Bauer, A. Travaux du groupe de glaciologie de la IX^e Expédition Antarctique Soviétique (été austral 1963–64). TAAF (Territoire des Terres Australes et Antarctiques Françaises), No. 32, 1965 p. 46–62. [Report of work of French and Soviet party on traverse in Antarctica. Reports density, snow stratigraphy and temperature and first measurement of strain pentagons.]Google Scholar

Miller, M. M. Mount Everest and the Mahalangur Himal 1963. Explorers Journal, Vol. 43, No. 3, 1965, p. 130–48. [General results including glaciology, geomorphology and climatic change]Google Scholar

Shipilov, F. D. Ledyanyye tsvety . Priroda , 1965, No. 2, p. 127–28. [Study of ice formations on ground or water and conditions for their occurrence.]Google Scholar

White, A. Arctic Norway expedition 1964. Gicce Cokka ice-cap. Exploration Review, No. 6, 1965, p. 14–15, 20. [Imperial College, London.]Google Scholar

Philberth, K. Sur la stabilisation de la course d’une sonde thermique. Comptes Rendus Hebdomadaires des Séances de l’Académie des Sciences (Paris), Sér. B, Tom. 262, No. 6, 1966, p. 456–59. [Discusses tendency of some thermal boring probes to turn towards horizontal and methods of avoiding this.]Google Scholar

Stevens, P. R. Williams, J. D. H. Soil studies in the Antarctic. Antarctic (Wellington), Vol. 4, No. 3, 1965, p. 120. [Studies on morainic samples. Possible use as age indicator.]Google Scholar

Von Brunn, V. Ice crystal photography—Norway Station, 1960. Antarktiese Bulletin (Pretoria), No. 12, 1965, p. 3–4. [Technique for photographing snow crystals.]Google Scholar

Adamson, A. W. Dormant, L. M. Adsorption of nitrogen on ice at 78°K. Journal of the American Chemical Society, Vol. 88, No. 9, 1966, p. 2055–57. [Data suggest non-polar ice surface. Annealing attributed to surface migration.]Google Scholar

Agarwal, V. K. Gilra, N. K. Crystal density in supercooled radiation detector. Nuclear Instruments and Methods, Vol. 40, No. 2, 1966, p. 238–40. [Calculation of density of ice nuclei formed in supercooled water by passage of high energy charged particle. Possible use as particle detector.]CrossRefGoogle Scholar

Antonov, A. V., and others. Temperaturnaya zavisimost’ diffuzionnykh parametrov neytronov v vode i vo l’du . Atamnaya Energiya , Tom 20, Vyp. 2, 1966, p. 164–65. [Letter. Discussion of reasons why theory does not fit experiments.]Google Scholar

Bullemer, B. Riehl, N. Bulk and surface conductivity of ice. Solid State Communications, Vol. 4, No. 9, 1966 p. 447–48. [Activation energy for surface currents in ice is much larger than that for bulk conductivity.]Google Scholar

Bullemer, B. Riehl, N. Hall-effect on protons in ice. Physics Letters, Vol. 22, No. 4, 1966, p. 411–12. [Measurement confirms positive sign of charge carriers and gives value for mobility and lifetime.]Google Scholar

Camp, P. R. Creamer, J. Rate of growth of ice at water-metal interfaces. Journal of Chemical Physics, Vol. 45, No. 7, 1966, p. 2709–10. [Letter. Measurement for various different substrates and modes of crystal orientation.]Google Scholar

De Achaval, E. M., and others. Chemical etching in ice crystals, by E. M. De Achaval, L. Levi and E. Saraski. Physica Status Solidi, Vol. 5, No. 2, 1964, p. K61–K63. [Study of etch pits and effect of stress.]Google Scholar

Delibaltas, P., and others. Diffusion von ¹⁸o in Eis-Einkristallen, [von] P. Delibaltas, O. Dengel, D. Heimreich, N. Riehl und H. Simon. Physik der kondensierten Materie, Bd. 5, Ht. 3, 1966, p. 166–70. [Measurement of diffusion coefficient of ¹⁸O in ice single crystals gives result that shows diffusion is by whole H₂O molecules. Vacancy mechanism suggested.]Google Scholar

De Micheli, S. M. De Lubart, L. Thermal etching of ice in vacuum. Physica Status Solidi, Vol. 5, No. 2, 1964, p. K57–K59. [Experimental study on various faces of ice single crystals.]Google Scholar

Dengel, O., and others. Diffusion von Tritonen in NH₄F-dotierten Eis-Einkristallen, [von] O. Dengel, E. Jacobs und N. Riehl. Physik der kondensierten Materie, Bd. 5, Ht. 1, 1966, p. 58–59. [Diffusion of tritons in NH₄F-doped ice found to be independent of doping.]Google Scholar

Dengel, O., and others. Messungen der Dielektrizitätskonstanten von reinem und NH₄F-dotiertem Eis, [von] O. Dengel, N. Riehl und A. Schleippmann. Physik der kondensierten Materie, Bd. 5, Ht. 2, 1966, p. 83–88. [Measurement of dielectric constant of pure and NH₄F doped ice as a function of frequency.]Google Scholar

Engelhardt, H. Riehl, N. Zur protonischen Leitfähigkeit von Eis-Einkristallen bei tiefen temperaturen und hohen Feldstärken. Physik der kondensierten Materie, Bd. 5, Ht. 2, 1966, p. 73–82. [Current-voltage characteristics of ice single crystals under high electric fields used to determine number and depth of proton traps and temperature dependence of proton mobility.]Google Scholar

Fukuta, N. Experimental studies of organic ice nuclei. Journal of the Atmospheric Sciences, Vol. 23, No. 2, 1966, p. 191–96 [329 compounds investigated.]Google Scholar

Gold, L. W. Dependence of crack formation on crystallographic orientation for ice. Canadian Journal of Physics. Vol. 44, No. 11, 1966, p. 2757–66. [Observations of both transcrystalline and grain-boundary cracks in columnar-grained ice compressed perpendicular to the columnar axis.]Google Scholar

Goyer, G. G., and others. Shock induced freezing of supercooled water, by G. G. Goyer, T. C. Bhadra and S. Gitlin. Journal of Applied Meteorology, Vol. 4, No. 1, 1965, p. 156–60. [Experimental study.]2.0.CO;2>CrossRefGoogle Scholar

Harrison, J. D. Tiller, W. A. Ice interface morphology and texture developed during freezing. Journal of Applied Physics, Vol. 34, No. 11, 1963, p 3349–55 [Study of formation cells during freezing of solutions. Textures formed are similar to those for pure water, but cause is different.]Google Scholar

Hayward, A. T. J. Growth of ice tubes. Nature, Vol. 211, No. 5045, 1966 p 172–73 [Letter. Water under vacuum with no air nuclei for boiling can be simultaneously supercooled and superheated. When such water freezes tubes of ice are frequently ejected from surface. Their mode of growth is reported. A film of the phenomenon is available on loan.]Google Scholar

Higuchi, K. Fukuta, N. Ice in the capillaries of solid particles and its effect on their nucleating ability. Journal of the Atmospheric Sciences, Vol. 23, No. 2, 1966, p. 187–90. [Pre-cooling on nuclei between –35° to –78°C. made them much more effective nuclei when at –2° to –3°C.]Google Scholar

