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Glaciological Literature

Published online by Cambridge University Press:  30 January 2017

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Copyright © International Glaciological Society 1966

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

References

General Glaciology

Doumani, G. A. ed. Antarctic bibliography. Vol. 1. Washington, Library of Congress, 1965. 506 p. $425.Google Scholar
Lliboutry, L. Traité de glaciologie. Tom. 1. Glace—neige—hydrologie nivale. Tom. 2. Glaciers—variations du climat—sols gelés. Paris, Masson et Cie., 1965. 2 vols.: vi, 427 p.; 429–1040 p.Google Scholar
Loewe, F. Arktis und Antarktis im Lichte neuerer Forschung. Polarforschung, Bd. 5, Jahrg. 34, Ht. 1–2, 1964 [pub. 1965], p. 22536. [Survey of recent glaciological and other research results in the Arctic and Antarctic regions.]Google Scholar
Pal’gov, N. N., ed. Akademiya Nauk Kazakhskoy SSR. Sektor Fizicheskoy Geografii. Glyatsiologicheskiye issledovaniya v Kazakhstane . Vyp. 5. Alma-Ata, Izdatel’stvo “Nauka” Kazakhskoy SSR [Publishing House “Nauka” of the Kazakh S.S.R.], 1965. 190 p. [Continuation of four volumes published 1961–64 entitled Mezhdsnarodnyy Geofizicheskiy God. Glyatsiologicheskiye issledovaniva v period MGG: Zailiyskiy i Dzhungarskiy Alatau (Vyp. 4., Zailiyskiy i Kirgizkiy Alatau) Contains the following papers, all in Russian with English summaries: K. G. Makarevich and P. F. Shabanov, “Ice discharge in the Talgar glaciers and its role in the river runoff”, p. 5–21; R. G. Golovkova, “Radiation and heat balance of accumulation zone of the Zailiysky Alatau glaciers”, p. 22–33; P. A. Sudakov, “On the problem of calculation of atmospheric precipitation in the high mountain areas of the Zailiysky Alatau”, p. 34–45; Ye. N. Vilesov, “Some results of itinerary temperature sounding of the Zailiysky Alatau glaciers”, p. 46–53; R. G. Golovkova and G. A. Rakhimzhanova, “On the problem of ablation heat regime of the central Tuyuksu glacier”, p. 54–61; V. A. Zenkova, “Glacier discharge of the Malaya Almatinka rivers of the Zailiysky Alatau range”, p. 62–72; P. F. Shabanov, “Experience in determination of liquid runoff from glacier fires”, p. 73–78; N. Ya. Barvenko, “On changes of velocity of ice movement on the Tuyuksu glacier of the Zailiysky Alatau mountain range”, p. 79–86; G. A. Tokmagambetov, “Physicomechanical properties of soils of morainic deposits of the Malaya Almatinka glaciers”, p. 87-l00; P. A. Cherkasov and N. V. Ycrasov, “Recent glaciation of the Second Tentek river basin in the Dzhungar Alatau range”, p. 101–16; P. A. Cherkasov, “Seismic sounding of the Aganakty-Tentekskaya river basin glaciers in the Dzhungar Alatau range”, p. 117–34; L. K. Didenko-Kislitsina, “On amount and age of the Dzhungar Alatau glaciation”, p. 135–57; R. V. Khonin, “Recent glaciation in the basin of the Belaya Berel river”, p. 158–71; R. V. Khonin, “On hydrologic regime of the Berel glaciers”, p. 172–80; N. N. Pal’gov, “Determination of natural flow of ice runoff, thickness and mass of mountain glaciers by means of method of balances”, p. 181–89.]Google Scholar
Shumskiy, P. A. Principles of structural glaciology: the petrography of fresh-water ice as a method of glaciological investigation. Translated from the Russian by David Kraus. New York, Dover Publications, 1964. xi, 497 p. $3.00.Google Scholar

Glaciological Instruments and Methods

Kennett, P. Use of aneroid barometers for height determinations on the Larsen Ice Shelf. British Antarctic Survey Bulletin, No. 7, 1965, p. 7780. [Advisability of using aneroid barometers instead of levelling on large ice sheets.]Google Scholar
Pelevin, V. S. Metod prokhodki skvazhin v tolshche l’da posredstvom vysokotemperaturnoy gazovoy strui Informationnyy Byolleten’ Sovetskoy Antarkticheskoy Ekspeditsii , No. 48, 1964, p. 3537.Google Scholar
Philberth, K. Über zwei Elektro-Schmelzsonden mit Vertikalstabilisierung. Polarforschung, Bd. 5, Jahrg. 34, Ht. 1–2, 1964 [pub. 1965], p. 27880. [Description of hotpoints for boring in ice which have good vertical stability.]Google Scholar
Schaefer, V. J. Preparation of permanent replicas of snow, frost, and ice. Weatherwise, Vol. 17, No. 6, 1964, p. 27987. [Survey of current techniques.]CrossRefGoogle Scholar
Smith-Johannsen, R. I. Resin vapour replication technique for snow crystals and biological specimens. Nature, Vol. 205, No. 4977, 1965, p. 120405. [Description of method.]Google Scholar
Wilgain, S., and others. Strontium 90 fallout in Antarctica, [by] S. Wilgain and E. Picciotto [and] W. de Breuck. Journal of Geophysical Research, Vol. 70, No. 24, 1965, p. 602332. [Measurements at “Base Roi Baudouin”, Scott Base and South Pole show three radioactive levels of use in glaciological dating.]Google Scholar

