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Glaciological Literature

Published online by Cambridge University Press:  30 January 2017

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Copyright © International Glaciological Society 1967

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

Armstrong, T. E., and others. Illustrated glossary of snow and ice, by T. [E.] Armstrong B. [B.] Roberts C. [W. M.] Swithinbank. Cambridge, Scott Polar Research Institute, 1966. v, 60 p., 79 photos. (Scott Polar Research Institute Special Publication No. 4.) [Revised and augmented edition of Armstrong and Roberts, “Illustrated ice glossary”, Polar Record, Vol. 8, No. 52, 1956, p. 4–12; Vol. 8, No. 54, 1956, p. 221; Vol. 9, No. 59. 1958. p. 90–96. Includes equivalent terms and indexes in Danish, Finnish, French, German, Icelandic, Norwegian, Russian and Spanish.]Google Scholar
Fletcher, J. O., ed. Proceedings of the symposium on the Arctic heat budget and atmospheric circulation. January 31 through February 4, 1966. Lake Arrowhead, California. Prepared for the. National Science Foundation. Santa Monica, California, Rand Corporation, 1966. xvii, 567 p. (Memorandum RM-5233-NSF.) [Includes the following papers as well as general information about the symposium: M. I. Budyko, “Polar ice and climate”, p. 3–21; J. O. Fletcher, “The Arctic heat budget and atmospheric circulation”, p. 23–43; J. M. Mitchell, Jr., “Stochastic models of air-sea interaction and climate fluctuation”, p. 45–74; A. A. Girs, “Heat regime of the Soviet Arctic related to the main atmospheric circulation patterns and their many yearly variations”, p. 75–110; Ye. P. Borisenkov, “A quantitative description of some characteristics of the general circulation and their relation to the radiation regime of the Arctic”, p. 111–34; F. Müller, “Evidence of climatic fluctuations on Axel Heiberg Island, Canadian Arctic Archipelago”, p. 135–56; P. Putnins, “The influence of Greenland on the general atmospheric circulation”, p. 157–77; M. R. Bloch, “Historical evidence of sea-level change and its relation to polar albedo”, p. 179–96; report of working group on some issues concerning climatic change and possible ways of resolving them, p. 197–99; N. Untersteiner, “Calculating thermal regime and mass budget of sea ice”, p. 203–13; W. I. Wittmann and J. J. Schule, Jr., “Comments on the mass budget of Arctic pack ice”, p. 215–46; Yu. P. Doronin, “Characteristics of the heat exchange”. p. 247–66; F. I. Badgley, “Heat budget at the surface of the Arctic Ocean”, p. 267–77; M. S. Marshunova and N. T. Chernigovsky, “Numerical characteristics of the radiation regime in the Soviet Arctic”. p. 279–97; E. Vowinekel and S. Orvig, “Possible changes in the radiation budget over the polar ocean”, p. 299–303; J. A. Businger, “Transfer of momentum and heat in the planetary boundary layer”, p. 305–32; report of working group on the heat and mass budget of the pack ice, p. 333–34; report of working group on radiation, climate, and cloud conditions in the Arctic, p. 335–39; report of working group on atmospheric advection and turbulent exchange of heat, moisture, and momentum, p. 340–42; L. R. Rakipova, “The influence of the Arctic ice cover on the zonal distribution of atmospheric temperature”, p. 411–41; L. K. Coachman, “Production of supercooled water during sea ice formation”, p. 497–529; R. D. Maxson and W. H. Munk, “The formation of bottom water”, p. 547–48 (abstract only); report of working grottp on heat, water, and ice exchange, p. 552–53; report of working group on development of oceanic circulation models, p. 554–55.]Google Scholar
Gellert, J. F. Neue chinesische Hochgebirgs- und Gletscherforschung in Innerasien. Petermann Geographische Mitteilungen, Jahrg. 110, 3. Quartalsht., 1966, p. 19899. [Short note on Chinese glacier and snow research in Central Asia.]Google Scholar
Haefeli, R. Creep and progressive failure in snow, soil, rock, and ice. Proceedings of the sixth International Conference on Soil Mechanics and Foundation Engineering, Montreal, 8–15 Sept. 1965, Vol. 3, 1966, p. 13448. [Comparisons between properties of these materials and implications in engineering.]Google Scholar
Heckel, V. Wolf, J. Hindúkuš. Praha, Sportovni a Turistické Nakladatelstvi, 1967. 228 p. [Photographic description of Czechoslovak expedition to the Hindu Kush in 1965.]Google Scholar
Perov, V. F. Materialy k izucheniyu snezhnikov, lednikov i merzlotnogo rel’yefa Khibinskikh Gor . Irformatsionnyy Sbornik o Rabotakh po Mezhdunarodnomu Geofzicheskomu Godu , No. 11, 1965, 192 p. [Observations in Murmanskaya Oblast’ during International Geophysical Year. E 957–58.]Google Scholar
Robin, G. de Q., ed. Glaciology. Annals of the International Geophysical rear, 1957–1958, Vol. 41, 1967, ix, 239 p. [Summarizes work done during International Geophysical Year, 1957–58, and during International Geophysical Cooperation, 1959; national reports; catalogue of material in Data Centres.]Google Scholar
Zabirov, R. D., ed. Glyatsiologicheskiye issledovaniya na Tyan’-Shane . Raboty Tyan’-Shan’skoy Fiziko-Geograficheskoy Slantsii , Vyp. 11, 1965, 117 p.Google Scholar
Zabirov, R. D. Kotlyakov, V. M., ed. Tezisy dokladov tret’yego vsesoyuznogo glyatsiologischeskogo simpoziuma . Frunze, Akademiya Nauk Kirgizskoy SSR [Academy of Sciences of the Kirgiz S.S.R.], 1965. 106 p. [Summaries of 77 papers on all aspects of glaciology.]Google Scholar