Hobbs, M. E. , and others. The dielectric constant of liquid water and various forms of ice according to significant structure theory, by M. E. Hobbs, M. S. Jhon and H. Eyring. Proceedings of the. National Academy of Sciences of the United Slates of America, Vol. 56, No. 1, 1966, p. 31–38. [Discussion based on modified version of Onsager’s model.]Google Scholar

Ida, M. Kawada, S. Dielectric dispersion of KOH-doped ice at low temperatures. Journal of the Physical Society of Japan, Vol. 21, No. 3, 1966, p. 561. [Evidence for KOH molecules substituting for H₂O molecules in the ice structure.]Google Scholar

Isaka, H. Soulage, G. Étude expérimentale de l’action glaçogène de l’iodure d’argent à la sous-saturation par rapport à l’eau. Comptes Rendus Hebdomadaires des Séances de l’Académie des Sciences (Paris), Sér. B., Tom. 262, No. 2, 1966, p. 1405–08. (Decrease in number of active nuclei and increase in size when humidity goes unsaturated with respect to water.]Google Scholar

Jaccard, C. Solute segregation at the curved surface of a growing crystal (steady slate). Physik der kondensierten Materie, Bd. 4, Ht. 5, 1966, p. 349–54 [Explanation of why impurities concentrate near outside of cylindrical crystal.]Google Scholar

Joss, J. Die Bestimmung der Rückstreuquerschnilte von Eis-Wasser-Gemischen bei einer Wellenlänge von 5,05 cm. Zeitschrift für angewandte Mathematik and Physik, Vol. 15, Fasc. 5, 1964, p. 509–39. [Laboratory tests on radar reflexion from ice-water mixtures. Possible use to distinguish hail from rain.]Google Scholar

Kaiser, G. Die Schmelzkeimbildung in Eis unter erhöhtem Druck. Berichte der Bunsengesellschofl für physikalische Chemie, Bd. 70, Nr. 6, 1966, p. 635–39. [Observations of size of melt figures formed in ice thermodynamically superheated by pressure, and deduction that their nucleation is at defects.]Google Scholar

Keegan, H. J. Weidner, V. R. Infrared spectral reflectance of frost. Journal of the optical Society of America, Vol. 56, No. 4, 1966, p. 523–24 (Letter. Measurement from 4000 to 450 cm.^–1.]CrossRefGoogle Scholar

Latham, J. Stow, C. D. The mechanism of charge transfer associated wills evaporation of ice. Journal of the Atmospheric Sciences, Vol. 23, No. 2, 1966, p. 245–47 [Experimental data already reported are shown to be inconsistent with Mason’s theory that individual charged molecules are evaporated.]Google Scholar

Lobodin, T. V. O. prichinakh elektrizatsii snezhnykh kristallov vo vremya meteley . Antarktika. Doklady komissii 1964 g. . Moscow, Izdatel’stvo Akademii Nauk SSSR [Publishing House of the Academy of Sciences of the U.S.S.R.], 1965, p. 110–15.Google Scholar

Nagle, J. F. Lattice statistics of hydrogen bonded crystals. I. The residual entropy of ice.—II. The Slater KDP model and the Rys F-model. Journal of Mathematical Physics, Vol. 7, No. 8, 1966, p. 1484–91; No. 8, 1966, p. 1492–96; [I: calculation of residual entropy giving better agreement with experiment than Pauling’s approximation. II: calculation of thermal properties of an ice-type lattice which shows proton ordering at low temperatures.]Google Scholar

Natori, M. Watanabe, T. Structural model of the hydrated electron. Journal of the Physical Society of Japan, Vol. 21, No. 8, 1966, p. 1573–78 [Calculation of energy levels of a trapped electron by itself or associated with a vacancy in ice.]Google Scholar

Niven, C. D. The magic surface. A discussion on the remarkable sliding quality of ice. New York, Pageant Press, 1963. 74 p [Popular discussion of ice friction and its explanation.]Google Scholar

Runnels, L. K. Ice. Scientific American, Vol. 215, No. 6, 1966, p. 118–24, 126. [Popular account of present knowledge on the crystal structure of ice and of point defects in ice.]Google Scholar

Rush, J. J., and others. Motions of water molecules in potassium ferroeyanide trihydrate, water, and ice: a neutron scattering study, [by] J. J. Rush and P. S. Leung and T. I. Taylor. Journal of Chemical Physics, Vol. 45, No. 4, 1966, p. 1352–17. [Measurement of inelastic scattering spectra; comparison with N.M.R. and infrared results.]Google Scholar

Suzuki, Y. Disorder entropy of ice. Contributions from the Inslilute of Low Temperature Science (Sapporo), Ser. A, No. 21, 1966, p. 1–44. [Calculation of the entropy of finite ice crystal due to random arrangement of hydrogen atoms.]Google Scholar

Tao, S. J. Green, J. H. Positron annihilation in materials under ionizing radiation. Journal of Chemical Physics, Vol. 44, No. 10, 1966, p. 4007–09. [Study of effect of irradiation on positron annihilation rates in water and ice. In ice at 77°K. free radicals frozen in the lattice are important.]Google Scholar

Ukhov, S. B. Staticheskiy metod issledovaniya uprugo-elasticheskikh deformatsiy l’da . Merzlotnyye Issledovaniya. Sbornik Stacey , No. 3, 1963, p. 354–61. [Use of bending tests to determine elastic modulus of ice.]Google Scholar

Vonnegut, B. Orientation of ice crystals in the electric field of a thunderstorm. Weather, Vol. 20, No. 10, 1965, p. 310–12. [Laboratory study of orientation of ice crystals by electric field.]Google Scholar

Whipple, H. E., ed. Forms of water in biologic systems. Annals of the New York Academy of Sciences, Vol. 125, 1965, 772 p. [Includes the following papers: P. R. Camp, “The formation of ice at water-solid interfaces”, p. 317–43; F. Heinmets, “The effect of various biologic compounds on proton conductivity and activation energy in ice”, p. 355–64; G. W. Gross, “Ion incorporation and activation energies of conduction in ice”, p. 380–89; C. Jaccard, “Mechanism of the electrical conductivity in ice”, p. 390–400; B. J. Luyet, “Phase transitions encountered in the rapid freezing of aqueous solutions”, p. 502–21; M. D. Persidsky and R. Victor, “New approaches in measuring the linear rate of ice crystallization in water and aqueous solutions”, p. 677–88.]Google Scholar

Adams, W. P. Glaciology, No. 1. Ablation and run-off on the White Glacier, Axel Heiberg Island, Canadian Arctic Archipelago. Axel Heiberg Island Research Reports, McGill University, Montreal. Jacobsen-McGill Arctic Research Expedition 1959–1962, 1966, [iii], v, 77 p. [Detailed study over two seasons which adds considerably to the quantitative knowledge of the melt process on High Arctic glaciers.]Google Scholar

Avsyuk, G. A. Obshchaya programma mezhdunarodnykh postoyannykh nablyudeniy za kolebaniyami sovremennykh lednikov . Trudy Zakavkazskogo Nauchno-Issledovatel’skogo Cidrometeorologicheskogo Instituta (Tiflis), Vyp. 13, 1963, p. 10–7. [Reports the Soviet part in the international programme.]Google Scholar

Bardin, V. I. Suyetova, I. A. Perimetr Antarktidy i byudzhet Antarkticheskogo lednikovogo pokrova . Antarktika. Doklady Kornissii 1964 g. . Moscow, Izdatel’stvo Akademii Nauk SSSR [Publishing House of the Academy of Sciences of the U.S.S.R.], 1965, p. 67–75. [Dimensions of continent and its ice cover.]Google Scholar

