Hostname: page-component-745bb68f8f-f46jp Total loading time: 0 Render date: 2025-01-13T08:48:57.180Z Has data issue: false hasContentIssue false
  • English
  • Français

Glaciological Literature

Published online by Cambridge University Press:  30 January 2017

Rights & Permissions [Opens in a new window]

Abstract

An abstract is not available for this content. As you have access to this content, full HTML content is provided on this page. A PDF of this content is also available in through the ‘Save PDF’ action button.
Type
Other
Information
Journal of Glaciology , Volume 8 , Issue 54 , 1969 , pp. 497 - 511
Copyright
Copyright © International Glaciological Society 1969

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

Conferences

[Cloud Physics.] Proceedings of the international conference on cloud physics, August 26–30, 1968, Toronto, Canada. Sponsors: International Association of Metcorolagy and Atmospheric Physics of the International Union of Geodesy and Geophysics, World Meteorological Organization, American Meteorological Society, Canadian Meteorological Society, National Research Council of Canada. No place, no publisher, [1968?]. xv, 873 p. [For details of relevant papers see elsewhere in this list.]Google Scholar
Gold, L. W. Williams, G. P., comp. Ice pressures against structures: proceedings of a conference held at Laval University, Quebec, 10–11 November 1966… with the papers and discussion presented at the seminar on ice formation on lakes and rivers, sponsored by the Canadian National Committee of the International Hydrologic Decade and held at Laval University, Quebec, 9 November 1966. Canada. National Research Council. Associate Committee on Geotechnical Research. Technical Memorandum No. 92, 1968, vi, 247 p. (NRC No. 9851.) $3.50. [Contains papers and discussions from these two meetings and appendixes with associated papers of interest. Papers include: R. F. Legget and L. W. Gold, “Ice pressure on structures—a Canadian problem”, p. 1–4; A. S. Krauss, “Plastic deformation of fresh-water ice”, p. 5–12; L. W. Gold, “Elastic and strength properties of fresh-water ice”, p. 13–23; W. F. Weeks and A. Assur, “The mechanical properties of sea ice”, p. 25–78; G. E. Frankenstein, “Strength of ice sheets”, p. 79–87; G. R. Kendall, “Meteorological information relevant to ice pressures”, p. 89–94; M. Drouin, “Static ice force on extended structures”, p. 95–108; N. Y. Lavoie, “Ice effects on structures in the Northumberland Strait crossing”, p. 109–15; H. R. Peyton, “Sea ice forces”, p. 117–23; J. Nuttall and L. W. Gold, “Model study of ice pressures”, p. 125–30; M. C. van Wijk, “The use of photogrammetry for measuring the movement of ice covers”, p. 131–34; L. W. Gold, “Observations on the movement of ice at a bridge pier”, p. 135–41; R. C. Sommerville and G. E. Burns, “Damage to a Winnipeg reservoir due to ice”, p. 143–51; D. E. Nevel, “Lifting forces exerted by ice on structures”, p. 155–61 B. Michel, “Thrust exerted by an unconsolidated ice cover on a boom”, p. 163–70; P. Donnelly, “An outline of the design and operation of the Montreal ice control structure”, p. 171–84; R. J. Kennedy, “On the expansion of a floating ice sheet with temperature change”, p. 185–87; P. Donnelly, “Montreal ice control structure failure of four stop-logs during winter 1966–67”, p. 189. Statements of research problems pertaining to ice pressures: C. Neill, “Bridge piers and similar isolated structures”, p. 191–94; M. Drouin, “Forces exerted by static ice covers on extended structures”, p. 194–96; B. Michel, “Ice formation and break-up in rivers”, p. 196–99; L. W. Gold, “The forces that ice can exert on structures”, p. 199–202. Papers presented to the seminar on ice formation: G. P. Williams, “Freeze-up and break-up of fresh-water lakes”, p. 203–15; C. E. Deslauriers, “Ice break-up in rivers”, p. 217–29; B. Michel, “Ice covers in rivers”, p. 231–47]Google Scholar

General glaciology

Bruman, J. R. Ice on the moon. Icarus, Vol. 8, No. 1, 1968, p. 198–201. [Proposes that maria and large craters with mare-like floors are result of collisions with large bodies of ice.]Google Scholar
Chorley, R. J., ed. Water, Earth and man. A synthesis of hydrology, geomorphology and socio-economic geography. London, Methuen and Co. Ltd., [c 1969]. xix, 588 p. [Integrated study of water on the Earth. Includes following articles on snow and ice: M. G. Marcus, “The hydrology of snow and ice”, p. 359–67; L S. Evans, “The geomorphology and morphology of glacial and nival arcas”, p. 369–80; B. A. Kennedy, “Periglacial morphometry”, p. 381–88; J. Rooney, “The economic and social implications of snow and ice”, p. 389–401.]Google Scholar
Clark, R. H. Fulton, J. F. The Canadian IHD program. Proceedings of the Western Snow Conference, 35th annual meeting, 1967, p. 105–11. [Review of Canadian activities in the International Hydrological Decade, 1965–74]Google Scholar
Embleton, C. King, C. A. M. Glacial and periglacial geomorphology. [London], Edward Arnold (Publishers) Ltd., 1968. xvi, 608 p.Google Scholar
Kusunoki, H. Atarashii seppyō no jutsugoshū . Seppyō, [Vol.] 29, [No.] 5, 1967, p. 155–62. [Japanese translation of Illustrated glossary of snow and ice, by T. E. Armstrong, B. B. Roberts and C. W. M. Swithinbank.]Google Scholar
Perov, V. F. Snezhniki, lednikl i merzlotnyy rel’yef Khibniskikh gor . Moscow, Izdatel’stvo “Nauka”, 1968. 120 p. (Rezul’Laty Issledovaniy po Mezhdunarodnym Geolizicheskim Proyektam. Glyatsiologiya, No. 22.) [Study of the role of snow patches, small glaciers, and periglacial conditions in geomorphological processes in the area in extreme north-west U.S.S.R. English summary, p. 110–11.]Google Scholar
Quervain, M. R. de. Prof. Dr. Robert Haefeli and die Schnee- and Eisforschung. Schweizerische Bauzeitung, Jahrg. 86, Ht. 31, 1968, p. 541–43. [Summary of R. Haefeli’s contributions to glaciology.]Google Scholar
Weller, G. E. The heat budget and heat transfer processes in Antarctic plateau ice and sea ice. ANARE Scientific Reports. Series A(IV). Glaciology. Publication No. 102, 1968, [vi], 155 p. [Study of surface heat balance and sub-surface balance on blue ice in the coastal ablation zone and sea ice.]Google Scholar
Zavatti, S. Terminologia geoglaciologica polare. Istiluto Geografico Polare. Pubblicazioni Scientifiche, 6, 1969, 20 p. [A list of English glaciological terms, mostly concerned with sea ice, with definitions in Italian and equivalents in Italian and other languages.]Google Scholar

Glaciological instruments and methods

Ambach, W. Eisner, H. Pb-210-Methode zur Datierung von Eis eines alpinen Gletschers. Acta Physica Austriaca, Bd. 27, Ht. 1–3, 1968, p. 271–74. [Data from Kesselwandferner, Austria, presented to show that method based on radioactivity of natural 210Pb can be used to date temperate glacier ice.]Google Scholar
Burge, W. Parker, D. C. Infrared survey in Antarctica. Antarctic Journal of the United States, Vol. 3, No. 4, 1968, p. 120. [Preliminary report of evaluation of air-borne survey which differentiates many snow and ice features.]Google Scholar
Davis, B. L. Blair, D. N. An isothermal cloud chamber for use with x-ray diffraction. Proceedings of the international conference on cloud physics, August 26–30, 1963, Toronto, Canada, [1068?], p. 275–79. [Technique for quantitative X-ray study of newly formed ice particles in artificial cloud.]Google Scholar
Gottfried, G. J. Campbell, C. J. A shielded thermistor probe with portable instrument for measuring snowpack temperatures. U.S. Forest Service Research Note RM-120, 1968, 3 p. [Device for measuring temperature profiles through snow to 0.1°C.]Google Scholar
Lliboutry, L. Implantation et exploitation d’un réseau de balises d’ablation glaciaire. (In Mélanges offierts par ses amis et disciples à Maurice Pardé. Paris, Editions Ophrys, 1968, p. 373–86.) [Practical rules for the use of stakes to measure ablation on a glacier.]Google Scholar
Matthews, B. Automatic measurement of frost-heave: results from Malham and Rodley (Yorkshire). Geoderma, Vol. 1, No. 2, 1967, p. 107–15. [Description of instrument.]CrossRefGoogle Scholar
Odencrantz, F. K. Humiston, L. E. Replicator for ice crystals. Review of Scientific Instruments, Vol. 39, No. 12, 1968, p. 1870–72. [Apparatus for making in the field replicas of small ice crystals suitable for optical or scanning electron microscope examination.]Google Scholar
Owe-Berg, T. G. Gaukler, T. A. Confinement of charged particles in a nonuniform AC field. Proceedings of the international conference on cloud physics, August 26–30, 1968, Toronto, Canada, [1968?], p. 861–65. [Apparatus for suspending charged ice particles or droplets.]Google Scholar
Sasaki, I. Tōkairin, A. Ēsu shitsudokei no teion tokusei ni tsuite . Seppyō, [Vol.] 30, [No.] 4,108, p. 103–10. [Tests on this hygrometer with small sensing element made of pith of a plant, show it to be very suitable for low temperature use, e.g. above an ice surface. English abstract.]Google Scholar
Smith, F. M., and others. Measuring snow depths by aerial photogrammetry: evaluation and recommendations, by F. M. Smith, C. F. Cooper and E. G. Chapman. Proceedings of the Western Snow Conference, 35th annual meeting, 1967, p. 66–72. [Discusses reliability and usefulness.]Google Scholar
Takahashi, K. Saishin sekisetsu shishikei ni tsuite . Seppyō, [Vol.] 30, [No.] 4, 1968, p. 111–14. [Report of a device for recording the maximum depth which snow attained. English abstract.]Google Scholar
Takahashi, Y. A practical and simple method for determining the number of ice nuclei in air. Proceedings of the international conference on cloud physics, August 26–30, 1968, Toronto, Canada, [1968?], p. 217–21.Google Scholar
Warner, C. Gunn, K. L. S. Measurement of snowfall by optical attenuation. Journal of Applied Meteorology, Vol. 8, No. 1, 1969, p. 110–21. [Description of method of measuring falling snow which gives good time resolution.]Google Scholar
Watanabe, S. Nezu, S. Sekisetsu chinkōryoku no ichi kansokurei . Seppyō, [Vol.] 30, [No.] 3, 1968. p. 70–72. [Measurement of force on a horizontal board I m above ground level. English abstract.]Google Scholar

