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Glaciological Literature

Published online by Cambridge University Press:  30 January 2017

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Copyright © International Glaciological Society 1969

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

References

General Glaciology

Hansen, J. E. Cheyney, H. Near infrared reflectivity of Venus and ice clouds. Journal of the Atmospheric Sciences, Vol. 25, No. 4, 1968, p. 62933. [Observations compatible with optically thin clouds of ice particles while not conclusively proving this.]2.0.CO;2>CrossRefGoogle Scholar
Wright, H. E. jr. Osburn, W. H., ed. Archie and alpine environments. Washington, D.C., [U.S.] National Academy of Sciences and National Research Council, 1968. 308 p. [Includes the following papers: L. A. Viereck, “Botanical dating of recent glacial activity in western North America”, p. 189–204; P. Clement and J. Vaudour, “Observations on the pH of melting snow in the southern French Alps”, p. 205–13; J. M. Soons, “Erosion by needle ice in the Southern Alps, New Zealand”, p. 217–27; E. Schenk “Fundamental processes of freezing and thawing in relation to the development of permafrost”, p. 229–36; E. M. Katasonov. “Features of deposits formed under permafrost conditions”, p. 237–40; D. L. Linton, “Divide elimination by glacial erosion”, p. 241–48; T. Pippan, “Tectonic and lithologic control on trough and cirque features in Caledonian, Hercynian, and Alpine mountains of Europe”, p. 249–54; F. Taillefer, “Extent of Pleistocene glaciation in the Pyrenees”, p. 255–66; 1. P. Gerasimov and R. P. Zimina, “Recent natural landscapes and ancient glaciation of the Pamir”, p. 267–69; D. S. Simonett and S. A. Morain, “Remote sensing from spacecraft as a tool for investigating Arctic environments”, p. 295–306.]Google Scholar

Glaciological Instruments and Methods

Pal’gov, N. N. K voprosu o metode balansov po opredeleniyu moshchnosti gornykh lednikov . Izuestiya Vsesoyuznogo Geograflcheskogo Obshchestva, Tom 99, Vyp. 2, 1967, p. 14244. [Further explanation of author’s method, which uses geometrical means to produce approximate values.]Google Scholar
Ueda, H. T. Hansen, B. L. Installation of deep-core drilling equipment at Byrd station (1966–1967). Antarctic Journal of the United States, Vol. 2, No. 4, 1967, p. 12021. [Details of equipment which bored 227 m into the ice.]Google Scholar

