Hostname: page-component-586b7cd67f-t8hqh Total loading time: 0 Render date: 2024-11-23T22:51:55.818Z Has data issue: false hasContentIssue false
  • English
  • Français

Glaciological Literature

Published online by Cambridge University Press:  30 January 2017

Rights & Permissions [Opens in a new window]

Abstract

An abstract is not available for this content. As you have access to this content, full HTML content is provided on this page. A PDF of this content is also available in through the ‘Save PDF’ action button.
Type
Other
Information
Journal of Glaciology , Volume 9 , Issue 56 , 1970 , pp. 289 - 300
Copyright
Copyright © International Glaciological Society 1970

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 Commitee 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 i interest. It should be noted that the Society does not necessarily hold copies of the items in this list, and also that the Society does not possess facilities for microfilming or photocopying.

References

Conferences

Shchukina,O. VE. Chetvertyy obshchesoyuznyy glyatsiologicheskiy simpozium [Fourth all-Union glaciological symposium].Vestnik Moskovskogo Unwersiteta, Ser. 5. God 24, No, 3, 1969, p. 122–23. I Report of symposium held in northern Caucasus al “El'brus”, 21 September-5 October 1968.]Google Scholar

General Glaciology

Bryazgin, N.N. Koptev., A. P. O spektral'nom al'bedo snczhno-ledyanogo pokrova [Spectral albedo of a snow or ice surface], Probiemy Arktiki i Antarktiki Vyp. 31, 1969, p. 79–83.Google Scholar
Fliri, F. ed. [Alpcnkundliche Studien, l.J Festschrift für Hans Kinzl zum siebzigsten Geburtstag Veröffentlichungen der Universität Innsbruck, 1, 1968, xi, 160 p. [Papers include: Fliri, F., “Beiträge zur Hydrologie und Glaziologie der Cordillera Bianca (Peru)”, p. 25–52; Heuberger, H., “Die Ötztalmündung (Inntal, Tirol)”, P. 53–90; H. Heuberger and H. Penz, “Verzeichnis der wissenschaftlichen Arbeiten von Univ.-Prof. Dr Hans Kinzl”, p. 149–156.]Google Scholar
Hoinkes, H.C. Raimund von Klebeisberg, 14.1a.1886 6.6.1067. Jahrbuch der Bayerischen Akademie der Wissenschajten 1968, p. 212–20. [Obituary.]Google Scholar
Kattekfel'D G. N., Frolov, P. M. O sushchestvovanii vody na Lune [On the existence of water on the moon], Izvestiya Vsesoyuznago Geograficheskogo Obshchestva, Tom 101, Vyp. 3, 1969, p. 260–64. [Discussion of possibility of ice, water and water vapour on the moon.]Google Scholar

Glaciological Instruments and Methods

Berdnikov, V.V. Kotyukov,, V. A. Opyt primeneniya geofizicheskikh metodov pri izuchenii reliktovykh merzlolnykh obrazovamy [The use of geophysical methods for studying relict frozen ground formationsl Izvestiya Akademii Nook SSSR, Seriya Geograjicheskaya, 1969. No. 5, p. 109–17. Bogokodskiy, V.V. Fizkheskiye melody issledovaniya lednikov·(Physical methods of investigating glaciers] Leningrad Gidrometeorologichcskoye Izdatel'stvo, 1968.214 p. [Book summarizing basic principles of gravimetric, seismic, and radar techniques used in glaciology. English summary.]Google Scholar
Evans, S. Smith, B.M.E. A radio echo equipment for depth sounding in polar ice sheets. Journal of Scientific Instruments (Journal of Physics, E), Ser, a, Vol. 2, No. 2, 1969. p. 131–36. [Discusses need for depth-sounding in glaciers, ice sheets, and ice shelves, and describes v.h.f. radar, designed specifically to produce continuous profiles of ice depth. Practical problems and results.]CrossRefGoogle Scholar
Gluck,, S. _ Épaisseur du Glacier Blanc (massif de I’Oisans) dans sa partie supérieure. Comptes Rendus Hebdomadaires des Séances de l’Académie des Sciences (Paris), Tom. 268, Sér. D, No. 12, 1969. p. 1583–85. [Seismic reflexion technique used to determine glacier thickness in accumulation area of this French glacier.]Google Scholar
Nelsln, D.E. Radar sounding of glaciers in the Icefield Ranges. (In Bushnell, V.C., Ragle, R.H. ed. Icefeld Ranges Research Project. Scientific results. Vol. 1. New York, American Geographical Society; Montreal, Arctic Institute of North America, 1969, p. 107.) [Successful use of technique in divide region of ice field.]Google Scholar

