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Glaciological Literature

Published online by Cambridge University Press:  30 January 2017

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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

Conferences

Ōura, H., ed. Physics of snow and ice: international conference on low temperature science. I. Conference on physics of snow and ice. II. Conference on cryobiology. August 14–15, 1966, Sapporo, Japan. (Twenty-fifth anniversary, the Institute of Low Temperature Science.) Proceedings, Vol. 1. [Sapporo], Institute of Low Temperature Science, Hokkaido University, 1967. 2 parts: xxix, 711 p.; xiii, 713–1414 p. [For details of papers see elsewhere in this list.]Google Scholar

General Glaciology

Astapenko, P. D. Treshnikov, A. F. Interrelationship between meteorology, oceanography and glaciology in Antarctic studies. Annals of the International Geophysical Year, Vol. 44, 1967, p. 96121. [Survey of work done during I.G.Y. and interrelation of results of these three disciplines.]Google Scholar
Dubovskoy, B. V. Kartograficheskiye issledovaniya SSSR v Antarktide za to let . Antarktika. Doklady liomissii 1965 g. Moscow, Izdatel’stvo Akademii Nauk SSSR, 1966, p. 13067. [Details of activity and accuracy of programme.]Google Scholar
Harrison, H. Schoen, R. I. Evaporation of ice in space: Saturn’s rings. Science, Vol. 157, No. 3793, 1967, p. 717576. [Estimate of rate of ice evaporation in space due to non-thermal processes and question of whether Saturn’s rings could be ice.]Google Scholar
Ivanov, V. B. Osnovnyye itogi sovetskikh glyatsiologicheskikh issledovaniy v Antarktide za 10 let (1956–1966 gg.) . Informatsionnyy By ulleten’ Sovetskoy Antarkticheskoy Ekspeditsii, No. 60, 1967, p. 515.Google Scholar
Peschanskiy, I. S. Ledovedeniye i ledofekhnika. Izdaviye 2–ye, dopolmennoye i pererabotannoye . Leningrad, Gidrometeorologicheskoye Izdatel’stvo, 1967. 462 p. [Ice physics, with special reference to floating ice.]Google Scholar
Slupetzky, H., and others. 16. Kurs für Hochgcbirgs- and Polarforschun (Obergurgl, Tirol, 18–25. September 1966), [von] H. and W. Slupetzky, D. Resmann. Mitteilungen der Osterreichischen Geographischen Gesellschaft, Bd. 108, Ht. 2–3, 1966, p. 30913. [Account of this course and its numerous glaciological papers.]Google Scholar
[U.S.S.R.: Glaciology.] Soobshchenffye o nauchnykh rabotakh po glyatsiologii 1963–1966 gg. . Moscow, Sovetskiy Geofizicheskiy Komitet, 1967. 31 p. [Soviet work and publications.]Google Scholar
Wood, P. H. Arctic research in western Europe; a directory of institutions. Washington, D.C., Arctic Institute of North America, 1967. vii, 296 p. [Listing of polar research institutions in is countries with brief descriptions of nature and scope of their interests.]Google Scholar

Glaciological Instruments and Methods

Beaumont, R. T. Field accuracy of volumetric snow samplers at Mt. Hood, Oregon. (In Ōura, H., ed. Physics of snow and ice.… Vol. 1, Pt. 2. [Sapporo], Institute of Low Temperature Science, Hokkaido University, 1967, p. 100713.) [Tests on different kinds of samplers.]Google Scholar
Bilello, M. A. Parrott, W. H. Some new or experimental equipment for use on snow and ice. Proceedings of the Eastern Snow Conference, Vol. 12, 1967, p. 114. [Describes: (1) nuclear technique to measure snow density, (2) snow disaggregator, (3) ice chipper, (4) soniscope, (5) modified Rammsonde, and (6) snow permeameter.]Google Scholar
Bogorodskiy, V. V., ed. Primenenive radiofizicheskikh metodov v okeanograficheskikh i ledovykh isstedovaniyakh . Leningrad, Arkticheskiy i Antarkticheskiy NauchnoIssledovatel’skiy Institut, 1965. 106 p. [Includes following papers presented at the first All-Union Conference on the Use of Radiophysical Methods in Oceanography and Ice Observations held in Leningrad, 23–24 January 1964: E. P. Borisenkov, “First All-Union Conference on the Use of Radiophysical Methods in Oceanography and Ice Observations and its problems”; V. V. Bogorodskiy and V. N. Rudakov, “Use of polarization and interference of electromagnetic waves for determining the thickness of sea ice”; V. N. Rudakov, “Flaw detection in snow and ice cover with the aid of electromagnetic waves”; V. V. Bogorodskiy and V. N. Rudakov, “Electromagnetic parameters of snow, ice, fresh and sea water”; V. S. Loshchilov and V. I. Shil’nikov, “Use and prospects of the radar method in aerial reconnaissance of ice”; V. V. Bogorodskiy and others, “Electrical phenomena which arise during water crystallization”; V. N. Tsvetkov, “Investigation ofmicro-nonhomogeneities in the water layer just beneath the ice in the Arctic”; L. I. Chapurskiy, “Detection of clouds against a snow background”; F. I. Melkov and P. A. Rublev, “Use of infra-red equipment during observations of ice conditions”.]Google Scholar
Brichkin, A. V., and others. Ognevoye bureniye lednikov v vysokogornykh usloviyakh . Izvestiya Vsesoyuznogo Geograficheskogo Obshchestva, Tom 99, Vyp. 2, 1967, p. 14748. [Method for deep drilling in glaciers in summer.]Google Scholar
Clothier, W. C. Microscope for use at temperatures near –190°C. Journal of Scientific Instruments, Vol. 44, No. 7, 1967, p. 53536. [Microscope used for visual observation of ice formation.]Google Scholar
Higashi, A. Oguro, M. Hikiage-hō ni yoru hyō-tankesshō no seisaku (1). Kōgakuteki kanzen tankesshō to teni . Ōyō Butsuri, [Vol.] 36, [No.] 12, 1967, p 98894. [Method of growth avoiding bubbles, vapour figures, and low-angle grain boundaries. Determination of dislocation densities.]Google Scholar
Hindman, E. E. jr. Rinker, R. L. Continuous snowfall replicator., Journal of Applied Meteorology, Vol. 6, No. 1, 1967, p. 12633. [Method of studying individual snow crystals and their concentration.]Google Scholar
Martinelli, M. jr. New snow-measuring instruments. (In Sopper, W. E. Lull, H. W., ed. Forest hydrology: proceedings of a National Science Foundation advanced science seminar held at the Pennsylvania State University…, Aug. 29–Sept. 10, 1965. Oxford and New York, Pergamon Press, 1966, p. 797800.) [Brief discussion on eight instruments for measuring hydrological strength and mechanical properties of snow, on the basis of published reports.]Google Scholar
Nakamura, T. Netsuban ni yoru sekisetsu usuita no sakusei . Teion-kagaku: Low Temperature Science, Ser. A, [No.] 24, 1966, p. 13337. [Method for making thin sections for structural studies.]Google Scholar
Sekurov, A. V. Osobennosti razrabotki elektrotermoburovogo kompleksa dlya bureniya I’da i rezul’taty yego ispytaniy v Mirnom v 1965–66 . Informatsionnyy Byulleten’ Sovetskoy Antarkticheskoy Ekspeditsii, No. 60, 1967, p.5962.Google Scholar
Smith, J. L. Willen, D. W. Gamma-transmission profiling radioisotope snow density and depth gage. Proceedings of the Western Snow Conference, 34th annual meeting, 1966, p. 6977. [Apparatus described. Easily portable and may be remote-controlled.]Google Scholar
Warner, O. R. Precipitation gages—types, methods and uses. Proceedings of the Western Snow Conference, 34th annual meeting, 1966, p. 7881. [Describes gauges used by U.S. Weather Bureau, and mentions new developments.]Google Scholar
Watanabe, Z. Mould of deposited snow. (In Ōura, H., ed. Physics of snow and ice.… Vol. 1, Pt. 2. [Sapporo], Institute of Low Temperature Science, Hokkaido University, 1967, p. 74150.) [Method of making a plaster of Paris mould around snow to allow its structure to be studied later at room temperature.]Google Scholar
Yosida, Z. Free water content of wet snow. (In Oura, H., ed. Physics of snow and ice.… Vol. 1, Pt. 2. [Sapporo], Institute of Low Temperature Science, Hokkaido University, 1967, p. 77384.) [History of development of calorimeter now in use to measure this, and details of’ the instrument.]Google Scholar