Baussart, M., and others. Étude photogrammetrique des glaciers du massif du Mont Blanc, par M. Baussart, M. Carbonnell et C. Cazabat. Annales de Géophysique, Vol. 21, No. 3, 1965, p. 450–61. [Discusses methods used in photogrammetric surveys of Mt. Blanc glaciers, and results obtained including movement and mass balance.]Google Scholar

Bellair, P. Un exemple de glaciation aberrante: les Îles Kerguelen. CNFRA . Bulletin d’Information, No 11, 1965, p. 1–27. [Review of knowledge of Quaternary, and especially the glacial deposits of the Courbet peninsula, Kerguelen.]Google Scholar

Bentley, C. R. Giovinetto, M. B. Studies in surface glaciology. Antarctic Journal of the U.S., Vol. 1, No. 5, 1966, p. 209. [An analysis is in progress of annual snow accumulation in Antarctica where annual snow layers have been dated back 15 years or more.]Google Scholar

Beschel, R. E. Egan, C. P. Geobotanical investigation of a 16th-century moraine on the Bucher Glacier, Juneau Icefield, Alaska. Proceedings of the 16th Alaskan Science Conference, College, Alaska, August 29-September 1, 1965, 1966, p. 114–15. [Date of formation of this moraine is considered to be near or slightly prior to A.D. 1600.]Google Scholar

Brecher, H. H. Surface velocity measurements on the Kaskawulsh Glacier, Yukon Territory, Canada. Ohio State University. Institute of Polar Studies. Report No. 21, 1966, ix, 73 p. [In this accumulation area there are no significant differences from mean seasonal velocities over the short time intervals.]Google Scholar

Brockamp, B. Das grönländische Inlandeis. Erdkunde, Bd. 20, Ht. 3, 1966, p. 208–11. [Comments on F. Loewe’s article in Erdkunde, Bd. 18, Ht. 3.]Google Scholar

Budd, W. F. Glaciological studies in the region of Wilkes, Eastern Antarctica, 1961. ANARE Scientific Reports, Ser. A (IV), Publication No. 88, 1966, 152 p. [Work started by U.S. glaciologists 1957–58 continued by Australian scientists. Accumulation, wind speed and snow drift, ice temperatures, snow compaction, surface strain-rate and mass budget studies.]Google Scholar

Bugh, J. E. Glacio-hydrological studies on the Lemon Creek Glacier near Juneau, Alaska. Proceedings of the 16th Alaskan Science Conference, College, Alaska, August 29–September 1, 1965, 1966, p. 112–13. [Glacier has been gradually diminishing in size over the past four decades. Present observations suggest that this trend is reversing itself.]Google Scholar

Colqui, B. S. Comparative earthquake-glacier observations in the southern Andes and Alaska. Proceedings of the 16th Alaskan Science Conference, College, Alaska, August 29-September 1, 1965, 1966, p. 116–17. [The peculiar conditions on the Agua Negra glacier, Argentina, are believed to represent conditions which may eventually be found on some Alaskan glaciers following the major earth tremors of 27 March 1964.]Google Scholar

Egan, C. P. Regime trends on the Juneau Icefield névé. Proceedings of the 16th Alaskan Science Conference, College, Alaska, August 29–September 1, 1965, 1966, p. 109–10. [Brief report.]Google Scholar

Gloss, G., and others. Photograrnmetric and glacier movement surveys in the Taku district, Alaska, by G. Gloss, G. Konecny, A. Chrzanowski, A. A1-Naqash, and M. M. Miller. Proceedings of the 16th Alaskan Science Conference, College, Alaska, August 29–September 1 1965, 1966, p. 108–09. [Brief details.]Google Scholar

Gold, T. The moon’s surface. (In Hess, W. N., and others, ed. The nature of the lunar surface: proceedings of the 1965 IAU-NASA symposium, edited by W. N. Hess, D. H. Menzel and J. A. O’Keefe. Baltimore, Johns Hopkins Press, 1966, p. 107–21.) [Suggests water slowly comes up from interior of moon to underlie low regions forming lunar glaciers whose flow may have produced observed distortion of mare ground.]Google Scholar

Govorukha, L. S. O sootnoshenii prikhoda i raskhoda l’da na Ostrove Ushakova v sovremennykh klimaticheskikh usloviyakh . Izuestiya Vsesoyuznogo Geograjicheskogo Obshchestva , Tom 98, Vyp. 1, 1966, p. 62–64. [Ice cover diminishing on island in north Kara Sea.]Google Scholar

Hansen, B. L. Langway, C. C. jr. Deep core drilling in ice and core analysis at Camp Century, Greenland, 1961–1966. Antarctic Journal of the U.S., Vol. 1, No. 5, 1966, p. 207–08.Google Scholar

Hashimoto, S., and others. Glaciological studies of the Antler Glacier, Alaska, by S. Hashimoto, H. Shimizu and K. Nakamura. Journal of the Faculty of Science, Hokkaido University, Ser. 4, Vol. 13, No. 3, 1966, p. 237–56. [Studies with special emphasis upon the mechanism of formation of ogives. The Antler Glacier is in the Juneau Icefield.]Google Scholar

Hattersley-Smith, G. Glacier research. Canadian Geophysical Bulletin, Vol. 18, 1965, p. 133–48. [Summary of work carried out in Canada during 1965; includes bibliography.]Google Scholar

Kennett, P. Gravity and magnetic measurements on Starbuck and Stubb Glaciers, Graham Land. British Antarctic Survey Bulletin, No. 9, 1966, p. 45–53. [Information on ice thickness of the glaciers and configuration of sub-ice topography.]Google Scholar

Kittredge, T. F., and others. Structure and deformation study of wave-ogives on the Vaughan Lewis Glacier, Juneau Icefield, Alaska, by T. Kittredge, T. F. Freers and T. Havas. Proceedings of the 16th Alaskan Science Conference, College, Alaska, August 29–September 1 1965, 1966, p. 110–11. [It is concluded that wave-ogives are formed at the base of this ice fall by compressive pressure causing shearing along the foliation planes.]Google Scholar

Konovalov, V. G. O primenenii metoda N. N. Pal’gova dlya kosvennykh opredeleniy moshchnosti lednika . Izvestiya Vsesoyuznogo Geograficheskogo Obshchestva , Tom 98, Vyp. 2, 1966, p. 157–60. [Limitations of Pal’gov’s method.]Google Scholar

Kotlyakov, V. M. Plam, M. Ya. Izucheniye veshchestvennogo balansa poverkhnosti gornykh i pokrovnykh lednikov . Trudy. Zakavkazskogo Nauchno-Issledovatel’skogo Gidrometeorologicheskogo Institute (Tiflis), Vyp. 13, 1963, p 34–38. [Discussion of differing roles of wind-blown snow in East Antarctica and Mount El’brus.]Google Scholar

Kotlyakov, V. M., and others. Noryye dannyye o rezhime snegonakopleniya vo vnutrennikh rayonakh vostochnoy Antarktidy . Informatsionnyy Byulleten’ Sovetskoy Antarkticheskoy Ekspeditsii , No. 57, 1966, p. 85–96. [Analysis of measurements made during traverses in 1961–62.]Google Scholar