Physics of Ice

Anderson, D. M. Undercooling, the freezing point depression, and ice nucleation of soil water. Israel journal of Chemistry, Vol. 6, No. 3, 1968, p. 34955. [Experimental results and discussion of nature of heterogeneous nucleation of ice near silicate surfaces in light of knowledge of water-like surface layer.]CrossRefGoogle Scholar
Barnaal, D. E. Lowe, I. J. Proton spin-lattice relaxation in hexagonal ice. Journal of Chemical Physics, Vol. 48, No. 10, 1968, p. 461408, [Measurement of relaxation time and its activation energy (59.0±0.4 kJ/mole) which does not agree with that for dielectric relaxation.]CrossRefGoogle Scholar
Berg, T. G. O., and others. Conversion of water vapor to ice by silver iodide, by T. G. O. Berg, J. E. Clutter, T. A. Gaukler, R. L. McDonald. Journal of the Atmospheric Sciences, Vol. 25, No. 3, 1968, p. 46469. [Experiments showing that water vapour first condenses and then freezes.]Google Scholar
Beukel, A. van den. Specific heat of ice near the “ferroelectric” transition temperature. Physica Status Solidi, Vol. 28, No. 2, 1968, p. 56568. [Two peaks observed in specific heat of HF-doped ice at 104° K and 132° K.]CrossRefGoogle Scholar
Burgman, J. O., and others. Proton dynamics in water and ice studied by inelastic scattering of slow neutrons, [by] J. O. Burgman and J. Sciesinski and K. Sköld. Physical Review, Second Ser., Vol. 170, No. 3, 1968, p. 80817. [Spectra of water and ice are significantly different.]Google Scholar
Dantl, G. Gregora, I. Dichte in hexagonalem Eis. Naturwissenschaften, Bd. 55, Ht. 4, 1968, p. 176. [Measurements to 5-figure accuracy. Newly frozen ice is denser than aged ice.]Google Scholar
Deryagin, B. V. Effect of lyophile surfaces on the properties of boundary liquid films. Discussions of the Faraday Society, No. 42, 1966 [c1967], p. 10919, 134–42. [Study of properties of water in boundary layers on quartz and glass show anomalies which are interpreted as showing that the usual state of water is metastable and that the stable state is denser. It does not freeze to ordinary ice. Discussion, p. 134–42.]Google Scholar
Gilra, N. K. Dass, N. Precrystallization theory applied to surface free energy of the water-ice interface. Journal of the Physical Society of Japan, Vol. 24, No. 4, 1968, p. 91012. [To obtain agreement with data on refractive index, density and viscosity of supercooled water a new set of data for surface free energy of the solid-liquid interface is needed.]CrossRefGoogle Scholar
Gromova, T. N., and others. Vliyaniye primesey poverkhnostno-aktivnykh veshchestv na l’doobtazuyushchuyu effektivnost’ rastvorov floroglyutsina, iodistogo serebra i iodistogo svintsa . Trudy Glavnoy Geofizicheskoy Observatorii im. A. I. Voyeykova (Leningrad), Vyp. 186, 1966, p. 1825. [Adding these substances lowers freezing temperature by several degrees.]Google Scholar
Hardy, S. C. Coriell, S. R. Morphological stability of a growing cylindrical crystal of ice. Journal of Applied Physics, Vol. 39, No. 7. 1968, p. 350507. [Experimental study of growth of ice cylinder with axis parallel to c-axis at low supercooling, and of radius at which cylindrical shape is unstable.]CrossRefGoogle Scholar
Holzapfel, W. Drickamer, H. G. Effect of pressure on the volume of the high-pressure (VII) phase of H2O and D2O. Journal of Chemical Physics, Vol. 48, No. 10, 1968. p. 4798800. [Measurement of X-ray lattice parameters up to 50 kbar.]Google Scholar
Itagaki, K. Electric field effect on creeping ice single crystals. Bulletin of the American Physical Society, Ser. 2, Vol. 13, No. 3, 1968, p. 367. [Abstract only. Bending creep of pure and HF-doped ice single crystals increased by about 10 to 20% when electric field of 600 V/cm r.m.s. at 60 Hz is applied.]Google Scholar
Jindal, B. K. Tiller, W. A. On electrostatic potentials at the ice/water interface. Surface Science, Vol. 9, No. 2, 1968, p. 13744. [Theory of formation of surface potential difference and comparison with experiment.]CrossRefGoogle Scholar
Kachurin, L. G. Gashin, L. I. O plotnosti i struktura l’da, rastushchego v potoke pereokhlazhdennogo aerozolya . Izvesiiya Akademii Nauk SSSR. Fizika Atmosfery i Okeana, Tom 4, No. 1, 1968, p. 9396. [Theory of formation of layered structure in hail. English translation in Izvestiya. Academy of Sciences, U.S.S.R. Atmospheric and Oceanic Physics. Vol 4, No 1, 1968, p 49–51.]Google Scholar
Kachurin, L. G., and others. Eksperimental’noye issledovaniye elektrokineticheskogo yavleniya, voznikayushchego pri kristallizatsii slabykh vodnykh rastvorov . Doklady Akademii Nauk SSSR, Tom 174, No. 5, 1967, p. 112225. (Study of potential difference between ice and water and dependence on freezing velocity and pH.]Google Scholar
Kamb, W. B. Ice polymorphism and the structure of water. (In Rich, A. Davidson, N., ed. Structural chemistry and molecular biology. San Francisco and London, W. H. Freeman and Co., [c 1968], p. 50742.) [Discussion of structure of water in the light of our knowledge of ice polymorphs.]Google Scholar
Kell, G. S. Whalley, E. Equilibrium line between ice I and III. Journal of Chemical Physics, Vol. 48, No. 5. 1968. p. 235961. [New studies show boundary to be nearly straight, thus removing evidence for an order-disorder transition.]Google Scholar
Khodzhayev, O. F., and others. Opticheskoye pogloshcheniye neytral’nogo kristallicheskogo l’da, y-obluchennogo pri –196° . Izvestiya Akademii Nauk SSSR. Seriya Khimiya, 1968, No. 2, p. 24649.Google Scholar
Mae, S. Void formation during non-basal glide in ice single crystals under tension. Philosophical Magazine. Eighth Ser., Vol. 18, No. 151, 1968, p. 10114. [Observation of void formation on crystals pulled perpendicular to c-axis. Explanation in terms of dislocation climb.]Google Scholar
Merlivat, L. Nief, G. Fractionnement isotopique lors des changements d’état solide-vapeur et liquide-vapeur de l’eau à des températures inférieures à 0° C. Tellus, Vol. 19, No. 1, 1967, p. 12227. [Measurement of fractionation of HDO relative to H2O when ice or supercooled water evaporates. English and Russian summaries.]Google Scholar
Morgan, G. M. jr. Allee, P. A. The production of potential ice nuclei by gasoline engines. Journal of Applied Meteorology, Vol. 7, No. 2, 1968, p. 24146. [Study of ice nuclei production when iodine is added to exhaust fumes from leaded automobile fuel.]Google Scholar
Nozik, A. J. Kaplan, M. Kinetics of the cubic-to-hexagonal phase transformation in ice doped with Mössbauer ions. Chemical Physics Letters, Vol. 1, No. 9, 1967, p. 39195. [Study of mechanism of transformation and activation energy. Dissolved ions decrease rate of transformation.]Google Scholar
Odencrantz, F. K., and others. Mechanism for multiplication of atmospheric ice crystals; apparent charge distribution on laboratory crystals, by F. K. Odencrantz, W. S. McEwan, P. St. Amand, W. G. Finnegan. Science, Vol. 160, No. 3834, 1968, p. 134546. [Replicas of ice crystals give evidence for existence of very fine whiskers and clustering caused by charge separation.]Google Scholar
Prask, H., and others. Frequency spectrum of hydrogenous molecular solids by inelastic neutron scattering: hexagonal H2O ice, [by] H. Prask and H. Boutin and S. Yip. Journal of Chemical Physics, Vol. 48, No. 8. 1968, p. 336776. [Measurements reported and used to deduce frequency distribution of thermal vibrations in ice.]Google Scholar
Radd, F. J. Oertle, D. H. Melting point behaviour of glacier ice. Nature, Vol. 218, No. 5148, 1968, p. 1242. [Letter. Discusses melting point of ice when melt water is unconfined. Observations of movement of clay particles through ice.]Google Scholar
Salomon, G. The friction and adhesion of ice. Wear, Vol. 11, No. t, 1968, p. 12. [Editorial article commenting on importance of results reported by H. H. Schulz and A. Knappworst, ibid., p. 320, and discussing physical implications.]Google Scholar
Schaefer, V. J. The generation of large numbers of ice crystals in an electric field. Journal of Applied Meteorology. Vol. 7, No. 3, 1968, p. 45255. [Observation of streamers of tiny ice crystals formed near wire with high d.c. charge.]Google Scholar
Schulz, H. H. Knappworst, A. Die Festkörperreibung des Eises als Relaxationseffekt. Wear Vol. 11. No. 1, 1968, p. 320. [Friction of ice on stainless steel studied from –170° C to 0° C. Results show variations of coefficient of friction that are anomalous. Discussion of this in terms of mechanical relaxation of ice. English summary.]Google Scholar
Shiloh, K. Sideman, S. Direct contact heat transfer with change of phase: evaporation rates in vacuum freezers. Canadian Journal of Chemical Engineering, Vol. 45, No. 5, 1967, p. 30005. [Factors affecting rate of evaporation from salt-water-ice slurries.]CrossRefGoogle Scholar
Stevenson, D. P. Molecular species in liquid water. (In Rich, A. Davidson, N., ed. Structural chemistry and molecular biology. San Francisco and London, W. H. Freeman and Co., [c 1968], p. 490506.) [Discussion of molecular processes involved in melting of ice.]Google Scholar
Van Hook, W. A. Vapor pressures of the isotopic waters and ices. Journal of Physical Chemistry, Vol. 72, No. 4. 1968, p. 123444. [Theory of isotope effect on vapour pressure.]Google Scholar
Whalley, E., and others. Ice IX: an anti-ferroelectric phase related to ice III, by E. Whalley. J. B. R. Heath and D. W. Davidson. Journal of Chemical Physics, Vol. 48, No. 5, 1968, p. 236270. [Dielectric measurements show decrease in permittivity attributable to ordering of hydrogen atoms.]Google Scholar
Yen, Y.-C. Onset of convection in a layer of water formed by melting ice from below. Physics of Fluids, Vol. 11, No. 6, 1968, p. 126370. [Experimental study to determine conditions for onset of convection.]Google Scholar
Young, I. G. Salomon, R. E. Dielectric behavior of ice with HCI impurity. Journal of Chemical Physics, Vol. 48, No. 4, 1968, p. 163544. [Results of measuring frequency and temperature dependence of conductivity, permittivity and relaxation time show that HCl dissolves substitutionally in ice at low concentra-t ions.]Google Scholar
Zimbrick, J. Kevan, L. Paramagnetic relaxation of trapped hydrogen atoms in irradiated frozen aqueous solutions. Journal of Chemical Physics, Vol. 47, No. 12, 1967. p. 500008. [Study of relaxation tinte, line width and line shape and interpretation in terms of trapping of hydrogen atoms at defect sites.]CrossRefGoogle Scholar