Physics of Ice

Bosen, J. F. Formula for approximation of the ratio of the saturation vapor pressure over ice to that over water at the same temperature. Monthly Weather Review, Vol. 92, No. 11, 1964, p. 508.Google Scholar
Brockamp, B. Querfurth, H. Untersuchungen über die Elastizitätskonstanten von See- and Kunsteis. Polarforschung, Bd. 5, Jahrg. 34, Ht. 1–2, 1964 [pub. 1965], p. 25362. [Ultrasonic measurements of the elastic waves show a temperature dependence of the longitudinal waves, as well as the shear waves.]Google Scholar
Bryant, G. W. Fletcher, N. H. Thermoelectric power of ice containing HF or NH3 . Philosophical Magazine, Eighth Ser., Vol. 12, No. 115, 1965, p. 16576. [Value depends markedly on type and concentration of impurities. Results compared with Jaccard’s theory.]Google Scholar
Chai, S. Y. Vogelhut, P. O. Activation energy of direct-current electrical conductivity of ice with HF and NH3 added. Science, Vol. 148, No. 3677, 1965, p. 159597 [Experimental determination as function of concentration.]Google Scholar
Chalmers, B. Williamson, R. B. Crystal multiplication without nucleation. Science, Vol. 148, No. 3678, 1965, p. 171718. [Observation of growth of disk-shaped crystals below ice layer into supercooled water. Fracture of neck of such crystals suggested as source of frazil ice.]Google Scholar
Chan, R. K., and others. Effect of pressure on the dielectric properties of ice 1, [by] R. K. Chan, D. W. Davidson, and E. Whalley. Journal of Chemical Physics, Vol. 43, No.7, 1965, p. 237683. [Measurements up to 2 kbar of static dielectric constant, relaxation time and d.c. conductivity and discussion of mechanisms.]Google Scholar
Davis, E. Strickland-Constable, R. F. Evaporation and growth of crystals from the vapour phase, (In Rutner, E., and others, ed. Condensation and evaporation of solids: proceedings of the International Symposium on Condensation and Evaporation of Solids, Dayton, Ohio, September 12–14, 1962, edited by E. Rutner, P. Coldftnger [and] J. P. Hirth. New York, London, Gordon and Breach, [c 1964], p. 66579.) [Measurements of rates of growth and evaporation of polycrystalline ice at 80°C. and 90°C. and interpretation of results in terms of mechanisms. Discussion by Motzfeldt and Hirth on p. 678–79.]Google Scholar
Dinger, J. E. Electrification associated with the melting of snow and ice. Journal of the Atmospheric Sciences, Vol. 22, No. 2, 1965, p. 16266. [Experimental results. Interpretation in terms of release of air bubbles.]Google Scholar
Dougherty, T. J. Electrical properties of ice. 1. Dielectric relaxation in pure ice. Journal of Chemical Physics, Vol. 43, No. 9, 1965, p. 324752. [Theoretical study generalizing work of Onsager and Dupuis and of Jaccard.]Google Scholar
Evans, L. F. Requirements of an ice nucleus. Nature, Vol. 206, No. 4986, 1965, p. 822. [Silver iodide is shown to assist nucleation of ice-1 even at pressures at which ice-III is the stable phase.]Google Scholar
Fukuta, N. Activated ice nucleation by sprayed organic solutions. Journal of the Atmospheric Sciences, Vol. 22, No. 2, 1965, p. 20711. [Ice nucleating ability of some organic materials is enhanced by spraying solutions of them. Activation temperatures approaching 0°C. are produced.]Google Scholar
Gold, L. W. The initial creep of columnar-grained ice. Part 1. Observed behavior.—Part II. Analysis. Canadian Journal of Physics, Vol. 43, No. 8, 1965, p. 141422; No. 8, 1965, p. 1423–34. [Part I: results of creep tests in uniaxial compression perpendicular to the long axes of the columns. Part II; analysis of experiments yields a power-law dependence on stress.]Google Scholar
Hickling, R. Nucleation of freezing by cavity collapse and its relation to cavitation damage., Nature, Vol. 206, No. 4987, 1965, p. 91517. [Suggestion that ice nucleates at the very high pressures in cavitation collapse.]Google Scholar
Higashi, A., and others. Bending creep of ice single crystals, [by] A. Higashi, S. Koinuma and S. Mae. Japanese Journal of Applied Physics, Vol. 4, No. 8, 1965, p. 57582. [Experiments on specimens cut from large glacier crystals. Stress and temperature dependence. Results consistent with Johnston’s dislocation theory.]CrossRefGoogle Scholar
Higuchi, K. Tyndall figures formed in crystallographic plane perpendicular to basal plane of ice crystals. Nature, Vol. 202, No. 4931, 1964. p. 48587.Google Scholar
Hobbs, P. V. The aggregation of ice particles in clouds and fogs at low temperatures. Journal of the Atmospheric Sciences, Vol. 22, No. 3, 1965, p. 296300. [The results predicted are found to be in quantitative agreement with the degree of sintering observed in aggregates of ice particles from natural ice fogs.]Google Scholar
Hobbs, P. V. Magono, C. The effect of air bubbles in ice on charge transfer produced by asymmetrical rubbing. Journal of the Atmospheric Sciences, Vol. 21, No. 6, 1964, p. 70607. [Letter from Hobbs discussing mechanism of effect found by Magono and Y. Shiotsuki, ibid., p. 666–70, with reply by Magono.]2.0.CO;2>CrossRefGoogle Scholar
Hobbs, P. V. Scott, W. D. Step-growth on single crystals of ice. Philosophical Magazine, Eighth Ser., Vol. 11, No. 113, 1965, p. 108386. [Theory to explain temperature dependence of step-growth rate and interaction between steps on the basal plane of ice.]Google Scholar
Hobbs, P. V. Scott, W. D. A theoretical study of the variation of ice crystal habits with temperature. Journal of Geophysical Research, Vol. 70, No. 20, 1965, p. 502534. [Theory based on velocity of step-growth on different faces of ice crystals.]Google Scholar