Ledenev, V. G. Yevdokimov, A. P. Izmencniya shel’fovykh Lednikov Zapadnogo i Eymeri . Informatsionnyy Byulleten’ Sovelskoy Antarkticheskoy Ekspeditsii , No. 55, 1965, p. 12–18. [New position of ice front recorded in 1965.]Google Scholar

Lockhart, L. B. jr., and others. Airborne radioactivity in Antarctica, by L. B. Lockhart, Jr., R. L. Patterson, Jr. and A. W. Saunders, Jr. Journal of Geophysical Research, Vol. 71, No. 8, 1966, p. 1985–91. [Results of measurements at “Little America” and South Pole.]Google Scholar

Martin-Chavannes, J. Le glacier d’Aletsch. Les Alpes. Revue du Club Alpin Suisse, 41^e An., 1^e Trimestre, 1965, p. 53–59. [Discussion of present and former glaciation in the area in the context of 1960 edition of 1: 10,000 map of the glacier.]Google Scholar

Matsuo, S. Miyake, Y. Gas composition in ice samples from Antarctica. Journal of Geophysical Research, Vol. 71, No. 22, 1966, p. 5235–41. [Glacier and iceberg ice contain more gases than sea or pond ice. Nitrogen shows greater retention in ice than other gaseous components.]Google Scholar

Merlivat, L., and others. Etude isotopique d’un glacier en Antarctique, [par] L. Merlivat, C. Lorius et G. Nief. Comptes Rendus Hebdomadaires des Séances de l’Académie des Sciences (Paris), Sér. B, Tom. 263, No. 5, 1966, p. 414–16 [Deuterium analysis of core from ice on edge of Antarctica used to deduce origin of different ice layers.]Google Scholar

Miller, M. M. Potter, D. M. Glacio-morphic effects of the Alaskan Good Friday earthquake, 1964. Proceedings of the 16th Alaskan Science Conference, College, Alaska, August 29–September 1, 1965, 1966, p. 118–22. [Brief report.]Google Scholar

Nougier, J. Glaciers des Kerguelen. Science de l’Avenir, No. 206, 1964, p. 250–55 283–84. [General description.]Google Scholar

Nutt, D. C. The drift dice island WH-5. Arctic, Vol. 19, No. 3, 1966, p. 244–62. [From 1962 to 1964 this island drifted south from the Arctic Ocean through Nares Strait and Baffin Bay.]Google Scholar

Petrov, V. N., and others. Periodichnost’ snegonakopleniya v Antarktide . Informatsionnyy Byulleten’ Sovetskoy Antarkticheskoy Ekspeditsii , No. 57, 1966, p. 97–106. [Analysis of size of annual layers observed in seven pits.]Google Scholar

Redpath, B. B. Geophysics, No. 1. Seismic investigations of glaciers on Axel Heiberg Island, Canadian Arctic Archipelago. Axel Heiberg Island Research Reports, McGill University, Montreal. Jacobsen-McGill Arctic Research Expedition 1959–1962, 1965, [iii], iv, 26 p. [Surveys on the White Glacier and Thompson Glacier; description of instruments; and results by refraction and reflection methods, with conclusions.]Google Scholar

Savel’yev, B. A. Glyatsiologicheskiye issledovaniya 4-y kompleksnoy antarkticheskoy ekspeditsii v 1959 godu . Merzlotnyye Issledovanáya. Sbornik Stacey , No. 3, 1963, p. 18–36. [Report of glaciological work on Antarctic Ice Sheet.]Google Scholar

Shumskiy, P. A. Ob izmeneniyakh antarkticheskogo lednikovogo pokrova . Antarktika. Doklady Komissii 1964 g. . Moscow, Izdatel’stvo Akademii Nauk SSSR [Publishing House of the Academy of Sciences of the U.S.S.R.], 1965, p. 155–72.Google Scholar

Swithinbank, C. W. M. Glaciology of the Ross Ice Shelf. Antarctic Journal of the U.S., Vol. 1, No. 5, 1966, p. 208. [Analysis by University of Michigan field parties during 1959–60, 1960-61 and 1961–62 seasons, including the movement, regime and morphology of the principal valley glaciers flowing into the Ross Ice Shelf.]Google Scholar

Weidick, A. Jakobshavns Isbras i fortid og nutid. Grønland, 1966, Nr. 11, p. 361–86. [Former extent of Jakobshavn Isbra: and its current iceberg production.]Google Scholar

Wilson, A. T. Variation in solar insolation to the South Polar region as a trigger which induces instability in the Antarctic Ice Sheet. Nature, Vol. 210, No. 5035, 1966, p. 477–78. [Evidence that changes in solar insolation in the polar regions, caused by periodic variation of obliquity of Earth’s ecliptic, can be related to occurrence of ice ages.]Google Scholar

Wood, W. A. The Icefield Ranges Research Project. Geographical Review, Vol. 56, No. 4, 1966, p. 586. [Account of a major surge in Steele Glacier, Yukon Territory, Canada.]Google Scholar

Zhantuarov, R. S. Markov, K. K. C. dinamike antarkticheskogo lednikovogo pokrova . Antarktika. Doklady Komissii 1964 g. . Moscow, Izdatel’stvo Akademii Nauk SSSR [Publishing House of the Academy of Sciences of the U.S.S.R.], 1965, p. 138–54.Google Scholar

Antonov, V. S., and others. Tipovyye osobennosti ledovogo rezhima sudokhodnykh rek arkticheskoy zony . Problemy Arktiki á Antarktiki , Vyp. 15, 1964, p. 11–17. [Three types of ice break-up.]Google Scholar

Avgevich, V. I. Primeneniye aerometodov y izuchenii morskikh polyarnykh l’dov . Izvestiya Vsesóvaznogo Geografscheskogo Obshcherlva , Tom 96, Vyp. 3, 1964, p. 197–205. [Discussion of method used to map Antarctic sea ice.]Google Scholar

Brown, J. R. Brown, D. W. Reverberation under Arctic sea-ice. Journal of the Acoustical Society of America, Vol. 40, No. 2, 1966, p. 399–444. [Strong dependence of under-ice back-scattering on surface roughness.]Google Scholar

Bulatov, S. N. Ginzburg, B. M., ed. Prognozy ledovykh yavleniy na rekakh i vodokhranilishchakh . Trudy Tsentral’nogo Instituta Prognozov , Vyp. 151, 1965, 176 p. [Observations of break-up and freeze-up in various parts of U.S.S.R., and associated forecasting methods.]Google Scholar

Chapman, R. P. Scott, H. D. Backscattering strengths of sea ice. Journal of the Acoustical Society of America. Vol. 39, No. 6, 1966, p. 1191–93. [Letter. Measurements for “point” sources of sound in sea-water scattered back from smooth young ice and heavily rafted winter ice.]Google Scholar

Doronin, Yu. P. O teplovom balans tsentral’noy Arktiki . Trudy Arkticheskogo i Antarkticheskogo Nauchno-Issledovatel’skogo Irlstituta , Tom 253, 1963, p. 178–84. [Heat balance of sea ice and of open leads.]Google Scholar

Korolcowna, H. Z obserwacji nad zamarzaniem Jeziora Mikolajskiego. Przeglad Geograf[czny, Vol. 36, No. 4, 1964, p. 729–32. [Some observations of the formation of the ice sheet on Mikolajki lake. Observations of formation of ice sheet on this lake, which differs from year to year.]Google Scholar

