, Vol. 47, No. 8, 1967, p. 2960–71. [Study of ice frozen from FeCl2 and FeSO4 solutions. Quenching liquid to −196°C produces cubic ice. Role of ferrous ions and their position in ice lattice discussed.]CrossRefGoogle Scholar
Nunn, K. R. Rowell, D. M. Regelation experiments with wires. Philosophical Mazagine, Eighth Ser., Vol. 16, No. 144, 1967, p. 1281–83. [Observations of velocity of movement of wires of various dimensions and thermal conductivities pulled through ice.]CrossRefGoogle Scholar
Nye, J. F. Theory of regelation. Philosophical Magazine, Eighth Ser., Vol. 16, No. 144, 1967, p. 1249–66. [Detailed study of theory of motion of a wire or other object through ice. Discussion of discrepancies between theory and experiment.]CrossRefGoogle Scholar
Odencrantz, F. K. Buecher, R. W. Temperature-dependence of the polarity of electrical charges on ice crystals. Science, Vol. 158, No. 3798, 1967, p. 256–57. [Sign of charge on ice crystals formed from supercooled cloud appears to be related to crystal habit.]CrossRefGoogle ScholarPubMed
Pruppacher, H. R. Interpretation of experimentally determined growth rates of ice crystals in supercooled water. Journal of Chemical Physics, Vol. 47, No. 5, 1967, p. 1807–13. [Measurements of growth rate in basal plane discussed on basis of theories that it is heat-flow controlled or molecular kinetic. Both phenomena are important.]CrossRefGoogle Scholar
Pruppacher, H. R. Some relations between the structure of the ice-solution interface and the free growth rate of ice crystals in supercooled aqueous solutions. Journal of Colloid and Interface Science, Vol. 25, No. 2, 1967. p. 285–94. [Measurements of growth rate of ice in supercooled water and solutions.]CrossRefGoogle Scholar
Schiller, R. Radiation chemistry of ice. I. Nature and pH dependence of the reducing species. Journal of Chemical Physics, Vol. 47, No. 7, 1967, p. 2281–83. [No free electrons detected in ice whereas they are found in water. pH dependence of H atom yield.]CrossRefGoogle Scholar
Stecher, T. P. Williams, D. A. An observational distinction between interstellar grain models. Publications of the Astronomical Society of the Pacific, Vol. 78, No. 465, 1966, p. 549–50. [How to distinguish between ice and graphite models by observation.]CrossRefGoogle Scholar
Townsend, D. W. Vickery, R. P. An experiment in regelation. Philosophical Magazine, Eighth Ser., Vol. 18. No. 144, 1967, p. 1275–80. [Measurements of the movement of objects of different geometries and thermal properties pulled through ice.]CrossRefGoogle Scholar
Vertsner, V. N. Zhdanov, G. S. Elektronno-mikroskopicheskoye issledovaniye nizkotemperaturnykh modifikatsiy l’da . Kristallografiya , Tom 10, No. 5, 1965, p. 715–22. [Observations of hexagonal, cubic and amorphous ice. English translation: Soviet Physics-Crystallography, Vol. 10, No. 5, 1966, p. 597–602.]Google Scholar
Webb, W. W. Hayes, C. E. Dislocations and plastic deformation of ice. Philosophical Magazine, Eighth Ser. Vol. 16, No. 143, 1967, p. 909–25. [Direct observations of dislocations using X-ray topographic technique.]CrossRefGoogle Scholar
Whalley, E. Bertie, J. E. The far infrared spectrum and long-range forces in ice. Journal of Colloid and Interface Science, Vol. 25, No. 2, 1967, p. 161–65. [Evidence from infrared spectra for long-range forces which may account for surface effects in ice.]CrossRefGoogle Scholar
Zimbrick, J. Kevan, L. Paramagnetic relaxation of trapped electrons in irradiated alkaline ices. Journal of Chemical Physics, Vol. 47, No. 7, 1967, p. 2364–71. [Study of relaxation times and line widths and interpretation.]CrossRefGoogle Scholar