Physics of Ice

Aknason, B. Equilibrium constant for the fractionation of deuterium between ice and water. Journal of Physical Chemistry, Vol. 73, No. 10, 1969, p. 3491–94. [Accurate experimental determination.]CrossRefGoogle Scholar
Bailey, W.A. Measuring heat losses through common greenhouse covering materials under different test conditions, [by] Bailey, W.A., Liu, R.C., Klueter, H.H., Krizek, D.T. (In Ho, C.Y., Taylor, R.E. ed. Thermal conductivity. Proceedings of the eighth conference held at Purdue University, West Lafayette Indiana October 7–10, 1968. New York, Plenum Press, 1969>. p. 941–48.) [Experiments show that ice or snow cover over the glass increases heat transmittance.]Google Scholar
Bennett, J.E. Trapped electrons produced by deposition of alkali-metal atoms on ice at 77°K. Part III. Invariance of electron spin resonance spectra with metal cation, by Bennett, J.E., Mile, B., Thomas, A.. Journal of the Chemical Society, Sect. A. 1969, [No.] 10, p. 1502–05. [Identical e.s.r. spectra result from deposition of Li, K, Na, Rb or Cs, so the cation is not involved in the trap.]CrossRefGoogle Scholar
Bertie, J.E. Absorptivity of ice I in the range 4 000–30 cm.-1 [by] Bertie, J.E., Labbé, H.J., Whalley, E. Journal of Chemical Physics, Vol. 50, No. 10, 1969. p. 4501–20. [Measurements and interpretation.]CrossRefGoogle Scholar
Bhadra, T.C Effects of physical stimulii, aeratign [sic], preheating, electric field on the supercooling and nucleation of water droplets. Indian Journal of Physics, Vol. 42, No. 8, 1968, p. 474–85. [Study of time to freeze droplets under various conditions. Shock waves had no effect, contrary to results for bulk water ]Google Scholar
Bhadra, T. C. Induction of freezing of bulk samples of supercooled water by physical stimulii. Indian Journal of Physics,Vol. 42. No. a. 1968. p. 91–102. [Experiments on effect of air content and of mechanical or electrical stimuli.]Google Scholar
Bhadra, T.C. On the feasibility of inducing cavitation in hailstones and supercooled water by low-intensity shock wave. Indian Journal of Physics,Vol. 42. Xo. to. 1968. p. 603–09. [No effect produced by ultrasonic waves on ice. Results used to discuss theory of hailstone break-up.]Google Scholar
Blair, D.N. Davis, B. L. Aging of silver iodide-sodium iodide generator effluent in moist dry air. Journal of Applied Meteorology. Vol. 8, No 4. 1969. p. 551–55. [Effect of storage of aerosol panicles on their efficiency as ice nuclei.]2.0.CO;2>CrossRefGoogle Scholar
Box, H.C. Hydroxyl radicals of X-irradiated single crystals of ice, [by] Box, H.C., Lilga, K.T., Budzinski, E.E., Deer, R. Journal of Chemical Physics,Vol. 50. No. 12, 1969, p. 5422–23. [Leiter. Electron spin resonance study at low temperatures.]CrossRefGoogle Scholar
Chiu, S.-Y Experiniental study of the ice-making operation in the inversion desalination freezing process, [by]Chiu, S.-Y, Fan, L.-T, Akins, R.G.. Industrial und Engineering Chemistry. Process Design and Development. Vol. 8, No 3. 1969. p. 347–56. [Experimental study of shape of ice crystals formed.]CrossRefGoogle Scholar
Cross, J.D. Speare., P. A. Electrical aspects of the evaporation of ice. British Journal of Applied Physics (Journal of Physics. D). Ser. 2,Vol. 2. No. 7. 1969. p. 1021–25. I Electrical charge due to evaporation of polycrystalline ice in vacuo found to be very small. Scanning electron microscopy suggests earlier results may be due to particles breaking off.]CrossRefGoogle Scholar
Davis,, B. L., Blair,, D. N. Role of substrate strain in ice nucleation. Journal of Geophysical Research. Vol. 74. No. 18. 1969. p. 4571–80. [Deformed AgI. CuS and AI2,SiO3 (OH)4 were much more efficient ice nuclei than undeformed specimens.]CrossRefGoogle Scholar
Dean, P. Remarks on the vibrations of disordered systems. Journal of the Physical Society of Japan,Vol. 26. Supplement, 1968 [pub. 1969]. p. 20–24. [Includes a discussion of vibrations of ice Ih on basis of two-dimensional theoretical model.]Google Scholar
Dillard, D.S. Timmc.rhaus., K. D. Low temperature conductivity of selected dielectric crystalline solids. (In Ho, C.Y-, Taylor, R.E. ed. Thermal conductivity. Proceedings of the eighth conference held at Purdue university. West Lafayette, Indiana, October 7–10. 1963. New York, Plenum Press. 1969. p. 949–68.) [Includes results for ice from 80 to 273 K.]Google Scholar
Dilorenzo, J. Kaplan, V. M.Phase transformations in doped ice: concentration effect m frozen ferrous solutions. Chemical Physics Letters,Vol. 3. No. 4, 1969. p. 216–18. [Mössbaucr studies of effect of Sn4+ and Eu3+ ions on ice with Fe ++ ions in solution.]CrossRefGoogle Scholar
Engelhardt,, H. Detection of single collisions of fast neutrons by nucleation of Tyndall Bowers in ice, [by] Engelhardt,, H., Müller-Krumbhaar., H., Bullemer, B., Riehl, N. Journal of Applied Physics. Vol. 40, No. 13, 1969 [pub. 19701, p. 5308–11. [Method of growing good single crystals of ice and of using them to detect neutrons by the nucleation of Tyndall flowers.]CrossRefGoogle Scholar
Fukuda, A. Higashi., A. X-ray diffraction topographic studies of dislocations in natural large ice single crystals. Japanese Journal of Applied Physics,Vol. 8. No. 8. 1969. p. 993–99. [Study of shape and Burgers vectors of dislocations in glacier ice from Mendenhall Glacier, Alaska.]CrossRefGoogle Scholar
Gitlin, S.N. Lin., S.-S. Dynamic nucleation of the ice phase in supercooled water. Journal of Applied Physics. Vol. 40, No 12. 1969. p. 4701–67. [Experiments which show that cavitation is a necessary but not a sufficient condition for dynamic nucleation of ice in supercooled water.]CrossRefGoogle Scholar
Gold,, L. W. Crack formation in ice during creep, Scripta Metallurgica. Vol. 3. No. 6, 1969. p. 367–70. [Correlation between density of cracks and creep deformation in columnar ice.]CrossRefGoogle Scholar
Haring, O.K. Slow neutron inelastic scattering study of light water and ice. Journal of Chemical Physics. Vol. 50. No. 12. 1969. p. 5279–96. [Study analysed to give proton motions in ice.]CrossRefGoogle Scholar
Hase, H. Kevan,, L. Paramagnetic relaxation of radiation-produced electrons in annealed glassy and polycrystalline alkaline ices. Journal of Physical Chemistry. Vol. 73. No. 10. 1969. p. 3290–93. [Measurements show spin-spin relaxation time depends on annealing while spin-lattice does nol. Explanation in terms of trap sites.CrossRefGoogle Scholar
Higashi, A. Hikiage hoo ni yoru hyōlankcsshō no seisaku (dai 2 hō)—X-sen topogurafu ni yoru ten-i no kansatsu [Growth of large single crystals of ice from water (2)—X-ray diffraction topographie observations ofdislocations]. [By]Higashi, A., Oguro, M., Fukuda, A. Ōyō Butsuri. [Vol.] 38, [No.] 6. 1969. p. 567–73. [Observations interpreted in terms of mechanism of growth. English summary.]Google Scholar
Isono, K. Iwai, K. Growth mode of ice crystals in air at low pressure. Nature. Vol. 223. No. 5211. 1969. p. 1149–50. [At low pressure ice crystals formed on solid nuclei are quasi-spherical with facets. Importance of these observations in study of noctilucent. and nacreous clouds.]CrossRefGoogle Scholar
Kamb, W.B. Structural studies of the high-pressure forms of ice. Transections of the American Crystallography Association. Vol. 5. 1969. p. 61–80. [Review of knowledge of high-pressure forms of ice.]Google Scholar
Krausz, A. S. A rate theory of strain relaxation. Materials Science and Engineering. Vol. 4. No. 4, 1969. p. 193–97.[Theory of strain relaxation in belter agreement with dislocation velocity measurements. Results compared with data on strain relaxation in ice.]CrossRefGoogle Scholar
Krausz, P.N. Salomon, R.E. Solubility of hydrogen chloride in ice. Journal of Physical Chemistry. Vol. 73. No. 8, 1969. p. 2680–83. [Determination from diffusion of HC1 into pure ice.Google Scholar
Lavrov, V. V. Osnovnyye zakonomernosti deformirovaniya l'da [Main principles in ice deformation]. Problemy Arktiki i Antarktiki. Vyp. 28, 1968. p. 42–45.Google Scholar
Lyashchenko, A.K. Malenkov, G.G. Rentgenograficheskoye izuchemye sistemy ftorid ammoniya led [X-ray diffraction study of the ammonium fluoride-ice system]. Zhumal Strukturnoy Khimii. Tom 10. No. 4, 1969, p. 724–25. [Determination of phase diagram and of lattice constant variations with concentration of dissolved NH4F in ice.]Google Scholar
Macklin, W.C Payne, G.S The spreading of accreted droplets. Quarterly Journal of the Royal Meteorological Society. Vol. 95. No. 40b, 1969, p. 724–30. [Measurement of amount of spreading of supercooled droplets accreting on an ice surface.]CrossRefGoogle Scholar
Mayoral, J.R. Isaka, H. Action glaçogène l'eau. Comptes Rendus Hebdomadaires des Séances de l’Académie des Sciences (Paris), Tom. 269, Sér. B, No. 3, 169, p. 145–48. [Evidence that phloroglucinols act as sublimation agents below water super-saturation.]Google Scholar
Miller, S.L. Clathrate hydrates of air in Antarctic ice. Science,Vol. 165. No. 3892. 1969. p. 489–90 [Calculations show these should form at pressure corresponding to 800 m depth. This explains gas bubble disappearance in cores at 1 200 m.]CrossRefGoogle ScholarPubMed
Nakahara, V. Phonon spectrum and thermal neutron scattering in light water ice. Journal of nuclear Science and Technology (Tokyo),Vol. 5. No. 12, 1968. p. 635–42. [Calculation of phonon spectrum and thermal neutron scattering law.]CrossRefGoogle Scholar
Odencrantz, F.K Freezing of water droplets: nucleation efficiency at temperatures above -5 C. Journal of Applied Meteorology. Vol. 8. No. 3, 1969. p. 322–25. [Laboratory studies show efficiency depends strong on experimental conditions.]2.0.CO;2>CrossRefGoogle Scholar
Orem, M.W. Adamson, A. W. Physical adsorption of vapor on ice. II. n-Alkalies. Journal of Colloid and Interface Science, Vol. 31,. No. 2,. 1969. p. 278–86. [Adsorption isotherms of simple non-polar hydrocarbon vapours on ice.]CrossRefGoogle Scholar
Pelah, I. Rum., S. L, Conductivity and Mössbauer measurements in doped ice. Journal of Chemical Physics, Vol. 51, No. 1,1969,. p. 383–87. [Conductance anomalies in ice with Sn4+ ions at same temperature as Mössbaucr anomalies.]CrossRefGoogle Scholar
Ryan, B.F. The growth of ice parallel to the basal plane in supercooled water and supercooled meta fluoride solutions. Journal of Crystal Growth. Vol. 5, No 4. 1969, p. 284–88. [Measxurements of dendritic growth rates.]CrossRefGoogle Scholar
Smith-johannsen,, R.I. Ice crystal agglomeration: T formation. Jounral of the Atmospheric Sciences Vol. 26, No. 3, 1969, p. 532–34. [Agglomerates collected from laboratory ice clouds frequently had T shape. Possible explanations discussed.]2.0.CO;2>CrossRefGoogle Scholar
Stein, G.D Angular and wavelength dependence of the light scattered from a cloud of particles formed by homogeneous nucleation. Journal of Chemical Physics. Vol. 51 No. 3., 1969. p. 938–42. I Experiments using laser light to study light scattering from ice particles formed via condensation by homogeneous nucleation ]CrossRefGoogle Scholar
Stow, C.D [tie charging of ice surfaces by natural ice particles. Quarterly Journal of the. Royal Meteorological Society, Vol. 95, No. 406, 1969, p. 797–800. [Letter commenting on paper by Scott, W.D, Hobbs, P.V. ibid.,Vol. 94. No. 402. 1968.p. 510–22, with reply by authors p. 799–800.]CrossRefGoogle Scholar
Wardman, P. Sediion., W A. Electron spin resonance studies of radicals condensed from irradiated water vapor: reactions of the radicals. Canadian Journal of Chemistry, Vol. 47, No. 12, 1969, p. 2149–54. [Studies in both H2O and D2O condensed after irradiation at 77 K.]CrossRefGoogle Scholar
Wardman, P. Sedbon, W.A. Electron spin resonance studies of radicals condensed from irradiated water vapor: paramagnetic relaxation of trapped electrons in ice. Canadian Journal of Chemistry, Vol 47 No 12, 1969. p. 2155–60. [Studies in both H2O and D2.O condensed after irradiation at 77 K]CrossRefGoogle Scholar
Weertman, J. Dislocation climb theory of steady-state creep. Transactions of American Society for Metals. Vol 61.No. 4. 1968. p. 681–94, [Critical review of high temperature creep theories. Includes hitherto unpublished data on creep of polycrystalline H2O and D2.O ice.]Google Scholar
Weisweiler., W. Bemerkungen zur Bildung der Eisdendriten. Zetsdtrifi für Meteorologie. Bd. 21. Ht 3–4 1969, p. 108–12. [Conditions of growth of different shapes of ice dendrites (snow crystals) from the vapour, Theory depending on vapour pressure difference between water and ice ]Google Scholar
Whalley, E. Change of high-frequency permittivity at an orientational order disorder transformation: a method of detecting very slow transformations. Journal of Chemical Physics. Vol. 51, No 1 1969, p 471–72. Letter Measurement of high-frequency permittivity used to detect presence of ice III-IX phase change ]CrossRefGoogle Scholar
WöRZ,, O Cole., R. H. Dielectric properties of ice I. Journal of Chemical Physics, Vol. 51, No. 4 1969 p. 1546–50. [Measurements from o° to -80 C. Deviations from Arrhenius rate equation below 50°C]CrossRefGoogle Scholar
Zatsepina, G.N. K voprosu o mekhanizme dvizheniya ionov H3O+I OH-vo l’du I vode [On the question of the movement of H2O+ and OH- ions in ice and water]. Zhumal Strukturnoy Khimii, Tom 10, No 2. 1969. p. 211–147. [Discussion of ionic mobility in ice assuming H3O+ moves along voids and OH moves along hexagonal framework in ice.]Google Scholar