Land ice. Glaciers. Ice shelves

Barkov, N. I. Stroyeniye snezhno-firnovoy tolshchi v rayone stantsii Lazarev . Trudy Sovetskoy Antarklicheskoy Ekspeditsii, Tom 48, 1967, p. 14551. [Pit studies down to 35 m.]Google Scholar
Barnett, D. M. Development, landforms and chronology of Generator Lake, Biffin Island, N.W.T. Geographical Bulletin (Ottawa), Vol. 9, No. 3, 1967, p. 16988. [Study of past developments of this ice-dammed lake.]Google Scholar
Bauer, A. I.e glacier de. l’Eqe (Fqip Sermia). Mouvement et variations du front (1959). Meddelelser om Gronland, Bd. 174, Nr. 2, 1868, 21 p. [Accurate measurements of the glacier front and deduction of advance and retreat since 1912. English abstract.]Google Scholar
Bauer, A., and others. Missions aériennes de reconnaissance au Groenland 197–1958. Observations aériennes et terrestres, exploitation des photographies aériennes, détermination des vitesses des glaciers vêlant dans Disko Bugt et Umanak Fjord par A. Bauer avec la collaboration de M. Baussart, M. Carbonnell, P. Kasser, P. Perroud et A. Renaud. Meddelelser om Gronland, Bd. 173. Nr. 3. 1968, 116 p., 20 plates, 8 maps. [Detailed account of work donc by aerial reconnaissance to prepare for main expedition. Includes velocity measurements on 20 glaciers. English summary.]Google Scholar
Bauer, A., and others. Mouvement et variation d’altitude de la zone d’ablation ouest (latitude moyenne 69° 40′ N) de l’indlandsis du Groenland entre 1948 et 1959, par A. Bauer avec la collaboration de W. Ambach et O. Schimpp. Meddelelser om Gronland, Bd. 174, Nr. 1, 1968, 79 p. [Account of work in ablation zone of Greenland ice sheet. Details of methods used to determine movements and altitudes. English summary.]Google Scholar
Behrendt, J. C. Gravity increase at the South Pole. Science, Vol. 155, No. 3765, 1967, p. 101517. [Time variation of gravity and possible glaciological interpretation.]CrossRefGoogle ScholarPubMed
Bokanenko, L. I. Avsyuk, Yu. N. Rezul’taty seysmogravimetricheskikh issledovaniy na zemle Kornlevy Mod . Trudy Sovetskoy Antarkticheskoy Ekspeditsii, Tom 48, 1967, p. 10527. [Study of internal structure of ice as determined seismically.]Google Scholar
Bortenschlager, S. Pollenanalytische Ergebnisse einer firnprofiluntersuchung am Kesselwandferner (3240 m, ötztal, Tirol). Grana Palynalogica, Vol. 7, No. 1, 1967, p. 25974. [Pollen analysis used to identify ablation surfaces. Appendix by W. Ambach and H. Eisner on glaciological interpretation.]Google Scholar
Burrows, C. J. Lucas, J. Variations in two New Zealand glaciers during the past Boo years. Nature, Vol. 216, No. 5114, 1967, p. 46758. [Lichenometric measurements.]Google Scholar
Carbonnell, M. Bauer, A. Exploitation des couvertures photographiques aériennes répétées du front des glaciers vêlant dans Disko Bugt et Umanak Fjord, juin juillet 1964. I. Nouvelles mesures photogrammétriques de la vitesse superficielle des glaciers du Groenland par M. Carbonnell. II. Accélération de l’écoulement des glaciers groenlandais vers leur front et détermination de leur débit solide par A. Bauer. Meddelelser om Gronland, Bd. 173, Nr. 5. 1968, 78 p. [Repeated aerial photog:aphs of calving glaciers used to deduce ice velocities and discharge. English summary.]Google Scholar
Chizhov, O. P. Byudzhet massy lednikov na ostrovakh severo-vostochnoy Atlantiki po issledovaniyam v period MGG . Geoflzicheskiy Byllleten’, No. 19, 1968, p. 2433. [Analysis of long-term records of snow accumulation with mass budget data in Svalbard, Zemlya Frantsa-Iosifa, Novaya Zemlya and Severnaya Zemlya].Google Scholar
Chizhov, O. P., and others. Oledeneniye Novoy Zemli . Rezul’taty Issledovan y po Programme Mezhdunarodnogo Geofizicheskogo Goda. IX Razdel Programmy MGG, No. 18, 1968, 339 p. [Description of glaciers of Novaya Zemlya as studied by the 1957–59 I.G.Y. expedition. Includes climate, heat budget, accumulation and ablation, ice movement, mass budget and geological history of glaciation. Comparison with neighbouring glacierized regions. English summary.]Google Scholar
Dewart, G. Anvers Island gravity survey. 1967. Antarctic journal of the United Stases, Vol. 2, No. 4, 1967, p. 118. [Preliminary data indicate ice thickness > 500 m.]Google Scholar
Dorofeyev, I. G. O graficheskom opredelenii moshchnosti dolinnykh lednikov i o vgryzanii nizhney chasti etikh lednikov v svoge lozhe . Izvestiya Vsesoyuznogo Geograficheskogo Obshchestva, Tom 99, Vyp. 2, 1967, p. 14446. [Determination of ice thickness by extrapolation of the valley profile below the glacier; comparison with seismic depths, and discussion of errors caused by erosion.]Google Scholar
Gall, H. Gletschermarken in Lasistan. Die Alpen, 44. Jahrg., 2. Quartal, 1968, p. 9497. [Brief description with photographs of glaciers in this region of Turkey where marks for measurement of glacier variations were set up.]Google Scholar
[Glaciers: Canada.] Hydrology of the Lewis Glacier, north-central Baffin Island, N.W.T., and a discussion of reliability of the measurements. Geographical Bulletin (Ottawa), Vol, 9, No. 3, 1967, p. 23261. [Mass balance and water balance of this distributary glacier of Barnes Ice Cap.]Google Scholar
Govorukha, L. S. Voprosy glyatsiologicheskoy izuchennosti sovetskoy Arktiki i osnovnyye osobennosti rezhinla yeye oledeneniya . Izvestiya Vsesoyuznogo Geograficheskogo Obshchestva, Tom 100, Vyp. 1. 1968, p. 2737.Google Scholar
Gow, A. J. Electrolytic conductivity of snow and glacier ice from Antarctica and Greenland. Journal of Gecphysical Research, Vol. 73, No. 12, 1968, p. 364349. [Measurements of conductivity of melt water of samples from pits and bore holes.]Google Scholar
Haase, E. Gedanken zu Schneegrenzbestimmungsmethoden aufgrund neuer Schneegrenzbestimmungen im Südschwarzwald. Berichte der Naturforschenden Gesellschaft zu Freiburg im Breisgau, Bd. 56, Ht. 1, 1966, p. 1722. [Attempt to define a small-regional snow line for the entire glacier system of the Haslach valley.]Google Scholar
Haefeli, R. Brandenberger, F. Rheologisch-glaziologische Untersuchungen im Firngebiet des grönländisehen Inlandeises. Meddelelser om Gronland, Bd. 177, Nr. 1, 1968, 340 p. [Results of deformation measurements on ice from Greenland ice sheet and of measurements on the flow of the ice sheet itself. One section (on strain quadrilaterals) by P. Gfeller. English summary.]Google Scholar
Hamilton, W. L. A change in the size-distribution of dust falling in the Polar regions over the past fourteen centuries. Polarforschung, Bd. 6, Jahrg. 36, Ht. 1–2, 1966 [pub. 19681, p. 10712. [Analysis of samples front Greenland and Antarctic ice and snow. Discussion of possible explanations of variations.]Google Scholar
Hamilton, W. L. Langway, C. C. jr. A correlation of microparticle concentrations with oxygen isotope ration in 700-year old Greenland ice. Earth and Planetary Science Letters, Vol. 3, No. 4, 1968, p. 36366. [Comparison of two measurements on 1.29 m of core from 300 m. depth gives accumulation rate of 36 cm ice year–1.]Google Scholar
Henoch, W. E. Stanley, A., comp. Glacier map of northern British Columbia and southeastern Alaska. Ottawa, Glaciology Section, Inland Waters Branch, Department of Energy, Mines and Resources, 5967. [Map to scale of 1: 1 000 000 showing distribution of glaciers and location of meteorological and hydrological stations. Copies obtainable from Map Distribution Office, Department of Energy, Mines and Resources, Ottawa, Ontario, Canada.]Google Scholar
Henoch, W. E. Stanley, A., comp. Glacier map of Yukon Territory and District of Mackenzie. Ottawa, Glaciology Section, Inland Waters Branch, Department of Energy, Mines and Resources, 1967. [Map to scale 1: 1 000 000 showing distribution of glaciers and location of meteorological and hydrological stations. Copies obtainable from Map Distribution Office, Department of Energy, Mines and Resources, Ottawa, Ontario, Canada.]Google Scholar