Lunde, T. Ice conditions at Svalbard 1946–1963. Norsk Polarinslilutl. Arbok, 1963 [pub. 1965], p. 61–80. [Maps and statistics. Evidence for 3–4 yr. cycle.]Google Scholar

Michel, B. Theory of formation and deposit of frazil ice. Proceedings of the Eastern Snow Conference, 20th annual meeting, 1963, p. 130–48. [Discussion, p. 143–48. Tests on conditions for formation and adhesion of frazil ice.]Google Scholar

Milne, A. R. Statistical description of noise under shore-fast sea ice in winter. Journal of the Acoustical Society of America, Vol. 39, No. 6, 1966, p. 1174–82. [Attempt to relate field measurements of noise to wind action and cracking origins.]Google Scholar

Nusser, F. Eisberge im Raum uni Kap Farvel. Der Wetterlotse, Jahrg. 18, No. 233, 1966, p. 107–10 [Origin and occurrence of icebergs in waters off Kap Farvel, South Greenland.]Google Scholar

Palosuo, E. Ice in the Baltic. Oceanography and Marine Biology, Vol. 4, 1966, p. 79–90. [Survey of processes involved in formation and melting of sea ice and maps showing statistical data.]Google Scholar

Popham, R. W. Samuelson, R. E. Polar exploration with Nimbus. (In Observations from the Nimbus I meteorological satellite. U.S. National Aeronautics and Space Administration. Special Report SP-89, 1965, p. 47–59.) [Observations of extent of ice.]Google Scholar

Popham, R. W. Samuelson, R. E. Polar exploration with Nimbus meteorological satellite. Arctic, Vol. 18, No. 4, 1965, p. 246–55. [Photographs by an advanced vidicon camera system and a high-resolution infra-red system were used to make extensive ice reconnaissance in Arctic and Antarctic.]Google Scholar

Schulze, O. Die Eisverhältnisse an der Prawda-Küste während der VI. sowjetischen Antarktisexpedition 1961/1962. Abhandlungen des Meteorologischen Dienstes der Deutschen Demokratischen Republik, Bd. 10, Ht. 75, 1965, p. 19–35. [Ice thickness measurements in Davis Sea.]Google Scholar

Spichkin, V. A. Rol’ ispareniya V poverkhnostnoy ablyatsii morskikh Nov . lnformatsionnyy Byulleten’ Sovetskoy Antarkticheskoy Ekspeditsii , No. 55, 1965, p. 34–36. [Greater in Antarctic than in Arctic, owing to lower relative humidity of air.]Google Scholar

Tsurikov, V. L. K voprosu o mezhdunarodnoy ledovoy nomenclature . Okeanologiya , Tom 6, Vyp. 2, 1966, p. 372–78. [Discussion of Canadian proposals to amend W.M.O. sea ice nomenclature.]Google Scholar

Untersteiner, N. A sonic device for measuring thickness changes at the bottom of floating ice . Antarctic Journal of the U.S., Vol. 1, No. 5, 1966, p. 208–09.Google Scholar

Woodcock, A. H. Melt patterns in ice over shallow waters. Limnology and Oceanography, Vol. 10 (Supplement), 1965, p. R290–R297. [Role of snow pressure and of convection cells in the water.]Google Scholar

Andrews, J. T. Pattern of coastal uplift and deglacierization, West Baffin Island, N.W.T. Geographical Bulletin (Ottawa), Vol. 8, No. 2, 1966, p. 174–93. [Uplift of the west coast has been slow compared to adjacent glacial dispersal zones.]Google Scholar

Andrews, J. T. Surface boulder orientation studies around the north-western margin of the Barnes Ice Cap, Baffin Island, Canada. Journal of Sedimentary Petrology, Vol. 35, No. 3, 1965, p. 753–58. [Orientation of surface boulders from ground and lateral moraines corresponds closely with known ice movement.]Google Scholar

Andrews, J. T. Shimizu, K. Three-dimensional vector technique for analyzing till fabrics: discussion and FORTRAN program. Geographical Bulletin (Ottawa), Vol. 8, No. 2, 1966, p. 151–65. [A programme for a three-dimensional vector analysis of till fabrics is presented.]Google Scholar

Andrews, J. T. Smithson, B. B. Till fabrics of the cross-valley moraines of north-central Baffin Island, Northwest Territories, Canada. Geological Society of America. Bulletin, Vol. 77, No. 3, 1966, p. 271–90. [Till fabric patterns show variations according to slope and location within valley. Origin of cross-valley moraines discussed.]Google Scholar

Bik, M. J. J. New methods in alpine glacial geomorphology. Zeitschrft für Geomorphologie, Nette Folge, Bd. 10, Ht. 3, 1966, p. 303–10. [Suggestions by several authorities.]Google Scholar

Broecker, W. S. Absolute dating and the astronomical theory of glaciation. Science, Vol. 151, No. 3708, 1966, p. 299–304. [Modification of Milankovitch theory to allow for two stable states of ocean-atmosphere system.]Google Scholar

Broecker, W. S. Glacial rebound and the deformation of the shorelines of proglacial lakes. Journal of Geophysical Research, Vol. 71, No. 20, 1966, p. 4777–83. [Rate of glacial retreat before formation of shoreline derived from curvature of its uplifted portion. Deduction of shapes of continental ice sheets.]Google Scholar

Brömssen, U. Von. Jordartsbildning och isaysmältning i Handölsáns dalgáng i västra Jämtland. Geologiska Föreningens i Stockholm Förhandlingar, Vol. 88, Pt. 1, No. 524, 1966, p. 90–112. [Formation of terraces and plains and ice recession in Handölsán valley, Jämtland, north Sweden.]Google Scholar

Cotton, C. A. Antarctic scablands. New Zealand journal of Geology and Geophysics, Vol. 9, Nos. 1–2, 1966, p. 130–33. [The scabland Iandscape has probably resulted from glacial erosion.]Google Scholar

Craig, B. G. Glacial Lake McConnell, and the surficial geology of parts of Slave River and Redstone River map-areas, District of Mackenzie. Canada. Geological Survey. Bulletin 122, 1965, viii, 33 p. [Area was completely glaciated by Wisconsin Laurentide ice sheet, which extended westward into Mackenzie Mountains.]Google Scholar

Falconer, G. Preservation of vegetation and patterned ground under a thin ice body in northern Baffin Island, N.W.T. Geographical Bulletin (Ottawa), Vol. 8, No. 2, 1966, p. 194–200. [A thin ice body in northern Baffin Island is undergoing rapid recession. This supports previous estimates of the occurrence of a markedly more nival period in parts of Arctic Canada two to three centuries ago.]Google Scholar

Gerasimov, I. Posledniv seuropevskiy lednikovyy pokrov . Moscow, Izdatel’stvo “Nauka” [Publishing House “Niauka”], 1965. 220 p. [Volume of papers covering the last glaciation over the whole of Europe.]Google Scholar

Gjessing, J. Some effects of ice erosion on the development of Norwegian valleys and fjords. Norsk Geografisk Tidsskrifl, Bd. 20, Ht. 8, 1965–66, [pub.] 1966, p. 273–99. [Combined glacial and fluvial erosion must have increased rate of erosion and deepened valleys much more than a fluvial erosion alone in the same time.]Google Scholar

Klohn, E. J. The elastic properties of a dense glacial till deposit. Canadian Geotechnical Journal, Vol. 2, No. 2, 1965, p. 116–40. [Field and laboratory measurements. Discussion, p. 129–40.]Google Scholar