Physics of ice

Arnold, G. P., and others. Neutron diffraction study of ice polymorphs. III. Ice Ic, [by] G. P. Arnold, E. D. Finch, S. W. Rabideau and R. G. Wenzel. Journal of Chemical Physics, Vol. 49, No. 10, 1968, p. 4365–69. [Neutron diffraction study at 80 K of polycrystalline D2O cubic ice.]CrossRefGoogle Scholar
Aufdermaur, A. N. Relations between the local heat and mass transfer and the local accretion rate. Proceedings of the international conference on cloud physics, August 26–30, 1963, Toronto, Canada, [1968?], p. 411–15. [Laboratory measurements.]Google Scholar
Bagdade, W. A. Far infrared absorption in disordered materials. Dissertation Abstracts, B, Vol. 28, No. 1, 1967, p. 312–B-313–B. [Analysis of absorption due to randomized charges applied, among other things, to ice Ih. Abstract of dissertation submitted to University of California, Berkeley. Copies of original available from University Microfilms, Ann Arbor, Mich., U.S.A. Order No. 67–8516.]Google Scholar
Bajorek, A., and others. Investigation of the dynamics of water molecules in crystallo-hydrates by neutron inelastic scattering, by A. Bajorek [and 9 others]. (In Neutron inelastic scattering. Proceedings of a symposium on neutron inelastic scattering held by the International Atomic Energy Agency in Copenhagen 20–25 May, 1968. Vol. 2, Vienna, I.A.E.A., 1968, p. 143–58.) [Neutron inelastic scattering used to determine translatory and rotatory frequencies of (among other things) H2O ice and comparison with infrared data.]Google Scholar
Bertie, J. E Far infrared spectra of the ices. Applied Spectroscopy, Vol. 22, No. 6, 1968, p. 634–40. [Comparison of spectra of ice Ih, Ic, II, V, VI and IX.]Google Scholar
Bol, W. X-ray diffraction and structure of water. Journal of Applied Crystallography, Vol. 1, Pt. 4, 1968 [pub. 1969], p. 234–41. [X-ray diffraction study of liquid water used to deduce radial distribution function which is compared with that for the various phases of ice.]CrossRefGoogle Scholar
Brickmann, J. Zimmermann, H. Lingering time of the proton in the wells of the double-minimum potential of hydrogen bonds. Journal of Chemical Physics, Vol. 50, No. 4. 1969, p. 1608–18. [Calculation of variation with time of chance of finding a proton in either of two wells of symmetrical or asymmetrical double-minimum potential due to quantum-mechanical tunnel effect.]Google Scholar
Brivati, J. A., and others. Unstable intermediates. Part LIX. Electron spin resonance studies from 4 to 77°K of hydrogen-bonded hydroxyl radicals in γ-irradiated ice, by J. A. Brivati, M. C. R. Symons, D. j. A. Tinling, and D. O. Williams. Journal of the Chemical Society, Sect. A, 1969, [Pt.] 4, p. 719–20. [Anomalous spectra at 77 K from hydrogen bonded hydroxyl radicals shown to result from librations frozen out at lower temperatures]CrossRefGoogle Scholar
Brownscombe, J. L. Thorndike, N. S. C. The freezing of water droplets in free fall. Proceedings of the international conference on cloud physics, August 26–30, 1963, Toronto, Canada, [1968?], p. 280–84. [Study of possibility of splintering during freezing.]Google Scholar
Bullemer, B., and others. Experiments on the nature of charge carriers in ice, by B. Bullemer, H. Engelhardt, L. Knoblauch, N. Richl and C. Schroder-Etzdorf. Solid State Communications, Vol. 6, No. 8, 1968, p. 545–47. [Guard-ring method used to separate bulk from surface conductivity and to establish that majority bulk carriers are protons.]CrossRefGoogle Scholar
Clee, T. E. Internal friction in ice near its melting point. Journal of Geophysical Research, Vol. 74, No. 4, 1969, p. 973–80. [Measurements in Athabasca Glacier for waves from 0.025 to 1.0 kHz show greater attenuation in pure shear than pure dilatation.]Google Scholar
Dantl, G. Alterungsvorgänge in einkristallinem Eis. Polarforschung, Bd. 6. Jahrg. 37, Ht. 1–2, 1967 [pub. 1968], p. 129–32. [Summary of physical properties dice single crystals which are found to change with time since crystal was grown.]Google Scholar
Dézsi, I., and others. Mössbauer study of SnCl2 and Dy(ClO4)3 in ice, by I. Dézsi, N. A. Eissa, L. Keszthelyi, B. MMiolnár, and D. L. Nagy. Physica Status Solidi, Vol. 30, No. 1, 1968, p. 215–18. [Mössbaucr lines in frozen solutions of both salts disappear above −90°C.]Google Scholar
DiLorenzo, J. V. Kaplan, M. Pseudo-melting of doped ice at −65° C. Chemical Physics Letters, Vol. 2, No. 7, 1968, p. 509–12. [Mössbauer studies on ice doped with both 57Fe and 151Eu give results quite different from those with either doping separately. The results indicate a pseudo-melting at −65°C.]Google Scholar
Drake, J. C. Electrification accompanying the bursting of air bubbles in melting ice. Proceedings of the international conference on cloud physics, August 26–30, 1963, Toronto, Canada, [1968?], p. 614–18.Google Scholar
Finch, E. D., and others. Neutron diffraction study of ice polymorphs. II. lee I I, [by] E. D. Finch, S. W. Rabideau, R. G. Wenzel and N. G. Nereson. Journal of Chemical Physics, Vol. 49, No. 10, 1968, P. 4361–65. [Neutron diffraction study of polycrystalline D2O ice II is in agreement with the structure predicted by Kamb.]CrossRefGoogle Scholar
Fischer, S. F., and others. Proton-phonon coupling in a hydrogen bonded system, [by] S. F. Fischer, G. L. Hofacker and J. R. Sabin. Physik der kondensierten Materie, Bd. 8. Ht. 4. 1969, p. 268–78. [A one-dimensional theory of proton movement in an ice-like system shows coupling with phonons.]Google Scholar
Fletcher, N. H. Ice nucleation behavior of silver iodide smokes containing a soluble component. Journal of the Atmospheric Sciences, Vol. 25, No. 6, 1968, p. 1058–60. [Calculation of nucleation ability on assumption that process is nucleation of droplet.]2.0.CO;2>CrossRefGoogle Scholar
Ford, T. A. Falk, M. Hydrogen bonding in water and ice. Canadian Journal of Chemistry, Vol. 46, No. 22, 1968, p. 3579–86. [Measurement of infra-red absorption spectra of ice and interpretation in terms of distribution of intermolecular energies.]Google Scholar
Fukuta, N. Some remarks on ice nucleation by metaldehyde. Proceedings of the international conference on cloud physics, August 26–30, 1968, Toronto, Canada, [1968?], p. 194–98. [Study of reasons for efficiency as nucleator, and of shape of crystals produced.]Google Scholar
Gabarashvili, T. G. Kartsivadze, A. I. Influence of electric fields upon processes of ice nucleus formation. Proceedings of the international conference on cloud physics, August 26–30, 1968, Toronto, Canada, [1968?], p. 188–93. [Experiments show sign of charge to be important.]Google Scholar
Gliki, N. V. Gromova, T. N. The simplest types of crystallization of supercooled water drops. Acta Crystallographica, Vol. 21, Pt. 7, Suppl., 1966, p. A258–59. [Abstract only. Study of freezing of drops with different impurities reveals three simple types of crystallization.]Google Scholar
Gokhale, N. R. Goold, J. jr. Ice-nucleating properties of meteoritic materials and soil particles. Proceedings of the international conference on cloud physics, August 26–30, 1968, Toronto, Canada, [1968?], p 238–42. [Experiments which indicate that meteoritic material is not very efficient at ice nucleation.]Google Scholar
Gukhman, A. A. Volynets, A. Z. O kharaktere sublimatsii l’da v vakuume . Iuzhenerno-Fizicleskiv Zhurnal, Tom 15, No. 5, 1968, p. 777–81. [Experiment and theory show stationary process is one in which phase transition occurs in a layer, not on geometric surface. English summary.]Google Scholar
Hallett, J. The influence of defect structure on the growth of ice crystals. Proceedings of the international conference on cloud physics, August.26–30, 1968, Toronto, Canada, [1968?], p. 199–203. [Dislocation structure may influence habit of ice crystals and explain e.g. triangular crystals.]Google Scholar
Hamilton, W. C. Iberis, J. A. Hydrogen bonding in solids: methods of molecular structure determination. New York, Amsterdam, W. A. Benjamin, Inc., 1968. xv, 284 p. [Book on hydrogen bonding. One chapter deals with ice and similar materials.]Google Scholar
Hardy, S. C. Coriell, S. R. Morphological stability and the ice-water interfacial free energy. Journal of Crystal Growth, Vol. 3–4, 1968, p. 569–73. [Measurement of growth rates of slightly perturbed single crystal ice cylinders, and calculation of surface free energy from results. Discussion by L. A. Tarshis.]CrossRefGoogle Scholar
Harling, O. K. The dynamics of liquid H2O and D2O and solid H2O from the inelastic scattering of epithermal neutrons. (In,Neutron inelastic scattering. Proceedings of a symposium on neutron inelastic scattering held by the International Atomic Energy Agency in Copenhagen 20–25 May, 1968. Vol. 1. Vienna, I.A.E.A., 1968, p. 507–19.) [Results of neutron inelastic scattering studies of H2O and D2O ice to give rotational and vibrational levels and Debye-Waller factor. Discussion in ibid., p. 521–22.]Google Scholar
Hase, H. Kevan, L. Spatial distribution of trapped electrons in alkaline ice produced by photoionization. Journal of the American Chemical Society, Vol. 90, No. 24, 1968, p. 6875–76. [Letter. Study of ice containing NaOH and K4Fe(CN)6 after photoionization. Difference from effect of y-irradiation.]CrossRefGoogle Scholar
Helmreich, D. Bullemer, B. Anomales elastisches Verhalten von Eis bei tiefen Temperaturen. Physik der kondensierten Materie, Bd. 8, Ht. 5, 1969, p. 384–92. [Elastic constants of ice single crystals show anomalies at c. 105 K which are attributed to a proton-ordering phase change.]Google Scholar
Higashi, A., and others. Growth of ice single crystals from the melt with special reference to dislocation structure, [by] A. Higashi, M. Oguro and A. Fukuda. Journal of Crystal Growth, Vol. 3–4, 1968, p. 728–32. [X-ray diffraction topographic study.]CrossRefGoogle Scholar
Higashi, A., and others. Strength of ice single crystals in relation to the dislocation structure, by A. Higashi, S. Mae and A. Fukuda. (In Proceedings of the international conference on the strength of metals and alloys, September 1967, Tokyo, Japan. Tokyo, Japan Institute of Metals, 1968, p. 784–89. (Transactions. Japan Institute of Metals, Vol. 9, Supplement.)) [X-ray topographic studies of ice crystals before and after basal glide, and results of mechanical tests in basal and non-basal glide.]Google Scholar
Higuchi, K. Kōri no kesshō seichō to yūkai . Kagaku no Jikken, [Vol.] 19, [No.] 1, 1968, p. 40–46. [Experiments for schools on growth of ice crystals and observation of Tyndall figures.]Google Scholar
Iaci, G. Lo Savio, M. Conversion 3S → 1S of positronium in the ice-water system. Physics Letters, Vol. 28A, No. 6, 1968, p. 458–59. [New suggestion to explain the behaviour of positronium annihilating in ice.]CrossRefGoogle Scholar
Irvine, W. M. Pollack, J. B. Infrared optical properties of water and ice spheres. Icarus, Vol. 8, No. 2, 1968, p. 324–60. [Critical review of literature on absorption coefficient and reflectivity of ice in infrared. Best values used to compute scattering albedo, asymmetry factor and normalized extinction cross-section of small ice spheres.]Google Scholar
Isono, K. Formation and growth of ice crystals at low pressure. Proceedings of the international conference on cloud pltysics, August 26–30, 1968, Toronto, Canada, [1968?], p. 270–74. [Habit of crystals grown at very low pressure.]Google Scholar
James, D. W. Thermal diffusivity of ice and water between −40 and +60°C. Journal of Materials Science, Vol. 3, No. 5, 1968, p. 540–43. [Measurement parallel to c-axis of single crystal ice.]CrossRefGoogle Scholar
Jellinek, H. H. G. Gouda, V. K. Grain growth in polycrystalline ice. Physica Status Solidi, Vol. 31, No. 1, 1969, p. 413–23. [Laboratory measurements of grain growth of pure ice and ice doped with NaCl.]CrossRefGoogle Scholar
Jhon, M. S. The significant structure theory applied to liquid water and heavy water. Dielectrical properties of liquid water and various forms of ice. The significant structure theory Of isomeric effects. Dissertation Abstracts, B, Vol. 28, No. 1, 1967, p. 135–B. [Dielectric properties of water deduced on assumption of ice-I-like and ice-Ill-like clusters. Theory also applied to solid phases. Abstract of dissertation submitted to University of Utah. Copies of original available from University Microfilms, Ann Arbor, Mich., U.S.A. Order No. 67–15284.]Google Scholar
Johnson, D. A. An experimental investigation of charge separation due Lo the fracture of freezing water drops. Proceedings of the international conference on cloud physics, August 26–30, 1968, Toronto, Canada, [1968?], p. 624–28. [Laboratory studies on pure water and solutions.]Google Scholar
Jones, S. J. Glen, J. W. The effect of dissolved impurities on the mechanical properties of ice crystals. Philosophical Magazine, Eighth Ser., Vol. 19, No. 157, 1969, p. 13–24. [Flow is greatly increased by small amounts of HF; NH3 and NH4F have much less, if any, effect.]Google Scholar
Kachurin, L. G. On the probability of crystallization. Journal of Physics, A, Ser. 2, Vol. 2, No. 1, 1969, p. 137–38. [Establishes the connection between equations for probability of crystallization of supercooled water droplets due to E. R. Bigg, A. E. Carte and L. G. Kachurin.]Google Scholar
Kachurin, L. G. Bekryayev, V. I. Electrification of crystallizing clouds. Proceedings of the international conference on cloud physics, August 26–30, 1968, Toronto, Canada, [1968?], p. 629–34. [Survey of results on drop freezing and the resulting charge.]Google Scholar