Hoekstra, P., and others. The migration of liquid inclusions in single ice crystals, [by] P. Hoekstra, T. E. Osterkamp, and W. F. Weeks. Journal of Geophysical Research, Vol. 70, No. 20, 1965, p. 503541. [Observation of rate of migration of brine pockets of KCl and NaCl and of solid KCl; discussion of mechanism.]CrossRefGoogle Scholar
Kevan, L. Cation interactions of trapped electrons in irradiated alkaline ice. Journal of the American Chemical Society, Vol. 87, No. 7, 1965, p. 148183. [Line-width studies on electron spin resonance spectra of irradiated alkaline H2O and D2O ice. Results show trapped electrons to be distributed over a radius of at least 3–4 Å.]Google Scholar
Kopp, M., and others. Measurement by NMR of the diffusion rate of HF in ice, [by] M. Kopp, D. E. Barnaal, and I. J. Lowe. Journal of Chemical Physics, Vol. 43, No. 9, 1965, p. 296571. [Measurement and interpretation of very high diffusion rate found.]Google Scholar
Latham, J. The effect of air bubbles in ice on charge transfer produced by asymmetric rubbing. Journal of the Atmospheric Sciences, Vol. 22, No. 3, 1965, p. 32528. [Measurement of charge developed when metal tube coated with ice slid over an ice incline both with and without bubbles in the ice.]Google Scholar
Latham, J. Stow, C. D. Electrification associated with the evaporation of ice. Journal of the Atmospheric Sciences, Vol. 22, No. 3, 1965, p. 32024. [Experimental study of charge developed when ice evaporates with a temperature gradient normal to its surface.]Google Scholar
Latham, J. Stow, C. D. The influence of impact velocity and ice specimen geometry on the charge transfer associated with temperature gradients in ice. Quarterly Journal of the Royal Meteorological Society, Vol. 91, No. 390, 1965, p. 46270.CrossRefGoogle Scholar
Latham, J., and others. Charge transfer between model ice crystals separated in an electric field, by J. Latham, R. E. Mystrom and J. D. Sartor. Nature, Vol. 206, No. 4991, 1965, p. 134445. [Measurement of critical distances for charge transfer between artificial ice crystals of various shapes.]CrossRefGoogle Scholar
Lavrov, V. V. Orazlichii svoystv l’da na szhatiye i na rastyazheniye . Doklady Akademii Nauk SSSR , Tom 162, No. 1, 1965, p. 5456. [Ratio of stress to plastic strain and ultimate strength much lower in tension. Effect attributed to gaps between grains. English translation in Soviet Physics—Doklady, Vol. 10, No. 5, 1965, p. 429–311Google Scholar
Leadbetter, A. J. The thermodynamic and vibrational properties of H2O ice and D2O ice. Proceedings of the Royal Society, Ser. A, Vol. 287, No. 1410, 1965, p. 40325. [Theoretical analysis of thermodynamic properties to deduce terms in the vibrational spectrum of H2O and D2O ice. Amplitudes of vibration of O, H and D atoms are deduced which agree well with X-ray and neutron scattering data.]Google Scholar
Macklin, W. C. Ryan, B. F. The structure of ice grown in bulk supercooled water. Journal of the Atmospheric Sciences, Vol. 22, No. 4, 1965, p. 45259. [Growth directions are not oriented exactly with the basal plane of the seed; complex structure resulting is studied by flash photography.]Google Scholar
Philip, J. R. Kinetics of growth and evaporation of droplets and ice crystals. Journal of the Atmospheric Sciences, Vol. 22, No. 2, 1965, p. 196206. [Theoretical study of the validity of quasi-stationary analysis of evaporation and condensation processes in small droplets and ice crystals.]Google Scholar
Power, B. A. Power, R. F. Vanillin, cis-terpin hydrate, and cis-terpin as ice nucleators. Science, Vol. 148, No. 3673, 1965, p. 1088. [These substances may be ice nuclei in the atmosphere.]Google Scholar
Teichmann, I. Schmidt, G. Untersuchungen über den reziproken Piezoeffekt des Eises. Physica Status Solidi, Vol. 8, No. 3, 1965, p. K14547. [Experiment yielding zero first order piezoelectric coefficient for ice. Second order effect measured.]Google Scholar
Todd, C. J. Ice crystal development in a seeded cumulus cloud. Journal of the Atmospheric Sciences, Vol. 22, No. 1, 1965, p. 7078. [Direct study of crystals collected in a cloud used to deduce details of nucleation and growth.]Google Scholar
Wakahama, G. Kōri no naibu-hakai ni tsuite . Teion-kagaku , Ser. A, Vol. 23, 1965, p. 3950. [Classification of various types of fracture in ice crystals and polycrystalline ice. English summary, p. 4849.]Google Scholar
Weissmann, M. Cohan, N. V. Molecular orbital study of the hydrogen bond in ice. Journal of Chemical Physics, Vol. 43, No. 1, 1965, p. 11923. [Theoretical calculation yielding values of bond energy and dipole moment in good agreement with experiment.]Google Scholar
Weissmann, M. Cohan, N. V. Molecular orbital study of ionic defects in ice. Journal of Chemical Physics, Vol. 43, No. 1, 1965, p. 12426. [Theoretical calculation of energy for diffusion of defects showing H3O+ to be more mobile.]Google Scholar
Whalley, E. Davidson, D. W. Entropy changes at the phase transitions in ice. Journal of Chemical Physics, Vol. 43, No. 6, 1965, p. 214849. [Discussion of slopes of lines in phase diagram of ice and implications in terms of ordering of structures and entropy.]Google Scholar
Wilson, G. J., and others. Dielectric properties of ices II, III, V, and VI, [by] G. J. Wilson, R. K. Chan, D. W. Davidson, and E. Whalley. Journal of Chemical Physics, Vol. 43, No. 7, 1965, p. 238491. [Measurements up to 300 kc./sec. and interpretation in terms of the structures.]Google Scholar