Müller, F. Barr, W. Postglacial isostatic movement in north-eastern Devon Island, Canadian Arctic Archipelago. Arctic, Vol. 19, No. 3, 1966, p. 263–69. [The ¹⁴C dates of marine shells indicate that the area was clear of ice as early as 15,500 R.P. and that the most rapid isostatic uplift took place between 9,000 and 8,000 B.P.]Google Scholar

Rudberg, S. Morphological processes and slope development in Axel Heiberg Island, Northwest Territories, Canada. Nachrichten der Akademie der Wissenschaflen in Göttingen, 2. Mathematisch-physikalische Klasse, Jahrg. 1963, Nr. 14, p. 211–28. [General physiography, former more extensive glaciation, assorting processes and mass movement, and influence of snow and ice.]Google Scholar

Rutten, M. G., and others. Ice-pushed ridges, permafrost, and drainage: a discussion, by M. G. Rutten.-a reply, by W. H. Mathews and J. R. Mackay. Journal of Geology, Vol. 73, No. 6, 1965, p. 895–96. [Discussion by Rutten of objections raised by Mathews and Mackay to his ideas on role of permafrost in development of ridges and reply by Mathews and Mackay.]Google Scholar

Smalley, I. J. Drumlin formation: a Theological model. Science, Vol. 151, No. 3716, 1966, p. 1379–80. [Theoretical explanation of separation of large clay particles from ice to form drumlins.]Google Scholar

Stepanov, I. N. O protsessakh vyvetrivaniya v ledovom ripe litogeneza . Litalogiya i Poleznyye Iskopayeme , No. 5, 1964, p. 109–10. [Discussion of weathering processes on and in glaciers. English translation: International Geological Reviews, Vol. 7, No. 12, 1965, p. 2182–83.]Google Scholar

Szupryczyński, J. Eskers and kames in the Spitsbergen area. Geographia Polonica, 6, 1965, p. 127–40. [Summary of recent Polish research in Vestspitsbergen.]Google Scholar

Theakstone, W. H. A note on some features of Pleistocene deglaciation in the Svartisen area. Norsk Geografisk Tidsskrift, Bd. 20, Ht. 8, 1965–66, [pub.] 1966, p. 300–04. [Evidence was found to indicate that ice “died” and stagnated in situ in at least one area a little north of Svartisen.]Google Scholar

Wright, H. E. jr. Frey, D. G. International studies on the Quaternary. New York, Geological Society of America, Inc., 1965. 565 p. [Papers on Quaternary studies in parts of the world other than U.S.A. and U.S.S.R. prepared for seventh Congress of International Association for Quaternary Research, Boulder, Colorado, 1965.]Google Scholar

Wright, H. E. jr. Frey, D. G. The Quaternary of the United Stales. Princeton, N. J., Princeton University Press, 1965. 922 p. [Review volume prepared for seventh Congress of International Association for Quaternary Research, Boulder, Colorado, 1965. Includes the following papers: R. F. Flint. “Introduction: historical perspectives”, p. 3–11; J. R. Curray, “Late Quaternary history, continental shelves of the United States”, p. 723–35; W. S. Brocker, “Isotope geochemistry and the Pleistocene climatic record”, p. 737–53; R E. Wilcox, “Volcanic-ash chronology”, p. 807–16; H. C. Fritts, “Dendrochronology”, p. 871–79; J. M. Mitchell, Jr., “Theoretical paleoclimatology”, p. 881–901.]Google Scholar

Annersten, L. Interaction between surface cover and permafrost. Biutetyn Peryglacjatny (Łódź), No. 15, 1966, p. 27–33. [Observations in the Labrador Peninsula.]Google Scholar

Ball, D. F. Late-glacial scree in Wales. Biutetvn Peryglacjalny (Łódź), No. 15, 1966, p. 151–63. [Distribution of scree as indication of nature of periglacial action in late Pleistocene.]Google Scholar

Black, R. F. Comments on periglacial terminology. Biuletyn Peryglacjalnv (Łódź), No. 15, 1966, p. 329–33. [Replies to questionnaire circulated by Commission de Géomorphologie Périglaciaire.]Google Scholar

Bout, P. Réponses au questionnaire dc la Commission de Géomorphologie Périglaciaire. Biulelyn Peryglacjalny (Łódź), No. 15, 1966, p. 335–55. [Notes on frozen soil and patterned ground terminology and replies to questionnaire circulated by Commission de Géomorphologie Périglaciaire.]Google Scholar

Chambers, M. J. C. Investigations of patterned ground at Signy Island, South Orkney Islands. I. Interpretation of mechanical analyses. British Antarctic Survey Bulletin, No. 9, 1966, p. 21–40. [Evidence from experimental work on Signy Island in assessing the relative importance of frost-heaving and solifluction in these processes.]Google Scholar

Corte, A. E. Particle sorting by repeated freezing and thawing. Biulelyn Peryglacjalny (Łódź), No. 15, 1966, p. 175–240. [Laboratory experiments described and used to distinguish three kinds of sorting which can occur as a result of freeze-thaw cycles.]Google Scholar

Cotet, P. La répartition des cryostructures pléistocènes sur le territoire de la Roumanie. Biulelyn Peryglacjalny (Łódź), No. 15, 1966, p. 35–38. [Distribution of fossil frost structures in Rumania.]Google Scholar

Cotet, P. Réponses ä l’enquête sur le problème de la notion et du ternie du “périglaciaire” Biuletyn Peryglacjalny (Łódź), No. 15, 1966, p. 357–60. [Comments on terminology of periglacial.]Google Scholar

Dahl, R. Block fields, weathering pits and tor-like forms in the Narvik mountains, Nordland, Norway. Geogrefrska Anneler, Vol. 48a, No. 2, 1966, p. 55–85. [Study of periglacial erosion processes. Discussion of use as indicator of lack of glaciation.]Google Scholar

Dillon, H. B. Andersland, O. B. Predicting unfrozen water contents in frozen soils. Canadian Geatechnicat Journal, Vol. 3, No. 2, 1966, p. 53–60. [Simple method presented, depending on relationship between temperature and certain physical properties of soil.]Google Scholar

Dirksen, C. Miller, R. D. Closed-system freezing of unsaturated soil. Proceedings. Soil Science Society of America, Vol. 30, No. 2, 1966, p. 168–73. [Experiments show that heaving is possible even without water transport from outside.]Google Scholar

Dylik, J. Problems of ice-wedge structures and frost-fissure polygons. Biuletyn Peryglacjalny (Łódź), No. 15, 1966, p. 241–91. [General discussion of causes of fissure polygons and ice wedges and their identification. French abstract.]Google Scholar

Dylik, J. Right and wrong in sceptical views on the problem of periglacial phenomena revealed in Pleistocene deposits. Bulletin de la Société des Sciences et des Lettres de Łódź, Classe 3, Vol. 16, No. 8, 1965, p. 1–28.Google Scholar

Dylik, J. Raynal, R. Tendances nouvelles dans les recherches périglaciaires depuis le Congrès International de Géographie à Rio de Janeiro. Biuletyn Peryglacjalnv (Łódź), No. 15, 1966, p. 5–26. [Review of work on periglacial phenomena, 1956–64.]Google Scholar