Katz, U. The ice-nucleating activity of electrically charged and uncharged CuS particles. Proceedings of the international conference on cloud physics, August 26–30, 1968, Toronto, Canada, [1968?], p. 183–87. [Experiments show electric charge does not noticeably affect nucleating ability.]Google Scholar
Kelly, D. J. Salomon, R. E. Dielectric behavior of NaOH-doped ice. Journal of Chemical Physics, Vol. 50, No. 1, 1969, p. 75–79. [Conductivity and dielectric constant from o to −25°C.]Google Scholar
Knight, C. A. The contact angle of water on ice; the nucleation of supercooled water drops. Proceedings of the international conference on cloud physics, August 26–30, 1968, Toronto, Canada, [1968?], p. 204–07. [Experiment that indicates a non-zero contact angle, and implications for ice nucleation.]Google Scholar
Knollenberg, R. G. A laboratory study of the local cooling resulting from the dissolution of soluble ice nuclei having endothermic heats of solution. Journal of the Atmospheric Sciences, Vol. 26, No. 1, 1969 p. 115–24.Google Scholar
Knollenberg, R. G. The local cooling ice nucleation model. Journal of the Atmospheric Sciences, Vol. 26, No. 1, 1969, p. 125–29. [Theory of high nucleation activity of soluble compounds with endothermic heats of solution.]2.0.CO;2>CrossRefGoogle Scholar
Knollenberg, R. G. A note on the volume free energy associated with soluble ice nuclei. Journal of the Atmospheric Sciences, Vol. 26, No. 1, 1969, p. 177–79.Google Scholar
Komabayasi, M. Shape instability of crystals of ice, carbon dioxide and ammonia grown in a cold chamber. Proceedings of the international conference on cloud physics, August 26–30, 1968, Toronto, Canada, [1968?], p. 260–64. [Theory of shape instability.]Google Scholar
Kotler, G. R. Tarshis, L. A. On the dendritic growth of pure materials. Journal of Crystal Growth, Vol. 3–4, 1968, p. 603–10. [Discussion of theories of dendritic growth and deduction of ice-water surface free energy and linear kinetic coefficient for molecular attachment.]Google Scholar
Latham, J. Experiments in cloud physics for physics students. Proceedings of the international conference on cloud physics, August 26–30, 1968, Toronto, Canada , [1968?], p. 828. [Report of undergraduate projects at University of Manchester Institute of Science and Technology including freezing and electrification of supercooled droplets, thermoelectric effect in ice and growth of ice crystals from the vapour.]Google Scholar
Layton, R. G. Nucleation of ice on single crystals. Proceedings of the international conference on cloud physics, August 26–30, 1968, Toronto, Canada, [1968?], p. 208–12. [Experiments on ice deposition and of ice nucleation from vapour at water saturation.]Google Scholar
Lebedev, D. P. Kristalloobrazovaniye na poverkhnosti sublimiruyushchegosya sloya v usloviyakh sublimatsii l’da v vakuume . Inzhenerno-Fizicheskiy.Zhurnal, Tom 15, No. 5, 1968, p. 794–803. [Experiments showing that process of sublimation in vacuum involves plastic deformation of ice and branch-like growth of crystals which break off. English summary.]Google Scholar
Lykov, A. V., and others. O nekotorykh osobennostyakh mekhanizma sublimatsii i obrazovaniya kristallov l’da v usloviyakh vakuuma . Inzhenerno-Fizicheskiy.Zhurnal, Tom 15, No. 5, 1968, p. 782–87. [Observations of changes in shape of ice crystals growing on cold body and explanation. English summary.]Google Scholar
Macklin, W. C. Ryan, B. F. Interpretation of the growth rates of ice dendrites in supercooled water. Journal of Chemical Physics, Vol. 50, No. 1, 1969, p. 551–52. [Letter. Discussion of implications of growth-rate measurements as a function of supercooling.]Google Scholar
Matsuo, S. Matsubaya, O. Vapour pressure of H2 18O ice. Nature, Vol. 221, No. 5179, 1969, p. 463–64. Measurement of difference of vapour pressure compared with H2 16O ice and deduction of fractionation factor.]Google Scholar
Noll, G. Käss, M. Untersuchung zur Segregation von Ammoniunifluorid bei Eis-Einkristallen. Physik der kondensierten Materie, Bd. 8, Ht. 4, 1969, p. 312–22. [Studies of ice crystals grown from NH4F solution showed non-stoichiometric incorporation in the ice. English and French abstracts.]Google Scholar
Novikov, P. A. Vagner, Ye. A. Issledovaniye mekhanizma teplo- i massoobmena pri sublimatsii l’da v vakuume . Inzhenerno-Fizicheskiy Zhurnal, Tom 15, No. 5, 1968, p. 788–93. [Theory of particle path from surface of a subliming body. English summary.]Google Scholar
Nozik, A. J. Mössbauer resonance studies of ions in ice. Dissertation Abstracts, B, Vol. 29, No. 3, 1968, p. 968–69. [Abstract of dissertation submitted to Yale University. Copies of original available from University Microfilms, Ann Arbor, Mich., U.S.A. Order No. 68–13186.]Google Scholar
Nozik, A. J. Kaplan, M. Paramagnetic and electric quadrupole hyperfine interactions of ferric ions in ice and FeCl3.6H2O. Journal of Chemical Physics, Vol. 49, No. 9, 1968, p. 4141–49. [Mössbauer resonance in 57Fe studied.]Google Scholar
Onsager, L. Runnels, L. K. Diffusion and relaxation phenomena in ice. Journal of Chemical Physics, Vol. 50, No. 3, 1969, p. 1089–1103. [Discussion of rate processes in ice. Dielectric and elastic relaxation attributed to Bjerrum defects, diffusion and proton spin relaxation to interstitial migration.]Google Scholar
Owe-Berg, T. G., and others. Conversion of water vapor to ice by silver iodide, [by] T. G. Owe-Berg, J. E. Clutter, T. A. Gaukler and R. L. McDonald. Journal of the Atmospheric Sciences, Vol. 25, No. 3, 1968, p. 464–69. [Cloud chamber experiments which show that water vapour first condenses and then freezes.]Google Scholar
Pena, J. A., and others. Freezing of water droplets in equilibrium with different gases, [by] J. A. Pena, R. G. de Pena and C. L. Hosier. Journal of the Atmospheric Sciences, Vol. 26, No. 2, 1969, p. 309–14. [Study of shattering of water droplets in equilibrium with different gases when frozen at temperatures between −4 and −14°C.]Google Scholar
Plaude, N. O. Ice-nucleation properties of silver iodide. Proceedings of the international conference on cloud physics, August 26130, 1968, Toronto, Canada, [1968?], p. 174–77. [Experiments on number of active nuclei produced.]Google Scholar
Rabideau, S. W., and others. Proton and deuteron NMR of ice polymorphs, [by] S. W. Rabideau and E. D. Finch and A. B. Denison. Journal of Chemical Physics, Vol. 49, No. 10, 1968, p. 4660–65. [Studies on ices Ih, Ic, II, V, VI and IX support bent hydrogen-bond model.]Google Scholar
Ramseier, R. O. Origin of preferred orientation in columnar ice. Journal of Crystal Growth, Vol. 3–4, 1968, p. 621–24. [Rule for determining from their crystal orientation which grains will grow in area at the expense of others.]Google Scholar
Rüter, H. Berechnung der Richtungsabhängigkeit der P-Wellen-Geschwindigkcit in polykristallinen Eisproben mit vorgegebener C-Achsen-Verteilung aus den elastischen Konstanten des Einkristalls. Polarforschung, Bd. 6, Jahrg. 37, Ht. 1–2, 1967 (pub. 1968], p. 175–77. [Method of calculating approximate P-wave velocities in ice of given distribution of c-axes. English abstract.]Google Scholar
St. Louis, P. T. Steele, R. L. Certain environmental effects on silver iodide ice nuclei. Proceedings of the international conference on cloud physics, August 26–30, 1968, Toronto, Canada, [1968?], p. 178–82. [Study of influence of water vapour and ultra-violet irradiation on nucleation effectiveness.]Google Scholar
Saunders, C. P. R. The influence of cloud electrification on ice crystal aggregation. Proceedings of the international conference on cloud physics, August 26–30, 1968, Toronto, Canada, [1968?], p. 619–23. [Laboratory experiments on effect of electric field on aggregation.]Google Scholar
Schaefer, V. J. Cheng, R. J. The effect of the nucleus on ice crystal structure. Proceedings of the international conference on cloud physics, August 26–30, 1968, Toronto, Canada, [1968?], p. 255–59. [Study of habit of ice crystals nucleated in various ways.]Google Scholar
Scott, W. D. Hobbs, P. V. The charging of ice surfaces exposed to natural ice particles. Proceedings of the international conference on cloud physics, August 26–30, 1968, Toronto, Canada, [1968?], p. 609–13. [Experimental study of charge transferred to an ice surface by impact of ice particle.]Google Scholar
Seidensticker, R. G. Longini, R. L. Impurity effects in ice. Journal of Chemical Physics, Vol. 50, No. 1, 1969, p. 204–13. [Statistics of proton population in ice doped with HF or NH3.]Google Scholar
Shimizu, K., and others. The rectification effects using the ices doped with electrolytes, [by] K. Shimizu, Y. Yoshida, M. SenO and H. Nozaki. Bulletin of the Chemical Society of Japan, Vol. 41, No. 10, 1968, p. 2325–30. [Observation of rectification by junctions between ice doped with proton donors and proton acceptors, including polymers.]Google Scholar
Shio, H. Magono, C. Kōri no masalsu denki to masatsu ni yoru hyōmen no henka . Scppyō, [Vol.] 29, [No.] 5, 1967, p. 140–49. [Variation with temperature and time. English abstract.]Google Scholar
Shio, H. Magono, C. Tankesshōhyō to takesshōhyō no aida no masatsu denki . Seppyō, [Vol.] 30, [No.] 2, 1968, p. 40–44.. [Effects which occur when ice rods of different temperature are rubbed together. English abstract.]Google Scholar
Siegle, G. Weithase, M. Spin-Gitter-Relaxation der Protonen in hexagonalem Eis. Zeitschrift für Physik, Bd. 219, Ht. 4, 1969, p. 364–80. [Measurements of proton spin-lattice relaxation times, which seem to be largely determined by motion of Schottky defects.]Google Scholar
Silver, E. G. A pulsed-neutron investigation of the effect of temperature on the decay of a thermal-neutron population in H2O ice. Nuclear Science and Engineering, Vol. 34, No. 3, 1968, p. 275–84. [Measurement of neutron energy spectrum and neutron diffusion parameters in comparison with effects in water.]Google Scholar
Smith-Johannsen, R. I. Ice crystals. Science, Vol. 163, No. 3870, 1969, p. 958. [Suggests that the whiskers found on replicas of ice crystals by F. K. Odencrantz and others, ibid., Vol. 560, No. 3834, 1968, p. 1345–46, are artifacts of the replication technique.]Google Scholar
Steele, R. L. Davis, C. I. Variation of ice nuclei effectiveness with liquid water. Journal of the Atmospheric Sciences, Vol. 25, No. 2, 1969, p. 329–30. [Effect of presence of liquid water fog on Agi nucleating effectivene;s.]Google Scholar
Sugisaki, M., and others. Calorimetric study of the glassy state. IV. Heat capacities of glassy water and cubic ice, [by] M. Sugisaki, H. Suga and S. Seki. Bulletin of the Chemical Society ofjapan, Vol. 41, No. 11, 1968, p. 2591–99. [Measurement of heat capacity and latent heat associated with glass to Ic and Ic to Ih transitions.]CrossRefGoogle Scholar
Takahashi, T. Thermoelectric properties under the influence of impurity concentration in ice single crystals. Proceedings of the international conference on cloud physics, August 26–30, 1963, Toronto, Canada, [1968?], p. 604–08. [Thermoelectric effect in ice with various impurities and after plastic bending.]Google Scholar
Thijssen, H. A. C., and others. Heterogeneous primary nucleation of ice in water and aqueous solutions, [by] H. A. C. Thijssen, M. A. G. Vorstman and J. A. Rods. Journal of Crystal Growth, Vol. 3–4, 1968, p. 355–59. [Effect of volume, degree of turbulence and rate of cooling.]Google Scholar
Treviño, S., and others. Lattice dynamics of hydrogen-bonded crystals, by S. Treviño, H. Prask and T. Wall and S. Yip. (In Neutron inelastic scattering. Proceedings of a symposium on neutron inelastic scattering held by the International Atomic Energy Agency in Copenhagen 20–25 May, 1968. Vol. 1. Vienna, I.A.E.A., 1968, p. 345–65.) [Dynamical properties of cubic H:O ice and HCI calculated and compared with optical and neutron spectroscopic data. Discussion, p. 362–65.]Google Scholar
Willis, E., and others. “Anomalous” water, by E. Willis, G. K. Rennie, C. Smart [and] B. A. Pethica. Nature, Vol. 222, No. 5189, 1969, p. 159–61. [Letter reporting repetition of Deryagin’s work on a dense form of water produced in fine glass capillaries. Mass spectroscopy, nuclear magnetic resonance both show liquid to behave like normal water.]Google Scholar
Wood, B. E. Smith, A. M. Spectral reflectance of water and carbon dioxide cryodeposits from 0.36 to 1.15 μ.. AIAA Journal (American Institute of Aeronautics and Astronautics), Vol, 6, No. 7. 1968, p. 1362–67. [Spectral reflectance of frost deposits measured eiperimcntally and used to calculate energy reflected for 6000 K black-body radiation.]Google Scholar
Workman, E. J. The possible role of ammonia in thunderstorm electrification. Proceedings of the international conference on cloud physics, August 26–30, 1968, Toronto, Canada, [1968?], p. 653–56. [Laboratory study of charge when drops of water with varying impurity content fall onto cold ice.]Google Scholar
Yannas, I. Vitrification temperature of water. Science, Vol. 160, No. 3825, 1968, p. 298–99. [Study of glass transition in water-glycerol solutions used to estimate transition temperature for water.]CrossRefGoogle ScholarPubMed
Yoshino, T. The reflection properties of radio waves on the ice cap. IEEE Transactions on Antennas and Propagation, Vol. AP-15, No. 4, 1967, p. 542–51. [Measurements of dielectric properties of snow and ice and resulting effect on radio waves in Antarctica. Comment by S. Evans, ibid., Vol. AP-16, No. 3, 1968, p. 363–64.]Google Scholar

