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Glaciological Literature

Published online by Cambridge University Press:  30 January 2017

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Copyright © International Glaciological Society 1973

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

Conferences

Aver’yanov, V. G. Pervoye zasedaniye Soveta Mezhdunarodnogo antarkticheskogo glyatsiologicheskogo proyekta [First meeting of the Council of the International Antarctic Glaciological Project]. Informatsionnyy Byulleten’ Sovetskoy Antarkticheskoy Ekspeditsii, No. 82, 1971, p. 8082. [Held in Paris, 26–28 May 1970.]Google Scholar
Brown, R. J. E., ed. Proceedings of a seminar on the permafrost active layer, 4 and 5 May 1971. Canada. National Research Council. Associate Committee on Geotechnical Research. Technical Memorandum No. 103, 1971, ii, 63 p. [The following papers were presented: R. J. E. Brown, “Characteristics of the active layer in the permafrost region of Canada”, p. 1–7; G. P. Williams, “Surface heat exchange and permafrost”, p. 8–11; J. D. Mollard, “Photo interpretation and the active layer”, p. 13–19; A. Cailleux, “Observations”, p. 20–25; J. R. Mackay, “Ground ice in the active layer and the top portion of permafrost”, p. 26–30; A. Heginbottom, “Some effects of a forest fire on the permafrost active layer at Inuvik, N. W. T.”, p. 31–36; L. C. Bliss and R. W. Wein, “Changes to the active layer caused by surface disturbance”, p. 37–46; J. R. Radforth, “Effects of off-road vehicle trials on the active layer in tundra”, p. 48–49; J. Y. C. Quong, “Highway construction and permafrost with special reference to the active layer”, p. 50–53; K. L. Hall, “Performance of experimental pipeline at Inuvik, N.W.T. in relation to active layer”, p. 54–62.]Google Scholar
[Conference: Icebergs.] Proceedings of the Canadian seminar on icebergs held at the Canadian Forces Maritime Warfare School, CFB Halifax, Halifax, Nova Scotia, Canada, December 6–7, 1971, under auspices of the Commander, Maritime Command, Canadian Forces. [Ottawa, Dept. of National Defence, 1971.] [viii]. 175 p. [For details of individual papers see elsewhere in this list.]Google Scholar
Golubev, G. N., and Kotlyakov, V. M. Mezhdunarodnyy simpozium po gidrologii lednikov v Kembridzhe [International symposium on the hydrology of glaciers at Cambridge]. Materialy Glyatsiologicheskikh Issledovaniy. Khronika. Obsuzhdeniya, Vyp. 17, 1970, p. 1520. [Glaciological Society symposium, 8–12 September 1969.]Google Scholar

General Glaciology

Gayevskaya, O. V. Izobrazheniye oblachnosti nad l’dom na televizionnykh snimkakh, poluchennykh so sputnikov sistemy “Meteor” [Cloud cover over ice shown in photographs obtained from “Meteor” satellites]. Antarktika. Doklady Komissii, 1969, [pub.] 1971, p. 12228.Google Scholar
[International Hydrological Decade.] Scientific framework of world water balance. Paris, UNESCO, 1971. 27 p. (Technical Papers in Hydrology, 7.) [Frozen water is included as a parameter of the hydrological cycle.]Google Scholar
[International Hydrological Decade.] Textbooks on hydrology. Analyses and synoptic tables of contents of selected textbooks. A contribution to the International Hydrological Decade. Paris, UNESCO, 1970. 185 p. (Technical Papers in Hydrology, 6.) [Part A contains the detailed analysis of 19 different works published in English, French, Russian, Spanish, German and Italian. Part B compares the contents of the hydrological textbooks available to the compilers, regardless of language.]Google Scholar
Kotlyakov, V. M., and Chernova, L. P., comp. Annotirovannyy spisok sovetskoy literatury po glyatsiologii (1967–1968 gg.) [Annotated list of Soviet publications in glaciology (1967–68)]. Materialy Glyatsiologicheskikh Issledovaniy. Khronika. Obsuzhdeniya, Vyp. 18, 1971, p. 219319. [Papers dealing with glaciers and ice cover in the U.S.S.R. and Antarctica, mechanical properties of snow and avalanches, and distribution of seasonal snow cover in non-glaciated areas of the U.S.S.R. English summary, p. 219.]Google Scholar
Vinogradov, O. N., and Krenke, A. N. Glyatsiologicheskiye issledovaniya Instituta Geografii AN SSSR na Kavkaze po programme Mezhdunarodnogo Gidrologicheskogo Desyatiletiya v 1966–1968 gg. [Glaciological investigations of the Institute of Geography of the Academy of Sciences of the U.S.S.R. in the Caucasus within the International Hydrological Decade in 1966–68]. Materialy Glyatsiologicheskikh Issledovaniy. Khronika. Obsuzhdeniya, Vyp. 17, 1970, p. 24352. [Main aim is to investigate run-off from representative glaciers, and changes in this caused by climatic variations. English summary, p. 303–04.]Google Scholar

Glaciological Instruments and Methods

Mikheyev, S. V. O burenii l’da ognevym sposobom [On the drilling of ice by the thermic method]. Materialy Glyatsiologicheskikh Issledovaniy. Khronika. Obsuzhdeniya, Vyp. 18, 1971, p. 16063. [Describes method of thermal drilling. English summary, p. 163.]Google Scholar