Land ice. Glaciers. Ice shelves

Bauer, A. Travaux du groupe de glaciologie de la IXe Expédition Antarctique Soviétique (été austral 1963–1964). La Houille Blanche, 1965, Nr. 5, p. 11524. [Condensed report of papers by Shumskiy and Bauer being published in Russian on variation of the ice cover of eastern Antarctica and of measurements made on a traverse.]Google Scholar
Bogorodskiy, V. V., and others. Elektromagnitnoye zondirovaniye antarkticheskogo lednika , [by] V. V. Bogorodskiy, V. N. Rudakov [and] V. A. Tyul’pin. Zhurnal Tekhnicheskoy Fiziki , Tom 35, Vyp. 6 1965, p. 115053. [Sounding between Mirny and “Pionerskaya” station gave a depth of 850 m. at a place of known depth of 900 m. English translation in Soviet Physics-Technical Physics, Vol. 10, No. 6, 1965, p. 886–88.]Google Scholar
Bullen, K. E. Goodspeed, M. J. Seismic investigations of Antarctic structure. Annals of the International Geophysical Year, Vol. 30, 1965, p. 21359. [Seismic measurements leading to the determination of the thickness of the ice cap, seismic ice velocities and some features of the structure below the ice.]Google Scholar
Debenham, F. The glacier tongues of McMurdo Sound. Geographical Journal, Vol. 131, Pt. 3, 1965, p. 36971. [Various problems arising from the earlier account by Wright and Priestley.]Google Scholar
Epstein, S., and others. Six-year record of oxygen and hydrogen isotope variations in South Pole firn, by S. Epstein, R. P. Sharp and A. J. Gow. Journal of Geophysical Research, Vol. 70, No. 8, 1965, p. 180914. [Stake, firn stratigraphy and isotope measurements compared.]Google Scholar
Giovinetto, M. B. Preliminary report on drainage systems of Antarctica. Polarforschung, Bd. 5, Jahrg. 34, Ht. 1–2, 1964 [pub. 1965], p. 24046. [Division of Antarctic Ice Sheet into drainage systems and estimate of individual mass balances.]Google Scholar
Gonfiantini, R. Some results on oxygen isotope stratigraphy in the deep drilling at King Baudouin station. Antarctica. Journal of Geophysical Research, Vol. 70, No. 8, 1965, p. 181519. [Accumulation deduced.]Google Scholar
Holdsworth, G. An examination and analysis of the formation of transverse crevasses, Kaskawulsh Glacier, Yukon Territory, Canada. Ohio State University. Institute of Polar Studies. Report No. 16, 1965, 91 p. [Observations to test Nye’s theory of the longitudinal strain rate on the surface of a valley glacier and Investigation of the mechanics and mode of formation of transverse crevasses.]Google Scholar
Lliboutry, L. How glaciers move. New Scientist, Vol. 28, No. 473, 1965, p. 73436. [Discussion on Glen’s, Nye’s, Weertman’s and the author’s theories.]Google Scholar
Loewe, F. Das grönländische Inlandeis nach neuen Feststellungen. Erdkunde, Bd. 18, Ht. 3, 1964, p. 189202. [Review of present knowledge of Greenland Ice Sheet. English summary.]Google Scholar
Lunde, T. On the firn temperatures and glacier flow in Dronning Maud Land. Norsk Polarinstitutt. Årbok, 1963 [pub. 1965], p. 724. (Den Norske Antarktisekspedisjonen, 1956–60. Scientific Results, No. 7.)Google Scholar
Mercer, J. H. Glacier variations in southern Patagonia. Geographical Review, Vol. 55, No. 3, 1965, p. 390413. [Results obtained in 1963 from the Upsala glacier and its vicinity.]CrossRefGoogle Scholar
Miller, M. M., and others. Tritium in Mt. Everest ice—annual glacier accumulation and climatology at great equatorial altitudes, [by] M. M. Miller, J. S. Leventhal and W. F. Libby. Journal of Geophysical Research, Vol. 70, No. 16, 1965, p. 388588. [Tritium used to verify semi-annual stratification on Khumbu Glacier and hence deduce accumulation of 1 7 m. water equivalent.]Google Scholar
Oechslin, M. Vaney, P. Mattmark.—La catastrophe de Mattmark. Les Alpes. Bulletin Mensuel du Club Alpin Suisse, 41e An., [No.] 10, 1965, p. 22226. [Avalanche of the Allalin Gletscher in August 1965.]Google Scholar
Pálmason, G. Gravity measurements in the Grimsvötn area. Jókull, ár 14, No. 3, 1964, p. 6166. [Gravity measurements and estimates of ice thickness on the Vatnajökull ice cap.]Google Scholar
Pillewizer, W. Bewegungsstudien an einem arktischen Gletscher. Polarforschung, Bd. 5, Jahrg. 34, Ht. 1–2, 1964 [pub. 1965], p. 24753. [Studies of block-flow by the calving of the Kongsvegen glacier in Vestspitsbergen.]Google Scholar