Land ice. Glaciers. Ice shelves

Ambach, W. Wärmehaushaltsstudie in Station Carrefour, EGIG, 1967. Polarforschung, Bd. 6, Jahrg. 37, Ht. 1–2, 1967 [pub. 1968], p. 172–74. [Measurement of heat balance at station “Carrefour”, Greenland ice sheet. English abstract.]Google Scholar
Ambach, W., and others. Vertikalverteilung radioaktiver Spaltprodukte im Akkumulationsgebiet eines alpinen Gletschers (Kesselwandferner, Otztaler Alpen), von W. Ambach, H. Eisner and F. A. Prantl. Acta Physica Austriaca, Bd. 27, Ht. 1–3, 1968, p. 46–49. [Study on Kesselwandferner, Austria, of vertical distribution of fission products in accumulation area.]Google Scholar
Brockamp, B. Pistor, P. Ein Beitrag zur seismischen Erforschung der Struktur des grönlandischen Inlandeises. Polarforschung, Bd. 6, Jahrg. 37, Ht. 1–2, 1967 [pub. 1968], p. 133–46. [Study of physical properties of upper layers of Greenland ice sheet by seismic reflection shooting. English abstract.]Google Scholar
Brockamp, B. Thyssen, F. Eine Anwendung der barographisch-topographischcn Kurvc zur Bestimmung der Bewegung von Inlandeisen. Polarforschung, Bd. 6, Jahrg. 37, Ht. 1–2, 1967 [pub. 1968], p. 125–29. [Method of measuring movement of ice sheets based on repeated measurements of barometric pressure by a traversing vehicle, with results for points on Greenland ice sheet. English abstract.]Google Scholar
Cameron, R. L., and others. Glaciology of the Queen Maud Land traverse, 1964–5965, South Pole-Pole of relative inaccessibility, by R. L. Cameron, E. [E.] Picciotto, H. S. Kane, and J. Gliozzi. Ohio State University’. Institute of Polar Studies. Report No. 23, 1968, viii, 136 p. [Measurements and observations, including firn temperature, density and snow accumulation.]Google Scholar
Dansgaard, W. Johnsen, S. J. Comment on paper by J. Weertman, “Comparison between measured and theoretical temperature profiles of the Camp Century, Greenland, borehole”. Journal of Geophysical Research, Vol. 74, No. 4, 1969, p. 1109–10. [Changes in the assumptions concerning vertical ice velccity can remove the disagreement between calculated and observed temperature prcfiles reported by Weertman, ibid., Vol. 73. No. 8, 1968, p. 2691–700.]Google Scholar
Dewart, G. Seismic investigation of ice properties and bcdreck topography at the confluence of two glaciers, Kaskawulsh Glacier, Yukon Territory, Canada. Ohio State University. Institute of Polar Studies. Report No. 27, 1968, xvii, 207 p. [Anisotropy in seismic velocities is duc mainly to foliation, not fabric. Study of bed-rock topography.]Google Scholar
Förtsch, O. Vidal, H. Seismo-glaziologische Untersuchungen im oberen Fischbachtal. Zeitschnift für Gletscherkunde und Glazialgeologie, Bd. 5, Ht. 2, 1968, p. 61–88. [Seismic measurements on $ülztalferner, Austria, interpreted in terms of glacier structure. English summary.]Google Scholar
Golubev, L. N. Formirovaniye rechnogo stoka v gorno-lednikovykh rayanakh (po issledouaniyarrs v tsentral’nem Tyos’-Shane) . Moscow, Izdatel’stvo “Nauka”, 1968. 88 p. (Rezul’taty Issledovany po Mezhdunarodnym Geofizicheskim Proyektam. talyatsiologiya. IX Radzel Programmy MGG, No. 20.) [Detailed study of run-off of small glacierized basin of Chon-Kzylsu river. English summary, p. 80–81.]Google Scholar
Haefeli, R. Changes in the behaviour of the Unteraar glacier in the last 125 years. Bulletin de l’Association Internationale d’Hydrologie Scientifique, 14e An., No. 1, 1969, p. 85–86. [Summary of a longer paper. Variations of ice thickness and velocity and connection with retreat.]Google Scholar
Heuberger, H. Die Alpengletscher im Spät- und Postglazial. Fine chronologische Übersicht. Eiszeitalter und Gegenwart, Bd. 19, 1968, p. 270–75. [Survey of fluctuations of Alpine glaciers since the late-glacial.]Google Scholar
Höllermann, P. Die rer.enten Gletscher der Pyrenäen. Geographica Helvetica, 23. Jahrg., [Ht.] 4, 1968, p. 157–68. [Description of present glaciers in the Pyrenees and their recent variations.]Google Scholar
Jaeger, F. Weiterer Rückgang der Gletscher am Kilimandjaro. Zeitschrift für Gletscherkunde und Glazialgeologie, Bd. 5, Ht. 2, 1968, p. 99–101. [Data on retreat of glaciers on Kilimanjaro.]Google Scholar
Kasser, P. Gletscherbeobachtungen in der Schweiz. Schweizerische Bauzeitung, Jahrg. 86, Ht. 31, 1968, p. 547–50. [Summary of Swiss glacier investigations.]Google Scholar
Loewe, F. Variations of the Qaumarujuk glacier (western Greenland) 1930–1967. Gerlands Beiträge zut Geophysik, Bd. 77, Ht. 3, 1968, p. 232–34. [Retreat and loss of height.]Google Scholar
Lorius, C., and others. Impuretés solubles contenues dans la glace de l’Antarctique, par C. Lorius et G. Baudin, J. Cittanova et R. Platzer, Tellus, Vol. 21, No. 1, 1959, p. 133–48. [Study of ionic concentrations in firn of coastal region of Terre Adélie. English and Russian abstracts.]Google Scholar
McLaren, W. A. A study of the local ice cap near Wilkes, Antarctica. ANARE Scientific Reports. Series A(IV). Glaciology. Publication No. 103, 1968, [vii], 82 p. [Surface and bed topography, accumulation and ice flow determined over a sector of this ice cap, and results used to test theories of glacier flow.]Google Scholar
Meier, M. F. Glaciers and water supply. Journal of the American Water Warks Association, Vol. 61, No. 1, 1969, p. 8–12. [Importance of glaciers as sources of water supply.]Google Scholar
Miller, H. Ceologische und glaziologische Studien in der Westantarktis 1964. Polarforschung, Ed. 6, Jahrg. 37, Ht. 1–2, 1957 [pub. 1968], p. 151–55. [Includes general survey of glaciological features near the Chilean base “General Bernardo O’Higgins”. English abstract.]Google Scholar
Miller, H. Der Höllentalfcrner im Wettcrsteingebirge, seine spät- und nacheiszeitliche Geschichte. zeitschrift für Gletscherkunde und Glazialgeologie, Bd. 5, Ht. 2, 1968, p. 89–97. [Marginal retreat of this German glacier since late-glacial.]Google Scholar
Müller, F. Mittelfristige Schwankungen der Oberflächengeschwindigkeit des Khumbugletschers am Mount Everest. Schweizerische Bauzeitung,, Jahrg. 86, Ht. 31, 1968, p. 569–73. [Study of surface velocity and ablation of the Khumbu glacier (Himalaya) for period of eight months and interpretation of fluctuations of velocity in terms of effects of melt water.]Google Scholar
Naruse, R. Endō, T. Paiagoniya hokubu no hyaga chösa Seppyō, [Vol.] 29, [No.] 6, 1967, p. 167–76. [Observations including ablation and surface ice velocity on Glaciar San Rafael, Glaciar Circo, Glaciar Soler and Glaciar Nef, Chile. English abstract.]Google Scholar
Ommanney, C. S. L., and others. Computer analysis of a glacier inventory of Axel Heiberg Island, Canadian Arctic Archipelago, by C. S. L. Ommanney and R. H. Goodman and F. Müller. Bulletin de l’Association Internationale d’Hydrologie Scientifique, 14e An., No. 1, 1969, p. 19–28. [Description of method for computer analysis of I.H.D. results with examples from Axel Heiberg Island.]Google Scholar
Østrem, G. Stanley, A. Glacier mass-balance measurements. A manual for field and office work. (Revised edition.) Ottawa, Canadian Department of Energy, Mines and Resources, Glaciology Subdivision; Oslo, Norwegian Water Resources and Electricity Board, Glaciology Section, 1969. [vi], 127 p. [Guide for personnel with limited backgrounds in glaciology making I.H.D. measurements. Copies obtainable from Hydrologisk Avd., Norges Vassdrags- og Elektrisitetsvesen, Boks 5091, Oslo 3, Norway.]Google Scholar
Petersen, U. El Glaciar Yanasinga, 19 años de observaciones instrumentales. Boletín de la Sociedad Geotógica del Perú, Tom. 40, 1967, p. 91–97. [Surveys of the snout of this glacier in Peru.]Google Scholar
Poirel, J. Quelques réflexions au sujet des moraines internes et des moraines de fond. Revue de Géomorphologie Dynamique, 18e An., No. 1, 1968, p. 17–26. [Review of internal and basal moraines and their formation and composition, including new observations on the Mer de Glace and glacier d’Argentière.]Google Scholar
Richardson, D. Glacier outburst floods in the Pacific Northwest. U.S. Geological Survey. Professional Paper 600–D, 1968, p. D79–D86. [Descriptions of ‘jökullhlaups”, particularly from glaciers of Mount Rainier, Washington, and discussion of their origin.]Google Scholar
Ruthe, K. Über die Wärmestruktur des antarktischen Eismantels. Polarforsohung, Bd. 6, Jahrg. 37, Ht. 1–2, 1967 [pub. 1968], p. 146. [Summary of paper to be published in Notos on thermal structure of Antarctic ice sheet.]Google Scholar
Shima, M. Yabuki, H. Nankyoku ni okeru uchū busshitsu ni kan-suru kenkyū (I) . Nankyoku Shiryō: Antarctic Record, [No.] 33, 1968, p. 53–64. [Chemical composition and size distribution of cosmic dust collected near “Syowa” station. English abstract.]Google Scholar
Suyetova, I. A. Osnovnyye morformetricheskiye kharakteristiki Antarktidy . Moscow, Izdatel’stvo “Nauka”, 1968. 72 p. (Rezul’taty Issledovaniy po Mezhdunarodnym Geofizicheskim Proyektam. Glyatsiologiya. IX Razdel Programmy MGG, No. 19.) [New study of area, thickness and volume of Antarctic ice sheet, and deductions concerning Antarctic mass balance and volumes of Quaternary ice sheets.]Google Scholar
Temple, P. H. Further observations of the glaciers of the Ruwenzori. Geografiska Annaler, Vol. 50A, No. 3, 1968, p. 136–50. [Observations of fluctuations of four glaciers on the Uganda slopes of the Ruwenzori.]Google Scholar
Temple, P. H. Survey of the Ruwenzori glaciers for recent changes. Nature and Resources, Vol. 5, No. 1, 1969, p. 13–14. [Report of Uganda work under I.H.D. programme.]Google Scholar
Trofimov, A. K. Ploshchad’ rasprostraneniya i osnovnyye etapy razvitiya chetvertichnogo oledeneniya Pamira i Gissaro-Alaya Izvestiya Vsesoyuznogo Geogrqficheskogo Obshchestva, Tom 100, Vyp. 6, 1968, p. 503–1–2. [Study of extent of glaciations in this region of central Asia.]Google Scholar
Vivian, R. Chinal, M. Fiches des glaciers français. Le glacier de Gebroulaz. Revue de Géographie Alpine, Tom. 57, [Fasc.] 2, 1969, p. 429–32. [Summary of knowledge of this glacier.]Google Scholar
Vivian, R. Jail, M. Fiches des glaciers français. Le glacier de Lepena. Revue de Géographie Alpine, Tom. 57, Fasc. 1, 1969, p. 225–27. [Summary of knowledge of this glacier.]Google Scholar
Vivian, R. Jail, M. Fiches des glaciers français. Le glacier du Mulinet. Revue de Géographie Alpine, Tom. 57, [Fasc.] 2, 1969, p. 425–28. [Summary of knowledge of this glacier.]Google Scholar