Physics of Ice

Barduhn, A. J. Desalination by crystallization processes. Chemical Engineering Progress, Vol. 63, No. 1, 1967, p. 98103. [Review of progress since 1965 in desalination of seawater by freezing and hydrate processes.]Google Scholar
Barzynski, H. Suhulte-Frohlinde, D. On the nature of the electron traps in alkaline ice. Zeitsthrf für Naturforschung, Bd. 22a, Ht. 12, 1967, p. 213132. [Nature of electron traps formed by y-irradiation in frozen NaOH solutions. The effect is large only in amorphous solids.]Google Scholar
Beaubouef, R. T. Chapman, A. J. Freezing of fluids in forced flow. International Journal of Heat and Mass Transfer, Vol. 10, No. 11, 1967, p. 158187. [Theoretical study of freezing of tee from water flowing past a cold surface. French, German and Russian abstracts.]Google Scholar
Bennett, J. E., and others. Trapped electrons produced by the deposition of alkali metal atoms on ice and solid alcohols at 77°K. I. Optical spectra and electron spin resonance spectra, by J. E. Bennett, B. Mile and A. Thomas. Journal of the Chemical Society, Sect. A, 1967, No. 9, p. 139399. [Deposition yields intensely coloured deposit whose spectra show structure due to interaction of electron with H atoms.]Google Scholar
Bondot, P. Etude du spectre de diffraction des rayons X par une glace vitreuse. Comptes Rendus Hebdomadaires des Séances de I’Académie des Sciences (Paris), Tom. 265, Sér. B, No. 5, 1967, p. 31658. [Comparison between X-ray diffraction pattern of vitreous ice and that of water.]Google Scholar
Brey, W. S. jr. Williams, H. P. Dielectric properties of ice and water clathrates. Journal of Physical Chemistry, Vol. 72, No. 1, 1968, p. 4952. [Measurement in audio-frequency range between −30° and 2°C. Clathrates show distribution of relaxation times and higher frequency loss maximum.]Google Scholar
Brian, P. L. T., and others. Vapor-flow limitations in a melter-condenser, [by] P. L. T. Brian, K. A. Smith, and L. W. Petri. Industrial and Engineering Chemistry. Process Design and Development, Vol. 7, No. 1, 1968, p. 2125. [Model for melting of ice crystals by direct contact with a condensing vapour.]Google Scholar
Bromer, D. J. Kingery, W. D. Flow of polycrystalline ice at low stresses and small strains. Journal of Applied Physics, Vol. 39, No. 3, 1968, p. 168891. [Tests on columnar ice in tension perpendicular to column axis. Results interpreted in terms of Nabarro-Herring creep with diffusion enhanced by grain-boundaries.]Google Scholar
Bullemer, B. Riehl, N. Hall-Effekt an Protonen in Eis. Physik der kondensierten Materie, Bd. 7, Ht. 3, 1968, p. 24860. [Allowing for surface conductivity, the Hall coefficient for protons in ice has been measured. The high mobility is interpreted in terms of correlated jumps.]Google Scholar
Camp, P. R. Spears, D. L. Conductivity changes produced in ice by optical irradiation 0.8 to 2.7 p. (In Ōura, H., ed. Physics of snow and ice.… Vol. 1, Pt. 1. [Sapporo], Institute of Low ‘Temperature Science, Hokkaido University, 1967, p. 581206.) [Experiments showing that optical irradiation applied to ice did not create electrical point defects.]Google Scholar
De Michell, S. M. E Licenblat, A. R. Experimental study of the evaporation of ice in controlled conditions of subsaturation. (In Ōura, H,. ed. Physics of snow and ice.… Vol. 1, Pt. 1. [Sapporo], Institute of Low Temperature Science, Hokkaido University, 1967, p. 25966.) [Study of evaporation rate and surface morphology of ice evaporating under controlled conditions.]Google Scholar
Dillon, H. B. Andersland, O. B. Deformation rates of polycrystalline ice. (In Ōura, H., ed. Physics of snow and ice.… Vol. 1, Pt. 1. [Sapporo]. Institute of Low Temperature Science, Hokkaido University, 1967, p. 31327.) [Compressive creep and constant strain-rate tests. Deduction of flow law and activation energy.]Google Scholar
Drake, J. C. Electrification accompanying the melting of ice particles. Quarterly, Journal of the Royal Meteorological Society, Vol. 94, No. 400, 1968, p. 17691. [Laboratory observation of convection currents in partly frozen droplets and of electric charging due to bubbles bursting after transference to the surface.]Google Scholar
Dye, J. E. Hobbs, P. V. The influence of environmental parameters on the freezing and fragmentation of suspended water drops. Journal of the Atmospheric Sciences, Vol. 25, No. 1, 1968, p. 8296. [Discussion of factors which might affect freezing behaviour, and laboratory experiments to show when splintering and shattering occur.]Google Scholar
Edwards, G. R. Evans, L. F. Ice nucleation by silver iodide. III. The nature of the nucleating site. Journal of the.Atmospheric Sciences, Vol. 25, No. 2, 1968, p. 24956. [Number of sites nucleating ice by freezing mechanism and by sorption at water saturation found experimentally.]Google Scholar
Eiben, K. Taub, I. A. Solvated electron spectrum in irradiated ice. Nature, Vol. 216, No. 5117, 1967, p. 78283. [Observation after intense 7–irradiation at 77°K.]Google Scholar
Gabarashvili, T. G. Gliki, N. V. Vozniknoveniye ledyanoy fazy y pereokhlazhdennoy vode pod vliyaniyem elektricheski zaryazhennykh kristallov kholesterol i naftalina . Izvestiya Akademii Nauk SSSR. Fizika Atmosfery i Okeana, Tom 3, No. 5, 1967, p. 57074. [Experiment to show that charged crystals are more effective nuclei, and theory of effect. English translation in Iz estiya. Academy of Sciences, U.S.S.R. Atmospheric and Oceanic Physics, Vol. 3, No. 5, 1967, p. 324–27.]Google Scholar
Genadiev, N. Interdependence between cooling rate and freezing temperature of waterdrops on metal plate. Comptes Rendus de l’Académie Bulgare des Sciences, Tom. 20, No. 12, 1967, p. 127174. [Experimental results, comparison with work of Gokhale, and theoretical discussion.]Google Scholar