Physics of Ice

Auek, A. H., jr. Inferences about ice nucleation from ice crystal observations. Journal of the Atmospheric Sciences, Vol. 29, No. 2, 1972, p. 31117. [Study of freezing nuclei and deposition nuclei as causes of ice crystals in natural cap clouds.]Google Scholar
Bruneaux-Poulle, J., and others. Contribution à l’étude des dépôts amorphes obtenus à basse température. I. Formation des dépôts amorphes, par. J. Bruneaux-Poulle, A. Defrain et N. T. Linh. Journal de Chimie Physique et Physico-chimie Biologique, Tom. 69, No. 1, 1972, p. 71-75. [Formation of amorphous ice at low temperature shown to be due to low mobility of molecules of vapour absorbed on the substrate. Effect of polymorphism on formation of amorphous ice. Preferred orientation of crystalline deposits of ice Ih and ice Ic.]CrossRefGoogle Scholar
Crowther, A. G. Preliminary investigation into the growth of ice crystals from the vapour in an electric field in the temperature range −11 to −15° C. Journal of Crystal Growth, Vols. 13–14, 1972, p. 24143. [Necdle-like crystals grow parallel to electric field. Explanation discussed.]Google Scholar
Davis, B. L. An examination of the theory of heterogeneous nucleation of ice. Journal of the Atmospheric Sciences, Vol. 29, No. 3, 1972, p. 55764. [Activity curves of AgI-bearing smoke used in theory of efficiency curve which are not in agreement with experiment.]2.0.CO;2>CrossRefGoogle Scholar
Devoto, R., and others. Adjustment of double-minimum potentials by means of a sum of Hulburt-Hirschfelder potentials, by Devoto, R., Sorarrain, O. M. and Boggia, L. M. Zeitschrift für physikalische Chemie (Leipzig), Bd. 247, Ht. 5–6, 1971, p. 28288. [New theoretical results obtained and compared with existing data on hydrogen bond in ice.]Google Scholar
Eldrup, M., and others. Position lifetimes in pure and doped ice and in water, [by] Eldrup, M. and Mogensen, O. and Trumpy, G. Journal of Chemical Physics, Vol. 57, No. 1, 1972, p. 495504. [Measurements in single crystal H2O, polycrystalline H2O, D2O and HF-doped ice. Three components found in all cases and attributed to ortho- and para-positronium and free positrons.]Google Scholar
Genadiev, N. P. Über die Verringerung der Aktivität von AgI-Teilchen in Wassertropfen bei deren mehrfachen Einfrierung. Doklady Bolgarskoy Akademii Nauk, Tom. 24, No. 12, 1971, p. 162932. [Study of nucleation activity of AgI particles in water droplets on repeated freezing and melting.]Google Scholar
Gerber, H. E. Size and nucleating ability of AgI particles. Journal of the Atmospheric Sciences, Vol. 29, No. 2, 1972, p. 39192. [Experimental determination of minimum size for particles to act as nuclei.]2.0.CO;2>CrossRefGoogle Scholar
Haas, J. and others. Diffusion de l’helium dans la glace monocristalline, [par] Haas, J., Bullemer et, B. Kahane, A. Solid State Communications, Vol. 9, No. 23, 1971, p. 203335. [Measurement of solubility and diffusion of He in ice −20 to −100° C.]CrossRefGoogle Scholar
Hasegawa, S., and others. Ice-crystal forming ability of the smoke emitted from the silver iodide-lead iodide system, by Hasegawa, S., Higashiyama, T., Fukuda, H. Reports, Research Laboratory Surface Science, Okayama University, Vol. 3, No. 5, 1971, p. 23136. [Conditions of mixture of PbI2 and AgI for most effective ice nucleus formation.]Google Scholar
Hasegawa, S., and others. Ice-crystal forming ability of the smoke emitted from the silver iodide-potassium iodide acetone system, by Hasegawa, S., Higashiyama, T., Shimada, M. Reports, Research Laboratory Surface Science, Okayama University, Vol. 3, No. 5, 1971, p. 23742. [Study of effectiveness of various proportions and of effect of ultra-violet irradiation.]Google Scholar
Hipolito, O., and Lobo, R. A study of Brout’s model for ferroelectrics. Investigations on hexagonal ice. Ferroelectrics, Vol. 1, No. 3, 1970, p. 16975. [Theoretical model developed and applied to ice where electrical susceptibility and transition temperature seem to agree well with experiments.]Google Scholar
Ho, K. K., and Kevan, L. Laser bleaching of trapped electron optical bands in γ-irradiated alkaline ice. International Journal for Radiation Physics and Chemistry, Vol. 3, No. 3, 1971, p. 19399. [Bleaching using narrow band laser light used to study nature of trapping sites.]Google Scholar
Huang, T., and others. Temperature dependence of the drift mobility of electrons in glassy 10 M sodium hydroxide ice, by Huang, T., Eisele, I., Kevan, L. Journal of Physical Chemistry, Vol. 76, No. 10, 1972, p. 150910. [Electrons generated by γ-irradiation and de-trappod by Xe light flash to give photoconductivity, and mobility determined 4–100 K.]CrossRefGoogle Scholar
Huber, H., and others. Surface structure of ice studied by proton channeling, [by] Huber, H., Jaccard, C. and Roulet, M. Radiation Effects, Vol. 12, Nos. 3–4, 1972, p. 24145. [Study of surface disorder shows evaporating ice has a clean surface above −75° C. Below −110° C without evaporation, radiation damage occurs in the bulk, and channelled irradiation produces disordered surface layer. Water vapour deposition at −157° C gives disordered structure.]Google Scholar
Huige, N. J. J., and Thijssen, H. A. C. Production of large crystals by continuous ripening in a stirrer tank. Journal of Crystal Growth, Vols. 13–14, 1972, p. 48387. [Ice crystals grown from sucrose solution by feeding with small, subcritical crystals.]Google Scholar
Ishmayev, S. N., and others. Termalizatsiya neytronov v H2O pri 318 i 77° K [Thermalization of neutrons in H2O at 318 and 77 K]. [By] Ishmayev, S. N., Sadikov, I. P. Chernyshov, A. A. Atomnaya Energiya, Tom 32, Vyp. 1, 1972, p. 3338. [Determination of thermalization time in ice at 77 K.]Google Scholar
Itagaki, K. HF diffusion in ice single crystals. Bulletin of the American Physical Society, Ser. 2, Vol. 17, No. 3, 1972, p. 264. [Abstract. HF diffusion through glacier ice single crystal has lower activation energy in strained than unstrained samples.]Google Scholar
Jaccard, C. Transport properties of ice. (In Horne, R. A., ed. Water and aqueous solutions: structure, thermodynamics, and transport processes. New York, etc.,Wiley-Interscience, [e1972], p. 2564.) [Review of physical properties of ice including electrical conductivity, diffusion, and mass transport by plastic deformation.]Google Scholar
Jellinek, H. H. G. The ice interface. (In Horne, R. A., ed. Water and aqueous solutions: structure, thermodynamics, and transport processes. New York, etc., Wiley-Interscience, [e 1972], p. 65107.) [Review of properties of ice surfaces.]Google Scholar
Jeneveau, A., and others. Étude du comportement électrique de la glace pure en basse temperature—ferroélectricité et charge d’espace, [par] Jeneveau, A., Sixou et, P. Dansas, P. Physik der kondensierten Materie, Vol. 14, No. 3, 1972, p. 25264. [Measurements of low-temperature depolarization currents in ice and their interpretation.]Google Scholar
Jones, D. R. H. Determination of the kinetics of ice–brine interfaces from data on temperature gradient zone migration. Philosophical Magazine, Eighth Ser., Vol. 25, No. 1, 1972, p. 97103. [Analysis of existing data for temperature-gradient migration of NaCl or KCl brine droplets through ice using properly calculated diffusivities.]Google Scholar
Jones, S. J., and Gilra, N. K. Increase of dislocation density in ice by dissolved hydrogen fluoride. Applied Physics Letters, Vol. 20, No. 8, 1972, p. 31920. [X-ray topography shows fivefold increase in dislocation density when HF is diffused into an ice crystal.]CrossRefGoogle Scholar
Jumawan, A. B., jr. An experimental study of self-diffusion in polycrystalline ice. Dissertation Abstracts International, B, Vol. 32, No. 9, 1972, p. 5163-B64-B. [Tritium diffusion in polycrystalline ice studied −6 to −37° C. Grain-boundary diffusion predominates.]Google Scholar
Kamb, W. B. Structure of the ices. (In Horne, R. A., ed. Water and aqueous solutions: structure, thermodynamics, and transport processes. New York, etc., Wiley-Interscience, [e 1972], p. 924.) [Review.]Google Scholar
Kawabata, K., and others. Optical absorption spectrum of trapped electron in crystalline ice at −150° C. Pulse radiolysis study, [by] Kawabata, K. Horii, H. and Okabe, S. Chemical Physics Letters, Vol. 14, No. 2, 1972, p. 22325. [Single crystals of D2O undergo pulse radiolysis at −150° C and visible and infra-red absorption studied with time.]Google Scholar