Icebergs. Sea, river and lake ice

Bilello, M. A. Water temperatures in a shallow lake during ice formation, growth and decay. Water Resources Research, Vol. 4, No. 4, 1968, p. 749–60. [Measurements in Seneca Lake; Michigan, show the water warms up after ice cover has formed, and cools down again in the thaw period.]Google Scholar
Campbell, W. J. Sea-ice dynamics. (In Sater, J. E., coordinator. Arctic drifting stations: a report on activities supported by the Office of Naval Research. Montreal, Washington, New York, Arctic Institute of North America, 1968, p. 189–96.) [Discussion of theory of ice drift and need for more information on theological properties of sea ice.]Google Scholar
Coakley, J. P. Rust, B. R. Sedimentation in an Arctic lake. Journal of Sedimentary Petrology, Vol. 38, No. 4, 1968, p. 1290–300. [Study of sedimentation processes in lake on Somerset Island, Canadian Arctic, which is ice-covered throughout the year apart from marginal melting in summer.]Google Scholar
Cook, R. G. Wade, M. D. jr. Successful ice dusting at Fairbanks, Alaska, 1966. Journal of the Hydraulics Division. Proceedings of the American Society of Civil Engineers, Vol. 94, No. HY1, 1968, p. 31–41. [Effect of dusting in hastening melting of river ice.]Google Scholar
Donn, W. L. Shaw, D. M. The maintenance of an ice-free Arctic Ocean. Progress in Oceanography, Vol. 4, 1967, p. 105–13. [Comparison of heat balance with and without sea ice.]Google Scholar
Harasimiuk, M., and others. Spostrzeżenia nad rolą wiosennego pochodu lodów w procesie akumulacji . Gzasopismo Geograficzne, Tom 39, Zeszyt 3, 1968, p. 273–81. [Effect of a single flood in placing ice fragments containing debris over a flood terrace. English summary.]Google Scholar
Heine, A. J. Brine in the McMurdo Ice Shelf, Antarctica. New Zealand journal of Geology and Geophysics, Vol. 11, No. 4, 1968, p. 829–39. [Results of bore-hole studies of brine infiltration.]Google Scholar
Milne, A. R. Sound propagation and ambient noise under sea ice. (In Albers, V. M., ed. Underwater acoustics. New York, Plenum Press, 1967, Vol. 2, ch. 7, p. 103–38.) [Effects of characteristics of Arctic seas and of ice cover.]Google Scholar
Nakamura, S. Ohoontsuku-kai nantōiki ni akeru hyōen: kansoku to kaisuimennai de no kaiyō kansoku ni tsuite . Seppyō, [Vol.] 30, [No.] 1, 1968, p. 1–6. [Interpretation of observations made each February. English abstract.]Google Scholar
Prebble, M. M. Ice breakout, McMurdo Sound, Antarctica. New Zealand journal of Geology and Geophysics, Vol. 11, No. 4, 1968, p. 908–21. [Relation between break-out of annual ice and shelf ice and the dispersal of pack ice in the Ross Sea.]Google Scholar
Prebble, M. M. Some implications arising from bottom soundings taken around Pram Point, Ross Island, Antarctica. New Zealand journal of Geology and Geophysics, Vol. 11, No. 4, 1968, p. 900–07. [Bottom soundings show earlier hypotheses on reasons for pressure ridges in sea ice and pressure rollers in ice shelf are false.]Google Scholar
Röthlisberger, H. Das Problem der Tragfähigkeit der Eisdecke anlässlich der Zürcher Seegfrörni. Schweizerische Bauzeitung, Jahrg. 86, Ht. 31, 1968, p. 565–69. [Studies to determine the safe bearing capacity of the lake ice on the Zürichsee.JGoogle Scholar
Wawrik, F. Langjährige Daten der Vereisung von Teichen des niederösterreichischen Waldviertels. Wetter and Leben, Jahrg. 20, Ht. 1–2, 1968, p. 19–24. [40 years of observations of freezing of lakes in Lower Austria.]Google Scholar