Hoinkes, H. C. Wendler, G. Der Anteil der Strahlung an der Ablation von Hintereis- und Kesselwand-ferner (Ötztaler Alpen, Tirol) im Sommer 1958. Archie far Meteorologic, Geophysik und Bioklirnatologie, Ser. B. Bd. 16, Ht. 2–3,1968, p. 195236. [Calculation of contribution of net radiation to ablation on these two Austrian glaciers confirms that this is most important source of energy as deduced previously for single points. English summary.]Google Scholar
Kapitsa, A. P. Podlednyy rel”yef Antarktidy . Moscow, Izdatel’stvo “Nauka”, 5968. 100 p. (Rezul’taty Issledovaniy po Mezhdunarodnym Geolzicheskim Proyektam.) [Analysis of all available data to produce map of sub-glacial relief. Discussion of ice flow, tectonic structure, evidence of uplift and of process of deglaciation. English abstract.]Google Scholar
Koerner, R. M. Kane, H. S. Glaciological studies at Plateau station. Antarctic Journal of the United States, Vol. 2, No. 4, 1967, p. 12223. [Pit stratigraphy giving mean annual accumulation.]Google Scholar
Konovalov, V. G. Izucheniye ablyatsii lednikov Srcdney Azii . Izvestiya Vsesoyuznogo Geograficheskogo Obshchestva, Tom 100, Vyp. 4, 1968, p. 30820. [Survey of work on ablation and its causes.]Google Scholar
Kotlyakov, V. M. Osobennosti akkumulyatsii na lednikakh v anomal’no snezhnyye zimy po issledovaniyam na El’bruse . Trudy.zakavkazskogo Nauchao-Issledouatgl’skogo Gidrometeorologicheskogo Instituta (Tiflis), Vyp. 20, 1966. p. 5764. [Study of snow accumulation in exceptionally snowy conditions when settling has to be allowed for throughout the entire snow depth.]Google Scholar
Kruchinin, Yu. A. Simonov, I. M. Izucheniye lednikovoy tektoniki i morfologii lednikov v rayon stantsii Novolazarevskoy (Antarktida) . Izvestiya Vsesoyuznogo Geograficheskogo Obshchestva, Tom 100, Vyp. 3, 1968, p. 21222. [Study of glacier surface features and their origin in this area.]Google Scholar
Lambert, G., and others. Datation d’une carotte de névé de la bordure de l’Antarctique par la mesure de la radioactivité naturelle et artificielle, [par] G. Lambert, C. Lorius et B. Ardouin. Earth and Planetary Science Letters, Vol. 3, No. 5, 1968, p. 42933. [Use of radioactive fallout layer to identify 5955 horizon and determine accumulation since. English summary.]Google Scholar
Lorius, C., and others. Densité de la glace et étude des gaz en profondeur dans un glacier antarctique, [par] C. Lorius, D. Raynaud et L. Dolle. Tellus, Vol. 20, No. 3, 1968, p. 44960. [Studies of density, air content, air pressure and constitution in 100 cm core from Terre Adélie.]Google Scholar
Lorius, C., and others. Teneurs en deutérium le long d’un profil de 106 m dans le névé antarctique. Application it l’étude des variations climatiques, [par] C. Lorius et R. Hagemann, G. Nief et E. Roth. Earth and Planetary Science Letters, Vol. 4, No. 3, 1968, p. 23744. [Deuterium content of cores used to infer recent temperature fluctuations and origin of ice. English summary.]Google Scholar
Maksimov, Ye. V. O sushchestvovanii svyazi mezhdu stadiyami oledeneniya i proyavleniyami seismichnosti . lzvestiya Vsesoyuznogo Geograficheskogo Obshchestva, Tom 100, Vyp. 1, 1968, p. 1526. [Correction in recent centuries between periods of seismic activity and glacier activity.]Google Scholar
Østrem, G. Pytte, R. Glasiologiske undersokelser i Norge 1967. Rapport fra Hydrologisk Avdeling, 1968, Nr. 4, 131 p., maps. [Report on year’s work on mass balance, sediment transport, glacier mapping, surveying and movement studies, and discharge prediction from glacier streams. English summary, p. 117–28.]Google Scholar
Ovenshine, A. T. Provenance of Recent glacial ice in lower Glacier Bay, southeastern Alaska. U.S. Geological Survey. Professional Paper 575-D, 1967, p. D198D202. [Estimates of ice flow in this region of southern Alaska about 200 years ago based on study of erratic blocks.]Google Scholar
Pal’gov, N. N. K voprosu o metode balansov po opredeleniyu moshchnosti gornykh lednikov . Izvestiya Vsesoyuznogo Geograficheskogo Obshchestva, Tom 99, Vyp. 2, 1967, p. 14244 [Reply to criticisms by V. G. Konovalov, ibid., Tom 98, Vyp. 2, 1966, p. 157–601Google Scholar
Paschinger, H. Die Pasterze in den Jahren 1962 bis 1966. Carinthia IL Mitteilungen des Naturhistorischen Landes- museums für Kärnten, 77. Jahrg., 1967. p. 8288. [Calculation of mass loss. Since 1966 the glacier surface has started to rise again.]Google Scholar
Pearce, D. C. Walker, J. W. An empirical determination of the relative dielectric constant of the Greenland ice cap. Journal of Geophysical Research, Vol. 72, No. 22, 1967. p. 574347. [Radar pulse propagation times at 30 MHz used to deduce relation between density and permittivity.]Google Scholar
Picciotto, E. E. Geochemical investigations of snow and firn samples from East Antarctica. Antarctic Journal of the United States, Vol. 2, No. 6, 1967, p. 23640. [Preliminary results of work on stable isotope ratios, radioactive horizon, 210Pb, and extra-terrestrial material.]Google Scholar
Post, A. Effects of the March 1964 Alaska earthquake on glaciers. U.S. Geological Survey. Professional Paper 544–D. 1967, vi, 42 p. [No evidence of large snow or ice avalanches or of dynamic glacier response or surges. Rock avalanches onto glaciers described.]Google Scholar
Reger, R. D. Recent history of Gulkana and College Glaciers, central Alaska Range, Alaska. Journal of Geology, Vol. 76, No. 1, 1968, p. 216. [Lichenometry used to date moraines and deduce former advances of these glaciers.]Google Scholar
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Rutishauser, H. Graphische Darstellung und Berechnung der Veränderung des Schmadri- und Breithorngletschers sowie der Tschingelgletscherzungc in der Zeit von 1927 bis 1960. Die Alpen, 44. Jahrg., 2. Quartal. 1968, p. 98103. [Determination of retreat, surface lowering and volume loss of these two Swiss glaciers.]Google Scholar
Scheibbner, F. Mahringer, W. Die Albedo der Sonnblickgletscher und ihre zeitlichen Variationen. Archit far Meteorologie, Geophysik und Bioklimatologie, Ser. B, Bd. 16, Ht. 2–3, 1968, p. 17494. [Measurement of albedo, both in visible range and total, and its short-period variability on this Austrian glacier. English summary.]Google Scholar
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Thyssen, F. Kohnen, H. Eisseismische Untersuchungen auf dem Schmiedinger Kees. Polarforschung, Bd. 6. Jahrg. 36, Ht. 1–2,1966 [pub. 1968], p. 7882. [Determination of seismic P-wave velocity and ice thickness of this glacier. English summary.]Google Scholar
Vivian, R. Jail, M. Fiches des glaciers français. Le glacier d’Arnes. Revue de Géographie Alpine, Tom. 56. Fasc. 3–4, 1968, p. 65558. [Summary of knowledge of this glacier.]Google Scholar
Vivian, R. Jail, M. Fiches des glaciers français. Le glacier des Evettes. Revue de Géographie Alpine, Tom. 56. Fasc. 3–4. 1968, p. 65154. [Summary of knowledge of this glacier.]Google Scholar
Weertman, J. Libby, W. F. Venus: ice sheets. Science, Vol. 160, No. 3835, 1968, p. 147374. [Letter by Weertman suggesting that ice sheets on Ventes as postulated by Libby are unreasonable. with reply by Libby that 10 km thick ice sheets might be all right because of high CO2 content.]Google Scholar
Weidick, A. Observations on some Holocene glacier fluctuations in West Greenland. Meddelelser om Grenland. Bd. 165, Nr. 6, 1968, 202 p., maps. [Detailed study of evidence of late-glacial, post-glacial and historical fluctuations of the margin of the Greenland ice sheet and of smaller glaciers in West Greenland.]Google Scholar