Ghormley, J. A. Enthalpy changes and heat-capacity changes in the transformations from high-surface-area amorphous ice to stable hexagonal ice. Journal of Chemical Physics, Vol. 48, No. 1, 1968, p. 50308. [Measurements indicate that ice Ic has higher heat capacity, and may be stable form of ice at low temperatures.]Google Scholar
Gilra, N. K., and others. Ultrasonic absorption by ice crystals in supercooled water, [by] N. K. Gilra, N. Dass and N. C. Varshneya. Journal of the Physical Society of Japan, Vol. 24, No. 2, 1968, p. 38082. [Theoretical study of variation of absorption with frequency, crystal size and kinematic viscosity, and effect of ultrasound on growth.]Google Scholar
Glen, J. W. Jones, S. J. The deformation of ice single crystals at low temperatures. (In Ōura, H., ed. Physics of snow and ice.… Vol. 1, Pt. 1. [Sapporo], Institute of Low Temperature Science, Hokkaido University, 1967, p. 26775.) [Tensile creep tests on ice single crystals from −50° to −70°C. Deduction of flow law and slip direction.]Google Scholar
Gold, L. W. Time to formation of first cracks in ice. (In Ōura, H., ed. Physics of snow and ice.… Vol. 1, Pt. 1. [Sapporo], Institute of Low Temperature Science, Hokkaido University, 1967, p. 35970.) [Observations used to determine activation energy. Results consistent with dislocation pile-up theories of crack nucleation.]Google Scholar
Higashi, A. Mechanisms of plastic deformation in ice single crystals. (In Ōura, H., ed. Physics of snow and ice.… Vol. 1, Pt. 1. [Sapporo], Institute of Low Temperature Science, Hokkaido University, 1967, p. 27789.) [Dislocation mechanism of slip of ice single crystals. Difference of behaviour in basal and non-basal glide.]Google Scholar
Higuchi, K. Yosida, T. Crystallographic orientation of frozen droplets on ice surfaces. (In Ōura, H., ed. Physics of snow and ice.… Vol. 1, Pt. 1. [Sapporo], Institute of Low Temperature Science, Hokkaido University, 1967, p. 7993.) [Photogrammetric measurements on snow particles consisting of several single crystals show crystallographic relations between orientations.]Google Scholar
Hill, M. J. Wyard, S. J. Low frequency electron spin resonance of irradiated ice and frozen solutions of hydrogen peroxide. Journal of Physics B, Ser. 2, Vol. 1, No. 2, 1968, p. 28994. [Study at 280 MHz and comparison with other data of spectrum attributed to OH in ice.]Google Scholar
Hogan, A. W. Ice nuclei from direct reaction of iodine vapor with vapors from leaded gasoline. Science, Vol. 158, No. 38°2, 1967, p. 100. [Large numbers of ice nuclei active at <−15°C generated by mixing iodine vapour with vapours from petrol if, and only if, the petrol contains lead.]Google Scholar
Itagaki, K. Particle migration on ice surfaces. (In Ōura, H., ed. Physics of snow and ice.… Vol. 1, Pt. 1. [Sapporo], Institute of Low Temperature Science, Hokkaido University, 1967, p. 23346.) [Observations of small glass beads on ice surfaces show migration and clustering when atmosphere is unsaturated.]Google Scholar
Jaccard, C. Electrical conductivity of the surface layer of ice. (In Ōura, H., ed. Physics of snow and ice.… Vol. 1, Pt. 1. [Sapporo], Institute of Low Temperature Science, Hokkaido University, 1967, p. 17379.) [Measurement of surface conductivity and effect of an air stream on it.]Google Scholar
Kobayashi, T. On the variation of ice crystal habit with temperature. (In Ōura, H., ed. Physics of snow and ice…. Vol. 1, Pt. 1. [Sapporo], Institute of Low Temperature Science, Hokkaido University, 1967, p. 95104.) [Experiments on surface migration of water molecules on ice agree with Mason’s results rather than Hallett’s.]Google Scholar
Krastanov, L., and others. On the ice-forming activity of the walls of an ice crystal, [by] L. Krastanov, G. Miloshev [and] L. Levkov. Comptes Rendus de l’Académie Bulgare des Sciences, Tom. 20, No. 9, 1967, p. 91518. [Theory of nucleation of 2–dimensional ice embryos on plane ice surfaces.]Google Scholar
Langer, G., and others. Ice nucleation efficiency of silver iodide at −20C on a particle count basis, [by] G. Langer, A. Lieberman and J. Rosinski. Journal of Applied Meteorology, Vol. 6, No. 5, 1967, p. 96365. [Results show anomalously low number of particles are active as nuclei.]Google Scholar
Levi, L. Electrical properties of ice doped with different electrolytes. (In Ōura, H., ed. Physics of snow and ice…. Vol. 1, Pt. 1. [Sapporo], Institute of Low Temperature Science, Hokkaido University, 1967, p. 15972.) [Study of d.c. conductivity of ice doped with HF and other hydracids, NH3 and also NH3 and HF together. Interpretation in terms of defect mobility.]Google Scholar
Levi, L. Gavanovich, S. Helical whiskers of ice. (In Ōura, H., ed. Physics of snow and ice…. Vol. 1, Pt. 1. [Sapporo], Institute of Low Temperature Science, Hokkaido University, 1967, p. 4350.) [Observation of whiskers formed in cold formvar solutions.]Google Scholar
Luyet, B. Attacks from different fronts on some complex cases of instability in aqueous solutions solidified at low temperatures. (In Ōura, H., ed. Physics of snow and ice…. Vol. 1, Pt. 1. [Sapporo], Institute of Low Temperature Science, Hokkaido University, 1967, p. 7178.) [Use of differential thermal analysis, dielectric measurements and X-ray diffraction.]Google Scholar
Luyet, B. Various modes of recrystallization of ice. (In Ōura, H., ed. Physics of snow and ice…. Vol. 1, Pt. 1. [Sapporo], Institute of Low Temperature Science, Hokkaido University, 1967, p. 5170.) [Description of various structural changes occurring in aqueous solutions solidified at low temperatures.]Google Scholar
Macklin, W. C. Payne, G. S. Some aspects of the accretion process. Quarterly Journal of the Royal Meteorological Society, Vol. 94, No. 400, 1968, p. 16775. [Experimental and theoretical studies of process of ice accretion from supercooled water droplets.]Google Scholar
Macklin, W. C. Ryan, B. F. Growth velocities of ice in supercooled water and aqueous sucrose solutions. Philosophical Magazine, Eighth Ser., Vol. 17, No. 145, 1968, p. 8387. [Measurement of component velocities of growth parallel and perpendicular to basal plane with up to so deg of supercooling.]Google Scholar