Glacial geology

Armstrong, R. L., and others. Glaciation in Taylor Valley, Antarctica, older than 2.7 million years, [by] R. L. Armstrong, W. Hamilton [and] G. H. Denton. Science, Vol. 159, No. 3811, 1968, p. 187–89. [Potassium-argon dating shows that glaciations in this area antedated and post-dated this age.]Google Scholar
Aseyev, A. A. Osnovnyye osobennosti klimata Valdayskogo lednikovogo pokrova v period yego maksimal’nogo raspostraneniya . Izaestiya Akademii Ilauk SSSR. Seriya Geografrcheskaya, 1969, No. 1, p. 17–26. [Reconstruction of climate at maximum of Weichsel glaciation.]Google Scholar
Büdel, J. Hang- and Talbildung in Südost-Spitzbergen. Eiszeitalter and Gegenwart, Bd. 19, 1968, p. 240–43. [Glacial and periglacial valley erosion in Svalbard.]Google Scholar
Caine, N. A model for alpine talus slope development by slush avalanching. Journal of Geology, Vol. 77, No. 1, 1969, p. 92–100. [Observations in Southern Alps, New Zealand, suggest talus accumulates in two ways, one of which involves material carried by slush avalanches.]Google Scholar
Clapperton, C. M. Channels formed by the superimposition of glacial meltwater streams, with special reference to the east Cheviot Hills, north-east England. Geografiska Annaler, Vol. 50A, No. 4, 1968, p. 207–20. [Discussion of behaviour of drainage channels in glaciers and how they may change from eng]aeia] to sub-glacial.]Google Scholar
Corbel, J. Karsts et glaciers quaternaires, Irlande et Laponie. Norois, 15e An., No. 60, 1968, p. 469–79. [Discussion of particular problems of glacial erosion and deposition in limestone areas. English summary.]Google Scholar
Crowell, J. C. Frakes, L. A. Late Paleozoic glacial facies and the origin of the South Atlantic Ocean. International Geological Congress. Report of the twenty-third Session, Czechoslovakia, 1968. Proceedings of Section 13. Other subjects, 1968, p. 291–302. [Reconstruction of form of ice cover of the Gondwanaland glaciation.]Google Scholar
Czeppe, Z. The annual rhythm of morphogenetic processes in Spitsbergen. Geographia Polonica, [No.] 14, 1968, p. 57–65. [Seasonal variation of various processes including periglacial ones.]Google Scholar
Duphorn, K. Ist der Oberharz im Pleistozän vergletschert gewesen? Eiszeitalter und Gegenwart, Bd. 19, 1968, p. 164–74. [Study of extent of Pleistocene glaciation in the Harz mountains. English summary.]Google Scholar
Everett, K. R. Behling, R. E. Pedological study in Wright Valley, southern Victoria Land. Antarctic Journal of the United States, Vol. 3, No. 4, 1968, p. 101–02. [Study of moraines below Meserve Glacier to see if age difference can be determined from soil profiles.]Google Scholar
Frakes, L. A., and others. Sedimentological aspects of the Darwin Tillite in the Darwin Mountains, by L. A. Frakes and J. E. Marzolf, T. W. Gevers, and L. N. Edwards and J. C. Crowell. Antarctic, Journal of the United States, Vol. 3, No. 4, 1968, p. 109–10. [Study of this tillite in Victoria Land, Antarctica, and deduction of glacial conditions under which it was deposited.]Google Scholar
George, F. Notes on some glaciation features of Ubekendt Ejland, West Greenland. Geographical Journal, Vol. 135, Pt. 1, 1969, p. 61–65. [Study of present-day cirque glacier and geomorphological features.]Google Scholar
Haase, E. Vorschläge zur Einteilung and Darstellung flächenhafter glazigener Ablagerungen. Neuesjahrbuch fur Geologie and Palaontologie. Monatshefte, Jahrg. 1967, Ht. 3, 1967, p. 159–63. [Suggestion that glacial deposits extending over an area should be subdivided according to their “horizontal density”, i.e. quantity of glacial material per unit area. English and French summaries.]Google Scholar
Hantke, R. Die Diffluenz der würmeiszeitlichen Rheingletschers hei Sargans (Kanton St. Gallen) and die spätglazialen Gletscherstände in der Walensee-Talung und im Rheintal. Eiszeitalter and Gegenwart, Bd. 19, 1968, p. 219–26. [Reconstruction of ice-age glacier surface where it split into two streams and deduction of ice flow. English abstract.]Google Scholar
Haynes, V. M. The influence of glacial erosion and rock structure on corres in Scotland. Geografiska Annaler. Vol. 50A, No. 4, 1968, p. 221–34. [Longitudinal profiles of corres compared with analytical curves, and interpretation of results in terms of structure and process.]Google Scholar
Hewitt, K. Ice-front deposition and the seasonal effect: a Himalayan example. Institute of British Geographers. Transactions, No. 42, 1967, p. 93–106. [Study of deposition of moraine at the front of Biafo Gyang, Kashmir, which may help interpretation of Pleistocene deposits.]Google Scholar
Higuchi, K. Hokkyoku-kai to sono chūhen-chiiki no kishō-teki yaku-wari [The influence of the Arctic ice on climatic change in the northern hemisphere]. Kishui Kenkyli Nōto, [No.] 91, 1967, p. 377–86.Google Scholar
Hoinkes, H. C. Wir leben in einer Eiszeit. (In Murawski, H., ed. Vom Erdkern bis zur Magnetosphere. Frankfurt am Main, Umschau Verlag, 1968, p. 275–88.) [Summary of present knowledge about ice ages.]Google Scholar
Jewtuchowicz, S. Accumulation in stagnant ice, with the Spitsbergen glaciers as example. Geographia Polonica, [No.] 13, 1968, p. 49–56. [Study of processes of deposition of moraine material from stagnant ice in southern Vestspitsbergen in 1959.]Google Scholar
Kirby, R. P. Variation in glacial deposition in a sub-glacial environment: an example from Midlothian. Scottish Journal of Geology, Vol. 5, Pt. 1, 1969, p. 49–53. [Study of drift section showing successive glacial and glaciofluvial deposition in a continuous subglacial environment.]Google Scholar
Kujansuu, R. On the deglaciation of western Finnish Lapland. Bulletin de la Commission Géologique de Finlande, No. 232, 1967, 98 p.Google Scholar
Lewis, C. A. Glacial landforms in Ireland: a guide to teaching. Geographical Viewpoint (Dublin), Vol. 1, No. 4, 1967, p. 201–14. [General description of glacial landforms in Ireland and of the processes believed to have formed them.]Google Scholar
Lüttig, G. Ist die Aeliefcncrgie ein Mass für die Alter der Endmoränen? Eiszeitallcr und Gegenwart, Bd. 19, 1968, p. 139–202. [Attempt to quantify method of estimating age of moraines from their shape. English abstract.]Google Scholar
Lukniš, M. Vaškovský, I. Quaternary of the west Carpathians. International Geological Congress. XXIII Session, Prague 1963. Guide to Excursion 31AC, Czechoslovakia. Bratislava, Geologickÿ Ústav Dionyza Stúra, 1967. 42 p. [Excursion guide to the Quaternary geology of the Vysoké Tatry and the river Vah valley.]Google Scholar
McDonald, B. Deglaciation and differential postglacial rebound in the Appalachian region of southeastern Quebec. Journal of Geology, Vol. 76, No. 6, 1968, p. 664–77. [Study of the deglaciation of last ice sheet in this region.]Google Scholar
McGinnis, L. D. Glaciation as a possible cause of mineral deposition. Economic Geology and Bulletin of the Society of Economic Geologists, Vol. 63, No. 4, 1968, P. 390–400. [Possibility that ice sheet might provide temporary head to reverse pre-glacial groundwater movements and cause precipitation of minerals near the ice sheet margins.]Google Scholar
Price, R. J. Moraines, sandar, kames and eskers near Breidamerkuijökull, Iceland. Institute of British Geographers. Transactions, No. 46, 1969, p. 17–43. [Study of glacial deposition features in front of this Icelandic glacier based on aerial photography and ground studies.]Google Scholar
Schwarzbach, M. Neuere Eiszeithypothesen. Eiszeitalter und Gegenwart, Bd. 19, 1968, p. 250–61. [Critical examination of new ice-age theories, none of which is completely satisfactory. Suggestion of “multilateral origin of an ice age”. English summary.]Google Scholar
Sergin, S. Ya. Issledovaniyc dinamika kolebaniy klimata i oleileneniya na protyazhenii chetvyertichnogo perioda . izvestiya Akademii Nauk SSSR. Serlya Geografisheskaya, 1968, No. 6, p. 88–98. [Mathematical model.]Google Scholar
Sharp, R. P. Semiquantitative differentiation of glacial moraines near Convict Lake, Sierra Nevada, California. Journal of Geology, Vol. 77, No. 1, 1969, p. 68–91. [Methods of testing age of Pleistocene moraines.]CrossRefGoogle Scholar
Slatt, R. M. Hoskin, C. M. Water and sediment in the Norris Glacier outwash area, Upper Taku Inlet southeastern Alaska. Journal of Sedimentary Petrology, Vol. 38, No. 2, 1968, p. 434–56. [Study of outwash fan from this glacier.]Google Scholar
Stroyev, P. A. Frolov, A. I. O subshirotnom razlome zemnoy kory krayevoy zony vostochnoy Antarktidy (10° z.d.−130° v.d.) . Izvestiya Akademii Nauk SSSR. Fizika Zemli, 1967, No 5, p. 86–91. [Ocean bottom off Antarctica shows troughs and crystal fractures related to glacio-isostatic mations due to variations in ice load. English translation in Izvesiya. Academy of Sciences, U.S.S.R. Physics of the Solid Earth, 1967, No. 5, p. 319–22.]Google Scholar
Suggate, R. P. The Paringa formation, Westland, New Zealand. Ney Zealand journal of Geology and Geophysics, Vol. 11, No. 2, 1968, p. 345–55. [Radiocarbon dates for retreat of last Otira Glaciation maximum. Subsequent uplift. Appendixes by C. A. Fleming, N. de B. Hornibrock and W. F. Harris.]Google Scholar
Szupryczyński, J. Glaciations in the Spitsbergen area. Geoiraphia Polonica, [No.] 14, 1968, p. 175–83. [Review of theories on number of glaciations in Svalbard and their age.]Google Scholar
Thompson, W. F. New observations on alpine accordantes in the western United States. Annals of the Association of American Geographers, Vol. 38, No. 4, 1968, p. 650–69. [Observations of timber lines, alp slopes and gipfelflur. Suggestion that gipfeifur is topographic record of interglacial tree-line above which periglacial erosion was very active.]Google Scholar
Yoshikawa, T. Hyūsei-taiseki-butsu to sono chikei ni kansuru jutsugo ni tsuite . Daishi kenkyū, [Vol.] 7, [No.] 2, 1968, p. 59–60. [Discussion of German terminology and its Japanese equivalents.]Google Scholar
Zamoruyev, V. V. Nekotoryye voprosy paleoglyatsiologii Zabaykal’ya v epokhu pozlneehttvertichnogo oledeneniya . lzvestiya Akademii.Nauk SSSR. Serffya Geograficherkaya, 1967, No. 6, p. 76–82. [Climatic conditions under which these glaciers formed.]Google Scholar
Zienert, A. Gleiche Würm-Rückzugsstadien in den Gebirgen Mitteleuropas und Ostafrikas. Eiszeitalter und Gegenwart, Bd. 19, 1968, p. 85–92. [Study of moraines of Mount Kenya and Kilimanjaro and question of correlation with Alps. English summary.]Google Scholar

Frost action on rocks and soil. Frozen ground. Permafrost

Baranowski, S. Termika tundry peryglacjalnej SW Spitsbergen . Wroclaw, Pagístwowe Wydawaictwo Naukowe, 1968. 76 p. (Acta Universitatis Wratislaviensis, No. 68, Studia Geograficzne, 10.) [Study of temperature in ground and lowest air layer and interpretation. English summary, p. 64–73.]Google Scholar
Barsch, D. Permafrost in der oberen subnivalen Stufe der Alpen. Geagraphica Helvetica, 24. Jahrg., [Ht.] 1, 1969, p. 10–12. [Discussion of present-day extent of permafrost in the Alps.]Google Scholar
Boyé, M. Défense et illustration de l’hypothése du “défonçage périglaciaire”. Biulelyn Peryglacjalny, No. 17, 1968, p. 5–56. [Discussion of role of freeze-thaw processes in periglacial and glacial erosion.]Google Scholar
Brown, R. J. E. Permafrost investigations in northern Ontario and northeastern Manitoba. Canada. National Research Council. Division of Building Research. Technical Paper No, 291, 1968, 40–35 p. [Study of occurrence of permafrost in this area of Canada.]Google Scholar
Cailleux, A. Periglacial of McMurdo Strait (Antarctica). Biuletyn Peryglacjalny, No. 17. 1968, p. 57–90. [General survey of features in McMurdo Sound and comparison with those in Arctic and elsewhere in Antarctic.]Google Scholar
Caine, N. The fabric of periglacial blockfield material on Mt. Barrow, Tasmania. Geograiiska Annaler, Vol. 50A, No. 4, 1968, p. 193–206. [Study of stone orientations and their interpretation in terms of solifluction processes.]Google Scholar
Demex, J. Cryoplanation terraces in Yakutia. Biuletyn Peryglacjalny, No. 17, 1968, p. 91–116. [Description of terraces and discussion of their development.]Google Scholar
Forsgren, B. Discussion of E. Schenk, “Zur Entstehung der Strangmoore und Aapamoore der Arktis und Subarktis”. Zeitschrift für Geomorphologie, Neue Folge, Bd. 13, Ht. 1, 1969, p. 119–23. [Criticism of theory of Schenk. ibid., Bd. 10, Ht. 4, 1966. p. 346–68, according to which string-bogs corne from frozen normal bogs.]Google Scholar
Forsgren, B. Studies of palsas in Finland, Norway and Sweden, 1964–1966. Biuletyn Peryglacjalny, No. 17, 1968, p. 117–23. [Review of investigations.]Google Scholar
Hoekstra, P. Moisture movement to a freezing front. Union de Géodésie et Géophysique Internationale. Association Internationale d’Hydrologie Scientifique. Assemblée générale de Berne, 25 sept.−7 oct. 1967. Céoohernie, précipitations, évaporation, humidité du sol, hydrométrie. Rapports et discussions, 1968, p. 411–17. [Laboratory study of moisture movement in unsaturated clay, silt and sand caused by freezing. Discussion by —. Váša, A. Volker and H. W. Anderson, p. 417.]Google Scholar
Kaplina, T. N. Istoriya mnogoletney merzlnty Mezenskogo severa . Izvestiya Akademii.Nauk SSSR. Seriya Geograficheskaya, 1969, No. 2, p. 89–96. [Region east of White Sea.]Google Scholar
Kirkby, M. J. Measurement and theory of soil creep. Journal of Geology, Vol. 75, No. 4, 1967, p. 359–78. [Includes discussion of importance of alternation of freezing and thawing.]Google Scholar
Liss, C.-C. Fossile Eiskeile (?) an der Patagonischen Atlantisküste. Zeitschriftfür Geomorphologie, Neue Folge, Bd. 13, Ht. 1, 1969, p. 109–14. [Description of possible ice wedges on the Atlantic coast of Patagonia.]Google Scholar
Lyczewska, J. L’accumulation fluvio-périglaciaire dans la partie centrale du bassin de la Nida, Pologne centrale. Biuletyn Peryglacjalny, No. 17, 1968, p. 125–47. [Origin of these periglacial deposits in central Poland.]Google Scholar
Mel’nikov, P. I. Problemy merzlotovedeniya)Problems of frozen ground research]. Vestnik Akadentii Nauk SSSR, 1968, No. 3, p. 86–89. [Survey of work of institute at Yakutsk.]Google Scholar
Mojski, J. E. Outline of loess stratigraphy in Poland. Biuletyn Peryglacjahy, No. 17, 1968, p. 149–70. [Description and age.]Google Scholar
Penner, E. Heaving pressure in soils during unidirectional freezing. Canadian Geotechnical Journal, Vol. 4, No. 4, 1967, p. 398–408. [Experimental and theoretical study cf ice lens formation in natural soil supports use of particle size as basis of assessing frost susceptibility.]Google Scholar
Pissart, A. Les polygones de fente de gel de 1’île Prince Patrick (Arctique Canadien—76° lat. N.). Biuletyn Peryglacjalny, No.:7, 1968, p. 171–80. [Description ofform and structure of frost crack polygons in this island of the Canadian Arctic Archipelago.]Google Scholar
Rognon, P., and others. Remarques sur le comportement des grès et granites vosgiens sous climat froid, [par] P. Rognon, M. Cussenot-Curien, C. Seyer et A. Weisrock. Revue Géographique de l’Est, Tom. 7, No. 4, 1967 [pub. 1968], p. 403–18. [Laboratory study of effect of freeze-thaw cycles on unweathered sandstones and granites from various parts of the Vosges, and gcomorphological consequences.]Google Scholar
Rohdenburg, H. Walther, D. Rezente Strukturböden in Giessen. Eiszeitalter und Gegenwart, Bd. 19, 1968, p. 279–82. [Patterned ground in this region of Germany.]Google Scholar
Rudberg, S. Wind erosion—preparation of maps showing the direction of eroding winds. Biuletyn Peryglacjalny, No. 17, 1968, p. 181–93. [Importance of wind direction in erosion under periglacial conditions; maps based on erosional features.]Google Scholar
Smith, H. T. U. “Piping” in relation to periglacial boulder concentrations. Biuletyn Peryglacjalny, No. 17, 1968, p. 195–204. [Discusses mechanism by which water may affect boulder fields.]Google Scholar
Starkel, L. Remarques sur l’étagement des processus morphogénétiques dans les Carpates au cours de la dernière glaciation. Biuletyn Peryglacjalny, No. 17, 1968, p. 205–20. [Discussion of sequence of periglacial geomorphological processes in the Carpathians during the last glaciation.]Google Scholar
Tak-Schneider, U. van den. Cracks and fissures of post-Allerød age in the Netherlands. Biuletyn Peryglacjalny, No. 17, 1968, p. 221–25. [Description.]Google Scholar
Tolstikhin, O. N. The meaning and calculation of the icing processes in the balance of the underground waters in the permafrost areas. Union de Géodésie et Géophysique Internationale. Association Internationale d’Hydrologie Scientifique. Assemblée générale de Berne, 25 sept.−7 oct. 1967. Eaux souterraines. Rapports et discussions, 1968, p. 361–67. [Discussion of how to assess amount of icing and its importance in natural water balance in parts of Siberia.]Google Scholar
Twomey, A. A. Black, R. F. Patterned-ground studies in Victoria Land. Antarctic Journal of the United States, Vol. 3, No. 4, 1968, p. 106–07. [Brief account of studies to establish conditions for sand and ice wedge formation.]Google Scholar
Vaumas, E. de. Recherches sur le modelé cryohydrique et cryofluvial. Biuletyn Peryglacjalny, No. 17, 1968, p. 227–301. [Study of depressions formed by periglacial phenomena in the Brenne and Velay regions of France.]Google Scholar
West, R. G. Evidence for pre-Cromerian permafrost in East Anglia. Biuletyn Peryglacjalny, No. 17, 1968, p. 303–04. [Observations of ice wedges in deposits of this age in this part of England.]Google Scholar
Whittow, J. B. A note on present day cryopedological phenomena in northern New South Wales, Australia. Biuletyn Peryglacjalny, No. 17, 1968, p. 305–10. [Frost soil phenomena above 1400 mat point at lat. 30° 31′ S.]Google Scholar
Williams, R. B. G. Some estimates of periglacial erosion in southern and eastern England. Biuletyn Peryglacjalny, No. 17, 1968, p. 311–35.Google Scholar
Yvard, J.-C. Fentes de gel périglaciaire de la région de Tours. Bulletin de l’Association Française pour I’ Etude du Quaternaire, 5e An., No. 16, 1968, p. 175–79. [Fossil ice wedges in this region of France.]Google Scholar