Glaciological instruments and methods

von Buttlar, H. Wiik, B. Enrichment of tritium by thermal diffusion and measurement of dated Antarctic MOW samples. Science, Vol. 149, No. 3690, 1965, p. 137173. [Construction features of continuous Bow thermal diffusion apparatus, and test measurements of apparatus, are described. Method was applied satisfactorily to tritium concentration of firn along profile in ice shelf of “Base Roi Baudouin”, Prinsesse Ragnhild Kyst.]CrossRefGoogle Scholar
Crozaz, G. Fabri, P. Mesure du polonium à l’échelle de 10−13 curie, traçage par le 208Po et application à la chronologie des glaces. Earth and Planetary Science Letters, Vol. 1, No. 6, 1966, p. 44648. [Method used to measure accumulation at Pole of Relative Inaccessibility.]CrossRefGoogle Scholar
Engman, E. T. Review of snow measuring instrumentation and evaluation of a pressure pillow snow-measuring device. Proceedings of the Eastern Snow Conference, 23rd annual meeting, 1966, p. 117. [Snow measuring techniques and instruments reviewed, and results discussed of evaluation of 12-ft. pressure pillow during 1964–65 season.]Google Scholar
Flowers, E. C. Helfert, N. F. Laboratory and field investigations of Eppleyradiation sensors. Monthly Weather Review, Vol. 94, No. 4, 1966, p. 25964. [Detailed study of accuracy under Antarctic conditions.]2.3.CO;2>CrossRefGoogle Scholar
Jochimsen, M. 1st die Grösse des Flechtenthallus wirklich ein brauchbarer Masstab zur Datierung von glazial-morphologischen Relikten? Geograflska Annaler, Vol. 48a, No. 3, 1966, p. 15764. [Critical assessment of lichenometrical method for dating moraines. English summary.]CrossRefGoogle Scholar
Magono, C. Tazawa, S. Design of “snow crystal sondes”. Journal of the Atmospheric Sciences, Vol. 23, No. 5, 1966, p. 61825. [Apparatus to observe vertical distribution and crystal shapes in a cloud. Results confirm Nakaya’s diagram of expected shapes.]2.0.CO;2>CrossRefGoogle Scholar
Matsuo, S. Miyake, Y. Gas composition in ice samples from Antarctica. Journal of Geophysical Research, Vol. 71, No. 22, 1966, p. 523541. [Chemical] composition of gas in ice was determined for iceberg ice, glacier ice, sea ice and pond ice. From results, ice is classified into four types.]CrossRefGoogle Scholar
Oelsner, C. Seismoakustik, eine neue Messmethode für die Gletschermechanik. Polarforschung, Bd. 6, Jahrg. 35, Ht. 1–2, 1965 [pub. 1967], p. 1927. [Observations of seismo-acoustic waves in Lovenbreen, Vestspitsbergen, correlated with flow of glacier stream and jerky slip of glacier on its bed.]Google Scholar
Philberth, K. Eine Schmelzsonde zur Messung des Temperaturprofils in Eiskalotten. Umschau in Wissenschaft und Technik, Jahrg. 1966, Ht. 11, p. 360. [A hotpoint instrument for temperature measurement of ice.]Google Scholar
Schönbächler, M. Zur Albedomessung auf Gletschern. Archiv, für Meteorologie, Geophysik und Bioklimatologie, Ser. 13, Bd. 14, Ht. 2, 1966, p. 18488. [Comparison ofsolarimeter and selenium photoelement. English and French summaries.]CrossRefGoogle Scholar
Schwerdtfecer, P. Weller, G. The measurement of radiative and conductive heat transfer in ice and snow. Archie für Meteorologie, Geophysik und Bioklimatologie, Ser. B, Bd. 15, Ht. 1–2, 1967, p. 2438. [Importance of radiative transfer in upper layers. Development of instruments to measure both terms. French and German summaries.]CrossRefGoogle Scholar