Maeno, N. Air bubble formation in ice crystals. (In Ōura, H., ed. Physics of snow and ice…. Vol. 1, Pt. 1. [Sapporo], Institute of Low Temperature Science, Hokkaido University, 1967, p. 20718.) [Investigation of formation of air bubbles in natural and artificial ice crystals and mode of their formation and metamorphosis.]Google Scholar
Maeno, N. Nuclei of Tyndall figures and surface melting of ice. Canadian Journal of Physics, Vol. 46, No. 4, 1968, p. 31315. [Attempt to identify nuclei. Submicroscopic gaseous inclusions are favoured.]Google Scholar
Maeno, N. Suihyókaiinen ni okeru kihb no hassei to hosoku . Teion-kagaku: Low Temperature Science, Ser. A, [No.] 24, 1966, p. 91109. [Microscopic observations. English summary.]Google Scholar
Magono, C. Shio, H. Frictional electrification of ice and change in its contact surface. (In Ōura, H., ed. Physics of snow and ice…. Vol. 1, Pt. 1. [Sapporo], Institute of Low Temperature Science, Hokkaido University, 1967, p. 13750.) [Explanation of frictional electrification when ice is rubbed on ice. Above −5°C the sign of the effect changes.]Google Scholar
Mascarenhas, S. Arguello, C. Studies on HF-doped ice thermo-electrets. Journal of the Electrochemical Society, Vol 115, No. 4, 1968, p. 38688. [Electrets prepared at −10° to −135°C and stored charge measured.]Google Scholar
Mellor, M. Smith, J. H. Creep of ice and snow. (In Ōura, H., ed. Physics of snow and ice.… Vol. 1, Pt. 2. [Sapporo], Institute of Low Temperature Science, Hokkaido University, 1967, p. 84355.) [Constant load compressive creep tests on sintered snow and bubbly polycrystalline ice.]Google Scholar
Michel, B. From the nucleation of ice crystals in clouds to the formation of frazil ice in rivers. (In Ōura, H., ed. Physics of snow and ice…. Vol. 1, Pt. 1. [Sapporo], Institute of Low Temperature Science, Hokkaido University, 1967, p. 52936.) [Use of heterogeneous nucleation theory to explain supercooling of water droplets and large water bodies.]Google Scholar
Nakamura, T. A water-like film produced by pressure on the surface of ice crystals. (In Ōura, H., ed. Physics of snow and ice…. Vol. 1, Pt. 1. [Sapporo], Institute of Low Temperature Science, Hokkaido University, 1967, p. 24758.) [Observation of glass plate pressed against ice showed water-like film down to −30°C.]Google Scholar
Odencrantz, F. K. Modification of habit and charge of ice crystals by vapor contamination. Journal of the Atmospheric Sciences, Vol. 25, No. 2, 1968, p. 33738.Google Scholar
Onaka, R. Takahashi, T. Vacuum UV absorption spectra of liquid water and ice. Journal of the Physical Society of Japan, Vol. 24, No. 3, 5968, p. 54850. [Cubic ice has a well-defined absorption band near 8.7 eV while hexagonal and amorphous ice show only a gradual rise of absorption from 7 to 10 eV.]Google Scholar
Onsager, L. Ferroelectricity of ice? (In Weller, E. F., ed. Ferroelectricity. Proceedings of the Symposium on Ferro-electricity, General Motors Research Laboratories, Warren, Michigan, 1966. Amsterdam, etc., Elsevier Publishing Co., 1967, p. 1619.) [Discussion of mechanism producing electrical properties of ice at low temperature.]Google Scholar
Parungo, F. P. Wood, J. Freezing of aqueous solutions of macromolecules. Journal of the Atmospheric Sciences, Vol. 25, No. 1, 1968, p. 15455. [Attempts to nucleate ice with macromolecules holding water showed no marked correlation with nuclear magnetic resonance line width.]Google Scholar
Pruppacher, H. R., and others. On the electrical effects that accompany the spontaneous growth of ice in supercooled aqueous solutions, [by] H. R. Pruppacher, E. H. Steinberger and T. L. Wang. Journal of Geophysical Research, Vol. 73, No. 2, 1968,p. 57184. [Measurements of potentials developed. Discussion of connection with Workman-Reynolds effect and thunderstorm electricity.]Google Scholar
Roberts, P. Hallett, J. A laboratory study of the ice nucleating properties of some mineral particulates. Quarterly Journal of the Royal Meteorological Society, Vol. 94, No. 399, 1968, P. 2534. [Results for kaolinite and montmorillonite and other natural substances including surface glacier debris.]Google Scholar
Rohatgi, P. K. Adams, C. M. jr. Effect of freezing rates on dendritic solidification of ice from aqueous solutions. Transactions of the Metallurgical Society of AIME, Vol. 239, No. 11, 1967, p. 172936. [Spacing between ice platelets related to freezing time and freezing rate.]Google Scholar
Rohatgi, P. K., and others. Dendritic crystallization of ice from aqueous solutions, [by] P. K. Rohatgi, S. M. Jain and C. M. Adams, Jr . Industrial and Engineering Chemistry. Fundamentals, Vol. 7, No. 1, 1968, p. 7279. [Spacing of ice platelets as function of distance, freezing rate and solute concentration, including effects in ternary and quaternary solutions.]Google Scholar
Schaefer, V. J. Ice nuclei from auto exhaust and organic vapors. Journal of Applied Meteorology, Vol. 7, No. 1, 1968, p. 14849. [Observation shows lead from automobile exhaust forms lead iodide and acts as efficient ice nucleator.]Google Scholar
Shubin, V. N., and others. Spektry opticheskogo pogloshcheniya kristallicheskogo l’da i zamorozhennykh kristallicheskikh vodnykh rastvorov , Doklady Akademii Nauk SSSR, Torn 174, No. 2, 1967, p. 41618. [Absorption spectra of ice and frozen LiClO4 and KOH solutions subjected to pulse radiolysis.]Google Scholar
Silver, E. G. Pulsed neutron measurement of the diffusion parameters in ordinary ice as a function of temperature. (In Pulsed neutron research. Proceedings of the Symposium on Pulsed Neutron Research held by the International Atomic Energy Agency at Karlsruhe, 10–14 May 1965. Vol. 1. Vienna, International Atomic Energy Agency, 1965, p. 3548.) [Measurement of parameters for diffusion of neutrons in ice.]Google Scholar
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Land ice. Glaciers. Ice shelves