Meteorological and climatological glaciology

Anderson, F. J. Freier, G. D. Freezing and hailstones. Proceedings of the international conference on cloud physics, August 26–30, 1968, Toronto, Canada, [1968?], p. 432–36. [Theory and experiments to show ring structure could be due to freezing from outside inwards.]Google Scholar
Aufdermaur, A. N. Windkanalaersuche and theoretische Betrachtungen zum lokalen Wärme- and Stoffnbergang an Hagelkornmodellen. Zürich, ETH, 1968. 69 p. (Eidgenössische Kommission zum Studium der Hagelbildung and der Hagelabwehr. Wissenschaftliche Mitteilung Nr. 60. [Also published as] Dissertation Nr. 4221, Eidgenössische Technische Hochschule. Zürich, Juris-Verlag, 1968.) [Theoretical and experimental study of heat transfer and accretion on isothermal model hailstones.]Google Scholar
Barry, R. G. Fogarsi, S. Climatology studies of Baffin Island, Northwest Territories. Canada. Department of Energy, Mines and Resources. Inland Waters Branch. Technical Bulletin No. 13, 1968, iv, 106 p. [Studies of vapour content and its horizontal transport and of conditions likely to cause accumulation or ablation.]Google Scholar
Borovikov, A. M. Supercooling of water in the atmosphere and the phase of various types of clouds. Proceedings of the international conference on cloud physics, August 26–30, 1963, Toronto, Canada, [1968?], p. 290–94. [Survey of work done by hydrometeorological service of U.S.S.R.]Google Scholar
Burdecki, F. Temperaturgradienten in der Antarktis. Polarforschung, Bd. 6, Jahrg. 37, Ht. 1–2, 1967 [pub. 1968], p. 147–51. [Calculation of temperature gradients and vertical lapse rates in Antarctica by extrapolation from higher latitudes gives different result from values deduced from ice sheet temperatures. Results imply climatic changes.]Google Scholar
Deirmendjian, D. Sun’s image on airborne ice crystals? Applied Optics, Vol. 7, No. 3, 1968, p. 556. [Observation of bright spot from airliner possibly due to specular reflection from platelike ice crystals.]Google Scholar
Diem, M. Klimadaten von den Queen Elizabeth Inseln, Canada, NWT. Polarforschung, Bd. 6, Jahrg, 37, Ht. 1–2, 1967 [pub. 1968], p. 155–69. [Climatic data for 5 stations in the Queen Elizabeth Islands, Canada, for 1951–65 are compiled for comparison with glacier variations.]Google Scholar
Goyer, G. G., and others. On the heat transfer to ice spheres and the freezing of spongy hail, [by] G. G. Goyer, S. S. Lin, S. N. Gitlin and M. N. Plooster. Journal of the Atmospheric Sciences, Vol. 26, No. 2, 1969, p. 319–26. [Measurement of the rate of heat transfer during melting and implications for theories of liquid water content of natural hailstones.]Google Scholar
Goyer, G. G., and others. The rate of heat transfer to dry and wet hailstone surfaces and its application to the freezing of spongy hail in a cloud model, [by] G. G. Goyer, S. S. Lin, S. N. Gitlin and M. N. Plooster. Proceedings of the international conference on cloud physics, August 26–30, 1968, Toronto, Canada, [1968?], p. 427–31. [Experiments show heat transfer to be unaffected by wetness.]Google Scholar
Grant, L. O. The role of ice nuclei in the formation of precipitation. Proceedings of the international conference on cloud physics, August 26–30, 1968, Toronto, Canada, [1968?], p. 305–10. [Observations of ice crystal concentrations at high altitude mountain stations.]Google Scholar
Gvelesiani, A. I. Kartsivadze, A. I. On the melting of spherical hailstones. Proceedings of the international conference on cloud physics, August 26–30, 1968, Toronto, Canada, [1968?], p. 422–26. [Laboratory study in conditions simulating natural environment.]Google Scholar
Higuchi, K. Sekkei no shōchō to kaki-kion no hendō . Kishō Kenkyū Nōto, [No.] 97, 1968, p. 286–90.Google Scholar
Hobbs, P. V. ice multiplication in clouds. Journal of the Atmospheric Sciences, Vol. 26, No. 2, 1969, p. 315–18. [Number of ice particles compared with number of ice nuclei in clouds with different top temperatures.]Google Scholar
Kachurin, L. G., and others. Kinetics of hailstone growth, radar reflectivity of growing hailstones and crystallizadon processes, [by] L. G. Kachurin, B. M. Vorobyov and A. I. Kartsivadze. Proceedings of the international conference on cloud physics, August 26–30, 1968, Toronto, Canada, [1968?], p. 472–77.Google Scholar
Kessler, E., and others. Growth by accretion in relation to hydrometeor starting height, cloud density and vertical air velocity, [by] E. Kessler, E. A. Newburg and]. Silver. Proceedings of the international conference an cloud physics, August 26–30, 1968, Toronto, Canada, [1968?], p. 464–71. [Theory of hailstone development.]Google Scholar
Koenig, L. R. Comments on atmospheric ice multiplication mechanisms. Proceedings of the international conference on cloud physics, August 26–30, 1968, Toronto, Canada, [1968?], p. 213–16. [Assessment of possible mechanisms.]Google Scholar
Koenig, L. R. Some observations suggesting ice multiplication in the atmosphere. Journal of the Atmospheric Sciences, Vol. 25, No. 3, 1968, p. 460–63. [Cloud physics evidence for multiplication of ice crystals. Mechanisms discussed.]Google Scholar
Knight, C. A. Knight, N. C. The final freezing of spongy ice: hailstone collection techniques and interpretations of structure. Proceedings of the international conference on cloud physics, August 26–30, 1968, Toronto, Canada, [1968?], p. 445–49. [Laboratory experiments indicate that recrystallization may mask hailstone structures unless precautions are taken.]Google Scholar
List, R., and others. A numerical experiment on the growth and feedback mechanisms of hailstones in a one-dimensional steady-state model cloud, [by] R. List, R. B. Charlton and P. I. Buttuls. Journal of the Atmospheric Sciences, Vol. 25, No. 6, 1968, p. 1061–74.Google Scholar
Macklin, W. C. Bailey, I. H. Growth parameters of artificial hailstones. Proceedings of the international conference on cloud physics, August 26–30, 1968, Toronto, Canada, [1968?], p. 437–40. [Experiments to test growth theories.]Google Scholar
Majzoub, M., and others. Variations and comparisons of deuterium and oxygen 18 concentrations in hailstones, [by] M. Majzoub, G. Nief and E. Roth. Proceedings of the international conference on cloud physics, August 26–30, 196 8, Toronto, Canada, [1968?], P. 450–54. [Measurements on two big hailstones and interpretation of growth history.]Google Scholar
Marwitz, J. D. Auer, A. H. Ice crystal growth by diffusion and accretion. Proceedings of the international conference on cloud physics, August 26–30, 1968, Toronto, Canada, [1968?], p. 249–54. [Analysis of published data to give size as function of time in clouds and comparison of result with experiments.]Google Scholar
Mason, B. J. The generation of electric charges and fields in precipitating clouds. Proceedings of the international conference on cloud physics, August 26–30, 1968, Toronto, Canada, [1968?], p. 657–62. [Study of possible processes including freezing process.]Google Scholar
Mason, B. J. Initiation of the ice phase in the atmosphere. Proceedings of the international conference on cloud physics, August 26–30, 1968, Toronto, Canada, [1968?], p. 163–73. [Survey of current problems.]Google Scholar
Mossop, S. C. Comparisons between concentration of ice crystals in cloud and the concentration of ice nuclei. Journal de Recherches Atmosphériques, Vol. 3, 1968, Nos. 1–2, p. 119–24. [Measurements of ice crystal concentrations in clouds give results often much larger than cloud-chamber measurements of ice nucleus concentration.]Google Scholar
Mossop, S. C. Ono, A. Measurements of ice crystal concentration in clouds. Journal of the Atmospheric Sciences, Vol. 26, No. 1, 1969, p. 130–37. [Measurements in Australia which show altostratus clouds have about same number of crystals as nuclei whereas cumulus and stratocumulus have 103 times as many.]Google Scholar
Ohtake, T. Freezing of water droplets and ice fog phenomena. Proceedings of the international conference on cloud physics, August 26–30, 1968, Toronto, Canada, [1968?], p. 285–89. [Mechanism of formation of ice fog.]Google Scholar
Ono, A. The shape and riming properties of ice crystals in natural clouds. Journal of the Atmospheric Sciences, Vol. 26, No. 1, 1969, p. 138–47. [Studies of growth and riming of columnar and planar ice crystals.]Google Scholar
Palmer, T. Y. Kreiss, W. T. Radiometric observations and the cloud melting zone. AMA Journal (American Institute of Aeronautics and Astronautics), Vol. 5, No. 11, 1967, p. 2075–77. [Theory of enhanced radar reflection from near freezing level in clouds, and measurements which support the model.]Google Scholar
Sarrica, O. Experimental evidences in hail structure. Proceedings of the international conference on cloud physics, August 26–30, 1968, Toronto, Canada, [1968?], p. 441–44. [Experiments on freezing water and melting hailstones.]Google Scholar
Schuepp, P. H. Studies of the local heat and mass transfer of spherical hailstone models. Proceedings of the international conference on cloud physics, August 26–30, 1968, Toronto, Canada, [1968?], p. 416–21. [Model laboratory experiment that allows transfer to rough particles to be studied.]Google Scholar
Schwerdtfeger, W. New data on the winter radiation balance at the South Pole. Antarctic journal of the United States, Vol. 3, No. 5. 1968, p. 193–94. [Data from 1965 which conflict with earlier reported values.]Google Scholar
Summers, P. W. Soft hail in Alberta hailstorms. Proceedings of the international conference on cloud physics, August 26–30, 1968, Toronto, Canada, [1968?], p. 455–59. [Description of this kind of hail and its frequency in Alberta.]Google Scholar
Vali, G. The freezing-nucleus content of precipitation and its relation to the formation of ice in the clouds. Proceedings of the international conference on cloud physics, August 26–30, 1968, Toronto, Canada, [1968?], p. 232–37. [Study which may help explain why some clouds glaciate at much higher temperatures than others.]Google Scholar
Weickmann, H. K. The hailstorm. Proceedings of the international conference on cloud physics, August 26–30, 1968, Toronto, Canada, [1968?], p. 400–10. [Survey of current knowledge about hailstones.]Google Scholar