Land Ice. Glaciers. Ice Shelves

Brocas, J. Picciotto, E. Nickel content of Antarctic snow: implications of the influx rate of extra-terrestrial dust. Journal of Geophysical Research, Vol. 72, No. 8, 1967, p. 2229–36. [Analysis of samples of firn. Concludes that total extra-terrestrial mass accreted by earth is 3–10 million tons per year.]CrossRefGoogle Scholar
Brunger, A. G., and others. Recession of the Hector and Peyto Glaciers: further studies in the Drummond Glacier, Red Deer valley area, Alberta, by A. G. Brunger, J. G. Nelson and I. Y. Ashwell. Canadian Geographer, Vol. 11, No. 1, 1967, p. 35–48. [Estimates based on photographs, tree-ring data, and ablation data.]CrossRefGoogle Scholar
Evers, W. Welches ist der höchste Berg Norwegens? Petermann Geographische Mitteilungen, Jahrg. 111, 4. Quartalsht., 1967, p. 278. [Whether Glittertind or Galdhopiggen is highest mountain of Norway depends on depth of snow and firn on Glittertind. In recent years this decreased so as to raise doubts, but it has now increased again.]Google Scholar
Ferrero, G. M. Moto ondoso in un ranale glaciale. Bollcttino del Comitato Glaciologico Italiano, 2 Ser., No. 12, Pt. 1, 1962, [pub.] 1966, p. 11–22. [Study of formation and propagation of waves in glacial channel containing viscous fluid, due to disturbance in part of channel. English summary.]Google Scholar
Harrison, A. E. Alaskan glacier surges. Alaska Sportsman, Vol. 33, No. 8, 1967, p. 14–16, 50. [Describes glacier surges with particular reference to Muldrow Glacier.]Google Scholar
Hochstein, M. P. Pressure ridges of the McMurdo Ice Shelf near Scott Base, Antarctica. New Zealand Journal of Geology and Geophysics. Vol. 10, No. 4, 1967, p. 1165–68. [Letter. Drilling and scientific equipment were tested in the pressure ridge area of the ice shelf near Scott Base. Some results of glaciological interest are presented.]CrossRefGoogle Scholar
Ives, J. D. Glacier terminal features in northeast Baffin Island: illustrations with descriptive notes. Geographical Bulletin, Vol. 9. No. 1, 1967, p. 62–70. [These include a normal valley glacier, the termini of a transection glacier system, an outlet glacier supplied by a plateau ice cap, and a cirque glacier.]Google Scholar
Ives, J. D. Glaciers. Canadian Geographical Journal, Vol. 74, No. 4, 1967, p. 110–17. [Pictorial introduction to glaciology.]Google Scholar
Lorius, C. Vallon, M. Étude structurographique d’un glacier antarctique. Comptes Rendus Hebdomadaires des Séances de l’Académie des Sciences (Paris), Sér. D, Tom. 265, No. 4, 1967, p. 315–18. [Interpretation of core from ice in coastal region of Terre Adélie interpreted in terms of origin of ice.]Google Scholar
McCorkell, R., and others. Aluminium-26 and beryllium-10 in Greenland ice, by R. McCorkell, E. L. Fireman and C. C. Langway. Science, Vol. 158, No. 3809, 1967, p. 1690–92. [Measurement of these radioisotopes in 200–year old Greenland ice.]CrossRefGoogle Scholar
Peretti, L. Charrier, G. Senalazione ed analisi pollinica di torba alla fronte attuale del Ghiacciaio del Rutor (Valle d’Aosta). Considerazioni di paleogeografia e paleoclimatologia locale. Bollettino del Comitato Glaciologico Italiano, 2 Ser., No. 14, Pt. 1, 1964, [pub.] 1967, p. 13–31. [Pollen analytical evidence that in the past the glacier has retreated still further than the present-day position.]Google Scholar
Tyulina, T. Yu. Puti resheniya problemy dvizheniya lednikov . Izuestiya Akademii Nauk SSSR. Seriya Geograficheskaya , 1967, No. 4, p. 118–21. [Review of methods of solving problems of glacier flow, particularly by model experiments.]Google Scholar
Vivian, R. Fiches des glaciers français. Le Glacier Blanc. Revue de Géographie Alpine, Tom. 55, Fasc. 4, 1967, p. 729–32. [Summary of knowledge of this glacier.]CrossRefGoogle Scholar
Vivian, R. Fiches des glaciers français. Le Glacier Noir. Revue de Géographie Alpine, Tom. 55, Fasc. 4, 1967, p. 733–36. [Summary of knowledge of this glacier.]CrossRefGoogle Scholar
Wood, W. A. Glaciology: chaos in nature. Explorers Journal, Vol. 45, No. 2, 1967, p. 79–87. [Investigations of Steele Glacier, Yukon Territory, Canada, during its catastrophic advance.]Google Scholar