Kawada, S. Dielectric dispersion and phase transition of KOH doped ice. Journal of the Physical Society of Japan, Vol. 32, No. 5, 1972, p. 1442. [Observations of dielectric properties show a sudden drop of ϵ′ and ϵ″ at 70 K and also anomaly in thermal analysis attributed to a phase change.]Google Scholar
Lacmann, R., and Stranski, I. N. Growth of snow crystals. Journal of Crystal Growth, Vols. 13–14, 1972, p. 23640. [Explanation of the constant spacing of dendrite branches as due to quasi-liquid film on ice surface and unwettability of edges at about −15° C.]Google Scholar
Le Petit, J.-P. Mise en évidence, en hyperfréquences, de phénomènes liés à la préfusion de la glace formée par voie irréversible. Comptes Rendus Hebdomadaires des Séances de l’Académie des Sciences (Paris), Sér. B, Tom. 274, No. 24, 1972, p. 131315. [Dielectric anomalies on heating ice formed from supercooled water above −10° C.]Google Scholar
Le Petit, J.-P. Mise en évidence et comportement de ’‘molecules d’eau libres” et de “solution interstitielle” dans la glace formée par voie irréversible à partir de solutions salines aqueuses. Comptes Rendus Hebdomadaires des Séances de l’Académie des Sciences (Paris), Sér. B, Tom. 274, No. 23, 1972, p. 127073. [Discontinuities in permittivity observed when aqueous solutions of NH4Cl and KCl are cooled through the. freezing process and when they are reheated.]Google Scholar
Levkov, L. K. Étude de la température de congélation des gouttelettes surrefroidies contenant du CuS soumises à une congélation repetée. Doklady Bolgarskoy Akademii Nauk, Tom. 24, No. 12, 1971, p. 162527. [Formation properties of ice from droplets containing CuS are unaffected by repeated freezing and thawing.]Google Scholar
Lin, D. P., and others. Paramagnetic relaxation study of spatial distribution of trapped radicals in γ-irradiated alkaline ice and organic glasses at 4.2° K, by Lin, D. P., Hamlet, P. and Kevan, L. Journal of Physical Chemistry, Vol. 76, No. 8, 1972, p. 122627. [Spatial distribution of trapped radicals studied by measuring characteristic paramagnetic relaxation time versus radiation dose.]Google Scholar
Liou, K.-N. Light scattering by ice clouds in the visible and infrared: a theoretical study. Journal of the. Atmospheric Sciences, Vol. 29, No. 3, 1972, p. 52436. [Theory of intensity and linear polarization for single scattering by long cylinders of ice.]2.0.CO;2>CrossRefGoogle Scholar
Minton, A. P. Relations between crystal structure, molecular electronic polarizability, and refractive properties of ice I. Journal of Physical Chemistry, Vol. 76, No. 6, 1972, p. 88689. [Derivation of refractive index of ice from scalar molecular polarizability and a structure factor deduced for the ice Ih lattice.]Google Scholar
Moorthy, P. N., and Rao, K. N. Hydrogen peroxide yield in gamma-irradiated air-saturated ice at 77° K. Radiation Effects, Vol. 14, Nos. 1–2, 1972, p. 11317. [Determination of yield as function of dose]Google Scholar
Muguruma, J. Kōri no denshisen shōsha sonshō [Electron irradiation damage in ice]. Ōyō Butsuri, [Vol.] 40, [No.] 5, 1971, p. 56571.Google Scholar
Muguruma, J. Kōri no sosei [Plasticity of ice]. Nippon Kinzoku Gakkai Kaihō, [Vol.] 10, [No.] 10, 1971, p. 65366. [Review.]Google Scholar
Ramachandra, Murty, A. S., and Murty, V. Ramana. A new effect of evaporation accelerating the ice phase in supercooled water. Journal of the Atmospheric Sciences, Vol. 29, No. 4, 1972, p. 78184. [Experiments show rain-water drops freeze more readily if evaporating.]Google Scholar
Offenbacher, E. L., and Roselman, I. Hardness anisotropy of single crystals of ice Ih . Bulletin of the American Physical Society, Ser. 2, Vol. 16, No. 12, 1971, p. 1424. [Abstract. Orientational dependence of Knoop hardness on pyramidal and basal planes of ice.]Google Scholar
Plumb, R. C. Squeak, skid, and glide. Unusual properties of snow and ice. Journal of Chemical Education, Vol. 49, No. 3, 1972, p. 179. [Why snow squeaks only when it is very cold, and why sand and studded tyres lose their effectiveness at low temperatures, explained by pressure depression of melting point of ice.]Google Scholar
Popova, S. I., and others. Opticheskiye postoyannyye zhidkom vody i l’da v oblasti 2000 ÷ 100 Å [Optical constants of liquid water and ice in the 100–2000 Å region]. [By] Popova, S. I. Al’perovichi, L. I., Zolotarev, V. M. Optika i Spektroskopiya, Tom 32, Vyp. 3, 1972, p. 54750. [Calculation from Kramers-Krönig relations. English translation in Optics and Spectroscopy, Vol. 32, No. 3, 1972, p. 28889.]Google Scholar
Puntezhis, S. A., and others. Vliyaniye primesey na nakopleniye i gibel’ gidroksil’nykh radikalov v kristallicheskom l’du, obluchenom γ-luchami pri 77° K [Effect of impurities on the accumulation and loss of hydroxyl radicals in crystalline ice irradiated with y-rays at 77 K]. [By] Puntezhis, S. A. Yershov, B. G. Pikayev, A. K. Doklady Akademii Nauk SSSR, Tom 196, No. 3, 1971, p. 64144. [Concentration of OH radicals in ice according to speed of cooling to 77 K and concentration of various impurities. English translation in Doklady of the Academy of Sciences of the U.S.S.R. Physical Chemistry Section, Vol. 196, Nos. 1–3, 1971, p. 7477.]Google Scholar
Rozental’, O. M. Struktura i vmerzaniye v led gidratatsionnykh kompleksov ionov. [Structure and freezing in ice of ionic hydration complexes]. Zhurnal Strukturnoy Khimii, Tom 12, No. 5, 1971, p. 91719. [Theoretical calculation of concentration and charge effects on freezing a solution assuming ideal stirring.]Google Scholar
Rozental’, O. M. Voprosy obrazovaniya l’da v vode i rastvorakh. I. Perestroyka struktury vody i l’dozarozhdeniye pod deystviyem uneshnikh faktorov [Problem of the formation of ice in water and solutions. I. Rearrangement of the structure of water and ice formation under the action of external factors]. Zhurnal Fizicheskoy Khimii, Tom 46, Vyp. 1. 1972, p. 19192. [On basis of Samoylov’s model, nucleation of ice in supercooled water by shock waves or electrical or ultrasonic fields is explained as being due to an increase in the proportion of oriented molecules. English translation in Russian Journal of Physical Chemistry, Vol. 46, No. 1, 1972, p. 111.Google Scholar
Rozental’, O. M. Voprosy obrazovaniya l’da v vode i rastvorakh. II. Kinetika kristallizatsii vodnykh rastvorov elektrolitov [Problem of the formation of ice in water and solutions. II. Kinetics of crystallization in aqueous electrolyte solutions]. Zhurnal Fizicheskoy Khimii, Tom 46, Vyp. 3, 1972, p. 65759. [Nucleation ability is related to ion hydration. Thus a solution of negatively hydrated ions is less able to freeze than one of positively hydrated ions. English translation in Russian Journal of Physical Chemistry, Vol. 46, No. 3, 1972, p. 37677.]Google Scholar
Salaita, G. N. Existence of measured discontinuity in the thermal neutron diffusion coefficient across the ice–water phase transition. Reply to comments. Nuclear Science and Engineering, Vol. 48, No. 2, 1972, p. 232. [Reply to criticisms by Williams, P. M. ibid., Vol. 47, No. 3, 1972, p. 389.]Google Scholar
Savel’yev, I. B. Aktivnoye vozdeystviye merzlogo dispersnogo osnovaniya na strukturu prikontaktnogo sloya namorozhennogo l’da [Active action of a frozen dispersed base on the structure of a contact layer of frozen-on ice]. Doklady Akademii Nauk SSSR, Tom 201, No. 1, 1971, p. 8689. [Experimental study of ice frozen on to various substrates.]Google Scholar
Shawyer, R. E., and Dean, P. Atomic vibrations in orientationally disordered systems: II. Hexagonal ice. Journal of Physics, C, Vol. 5, No. 10, 1972, p. 102837. [Theoretical study of vibrations in H2O and D2O ice Ih. Broad agreement with experiment.]Google Scholar
Southern, E., and Walker, R. W. Friction of rubber on ice. Nature, Physical Science, Vol. 237, No. 78, 1972, p. 14244. [Measurements −1° C to −40° C show friction—velocity curves at all temperatures are similar in shape, with maximum occurring. Results similar to friction of rubber on other smooth surfaces.]Google Scholar
Whalley, E. The dipole moment derivative of the hydrogen bond in ice. Canadian Journal of Chemistry, Vol. 50, No. 3, 1972, p. 31014. [Calculation gives value which is less than that found from far infra-red spectrum, most of intensity therefore attributed to specific H-bond interactions.]Google Scholar