Everett, K. R. Slope movement and related phenomena. (In Wilimovsky, N. J. Wolfe, J. N. ed. Environment of the Cape Thompson region, Alaska. Oak Ridge, Tenn. U.S. Atomic Energy Commission. Division of Technica Information Extension, 1966, p. 172–220.) [Cape. hompson region, Alaska. Down-slope movements are most pronounced during freeze-up and thaw. The rate and amount is greater on the south-east-facing slope than on the north-west-facing slope by a factor of 2 or 3.]Google Scholar

Gregory, K. J. Aspect and landforms in north east Yorkshire. Biulelyn Peryglacjalnv (Łódź), No. 15, 1966. p. 115–20. [Analysis of orientation of nivation benches.]Google Scholar

Hamelin, L.-E. Glaciers et modelé périglaciaire. Cahiers de Géographie de Québec, 9^e An., No. 18, 1965, p. 239–42. [Interrelation between glaciers and periglacial processes.]Google Scholar

Hoekstra, P., and others. Frost-heaving pressures, by P. Hoekstra. E. Chamberlain and T. Prate. Highway Research Record, No. 101, 1965, p. 28–38. ([U.S.] National Research Council Publication No. 1318.) [Laboratory measurements.]Google Scholar

Jackson, A. Uhlmann, D. R. Particle sorting and stone migration due to frost heave. Science, Vol. 152, No. 3721, 1966, p. 545–46. [Discussion of mechanism.]Google Scholar

Lewis, C. A. The nivational landforrns and the reconstructed snowline of Slaettaratindur, Faeroe Islands. Bialett’n Peryglacjalny (Łódź), No. 15, 1966, p. 293–302.Google Scholar

Mackay, J. R. Stager, J. K. Thick tilted beds of segregated ice, Mackenzie Delta area, N.W.T. Biulelyn Peryglacjalny (Łódź), No. 15, 1966, p. 39–43. [Observation and interpretation of these structures as horizontal layers of ground ice subsequently deformed by glacier action.]Google Scholar

Morariu, T. Savu, A. Quelques problèmes du périglaciaire en Roumanie. Biuletyn Peryglacjalny (Łódź), No. 15, 1966, p. 53–61. [General description of periglacial relief in Rumania.]Google Scholar

Péwé, T. L. Paleoclirnatic significance of fossil ice wedges. Biulelyn Peryglacjalny (Łódź), No. 15, 1966, p. 65–73. [Observations in Alaska suggest that ice wedges form actively only when mean annual air temperature is below −6 to −8°C. Discussion, p. 72–73.]Google Scholar

Portmann, J.-P. Sols gelés en permanence. Les Alpes. Revue du Club Alpin Suisse, 42^e An., 2^e Trimestre, 1966, p. 158–60. [Brief discussion of permafrost and problems of frozen-ground engineering, and of frozen ground in Neuchâtel region of Jura.]Google Scholar

Tricart, J. Quelques aspects des phénomènes périglaciaires quaternaires dans la Péninsule Ibérique. Biuletyn Peryglacjalny (Łódź), No. 15, 1966, p. 313–27. [Description of periglacial phenomena in the Iberian Peninsula.]Google Scholar

Ugolini, F. C. Soils of the Mesters Vig district, northeast Greenland. 1. The Arctic Brown and related soils.-2. Exclusive of Arctic Brown and podzol-like soils. Meddelelser om Grenland, Bd. 176, Nr. 1, 1966, 22 p.; Nr. 2, 1966, 25 p. [1: Arctic Brown soil in Greenland is a link between the North American and Eurasian continents and establishes the Arctic Brown as a circumpolar soil. 2: cryopedogenie and gelifluction processes are very important factors affecting morphology and occurrence of the different types of soils.]Google Scholar

Watson, E. Two nivation cirques near Aberystwyth, Wales. Biuletyn Peryglacjalny (Łódź), No. 15, 1966, p. 79–101. [Description of small cirques believed to have been formed by motionless snow patches. Discussion, p. 98–101.]Google Scholar

Yao, L. Y. C. Broms, B. B. Excess pore pressures which develop during thawing of frozen fine-grained subgrade soils. Highway Research Record, No. 101, 1965, p. 39–56. ([U.S.] National Research Council Publication No. 1318.) [Method of calculation.]Google Scholar

Bastin, F. E. Observations météorologiques en surface. (a) A la base Roi Baudouin du t janvier 1959 au 31 janvier 1860. (b) En mer du 14 décembre 1958 au 14 février 1959. Expédition Antarctique Belge 1959. Publications, Sér. A, No. 1, 1966, 108 p.Google Scholar

Benson, C. S. Rogers, G. W. Alaskan air pollution—the nature of ice fog and its development and settlement implications. Proceedings of the 16th Alaskan Science Conference, College, Alaska, August 29-September 1,1965, 1966, p. 233–45. [Ice fog is defined as low-temperature air pollution and will occur when air temperatures go below −35°C. The Fairbanks ice fog area vertical thickness varies between 10 and 30 m. The dynamics within the inversion layer associated with ice fog have been investigated.]Google Scholar

Coroniti, S. C., ed. Problems of atmospheric and space electricity. Proceedings of the third International Conference on Atmosphere and Space Electricity, Montreux, 1963. Amsterdam, Elsevier Publishing Co., 1965. xiv, 616 p. [includes the following papers in which the theory of thunderstorm electrification is discussed: B. J. Mason, “Charge generation in thunderstorms”, p. 239–54.; C. B. Moore, “Charge generation in thunderstorms”, p. 255–62; D. Müller-Hillebrand, “Comment”, p. 263–67; N. S. Shishkin, “The role of coagulation of charged cloud particles in the development of thunderstorm phenomena”, p. 268–79; M. Brook, “Thunderstorm electrification”, p. 280–83; J. Latham, “Possible reconciliation of the work of Reynolds et al. with the temperature-gradient theory”, p. 284; B. Vonnegut, “Thunderstorm theory”, p. 285–95; E. J. Workman, “Thunderstorm electricity”, p. 296–303; J. A. Chalmers, “Charge generation in thunderstorms”, p. 304–06; J. D. Sartor, “Induction charging thunderstorm mechanism”, p. 307–10; P. B. MacReady, Jr., ‘Thunderstorm charging mechanisms”, p. 311; A. Puhringer, “Comment”, p. 312; “Discussions”, p. 313–20]Google Scholar

Dort, W. jr. Rapid reconnaissance of heat-flow patterns in snow-covered thermal areas. journal of Geophysical Research, Vol. 71, No. 18, 1966, p. 4439–40 [Use of pattern of snow depth to give information about local variations of heat flow.]Google Scholar

Gunn, R. Thunderstorm electrification of hail and graupel by polar dribble. Science, Vol. 151, No. 3711, 1966, p. 686–87. [Possible method of generating thunderstorm electrification.]Google Scholar

Havens, J. M. Meteorology, No. 2. Meteorology and heat balance of the accumulation area, McGill Ice Cap, Canadian Arctic Archipelago—summer 1960. (Upper Ice Station I: 79° 41’ N, 90° 27’ W, 1530 m.). Axel Heiberg Island Research Reports, McGill University, Montreal. Jacobsen-McGill Arctic Research Expedition 1959–1962, 1964, [iii], viii, 87 p. +errata slip. [Includes sections on glacial-meteorology and heat balance at a melting snow surface. Also notes on fog and rime, snowfall amounts, and drifting and blowing snow.]Google Scholar