Icebergs. Sea, River and Lake Ice

Brown, J. R. Milne, A. R. Reverberation under Arctic sea-ice. Journal of the Acoustical Society of America, Vol. 42, No. 1, 1967, p. 78–82. [Measurements of backscattering strength and correlation with surface roughness.]CrossRefGoogle Scholar
Carstens, T. Experiments with supercooling and ice formation in flowing waters. Geofysiske Publikasjoner, Vol. 26, No. 9, 1966, 18 p. [Confirms that supercooling is function of rate of heat loss and of quality of flow.]Google Scholar
Iizuka, H., and others. Microorganisms in plankton-ice of the Antarctic Ocean, [by] H. Iizuka, I. Tanabe and H. Meguro. Journal of General and Applied Microbiology, Vol. 12, No. 1, 1966, p. 101–02.CrossRefGoogle Scholar
Kagan, B. A. O prilivnom dreyfe l’da . Izvestiya Akademii Nauk SSSR. Fizika Atmosfery i Okeana , Tom 3, No. 8, 1967, p. 881–89. [Formulae for velocity of ice drift, tidal level oscillations, profile of tidal current and eddy coefficients. English translation in Izvestiya. Academy of Sciences, U.S.S.R. Atmospheric and Oceanic Physics, Vol. 3, No. 8, 1967 [pub. 1968], p. 512–16.Google Scholar
Kheysin, D. Ye. O chicle Reynoldsa dlya bitykh l’dov . Problemy Arktiki i Antarktiki , Vyp. 26, 1967, p. 53–56.Google Scholar
Koptev, A. P. O roll snezhnogo pokrova v protsessakh teploobmena . Problem, Arktiki i Antarktiki , Vyp. 22, 1966, p. 82–89. [Effect when snow cover lies on floating ice.]Google Scholar
Kupetskiy, V. N. O lyuministsentsii morskikh l’dov . lzvestiya Vsesoyuznogo Geograicheskogo Obshchestva , Tom 99, Vyp. 1, 1967, p. 67–70. [Further examples of observation of this phenomenon.]Google Scholar
Lake, R. A. Heat exchange between water and ice in the Arctic Ocean. Archiv fib. Meteorologie, Geophysik and Bioklimatologie, Ser. A, Bd. 16, Ht. 2–3. 1967, p. 242–59. [Evaluation of heat balance terms on bottom surface of sea ice on basis of measurements of ice and water temperature, current velocity, and ablation or accretion of ice.]CrossRefGoogle Scholar
Mahrenholtz, O. Zur Tragfähigkeit von Eisdecken. Zeitschrift für angewandte Mathematik and Mechanik, Bd. 46, Sonderheft, 1966, p. T170–73. [Computation of load-bearing capacity of ice layers.]CrossRefGoogle Scholar
Meguro, H., and others. Ice flora (bottom type): a mechanism of primary production in polar seas and the growth of diatoms in sea ice, by H. Meguro, K. Ito and H. Fukushima. Arctic, Vol. 20, No. 2, 1967, p. 114–33. (Study of diatoms which cause layered structure of sea ice off Barrow, Alaska.]CrossRefGoogle Scholar
Nazintsev, Yu. L. O ravnovesnom sostoyanii polyarnykh l’dov . Problemy Arktiki i Antarktiki , Vyp. 25, 1967, p. 77–83. [Factors affecting maximum thickness and rate of growth of floating ice in Arctic Ocean.]Google Scholar
Payne, F. A. Further measurements on the effect of ice cover on shallow-water ambient sea noise. Journal of the Acoustical Society of America, Vol. 41, No. 5, 1967, p. 1374–76. [Measurements at Prince Edward Island.]CrossRefGoogle Scholar
Robinson, E. S. Seismic wave propagation on a heterogeneous polar ice sheet. Journal of Geophysical Research, Vol. 73, No. 2, 1968, p. 739–53. [Analysis of Antarctic results in terms of wave-guide theory of seismic propagation.]CrossRefGoogle Scholar
Shesterikov, N. P. O pogloshchenii solnechnoy radiatsii l’domod snezhnitsey . Problemy Arktiki i Antarktiki , Vyp. 25, 1967, p. 66–70. [Floating ice.]Google Scholar
Zakharov, V. F. Bulatov, L. V. K otsenke velichiny stayayshego l’da v otkrytom more . Problemy Arktiki i Antarktiki , Vyp. 22, 1966, p. 127–28. [Method of approximate calculation of amount of melting which takes place as temperature rises.]Google Scholar