Post, A. S. Alaskan glaciers: recent observations in respect to the earthquake-advance theory. Science, Vol. 148, No. 3668, 1965, p. 36668. [Aerial studies show rockfalls but no significant snow and ice avalanches or catastrophic advances.]Google Scholar
Ragle, R. H., and others. Effects of the 1964 Alaskan earthquake on glaciers and related features, [by] R. H. Ragle, J. E. Sater and W. O. Field. Arctic, Vol. 18, No. 2, 1965, p. 13537.Google Scholar
Rüegg, W. La Cordillère Blanche du Pérou et la catastrophe du Huascaran. Les Alpes. Revue du Club Alpin Suisse, 38e An., 4e Trimestre, 1962, p. 27580. [Account of the formation of glacier-lagoons, of the rupture of the rock bastion and ice cap of the north Huascaran in 1962 and the resulting disastrous ice, snow and rock avalanche.]Google Scholar
Rundle, A. S. Glaciological investigations on Sukkertoppen ice cap, southwest Greenland, summer 1964. Ohio State University. Institute of Polar Studies. Report No. 14, 1965, 11 p. [Temperatures at depth indicate that much of the ice cap is temperate. Snow pit and core analysis show significant variation in accumulation.]Google Scholar
Savage, J. C. Paterson, W. S. B. Additional borehole measurements in the Athabasca Glacier. Journal of Geophysical Research, Vol. 70, No. 14, 1965, p. 351113. [Results for 1963 confirming results of previous years. Also lists errata and corrigenda for Paterson and Savage, ibid., Vol. 68, No. 15, 1963, p. 4537–43, and Savage and Paterson, ibid., Vol. 68, No. 15, 1963, p. 4521–36.]Google Scholar
Schytt, V. Notes on glaciological activities in Kebnekaise, Sweden, during 1964. Geografiska Annaler, Vol. 47A, No. 1, 1965, p. 6571. [Accumulation, ablation and mass balance of Storglaciaren during 1964. Variations of Swedish glaciers in 1964.]Google Scholar
Shumskiy, P. A. Yevteyev, S. A. O napravlenii sovremennykh izmeneniy antarkticheskogo lednikovogo pokrova . (In Antarktika. Doklady Komissii 1962 . Moscow, Izdatel’stvo Akademii Nauk SSSR [Publishing House of the Academy of Sciences of the U.S.S.R.], 1963, p. 6086.) [Discusses possible methods for determining recent changes and their causes.]Google Scholar
Shumskiy, P. A. Zotikov, I. A. O donnom tayanii shel’fovykh lednikov Antarktidy . (In Antarktika. Doklady Komissii 1962 . Moscow, lzdatel’stvo Akademii Nauk SSSR [Publishing House of the Academy of Sciences of the U.S.S.R.], 1963, p. 87108.) [Discussion of methods for determining bottom melting and deduction of mean rate.]Google Scholar
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Stenborg, T. Problems concerning winter run-off from glaciers. Geografiska Annaler, Vol. 47A, No. 3, 1965, p. 14184. [Factors which determine the run-off from glaciers during the winter and the general conditions for this run-off in different environments.]Google Scholar
Suetova, I. A. Morfometricheskiye kharakteristiki Antarktidy (ploshchadi, gipsograficheskaya krivaya poverkhnosti, srednyaya vysota i ob”yem) . (In Antarktika. Doklady Komissii 1962 . Moscow, Izdatel’stvo Akademii Nauk SSSR [Publishing House of the Academy of Sciences of the U.S.S.R.], 1963, p. 2834.)Google Scholar
Szupryczyński, J. Relief of the marginal zone of Werenskioldbreen. Norsk Polarinstitutt. Årbok, 1963 [pub. s 965], p. 89107. [Vestspitsbergen. Field work in 1960.]Google Scholar
Taylor, L. D. Glaciological studies on the South Pole traverse 1962–1963. Ohio State University. Institute of Polar Studies. Report No. 17, 1965, 25 p. [Detailed pit studies, accumulation, temperature, firn properties, etc., at 25 stations over a 1,448 km. traverse between the South Pole and the Queen Maud Range and Horlick Mountains.]Google Scholar
Thorarinsson, S. Sudden advance of the Vatnajökull outlet glaciers 1930–1964. Jökull Ar 14, No. 3, 1964, p. 7689. [Gives details, and a list, of nine glaciers affected by sudden advances from 1890 to 1964.]Google Scholar
Westphal, J. A. In situ acoustic attenuation measurements in glacial ice Journal of Geophysical Research, Vol. 70, No. 8, 1965, p. 184953. [Attenuation of acoustic waves measured in Blue Glacier. Mechanism discussed.]Google Scholar
Zorikov, I. A. Teplovoy rezhim lednika tsenural’noy Antarktidy . (In Antarktika. Doklady Komissii 1961 . Moscow, Izdatel’stvo Akademii Nauk SSSR [Publishing House of the Academy of Sciences of the U.S.S.R.], 1962, p. 2740.) [Theoretical model suggests melting occurs at bed in central Antarctic. Discussion of dispersal of melt water.]Google Scholar