Land Ice. Glaciers. Ice Shelves

Ambach, W. Ein Beitrag zur Kenntnis des Wärmehaushaltes des grönländischen Inlandeises. Polarforschung Bd. 6. Jahrg. 38, Nr. 1–2 1968 [pub. 1969], p. 207–11. [Measurement of nearly balanced heat budget in May-July on Greenland ice sheet. English abstract.]Google Scholar
Andkrton, P.W. Structural geology of a glacier confluence. Kaskawulsh Glacier. Yukon Territory Canada Dissertations Abstracts. B. Vol. 28, No 9. 1968. p. 3747.B. [Strain-rate measurements and fabric studies. Abstract of dissertation submitted to Ohio State University, 1967. Microfilm order (University Microfilms. Ann Arbor, Mich.. L.S.A.Î no. 68-2945.]Google Scholar
Bailey, j.T. Evans, S. Radio echo-sounding on the Brunt Ice Shelf. British Antarctic Survey Bulletin No 17, 1968, p. 1–12. [Analysis of records obtained on a journey from Halley Bay to a sub-station in Coats Land, 300 km to the south.]Google Scholar
Bondarev, L.G. Orozgozhoyev, B.O. Basseyny pravykh pritikov r. Sary-Dzhaz mezhdu usfyami rek Ak-Shiyrak i Kuylyu (vklyuchaya basseyn Kuylyu) [The basin of right-hand tributaries of the river Sary-Dzhaz to the mouth of the rivers Ak-Shiyrak and Kuyly (including the river Kuylyu basin], Katalog lednikov SSSR [Catalogue of glaciers of the U.S.S.R.]. Tom 14, Vyp. 2. Chast' 7. Leningrad, Gidrometeorolo-gicheskoye Izdatel stvo. 1969. 58 p. | Part of the I.H.D. catalogue of glaciers of the U.S.S.R giving details of what is known of the glaciers in this part of Central Asia including the Terskey Alatau. The Tom and Vyp. numbers correspond with those of Resursy poverkhnostnykh vod SSSR (Surface water resources of the U.S.S.R.].]Google Scholar
Bull, C.B. Marangunic, B. Glaciological effects of debris slide on Sherman Glacier. (In [U.S.] National Research Council. Division of Earth Sciences. Committee on the Alaska Earthquake. The great Alaska earthquake; hydrology. Part A. Washington, D.C., National Academy of Sciences, 1968, p. 309–17. (Publication 1603.)) [Earthquake-induced debris, about 1.3 m thick and covering third of ablation area, prevents melting of underlying ice and has thus changed regime of Sherman Glacier, Alaska, since 1964.]Google Scholar
Campbell, P.I. Glacier surveys in British Columbia, by Campbell, P.I., Reid, I.A, Shastal, J. Canada. Department of Energy, Mines and Resources. Inland Waters Branch. Water Survey of Canada. Report Series No. 5. 1969. v, 18 p., maps [in folder at back]. [Studies of volume changes of Sentinel, Sphinx, Nadahini. Kokanee and Bugaboo Glaciers.)Google Scholar
Cherkaksov, P.A. Yerasov, N.V. Reki Tcntek, Rgayty. Katalog lednikov SSSR [Catabgue of glaciers of the U.S.S.R.], Tom 13, Vyp. 2, Chast' 7. Leningrad, Gidrometeorologicheskoye Izdatel'stvo, 1969. 82 p. [Part of the I.H.D. catalogue of glaciers of the U.S.S.R. giving details of what is known of the glaciers in this part of the Dzhungarskiy Alatau. The Tom and Vyp. numbers correspond with those of Resursy poverkhnostnykh nod SSSR [Surface water resources of the U.S.S.R.].]Google Scholar
Cronk, C. Glaciological investigations near the ice sheet margin, Wilkes station, Antarctica. Dissertations Abstracts·, B, Vol. 29, No. 3, 1968, p. 1066-B. [Pit and stake measurements, ice temperature and movement measurements and their analysis. Abstract of dissertation submitted to Ohio State University, 1968. Microfilm order (University Microfilms, Ann Arbor, Mich., U.S.A.) no. 68-12826.]Google Scholar
Davvdov, L.K. Krupneyshiye ledniki Sredney Azii—Ledniki Fedchenko i Zeravshanskiy. Rezultaty meteorologicheskikh i gidrologicheskikh issledovaniy [The biggest glaciers of Central Asia—Lednik Fedchenko and Lednik Zeravshanskiy. Results of meteorological and hydrological studies]. [Leningrad], Izdatel'stvo Leningradskogo Universiteta, 1967. 263 p. [Results of I.G.Y. studies on these glaciers.]Google Scholar
Denisov,, YE. P., Niikol'skaya,, V. V. Poxdnclednikov'ye v basseyen Amura [Modern glacicrization in the Amur basin]. Izvestiya Vsesoyuznogo Geograficheskogo Obshechestva, Tom 100, Vyp. 2, 1968, p. 132–35. [Description of small glaciers in this region of U.S.S.R.]Google Scholar
Dort, W jr.,. Firn-ice relationships, Sandy Glacier, southern Victoria Land, Antarctica, by Dort, W jr.,, Roots, E.F, Derbyshire, E. Geografiska Annaler, Vol. 51A, No. 3, 1969, p. 104–11. [Pit studies through alternate layers of ice and sand and interpretation.]Google Scholar
Fashchevskiy, B.V. O lednikovom pilaniî rek Gornogo Altaya [On the glacial streams of the Altay mountains]. Izoestiya Vsesoyuznogo Geograficheskogo Obshchestva, Tom 101, Vyp. 4, 1969, p. 365–69. [Hydrographs oi glacial streams and their causes.].Google Scholar
Field, W.O. The effect of previous earthquakes on glaciers. {In | U.S.] National Research Council. Division oi Earth Sciences. Committee on the Alaska Earthquake. The great Alaska earthquake; hydrology. Part A. Washington, D.C., National Academy of Sciences, 1968, 252-65. (Publication 1603.)) [Discusses different responses of Alaskan glaciers to 1899, 1958 and 1964 earthquakes, as well as other smaller earthquakes.]Google Scholar
Field, W.O. Effects on glaciers; introduction. {In [U.S.] National Research Council. Division of Earth Sciences. Committee on the Alaska Earthquake. The great Alaska earthquake; hydrology. Part A. Washington, D.C., National Academy of Sciences, 1968, p. 247–51. (Publication 1603.)) [Reviews work described in this section of volume devoted to 1964 earthquake.]Google Scholar
Flohn, H Zum Klima und Wasserhaushalt des Hindukuschs und der benachbarten Hochgebirge. Erdkunde. Bd. 23, Ht. 3, 1969, p. 205–15. [Precipitation and run-otf in Hindu Kush and neighbouring mountains; includes discussion of contribution from glaciers and snow melt. English summary, p. 205.]CrossRefGoogle Scholar
Giessino,, Y. Trcdje etappe av Dronning Maud Land traversen. Norsk Polarinstitutt. Arbok, 1967 [pub. 1969]. p. 233–37. [Third part of traverse of Dronning Maud Land ("Plateau" station to lat. 78° 42' S., long. 6° 52’ W.) in 1967–68 as part of U.S. Antarctic Research Program. English summary.]Google Scholar
Govorukha,, L. S. Otkryt novyy lednikovyy rayon [A new glacial region has been discovered]. Prtroda, 1969, No. 7, p. 63–65. [Many glaciers found in 1967 in north-east Taymyr, U.S.S.R.]Google Scholar
Hamilton, W.L. Microparticle deposition on polar ice sheets. Ohio State University. Institute of Polar Studies. Report No. 29, 1969, vii, 77 p. (Study of micro-particle deposition in Antarctic and Greenland ice sheets and variations in size, concentration and kind of particle.]Google Scholar
Johnson, N.M. Ragle, R.H. Analysis of flow characteristics of Allen II slide from aerial photographs. (In [U S] National Research Council. Division of Earth Sciences. Committee on the Alaska Earthquake. The great Alaska earthquake; hydúrology. Part A. Washington, D.C., National Academy of Sciences, 1968. p. 369–73- (Publication 1603.)) [Some principles of flow mechanics illustrated by Allen II rock slide, Allen Glacier, and by other rock slides resulting from 1964 Alaska earthquake.]Google Scholar
Kjartansson,, G. Steinsholtshlaupiö 15. Janaúar 1967. NatturufrsMngurinn, Arg. 37, Ht. 3–4, 1967 [pub. 1968]. p 120–69. [Jökullhtaup which began as rock slide at Steinsholt, south Iceland, in 1967. English summary.]Google Scholar
Koblents,, YA. P. O dvizhenii lednika v rayone Mirnogo [Glacier movement in the region of Mirny]. Informatsionnyy Byulleten' Souetskoy Antarktklteskoy Ekspeditsii, No. 70, 1968, p. 32–35.Google Scholar
Konovalov, V.G. Rol* ablyatsii v obshchem byudzhete veshchestva i cvolyutsii gornogo lednika [Role of ablation in the budget and evolution of mountain glaciers]. Izvestiya Vsesoyuznogo Geograficheskogo Obshchestva,Tom 101, Vyp. 4, 1969, p. 296–305. [Discussion of importance of ablation in determining mass balance of glaciers.]Google Scholar
Kotlyakovv, M. Snezhnyy pokrov zemli i ledniki [Snow cover of the earth and glaciers]. Leningrad,Gidrometeorologicheskoye Izdatel'stvo, 1968. 479 p. [Interrelationship.]Google Scholar
Kupetskiy, V.N. O tendentsii sovremennogo morskogo i nazemnogo oledeneniya v svyazi s solnechnoy aktivnost'yu [The tendency of present sea and land glaciation in connexion with solar activity]. Izvestiya Vsesoyuznogo Geograficheskogo Obshchestva,Tom 101, Vyp. 5, 1969, p. 428–32.Google Scholar
LaChapelle, E.R The character of snow avalanching induced by the Alaska earthquake. (In [U.S I National Research Council. Division of Earth Sciences. Committee on the Alaska Earthquake. The great Alaska earthquake; hydrology. Part A Washington, D.C., National Academy of Sciences, 1968, p. 355–61 (Publication 1603.)) [Reviews technical aspects of snow avalanche formation influenced by 1064 'earthquake.]Google Scholar
Lliboutry, L. HOW ice sheets move. Science Journal, Vol. 5, No. 3, 1969, p. 50–55. [Popular account of current ideas on How in ice sheets.]Google Scholar
Marangunic, C. Bull, C.B.B. The landslide on the Sherman Glacier. (In [U.S.] National Research Council. Division ol Earth Sciences. Committee on the Alaska Earthquake. The great Alaska earthquake; hydrology. Part A. Washington, D.C., National Academy of Sciences, 1968. p. 383–94. (Publication 1603)) [Detailed description of physical features and sliding mechanism of debris slide, induced by 1664 Alaska earthquake and now covering third of ablation area of glacier.]Google Scholar
Marcus, M.G. Effects on glacier-dammed lakes in the Chugach and Kenai Mountains. {In [U S ] National Research Council. Division of Earth Sciences. Committee on the Alaska Earthquake. The great Alaska earthquake; hydrology. Part A. Washington, D.C., National Academy of Sciences. 1968. p 320–4.7 (Publication 1603.)) [No appreciable response observed after Alaska earthquake, 1964.]Google Scholar
Markin, V. Λ. Teplovoy balans, usloviya yego formirovaniya i ablyatsiya lednikov o. Zapadnyy Shpitsbergen v 1965 [Heat balance, the conditions of formation and ablation of glaciers in Vestspitsbergen in 1965] Problemy Arktiki·i Antarktiki, Vyp. 29, 1968, p. 80–88.Google Scholar
Nye, J.F. The advance and retreat of glaciers. Weather,Vol. 24. No. 12, 1969,p. 501–12. [Text of sixth Margary Lecture summarizing relation between weather and climate and glaciers.]CrossRefGoogle Scholar
Panov, V.D Kravtsova, V.I. Basseyn reki Kubani [Basin of (he river Kuban'). Katalog lednikov SSSR [Catalogue of glaciers of the U.S.S.R.],Tom 8, Chasti 1–4. Leningrad. Gidrometeorologicheskoye Izdatei'stvo 1967. 124 p. [Part of the I.H.D. catalogue of glaciers of the U.S.S.R. giving details of what is known of the glaciers in this part of North Caucasus. The Tom numbers correspond with those of Resursy poverkhnostnykh nod SSSR [Surface water resources of the U.S-S.R.].]Google Scholar
Pathrson, W.S. B. The physics of glaciers. Oxford, etc., Pergamon Press, 19G9. viii, 250 p. (The Commonwealth and International Library. Geophysics Division.) [Intended for those starting research in elacier studies.]Google Scholar