Land Ice. Glaciers. Ice Shelves

Ageta, Y., and Naruse, R. Measurements of ice flow around Skallen Rock, south of Syowa station, Antarctica. Nankyoku Shiryō; Antarctic Record, No. 42, 1971, p. 6164. [No significant differences in velocity were observed from stake measurements made in February–October–February.]Google Scholar
Barkov, N. I. Shel’fovyye ledniki Antarktidy [Ice shelves of Antarctica]. Leningrad, Gidrometeorologicheskoye Izdatel’stvo, 1971. 226 p. [Based on 1960–61 observations on the West, Shackleton, Lazarev and Novolazarevskiy ice shelves.]Google Scholar
Bazheva, V. Ya., and Krenke, A. N. Stroyeniye ledyanoy tolshchi Marukhskogo lednika (po rezul’tatam glubokogo bureniya letom 1967 g.) [The structure of Lednik Marukh ice body (according to the results of deep drilling in summer 1967)]. Materialy Glyatsiologicheskikh Issledovaniy. Khronika. Obsuzhdeniya, Vyp. 17, 1970, p. 28896. [Presents results from examination of core samples. Four zones of metamorphism found. English summary, p. 306.]Google Scholar
Bogacki, M. Eolian processes on the forefield of the Skeidarárjökull (Iceland). Bulletin de l’Académie Polonaise des Sciences. Série des Sciences Géologiques et Géographiques, Vol. 18, No. 4, 1970, p. 27987. [Study of activity of winds carrying volcanic dust.]Google Scholar
Bradley, R. S., and Miller, G. H. Recent climatic change and increased glacierization in the Canadian Arctic. Nature, Vol. 237, No. 5355, 1972, p. 38587. [During the past decade, mean annual temperatures on Baffin Island have been increasing, but so has glacierization.]Google Scholar
Brochu, M. Observations de névés sur les côtes du nord-ouest du Nouveau-Québec. Revue de Géographie de Montréal, Vol. 26, No. 2, 1972, p. 22023. [Describes types of firn patches observed from the sea on the coast between Ivujivik and Maricourt Fjord.]Google Scholar
Cherkasov, P. A., and Finansov, V. N. Metodika i programma rascheta insolyatsii fizicheskoy poverkhnosti lednikov na ETsVM tipa “M-20” [Methods and programme of calculating insolation of glacier surface by the computer “M-20”]. Materialy Glyatsiologicheskikh Issledovaniy. Khronika. Obsuzhdeniya, Vyp. 18, 1971, p. 14759. [Describes calculation of direct solar radiation on the horizontal or sloping surface of a glacier. English summary, p. 159.]Google Scholar
Churski, Ż. Genesis and evolution of the river system in the forefield of the Skeidarárjökull (Iceland). Bulletin de l’Académie Polonaise des Sciences. Série des Sciences Géologiques et Géographiques, Vol. 20, No. 1, 1972, p. 4753. [River evolution here may result from ablation processes, ground water, dead ice melt water, or spring melt water.]Google Scholar
Churski, Ż. Results of observations of water-level fluctuations in the Sandgigkvisl river (Iceland) in summer 1968. Bulletin de l’Académie Polonaise des Sciences. Série des Sciences Géologiques et Géographiques, Vol. 18, No. 4, 1970, p. 25968. [Investigations in the proglacial area of the receding Skeiðarárjökull.]Google Scholar
Dolgushin, L. D., and Osipova, G. B. Novyye dannyye o pul’satsiyakh sovremennykh lednikov [New data on the recent glacier surges]. Materialy Glyatsiologicheskikh Issledovaniy. Khronika. Obsuzhdeniya, Vyp. 18, 1971, p 191217. [Discusses occurrence and causes of surging glaciers with reference to those in the U.S.S.R. English summary, p. 21718.]Google Scholar
Dorofeyev, I. G. Chto proizoshlo s lednikom Fedchenko za tridtsatiletniy period (1928–1958 gg.) [What happened to Lednik Fedchenko during the thirty years 1928–58]. Izvestiya Vsesoyuznogo Geograficheskogo Obshchestva, Tom 104, Vyp. 1, 1972, p. 3639. [Recorded measurements of the shrinkage of this glacier in the Pamir.]Google Scholar
Dyurgerov, M. B. Metodika opredeleniya sredneyy sutochnoy poverkhnostnoy ablyatsii lednikov [Methods of determination of the mean surface ablation of glaciers]. Materialy Glyatsiologicheskikh Issledovaniy. Khronika. Obsuzhdeniya, Vyp. 18, 1971, p. 8692. [Accuracy of stake method is discussed with particular reference to results from Lednik Dzhankuat. English summary, p. 9192.]Google Scholar
Fleisher, P. J., and Sales, J. K. Laboratory models of glacier dynamics. Geological Society of America. Bulletin, Vol. 83, No. 3, 1972, p. 90510. [Models of glaciers were produced by pouring a mixture of moulding plaster and water down a prefashioned trough of non-absorbent material.]Google Scholar
Freydlin, V. S Primeneniye funktsii vliyaniya dlya rascheta gidrografa stoka i grafika vodopodachi lednika Dzhankuat [The application of the functions of influence for the computation of a discharge hydrograph and the inflow curve of Lednik Dzhankuat]. Materialy Glyatsiologicheskikh Issledovaniy. Khronika. Obsuzhdeniya, Vyp. 18, 1971, p. 9295. [English summary, p. 95.]Google Scholar
Galon, R. Mechanism and stages of retreating of the Skeidarárjökull (Vatnajökull, Iceland). Bulletin de l’Académie Polonaise des Sciences. Série des Sciences Géologiques et Géographiques, Vol. 18, No. 4, 1970, p. 24549. [Studies of marginal deposits and landforms showed that Skeiðarárjökull retreated in several phases since its advance 80 years ago.]Google Scholar
Golovkov, V. P. K voprosu ob absolyutnom izmerenii skorosti dvizheniya lednikovykh mass magnitnym metodom [On the problem of absolute measurement of speed of glacier mass movement by the magnetic method]. Informatsionnyy Byulleten’ Souetskoy Antarkticheskoy Ekspeditsii, No. 82, 1971, 54–56.Google Scholar
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Icebergs. Sea, River and Lake Ice