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Vivian, R. Gabbero, J.-C. Fiches des glaciers français. Le glacier des sources de l’Isère. Revue de Géographie Alpine, Tom. 56, Fase. 1, 1968, p. 20911. [General description.]Google Scholar
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Icebergs. Sea, River and Lake Ice

Addison, J. R. Pounder, E. R. The electrical properties of saline ice. (In Ōura, H., ed. Physics of snow and ice…. Vol, 1, Pt. 1. [Sapporo], Institute of Low Temperature Science, Hokkaido University, 1967, p. 64960.) [Measurements of dielectric constant and resistivity of laboratory-grown saline ice from 20 Hz to 10 kHz and various salinities.]Google Scholar
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Glacial Geology

Barnett, D. M. Peterson, J. A. Comments on “Sur le lieu de fonte sur place de la calotte glacière [sic] de Scheffer”. Canadian Geographer, Vol. 12, No. 1, 1968, p. 5354. Criticisms of paper by Laverdière, ibid., Vol. 11, No. 2, 1967, p. 86–95.]Google Scholar
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Carryer, S. J. The glacial deposits along the northern flank of the Mount Hutt Range. New Zealand journal of Geology and Geophysics, Vol. 10, No. 4, 1967, p. 113644.Google Scholar
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Gripp, K. Der Abbau des würmzeitlichen Eises im Bereich des Kattegat. Meddelelser fra Dansk Geologisk Forening, Bd. 17, Ht. 1, 1967, p. 5875. [Deglaciation and moraine formation during latest glaciation in Kattegat region. English summary. Critical comment by S. A. Andersen and answer by Gripp in ibid., p. 138–45.]Google Scholar
van der Hammen, T. and others. Stratigraphy, climatic succession and radiocarbon dating of the last glacial in the Netherlands, [by] T. van der Hammen, G. C. Maarleveld, J. C. Vogel and W. H. Zagurijn. Geologie en Mijnbouw, Jaarg. 46, Nr. 3, 1967, p. 7995. [Field data, pollen analysis and 14C dating used to construct climatic curve.]Google Scholar
Hattersley-Smith, G. Long, A. Postglacial uplift at Tanquary Fiord, northern Ellesmere Island, Northwest Territories. Arctic, Vol. 20, No. 4, 1967, p. 25560. [Radiocarbon dating of date of retreat of ice from head of fjord and of subsequent rate of uplift.]Google Scholar
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Hoppe, G. Grimsey and the maximum extent of the last glaciation of Iceland. Ceografska Annaler, Vol. 50A, No. 1, 1968, p. 1624. [This island 40 km north of the mainland is shown to have been glaciated, probably during the Würm.]Google Scholar
Lamb, H. H. Bloch, M. R. Volcanic dust, melting of ice caps, and sea levels. Palaeogeography, Palaeoclimatology, Palaeoecology, Vol. 4, No. 3, 1968, p. 21926. [Criticism by Lamb of paper by Bloch, ibid., Vol. 1, 1965, p. 127–42, and reply by Bloch.]Google Scholar
Laverdière, C. Sur le lieu de fonte sur place de la calotte glaciaire de Scheffer. Canadian Geographer, Vol. 11, No. 2, 1967, p. 8695. [Interest of Labrador-Ungava as one of final refuges of Wisconsin ice sheet.]Google Scholar
Maksimov, Ye. V. Absolyutnaya khronologiya stadiy sokrashcheniya gornykh Iednikov . Sovetskaya Geologiya, 1966, No. 3, p. 8496. [Comparison of data from many parts of world since last glaciation.]Google Scholar
Mercer, J. H. Variations of some Patagonian glaciers since the Late-glacial. American Journal of Science, Vol. 266, No. 2, 1968, p. 91109. [Glacier fluctuations have been broadly in phase with those in northern hemisphere, but advance in recent centuries was relatively weaker.]Google Scholar
Parry, J. T. Geomorphology. Canadian Geographer, Vol. 11, No. 4, 1967, p. 280311. [History of geomorphological study in Canada, including considerable amount of study of glaciers and glacial and periglacial geomorphology.]Google Scholar
Péwé, T. L. Quaternary climatic variations in Antarctica as suggested by glacial fluctuations. (In Pleistocene and post-Pleistocene climatic variations in the Pacific area. Honolulu, Bishop Museum Press, 1966, p. 5782.) [Study of glacial chronology in ice-free areas surrounding McMurdo Sound, 1959–58, enables possible glacial events and climatic changes in region to be outlined.]Google Scholar
Porter, S. C. Glaciation of Chagvan Bay area, southwestern Alaska. Arctic, Vol. 20, No. 4, 1967, p. 22746. [Interpretation of morphologic and stratigraphie evidence in this region.]Google Scholar
Portmann, J.-P. Pétrographie des formations glaciaires à l’est du lac de Bienne (Suisse). Eclogae Geologicae Helvetiae, Vol. 59, No. 2, 1966, p. 697722.Google Scholar
Portmann, J.-P. Qu’attendre de la géologie du Quaternaire? Bulletin de la Société.Neuchdteleise des Sciences Naturelles, Tom. 90, 1967, p. 28590. [The practical applications of the Quaternary geology and the perspective for the future.]Google Scholar
Roed, M. A., and others. The Athabasca Valley erratics train, Alberta, and Pleistocene ice movements across the Continental Divide, by M. A. Roed, E. W. Mountjoy and N. W. Rutter. Canadian journal of Earth Sciences, Vol. 4, No. 4, 1967, p. 62532. [In late (?) Wisconsin time, Cordilleran ice in Jasper National Park area partly derived from west of Continental Divide.]Google Scholar
Schulz, W. Über glazigene Schrammen auf dem Untergrund und sichelförmige Marken auf Geschieben in Norddeutschland. Geographische Berichte, 12. Jahrg., Ht. 43, 1967, p. 12542. [Compilation of observations of striae on bed-rock and crescentic marks on boulders in north Germany. Russian and English summaries.]Google Scholar
Sweizer, G. Le tardiglaciaire et le niveau des neiges permanentes dans les hautes montagnes des Alpes Maritimes. L’exemple du bassin supérieure de la Tinée. Méditerranée, 9e An., No. 1, 1968, p. 2340. [Study of Late-glacial stages in western Alps and corresponding snow line.]Google Scholar
Tremblay, G. Observations et mesures sur les blocs glaciels du cap à l’Orignal. Cahiers de Géographie de Québec, 11e An., No. 23,/967, p. 40211. [Study of erratic boulders on a beach of St. Lawrence River. Method of their movement by ice discussed. English summary.]Google Scholar
Veyret, P. L’épaulement de la vallée glaciaire. A partir de la vallée de Chamonix, une nouvelle conception du problème. Revue de Géographie Alpine, Tom. 56, Fasc. 1, 1968, p. 4364. [Discussion of form of upper part of glacial valley wall.]Google Scholar
Viers, G. Le modelé quaternaire dans le bassin du Rio Tordillo (République Argentine, province de Mendoza). Revue Géographique des Pyrénées et du Sud-Ouest, Tom. 38, [Faso.] 4, 1967, p. 35155, maps at back. [Description of present-day glaciers and Quaternary ones which did not descend much further but were more numerous.]Google Scholar