Icebergs. Sea, River and Lake Ice

Andriyashev, A. P. O mikroflore i faune, svyazannoy s antarkticheskim pripaynym l’dom .,Zoologicheskiy,Zhurnal, Tom 46, Vyp. 10, 1967, p. 158592. [Study of algae, diatoms, etc., associated with Antarctic ice.]Google Scholar
Carey, K. L. The underside of river ice, St. Croix River, Wisconsin. U.S. Geological Survey. Professional Paper 575-C, 1967, p. C195C199. [Measurement of roughness coefficient and comparison with roughness of the bed.]Google Scholar
Deveau, J.-P. Quelques idées récentes sur les glaces de l’estuaire du Saint-Laurent. Revue de Géographie Alpine, Tom. 56, Fasc. 3–4, 1968, p. 60310. [Report of recent work on the ice of the St Lawrence estuary.]CrossRefGoogle Scholar
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Lorenz, G. Meier, S. Die Eislage im Kongsfjord (West-Spitzbergen) 1964/65. Polarforschung, Bd. 6, Jahrg. 36, Ht. 1–2, 1966 [pub. 1968], p. 10306. [Observations of sea ice formation and decay in fjords in this region of Svalbard. English summary.]Google Scholar
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Marshall, N. The icefields round Iceland in spring 1968. Weather, Vol. 23, No. 9, 1968, p. 36876. [Reasons for exceptional spread of sea ice.]Google Scholar
Mikhailova, Ye. N., and others. O raschete dreyfa l’dov i techeniy v arkticheskom basseyne . Doklady Akademii Nark SSSR, Tom 175, No. 6, 1967, p. 127376. [Mathematical theory assuming ice to be solid in the vertical and fluid in the horizontal.]Google Scholar
Milne, A. R., and others. Ambient noise under sea ice and further measurements of wind and temperature dependence, [by] A. R. Milne, J. H. Ganton and D. J. McMillin. Journal of the Acoustical Society of America. Vol. 41, No. 2, 1967, p. 52528. [Letter. Noise under shore-fast ice related to wind and temperature changes. that under moving ice is not so easily accounted for.]CrossRefGoogle Scholar
Serikov, M. I. Prochnostnyye kharakteristiki morskogo antarkticheskogo l’da . Trudy Sovetskoy Antarkticheskoy Ekspeditsü, Tom 48, 1967. p. 19093. [Results of shear. compressive and impact tests.]Google Scholar
Sirounian, V. Effect of temperature. angle of observation, salinity, and thin ice on the microwave emission of water. Journal of Geophysical Research, Vol. 73, No. 14, 1968, p. 448186. [Computation of effect of ice layer shows considerable change when thickness is of order of wavelength. Possibility of determining ice thickness by airborne passive microwave radiometry.]CrossRefGoogle Scholar
Smirnov, V. N. Lin’kov, Ye. M. Ob istochnike vysokochastotnykh seysmicheskikh vozmushcheniy i izgibogravitatsionnykh voln v Antarktike . Izvestiya Akademii Nauk SSSR. Fizika.Zemli, 1967, No. 8. p. 8892. [These disturbances and waves are the result of glacier calving. English translation in IzvesÍya. Academy of Sciences. U.S.S.R. Physics of the Solid Earth, 1967, No. 8, [pub. 1968,] p. 542–45.]Google Scholar
Sokolov, A. L. Gorbunov, Yu. A. Nekotoryye printsipy metodiki kratkosrochnykh prognozov raspredeleniya l’dov . Problemy Arktiki i Antarktiki. Vyp. 27, 1967, p. 7481.Google Scholar
Untersteiner, N. Natural desalination and equilibrium salinity profile in perennial sea ice. Journal of Geophysical Research, Vol. 73, No. 4, 1968, p. 125157. [Discussion of mechanisms of brine migration.]Google Scholar
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Weller, G. Heat-energy transfer through a four-layer system: air, snow, sea ice, sea water. Journal of Geophysical Research, Vol. 73, No. 4, 1968, p. 120920. [Experimental determination of heat-energy transfer through sea ice near Mawson and discussion of results.]Google Scholar