Allen, J. An analysii of the effect of bottom scouring icebergs. (In Proceedings of the Canadian seminar on icebergs … 1971 …, [1971], p. 11011.) [Detailed investigations of icebergs, including movement, shape and changes in surface topography, geological effects, marine life, and effects on adjacent water and bottom.]Google Scholar
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Banke, E., and Smith, S. D. Wind forces on icebergs. (In Proceedings of the Canadian seminar on icebergs … 1971 …, [1971], p. 15660.) [Mathematical treatment.]Google Scholar
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Grant, D. A. Iceberg tracking off the Labrador coast by aircraft of Maritime Command, 1970–1971. (In Proceedings of the Canadian seminar on icebergs … 1971 …, [1971], p. 6279.) [Approximate rate of movement 01–4 selected icebergs in 1970 was 1 knot, but there was no discernible movement in 1971. Details are given of the dyes used to mark the icebergs.]Google Scholar
Gudkovich, Z. M., and others. “Polyusnyy priliv” v atmosfere vysokikh shirot i kolebaniya ledovitosti arkticheskikh morey [The atmospheric “polar tide” at high latitudes and fluctuations in icing of the Arctic seas]. [By] Gudkovich, Z. M., Sarukhanyan, E. I., Smirnov, N. P. Doklady Akademii Nauk SSSR, Tom 190, No. 4, 1970, p. 95457. [Study of 14-month fluctuations in atmospheric pressure above the Arctic Ocean. English translation in Doklady of the Academy of Sciences of the U.S.S.R. Earth Science Sections, Vol. 190, Nos. 1–6, 1970, p. 23840.]Google Scholar
Hamelin, L.-E. Le glaciel de Iakoutie en Sibérie nordique. Biuletyn Peryglacjalny, No. 21, 1972, p. 7586 [Observations on the floating ice of the rivers Lena and Aldan, also on the structure of the non-tidal river-banks.]Google Scholar
Harwood, T. A. The iceberg problem. (In Proceedings of the Canadian seminar on icebergs …, 1971 …, [1971], p. 12.) [Outline of main problems.]Google Scholar
Harwood, T. A. All overview of methods of iceberg tracking. (In Proceedings of the Canadian seminar on icebergs …, 1971… [1971], p. 5051.) [Summary of off- and on-berg methods.]Google Scholar
Holdsworth, G., and McLaren, P. Proglacial lake studies, Barnes Ice Cap, Baffin Island—progress report. Arctic Circular, Vol. 21, No. 3, 1971, p. 16475. [Processes of calving and of formation of sublacustrine moraines were studied.]Google Scholar
Kaleri, Ye. Yu., and others. Ob anizotropii zapazdyvaniya radiovoln v morskom l’du [Anisotropy of radio-wave delay in sea ice]. [By] Kaleri, Ye. Yu. Kluga, A. M. Petrov, A. N. Finkel’shteyn, M. I. Izvestiya Akademii Nauk SSSR. Fizika Atmosfery i Okeana, Tom 7, No. 10, 1971, p. 11516. [Experiments confirm earlier theory. English translation in Izvestiya. Academy of Sciences, U.S.S.R. Atmospheric and Oceanic Physics, Vol. 7, No. 10, 1971, p. 738.]Google Scholar
Kornilov, N. A., and Komova, V. V. Ledovyye usloviya plavaniya d/e “Ob’ ” v antarkticheskikh vodakh letom 1968–69g. [Ice conditions during navigation of the Ob’ in Antarctic waters in the summer of 1968–69]. Trudy Sovetskoy Antarkticheskoy Ekspeditsii, Tom 57, 1971, p. 24675. [Includes appendix, p. 25775, of observations, mainly between “Molodezhnaya” and Mirny.]Google Scholar
Lazier, J. Circulation of water along the Labrador coast. (In Proceedings of the Canadian seminar on icebergs … 1971 …, [1971], p. 1618.) [Detailed knowledge of current velocities is the only way to predict the movement of ice accurately.]Google Scholar
Løken, O. H., and others. Iceberg studies in the Glaciology Subdivision, [by] Løken, O. H., Ommanney, C. S. L., Holdsworth, G. and U., and Arnold, U. [sic, i.e. K.] C. (In Proceedings of the Canadian seminar on icebergs … 1971 …, [1971], p. 12834.) [Current work is described on an inventory of all tidewater glaciers calving into the Canadian Arctic, the mechanism of calving, the rate of iceberg discharge from various glaciers, and the distribution of icebergs in selected areas.]Google Scholar
Losev, S. M. O ploshchadnykh kharakteristikakh ledyanogo pokrova [On areal characteristics of the ice cover]. Problemy Arktiki i Antarktiki, No. 39, 1972, p. 4754. [Measurement of sea ice by air photography.]Google Scholar
McClain, E. P. Quantitative use of satellite vidicon data for delimiting sea ice conditions. Proceedings of [the] 21st Alaska Science Conference, … College, Alaska, August 16–19, 1970, [1970], p. 21. [Abstract. Describes and discusses technique, some improvements, and results.]Google Scholar
Milne, A. R. Thermal tension cracking in sea ice: a source of underice noise. Journal of Geophysical Research, Vol. 77, No. 12, 1972, p. 217792. [Summarizes observations that relate the rheological properties of sea ice to the production of tension cracks, the crack noises to the underwater wave forms produced, and the statistics of cracking to the variations of the noise envelope with time.]Google Scholar
Nikolayev, S. Ye. Vliyaniye gidrometeorologicheskikh usloviy na prochnostnyye svovstva pripaynogo l’da zaliva Alasheyeva v 1969 g. [The influence of hydrometeorological conditions on the strength of the fast ice of Alasheyev Bight in 1969]. Informatsionnyy Byulleten’ Sovetskoy Antarkticheskoy Ekspeditsii, No. 81, 1971, p. 8083.Google Scholar
Nipcon, P., and others. Measurements of light transmission in shorefast ice, [by] Nipcon, P., Osterkamp, T. E. and Weller, G. Proceedings [of the] 22nd Alaska Science Conference, College, Alaska, August 17 to 19, 1971, 1971, p. 122. [Abstract. Measurements made with photo-cells in core holes.]Google Scholar
Pelletier, B. R. Side scan sonar surveys and ice scouring in the Beaufort Sea. (In Proceedings of the Canadian seminar on icebergs … 1971 …, [1971], p. 4849.) [Summary. Scouring may be caused by the keels of large pressure ridges in the ice and by icebergs.]Google Scholar
Peters, R. Underwater profiles of icebergs. (In Proceedings of the Canadian seminar on icebergs … 1971 …, [1971], p. 11314.) [Describes preliminary tests using an echo-sounder transducer lowered over the side of the ship.]Google Scholar
Reimnitz, E., and Bruder, K. F. River discharge into an ice-covered ocean and related sediment dispersal, Beaufort Sea, coast of Alaska. Geological Society of America. Bulletin, Vol. 83, No. 3, 1972, p. 86166. [Describes process of river ice break-up and subsequent discharge. Little sediment appears to be rafted away from deltas during final break-up of sea ice.]Google Scholar
Sanderson, R. M., and Davis, G. P. Ice conditions through the North-west Passage. Marine Observer, Vol. 42, No. 236, 1972, p. 6980. [Description of general ice conditions, particularly the pattern of break-up from mid-June to early September.]Google Scholar
Seifert, W. J., and Langleben, M. P. Air drag coefficient and roughness length of a cover of sea ice. Journal of Geophysical Research, Vol. 77, No. 15, 1972, p. 270813. [Roughness parameters of ice cover studied from observations of wind and temperature profiles obtained from an ice field drifting in the Gulf of St. Lawrence.]Google Scholar
Shamont’yev, V. A. Ledovyye uslovyye v rayone Mirnogo v 1968 g. [Ice conditions in the Mirny area in 1968]. Trudy Sovetskoy Antarkticheskoy Ekspeditsii, Tom 55, 1972, p. 17481. [Fast ice conditions in the Davis Sea.]Google Scholar
Solomon, H. Note on the no-stress boundary condition at the edge of the ice pack. Arctic, Vol. 25, No. 1, 1972, p. 5759. [Mathematical treatment of conditions governing ice drift.]Google Scholar
Strilaeff, P. W., and Wedel, J. H. Measurement of discharge under ice cover. Canada. Dept. of Energy, Mines and Resources. Inland Waters Branch. Technical Bulletin No. 29, 1970, vi, 14 p. [Problems encountered in northern areas of Canada, and procedures used to overcome them, are discussed.]Google Scholar
Sturm, M. Über die Auswirkungen des horizontalen Wärmetransportes durch den Fehmarnbelt auf die Eisverhältnisse in der südlichen Ostsee. Petermanns Geographische Mitteilungen, Jahrg. 115, Quartalsht. 4, 1971, p. 26267. [Influence of heat advection from Danish waters passing into the Baltic Sea on the melting of sea ice in the southern Baltic was studied, using 1949–61 estimates of the heat balance of the sea in the vicinity of the Fehmarnbelt lightship.]Google Scholar
Untersteiner, N. Arctic Ice Dynamics Joint Experiment. Proceedings of [the] 21st Alaska Science Conference, … College, Alaska, August 16–19, 1970, [1970], p. 22. [Abstract. Outlines AIDJEX project.]Google Scholar
Voyevodin, V. A. O razmerakh aysbergov v rayone Zemlya Frantsa-Iosifa i Shpitsbergena [On the measurements of icebergs in the region of Zemlya Frantsa-Iosifa and Spitsbergen]. Problemy Arktiki i Antarktiki, No. 39, 1972, p. 13840. [Measurement of depth of icebergs by air photography.]Google Scholar
Webb, M. S. Surface water temperature and ice regimes of Georgian Bay. Water Resources Research, Vol. 8, No. 3, 1972, p. 37289. [Data from airborne radiation thermometer surveys were used to determine areal patterns of surface water temperature and their seasonal variation. Ice coverage showed wide year to year variation, maximum area ranging from 40% to 90% of the whole.]Google Scholar
Wu, J. A note on surface roughness and resistance coefficient of sea ice. Journal of Geophysical Research, Vol. 77, No. 18, 1972, p. 327277. [Analyses further Untersteiner and Badgley’s data (ibid., Vol. 70, No. 18, 1965, p. 457377) and compares with results obtained by others.]Google Scholar
Yoshida, Y., and others. Nankyoku Victoria Land no dry valley chōsa hōkoku. IX. 1970–1971 nen no dry valley chōsa—chikyū-butsurigakuteki kenkyū o chūshin to shita—ni tsuite (yohō) [Report on investigation of a dry valley in Victoria Land in the Antarctic. IX. About the investigation of a dry valley, 1970–71—mainly a geophysical study—preliminary report]. [By] Yoshida, Y., Yoshisa, S., Moriwaki, K., Torii, Y. .Nankyoku Shiryō: Antarctic Record, No. 42, 1971, p. 6586. [Study of Lake Vanda included observations on the thickness and temperature of lake ice, and sublimation from, and intensity of solar radiation under, the ice surface. English summary, p. 65.]Google Scholar