Péwé,, T. L. Avalanches on glaciers and the effects of snowslidcs; introduction. (In [U.S.] National Research Council. Division of Earth Sciences. Committee on the Alaska Earthquake. The great Alaska earthquake: hydrologr. Part A. Washington. D.C., National Academy of Sciences, 1968, p. 349–54. (Publication 1603 )) [Reviews work described in this section of volume devoted to 1964 earthquake.]Google Scholar
Pillewizer, W. Zur Karte des Kongsvegen-Kroncbre 1: 50,000, Westspitzbergen. Petermanns Geographische Mitteilungen, Jahrg. 111, Quartalsht. 2. 1967, p.,53–57, maps. [Map of Kongsvegen and Kronebreen. Vestspitsbergen, with description of these glaciers. Field-work during German expeditions in 1962 and 1964–65.]Google Scholar
Pillewizer, W. Die wissenschaftlichen Ergebnisse der deutschen Spitzbergenexpedition 1964–1965. Die glaziologischen Arbeiten, [Pillewizer von, J. W., Meier, S., Lorenz, G., Militzer, l., Voigt, U., Oelsner, C. Geodätische und Geophysikalische Veröffentlichungen, Reihe 3, Ht. 9, 1967, 52–138. [Results of glaciological investigations in Kongsfjorden region, Vestspitsbergen. during East German expedition in 1964–65·mainly glacier flow, regime and thickness.]Google Scholar
Plafker, G. Source areas of the Shattered Peak and Pyramid Peak landslides at Sherman Glacier. (In 1U S ) National Research Council. Division of Earth Sciences, Committee on the Alaska Earthquake The great Alaska earthquake,- hydrology. Part A. Washington. D.C., National Academy of Sciences, 1968, p. 374 8a (Publication 1603.)) [Discusses topographic and geologic factors contributing to these landslides which were induced by 1964 Alaska earthquake, and describes dimensions.]Google Scholar
Post, A.S Effects on glaciers. (In [U.S.] National Research Council. Division of Earth Sciences. Committee on the Alaska Earthquake. The great Alaska earthquake; hydrology. Part A. Washington. D.C., National Academy ol Sciences, 1968, p. 266–308. (Publication 1603.)) [Results discussed of air photograph investigations comparing photographs of individual glaciers taken before and after Alaska earthquake of 1964 ]Google Scholar
Renaud, A. Eludes physiques et chimiques sur la glace de l'indlandsis du Groenland 1959 par A Renaud avec des contributions de [14 autres]. Meddelelser om Grønland. Bd. 177. Nr. 2. 1969 133 p [Study of hydrogen and oxygen isotope ratio, of 210Pb, and of gas composition in Greenland icejGoogle Scholar
Sadler, I. Observations on the ice caps of Galindez and Skua Islands, Argentine Islands, 1960–66 British Antarctic Survey Bulletin, No. 17, 1968, p. 21–49. [Accumulation and ablation measurements 1965–66]Google Scholar
Schram, K. Untersuchung der vertikalen Komponente der Gletscherbewegung und der Deformation des Eises im Zungengcbicl des Hintereisferners. Bericht des. Naturwissenschaftlich-medizinischen Vereins in Innsbruck. Bd. 54 1966, p. 75–150. [Measurement of vertical component of glacier velocity on tongue of this glacier and of strain-rate. English summary.]Google Scholar
Schweizer, G. Büsserschnee in Vorderasien. Erdkunde, Bd. 23, Ht. 3. 1969, p. 200–05. [Penitente formations in Middle East. English summary, p. 200.]Google Scholar
Seckel, H. Storer, M. Höhcnänderung des grönländischen Inlandeises 1959–1968. Polarforschung Bd 6 Jahrg. 38, Nr 1–2 1968 [pub. 1969J, p. 215–21. [Results of two levelling profiles of Greenland ice sheet and comparison of surface altitudes and waves. English abstract.]Google Scholar
Shreve, R. L. Sherman landslide. (In [U.S.] National Research Council. Division of Earth Sciences Committee on the Alaska Earthquake. The great Alaska earthquake; hydrology. Part A. Washington DC National Academy of Sciences, 1968, p. 395–401. (Publication 1603.)) [Discusses unusual features of landslide on Sherman Glacier, triggered by 1964 Alaska earthquake.]Google Scholar
[SOVIET CENTRAL. ASIA: GLACIOLOGY.] Teplovoy i vodnyy rez.him lednikov Kazakhslana [Heal and water regime of the glaciers of Kazakhstan]. Akademiya. Nauk Kazakhshoy SSR. Sektor Fizicheskoy Geografii. Glyatsiologicheskiyc issledovaniya v Kazakhstane [Academy of Sciences of the Kazakh S.S.R. Sector of Physical Geography. Glaciological investigations in Kazakhstan}. Vyp. 8. Alma-Ata, Izdatel'stvo “Nauka” Kazakhskoy SSR, 10,69. 160 P-[Contains the following papers, all in Russian with English summaries: N. N. Pal'gov, “Hydrologie balance of the glacio-nival landscape (as represented by the Maloalmatinka glacio-nival bell)”, p. 5–16; Ye. N. Vilesov, “Contemporary glacierization of the Kazakhstan Altay”, p. 17–27; K. G. Makarevich, “Regime and budget problems of the Berel'sk glaciers in the Altay”, p. 28–40; K. G. Makarevich and others. “Electrical sounding of the Lednik Korzhenevskiy, its run-off and mass balance”, by K. G. Makarevich, I. Ya. Fedulov and S. A. Borovinskiy, p. 41–50; G. A. Rakhimzhanova and T. Ya. Denisova. “Weather characteristics of the basic forms of atmospheric circulation during the warm season in the Zailiyskiy Alatau glaciers”, p. 51–57; P. A. Sudakov and G. A. Tokmagambetov, “Preliminary data on distribution of precipitation and snow reserves in the nival-glacial zone in the south-eastern part of the Chiliko-Keminskiy mountain complex”. p. 58–68; P. A. Sudakov and V. A. Chekhonadskaya, “Quantitative assessment of the total annual précipitation in the Zailiyskiy Alatau”, p. 69–74; P- A. Sudakov and others, “Snow accumulation on the glaciers of the Zailiyskiy Alatau range”, by P. A. Sudakov, G. A. Tokmagambetov and V. A. Chekhonadskaya. p. 75–86; G. A. Tokmagambetov and P. A. Sudakov, “Structure of the firn-ice layer in the accumulation region of glaciers in the south-eastern part of the Chiliko-Keminskiy mountain complex”, p. 87–90; P. A. Cherkasov, “Basic features of contemporary glacierization of the Biyon and Aksu river basins in the Dzhungarskiy Alatau”, p. 91–108; V. A. Chekhonadskaya and others. “On the question of the distribution of atmospheric precipitation in the Dzhungarskiy Alatau”, by V. A. Chekhonadskaya, N. V. Yerasov and R. S. Bekten'yarov, p. 109- 13; V. A. Chekhonadskaya. “Ice melting and run-off from glaciers of the rivers Aksu and Biyon in the Dzhungarskiy Alatau”, p. 114–23; A. P. Voloshina, “Investigation of heal balance in the firn area of Lednik Tsentral'nyy Tuyuksu”, p. 124 40; N. N. Pal'gov. “The firn line as an index of the hydrological regime of glaciers”, p. 141–48; K. G. Makarevich and P. F. Shabonov, “Ice ablation and run-off from the Maloalmatinka glaciers during the period 1963 67”, p. 149–57.]Google Scholar
Stenborg, T. Channel formation and glacier drainage. Geogrnfiska Annaler, Vol, 51A, No. 3, 1909, p. 112—13. [Comments on C. M. Clappcrton's paper, ibid., Vol. 50A, No 4. 1968, p. 207–20. concerning interpretation of melt-water channels and physics of penetration of water in glaciers.]Google Scholar
Thompson, R.D. Glaciological research on Mt. Ruapehu. .New Zealand Geographical Society Record. No. 45. 1968. p. 6–8. [Aims of a project to measure meteorological and mass balance quantities on the. Whakapapanui Glacier, North Island. New Zealand. |Google Scholar
Traxl, E. Firnfeldschwaukungen, Gletscherhaushalt und Klimaelemente. Carinthia II. Mitteilungen des Naturwissenschaftlichen Vereines fur Kärnten. 78. Jahrg.. 1968, p. 5–17. [Relation between variations in accumulation. glacier fluctuations, and meteorological elements,]Google Scholar
Tushinskiy, G. K" ed. Otedeneniye El’brnsa [Glacierization of El'bras}. [Moscow], Izdatel'stvo Moskovskogo Universiteta, 1968. 345 p. [Book on the glaciers flowing from this volcanic mountain in the Caucasus with sections by many individual authors on all aspects of the glaciulogy.]Google Scholar
Tuthill, S.J. Earthquake-triggered rock avalanches and glacial stagnation in south central Alaska. (In [U.S.] National Research Council. Division of Earth Sciences. Committee on the Alaska Earthquake. The great Alaska earthquake; hydrology. Part A. Washington, D.G.. National Academy of Sciences. 1968, p. 362–08. (Publication 1603.)) [Discusses rock avalanche slides, resulting from 1964 earthquake, on to four glaciers (Sherman, Slide, Martin River, Schwan) which will affect regime of these glaciers.]Google Scholar
Tuthill, S.J., Postearthquake studies at Sherman and Sheridan glaciers, by Tuthill, S.J., Field, W.O., Clayton, L. {In [U.S.J National Research Council. Division of Earth Sciences. Committee on the Alaska Earthquake. The great Alaska earthquake; hydrology. Part A. Washington, D.C, National Academy of Sciences, 1968, p. 318–28. (Publication 1603.)) [Predictions of future glaciological and ecological behaviour of Sherman Glacier, as a result of earthquake-induced rock avalanche of 1964, compared with unaffected Sheridan Glacier.]Google Scholar
Vilesov,, YE. N. Khonin, R.V. Basseyny levykh pritokov r. Ili ot ust'ya r. Kurty do ust'ya r, Turgen’ [Basins of the left tributaries of the river Ili from the mouth of the Kurty to the mouth of the Turgen']. Katalog lednikov SSSR [Catalogue of glaciers of the U.S.S.R.]. Tom 13, Vyp. 2, Chast' 1. Leningrad, Gidro-meteorologicheskoye Izdatel'stvo, 1967. 79 p. [Part of the I.H.D. catalogue of glaciers of the U.S.S.R. giving details of what is known of the glaciers in the basin of Ozero Balkhash. The Tom and Vyp. numbers correspond with those of Resursy poverkhnoslnykh vod SSSR [Surface wetter resources of the U. S.S.R.}.]Google Scholar
Vivian, R. Fiches des glaciers français. Glaciers des Bossons et de Taconna. Reçue de Géographie Alpine, Tom. 57. Fasc. 4, 1969, p. 871–74. [Summary of knowledge of these glaciers.]CrossRefGoogle Scholar
Vivian, R. Chinai, M. Fiches des glaciers français. Le glacier de Ghavière. Revue de Géographie Alpine, Toni. 57, Fase. 4, 1969, p. 875–77. | Summary of knowledge of this glacier.]CrossRefGoogle Scholar
Wagner, W.P. Description and evolution of snow and ice surface forms on the Kaskawulsh Glacier. (In Bushneil, V.C., Ragle, R.H. ed. Icefield Ranges Research Project. Scientific results. Vol. 1. New York, American Geographical Society; Montreal, Arctic Institute of North America, 1969, p. 51–53.) [Study in pits of sequential development of surface and sub-surface features in accumulation area in summer.]Google Scholar
Wagner, W.P. Snow facies and stratigraphy on the Kaskawulsh Glacier. (In Bushneil, V.C., Ragle, R.H. ed. Icefield Ranges Research Project. Scientific results. Vol. 1. New York, American Geographical Society; Montreal. Arctic institute of North America, 1969, p. 55–62.) [Measurements of snow temperature, density, hardness, accumulation and stratigraphy in accumulation area and deductions.]Google Scholar
Zinger,, YE. M., Troitskiy., L. S. Sovetskiye glyatsiologicheskiye issledovaniya na Shpitsbergene v 1967 g. [Soviet glaciological studies in Spitsbergen in 1967]. Izvestiya Akademii A'auk SSSR. Seriya Geograficheskaya, 1968, No. 3, p. 161–62. [Organized by Institut Geografii and led by Zinger,]Google Scholar