Icebergs. Sea, River and Lake Ice.

Berdennikov, V. P. Dynamic conditions of formation of ice jams on rivers. Soviet Hydrology . Selected Papers, 1964, No. 2, p. 10108. [Discussion of factors involved and method of estimating breaking point of ice during ice jams.]Google Scholar
Bukina, L. A. O zavisimosti ot temperatury otnosheniya tolshchiny k diametru kristallov vnutrivodnogo l’da diskoobraznoy formy . lzvestiya Akademii, Nauk SSSR. Seriya Geofizicheskaya , 1963, No. 1, p. 18890. [English translation: Bulletin of the Academy of Sciences of the U.S.S.R. Geophysical Series, 1963, No. 1, p. 112–141Google Scholar
Campbell, W. J. The wind-driven circulation of ice and water in a Polar ocean. Journal of Geophysical Research, Vol. 70, No. 14, 1965, p. 3279301. [A steady-state theory for the circulation of a wind-driven, baroclinic, ice-covered ocean is presented.]CrossRefGoogle Scholar
Chapman, R. P. Scott, H. D. Backscattering strength of young sea ice. Journal of the Acoustical Society of America, Vol. 36, No. 12, 1964, p. 241718. [Letter. Measurements of acoustic scattering.]Google Scholar
Clarke, P. C. Lamb, H. H. Arctic pack-ice. Weather, Vol. 20, No. 11, 1965, p. 35960. [Letter on the usual extent of sea ice in the Greenland-Iceland area, and a reply by H. H. Lamb.]Google Scholar
Henry, W. K. The ice jam floods of the Yukon River. Weatherwise, Vol. 18, No. 2, 1965, p. 8185. [General description of formation of ice jams and resulting floods.]Google Scholar
Hoare, R. A., and others. Solar heating of Lake Fryxell, a permanently ice-covered Antarctic lake, by R. A. Hoare, K. B. Popplewell, D. A. House, R. A. Henderson, W. M. Prebble and A. T. Wilson. Journal of Geophysical Research, Vol. 70, No. 6, 1965, p. 155558. [Study shows solar energy to be only possible source keeping lake unfrozen.]CrossRefGoogle Scholar
Kumagori, T., and others. Kaiyō-Maru ni yoru pakkuaisu oyobi hyōzan no kansoku , [by] T. Kumagori, S. Yanagawa, T. Isouchi, I. Kotake [and] K. Matsuike. Antarctic Record (Tokyo), No 19, 1963, p. 8590. [Observations from ship in Indian and South Atlantic Oceans. English summary.]Google Scholar
Luosto, U. Saastamoinen, P. Observations about ice-shocks on Lake Sääksjärvi. Geophysica, Vol. 9, No. 1, 1964, p. 8792. [Amplitude of acoustic waves and dependence of frequency on conditions.]Google Scholar
Needham, H. D. Ice-rafted rocks from the Atlantic Ocean off the coast of the Cape of Good Hope. Deep Sea Research, Vol. 9, Nov.-Dec. 1962, p. 47586. [Observation of “erratics” trawled from sea and discussion of their origin.]Google Scholar
Nezhikhovskiy, R. A. Coefficients of roughness of bottom surface of slush-ice cover. Soviet Hydrology. Selected Papers, 1964, No. 2, p. 12750. [Review of existing formulae.]Google Scholar
Ragotzkie, R. A. Friedman, I. Low deuterium content of Lake Vanda, Antarctica. Science, Vol. 148, No. 3674, 1965, p. 122627. [Measurements confirm theories about formation of this ice-covered lake.]CrossRefGoogle ScholarPubMed
Richards, T. L. The meteorological aspects of ice cover on the Great Lakes. Monthly Weather Review, Vol. 92, No. 6, 1964, p. 297302. [Discussion of observations of formation and break-up.]Google Scholar
Rymsha, V. A. Donchenko, R. V. Characteristics of the conditions of the formation and development of ice during rapid freezing of rivers and reservoirs. Soviet Hydrology. Selected Papers, 1964, No. 2, p. 11726.Google Scholar
Shaw, J. B. Growth and decay of lake ice in the vicinity of Schefferville (Knob Lake), Quebec. Arctic, Vol. 18, No. 2, 1965, p. 12332. [Detailed account showing thickness of ice and snow, and dates of break-up of ice.]Google Scholar
Shirtcliffe, T. G. L. Lake Bonney, Antarctica: cause of the elevated temperatures. Journal of Geophysical Research, Vol. 69, No. 24, 1964, p. 525768. [Explanation of high temperature of this ice-covered lake in terms of past history of water inflow.]Google Scholar
Tsuri]kov, V. L. Analiz narastaniya morskogo l’da pod snezhnym pokrovom . Okeanologiya , Tom 3, Vyp. 3, 1963, p. 45969. [Comparison of various theories.]Google Scholar
Untersteiner, N. Badgley, F. I. The roughness parameters of sea ice. Journal of Geophysical Research, Vol. 70, No. 18, 1965, p. 457377. [Observations of velocity profiles of wind and water show the roughness length of Arctic sea ice to vary greatly.]CrossRefGoogle Scholar