Physics of ice

Bertie, J. E. Whalley, E. Optical spectra of orientationally disordered crystals. II. Infrared spectrum of ice Ih and ice le from 360 to 50 cm−1 . Journal of Chemical Physics, Vol. 46, No. 4, 1967, p. 127184. [Observation of spectra and their interpretation including discussion of effect of proton disorder.]CrossRefGoogle Scholar
Bigg, E. K. Giutronich, J. Ice nucleating properties of meteoritic material. Journal of the Atmospheric Sciences, Vol. 24, No. 1, 1967, p. 4649. [Attempt to duplicate processes by which meteors disintegrate and estimate the effectiveness of resulting particles as ice nuclei.]2.0.CO;2>CrossRefGoogle Scholar
Blicks, H., and others. Diffusion von Protonen (Tritonen) in reinen und dotierten Eis-Einkristallen, [von] H. Blicks, O. Dengel und N. Riehl. Physik der kondensierten Materie, Bd. 4, Ht. 5, 1966, p. 37581. [Measurement of diffusion of tritium in ice.]Google Scholar
Brepson, R. Premiers résultats obtenus avec le viscomètee à glace de Grenoble. Comptes Rendus Hebdomadaires des Séances de l’Académie des Sciences (Paris), Sér. B, Tom. 263, No. 15, 1966, p. 87679. [Description of the Grenoble ice viscometer and first results for friction of ice.]Google Scholar
Brown, A. J. Whalley, E. Preliminary investigation of the phase boundaries between ice VI and VII and ice VI and VIII. Journal of Chemical Physics, Vol. 45, No. 11, 1966, p. 436061.CrossRefGoogle Scholar
Brownscombe, J. L. Mason, B. J. Measurement of the thermoelectric power of ice by an induction method. Philosophical Magazine, Eighth Ser., Vol. 14, No. 131, 1966, p. 103747. [Description of method requiring no contact electrodes. Results compared with Jaccard’s theory.]CrossRefGoogle Scholar
Cubiotti, G. Geracitano, R. Ferroelectric behaviour of cubic ice. Physics Letters, Vol. 24a, No. 3, 1967, p. 17980. [Cubic ice is ferroelectric with Curie point at c. −80°C.]CrossRefGoogle Scholar
Dass, N. Gilra, N. K. Refractive index of liquids on supercooling-water. Journal of the Physical Society of Japan, Vol. 21, No. 10, 1966, p. 203942. [Suggests that measurements may give improved value for water-ice interfacial free energy.]CrossRefGoogle Scholar
Defrain, A. Linh, N. T. Détection par diffraction des rayons X et par analyse thermioue différentielle de la glace et du phénol amorphes. Comptes Rendus Hebdomadaires des Séances de l’Académie des Silences (Paris), Sér. C, Tom. 263, No. 22, 1966, p. 133639. [X-ray and differential thermal analysis used to study formation of amorphous ice and its transformation into ice 1h and 1c.]Google Scholar
Dillard, D. S. Timmerhaus, K. D. Low temperature thermal conductivity of solidified H2O and D2O. Pure and Applied Cryogenics, Vol. 4, 1966. p. 3544. [Results of measurements 100°K. to 253°K. French summary.]Google Scholar
Drake, J. C. Mason, B. J. The melting of small ice spheres and cones. Quarterly Journal of the Royal Meteorological Society, Vol. 92, No. 394, 1966, p. 50009. [Times of melting measured and compared with theory.]CrossRefGoogle Scholar
Dupuy, D. Calorimètre à flux de froid constant pour la mesure absolue de l’eau liquide incluse dans la glace tempérée. Comptes Rendus Hebdomadaires des Séances de l’Académie des Sciences (Paris), Sér. B, Tom. 263, No. 9, 1966, p. 63839. [Description of instrument to determine absolute value of liquid water content of ice calorimetrically.]Google Scholar
Evans, L. F. Ice nucleation by amino acids. Journal of the Atmospheric Sciences, Vol. 23, No. 6, 1966, p. 75152.[Detailed study of behaviour of certain amino-acids in cloud chambers and in supercooled droplets.]2.0.CO;2>CrossRefGoogle Scholar
Evans, L. F. Two-dimensional nucleation of ice. Nature, Vol. 213, No. 5074, 1967, p. 38485. [The first stage in the nucleation of ice on organic nucleators is the growth of monolayer patches of ice on the nucleator surface.]CrossRefGoogle Scholar
Fletcher, N. H. The freezing of water. Science Progress, Vol. 54, No. 214, 1966, p. 22741. [Review of recent progress in ideas of how water freezes.]Google Scholar
Ghormley, J. A. Adsorption and occlusion of gases by the low-temperature forms of ice. Journal of Chemical Physics, Vol. 46, No. 4, 1967, p. 132125. [Observations on amorphous and cubic ice.]CrossRefGoogle Scholar
Gokhale, N. R. Time dependence of heterogeneous nucleation. Journal of Geophysical Research, Vol. 71, No. 14, 1966, p. 335156. [Laboratory study. Complex behaviour found during initial freezing and interpreted in terms of dependence of freezing temperature on rate of cooling.]CrossRefGoogle Scholar
Hall, P. G., and others. The adsorption of water vapour by lead iodide, [by] P. G. Hall, L. Glasser and D. D. Liebenberg. Surface Science, Vol. 5, No. 3, 1966, p. 30915. [Study of adsorption isotherm and dielectric properties. Ice nucleating properties of Pblr discussed in connection with dielectric ordering.]CrossRefGoogle Scholar
Hindman, E. E. jr. The phase change in an artificial supercooled cloud upon heterogeneous and homogeneous nucleation. Journal of the Atmospheric Sciences, Vol. 23, No. 1, 1966, p. 6773. [Cloud chamber studies.]2.0.CO;2>CrossRefGoogle Scholar