Glacial Geology

Andrews, J. T. Notes on glacioisostatic rebound studies, Baffin Island, Northwest Territories, Canada. Coastal Research Nodes, Vol. 2, No. 7, 1968, p. 1114. [Summary of available data.]Google Scholar
Andrews, J. T. Postglacial rebound in Arctic Canada: similarity and prediction of uplift curves. Canadian Journal of Earth Sciences, Vol. 5, No. 1, 1968, p. 3947. [Analytic form of uplift curves show similar response with time. Hence relaxation time and amount of residual uplift can be deduced.]Google Scholar
Aseyev, A. A. Dynamik und geomorphologische Wirkung der europäische Eisschilde. Petermanns Geographische Mitteilungen, 112. Jahrg., 2. Quartalsht., 5968, p. 11215. [Reconstruction of surface form and temperature conditions of European Pleistocene ice sheets and discussion of their geomorphological effect. English and Russian summaries.]Google Scholar
Barbaroux, L. Le Quaternaire de la Péninsule de Bragger et régions voisines (Spitsberg occidental). Bulletin de l’Association Française pour l’ Etude du Quaternaire, 4e An., No. 13, 1967, [pub. 1968,] p. 28192. [Connexion between neotectonic isostasy and Quaternary deposits in Svalbard. Two main stages of deglaciation identified. English summary.]Google Scholar
Dahl, R. Late-glacial accumulations, drainage and ice recession in the Narvik-Skjommen district, Norway. Norsk Geografisk Tidsskrift, Bd. 22, Ht. 2, 1968, p. 10165, plates in folder at back. [Description and discussion of features to illustrate course of deglaciation after Tromso-Lyngen sub-stage.]Google Scholar
Ergenzinger, P. Die eiszeitliche Vergletscherung des Bayerischen Waldes. Eiszeitalter und Gegenwart, Bd. 18. 1967, p. 15268. [Use of geomorphological evidence to establish maximum extent of Würm and Riss glaciation in this region of Germany and in the neighbouring regions of Czechoslovakia. English summary.]Google Scholar
Frakes, A. Crowell, J. C. Late paleozoic glacial geography of Antarctica. Earth and Planetary Science Letters. Vol. 4, No. 3, 1968, p. 25356. [Directional features of Permian(?) glacial rocks used to reconstruct source areas of ice.]Google Scholar
German, R., and others. Die Höhenlage der Schichtengrenze Tertiär-Quartär im mittleren Oberschwaben, von R. German, J. Lohr, D. Wittmann und P. Brosse. Eiszeitalter and Gegenwart, Bd. 18, 1967, p. 10409. [Deduction of contour map for Tertiary-Quaternary boundary, and discussion of implications including those for glacial morphology. English summary.]Google Scholar
Gillberg, G. Distribution of different limestone material in till. Geologiska Füreningens i Stockholm Förhandlingar, Vol. 89, Pt. 4, No. 531, 1967, p. 40109. [Suggests abrasions more important than quarrying; study of processes in formation and deposition.]Google Scholar
Gillberg, G. Lithological distribution and homogeneity of glaciofluvial material. Geologicaa Föreningens i Stockholm Förhandlingar, Vol. 90, Pt. 2, No. 533, 1968, p. 189204. [Lithological analysis of material from eskers and outwash deltas shows it to be of extremely local origin and very homogeneous.]Google Scholar
Goodell, H. G., and others The Antarctic glacial history recorded in sediments of the Southern Ocean. [by] H. G. Goodell, N. D. Watkins, T. T. Mather and S. Koster. Palaeogeography, Palaeoclimatology, Palaeoecology. Vol. 5, No. 1, 1968. p. 4162. [Study of Late Tertiary Antarctic glaciation based on sediment types and dated by palaeomagnetism.]Google Scholar
Haynes, V. M. Nature of glaciated landforms. Nature. Vol. 217, No. 5133, 1968, p. 103536. [Fit of analytic curves to longitudinal profiles of corries.]Google Scholar
Holtedahl, H. Notes on the formation of fjords and fjord-valleys. Geografiska Annaler, Vol. 49a. Nos. 2–4. 1967, p. 588203. [Discussion of formation of fjords in light of new data.]Google Scholar
Johansson, H. G. Striae and fabric analysis in a moraine exposure in Västerbotten, N. Sweden. A preliminary report. Geologiska Föreningens i Stockholm Förhandlingar, Vol. 90, Pt. 2, No. 533, 1968, p. 20512. [Field and laboratory studies of till deposits and deduction of relation to ice movement.]Google Scholar
Jordan, H. Meyer, K.-D. Gletscherschrammen bei Burgstemmen südlich von Hannover. Eiszeitalter und Gegenwart, Bd. 18, 1967, p. 198203. [Description of glacial striae in this region of Germany. English summary.]Google Scholar
Koark, H. J. Ober einen subglazialen Evorsionsring. Geografuka Avaler, Vol. 49a, Nos. 2–4, 1967, p. 2260. [Description of ring-shaped pot-hole and discussion of its mode of origin.]Google Scholar
Laverdière, C. Réponse aux “Comments on ‘Sur le lieu de fonte sur place de la calotte glaciaire de Scheffer’” de Barnett et Peterson. Canadian Geographer, Vol. 12, [No.] 2, 1968, p. 11620. [Reply to criticism of author’s paper, ibid., Vol. 11, [No.] 2, 1967. p. 86–95, made by D. M. Barnett and J. A. Peterson, ibid.. Vol. 12. [No.] 1, 1968, p. 53–54–]Google Scholar
Matthews, B. Late Quaternary events in northern Ungava, Quebec: the glaciation of the Deception Bay. Lac Watts and Sugluk areas. McGill Sub-Arctic Research Laboratory. Research Paper No. 23, 1967. p. 4262. [Presents account of pattern of glaciation in area. and study of orientation of free erratic boulders.]Google Scholar
Mercer, J. H. The discontinuous glacio-eustatic fall in Tertiary sea level. Palaeogeography, Palaeoclimatology. Palaeoecology, Vol. 5, No. 1, 1968, p. 7785. Reconstruction of build-up of Antarctic ice sheet and Greenland ice sheet.Google Scholar
Mercer, J. H. Glacial geology of the Reedy Glacier area, Antarctica. Geological Society of America. Bulletin. Vol. 79, No. 4, 1968, p. 47185. [Basal till, lateral moraines and ice-marginal lake sediments used to deduce glacial history in this area south of Ross Ice Shelf.]Google Scholar
Messerli, B. Die eiszeitliche und die gegenwärtige Vergletscherung im Mittelmeerraum. Geographica Helvetica, 22. Jahrg., [Ht.] 3, 1957, p. 105228. [Review of Pleistocene and contemporary glaciers in Mediterranean area, and deduction of snow line maps. English summaries to various sections.]Google Scholar
Okamoto, Y. Kita-hankyū no daiyonki hyōga zensen tu jumoku genkaisen seibutsugun no söhanteki nanka to Nihon no teil hyoga . Hiroshima-daigaku Kyōikugaku-bu Kiyō, [Sect.] 3, [Vol.] 16, 1967, p. 5365. [Evidence for glaciation at low altitudes in Japan. English summary-1Google Scholar
Okamoto, Y. Sakkonrcki o fukumu yamajari-sō no bunpu to Nihon no teii hyóga soyō . Hiroshima-daigaku Kyōikugahu-bu Kiyō, [Sect.] 3, [Vol.] 16, 1967, p. 6780. [Direct evidence of glaciation in various parts of Honshu, Japan.]Google Scholar
Penny, L. F. Catt, J. A. Stone orientation and other structural features of tills in east Yorkshire. Geological Magazine, Vol. 104. No. 4. 1967, p. 34460. [Observations on stones and sand grains, and study of deformation structures.]Google Scholar
Robinson, A. H. W. The submerged glacial landscape off the Lincolnshire coast. Institute of British Geographers. Transactions, No. 44, 1968, p. 11932. [Hydrographie surveys, bottom sampling and seismic profiles used to study glacial geomorphology of bed of North Sea.]Google Scholar
Rutford, R. H., and others. late Tertiary glaciation and sea-level changes in Antarctica. [by] R. H. Rutford. C. Craddock and T. W. Bastien. Palaeogeography, Palaeoclimatology, Palaeoecology, Vol. 5, No. 1, 1968, p. 1539. [Evidence for Tertiary glaciation.]Google Scholar
Souchez, R. A. Glacial-geological investigations in southern Victoria Land. Antarctic Journal of the United States. Vol. 2, No. 6, 1967, p. 25152. [Report of work on moraine field of tipper Ferran Glacier.]Google Scholar
Thomas, C. W. Antarctic ocean-floor fossils: their environment and possible significance as indicators of ice conditions. Pacific Science, Vol. 22, No. 1, 1968, p. 4551. [Use of amount of calcareous remains in sediments to give information about ice-cover conditions.]Google Scholar
Zienert, A. Vogesen- und Schwarzwald-Kare. Eiszeitalter und Gegenwart, Bd. 18, 1967. p. 5175. [Study of glacial cirques in the Vosges and Schwarzwald (Black Forest). Statistical analysis used to associate these with various Würm stadials. English summary.]Google Scholar