Glacial geology

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Bloch, M. R. Die Beeinflussung der Albedo von Eisflächen durch Staub und Ihre Wirkung auf Ozeanhöhe and Klima. Geologische Rundschau, Bd. 54, 1964, p. 51522. [Albedo changes through the dusting of ice sheets are proposed as cause for glacial periods.]Google Scholar
Dahl, R. Plastically sculptured detail forms on rock surfaces in northern Nordland, Norway. Geografiska Annaler, Vol. 47A, No. 2, 1965, p. 83140. [The deviations of the sculptured forms are mainly due to deviated ice flow.]Google Scholar
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Donn, W. L., and others. Pollen from Alaska and the origin of ice ages, by W. L. Donn, M. Ewing and P. Colinvaux. Science, Vol. 147, No. 3658, 1965, p. 63233. [Reply by Donn and Ewing to criticism by Colinvaux, ibid., Vol. 145, No. 3633, 1 p. 707–08, of their ice-age theory with further reply by Colinvaux.]CrossRefGoogle Scholar
Dort, W. jr. Nearby and distant origins of glacier ice entering Kansas. American Journal of Science, Vol. 263, No. 7, 1965, p. 598605. [Stratigraphy in Kansas provides field evidence in support of Flint’s concept of ice sheet expansion processes.]Google Scholar
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Fulton, R. J. Silt deposition in late-glacial lakes of southern British Columbia. American Journal of Science, Vol. 263, No. 7, 1965, p. 55370. [Silt deposited in glacial lakes; varves are thick in lower parts of the deposit, grading thinner upward; much of the silt was derived from melt-water erosion of till and maximum deposition occurred as the ice receded from adjacent uplands.]Google Scholar
Gjessing, J. On ‘plastic scouring’ and ‘subglacial erosion’. Norsk Geografisk Tidsskrift, Bd. 20, Ht. 1–2, 1965–66, [pub.] 1965, p. 137. [Detailed account with good photographs of striae, roches moutonnées and sundry glacial erosion forms.]Google Scholar
Hollin, J. T. Wilson’s theory of ice ages. Nature, Vol. 208, No. 5005, 1965, p. 1216. [Comments on theory by A. T. Wilson, ibid., Vol. 201, No. 4915, 1964, p. 147–49.]Google Scholar
Jones, O. T. The glacial and post-glacial history of the lower Teifi valley. Quarterly Journal of the Geological Society of London, Vol. 121, Pt. 2, No. 482, 1965, p. 24781. [Because the coast-line of Cardigan Bay (Wales) was under ice, a great volume of melt water from the ice surface entered the Teifi Valley and caused rapid erosion of the gorges there. Distribution of deposits formed during the glacial period and the subsequent system of lakes are described.]Google Scholar
Koaze, T. Shōwakichi firkin, rogan chiiki no chikei . Antarctic Record (Tokyo), No. 20, 1964, p. 6174. [Glacial geomorphology and moraine evidence of retreat of ice sheet.]Google Scholar
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Martin, S. W. Glacial lakes in the Bolivian Andes. Geographical Journal, Vol. 131, Pt. 4, 1965, p. 51926. [General account.]Google Scholar
Messerli, B. Erciyas Dagh 3916 m (Türkei). Die eiszeitliche Vergletscherung eines Vulkans. Les Alpes. Revue du Club Alpin Suisse, 41e An., 2e Trimestre, 1965, p. 12232. [Present and former glacicrization of this Turkish mountain during Würm and Riss glaciations.]Google Scholar
Mitchell, G. F. The Quaternary deposits of the Ballaugh and Kirkmichael districts, Isle of Man. Quarterly Journal of the Geological Society of London, Vol. 121, Pt. 3, No. 483, 1965, p. 35981. [Last glaciation ice advanced against the Isle of Man from the north depositing large amounts of drift. At the end of the late-glacial time sands and gravels were set free burying these deposits to a depth of 12 m.]Google Scholar
Niewiarowski, W. Kemy i formy pokrewne w Danii oraz Rozmieszycyenie Obszarów kemowych na terenie Peribalticum w obrçbie ostatniego zlodowacenia. Zeszyty Naukowe Uniwersytetu Mikolaja Kopernika w Toruniu, Zeszyt 11, Geografia 4, 1965, p. 3157. [Kames and related land-forms in Denmark; distribution of kame landscapes neighbouring the Baltic, within the area of last glaciation. English translation of summary, p. 109–16.]Google Scholar
Peterson, J. A. Ice-push ramparts in the George River basin, Labrador-Ungava. Arctic, Vol. 18, No. 3, 1965, p. 18993.Google Scholar
Seret, G. La succession des épisodes fluviatiles périglaciaires et fluvioglaciaires à l’aval des glaciers. Zeitschr ft flit Geomorphologie, Neue Folge, Bd. 9, Ht. 3,1965, p. 30520. [In each of three cases at the time of advancing and maximum glacierization there was a fluviatile periglacial deposit. Only with higher temperatures was the fluvio-glacial phase apparent.]Google Scholar
Strömberg, B. Mappings and geochronological investigations in some moraine areas of south-central Sweden. Geografiska Annaler, Vol. 47A, No. 2, 1965, p. 7382. [In these areas no evidence has been obtained for an interpretation of moraines lying at right angles to the last direction of ice movement as “annual moraines”.]Google Scholar
Theakstone, W. H. Contorted glacial lake sediments, and ice blocks in outwash deposits at Østerdalsisen, Norway. Geografiska Annaler, Vol. 47A, No. 1, 1965, p. 3944. [General account, including drainage conditions, nature of deposits and origin of structures.]CrossRefGoogle Scholar
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Thorarinsson, S. On the age of the terminal moraines of Brúarjökull and Hálsajökull., Jökull, Ár 14, No. 3, 1964, p. 6776. [A tephrochronological study.]Google Scholar
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Wundt, W. Die Bedeutung der Strahlungskurve nach den Anschauungen von Bacsák im Zusammenhang mit den Untersuchungen von Milankovitch und Woerkom. Geologische Rundschau, Bd. 54, 1964, p. 47886. [Re-analysis of the correlation between solar radiation curves and ice ages.]Google Scholar

Frost action on Rocks and Soil. Frozen Ground. Permafrost

Annersten, L. J. Background for the Knob Lake permafrost studies. (In Bird, J. B., ed. Permafrost studies in central Labrador-Ungava. McGill Sub-Arctic Research Papers, No. 16, 1964, p. 132.) [Principles involved and description of environments at Knob Lake.]Google Scholar
Annersten, L. J. Investigations of permafrost in the vicinity of Knob Lake 1961–62. (In Bird J. B., ed. Permafrost studies in central Labrador-Ungava. McGill Sub-Arc& Research Papers, No. 16, 1964, p. 51137.) [Effect of soil surface covers on soil temperature.]Google Scholar
Bibikova, E. S. On the utilization of the data of the nalyed (interstitial or subsurface ice) cadaster in the analyses of flow of some rivers of the northeastern USSR. Soviet Hydrology. Selected Papers, 1964, No. 2, p. 15055. [Estimate of total water contents of naleds in north-east U.S.S.R.]Google Scholar
Bonnlander, B. Major-Marothy, G. M. Permafrost and ground temperature observations, 1957. (In Bird J. B., ed. Permafrost studies in central Labrador-Ungava. McGill Sub-Arctic Research Papers, No. 16, 1964, p. 3355.) [Results.]Google Scholar
Brown, R. J. E., ed. Proceedings of the first Canadian conference on permafrost, 17 and 18 April 1962. Canada. National Research Council. Associate Committee on Soil and Snow Mechanics. Technical Memorandum No. 76, 1963, 231 p. [Report of conference with 13 out of 19 papers reproduced.]Google Scholar
Hard, G. Noch einmal: “Erdkegel”. Einige Ergänzungen zu den Beobachtungen von G. Selzer (1959). Eiszeitalter und Gegenwart, Bd. 15, 1965, p. 10207. [Special distribution, shape and vegetation cover of earth-cones, and conditions under which they are formed.]Google Scholar
Mazurov, G. P. Tikhonova, E. S. Preobrazovaniye sostava i svoystv gruntov pri mnogokratnom zamorazhivanii . Vestnik Leningradskogo Universiteta , Tom 18, Vyp. 3, 1964, p. 3544. [Observations on disintegration and sorting in sands but not clays. English summary.]Google Scholar
Ohlson, B. Frostaktivität, Verwitterung und Bodenbildung in den Fjeldgegenden von Enontekiö, Finnisch-Lappland. Fennia, 89, No. 3, 1964, 182 p. [Study of frost action on rocks and soils in Enontekiö region, Finnish Lapland.]Google Scholar
Packer, R. W. Stability slopes in an area of glacial deposition. Canadian Geographer, Vol. 8, No. 3, 1964, p. 14751. [Study of processes producing change in deglaciated areas of southern Ontario.]Google Scholar
Ugolini, F. C. Bull, C. Soil development and glacial events in Antarctica. Quaternaria (Rome), 7, 1965, p. 25169. [Variation in the ice cover, glacier action and soil formation, and Antarctic soils.]Google Scholar