Hobbs, P. V. Burrows, D. A. The electrification of an ice sphere moving through natural clouds. Journal of the Atmospheric Sciences, Vol. 23, No. 6, 1966, p. 75763. [Measurements made by whirling ice sphere in natural clouds and snowfall.]2.0.CO;2>CrossRefGoogle Scholar
Ida, M., and others. Dielectric dispersion of impure ice at low temperatures, by M. Ida, N. Nakatani, K. Imai and S. Kawada. Science Reports of Kanazawa University, Vol. 11, No. 1, 1966, p. 1322. [Many different impurities used. Some gave dielectric dispersion below −100°C. while others did not.]Google Scholar
Itagaki, K. Self-diffusion in single-crystal ice. Journal of the Physical Society of Japan, Vol. 22, No. 2, 1967, p. 42731.[Tritium tracer method used. Activation energy measured to be higher perpendicular to basal plane.]CrossRefGoogle Scholar
Kamb, W. B., and others. Structure of ice V, by [W.] B. Kamb, A. Prakash and C. Knobler. Acta Cryslallographica, Vol. 22, Pt. 5, 1967, p. 70615. [Detailed report of determination of structure of ice V.]CrossRefGoogle Scholar
Latham, J. Stow, C. D. The distribution of charge within ice specimens subjected to linear and non-linear temperature gradients. Quarterly Journal of the Royal Meteorological Society, Vol. 93, No. 395, 1967, p. 12125. [Theory which accounts for reported dependence of the thermoelectric effect in ice.]CrossRefGoogle Scholar
Macklin, W. C. Payne, G. S. A theoretical study of the ice accretion process. Quarterly Journal of the Royal Meteorological Society, Vol. 93, No. 396, 1967, p. 195213. [Study of the assumptions underlying the simple heat balance relations hitherto used to predict the surface temperatures of ice deposits being formed by the accretion of supercooled water droplets.]CrossRefGoogle Scholar
Maybank, J. Barthakur, N. The ice nucleation behaviour of amino-acid particles. Canadian Journal of Physics, Vol. 44, No. 10, 1966, p. 243145. [Evidence that below −20°C. some nuclei can act when not supersaturated with respect to supercooled water, i.e. as true sublimation nuclei.]CrossRefGoogle Scholar
Michaels, A. S., and others. Impurity effects on the basal plane solidification kinetics of supercooled water, by A. S. Michaels, P. L. T. Brian and P. R. Sperry. Journal of Applied Physics, Vol. 37, No. 13, 1966, p. 464961. [Measurements of growth rate for pure water and dilute solutions of ionic salts.]CrossRefGoogle Scholar
Proctor, T. M. jr. Low-temperature speed of sound in single-crystal ice. Journal of the Acoustical Society of America, Vol. 39, No. 5, Pt. 1, 1966, p. 97277. [Measurement of all single-crystal elastic constants down to 65°K.]CrossRefGoogle Scholar
Ramseier, R. O. Zone-melting apparatus for growing ice crystals. Materials Research Bulletin, Vol. 1, No. 4, 1966, p. 29397. [A zone-melting apparatus using an infrared heat lamp is described. Ice monocrystals can be grown from a polycrystalline charge without using a single-crystal seed.]CrossRefGoogle Scholar
Seeger, A. Wobser, G. Anordnung paralleler Versetzungen in anisotropen Medien. Physica Status Solidi, Vol. 17, No. 2, 1966, p. 70924. [Calculation of stable configurationsof dislocations usinganisotropic elasticity. Can be applied to ice.]CrossRefGoogle Scholar
Shubin, V. N., and others. Pulse radiolysis of crystalline ice and frozen crystalline aqueous solutions, [by] V. N. Shubin, V. A. Zhigunov, V. I. Zolitarevskiy [and] P. I. Dolin. Nature, Vol. 212, No. 5066, 1966, p. 1002, 1035. [Letter. Results for ice and frozen LiClO4 and KOH solutions not in agreement with solvated electron theory.]CrossRefGoogle Scholar
Siegel, S. Rennick, R. Isotope effects in the 77°K γ irradiation of ice. Journal of Chemical Physics, Vol. 45, No. 10, 1966, p. 371220. [Mass spectroscopy study of yield of H2, D2, and HD when H2O−D2O mixtures are irradiated.]CrossRefGoogle Scholar
Thomann, H. Size of ice crystals formed during rapid expansion of humid air. Physics of Fluids, Vol. 9, No. 5, 1966, p. 896902. [Measurement by measuring humidity of samples sucked into small pitot tubes.]CrossRefGoogle Scholar
Whalley, E., and others. Dielectric properties of ice VII. Ice VIII: a new phase of ice, by E. Whalley, D. W. Davidson and J. B. R. Heath. Journal of Chemical Physics, Vol. 45, No. 11, 1966, p. 397682. [Study of dielectric properties of ice VII and observation that at about 0°C. it transforms to a phase whose molecules are orientationally immobile to be called ice VIII.]CrossRefGoogle Scholar
Yang, L. C. Good, W. B. Crystallization rate of supercooled water in cylindrical tubes. Journal of Geophysical Research, Vol. 71, No. 10, 1966, p. 246569. [Observation of factors affecting this and attempt to explain them. Comments by C. A. Knight and reply by authors, ibid., Vol. 71, No. 24, 1966, p. 6145–49.]CrossRefGoogle Scholar
Yuferov, V. B. Busol, F. I. Issledovaniye sorbtsii vodoroda i neona sloyami skondensirovannykh tverdykh gazov . Zhurnal Tekhnicheskoy Fiziki , Tom 36, Vyp. 11, 1966, p. 204250. [Includes adsorption on ice at Iq.° to 20°K. English translation: Soviet Physics—Technical Physics, Vol. 11, No. 11, 1967, p. 1518–241Google Scholar