Glacial Geology

Andrews, J. T. Barry, R. G. Zamechaniya po povodu stat’i ob otsupanii amerikanskogo lednika . Izvestiya Vsesoyuznogo Geograficheskogo Obshchestva , Tom 99, Vyp. 3, 1967, p. 230–31. [Comments on paper by N. R. Malkin, ibid., Tom 98, Vyp. 4, 1966, p. 326–32.]Google Scholar
Denton, G. H. Stuiver, M. Late Pleistocene glacial stratigraphy and chronology, northeastern St. Elias Mountains, Yukon Territory, Canada. Geological Society of America. Bulletin, Vol. 78, No. 4, 1967, p. 485–510. [Interpretation based on twenty 14C dates.]CrossRefGoogle Scholar
Donn, W. L. Ewing, M. A theory of ice ages. III. Science, Vol. 152, No. 3720, 1966, p. 1706–12. [Modification of theory proposed in Science, Vol. 127, No. 3307, 1958, p. 1159–62.]CrossRefGoogle ScholarPubMed
Gillberg, G. Further discussion of the lithological homogeneity of till. Geologiska Ftireningens i Stockholm Förhandlingar, Vol. 89, Pt. 1, No. 528, 1967, p. 29–49. [Study of moraines using granulometry, Ca analysis and distribution diagrams. Interpretation in terms of ice movement.]CrossRefGoogle Scholar
Gjessing, J. Potholes in connection with plastic scouring forms. Geografiska Annaler, Vol. 49a, No. 2–4, 1967. p. 178–87. [Description of form of potholes and discussion of their origin.]CrossRefGoogle Scholar
Grosval’d, M. G. Novaya lednikovaya gipoteza. A. T. Uilson: Velikiy shel’fovy lednik Antarktidy i drevniye oledeneniya Zemli . Materialy Glyatsiologicheskikh Issledovaniy. Khronika. Obsuzhdeniya , 12, 1966, p. 315–18. [Critique of Wilson’s hypothesis in light of recent mass balance calculations.]Google Scholar
Hälbich, I. W. Observations on primary features in Fish River series and the Dwyka series in South West Africa. Transactions and Proceedings of the Geological Society of South Africa, Vol. 67, 5964 [pub. 1967], p. 95–109. [Direction of movement of glaciers determined.]Google Scholar
Katasonov, Ye. M. L’dy v morskikh otlozheniyakh . Priroda , 1967, No. 6, p. 107–10. [Buried sea ice in northern Siberia.]Google Scholar
King, C. A. M. Buckley, J. T. The chronology of deglaciation around Eqe Bay and Lake Gillian, Baffin Island, N.W.T. Geographical Bulletin, Vol. 9, No. 1, 1967, p. 20–32. [The stages of deglaciation are traced and related to sea-level.]Google Scholar
Malkin, N. R. Otstupaniye amerikanskogo lednika i smeshcheniye putel tsiklonov . Izvestiya Vsesoyuznogo Geograficheskogo Obshchestva , Tom 98, Vyp. 4, 1966, p. 326–32. [Discussion of North American glacial history in terms of theory of glacier fluctuations based on changing paths of depressions.]Google Scholar
Mercer, J. H. Glacier resurgence at the Atlantic/sub-boreal transition. Quarterly Journal of the Royal Meteorological Society, Vol. 93, No. 398. 1967. p. 528–34. [Suggests the cool phase was as severe as at the start of the sub-Atlantic.]CrossRefGoogle Scholar
Shumilov, N. A. O dinamike pokrovnykh lednikov posiednego oledeneniya . Izvestiya Vsesoyuznoga Geograficheskogo Obshchestva , Tom 99, Vyp. 3, 1967, p. 195–207.Google Scholar
Worsfold, R. J. Physiography and glacial geomorphology of Heimefrontfjella, Droning Maud Land. British Antarctic Survey Bulletin, No. 11, 1967, p. 49–57. [Results of geological and topographical surveying carried out in 1963–64 and 1964–65 from Halley Bay station.]Google Scholar