Frost Action on Rocks and Soil. Frozen ground. Permafrost

Adolphe, J.-P. Etude de quelques cristallisations provoquées par gel expérimental. Cahiers Géologiques. An. 1966, Nos. 79–80, [pub.] 1967, p. 91117. [Study of crystallization and movement of ions in chalk saturated with water and subjected to repeated freeze-thaw.]Google Scholar
Bisal, F. Nielsen, K. F. Effect of frost action on the size of soil aggregates. Soil Science, Vol. 104, No. 4, 1967, p. 26871. [Field and laboratory tests on effect of water content at time of freezing on size of aggregates in soil.]Google Scholar
Dostovalov, B. N. Kudryavtsev, V. A. Obshcheye merzlolovedeniye . Moscow. lzdatel’stvo Moskovskogo Universiteta. 1967. 404 p. [Textbook for geology departments at university level.]Google Scholar
Hamelin, L.-E. Cook, F. A. Le périglaciaire par l’image: Illustrated glossary of periglacial phenomena. Québec, Les Presses de l’Université Laval, 1967. xi, 237 p. (Travaux et Documents du Centre d’Études Nordiques, 4.) [Selection of illustrations of periglacial phenomena with descriptive texts in French and English.]Google Scholar
Hewitt, K. The freeze-thaw environment of the Karakoram Himalaya. Canadian Geographer, Vol. 12, [No.] 2, 1968, p. 8598. [Results of meteorological observations which give information on number of freeze-thaw cycles.]Google Scholar
Kirillov, V. A. Osnovnyye tipy geoelektricheskogo razreza tolshchi merzlykh porod po periodam v godovom tsikle . Geologiya i Geoflzika, 1967, No. 8, p. 7582. [Variations in dielectric properties.]Google Scholar
Konishchev, V. N. Maslov, A. D. Mckhanizm rosta singeneticheskikh poligonal’no-zhit’nykh I’dov . Vestnik Moskovskogo Universitela, Ser. 5, God 23, No. 4, 1968, p. 4451. [Discussion of method of growth of ice veins in Quaternary deposits of the permafrost area. English summary.]Google Scholar
Konstantinova, G. S. Deshifrirovaniye merzlotnykh form rel’yefa i merzlotnykh yavleniy tundrovykh ravnin . Vestnik Moskovskogo Universiteta, Ser. 5, God 23, No. 1, 1968, p. 97102. [On aerial photographs.]Google Scholar
Kovalev, P. V. Glyatsial’nyye i periglyatsial’nyye selevyye potoki Bol’shogo Kavkaza . Trudy Zakavkazskogo Nauchno-Issledovatel’skogo Gidrometeorologicheskogo Instituta (Tiflis), Vyp. 22, 1966, p. 20818. [Classification of causes of solifluction.]Google Scholar
Lambert, A. La formation de glace dans les conduits karstiques, les roches fissurées et les pierriers. Revue de Géographie Physique et Géologie Dynamique, Deuxième Sér., Vol. 9, Fase. 4, 1967, p. 32123. [Ice formations similar to those in caves found in voids of permeable rock mass.]Google Scholar
Pissart, A. Les pingos de l’île Prince Patrick (76° N-120° W). Geographical Bulletin (Ottawa), Vol. 9, No. 3. 1967, p. 189217. [Study of pingos in this island of Canadian Arctic Archipelago. English summary.]Google Scholar
Sartz, R. S. A test of three indirect methods of measuring depth of frost. Soil Science, Vol. 104, No. 4, 1967, p. 27378. [Field tests over two years compared.]Google Scholar
Zhigarev, L. A. Prichiny i mekhanizm razvitiya solifluktsii . Moscow, Izdatel’stvo “Nauka”, 1967. 157 p. [Nature of solifluction deposits and the causes and mechanism of the movement.]Google Scholar

Meteorological and Climatological Glaciology

Bartishvili, G. S. Kuvayeva, G. M. Ob obrazovanii nekotorykh vidov konzhelyatsionnugo l’da v atmosfere [On the formation of certain forms of congelation ice in the atmosphere]. Trudy, akavkazskogo NauchnIssledovalel’sko o Gidrometeorologicheskogo Instituta (Tiflis), Vyp. 20, 1966, p. 3139. [Detailed study of hailstones made in the field without freezing. Discussion of mode of formation.]Google Scholar
Carte, A. E. Kidder, R. E. Transvaal hailstones. Quarterly journal of the Royal Meteorological Society, Vol. 92, No. 391, 1966, p. 38295. [Detailed study of structure of hailstones. Discussion ibid., Vol. 93, No. 398, 1967, p. 560–61.1Google Scholar
Khemani, L. T. Nature of hail embryos-a suggestion. Journal of the Meteorological Society of Japan, Ser. 2, Vol. 45, No. 4, 1967, p. 27578. [Chemical analysis of rain shows higher ionic concentrations if the rain was associated with hail, which corroborates Latham’s idea that hail forms on giant aerosols.]Google Scholar
Knight, C. A. On the mechanism of spongy hailstone growth. Journal of the Atmospheric Sciences, Vol. 25, No. 3, 1968, p. 44044. [Theory of spongy hailstone growth based on constitutional supercooling.]Google Scholar
Knight, C. A. Knight, N. C. Spongy hailstone growth criteria. I. Orientation fabrics. II. Microstructures. Journal of the Atmospheric Sciences, Vol. 25, No. 3, 1968. p 44559. [Study of artificial hail grown in spongy condition and comparison with natural hail.]Google Scholar
Loup, J., and others. Le verglas dans les Alpes du Nord et leur avant pays, par J. Loup, J. Lovie [et] J. Mattasoglio. Revue de Géographie Alpine, Tom. 56, Fase. 3–4, 1968, p. 55360. [Occurrence of glazed ice on roads in the northern Alps and methods of combating it. German abstract.]Google Scholar
Macklin, W. C. Bailey, I. H. The collection efficiencies of hailstones. Quarterly Journal of the Royal Meteorological Society, Vol. 94, No. 401, 1968, p. 39396. [Measurements on spheres and artificial hailstones in an icing tunnel and calculation of critical liquid water concentration of large natural hailstones.]Google Scholar