Icebergs. Sea, River and Lake Ice

Antonov,, V S Ledovyy rezhim ust'ycvoy oblasti r. Leny v yestestvennom i zaregulirovannom sostoyanii [Natural and controlled ice regime of the mouth of the river Lena]. Izvestiya Vsesoyuznogo Geograficheskogo Obshchestva,Tom 101, Vyp. 3, 1969. p. 201–09.Google Scholar
Buynitskiy, V.K.H. Stroyeniye, osnovnyye svoystva i prochnost' morskikh antarkticheskikh I'dov [Structure main properties and strength of Antarctic sea ice], Informatsionnyy Byulleten' Sovetskoy Antarkticheskoy Ekspeditsii No. 05. 1967. p. 90–104.Google Scholar
Buynitskiy, V. KH. Vliyaniye mikroskopicheskikh vodorosley na stroyeniyc i prochnost' morskikh autarkticheskikh l’dov [Influence of microscopic algae on the structure and strength of Antarctic sea ice]. Okeano-logiya. Tom 8. Vyp. 6. 1968. p. 971–79.Google Scholar
Heinsheimer, J.J. ¿QUC cantidad de hielo flota en los mares? Boletin del Servicio de Hidrografia Naual (Buenos Aires), Vol 4. No. 2. 1967 [pub. 1968], p. 215–23. [Estimate of total volume of sea ice and of icebergs floating in the sea. English and German summaries.]Google Scholar
Hoshiai, T. Shōwa-kichi ni okeru kaihyōka no kororofiru-a ryō to kankvō-jōken no kisetsu-henka [Seasonal variation of chlorophyll-a and hydrological conditions under sea ice at “Syowa” station Antarctica] Nankyoku Shiryō: Antarctic Record. No. 35. 1969. p. 52–67. [Study of conditions under sea ice including marked effect of thaw water. English abstract.]Google Scholar
Kühnel, I. Die Eisabschmelzzeiten für die Ostsee östlich der Linie Trelleborg-Arkona und für den Finnischen und Rigaischen Meerbusen sowie für die südlichen Randbezirke der Bottcnsee. Deutsdu Hydrographische Zeitschrift. Jahrg. 21 Ht. 1. 1968, p. 15–20. [Calculaiion of times of melting of ice for very cold and normal winters for areas of Baltic Sea south of lat. 61° N. and east of line Trelleborg-Arkona and for Gulfs of Finland and Riga and southern peripheral areas of Gulf of Bothnia.]CrossRefGoogle Scholar
Litinskiy,, V A Obnaruzheniye ostatkov amerikanskoy dreyluyushchey stantsii “Charit” V rayone k sevcru ot o Vrangelya [Discovery of the remains of the American drifting station “Charlie” in the region north of Ostrov Vrangelya. Problemy Arktiki i Antarktiki, Vyp. 28. 1968. p. 140–45. [May 1966. Course of drift since 1962 estimated.]Google Scholar
Schmidt, E. Über die Ursache von Rissen in der Eiskappe des nördlichen Polarmeeres. Archiv für Meteorologie Geaphysik, und Bioklimatologie, Ser. A. Vol. 18, No. 3–4. 1969. p. 39, 94. [Long. racks in sea ice over Arctic Ocean can be caused by wind generated stress. English summary.]Google Scholar
Snider, C.R Linklater., G. D. Great Lakes ice season of 1968. Monthly Weather Review, Vol. 97. No 4 1969, p. 315–32. [Theory and practice of ice forecasting and results for 1967–68.]2.3.CO;2>CrossRefGoogle Scholar
Strübing, K. Über Zusammenhänge zwischen der Eisführung des Ostgrönlandstroms und der atmosphärischen Zirkulation über dem Nordpolanneer. Deutsche Hydrographische Zeilschrifi, Jahrg. 20, Ht 6 1967 p 257–65 [Relation between ice transport in East Greenland current and atmospheric circulation over Arctic Ocean English and French summaries.]CrossRefGoogle Scholar
Tunnell, G. A Synoptic ice maps of the Meteorological Office. Journal of the Institute of Navigation. Vol 21 No. 4. 1968. p. 439–47- [Describes preparation every 10 days of maps showing distribution of ice in Arctic Basin and areas adjacent to North Atlantic Ocean.]CrossRefGoogle Scholar
Untersteiner, N. Maykut., G. A. Arctic sea ice. Naval Research Reviews. Vol. 22. No. 5. 1969 p 12–13. [Presents results of thermodynamic model which describes growth and decay of sea ice. No evidence to support idea that Arctic ice is melting.]Google Scholar
Vasil’yev,, S S luchininov,, V. S. Elektrirhcskiye kharakteristiki l'da [Electrical characteristics of icel. Trudy Arkticheskogo 1 Atitarkhclieskogo Nauchno-Issledovatel’skego Instituta,Tom 284. 1968 p 115–19.[Dielectric penetration of fresh-water and salt-water ice.]Google Scholar
Ventdrov,, S. L., Stezhenskaya., I. N. Izmeneniya strokov ledovykh faz posle sozdaniya krupnykh vodo-khranivlishch [Change of glacial regime after the creation of storage reservoirs]. Izvestiya Akademii. Yauk SSSR. Seriya Geagraficheskaya. 1969. No. 1. p. 50–58. [Discussion of factors causing change in duration of ice on rivers after reservoir construction.]Google Scholar
Voyevodin, V.A. Mironov., L. V. Opyt opredeleniya tolshchiny plavuchikh l'dov pri pomoshchi stereofoto-grammctrichcskoy obrabotki aerosnimkov [Attempt to determine the thickness of floating ice with stereo air photographs]. Okeanologiya,Tom 8. Vyp. 2. 1968, p. 327–36. [Measurement of height above water and computation of total thickness.]Google Scholar
Yeskin, L.I. Morskiye I'dy Yuzhnogo Okeana [Sea ice of the Southern Ocean]. Problemy·Arktiki i Antarktiki. Vyp. 31, 1969. p. 24–30. [General characteristics, especially in Mirny region.]Google Scholar
Zaytsf., V V A., Lomakin., Λ. N. Radioieplovoye izlucheniye ledyanogo pokrova v diapazone 3-10 cm Radiothermal radiation of the ice cover in the 3-10 cm range]. Trudy Arkticheskogo i Antarkticheskogo Nauchmo-Issledovatel’ skogo Instituta. Tom 284, 1968. p. 84–88. [Observations on fresh-water floating ice ]Google Scholar
Zubkovich, S.G. Vliyaniye sherokhovatosti granits vozdukh-led i led-voda na effektivnost' radiotekhnicheskikh interferentsionnykh metodov opredeleniya tolshchiny l'da [influence of roughness at the ice-air and ice-water interface on the effectiveness of radio interference methods of determining ice thickness], Trudy Arkticheskogo i Antarkticheskogo Nauchna~Issledovatel'skogo Institute,Tom 284. 1968. p. 89–99.Google Scholar