Land ice. Glaciers. Ice shelves

Ambach, W. Awecker, P. Zur Lichtstreuung im Gletschereis. Archiv far Meteorologic, Geophysik und Bioklimatologie, Ser. B, Bd. 15, Ht. 1–2, 1967, p. 17585. [Theory of extinction of light in glacier ice and of variation of albedo with angle. English and French summaries.]CrossRefGoogle Scholar
Aver’yanov, V. G., ed. Glyatsiologicheskiye issledovaniya v rayon stantsii Novolazarevskoy. Metodika i materialy nablyudeniy . Leningrad, Arkticheskiy i Antarkticheskiy Nauchno-IssIedovatel’skiy Institut [Arctic and Antarctic Research Institute], 1966. 53 p. [Snow and firn temperatures, snow accumulation, directions of striae; observed in 1963–64 in Dronning Maud Land.]Google Scholar
Bauer, A. Le bilan de masse de l’lndlandsis du Groenland n’est pas positif. Bulletin de l’Association Internationale d’Hydrologie Scientifique, 11e An., No. 4, 1966, p. 812. [According to recent calculations the mass budget is negative and recent observations bear out this conclusion.]CrossRefGoogle Scholar
Bauer, A. Nouvelle estimation du bilan de masse de l’Indlandsis du Groenland. Deep Sea Research, Vol. 14, No. 1, 1967, p. 1317. [Greenland ice sheet mass balance is negative with an amount of water equivalent of −100 km3/yr. Recent data on retreat of Greenland ice sheet are given.]Google Scholar
Beitzel, J. E., and others. Geophysical studies on the South Pole-Queen Maud Land traverse, Il, by J. E. Beitzel, J. W. Clough and C. R. Bentley. Antarctic Journal of the U.S., Vol. 1, No. 4, 1966, p. 13233. [Ice surface elevations along the traverse route determined, radio-frequency depth measurements made, velocity determinations by wide-angle reflection technique attempted.]Google Scholar
Bergeron, T. The possible role of snowdrift in building up high inland ice-sheets. Progress in Oceanography, Vol. 3, 1965, p. 38590. [Of the accumulation near the centre of Greenland only a minority can be due to true snowfall from clouds.]CrossRefGoogle Scholar
Brockamp, B. Über einige geophysikalische Ergebnisse der internationalen Grönland-Expedition ECIG 1959. Polarforschung, Bd. 6, Jahrg. 35, Ht. 1–2,1965 [pub. 1967], p. 4266. [Summary of EGIG results in 1959 on surface profile and seismic and gravity observations. English summary.]Google Scholar
Brockamp, B. Kohnen, H. Ein Beitrag zu den seismischen Untersuchungen auf dem grönländischen Inlandeis. Polarforschung, Bd. 6, Jahrg. 35, Ht. 1–2,1965 [pub. 1967], p. 212. [Compressional and shear wave velocities from seismic records of EGIG 1959 used to derive elastic constants for ice. Temperature dependence of the velocities is discussed. English summary.]Google Scholar
Deutsch, S., and others. Oxygen isotope study of snow and firn on an alpine glacier, by S. Deutsch, W. Ambach and H. Eisner. Earth and Planetary Science Letters, Vol. 1, No. 4, 1966, p. 197201. [Measurement of accumulation based on seasonal variations of oxygen isotope ratio appears to be unreliable.]CrossRefGoogle Scholar
Ek, C. Faible agressivité des eaux de fonte des glaciers: l’exemple de la Marmolada (Dolomites). Annales de la Société Géologique de Belgique. Bulletin, Tom. 89, No. 6, 1966, p. 17788. [Measurements of pH of melt water from glaciers in limestone area. Discussion, p. 186–88.]Google Scholar