Snow

Dickson, R. R. Posey, J. Maps of snow-cover probability for the northern hemisphere. Monthly Weather Review, Vol. 95, No. 6, 1967. p. 34753. [Presentation of maps of probability of snow cover t inch (2.54 cm) or more in depth at end of each month September to May.]Google Scholar
Dolov, M. A. Zalikhanov, M. Ch. Temperaturnoye pole i potoki tepla v snezhnom pokrove . Trudy Zakavkazskogo Nauchno-Issledovatel’skogo Gidrometeorologicheskogo Instituta (Tiflis), Vyp. 22, 1966, p. 17886. [Separate investigation of both temperature field and heat flux in both wet and dry snow.]Google Scholar
Essington, E. H. Smith, J. L. Snow-evaporation reduction: migration of evaporation suppressants through snow. Transactions of the American Nuclear Society, Vol. 10, No. 1, 1967, p. 77. [Summary. Experiments on ability of hexadecanol to penetrate snow and reduce evaporation.]Google Scholar
Fraser, C. Avalanches. Geographical Magazine, Vol. 40, No. 8, 1967, p. 68085. [Popular account.]Google Scholar
Gary, H. L. Colthard, G. B. Snow accumulation and disappearance by aspect and vegetation type in the Santa Fe basin, New Mexico. U.S. Dept. of Agriculture. Forest Service Research, Note RM-93, 1967, 11 p. [Observations of snow cover on north and south aspects, under various tree covers and grass.]Google Scholar
Gold, L. W. Micrometeorological observations of the snow and ice section, Division of Building Research, National Research Council. (In Proceedings of the first Canadian Conference on Micrometeorology. Pt. 1. Toronto. Meteorological Service of Canada, 1967, p. 13644.) [Observations on heat and moisture exchange between the atmosphere and snow, water and soil surfaces. Also published as Canada. National Research Council. Division of Building Research. Research Paper No. 351.]Google Scholar
Izotov, V. F. Khod nakopleniya i tayaniya snega pod pologom zabolochennykh lesov severnoy podzony taygi . Meteorologiya i Gidrologiya, 1967, No. 11, p. 8691.Google Scholar
Khodakov, V. G. Raspredeleniye, svoystva i gidrologichcskaya rol’ snezhnogo pokrova severnoy chasti Uralskikh gor . Izvestiya Akademii Nauk SSSR, Seriya Geograficheskaya, 1967, No. 4, p. 12226.Google Scholar
Kuvayeva, G. M. K voprosu opredeleniya velichiny koeffitsiyenta diffuzii vodyanogo para v snegu . Trudy Zakavkazskogo Nauchno-Issledovatel’skogo Gidrometeorologicheskogo Instituts (Tiflis), Vyp. 20, 1966. p. 7578. [Results of experiments in the field and laboratory.]Google Scholar
Kuvayeva, G. M., and others. Fizicheskiye svoystva snezhnogo pokrova Bol’shogn Kavkaza . Rezul’taty Issledovaniy po Programme Mezhdunarodnogo Geofizicheskogo Goda. IX Razdel Programmy MGG, No. 17, 1967, 196 p. [Study of radiation properties, effect of porosity, heat balance. recrystallization and mechanical properties of snow, and study of snow avalanches and methods of avalanche defence. English summary.]Google Scholar
Loup, J. Lovie, C. Sur la fréquence des avalanches en haute Tarentaise. Revue de Géographie Alpine, Tom. 55, Fasc. 4, 1967, p. 587604. [Investigation of various factors affecting avalanche frequency in this region of France.]Google Scholar
Morozov, G. A. Raschet izmeneniya plotnosti snezhnogo pokrova pod deystviyem diffuzii, konvektsii vodyanogo para v nem . Meteorologiya i Gidrologiya, 1967, No. 6, p. 98103. [Experimental determination of the water-vapour distribution coefficient for various snows, and deduction of formulae for computation.]Google Scholar
Moskalev, Yu. D. Raschety ustoychivosti snezhnoy tolshchi po uglam sdviga . Trudy Zakavkazskogo Nauchno-Issledovatel’skogo Gidrometeorologicheskogo Instituta (Tiflis), Vyp. 20, 1966, p. 15665. [Method for graphical and analytical solutions of snow stability problems.]Google Scholar
Ōnuma, T., and others. Nókóchi ni okeru yasetsu sokushinhó ni kansuru kenkya (sono 2). Herikoputá ni yoru yúsetsu sokushin . Seppyo, Vol. 29, No. 3, 1967, p. 7883. [Use of airborne black powder in snow melting and method of estimating amount of settled powder by measuring albedo. English summary.]Google Scholar
Planhol, X. de. L’ancien commerce de la neige en Corse: neige d’Ajaccio et neige de Bastia. Méditerranée, 9e An., No. 1, 1968, p. 522. [History of the trade in snow from Corsica.]Google Scholar
Salomonson, V. V. Marlatt, W. E. Anisotropic solar reflectance over white sand, snow and stratus clouds. Journal of Applied Meteorology, Vol. 7, No. 3, 1968, p. 47583. [Aerial measurements show main anisotropy for snow to be due to specular reflection.]Google Scholar
Samukashvili, R. D. Proniknoveniye solnechnoy radiatsii v tolshchu snezhnogo pokrova v period yego tayaniya na vysokogornoy observatorii El’brus . Trudy Zakavkazskogo Nauchno-Issledovatel’skogo Gidrometeorologicheskogo Institute (Tiflis), Vyp. 22, 1966, p. 18793. [Observations on penetration of direct scattered and global radiation into snow.]Google Scholar
Smith, J. L. Use of nuclear techniques in snow and related watershed management. Transactions of the American.nuclear Society, Vol. 10, No. 1, 1967, p. 78. [Summary. Radioactive gauge to measure density and water content of layer in snow cover.]Google Scholar
Yablokov, A. A. O snezhnom pokrove Zaladnogo Tyan’-Shanya. Po dannym nablyudeniy v basseyne reki Kyzylcha . Izvestiya Vsesoyuznogo Geograficheskogo Obshchestva, Tom 100, Vyp. 3, 1968, p. 15862. [Data on snow cover in this region of Uzbekistan.]Google Scholar
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