Frost Action on Rocks and Soil. Frozen Ground. Permafrost

Angély, G. Anciens glaciers rocheux dans l’est des Pyrénées centrales. Revue Géogeaphiyue des Pyrénées et du Sud-Onest, Tom. 38, [Fase.] 1, 1967, p. 528. [Description of three very different rock glaciers.]Google Scholar
Aristov, I. F. Nekotoryye dannyye o moroznom vyvetrivanii i soliflyuktsii v nizkogornoy i srednegornoy zonakh khrebta Kirgizskiy Ala-Too . Izvestiya Akademii Nauk Kirgizskoy SSR. Geografieheskoye Obshchesevo, Vyp. 6, 1966, p. 10506.Google Scholar
Atakanov, U. A. O mnogoletnemerzlykh gornykh porodakh na Sary-Dzhazskikh syrtakh . Izvestiya Akademii Nauk Kirgizskoy SSR. Geograflcheskoye Obshchestvo, Vyp. 6, 1966, p. 7783. [Conditions of occurrence and development of permafrost in this region of Tien-Shan.]Google Scholar
Ball, D. F. Goodier, R. Large sorted stone-stripes in the Rhinog mountains, North Wales. Geográfrska Annaler, Vol. 50a, No. 1, 1968, p. 5459. [Description of patterns 5 to 8 m wide formed during periglacial conditions.]Google Scholar
Brown, J. Tundra soils formed over ice wedges, northern Alaska. Proceedings. Soil Science Society of America, Vol. 31, No. 5, 1967, p. 68691. [Study of these soils and discussion of the role of the ice wedges in their formation and development.]Google Scholar
Brown, R. J. E. Permafrost investigations in British Columbia and Yukon Territory. Canada. National Research Council. Division of Building Research. Technical Paper No. 253, 1967, 115 p. [Investigation of conditions in which permafrost forms.]Google Scholar
Cailleux, A. Hamelin, L.-E. Périglaciaire actuel sur le littoral du Bic (Bas-Saint-Laurent). Cahiers de Géographie de Québec, 11e An., No. 23, 1967, p. 36178. [Study of various periglacial processes in the lower St. Lawrence estuary.]Google Scholar
Corte, A. E. Soil mound formation by multicyclic freeze-thaw. (In Ōura, H., ed. Physics of snow and ice…. Vol. 1, Pt. 2. [Sapporo], Institute of Low Temprrature Science, Hokkaido University, 1967. p. 133338.) [Laboratory studies of mound formation following many cycles of freezing and thawing.]Google Scholar
Crampton, C. B. Taylor, J. A. Solifluction terraces in South Wales. Biueelyn PerygIatjalny, No. 16, 1967, p. 1536. [Interpretation of terraces as formed by thin layers of surface debris moving by frost action over permafrost.]Google Scholar
Dionne, J.-C. Modelé periglaciaire de la région de Mont-Joli, Québec. Cahiers de Géographie de Québec, Ile An., No. 23, 1967, p. 398401. [Description of periglacial landforms in this region of the St. Lawrence estuary.]Google Scholar
Donner, J. J., and others. Ice wedges in south-eastern Finland, by J. J. Donner, V. Lappalainen and R. G. West. Geologiska Föreningens i Stockholm Fdrhandlingar, Vol. 90, Pt. 1, No. 532, 1968, p. 11216. [Ice wedge casts in the Salpausselkä I end moraine attributed to Younger Dryas.]Google Scholar
Dutkiewicz, L. The distribution of periglacial phenomena in NW-Sörkapp, Spitsbergen. Biuletyn PerygIatjalny, No. 16, 1967, p. 3783. [Study of various frost forms, of the efficacy of frost action and of the different zones, leading to a detailed map of frost phenomena in this region.]Google Scholar
Dylik, J. The main elements of Upper Pleistocene paleogeography in central Poland. Biuletyn PerygIatjalny, No. 16, 1967, p. 85115. [Includes discussion of periglacial deposits and fossil structures.]Google Scholar
Elsasser, H. Der Strukturboden auf der Fuorcla da Fàller (Fallerfurka). Die Alpen, 44. Jahrg., 1. Quartal, 1968, p. 3842. [Popular introduction to patterned ground and description of the different types found in this part of Switzerland.]Google Scholar
Everett, K. R. The morphology of the slopes of Ogotoruk Creek Valley, northwest Alaska. Biuletyn Pervglacjalny, No. 16, 1967, p. 11731. [Interpretation of structure and movement of these slopes from trenches cut through them.]Google Scholar
Goździk, J. S. Fauchage des fentes en coin dû aux mouvements de masses sur des pentes douces. Biuletyn Peryglacjalny, No. 16, 1967, p. 13346. [Study of frost wedges on very slight slopes shows that the upper layers are undergoing downhill displacements. English summary.]Google Scholar
Grave, N. A. Temperature regime of permafrost under different geographical and geological conditions. (In Ōura, H., ed. Physics of snow and ice…. Vol. 1, Pt. 2. [Sapporo], Institute of Low Temperature Science, Hokkaido University, 1967, p. 1339-43.) [Discussion of what determines temperature regime.]Google Scholar
Guillien, Y. Pinot, J.-P. Formations glaciaires et interglaciaires autour des Grands Lacs. Bulletin de l’Association Française pour l’Étude du Quaternaire, 3e An., No. 6, 1966, p. 3139. [Report on glacial and interglacial deposits around the Great Lakes of North America based on the excursions of seventh Congress of INQUA.]Google Scholar
Holmes, G. W., and others. Pingos in central Alaska, by G. W. Holmes, D. M. Hopkins and H. L. Foster. U.S. Geological Survey. Bulletin 1241–H, 1968, iv, 40 p. [Study of distribution, form, vegetation, hydrology, micro-relief, evolution and age.]Google Scholar
Horiguchi, K. Shimobashira no seichà katei no kansatsu . Teion-kagaku: Law Temperature Science, Ser. A, [No.] 25, 1967, p. 17177. [Ciné film observation of growth of needle ice from soil in laboratory. English summary.]Google Scholar
Ivanov, N. S. Gavril’yev, R. I. Teplofrzicheskiye svoyslva merzlykh gornykh porod . Moscow, Izdatel’stvo “Nauka”, 1965. 72 p. [Compilation of data on properties of frozen ground and discussion of theory.]Google Scholar
Jahn, A. Some features of mass movement on Spitsbergen slopes. Geografiska Annaler, Vol. 49a, Nos. 2–4, 1967, p. 21325. [Description of solifluction, rock falls and avalanches. Field work in Hornsund area, Vestspitsbergen.]Google Scholar