Snow

Alford, D. L. Estimating depth-load values in the spring alpine snowpack. Proceedings of the Western Snow Conference, 35th annual meeting, 1967, p. 50–54. [Discusses problems of field techniques for sampling and measuring amount of water present in snow.]Google Scholar
Alford, D. L. Keeler, C. M. Stratigraphie studies of the winter snow layer, Mount Logan, St. Elias Range. Arctic, Vol. 21, No. 4, 1968, p. 245–54. [Results of traverse measurements of snow cover properties in this region of Yukon Territory, Canada, and interpretation in terms of climate.]Google Scholar
Anderson, H. W. Snow accumulation as related to meteorological, topographic, and forest variables in central Sierra Nevada, California. Union de Géodésie et Géophysique Internationale. Association Internationale d’Hydrologie Scientifique. Assemblée générale de Berne, 25 sept. −7 oct. 1967. Commission des Eaux de Surface. Aspects hydrologiques de l’utilisation des eaux. Rapports et discussions, 1968, p. 215–24. [Observations at 250 widely differing sites and analysis of results.]Google Scholar
Austin, P. M. Kraus, M. J. Snowflake aggregation—a numerical model. Proceedings of the international conference on cloud physics, August 26–30, 1968, Toronto, Canada, [1968?], p. 300–04.Google Scholar
Bossolasco, M., and others. Le proprietà fisiche del manto nevoso a Sauze d’Oulx (1865 m), di M. Bossolasco, G. Ciccioni e G. Flocchini. Geofisica e Meteorologia, Vol. 17, No. 3–4, 1968, p. 57–79. [Measurement of physical properties of snow cover in this area of Italy over three winters. English summary.]Google Scholar
Bowles, D. Bridger data system multipoint snowpack thermometry. Proceedings of the Western Snow Conference, 35th annual meeting, 1967, p. 29–34. [Study to determine if air-snow interface temperature gradient can be used as reliable indicator of snow depth and accumulation.]Google Scholar
Bridgman, Dick. Snow rollers. Weather, Vol. 24, No. 3, 1969, p. 103. [Two photographs and short description of conditions of formation of snow rollers on Lakehead Airport, Fort William, Ontario, Canada.]Google Scholar
Brochu, M. Existence d’une zone périglaciaire dans la région sommitale du Pic (o Pico) dans l’île du Pic aux Açores. Zeitschrift für Geomorphologie, Neue Folge, Bd. 13, Ht. 1, 1969, p. 115–18. [Snow during winter on summit of o Pico in the Azores. English and German abstracts.]Google Scholar
Browzin, B. S. Comparative study of snow type hydrology of northeastern Canada and of plains of Russia and Siberia. Union de Géodésie et Géophysique Internationale. Association Internationale d’Hydrologie Scientifique. Assemblée générale de Berne, 25 sept. −7 oct. 1967. Commission des Eaux de Surface. Aspects hydrologiques de l’utilisation des eaux. Rapports et discussions, 1968, 13.204–14. [Study of mean monthly river flow patterns and differences in various Arctic regions. Discussion by P. B. M. Ouma and A. Kosiba, p. 213–14.]Google Scholar
Buykov, M. V. Theory of snowfall formation in the supercooled stratus clouds. Proceedings of the international conference on cloud physics, August 26–30, 1968, Toronto, Canada, [1968?], p. 311–25.Google Scholar
Daguchi, M. Fukui chihó ni okeru sekisetsu no butsurigakuteki seishitsu (daiippō: harusaki no sanchi sekisetsu) The physical character of snow in the Futui region (report no. 1: mountain snow in early spring)]. Seppyō, [Vol.] 30, [No.] 3, 1968, p. 61–69. [Observations of temperature, hardness, grain size and free water content. English abstract.]Google Scholar
Daguchi, M. Hakusan no sekkei chōsa hōkoku (daiippō: sekkei no butsurigaku seishitsu) . Seppyō, [Vol.] 30, [No.] 3, 1968, p. 81–88. [Description of condition in summer. English abstract.]Google Scholar
Doi, T. Sekka-zusetsu: illustrations of snow crystals, written by Toshitsura Doi (1789–1848). —A commentary on the Sekka-zusetsu by Teisaku Kobayashi. Tokyo, Tsukiji Shokan Publishing Co. Ltd. [c 1968]. [iii], [i], 34, [i], 32, [iv], 165, [xii] p. [Facsimile and commentary on two books of illustrations of snow crystals published in Japan in 1833 and 1840.]Google Scholar
Fan, S. S. T. Yen, Yin-Chao. Nonsteady compressible flow through anisotropie porous mediums with particular reference to snow. Water Resources Research, Vol. 4, No. 3, 1968, p. 597–606. [Calculation of flow for van der Waals and ideal gas. Application to flow in snow of Antarctic icc sheet.]Google Scholar
Farnes, P. E. Criteria for determining mountain snow pillow sites. Proceedings of the Western Snow Conference, 35th annual meeting, 1967, p. 59–62. [Evaluates good sites for installing snow gauges.]Google Scholar
Ferland, M. Les régimes de température accompagnant les chutes de neige. Cahiers de Géographie de Québec, 12e An., No. 25, 1968, p. 145–52. [Correlation between amount of snowfall and temperature.]Google Scholar
Fréchette, J.-G. Accumulation de la neige sous divers types de couverts forestiers. Cahiers de Géographie de Québec, 12e An., No. 25, 1968, p. 141–44. [Study of snow accumulation under various forest conditions.]Google Scholar
Gand, H. R. in der. Neue Erkenntnisse über das Schneegleiten Schweizerische Bauzeilung, Jahr. 86, Ht. 31, 1968, p. 557–59. [Study of the sliding of snow cover over the ground and methods of minimizing it.]Google Scholar
Higuchi, K. Growth of ice crystals under radiative cooling. Proceedings of the international conference on cloud physics, August 26–30, 1969, Toronto, Canada, [1968?], p. 265–69. [Theory of growth of ice crystals in the air in polar regions.]Google Scholar
Kennedy, J. M., and others. Microwave radiometric sensing of the physical parameters of snow, by J. M. Kennedy, R. T. Sakasnoto and A. T. Edgerton. Proceedings of the Western Snow Conference, 35th annual meeting, 1967, p. 18–23. [Data obtained may be used to determine melt condition of in situ snow, thickness of snow packs, and, possibly, snow density and point in time when water bodies begin to freeze.]Google Scholar
Kuroda, M. Sekisetsusó no antei to nadare no bunrui . Seppvō, [Vol.] 29, [No.] 5, 1967, p. 131–39.Google Scholar
Kusakabe, M. Shikoku no yuki . Seppvō, [Vol.] 30, [No.] 1, 1958, p. 7–18. [Use of recording the period and area of heavy snowfall. English abstract.]Google Scholar
Leonard, R. E. Eschner, A. R. Albedo of intercepted snow. Water Resources Research, Vol. 4, No. 5, 1968, p. 931–35. [Measurements above a red pine plantation after snowfall showed low albedo compared with snow on ground.]Google Scholar
Ludlum, D. Snowfall at San Francisco. Weatherwise, Vol. 21, No. 6, 1969, p. 230–37. [Report of six instances of snow in San Francisco in last loo years and contemporary reports of 1887 fall.]Google Scholar
Magono, C. Problems on physical understanding of snowfall phenomena. Proceedings of the international conference on cloud physics, August 26–30, 1968, Toronto, Canada, [1968?], p. 243–48. [Survey of current problems.]Google Scholar
Ono, M. Suzuki, M. Maikuro-ha ni taisuru yuki no tōka gensuiryō . Seppyō, [Vol.] 29, [No.] 5, 1967, p. 150–55. [For snow layers up to 30 cm. English abstract.]Google Scholar
Orheim, O. Studies of surface snow at Plateau station. Antarctic Journal of the United States, Vol. 3, No. 2, 1968, p. 37. [Study of changes in hardness during the summer.]Google Scholar
Orheim, O. Surface snow metamorphosis on the Antarctic plateau. Norsk Polarinstitutt. Årbok, 1966 [pub. 1968], p. 84–91 [Observations in area between Pole of relative inaccessibility and “Plateau” station in 1965–67. Mainly surface hardness and reduction in sastrugi heights.]Google Scholar
Plasschaert, J. H. M. Weather and avalanches. Weather, Vol. 24, No. 3, 1969, p. 99–102. [Short account of the role played by weather in the build-up and release of avalanches.]Google Scholar
Podzimek, J. Aerodynamic conditions of ice crystal aggregation. Proceedings of the international conference on cloud physics, August 26–30, 1969, Toronto, Canada, [1968?], p. 295–99. [In terpretation of laboratory model experiments.]Google Scholar
Poggi, A. La mesure des precipitations neigeuses. Union de Géodésie et Géophysique Internationale. Association Internationale d’Hydrologie Scientifique. Assemblée générale de Berne, 25 sept. −7 oct. 1967. Géochentie, précipitations, évaporation, humidité du sol, hydrométrie. Rapports et discussions, 1968, p. 237–42. [Comparative study of snow gauges and of use of Alter’s shield. Discussion by Nguyen Ba Cuong and C. Jaccard p. 242.]Google Scholar
Pysklywec, D. W., and others. Snowmelt at an index plot, [by] D. W. Pysklywec, K. S. Davar [and] D. I. Bray. Water Resources Research, Vol. 4, No. 5, 1968, P. 937–46. [Measurement of snow melt and meteorological parameters and test of three methods of predicting melting.]Google Scholar
Rosinski, J. Langer, G. Particle and deuterium content in snow. Proceedings of the international conference an cloud physics, August 26–30, 1968, Toronto, Canada, [1968?], p. 331–35. [Results of analysis of snow in Colorado, U.S.A.]Google Scholar
Rosinski, J., and others. Removal of aerosol particles and fractional separation of HDO-H20 during snowstorms, [by] J. Rosinski, G. Langer and R. Bleck. Journal of the Atmospheric Sciences, Vol. 26, No. 2, 1969, p. 289–301. [Concentration of D and insoluble particles proportional to size of snow crystal.]Google Scholar
Spink, P. C. Scottish snowbeds in summer 1968. Weather, Vol. 24, No. 3, 1969, p. 115–17. [Report of state of snow-beds in July 1968.]Google Scholar
Sugimort, M. Kagami, Y. Fukui chihō no heichi sekisetsu no kansoku kekka ni tsuite . Seppyō, [Vol.] 30, [No.] 1, 1968, p. 19–25. [Microphotography of snow cover in this place in Japan. English abstract.]Google Scholar
Takahashi, K., and others. Bassai sekichi no nadare hassei keika . Seppyō, [Vol.] 30, [No.] 1, 1968, p. 26–30 [Experimental study of effect of cutting trees on avalanche formation. English abstract.]Google Scholar
Theakston, F. H. Naraine, D. Quantitative analysis of snow deposition by use of models in a water flume. Proceedings of the Western Snow Conference, 35th annual meeting, 1967, p. 55–58. [Describes model used to study snow deposition on roofs. Light white sand, simulating snow-storms, is injected into fluid flow created by open channel water flume and passes over model buildings, fences, trees, and undulating terrain.]Google Scholar
Wakabayashi, R. Yamamura, M. Hokkaidō ni okeru hanjō nadare no ichitokuchō . Seppyō, [Vol.] 30, [No,] 3, 1968, p. 75–80. [Description of these avalanches and the processes occurring in them. English abstract.]Google Scholar
Wexler, R. Formation and growth of ice crystals in stratiform clouds. Proceedings of the international conference on cloud physics, August 26–30, 1968, Toronto, Canada, [1968?], p. 322–26. [Theory.]Google Scholar
Zingg, T. Maximale Schneelasten in der Schweiz. Schweizerische Bauzeitung, Jahrg. 86, Ht. 31, 1968, p. 555–57. [Maximum snow accumulation in Switzerland as a function of altitude.]Google Scholar