Havens, J. M., and others. Meteorology, No. 4. Comparative meteorological survey and a short-term heat balance study of the White Glacier, Canadian Arctic Archipelago—summer 1962, [by] J. M. Havens, F. Müller and G. C. Wilmot. Axel Heiberg Island Research Reports, McGill University, Montreal. Jacobsen-McGill Arctic Research Expedition 1959–1962, 1965, [iii], vi, 68 p. [Includes result of measurements and analysis. Discusses validity of various methods of calculating heat balance for periods of 1–2 days.]Google Scholar

Howell, W. E. Twelve years of cloud seeding in the Andes of northern Peru. Journal of Applied Meteorology, Vol. 4, No. 6, 1965, p. 693–700. [Report on success of project using silver iodide.]Google Scholar

Lacy, R. E. Frost patterns on brickwork. Weather, Vol. 21, No. 4, 1966, p. 135–37. [Photographs of effect and discussion of origin.]Google Scholar

List, R., and others. Heat exchange ratios of hailstones in a model cloud and their simulation in a laboratory, [by] R. List, P. H. Scheupp and R. G. J. Methot. Journal of the Atmospheric Sciences, Vol. 22, No. 6, 1965, p. 710–18. [Theoretical studies of contribution of different terms to heat balance of hailstones.]Google Scholar

Longlay, R. W. Thompson, G. E. A study of the causes of hail. Journal of Applied Meteorology, Vol. 4, No. 1, 1965, p. 69–82. [Analysis of data for southern Alberta 1959–63.]Google Scholar

Mather, K. B. Miller, G. S. Wind drainage off the high plateau of eastern Antarctica. Nature, Vol. 209, No. 5020, 1966, p. 281–84. [Compilation of data for East Antarctica shows drainage wind determines predominant wind direction.]Google Scholar

Sansom, H. W. The use of explosive rockets to suppress hail in Kenya. Weather, Vol. 21, No. 3, 1966, p. 86–91. [Success reported. Discussion of theories.]Google Scholar

Schleusener, R. A., and others. Hailfall data from a fixed network for the evaluation of a hail modification experiment, by R. A. Schleusener, J. D. Marwitz and W. L. Cox. Journal of Applied Meteorology, Vol. 4, No. 1, 1965, p. 61–68. [Detailed statistical study shows present data inadequate to allow effectiveness of hail modification to be assessed.]Google Scholar

Soulage, G. Methods of measurement of ice nuclei concentrations. Pure and Applied Geophysics, Vol. 60, No. 1, 1965, p. 183–88. [Discussion of relative advantages of different methods and precautions necessary.]Google Scholar

Taylor, C. B. Tritium in Southern Hemisphere precipitation 1953–1964. Tellus, Vol. 18, No. 1, 1966, p. 105–31. [Includes data from snow in various parts of Antarctica.]Google Scholar

Tsitovich, H. T. A. K voprosu o stokovom vetre . Trudy Tsentraznoy Aerologicheskoy Observatorii. , No. 68, 1965, p. 67–75. [Observations in Antarctica.]Google Scholar

Vittori, O. List, R. Comment on “On the effect of explosion waves on hailstone models”. Journal of Applied Meteorology, Vol. 5, No. 1, 1966, p. 132–34. [Comments by Vittori on List’s article (ibid., Vol. 2, No. 4, 1963, p. 494–97) and reply by List.]Google Scholar

Duce, R. A., and others. Iodine, bromine, and chlorine in winter aerosols and snow from Barrow, Alaska, by R. A. Duce J. W. Winchester T. W. Van Nahl. Tellus, Vol. 18, No. 2, 1966, p. 238–48.Google Scholar

Dunham, S. B. Electrostatic charging by solid precipitation. Journal of the Atmospheric Sciences, Vol. 23, No. 4, 1966, p. 412–15. [Measurement of charge produced when snow strikes various surfaces at high speed.]Google Scholar

Fukuhara, K. On the snowfall forecasting. Part 5. Journal of Meteorological Research, Vol. 17, No. 6, 1965, p. 396–400. [Study of condition of atmosphere leading to heavy falls of snow.]Google Scholar

Kogan, R. M., and others. Determination of water equivalent of snow cover by method of aerial gamma-survey, by R. M. Kogan, M. V. Nikiforov, Sh. D. Fridman, V. P Chirkov and A. F. Yakovlev. Soviet Hydrology. Selected Papers, 1965, No. 2, p. 183–87. [Methods measuring natural y-activtty of soil.]Google Scholar

Kumai, M. Microspherules in snow and ice-fog crystals. Journal of Geophysical Research, Vol. 71, No. 14, 1966, p. 3397–404. [Spherules found in snow crystals, ice-fog crystals, fallout particles, and fly ash, from Greenland, the United States and Japan, described.]Google Scholar

LaChapelle, E. R. The control of snow avalanches. Scientific American, Vol. 214, No. 2, 1966, p. 92–101. [General survey of present knowledge.]Google Scholar

Martinelli, M. jr. An estimate of summer runoff from alpine snowfields. Journal of Soil and Water Conservation, Vol. 20, No. 1, 1965, p. 24–26. [Uses aerial photographs of part of Front Range, central Colorado.]Google Scholar

Martinelli, M. jr. Davidson, K. D. An example of damage from a powder avalanche. Bulletin de l’ Association Internationale d’Hydrologie Scientifique, 11^e An., No. 3, 1966, p. 26–34. [Movement of a truck used to deduce air velocity.]Google Scholar

Meiman, J. R. Slaughter, C. W. Spread of cetyl−1−C¹⁴ alcohol on a melting snow surface. Bulletin de l’ Association Internationale d’Hydrologie Scientifique, 11^e An., No. 3, 1966, p. 5–8. [Measurements of spread of substance used to reduce evaporation.]Google Scholar

Morris, J. Y. O’Loughlin, C. L. Snow investigations in the Craigieburn Range. Journal of Hydrology (New Zealand), Vol. 4, No. 1, 1965, p. 2–16. [Test of snow survey techniques.]Google Scholar

Nyberg, A. A study of the evaporation and the condensation at a snow surface. Arkin för Geofysik, Bd. 4, Ht. 25, 1966, p. 577–90. [Instrument to measure evaporation or condensation accurately.]Google Scholar

Rantz, S. E. Snowmelt hydrology of a Sierra Nevada stream. U.S. Geological Survey. Water Supply Paper 1779-R, 1964, 36 p. [Report of comparison between calculated and observed run-off.]Google Scholar

Vanni, M. Pour une classification géographique des avalanches. Bollettieo del Comitato Glaciologito Italian, 2 Ser., No. 12, Pt. 2, 1961–62, [pub.] 1966, p. 39–54. [Classification based on distribution in altitude of formation in the various mountain regions.]Google Scholar

Yefremov, P. V. Shelepova, G. S. K voprosu o tochnosti rascheta intensivnosti snegotainiya . Trudy Tsentral’nogo Instituta Prognozov , Vyp. 134, 1964, p. 77–84. [Comparison of various calculations with observation.]Google Scholar

Yel’mesov, A. M. K voprosu o mekhanicheskikh svoystvakh snezhnogo pokrova . Trudy 7‘akavkazskogo Nauchno-Issledovatel’skogo Gidrometeorologicheskogo Instituta (Tiflis), Vyp. 13, 1963, p. 52–60. [Formulae given to express results of experimental and theoretical studies.]Google Scholar