Meteorological and Climatological Glaciology

Bugayev, V. A. Zakiyev, Kh. Ya. Tsirkulyatsiya atmosfery i zastrugi v Vostochnoy Antarktide . (In Antarktika. Doklady Komissii 1962 . Moscow, Izdatel’stvo Akademii Nauk SSSR [Publishing House of the Academy of Sciences of the U.S.S.R.], 1963, p. 13037.) [Use of sastrugi to determine patterns of atmospheric circulation.]Google Scholar
Goyer, G. G. Effects of lightning on hydrometcors. Nature, Vol. 206, No. 4990, 1965, p. 120309. [Effect on hailstones, supercooled droplets, cloud droplets and ice crystals discussed.]Google Scholar
Hallett, J. Rime or not rime? Weather, Vol. 20, No. 8, 1965, p. 260. [The rime often seen on the crystalline branches of hoar frost crystals shows that rime formation is often associated with hoar frost.]Google Scholar
Havens, J. M. Weather note: a November rain on the Greenland inland ice. Meteorological Magazine, Vol. 93, No. 1105, 1964, p. 22831. [Observations in 1963 at lat. 66° 29′ N., long. 46° 22′ W.]Google Scholar
Lied, N. T. Stationary hydraulic jumps in a katabatic flow near Davis, Antarctica, 1961. Australian Meteorological Magazine, No. 47, 1964, p. 4051. [The most spectacular aspects of katabatic winds are the “standing jump” on the coastal slopes of the ice sheet, which take the form of a wall of drift snow 30–100 m. high.]Google Scholar
Macklin, W. C. Factors affecting the heat transfer from hailstones. Quarterly Journal of the Royal Meteorological Society, Vol. 90, No. 383, 1964, p. 8490.Google Scholar
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Snow

Businger, J. A. Eddy diffusion and settling speed in blown snow. Journal of Geophysical Research, Vol. 70, No. 14, 1965, p. 330713. [Theoretical analysis to explain the large eddy diffusivity for blowing snow.]Google Scholar
Gayvoronskiy, I. I., and others. K voprosu o temperaturnykh granitsakh primenimosti metoda iskusstvennykh vozdeystviy s pomoshch’yu tverdoy uglekisloty , [by] I.I. Gayvoronskiy, L. I. Krasnovskaya, Yu. A. Scregin [and] N. V. Smirnova. Trudy Tsentral’noy Aerologicheskoy Observatorii , No. 51, 1963, p. 1419.Google Scholar
Herman, J. R. Precipitation static and electrical properties of blowing snow at Byrd Station, Antarctica. (In Waynick, A. H., ed. Geomagnetism and aeronomy. Washington, D.C., American Geophysical Union, 1965, p. 22136. (Antarctic Research Series, Vol. 4.) (National Research Council Publication No. 1275.)) [Study of radio noise. Deductions about charge carried by blizzard particles.]Google Scholar
Hobbs, P. V. The effect of time on the physical properties of deposited snow. Journal of Geophysical Research, Vol. 70, No. 16, 1965, p. 390307. [Explanation, in terms of growth of ice necks between particles, of changes in various mechanical properties of snow.]Google Scholar
Latham, J. The electrification of snowstorms and sandstorms. Quarterly Journal of the Royal Meteorological Society, Vol. 90, No. 383, 1964, p. 9195. [Analysis of observations and explanation in terms of charge transfer due to temperature gradients.]Google Scholar
Latham, J. “Elektrische” Schneestürme. Umschau, Bd. 65, Ht. 1, 1965, p. 28. [Summary of literature on electrification of snowstorms and its origin.Google Scholar
Sommerfeld, R. Businger, J. A. The density profile of blown snow. Journal of Geophysical Research, Vol. 70, No. 14, 1965, p. 330306. [Optical technique for measuring the density of snow suspended in air. Results indicate eddy diffusivity for snow is much larger than eddy viscosity of wind profile.]Google Scholar
Wakahama, G. Mizu o fukunda sekisetsu no hentai . Teion-kagaku , Ser. A, Vol. 23, 1965, p. 5166. [Four series of experiments, using: (1) dry compact snow at 0°C.; (2) wet compact snow; (3) compact snow immersed in water at 0°C.; (4.) compact snow immersed in water at 0°C. and loaded with a weight. English summary, p. 64–65.]Google Scholar
Wilson, A. T. House, D. A. Chemical composition of south polar snow. Journal of Geophysical Research, Vol. 70, No. 22, 1965, p. 551518.Google Scholar
Wilson, A. T. House, D. A. Fixation of nitrogen by aurora and its contribution to the nitrogen balance of the Earth. Nature, Vol. 205, No. 4973, 1965, p. 79394. [Chemical analysis of South Polar snow shows 0.005 p.p.m. N as NO3 - and NO2 - believed to be of geophysical origin.]Google Scholar
Woodward, R. N. Strontium-90 and cw.sium-137 in Antarctic snows. Nature, Vol. 204, No. 4965, 1964, p. 1291. [Measurements of Sr show main influx of fission products in 1955. Cs results are more variable.]Google Scholar
Yen, Yin-Chao. Effective thermal conductivity and water vapor diffusivity of naturally compacted snow. Journal of Geophysical Research, Vol. 70, No. 8, 1965, p. 182125. [Experimental study of influence of air flow.]Google Scholar
Yosida, Z. Yūsetsusui no sekisetsunai shintō . Teion-kagaku , Ser. A, Vol. 23, 1965, p. 116. [Theoretical analysis of the ability of water to penetrate through snow cover. English abstract.]Google Scholar