Glacial Geology

Alexandrowicz, S. W. Formen der glazigenen Storungen miozäner Braunkohlenformation in Turoszów an der Nysa (Westpolen). Bulletin de l’Académie Polonaise des Sciences. Série des Sciences de la Terre, Vol. 19, No. 1, 1971, p. 4554. [Forms of disturbances caused by static non-uniform loading with ice masses or dead ice of the Miocene brown coal formation in this region of Poland were investigated.]Google Scholar
Andrews, J. T., and Barnett, D. M. Analysis of strandline tilt directions in relation to ice centers and postglacial crustal deformation, Laurentide ice sheet. Geografiska Annaler, Vol. 54A, No. 1, 1972, p. 111. [Considers results and implications of projecting the directions of strandline tilts from 36 sites within this area toward the supposed areas of maximum ice thickness. Data examined for evidence to support hypothesis that centres of crustal uplift migrated as the form of the ice sheet changed.]Google Scholar
Andrews, J. T., and Dugdale, R. E. Quaternary history of northern Cumberland Peninsula, Baffin Island, N. W. T. Part 5. Factors affecting corrie glacierization in Okoa Bay. Quaternary Research, Vol. 1, No. 4, 1971, p. 53251. [Each of 165 corries is described by 17 variables detailing shape, location and geometry, and having some relationship to the glaciological conditions in each corrie. Elevation and orientation were important factors.]Google Scholar
Bardin, V. I., and Konopleva, V. I. O protsessakh vyvetrivaniya i probleme geokhronologii lednikovogo perioda Antarktidy [Processes of weathering and the problem of geochronology of the ice age in Antarctica]. Antarktika. Doklady Komissii, 1969, [pub.] 1971, p. 10212.Google Scholar
Bernard, C. Les marques sous-glaciaires d’aspect plastique sur la roche en place (p-forms). Interpretation génétique (III). Revue de Géographie de Montréal, Vol. 26, No. 2, 1972, p. 17791. [Plastic scouring, causing sickle-troughs, may be due to cavitation by glacial melt water.]Google Scholar
Borisov, P. M., and Grosval’d, M. G. Nordkapskoye techeniye i oledeneniye Barentseva shel’fa [The North Cape current and glacial history of the Barents shelf]. Materialy Glyatsiologicheskikh Issledovaniy. Khronika. Obsuzhdeniya, Vyp. 18, 1971, p. 17983. [Effect of Pleistocene glaciation on continental shelf, and conditions in which it melted.]Google Scholar
Brook, D. Physiography and glacial geomorphology of the Theron Mountains. British Antarctic Survey Bulletin, No. 27, 1972, p. 2537. [Particular reference to weathering processes, glacial activity, melt phenomena and patterned ground.]Google Scholar
Carrara, P., and Andrews, J. T. The Quaternary history of northern Cumberland Peninsula, Baffin Island, N.W.T. Part 1. The late- and neoglacial deposits of the Akudlermuit and Boas glaciers. Canadian Journal of Earth Sciences, Vol. 9, No. 4, 1972, p. 40314. [Moraines described and chronology developed.]Google Scholar
Clapperton, C. M. Geomorphology of the Stromness Bay-Cumberland Bay area, South Georgia. British Antarctic Survey Scientific Reports, No. 70, 1971, 25 p., map [in end-pocket]. [Detailed study of glacial, periglacial and marine processes of landform development in this ice-free area. Glacial advances in the 1870’s and 1920’s are commented upon, as well as earlier glaciations.]Google Scholar
Dionne, J.-C. Caractéristiques des blocs erratiques des rives de l’estuaire du Saint-Laurent. Revue de Géographie de Montréal, Vol. 26, No. 2, 1972, p. 12552. [Six types of accumulation of erratic blocks are distinguished and described.]Google Scholar
Dugdale, R. E. The Quaternary history of the northern Cumberland Peninsula, Baffin Island, N.W.T. Part 3. The late glacial deposits of Sulung and Itidlirn valleys and adjacent parts of the Maktak-Narpaing Trough. Canadian Journal of Earth Sciences, Vol. 9, No. 4, 1972, p. 36674. [Four moraines described and dated.] Fillon, R. H. Possible causes of the variability of postglacial uplift in North America. Quaternary Research, Vol. 1, No. 4, 1971, p. 52231. [Discussion and conclusions drawn therefrom.]Google Scholar
Gaunt, G. A. A temporary section across the Escrick moraine at Wheldrake, east Yorkshire. Journal of Earth Sciences (Leeds), Vol. 8, No. 1, 1970, p. 16370. [Discusses composition and mode of formation of moraine.]Google Scholar
Grosval’d, M. G., and Serebryannyy, L. R. Geografiya materikogo oledeneniya severa Yevropy v verkhnem pleystotsene [The geography of the late Pleistocene glaciations of northern Europe]. Materialy Glyatsiologicheskikh Issledovaniy. Khronika. Obsuzhdeniya, Vyp. 17, 1970, p. 22331. [General survey of conditions giving rise to present geography. Suggests it is necessary to distinguish between ice sheets on land and those extending over the sea. English summary, p. 231.]Google Scholar
Guimont, P. Broutures glaciaires sur grès de Potsdam, Saint-Hermas, Québec. Revue de Géographie de Montréal Vol. 26, No. 2, 1972, p. 20206. [Describes various types of glacial chattermarks in sandstone.]Google Scholar
Hyne, N. J., and others. Quaternary history of Lake Tahoe, California–Nevada, [by] Hyne, N.J. Chelminski, P. Court, J. E. Gorsline, D. S. Goldman, C. R. Geological Society of America. Bulletin, Vol. 83, No. 5, 1972, p. 143548. [Sediments and structure of the lake reflect glacial activity during the Pleistocene.]Google Scholar
King, R. B. Lobes in the Cairngorm Mountains, Scotland. Biuletyn Peryglacjalny, No. 21, 1972, p. 15367 [Stone-banked and vegetation-covered lobes were recognized, the former dating from the Little Ice Age and the latter from Zone IV, and compared with lobes in the Kebnekaise region of northern Sweden]Google Scholar
Klassen, R. W. Wisconsin events and the Assiniboine and Qu‘Appelle valleys of Manitoba and Saskatchewan. Canadian Journal of Earth Sciences, Vol. 9, No. 5, 1972, p. 54460. [Describes likely course of events leading to formation of these valleys during the Early Wisconsin.]Google Scholar
Kornilov, G. A. Iz istorii pozdnego pleystotsena Chukotskogo poluostrova [On the late Pleistocene of Chukotskiy Poluostrov]. Izvestiya Akademii Nauk SSSR. Seriya Geograficheskaya, 1972, No. 1, p. 11823. [Based on field studies, 1955–65.]Google Scholar