Jumikis, A. R. Upward migration of soil moisture by various mechanisms upon freezing. (In Ōura, H., ed. Physics of snow and ice. Vol. 1, Pt. 2. [Sapporo], Institute of Low Temperature Science, Hokkaido University, 1967, p. 138799.) [Conditions under which different transfer mechanisms act.]Google Scholar
Kinosita, S. Heaving force of frozen soils. (In Ōura, H., ed. Physics of snow and ice…. Vol. 1, Pt. 2. [Sapporo], Institute of Low Temperature Science, Hokkaido University, 1967, p. 134560.) [Field and laboratory measurements.]Google Scholar
Kinosita, S., and others. Dennetsu de atatameta tochi no shimobashira . Teionkagaku: Low Temperature Science, Ser. A, [No.] 25, 1967, p. 18595. [By heating the surface, needle ice can be induced to form there instead of only at depth. Study of the formations. English summary.]Google Scholar
Kinosita, S., and others. Tbjoryoku. II. Genjö sokutei kekka ni tsuite . Teion-kagaku: Low Temperature Science, Ser. A, [No.] 24, 1966, p. 28597. [Measurement of force on rigid iron disc. English summary.]Google Scholar
Mackay, J. R. Underwater patterned ground in artificially drained lakes, Garry Island, N.W.T. Geographical Bulletin (Ottawa), Vol. 9, No. 1, 1967, p. 3344. [Vertical heaving under winter ice cover may help to form patterned ground under lakes on island on rim of Mackenzie Delta.]Google Scholar
Martini, A. Preliminary experimental studies on frost weathering of certain rock types from the West Sudetes. Biuletyn Peryglacjalny, No. 16, 1967, p. 14794. [Laboratory study of frost weathering compared with field data.]Google Scholar
Moign, A. Guilcher, A. Une flèche littorale en milieu périglaciaire arctique: la flèche de Sars (Spitsberg). Norois, 14e An., No. 56, 1967, p. 54968. [Evolution of the Sars spit, Vestspitsbergen, described, including influence of sea ice and glacial origin of material.]Google Scholar
Mudrov, Yu. V. Tumel’, N. V. Le rôle de la tixotrophie dans l’évolution du microrelief des pays du nord et des hautes montagnes. Biuletyn Peryglacjalny, No. 16, 1967, p. 195201. [Under certain physical influences, without changing its water content, a soil may become liquid and flow, returning to the solid state when the influence is removed. Role of this process in development of microrelief in cold climates.]Google Scholar
Mycielska-Dowgiałło, E. Formy szczelinowe i inwolucyjne w piaskach i zwirach doliny Wisly kolo Tarnobrzega . Biulelyn Peryglacjalny, No. 16, 1967, p. 20315. [English summary p. 213–15.]Google Scholar
Penner, E. Pressures developed during the unidirectional freezing of water-saturated porous materials. Experiment and theory. (In Ōura, H., ed. Physics of snow and ice…. Vol. 1, Pt. 2. [Sapporo], Institute of Low Temperature Science, Hokkaido University, 1967, p. 140112.) [Theory of origin of pressures in ice lens growth and experiments with glass bead pads to test this.]Google Scholar
Roberts, D. Occurrences of weathering pits from Soray, northern Norway. Geografrska Annaler, Vol. 50A, No. 1, 1968, p. 6063. [Description of these pits and discussion of their origin; microgelivation thought to be most important causative factor.]Google Scholar
Rohdenburg, H. Eiskeilhorizonte in südniedersächsischen and nordhessischen Lössprofllen. Biuletyn Peryglacjalny, No. 16, 1967, p. 22545. [Ice wedges identified in loess profiles in this part of Germany interpreted in terms of climatic variations.]Google Scholar
Soons, J. M. Rainer, J. N. Micro-climate and erosion processes in the Southern Alps, New Zealand. Geografrslca Annaler, Vol. 50A, No. 1, 1968, p. 115. [Includes discussion of importance of needle ice as agent of erosion.]Google Scholar
Svensson, H., and others. Polygonal ground and solifluction features. Photographic interpretation and field studies in northernmost Scandinavia, by H. Svensson, H. Källander, A. Maack and S. Ohrngren. Lund Studies in Geography, Ser. A, No. 40, 1967, 67 p. [Four papers: H. Svensson, “A tetragon patterned block field”, p. 8–23; H. Källander, “Patterned ground and solifluction at North Cape, Ma,geray”, p. 24–40; A. Maack, “Fossil ice-wedge polygons in the Kunes and Bätsfjord areas”, p. 41–57; S. Ohrngren, “Polygon fields on the Laksefjord, Finnmark”, p. 58–67.]Google Scholar
Tanuma, K. Tojáryo to gansui-hi no kankei. I . Teíon-kagaku: Low Temperature Science, Ser. A, [No.] 25, 1967, p. 17984. [Study of amount of frost heaving during unidirectional freezing in an “open system”. English summary.]Google Scholar
Turbin, L. L. Konyukhov, A. G. Merzlotnyye obrazovaniya vnutrennego Tyan’ Shanya . Izvestiya Akademii Nauk Kirgizskoy SSR. Geograilcheskoye Obshchestvo, Vyp. 6, 1966, p. 10710. [General description of features observed.]Google Scholar
Uhlmann, D. R. Jackson, K. A. Frost heave in soils. The influence of particles on solidification. (In Ōura, H., ed. Physics of snow and ice…. Vol. 1, Pt. 2. [Sapporo], Institute of Low Temperature Science, Hokkaido University, 1967, p. 136173.) [Theoretical study of frost heave rate in various soils and comparison with observations.]Google Scholar
Williams, R. E. Ground water flow systems and related highway pavement failure in cold mountain valleys. Journal of Hydrology (Amsterdam), Vol. 6, No. 2, 1968, p. 18393. [Includes study of formation of ice lenses in valleys and effect of highways on them.]Google Scholar
Yefimov, A. I. Dukhin, I. Y. E. Maksimal’nyye glubiny zaleganiya mnogoletnemerzlykh gornykh porod . Geologiya i Geqfizika, 1966, No. 7, p. 9297. [Calculated and observed depths from various parts of northern hemisphere.]Google Scholar
Yong, R. N. On the relationship between partial soil freezing and surface forces. (In Ōura, H., ed. Physics of snow and ice… Vol. 1, Pt. 2. [Sapporo], Institute of Low Temperature Science, Hokkaido University, 1967, p. 137585.) [Role of surface forces in determining amount of unfrozen water in frozen soils, and effect of this on strength.]Google Scholar