Fristrup, B. The Greenland ice cap. København, Rhodos, 1966. 312 p. [History of exploration and summary of glaciological research. English translation, extended and brought up to date, of Danish original, Indlandsisen, København, 1963.]Google Scholar
Frolov, A. I. Gravitatsionnoye pole i stroyeniye podlednogo rel’yefa po transe Britansko-Novozelandskoy ekspeditsii . Akademiya Nauk SSSR. Izvestiya. Fizika Zemli , 1965, No. 9, p. 10913. [Discussion of errors in elevation data make gravity depths determined by Commonwealth Trans-Antarctic Expedition wrong; these data are re-interpreted. English translation in Izvestiya. Academy of Sciences, U.S.S.R. Physics of the Solid Earth, 1965, No. 9 [pub. 1966], P. 650–53.]Google Scholar
Giovinetto, M. B. Schwerdtfeger, W. Analysis of a 200 year snow accumulation series from the South Pole. Archiv für Meteorologie, Geophysik und Bioklimaeologie, Ser. A, Bd. 15, Ht. 2, 1966, p. 22750. [Identification of annual layers, discussion of accuracy, search for secular and periodic variations.]CrossRefGoogle Scholar
Govorukha, L. S. Novyye glyatsiologicheskiye issledovaniya na Seversoy Zemle . Materialy Glyaisiologicheskikh Issledovaniy. Khronika. Obsuzhdeniya , 12, 1966, p. 5052. [Work in summer of 1965.]Google Scholar
Grove, J. M. The Little Ice Age in the massif of Mont Blanc. Institute of British Geographers. Transactions, No. 40, 1966, p. 12943. [Glacier fluctuations in historical times.]CrossRefGoogle Scholar
Gus’kov, A. S. Khodakov, V. G. Osobennosti formirovaniya veshchestvennogo balansa lednikov Polyarnogo Urala V 1964–65 byudzhetnom godu . Materialy Glyaisiologicheskikh Issledovaniy. Khronika. Obsuzhdeniya , 12, 1966, p. 26567.Google Scholar
Hattersley-Smith, G. Note on ice shelves off the north coast of Ellesmere Island. Arctic Circular, Vol. 17, No. 1, 1965–66 [pub. 1967], p. 1314. [Further break-up since massive calving from Ward Hunt Ice Shelf in winter of 1961–62.]Google Scholar
Hochstein, M. Morphologie der westantarktischen Eiskappe zwischen Mary-Byrd- [sic] und Edith-Ronne-Land. Polarforschung, Bd. 6, Jahrg. 33, Ht. 1–2,1965 [pub. 1967], p. 2731. [Morphology of surface and bed of the Western Antarctic ice sheet between Marie Byrd Land and Fechner Ice Shelf.]Google Scholar
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Kick, W. Schlagintweits Vermessungsarbeiten am Nanga Parbat 1856. Deutsche Geodätische Kommission, Reihe C, Nr. 97, 1967, 146 p. [Includes glacier mapping and descriptions of measurements of ice velocity in 1856 and 1934; situation of moraines and results for determinations of glacier variations in general.]Google Scholar
Konecny, G. Faig, W. Studies of ice movements on the Ward Hunt Ice Shelf by means of triangulationtrilateration. Arctic, Vol. 19, No. 4, 1966, p. 33742. [Shelf ice movements of 30 cm. with respect to solid ground were obtained between 1964 and 1965. The relative position change between markers on shelf ice was less than 4 cm.]CrossRefGoogle Scholar
Law, P. Movement of the Amery Ice Shell Polar Record, Vol. 13, No. 85, 1967, p. 43941. [On 13 January 1965, the crew of a Soviet aircraft reported that the ice front of the shelf was roughly 80 to 100 km. further south than shown on the map.]CrossRefGoogle Scholar
Leós, Á. Íshellir I Hattardal. Jökull, [Vol.] 3, Ár. 15, 1965, p. 12124. [Observations of ice cave at Hattardalur, north-west Iceland, in 1963–65.]CrossRefGoogle Scholar
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Icebergs. Sea, river and lake ice