Frost Action on Rocks and Soil. Frozen Ground. Permafrost

Bendix-Almgreen, S. E., and others. Notes on the geology and geomorphology of the Carey Øer, north-west Greenland, [by] S. E. Bendix-Almgreen, B. Fristrup and R. L. Nichols. Meddelelser om Grønland, Bd. 164, Nr. 8, 1967, 16 p. [Periglacial features such as frost-cracks, solifluction lobes, frost mounds, frost-shattered rock, talus, permafrost and snowbank trimlines are common in this group of small islands.]Google Scholar
Chambers, M. J. G. Investigations of patterned ground at Signy Island, South Orkney Islands. II. Temperature regimes in the active layer. British Antarctic Survey Bulletin, No. 10, 1966, p. 71–83. [Analysis of soil temperature records shows surface meteorological data to be inadequate for predicting freeze-thaw cycles.]Google Scholar
Gentileschi, M. L. Forme crionivali sul Gran Sasso d’Italia. Bollettino della Society Geografica italiana, Ser. 9, Vol. 8, Fase. 1–3, 1967, p. 34–61. [Description of periglacial forms above 2 000 m in this part of Italy. English summary.]Google Scholar
Gentileschi, M. L. Forme crionivali sulla Maiella. Bollettino della Socield Geografca Italian, Ser. 9, Vol. 8, Fase. 7–9, 1967, p. 325–50. [Description of periglacial forms above 2 000 m in this part of Italy. English summary.]Google Scholar
Schenk, E. On the formation of string bogs and aapamoors of the Arctic and Antarctic. Zeitschrift für Geomorphologie, Bd. 10, Ht. 4, 1966, p. 346–68. [These formations are attributed to collapse of permafrost.]Google Scholar
Washburn, A. L. Instrumental observations of mass-wasting in the Mesters Vig district, northeast Greenland. Meddelelser om Grenland, Bd. 166, Nr. 4, 1967, 296 p. [Quantitative observations carried out from 1956 to 1961 at a number of experimental sites and resulting conclusions.]Google Scholar
Werner, M., and others. On the detection of water on the Moon, [by] M. Werner, T. Gold and M. Harwit. Planetary and Space Science, Vol. 15, No. 4, 1967, p. 771–74. [If permafrost layer exists below surface of Moon it should produce water vapour detectable from Earth.]CrossRefGoogle Scholar
Williams, P. J. Pore pressures at a penetrating frost line and their prediction. Géolechnique, Vol. 16, No. 3, 1966, p. 187–208. [Apparatus described for determining pore pressures developed immediately below a penetrating frost line.]CrossRefGoogle Scholar
Zamoruyev, V. V. Kamennyye gletchery v khrebte Khamar-Daban . Izvestiva Vsesoyuznogo Geograficheskogo Obshchestva , Tom 97, Vyp. 1, 1965. p. 80–81.Google Scholar