Glacial Geology

Andersen, B. G. Glacial geology of western Troms, north Norway. .Norges Geologiske Undersekalse, No. 256. 1968 160 p. [Moraine chronology study indicates six main glacial phases,]Google Scholar
Andrews, J.T. The shoreline relation diagram: physical basis and use for predicting age of relative sea levels (evidence from Arctic Canada). Arctic and Alpine Research. Vol. 1. No. 1, 1969, p. 67–78 [SR diagram constructed from equation of form of post-glacial uplift, and used to predict age and elevation of marine limits, glacial lake strand-lines, and lower relative sea-levels.]CrossRefGoogle Scholar
Anundsen, K. SIMONSEN, Λ. Et pre-borealt breframstøt på Hardangervidda og i områdel mellom Bergenbanen og Jotunheimen. Årbok for Universitetet i Bergen. Matematisk-Naturvitenskapelig Serie, 1967, No. 7. [pub. 1968], 42 p. [Moraine ridges in Hardanger and Sogn, west Norway, indicate Pre-Boreal re-advance of inland ice. English summary.}Google Scholar
Biju-Duval,, B., Gariel,, O. Nouvelles observations sur les phénomènes glaciaires, “éocambnens de la bordure nord de la synéclise de Taoudcni, entre le Hank et le Tanezrouft, Sahara occidental. Palaeogeography, Palaeoclimatology, Palaeoecology, Vol. 6, No. 4, 1969, p. 283–315. [Observations of “Eocambrian tillite” in this part of North Africa.]Google Scholar
Bjørlykke,, K, The Eocambrian “Reusch moraine” at Bigganjargga and the geology around Varangerljord; northern Norway. .Norges Ceologiske Undersekelse, No. 251, 1967, p. 18–44. [Field-work in 1965. Norwegian summary.]Google Scholar
Braytseva, O.A. Yevteyeva, I.S. Kolebaniya klimata i pleystotsenovyye oledenemya na Kamchatke [Fluctuations of climate and Pleistocene glaciations in Kamchatka]. Geologiya i Geofizika, 1968, No. 5, p. 16–22.Google Scholar
Bryson, R.A. Radiocarbon isochrones on the disintegration of the Laurenude ice sheet, by Bryson, R.A., Wendland, W.M., Ives, J.D., Andrews, J.T. Arctic and Alpine Research, Vol. 1, No. 1, 1969, p. 1–13. [Utilizes existing radiocarbon and geological data to map ice sheet perimeter through time (13 000-5 000 B.P.). Implications of results discussed.]CrossRefGoogle Scholar
Chebotakeva, N.S. Paleogeografiya i khronologiya poslednego yevropeyskogo lednikovogo pokrova [Palaeogeography and chronology of the last European ice sheet], Izvestiya Akademii Nauk SSSR. Seriya Geograficheskaya, 1967, No. 6, p. 94–98.Google Scholar
Corbel,, ]. Recherches sur l'inlandsis quaternaire en Norvège septentrionale. Tramsø Museums Skrifter, Vol. 7, Ht. 6, 1968, p. 75–95. [Study of Quaternary ice sheet in northern Norway. Norwegian summary.] CURRY, R. R. Holocene climatic and glacial history of the central Sierra Nevada, California. Geological Society of America. Special Paper No. 123, 1969, p. 1–47. [Chronology of climatic fluctuations based on fluctuations of mean snowfall.]Google Scholar
Gerasimov, I.P. ed. Posledniy lednikovyy pokrov na senero-zapade yevropeyskoy chasti SSSR [The last glaciation in the north-west of European U.S.S.R.]. Moscow, Izdatel'stvo “Nauka”, 1969. 322 p. [Papers for eighth INQUA congress, Paris, 1969.]Google Scholar
Hamilton, T.D. Glacial geology of the lower Alatna valley, Brooks Range, Alaska. Geological Society of America. Special Paper No. 123, i960, p. 181–223. [Interpretation of evidence of multiple glaciations oldest of which is thought to be Illinoian in age.]Google Scholar
Hansen, K. Glacialgeologiske og sedimentologiske undersogelser ved Eqc—Vestgranland. Meddelelser fia Dansk Geologisk Forening, Bd. 18, Ht. 3-4, 1968, p. 306–14. [Study of moraines and glacial deposits in Eqe bay, West Greenland. English summary.]Google Scholar
Hillefors,, Â. Västsveriges glaciala historia och morfologi. Naturgeograliska studier. Meddelanden frdn Lunds Uinversitets Geografiska Institution Avhandlingar, 60, 1969, 319 p. [General geographical study of glacial deposits in this region of Sweden. English summary, p. 294–305, English translations of figure captions.]Google Scholar
Hult, J. Some aspects of the shore formations on lake Lylykkäänjärvi, Finland. Fennia, 97, No. 5, 1968 [1967–68 on cover], 22 p. [Ice ramparts on south-western and north-western shores formed by ice-push.]Google Scholar
Ives, J.D. Buckley, J.T. Glacial geomorphology of Remote Peninsula, Baffin Island, N.W.T.. Canada. Arctic and Alpine Research, Vol. 1, No. 2, 1969. p. 83–95. [Physiography described (high mountains, coastal uplands, glacial troughs, coastal lowlands) and used to interpret glacial geomorphology, especially significance of moraines. Probable appearance during Pleistocene discussed.]CrossRefGoogle Scholar
Jones, J A A The truth about ice-shove or the origins of certain “ice-shove” features on the lakeshores of central Labrador-Ungava. Geographical Articles (Cambridge). No. 11, 1968, p. 4.7-54. [Reviews and discusses work on lake-shore ice damage.]Google Scholar
King, C.A.M., Buckley, J.T. Geomorphological investigations in west-central Baffin Island, N.W.T.,Canada. Arctic and Alpine. Research, Vol. 1, No. 2, 1969. p. 105–19. [Presents details of glacial, glacio-fluvial, and periglacial forms of west coast region, between Eqe Bay and Foley Island. Comments on icings on edge of coastal flats.CrossRefGoogle Scholar
Klaer, W. Glazialmorphologische Probleme in den Hochgebirgen Vorderasiens. Erdkunde, Bd. 23, Ht. 3, 1969. p. 192–200. [Dominant influence of radiation on geomorphological processes in the high mountain regions of the Middle East. English summary, p. 192–93.]CrossRefGoogle Scholar
Klkmsdal, T. A Lista-stage moraine on Jahren. Norsk Geografisk Tidsskrifi, Bd. 23, Ht. 4, 1969, p. 193–99. [Tracing of moraine near south-west coast of Norway that marks edge of ice sheet about 14 000 years B.P.]CrossRefGoogle Scholar
Krinsley, D.H Recognition of pre-Pleistocenc glacial environments. Bulletin of the American Association of Petroleum Geologists, Vol. 53, No. 3, 1969, p. 727. [Abstract only. Survey of methods of identification.] Lauer, W. Die Glaziallandschaft des südchilcnischen Seengebietes.Acta Geograplnca, 20, 1968, p. 215–30. [Glacial geology of lake district in south Chile. Field-work in 1956–58 and 1966.]Google Scholar
LaverdiÈre,, C. The Scheffcr ice-sheet: a reply to Ives' comments. Canadian Geographer, Vol. 13, |No.J 3, ibid. p. 269–83. [Reply (in French) to J. D. Ives' comments, ibid., Vol. 12, [No.] 3, 1968, p. 192–203.]Google Scholar
LaverdiÈre,, C Les types de broutures glaciaires (glacial challermarks): 2, observations effectuées au Québec. [Par] Laverdière, C., Bernard, C., {-G., J.] Dionne. Revue de Géographie de Montréal, Vol. 22, No. 2, 1968, p. 159–73. [Detailed descriptions and photographs of glacial chattermarks collected in Quebec]Google Scholar
Mercer, J.H. Glaciation in southern Argentina more than two million years ago. Science, Vol. 164, No. 3881, 1969, p. 823–35. [Till beds covered by lava deposits that can he dated by potassium-argon method.]CrossRefGoogle ScholarPubMed
Miller, C D Chronology of neoglacial moraines in the Dome Peak area, North Cascade Range, Washington. Arctic and Alpine Research, Vol. 1, No. 1, 1969, p. 49–65. [Describes project to: map and date post-Wisconsin moraines located beyond present termini of glaciers in Dome Peak vicinity; develop detailed chronology of glacier fluctuations for Dome Peak area during neo-glaciation; and compare and correlate sequence with other neo-glacial chronologies elsewhere in north-west North America.]CrossRefGoogle Scholar
Mohan, J.M. Bryson, R.A. The contribution of Lauientide ice wastage to the eustatic rise of sea level: 10,000 to 6,000 n.p. Arctic and Alpine Research, Vol. 1, No. 2, 1969, p. 97–104. [Wasting of Laurentide ice was major source of rise (nearly three-quarters), while European contribution accounted for remainder.]Google Scholar
Mörner,, N.-A. The late Quaternary history of the Kattegatt sea and the Swedish west coast. Déglaciation, shorelevel displacement, chronology, isostasy and eustasy. Sveriges Geologiska Undersökning, Avhandlingar och Uppsatser, Ser. C, No. 640, Arsbok 63, No. 3, 1969, 487 p. [Russian summary.]Google Scholar
Peterson,, J. A. Cirque morphology and Pleistocene ice formation conditions in southeastern Australia. Australian Geographical Studies, Vol. 6, No. 1, 1968, p. 67–83. [Studies in New South Wales and Tasmania.]CrossRefGoogle Scholar
Peterson, J.A. Robinson, G. Trend surface mapping of cirque floor levels. Nature. Vol. 222, No. 5188. 1969, p. 75–76· [Study of distribution of cirque floor levels in Tasmania, and of regional and local causes of variation,]CrossRefGoogle Scholar
Pratt, R. Schlee, J. Glaciation on the continental margin off New England. Geological Society of America. Bulletin, Vol. 80, No. 11, 1969. p. 2335–41. [Estimate of maximum limit of last glaciation off this part of eastern coast of U.S.A.]CrossRefGoogle Scholar
Reite, A.J. Lokalglaciasjon på Sunnniøre. (On the mountain glaciation of Sunnmare, west Norway.) Norges Geologiske Undersekelse, No. 247, Arbok 1966, [pub.] 1967. p. 262–87. [Describes terminal moraines deposited by cirque glaciers in late-glacial or post-glacial time. English summary.]Google Scholar
Resske, F. Topographic, Morphologie und Morphogcnesc einer Eisrandlage. Hamburger Geographische Studien, Sonderheft, 1968, vi. ia2 p., maps [in folder at back], [Intensive topographical, cartographic and morphological study of 230 ha area of the edge of Wurm ice sheet.]Google Scholar
Shcherbakova,, YE. M. O polozhenii drevney snegovoy granitsy na Bol'shom Kavkaze [On the position of the old snow line in the Great Caucasus]. Vestnik Moskomkogo Universiteta, Ser. 5, God 24, No. 6, 1969, p. 8–15. [Need to distinguish climatic (or regional) and orographie snow lines when interpreting traces of old glaciations. English abstract, p. 15.]Google Scholar
Sollid, J.L. A 48,000 years old tree stump, presumably of spruce, found in Ringerikc, south Norway. Norsk Geografisk Tidsskrift. Bd. 23, Ht. 3, 1969, p. 131–33. [Find of tree stump whose radio-carbon date implies lower parts of southern Norway were ice-free at this time.]CrossRefGoogle Scholar
Sollid, J.L. Iskulminasjoner i Sör-Norge under deglasiasjonen. Geologiska Föreningens i Stockholm Förhandlingar, Vol. 90, Pt. 3. No. 534, 1968, p. 473. [Abstract only. Discussion of location of ice divide as ice sheet melted over south Norway.]Google Scholar
SzupryczyŃski,, J. Niektóre zagadnienia czwartorz$$du na obszarze Spitsbergenu. Prace Geograficzne, No. 71, 1968, 128 p. [Study of Quaternary in Spitsbergen. Field-work in 1959, i960 and 1963. English and Russian summaries.]Google Scholar
Tremblay, G. Note sur les crêtes morainiques de Saint-François-de-Salles (région du Lac-Saint-Jean, Québec).Cahiers de Géographie de Québec, 12e An.. No. 27, 1968. p. 429–42. [Study of origin of moraine ridges in this region.]CrossRefGoogle Scholar
Trofimov, A.K. O rezhime lednikov Pamira v golostene [Regime of Pamir glaciers in the Holocene]. Izvestiya Vsesoyuznogo Geograficheskogo Obshchestva, 'Yarn 101, Vyp. 2, 1969, p. 118–24. [Geomorphological study and deductions.]Google Scholar
Weis, P. L, Glacial drainage in the Skagit Valley, Washington. U.S. Geological Survey. Professional Paper 650-C,1969, p. C71–C74. [Explanation of anomalous V-shaped valley as having been under a drainage divide of the ice sheet.]Google Scholar
West, R.G. Pleistocene geology and biology with especial reference to the British Isles, London, Longmans, Green and Go. Ltd., 1968. xiii. 377 p. [General account of Pleistocene in glaciated and non-glaciated regions of northwest Europe. Includes chapters on ice and glaciers, and glacial geology.]Google Scholar
White, G.W. The first appearance in Ohio of the theory of continental glaciation. Ohio Journal of Science, Vol. 67, No. 4, 1967, p. 210–17. [Report of S. St. John's early adoption of the glacial theory and his application of it in Ohio.]Google Scholar
White, G.W. Pleistocene deposits of the north-western Allegheny Plateau, U.S.A. Quarterly Journal of the Geological Society of London, Vol. 124, Pt. 2. No. 494, 1969 [for 1968], p, 131-51, [Recent deep excavations have made possible a study of sections through till sheets which give more evidence on their nature and extent. Discussion, p. 149–51.]Google Scholar
Wright, H.E.jr Quaternary geology and climate. Vol. 16. of the Proceedings of the V11 Congress of the International Association for Quaternary Research. Washington, D.C., [U.S.] National Academy of Sciences, 1969, ix, 162 p. [Includes the following papers: Picard, K.E., “Pleistocene tectonics and glaciation in Schleswig-Holstein, Germany”, p. 67–71; Gerasimov, I.P., “Degradation of the last European ice sheet”, p. 72–78; Chebotareva, N.S., “Recession of the last glaciation in northeastern European USSR”, p. 79–83; Strelkov, S.A., “Main events in the evolution of relief in northern Eurasia and their tentative correlation with those in North America”, p. 84–88; F. M. Synge, “The Wurm ice limit in the west of Ireland”, p. 89–93; Dreimanis, A., Vagners, U.J., “Lithologie relation of till to bedrock”, p. 93–98; Bayroek, L.A., “Incomplete continental glacial record of Alberta, Canada”, p. 99–103; N. W. Rutter. “A Late-Pleistocene glacial advance. Bow River Valley, Alberta, Canada”, p. 104–09; IX S. Simone» and Brown, D.A., “Uses of satellite-borne radar to study Antarctic ice conditions”, p. 110–15; J· Demek, “Importance of slope deposits in the study of landscape development”, p. 130–33.]Google Scholar
Young, J.A. T. Variations in till microfabric over very short distances. Geological Society of America. Bulletin, Vol. 80, No. 11, 1969, p. 2343–52. [Measurements of stone orientations and variations with depth and laterally,]CrossRefGoogle Scholar