Kortsenshteyn, V. N. O vliyanii periodicheskikh oledeneniy na formirovaniye unikal’nykh gazovykh mestorozhdeniy severa Tyumenskoy Oblasti [Effect of periodic glaciations on the formation of the unique gas fields in the northern part of Tyumenskaya Oblast’]. Doklady Akademii Nauk SSSR, Tom 191, No. 6, 1070, p. 136669. [English translation in Doklady of the Academy of Sciences of the U.S.S.R. Earth Science Sections, Vol. 191, Nos. 1–6, 1971, p. 22730.]Google Scholar
Lapparent, A. F. de, and others. Phénomènes glaciaires et périglaciaires dans la Montagne de Bamyan (Hindu Kuch occidental, Afghanistan), [par] de Lapparent, A. F. Bouyx, E., Pias, J. Comptes Rendus Hebdomadaires des Séances de l’Académie des Sciences (Paris), Sér. D, Tom. 274, No. 15, 1972, p. 214144. [Describes glacial deposits and periglacial features in this region of the Hindu Kush.]Google Scholar
Lohse, H.-H., and Vortisch, W. Mineralogische Untersuchungen an einigen Moränen SO-Schonens. Vorläufiger Bericht. Geologiska Föreningens i Stockholm Förhandlingar, Vol. 94, Pt. 1, No. 548, 1972, p. 2334. [Tills of different ages from south-east Skåne, Sweden, differed in clay mineral content; their history could be deduced from this.]Google Scholar
Lundqvist, J. Kvartärgeologisk forskning i Sverige 1946–70. Geologiska Foreningens i Stockholm Förhandlingar, Vol. 93, Pt. 2, No. 545, 1971, p. 30334. [Review of Quaternary research in Sweden during the period 1946–70.]Google Scholar
Madole, R. F. Neoglacial facies in the Colorado Front Range. Arctic and Alpine Research, Vol. 4, No. 2, 1972, p. 11930. [Describes the principal facies and estimates ages. Discusses distribution in relation to climatic changes.]Google Scholar
Mercer, J. H. Chilean glacial chronology 20,000 to 11,000 carbon-14 years ago: some global comparisons. Science, Vol. 176, No. 4039, 1972, p. 111820. [Fluctuations match those of the Laurentide ice sheet east of the Mississippi River, but differ from accepted sequence in New Zealand. Corresponding pattern is not apparent in the Antarctic palaeotemperature curve deduced from changes in oxygen isotope ratios.]Google Scholar
Mickelson, D. M., and Borns, H. W., jr. Chronology of a kettle-hole peat bog, Cherryfield, Maine. Geological Society of America. Bulletin, Vol. 83, No. 4, 1972, p. 82731. [Results of observations include speculation about the Quaternary glaciation of this area.]Google Scholar
Monaco, A., and others. L’âge des dépôts quaternaires sur le plateau continental du Roussillon (Golfe du Lion), [par] Monaco, A., Thommeret, J., Thommeret, Y. Comptes Rendus Hebdomadaires des Séances de l’Académie des Sciences (Paris), Sér. D. Tom. 274, No. 16, 1972, p. 228083. [Dating of deposits in this area enable them to be attributed to the various stages of Quaternary glaciation.]Google Scholar
Naylor, D., and others. Pleistocene deposits exposed along the Yukon coast, [by] Naylor, D., McIntyre, D. J. and McMillan, N. F. Arctic, Vol. 25, No. 1, 1972, p. 4955. [Sediments are described and dates of deposition in relation to movements of the Pleistocene ice sheet discussed.]Google Scholar
Page, N. R. On the age of the Hoxnian interglacial. Geological Journal (Liverpool), Vol. 8, Pt. 1, 1972, p. 12942. [On the basis of new radiocarbon datings, the chronology for East Anglia is reappraised. Suggests the Hoxnian interglacial is dated between 25000 and 21000 B.P.]CrossRefGoogle Scholar
Piper, D. J. W. Pleistocene superficial deposits, Balcombe area, central Weald. Geological Magazine, Vol. 108, No. 6, 1971, p. 51723. [Distribution of these deposits, which formed in periglacial conditions, indicates most of the landforms are relict Pleistocene features.]Google Scholar
Price, R. J. The unquiet landscape. Legacy of the Pleistocene ice sheets. Geographical Magazine, Vol. 44, No. 10, 1972, p. 68771. [General description of glacial deposits and landforms, illustrated by photographs of Iceland.]Google Scholar
Saint-Onge, D.-A. La stratigraphie du Quaternaire des environs de Fort-Assiniboine, Alberta, Canada. Revue de Géographie de Montréal, Vol. 26, No. 2, 1972, p. 15363. [Study of sequence of deposits filling ancestral valley system. Effect of Wisconsin glaciation was followed and dated.]Google Scholar
Sissons, J. B. Dislocation and non-uniform uplift of raised shorelines in the western part of the Forth valley. Institute of British Geographers. Transactions, No. 55, 1972, p. 14559. [Results suggest that the hypothesis that raised shorelines in areas of glacial rebound have uniform or gradually changing gradients does not apply to this area.]Google Scholar
Troitskiy, L. S. O golotsenovykh stadiyakh oledeneniya na Shpitsbergene [On the Holocene glaciation stages in Svalbard]. Materialy Glyatsiologicheskikh Issledovaniy. Khronika. Obsuzhdeniya, Vyp. 18, 1971, p. 6368. [Study of moraines, and conclusions drawn from this. English summary, p. 6768.]Google Scholar
Vortisch, W. Untersuchungen im Pleistozän SO-Schonens. Geologiska Föreningens i Stockholm Förhandlingar, Vol. 94, Pt. 1, No. 548, 1972, p. 3568. [A study of the geology of south-east Skåne, Sweden, enables Quaternary ice movements in this region to be followed.]Google Scholar
Weidick, A. Holocene shore-lines and glacial stages in Greenland—an attempt at correlation. Grønlands Geologiske Undersøgelse. Rapport No. 41, 1972, 39 p. [Dates of former sea-levels were determined by dating shells collected in west Greenland, the results being compared to published information from other parts of Greenland in order to check the deduced uplift. The result was then used to determine the extent of the inland ice.]Google Scholar
White, W. A. Deep erosion by continental ice sheets. Geological Society of America. Bulletin, Vol. 83, No. 4, 1972, p. 103756. [Suggests that ice sheets effected great erosion and shaped the major topographic features of the areas they covered.]Google Scholar
Wright, F. F. Yakutat Bay, Alaska—a product of coastal plain deglaciation. Proceedings of [the] 21st Alaska Science Conference, … College, Alaska, August 16–19, 1970, [1970], p. 107. [Abstract. Describes formation and glacial geology of bay.]Google Scholar