Meteorological and Climatological Glaciology

Bailey, I. H. Macklin, W. C. Heat transfer from artificial hailstones. Quarterly Journal of the Royal Meteorological Society, Vol. 94, No. 399, 1968, p. 93–98. [Rates of melting measured.]CrossRefGoogle Scholar
Bailey, I. H. Macklin, W. C. The surface configuration and internal structure of artificial hailstones. Quarterly Journal of the Royal Meteorological Society, Vol. 94, No. 399, 1968, p. 1–11. [Study of hailstones grown in a wind tunnel. Drag coefficients measured.]CrossRefGoogle Scholar
Browning, K. A. The growth environment of hailstones. Meteorological Magazine, Vol. 96, No. 1140, 1967, p. 202–11. [Discussion of two models.]Google Scholar
Browning, K. A. The lobe structure of giant hailstones. Quarterly Journal of the Royal Meteorological Society, Vol. 92, No. 391, 1966. p. 1–14. [Photographs of thin sections through 5 giant hailstones presented to portray their bubble and crystal structures.]CrossRefGoogle Scholar
Macklin, W. C. Bailey, I. H. On the critical liquid water concentrations of large hailstones. Quarterly Journal of the Royal Meteorological Society, Vol, 92, No. 392, 1966, p. 297–300.CrossRefGoogle Scholar
Marshunova, M. S. Rusin, N. P. Sravnitelnaya kharakteristika radiatsionnogo rezhima Arktiki i Antarktiki . Problemy Arktiki i Antarktiki , Vyp. 24, 1966, p. 30–34.Google Scholar
Mossop, S. C., and others. Studies of ice crystals in natural clouds, by S. C. Mossop, A. Ono and K. J. Heffernan. Journal de Recherches Atmosphériques, Vol. 3, No. 2, 1967, p. 45–64. [Continuous particle sampler used in aircraft to replicate particles in clouds. Shapes under different conditions illustrated. Concentration of ice particles larger than expected.]Google Scholar
Pyatnenkov, B. A. O radiatsionnom balanse atmosfery Antarktiki . Problemy Arktiki i Antarktiki , Vyp. 24, 1966, p. 35–45. [Discussion of factors affecting radiation in Antarctic.]Google Scholar
Rosinski, J. Solid water-insoluble particles in hailstones and their geophysical significance. Journal of Applied Meteorology, Vol. 5, No. 4, 1966, p. 481–92. [Number and concentration of particles found and interpreted.]2.0.CO;2>CrossRefGoogle Scholar
Young, R. G. E. Browning, K. A. Wind tunnel tests of simulated spherical hailstones with variable roughness. Journal of the Atmospheric Sciences, Vol. 24, No. 1, 1967, p. 58–62. [Determination of drag coefficient.]2.0.CO;2>CrossRefGoogle Scholar

Snow

Aldaz, L. Deutsch, S. On a relationship between air temperature and oxygen isotope ratio of snow and fun in the South Pole region. Earth and Planetary Science Letters, Vol. 3, No. 3, 1967, p. 267–73. [Relationship between oxygen isotope ratio and temperature of effective condensation level]CrossRefGoogle Scholar
Burrows, D. A., and others. Factors affecting the electric charge acquired by an ice sphere moving through natural snowfall, [by] D. A. Burrows, P. V. Hobbs and W. D. Scott. Monthly Weather Review, Vol. 95, No. 12, 1967, p. 878–83. [Measurements show positive charge when graupel present, otherwise sign depends on atmospheric electric field. Mechanism discussed.]2.3.CO;2>CrossRefGoogle Scholar
Gunn, K. L. S. The number flux of snow crystals at the ground. Monthly Weather Review, Vol. 95, No. 12, 1967, p. 921–24. [Measurements show that main contribution to increase in snowfall rate is formation of new crystals rather than growth of existing ones.]2.3.CO;2>CrossRefGoogle Scholar
Magono, C. Orikasa, K. Models of charge distribution in and under clouds during snowfall. Journal of the Meteorological Society of Japan, Vol. 44, No. 5, 1966, p. 280–85. [Several models proposed which explain observed surface electric fields.]Google Scholar
Magono, C. Orikasa, K. On the disturbance of surface electric field caused by snowfall. Journal of the Meteorological Society of Japan, Vol. 44, No. 5, 1966, p. 260–79. [Analysis of results of observations.]Google Scholar
Protsenko, V. K Ob izmerenii plotnosti snezhnogo pokrova . Meteorologca i Gidrologiya , 1967, No. 7, p. 105–07. [Comparison of measurement using permanent markers with 1 km survey strips.]Google Scholar
Vanni, M. La marche de la limite inférieure du manteau neigeux temporaire dans la vallée de St. Barthélemy au cours des hivers 1964–65 et 1965–66. Bollettino del Comitato Glaciologico Italiano, 2 Ser., No. 13, Pt. 2, 1962–63, [pub.] 1967, p. 43–54. [Data on the behaviour of the lower limit of the temporary snow cover and some conclusions drawn.]Google Scholar
Vanni, M. Le valanghe nell’alta Valtournanche. Bollettino del Comitato Glaciologico Italiano, 2 Ser., No. 12, Pt. 2, 1961–62, [pub.] 1966, p. 55–64. [Describes avalanches of Valtournanche region, Aosta valley.]Google Scholar
Yen, Y. C. The rate of temperature propagation in moist porous mediums with particular reference to snow. Journal of Geophysical Research, Vol. 72, No. 4, 1967, p. 1283–88. [Heat transfer equation, neglecting effect of radiation and convection but including effect of vapour diffusion in porous media, formulated and solved numerically for snow, in density range from 0.1 to 0.45 g/cm3.]CrossRefGoogle Scholar