Frost action on Rocks and Soil. Frozen Ground, Permafrost

Black, R.K. Climatically significant fossil periglacial phenomena in northcentral United States. Biuletyn Peryglacjalny, No. 20, 1969, p. 235–38. [Discussion of which periglacial phenomena are of most use in interpreting palaeoclimates.]Google Scholar
Bobov, N. G, Formirovaniye plaslovykh zalezhey I'da [Formation of sheet ice fields]. Izeestiya Akademii. Nauk SSSR. Seriya Geograficheskaya, 1969, No. 6, p. 63–68. [Formation of horizontal ice layers in frozen ground.]Google Scholar
Brown, R.J. E. Permafrost map of Canada. Canadian Geographical Journal,Vol. 76. No. 2, 10.68. p. 56–63. [Map accompanied by description of Canadian research on distribution and nature of permafrost, and associated engineering problems.)Google Scholar
Dionne, J.-C. Bibliographie du périglaciaire du Québec. Renie de Géographie de Montréal, Vol. 22, No 2. 1908, p. 175–80. [A bibliography of periglacial studies in Quebec.]Google Scholar
Furrer, G.J. Untersuchungen an Strukturböden in Ostspitzbergen, ihre Bedeutung für die Erforschung rezenter und fossiler Frostmusterformen in den Alpen bzw. im Alpenvorland. Polarforschimg. Bd. 6, Jahrg. 38. Nr. 1–2, 1968 [pub. 1969]. p. 202–06. [Observations of stone orientation in patterned ground in Svalbard and discussion.]Google Scholar
Furrer, G.J Vergleichende Beobachtungen am subnivalen Farinemchatz in Ostipitzbergen und in den Schweizer Alpen. Wiesbaden. Franz Steiner Verlag GmbH. 1969. vii, 40 p. (Ergebnisse der Stauferland-Expedition 1967. Deutsche Expedition nach Südost-Spitzbergen, Ht. 9.) [Comparison of patterned-ground forms in Svalbard with those in the Alps.]Google Scholar
Gabert, P. Lalutridou, J.-P. Gélifraction artificielle et gélifraction au cours du Quaternaire. Étude comparée à propos des calcaires lacustres de la région d'Aix-en-Provencc. Méditerranée. 10° An., No, 3, 1969. p. 293–312. [Cold-chamber experiments on frost action on calcareous rocks and comparison with Quaternary deposits in this region of France.]CrossRefGoogle Scholar
Gardner, J. Snowpatches: their influence on mountain wall temperatures and the geomorphic implications. Geografiska Annaler, Vol. 51.A, No. 3, 1969, p. 114–20. [Measurements on two snow-patches in the Rocky Mountains, Canada, and discussion of implications for freeze-thaw rock shattering.]CrossRefGoogle Scholar
Goodier, R. Ball., D. F. Recent ground pattern phenomena in the Rhinog Mountains, North Wales. Geografiska Annaler, Vol. 51.A. No. 3, 1969. p. 121–26. [Description of patterned ground phenomena, some formed from an old wall, attributed to conditions between A.D. 1550 and 1750. |CrossRefGoogle Scholar
Gordunov, A.P. Vechnaya merzlota Tyan'-Shanya [Permafrost in the Tien Shan]. Frunze, Izdatel'stvo “Him”. 1967. 165 p.Google Scholar
Gorbunov, A.P. KonkashpayeV, G.K.. Nekotoryye merzlotnyye toponimy Tyan'-Shanya i Pamira [Some permafrost place-names of the Tien. Shan and the Pamir], Vestnik Moskovskogo Universiteta, Ser. g, God 24, No. 6, 1969, p. 83–84. [Place-names that indicate presence of permafrost, icing fields and taliks. English abstract, p. 84. |Google Scholar
Gravis, G. Fossil, F. slope deposits in the northern Arctic asymmetrical valleys. Biuletyn Peryglacjalny. No. 20, 1969. p. 239–57. [Study of these deposits in Kular range (northern Yakuliya).]Google Scholar
Habrich, W. Vegetationshöcker auf steilgeneigten Terassenhängen in der Frostschultzone Nordostkanadas. Polarforschung. Bd. 6. Jahrg. 38, Nr. 1–2, 1968 [pub. 1969), p, 212-15. [Extension of Biidel's classification of frost soil patterns to include vegetation hummocks on steep terrace slopes. English abstract.]Google Scholar
Jahn,, Λ Structures périglaciaires dans les loess de la Pologne. Biuletyn Peryglacjalny, No 20. 1969, p. 81–97. [Study of frost structures in loess in Poland.]Google Scholar
Kostvavkv, A.G. La zone périglaciaire des plaines de l'Europe de l'Est et de la Sibérie de l'Ouest au Pleistocene. Biuletyn Peryglacjalny, No. 2.o. 1969. p. 259–97. | Discussion of phenomena occurring near the margins of the Pleistocene ice sheet.]Google Scholar
Macnamara, E.E. Soils and geomorphic surfaces in Antarctica. Biuletyn Peryglacjalny, No. 20, 1969, p. 299–320. [Comparison of soils in Enderby Land with those from ice-free areas in Victoria Land and Dronning Maud Land and discussion of weathering processes.]Google Scholar
Pαεγε,, R., PISSART,, A. Periglacial structures in the I,a te-Pleistocene stratigraphy of Belgium. Biuletyn Peryglacjalny, No. 20, 1969, p. 321–36.Google Scholar
Shpolyanskaya, N.A. Osobennosti vechnoy i sczonnoy merzloty zapadnoy Sibiri [Peeularities of perennial and seasonal frozen ground in West Siberia]. Vestnik Moskovskogo Universiteta, Ser. 5. God 24. No. 3. 1969, p. 88–94. [Maps of occurrence, temperature and thickness of frozen soil and of seasonal freezing and thawing of rocks, and discussion. English summary, p. 94.]Google Scholar
Svensson, H. A type of circular lakes in northernmost Norway. Geografiska Annaler, Vol. 51. A, Nos. 1-2, 1969, p. 1–12. I Lakes interpreted as collapse of frost mounds originating as palsas or pingos. Also published as Lund Studies in Geography, Ser. A, No. 45, 1969.]Google Scholar
Tedrow, J. C F. Thaw lakes, thaw sinks and soils in northern Alaska. Biuletyn Peryglacjalny. No. 20, 1969. p. 337–44. [Study of these phenomena which occur in poorly drained terrain underlain by permafrost.]Google Scholar
Tyrtikov, A.P. Vliyaniye rastitel’nogo pokrava na promer zaniye i protaivaniye gruntov [Influence of vegetation on freezing and thawing of soils]. Moscow, Izdatel'stvo Moskovskogo Universiteta. 1969. 192 p. Vostokova, A. V. Otobrazheniye vechnoymcrzloty na kartakh koropleksnykh atlasov [Representation of permafrost on the maps of complex atlases], Vestnik Moskovskogo Universiteta, Ser. 5. God 23. No. 4. 1968. p. 66–72. [Survey of present practice and recommendations for future.]Google Scholar
Washburn, A.L. Weathering, frost action, and patterned ground in the Mestcrs Vig district, northeast Greenland. Meddelelser om Grönland. Bd. 176, Nr. 4, 1969, 303 p.Google Scholar
Williams, P.J. Properties and behaviour of freezing soils. Norges Geotekniske Institutt. Publikasjon No. 72. 1968. 119 p. [Seven papers. French summaries. Also published as Canada. National Research Council. Division of Building Research. Research Paper No. 359..]Google Scholar

Meteorological and Climatological Glaciology

Budvko, M. I. On the causes of climate variations. Meddelanden frân Sveriges Meteorologiska och Hydrologiska Institut. Ser. B. Nr. 28, 1968. p. 6–13. [Discussion of phenomena and their possible causes. Importance of volcanic activity.]Google Scholar
Davitaya, F. F. Atmospheric dust content as a Factor affecting glaciation and climatic change. Annals of the Association of American Geographers. Vol. 59. No. 3. 1969. p. 552–60. [Evidence Brenn solar radiation records and from samples of firn from glaciers that atmospheric dust is increasing and effect of this on albedo and hence mass balance.]CrossRefGoogle Scholar
Grunow, J. Tollner,, H. Nebelniederschlag im Hochgebirge. Archiv für Meteorologie, Geophysik und Ftia-klimatologie. Ser. B, Vol. 17, Nos. 2–3, 1969, p. 201–28. [Method of measuring deposits from fog on Sannblick and relevance of results for mass balance calculations of glaciers.]CrossRefGoogle Scholar
Hess, M. The influence of mountain glaciers on the climate with the Fedchenko glacier in Pamir as example. Przegląd Geografiziczny,Tom 39, Zeszyt 4. 1967. p. 771–74 [Based on author's work on glacier in 1957.]Google Scholar
Page,, J. K. Heavy glaze in Yorkshire—March 1969. Weather. Vol. 24. No. 12. 1969, p. 486–95. [Report of unusually severe icing conditions in this part of England.]CrossRefGoogle Scholar
Pedgley, D.F.. Snow and glaze on Christmas Eve 1968. Weather,Vol. 24. No. 12. 1969, p. 480–85. [Unusual occurrence of snow following rain in Britain. Meteorological explanation.]CrossRefGoogle Scholar
Prodi, F. X-ray images of hailstone's. Journal of Applied Meteorology, Vol. 8, No. 3, 1969,. p. 458–59. [Use of this technique to study particle patterns and bubbles in hailstones.]2.0.CO;2>CrossRefGoogle Scholar