Meteorological and Climatological Glaciology

Aufdermaur, A. N. Joss, J. A wind tunnel investigation on the local heat transfer from a sphere, including the influence of turbulence and roughness. Zeitschrift filr angewandte Mathematik and Physik, Vol. 18, Fase. 6, 1967, p. 85266. [Model experiments on heat transfer from objects shaped like natural hailstones.]Google Scholar
Browning, K. A. Beimers, I. G. D. The oblateness of large hailstones. Journal of Applied Meteorology, Vol. 6, No. 6, 1967, p. 107581. [Study of sections of large hailstones to show how shape changes with time.]Google Scholar
Gensler, G. A. Typische Schnee- and Witterungsverhältnisse im Sommer in den Alpen. Les Alpes. Revue du Club Alpin Suisse, 42e An., No. 2, 1966, p. 8185. [Relationship between Alpine snow line and summer weather.]Google Scholar
Gitlin, S. N., and others. The liquid water content of hailstones, [by] S. N. Gitlin and G. G. Goyer and T. J. Henderson. Journal of the Atmospheric Sciences, Vol. 25, No. 1, 1968, p. 9799. [Calorimetric measurements of hailstones in Kenya, Colorado and South Dakota.]Google Scholar
List, R. Dussault, J.-G. Quasi steady state icing and melting conditions and heat and mass transfer of spherical and spheroidal hailstones. Journal of the Atmospheric Sciences, Vol. 24, No. 5, 1967, p. 52229. [Theory of heat and mass exchange of hailstones. Axial ratio shown to be unimportant.]Google Scholar
MacCready, P. B. jr. Baughman, R. G. The glaciation of an AgI-seeded cumulus cloud. Journal of Applied Meteorology, Vol. 7, No. 1, 1968, p. 13235. [Direct observation of cloud particles shows seeded cloud to consist entirely of ice particles.]Google Scholar
Ohtake, T. Alaskan ice fog. I. (In Ōura, H., ed. Physics of snow and ice…. Vol. 1, Pt. 1. [Sapporo], Institute of Low Temperature Science, Hokkaido University, 1967, p. 10558.) [Electron-microscope study of nuclei in ice fog particles and study of conditions of formation of ice fog.]Google Scholar
Rosinski, J. Insoluble particles in hail and rain. Journal of Applied Meteorology, Vol. 6, No. 6, 1967, p. 106674. [Includes study of particles in hailstones.]Google Scholar
Vittori, O. A. Prodi, V. Scavenging of atmospheric particles by ice crystals. Journal of the Atmospheric Sciences, Vol. 24, No. 5, 1967, p. 53338. [Ice crystals growing in supercooled clouds studied to determine their ability to include foreign particles.]Google Scholar
Weller, G. E. Radiation fluxes over an Antarctic ice surface, Mawson, 1961–62. ANARE Scientific Reports. Series A(IV). Glaciology. Publication No. 96, 1967, [vi], 106 p. [Measurement for two years of upwards and downwards flux of both short and long wavelength radiation. Radiation balance deduced.]Google Scholar

Snow

Ager, B. Snow cover properties and winter climate in north Sweden. (In Ōura, H., ed. Physics of snow and ice…. Vol. 1, Pt. 2. [Sapporo], Institute of Low Temperature Science, Hokkaido University, 1967, p. 102936.) [Grain-size and density distributions for different snow types, hardness of snow, and effect of winter climate.]Google Scholar
Akitaya, E. Shimo zarame yuki no kenkyii. II . Teion-kagaku: Low Temperature Science, Ser. A, [No.] 25, 1967, p. 3747. [Laboratory study of conditions under which depth hoar crystals form. English summary.]Google Scholar
Akitaya, E. Some experiments on the growth of depth hoar. (In Ōura, H., ed. Physics of snow and ice…. Vol. 1, Pt. 2. [Sapporo], Institute of Low Temperature Science, Hokkaido University, 1967, p. 71323.) [Laboratory study. Depth hoar classified into two types.]Google Scholar
Ambühl, E. 25 ans de mensuration de la neige ä la cabane Rotondo CAS (2 585 m) (1940–1965). Les Alpes. Revue du Club Alpin Suisse, 42e An., No. 2, 1966, p. 91102. [Account of 25 years of snow surveying from station “cabane Rotondo CAS” at the base of the Witenwasserental.]Google Scholar
Anderson, E. A. Development and testing of snow pack energy balance equations. Water Resources Research, Vol. 4, No. 1, 1968, p. 1937. [Method of computing energy balance on a continuous basis described and tested with 5 years of data from Central Sierra Snow Laboratory.]Google Scholar
Anderson, H. W. West, A. J. Snow accumulation and melt in relation to terrain in wet and dry years. Proceedings of the Western Snow Conference, 33rd annual meeting, 1965, p. 7382. [Analysis of data from 163 snow courses in central Sierra Nevada, California, followed by recommendations for selection of sites for snow courses, depending on nature of terrain.]Google Scholar
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Benson, C. S. Polar regions snow cover. (In Ōura, H., ed. Physics of snow and ice…. Vol. 1, Pt. 2. [Sapporo], Institute of Low Temperature Science, Hokkaido University, 1967, p. 103963.) [General discussion of the different phenomena which occur in snow, both seasonal and perennial, as products and indicators of climate.]Google Scholar
Bilello, M. A. Relationships between climate and regional variations in snow-cover density in North Alnerica. (In Ōura, H., ed. Physics of snow and ice…. Vol. 1, Pt. 2. [Sapporo], Institute of Low Temperature Science, Hokkaido University, 1967, p, 101528.) [Analysis of observations shows four main categories. Nomograph using air temperature and wind speed.]Google Scholar
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Bryukhanov, A. V., and others. On some new approaches to the dynamics of snow avalanches, by A. V. Bryukhanov, S. S. Grigoryan, S. M. Myagkov, M. Ya. Plam, I. Ya. Shurova, M. E. Eglit and Yu. L. Yakimov. (In Ōura, H., ed. Physics of snow and ice…. Vol. 1, Pt. 2. [Sapporo], Institute of Low Temperature Science, Hokkaido University, 1967, p. 122341.) [Theoretical study of avalanche motion and experimental methods used for testing these theories.]Google Scholar
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