Adams, W. P. Shaw, J. B. Improvements in the measurement of a lake ice cover. McGill Sub-Arctic Research Papers, No. 21, 1966, p. 19194. [Suggested procedure in measurement of white ice and snow depth, black ice, and hydrostatic water level.]Google Scholar
Adams, W. P., and others. The bathymetry and ice cover of lakes in the Schefferville area, by W. P. Adams, J. B. Shaw and D. R. Archer. McGill Sub-Ardic Research Papers, No. 21, 1966, p. 20112. [Preliminary presentation of data. Further data should considerably improve knowledge of ice growth in the area and provide a firm basis for a detailed analysis of the many years of ice measurements filed.]Google Scholar
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Archer, D. R. Findlay, B. R. Comments on littoral ice conditions at one site at Knob Lake, April 1965. McGill Sub-Arctic Research Papers, No. 21, 1966, p. 18990. [Conditions near margin of ice sheet varied greatly. A difference in ice surface levels of 4.8 inches (13 cm.) was calculated.]Google Scholar
Bellair, P. Icebergs sur les côtes de Kerguelen. TAAF (Territoire des Terres Australes et Antarctiques Françaises), No. 34, 1966 , p. 38 . [General description.] Google Scholar
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Glacial geology

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Frost action on rocks and soil. Frozen ground. Permafrost

Arnborg, L., and others. Water discharge in the Colville River 1962, by L. Arnborg, H. J. Walker and J. Peippo. Geografiska Annaler, Vol. 48a, No. 4, 1966, p. 195210. [Hydrological characteristics of the surface drainage in an area of continuous permafrost on the Arctic slope.]CrossRefGoogle Scholar
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Seppälä, M. Recent ice-wedge polygons in eastern Enontekiö. northernmost Finland. Reports from the Kevo Subarctic Research Station (Turku), 3, 1966. p. 27487. [Observations in 1965.]Google Scholar
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Worsley, P. Fossil frost wedge polygons at Congleton, Cheshire, England. Geografiska Annaler, Vol. 48a, No. 4, 1966, p. 21119. [Observation of a form rarely exposed in temperate latitudes. Origin and age discussed.]CrossRefGoogle Scholar

Meteorological and climatological glaciology

Goldthwait, R. P. Evidence from Alaskan glaciers of major climatic changes. (In World climate from 8000 to 0 B.C. Proceedings of the international symposium held at Imperial College, London, 18–19 April 1966. London, Royal Meteorological Society, 1966, p. 4053.) [Includes close of Wisconsin glaciation, Hypsithermal period, early Neoglacial time, and later Neoglacial, and the Little Ice Age.]Google Scholar
Hallett, J. Charge separation and the growth of hail. Weather, Vol. 22, No. 2, 1967, p. 80. [Letter.]Google Scholar
Karbaum, H., and others. Deutsche Spitzbergen Expedition 1962. Hydrometeorologische Arbeiten am mittleren Lovéngletscher in der Kingsbay. [By] H. Karbautn, H. Schmidt, W. Schöne, R. Wiedrich. Nationalkomitee fair Geodäsie and Geophysik der Deutschen Demokratischen Republik bei der Deutschen Akademie der Wissenschaften zu Berlin, Reihe 3, Ht. 2, 1966, 101 p. [Hydrometcorological measurements at middle Lovenbreen, Vestspitsbergen, 1962. Topographical map, scale 1: 10,000.]Google Scholar
Koenig, L. R. Numerical test of the validity of the drop-freezing/spLintering hypothesis of cloud glaciation. Journal of the Atmospheric Sciences, Vol. 23, No. 6, 1966, p. 72640. [Numerical experiment using computer to see whether mechanism is important.]2.0.CO;2>CrossRefGoogle Scholar
Manley, G. The problem of the climatic optimum: the contribution of glaciology. (In World climate from 8000 to 0 B.C. Proceedings of the international symposium held at Imperial College, London, 18–19 April 1966. London, Royal Meteorological Society, 1966, p. 3439.)Google Scholar
Parker, G. Harrison, A. A. Freezing drizzle in south-east England on 20 January 1966. Meteorological Magazine, Vol. 96, No. 1137, 1967, p. 10812. [Freezing drizzle coated the greater part of southern England with a thin skin of ice and the opportunity was taken to investigate its effects in as many fields as possible.]Google Scholar
Stewart, J. B. A preliminary study of the occurrence of ice crystals in layer clouds. Meteorological Magazine, Vol. 96, No. 1134, 1967, p. 2327. [Flights to investigate occurrence of ice crystals in layer clouds.]Google Scholar
Vinje, T. E. Some results of micrometeorological measurements in Antarctica. Archie far Meteorologie, Geophysik and Bioklimatologie, Ser. A, Bd. 16, Ht. 1, 1967, p. 3143. [”Norway” station, Antarctica. Results suggest sensible heat enters snow by permeation of air. Eddy heat transfer coefficient calculated. French and German summaries.]CrossRefGoogle Scholar
Wexler, R. Donaldson, R. J. jr. The spread of ice in cumulus clouds. Journal of the Atmospheric Sciences, Vol. 23, No. 6, 1966, p. 75356. [Theoretical study based on Bigg’s criterion of droplet freezing.]2.0.CO;2>CrossRefGoogle Scholar