Snow

Benson, C.S. The seasonal snow cover of Arctic Alaska. Arctic Institute of Worth America. Research Paper No. 51,1969, vi, 86 p. [Studies of physical properties of surface layer of seasonal snow and physical processes occurring in, above, and below it are described and discussed.]Google Scholar
Boziiinskiy,, Λ. N. Kriterii obrusheniya snezhnykh lavin [The criteria of snow avalanche formation]. Itogi. Nauki. Seriya Geografiya. Gidrologiya Sushi. Glyatsinlogiya. 1967. [pub.] 1968. p. 42–59. [Critical review of snow layer stability. English summary.]Google Scholar
Clarke, P.C. Snowfalls over south-east England. 1954–1969. Weather,Vol. 24. No. 11, 1969. p. 438–47. [Analysis of frequency of snowfall and meteorological conditions which produce it.]CrossRefGoogle Scholar
Eglit, M.E. Tcorelicheskiye podkhody dvizheniya snezhnykh lavin [The theoretical approach to avalanche dynamics). Itogi Nauki. Seriya Geografiya. Gidrologiya Sushi. Glyalsiohgiya. 1967. [pub.] 1968. p. 60–97. [Critical review of theories of avalanche motion. English summary.]Google Scholar
Grew, E. Mellor., M. High snowfields of the St Elias Mountains.(In Bushneil, V., CRagle, R.H., ed. Icefield Ranges Research Project. Scientific results. Vol. 1. New York, American Geographical Society; Montreal. Arctic Institute of North America, 1969, p. 75–87.) [Effect of surface altitude on snow properties deduced from comprehensive measurements during summer.]Google Scholar
Higuchi, K.. Nihon ni okeru sekkei no hyōgagaku-teki kenkyü |Glaciological studies on permanent snow-patches formed in gulleys in Japan]. Seppyō, [Vol.] 30. [No.] 6. 1968. p. 195–207. [Review of previous observations of permanent snow-patches in Japan. English abstract.]Google Scholar
Jayaweeka, K. Cottis, O.L.F. R, E. Fall velocities of plate-like and columnar ice crystals. Quarterly Journal of the. Royal Meteorological Society,Vol. 95. No. 406. 1969, p. 703–09. [Model experiments used to provide data for theoretical calculation of ice crystal terminal fall velocities.!CrossRefGoogle Scholar
Kikuchi, K. Nankyoku no yuki-nikki [Snow diary at “Syowa” station]. Kyokuchi: Polar. News. [Vol.] 5. [No.] 1, 1969, p. 52–58. [Record of snow crystal forms of precipitation.]Google Scholar
Kravtsova, V. 1. Primeneniye aerofotogrammetricheskikh i kartogrficheskikh metodov v issledovaniyakh lavin [The use of aerial photogrammetric and cartographic methods for avalanche studies]. Itogi. Nauki. Seriya Geografiya. Gidrologiya Sushi. Glyalsiohgiya. 1967, [pub.] 1968. p. 117–32. [Review of applications of these methods. English summary.]Google Scholar
LaChapelle, E.R., Field guide to snow crystals. Seattle and London. University of Washington Press. [1969]. ix. 101 p., illus.Google Scholar
Lisignoli, C.A., Observaciones sobre la relación entre la durez a v la densidad de la nieve en el Antärtico. [by] Lisignoli, C.A., Dalinger, R.E., Machado, E. Contribución del institute Antartico Argentina. No. 92, 1967, 13 p. [Reports results on relation between hardness (i.e. resistance to penetration) and density of snow from 9 pits on Filchncr lee Shelf, Antarctica.]Google Scholar
Manley, G. Snowfall in Britain over the past 300 years. Weather. Vol. 24, No. 11. 1969. p. 428–37. [Study of records of snowfall.]CrossRefGoogle Scholar
Moskalev,, YU. D., ed. Laviny Sredney Azii [Avalanches of Central Asia]. Trudy Srcdneaziatskogo Xauchno-Issledovatel'skogo Gidrometeorologicheskogo Institute, Yyp. 48 (63}, 1969. 164 p. [Collected papers containing the following, all in Russian: Kosarev, M.V.. “Fundamental results in the study of conditions of formation of avalanches on the southern slopes of western Tyan'-Shan”. p. 5–19; Denisov,, YU. M.. “Formation and movement of incompressible snow avalanches”, p. 2o-31; Yu. P. Moskalev. “On empirical equations for the prediction of snow avalanches and on avalanche calculations”, p. 32–61; Moskalev,, YU. D., Yefimov, M.K., “Snowfall conditions in western Tyan'-Shan in connexion with the avalanche formation problem”. p. 62–77; Kharitonov, G.G.. “Snow cover in the region of the avalanche station Naugarzan as a factor in avalanche formation”, p. 78–90; Yefimov, M.K., “The struggle against avalanches in western Tyan'-Shan”, P· 91-103; Korolev, A.I., “On the possibility of control of stability and consolidation of snow on ploughed slopes”, p. 104–11; Runich, A.V., Yemel’yanov, Yu.N. , “Estimation of the altitude range of avalanche activity in western Tyan'-Shan”. p. 112–22; Yu. N. Yemel'yanov and others. “Experience in the study of avalanches in the Pskem river basin”, by Yemel’yanov, Yu.N., Kanayev, L.A., Chirkova, A.A.. p. 123–38; Kozhovnikov, V.S., “Avalanches in the Dukanl river basin”, p. 139–45; Korolev, A.I., “Peculiarities of the wetting of the surface layers of snow in the absence of solar radiation and the possibility of the development in them of avalanches with point fractures”, p. 146–51; Kamalov, B.A., “Regime of accumulated snow in the Syrdar'i basin”, 152-56.]Google Scholar
Nyberg, A. Some observations of snow melt. Meddelanden frail Sveriges Meteorologiska och Hydrologiska Institut, Ser. B, Nr. 28, 1968, p. 35–41. [Description of apparatus lor measuring amount of water running out from snow layer and of observations made with it and compared with those calculated from meteorological observations.]Google Scholar
Öura,, K. Jifubuki no hasset ni kansuru kenkyü [A study of the origin of glacial blizzards], Seppyô, [Vol.] 30, [No.] 6, 1968, p. 169–75. [Criterion for initiation ol blizzard in turbulent air.)Google Scholar
Plotnikov, V.V.K. kharakteristike snezhnikov na Visherskom Urale [Characteristics of the snow-beds in the Vishera Urals]. Izvestiya Vsesoyuznogo Geograficheskogo Obshchestva,Tom 101, Vyp. 3, 1969, p 265–69. [Description of snow-beds and statistics of their location.]Google Scholar
Roberts, T.D. Murray, J.S. Electrostatic precipatkra [sic] of ice fog. Northern Engineer, Vol. 1, No. 1, 1968, p. 4–5. [Laboratory experiments involving electrostatic precipitation prove satisfactory and hold promise for development on large scale.]Google Scholar
ShÔda,, M. Nadare kenkyū no keikō [Tendencies in avalanche studies], Seppyö, [Vol.] 30, [No.] 6, 1968, p. 188–95.Google Scholar
Shurova, I., YE. Mekhanizm vzaimodeystviya dvizhushcheysya snezhnoy massy s nepodvizhnym prcpyatstviyem [The interaction mechanism between avalanching snow masses and stationary structures]. Itogi Nattki. Seriya Geografiya. Gidrologiya Sushi. Gtyatsiokgiya, 1967, [pub.] 1968, p. 98–116, [Critical survey of available methods for calculating avalanche impact. English summary.]Google Scholar
Stevenson, C.M. The snowfalls of early December 1967. Weather, Vol. 23, No. 4, 1968, p. 156–61. [Reasons for heavy fall of snow along south coast of England in December 1967.CrossRefGoogle Scholar
Sulakvelidze, G.K. ed. Fizika snega i snezhnykh lavin [Physics of snow and snow avalanches], Trudy Vysoko-gornogo Geofizicheskogo Instituts, Vyp. 15, 1969, 192 p. p [Collected papers on physics of snow and avalanches. Contains the following papers, all in Russian: Dolov, M.A., “Some questions on the structure of snow cover and the thermophysical properties of moist snow”, p. 3–26; Kumykov, Kh.K., El'mesov, A.M., “On the calculation of the velocity of movement of snow avalanches”, p. 27 35; Dolov, M.A., Kislov, B.V., “Stress relaxation in a snow cover”, p. 36–44; Zalikhanov, M.Ch, Gutiyev, A.V., “Avalanche dangers of the valleys of the rivers Gizel'don and Baddon”, p. 45–60; Zalikhanov, M.Ch, Akayeva, L.A, “The influence of avalanches on the upper tree limit in Kabardino-Balkarin”, p. 61–68; Burtakov, L.A, Kiryukhin, B.V, “On the question of the conditions of formation of avalanche floods in the Baksan gorge”, p. 69–80; Gerasimov, V.A, “Glacial avalanche floods and some questions of the fight against them”, p. 81–91; P. D. Samukashvili, “Incoming short-wave radiation on slopes in the El'brus region”, p. 92–140; Samukashvili, P.D, “On the principal terms in the radiation balance at 'Ledovaya' base”, p. 141–66; Samukashvili, P.D. “On the principal terms in the radiation balance at the spa Nal'chik”, p. 167–86; “Varden Sergeyevich Chitadze (1924–1968)”, p. 187–88.]Google Scholar
Troshkina,, YE. S. Vertikal'naya poyasnost' lavino-obrazovaniya na Barguzinskom khrebte [The altitudinal zonality of avalanche formation in the Barguzin range]. Vestnik Moskovskogo Universitela, Ser. 5, God 24, No. 6, 1969, p. 59–62. I Avalanche danger largest in zone of degraded cirques and deep erosion valleys above tree limit. English abstract, p. 62.]Google Scholar
Ushakova, L.A. Poverkhnostnyye svoystva snega i protsess metamorfizma [Surface properties of snow and the process of metamorphism]. [By] Ushakova, L.A., Kvlividze, V.I., Sklyankin, A.A.. Itogi Nauki. Seriya Geografiya. Gidrologiya Sushi. Glyatsiotogiya, 1967, [pub.] 1968, p. 9–41. [Literature survey on existence of liquid-like layer on ice surface and its role in snow cover metamorphism, English summary.]Google Scholar
Wakahama, G. Sekisetsu-nat e no yūsetsu-sui no shintō [The permeation of snow melt water into snow cover]. Seppyö, [Vol.] 30, [No.] 6, 1968, p. 175–88. [Experimental study of the manner and speed with which water permeates into snow cover. English abstract.]Google Scholar
Yosida, Z. Snow cover mechanics. Science and Technology· (New York), No. 87, 1969. p. 28–29, 32–38. [Review of snow metamorphosis and snow mechanics and their practical applications.]Google Scholar