Snow

Adams, W. P. Findlay, B. F. Snow measurement in the vicinity of Knob Lake, central Labrador-Ungava, winter 1964–65. Proceedings of the Eastern Snow Conference, 23rd annual meeting, 1966, p. 2640. [Part of hydrologic study carried out by McGill Sub-Arctic Research Laboratory.]Google Scholar
Adams, W. P., and others. Snowfall and snowcover at Knob Lake, central Labrador-Ungava, by W. P. Adams, W. R. Cowan, B. F. Findlay, J. S. Gardner and R. J. Rogerson. McGill Sub-Arctic Research Papers, No. 22, 1966, p. 11440. [Amount and character of snowfall in area, variations in snow cover on ground, and developments within snow cover, each winter, discussed for period 1954–66.]Google Scholar
Akkuratov, V. N. Meteorologicheskiye usloviya obrazovaniya lavin v Khibinaka . Materialy Glyatsiologicheskikh Issledovaniy. Khronika. Obsuzhdeniya , 12, 1966. p. 13238.Google Scholar
Bryukhanov, A. V. O mekhanizme dvizheniya snezhnykh lavin . Vestnik Moskovskogo Universiteta. Seriya 5. Geografiya , 1966, No. 2, p. 9296. [Experiments with stereoscopic photography.]Google Scholar
Cowen, R. Snow survey at Schefferville 1964–65. McGill Sub-Arctic Research Papers, No. 21, 1966, p. 13545. [Distribution of snow was similar to patterns described in previous years.]Google Scholar
Drigo, A., and others. Misure dell’equivalente in acqua del manto nevoso col metodo dell’assorbimento dei raggi gamma, effettuate alla Fedaja (Marmolada) nel 1959–60 a nel 1960–61, [by] A. Drigo, A. Cecchetti, G. Fratucello. Bollettino del Comitato Glaciologico Italian, 2 Ser., No. 11, Pt. 2, 1860–61, [pub.] 1965, p. 5356. [Measurement of water equivalent of snow around Lao della Fedaja by means of gamma ray absorption.]Google Scholar
Fukuta, N. Activation of atmospheric particles as ice nuclei in cold and dry air. Journal of the Atmospheric Sciences, Vol. 23, No. 6, 1966, p. 74150. [Possibility that ice in micro-capillaries in atmospheric particles may exist in equilibrium with a dry atmosphere.]2.0.CO;2>CrossRefGoogle Scholar
Haupt, H. F. Infiltration, overland flow, and soil movement on frozen and snow-covered plots. Water Resources Research, Vol. 3, No. 1, 1967, p. 14561. [Snow cover, by cooling rain-water, tends to preserve soil frost and keep it visibly intact. Snow absorbs raindrop energy much as dense vegetation does.]CrossRefGoogle Scholar
Houghton, D. M. Snow and ice puzzles. Weather, Vol. 22, No. 5, 1967, p. 187. [Explanation of uneven thawing of snow on a lawn, shown in photograph in Weather, Vol. 21, No. 12, 1966, p. 446–47.]Google Scholar
Latham, J. Stow, C. D. A laboratory investigation of the electrification of snowstorms. Quarterly Journal of the Royal Meteorological Society, Vol. 93, No. 395, 1967, p. 5568. [Artificial snowstorms created inside a large cold room by blowing snow crystals over a snow surface.]CrossRefGoogle Scholar
Leaf, C. F. Free water content of snowpack in subalpine areas. Proceedings of the Western Snow Conference, 34th annual meeting, 1966, p. 1724. [Summarizes detailed observations made in Colorado.]Google Scholar
Mustonen, S. E. Ilmasto- ja maastotekijöiden vaikutuksesta lumen vesiarvoon ja roudan syvyyteen. Acta Forestalia Fennica, 79, 1, 1965, [pub.] 1966, 40 p. [Effect of meteorological and terrain factors on water equivalent of snow cover and on frost depth. English summary.]CrossRefGoogle Scholar
Pedgley, D. E. The shapes of snowdrifts. Weather, Vol. 22, No. 2, 1967, p. 4248.CrossRefGoogle Scholar
Popham, R. W., and others. Second progress report on satellite applications to snow hydrology, by R. W. Popham, A. F. Flanders and H. Neiss. Proceedings of the Eastern Snow Conference, 23rd annual meeting, 1966, p. 10919. [Possibility discussed of forecasting water supply from snow cover on mountains from observations made by Nimbus and TIROS meteorological satellites.]Google Scholar
Potter, J. G. Snow cover. Canada. Department of Transport. Meteorological Branch. Climatological Studies, No. 3, 1965, 69 p. [All available data of snow cover, not snowfall, from the various weather observing stations in Canada.]Google Scholar
Zanon, G. Ricerehe suila neve in Francia e in Svizzera. Osservazioni e prospettive delle ricerche nivometriche in Italia. Bollettino del Comitato Glaciologico Italiano, 2 Ser., No. 11, Pt. 2, 1960–61, [pub.] 1965, p. 5780. [Comparison of snow cover studies in France, Switzerland and Italy and suggested modifications in methods used in Italy. English summary, p. 79.]Google Scholar