Frost Action on Rocks and Soil. Frozen Ground. Permafrost

Afanasenko, V. Ye. Dinamichnost’ dolinnykh talikov v predelakh Polousnogo Kryazha [Valley taliks within the Polousnyy Kryazh]. Merzlotnyye Issledovaniya, Vyp. 11, 1971, p. 12429. [Study of tabetisols (unfrozen layers within permafrost) in Yakutskaya A.S.S.R.]Google Scholar
Akili, W. Stress-strain behavior of frozen fine-grained soils. Highway Research Record, No. 360, 1971, p. 18. [Investigation of effect of below-freezing temperature, constant axial deformation rates and soil type.]Google Scholar
Alekseyev, V. R. Naledi kak forma oledeneniya i ikh geneticheskaya klassifikatsiya [Icings as a glaciation form and their genetic classification]. Muterialy Glyatsiologicheskikh Issledovaniy. Khronika. Obsuzhdeniya, Vyp. 17, 1970, p. 14554. [Characterisitcs of icings described with reference to those of Siberia and the Far East. English summary, p. 172.]Google Scholar
Aleshinskaya, Z. V., and others. Periglacial phenomena and some paleogeographical problems of central Tian-Shan, [by] Aleshinskaya, Z.V. Bondarev, L. G. Gorbunov, A. P. Biuletyn Peryglacjalny, No. 21, 1972, p. 513. [Detailed study of the Taragay basin.]Google Scholar
Ananyan, A. A., and Poltev, N. F. Rezul’taty laboratornykh issledovaniy nekotorykh teplofizicheskikh svoystv rykhlykh gornykh porod po rayonam Bodaybo i Aldana [Results of laboratory research on heat properties of friable soils in the Bodaybo and Aldan regions]. Merzlotnyye Issledovaniya, Vyp. 11, 1971, p. 19298. [Freezing and thawing experiments.]Google Scholar
Bashlakov, Ya. K. Formirovaniye i ablyatsiya naledey v usloviyakh Zabaykal’ya [Formation and ablation of icings in the conditions of Zabaykal’ye]. Materialy Glyatsiologicheskikh Issledovaniy. Khronika. Obsuzhdeniya, Vyp. 17, 1970, p. 15458. [Distinguishes between icings of mountains and those of intermountain basins. Presents observations on formation and melting of a large icing in the Ingamakit river basin, Buryat-Mongol’skaya A.S.S.R. English summary, p. 172.]Google Scholar
Baulin, V. V., and others. Rasprostraneniye vechnomerzlykh porod v rayone shirotnogo techeniya r. Obi [Distribution of permanently frozen soils near the middle course of the river Ob’]. [By] Baulin, V. V., Yefimov, I. V., Timofeyev, V. G. Merzlotnyye Issledovaniya, Vyp. 11, 1971, p. 14251. [West Siberian lowland.]Google Scholar
Belopukhova, Ye. B. Otrazheniye klimaticheskikh izmeneniy v morfologii povtorno-zhil’nykh l’dov [The reflection of climatic variations in the morphology of veined ice]. Merzlotnyye Issledovaniya, Vyp. 11, 1971, p. 17378. [Studies in the northern part of the West Siberian lowland.]Google Scholar
Bogorodskiy, V. V., and others. Elektricheskiye kharakteristiki sistem gornaya poroda-led [Electrical properties of rock-ice systems]. [By] Bogorodskiy, V. V. Khokhlov, G. P. Fedorov, B. A. Trepov, G. V. Doklady Akademii Nauk SSSR, Tom 190, No. 1, 1970, p. 8890. [Laboratory study. Also assesses feasibility of using radio methods for permafrost introscopy. English translation in Doklady of the Academy of Sciences of the U.S.S.R. Earth Science Sections, Vol. 190, Nos. 1–6, 1970, p. 13.]Google Scholar
Bournérias, M. Pyramides rocheuses d’éjection en milieu périglaciaire, Puvirnituq, Nouveau-Québec. Revue de Géographie de Montréal, Vol. 26, No. 2, 1972, p. 21419. [Describes process of frost heaving of large angular stones around this region of the eastern coast of Hudson Bay.]Google Scholar
Brochu, M. Premières observations de dépôts de solifluxion fossiles en Gaspésie. Biuletyn Peryglacjalny, No. 21, 1972, p. 1520. [Examination and subsequent dating of slope deposits, caused by solifluction, observed in the Gaspé Peninsula, Quebec.]Google Scholar
Brochu, M. Réflexions sur la notion de pergélisol stricto sensu et lato sensu . Compte Rendu Sommaire des Séances de la Société Géologique de France, 1971, Fasc. 10, p. 272. [Discusses the definition of permafrost.]Google Scholar
Clark, R. Periglacial landforms and landscapes in the Falkland Islands. Biuletyn Peryglacjalny, No. 21, 1972, p. 3350. [General description, referring to past and present climatic conditions.]Google Scholar
French, H. M. Asymmetrical slope development in the Chiltern Hills. Biuletyn Peryglacjalny, No. 21, 1972, p. 5173. [Model of asymmetrical slope and valley development is proposed which stresses the importance of fluvial processes in periglacial environments, referring to Pleistocene conditions in this region of southern England.]Google Scholar
Gavrilova, M. K. Teplovoy balans poverkhnosti nalednoy doliny v tsentral’noy Yakutii [Heat balance regime of the surface of a valley containing icings in central Yakutiya]. Materialy Glyatsiologicheskikh Issledovaniy. Khronika. Obsuzhdeniya, Vyp. 17, 1970, p. 15966. [English summary, p. 172.]Google Scholar
Guiter, V. Une forme montagnarde: le rock-glacier. Revue de Géographie Alpine, Tom. 60, Fasc. 3, 1972, p. 46787. [Describes in some detail the characteristics of rock glaciers in various parts of the world and discusses their formation.]Google Scholar
Hedges, J. Expanded joints and other periglacial phenomena along the Niagara escarpment. Biuletyn Peryglacjalny, No. 21, 1972, p. 87126. [Describes occurrence and suggests mode of formation of fissures (expanded joints); also discusses block streams, solifluction aprons, slope colluvium, the West Union talus, and two associated erosional forms.]Google Scholar
Higashi, A., and Corte, A. E. Growth and development of perturbations on the soil surface due to the repetition of freezing and thawing. Memoirs of the Faculty of Engineering, Hokkaido University, Vol. 13, Suppl., 1972, p. 4963. [Describes laboratory experiments on the formation of frost mounds.]Google Scholar
Hyvönen, O. Palsojen morfologiasta ja esiintymisestä Fennoskandiassa. Terra, Vol. 84, No. 2, 1972, p. 7277. [Reviews morphology and distribution of palsas in north Sweden and Finland. English summary, p. 72.]Google Scholar
James, P. A. The periglacial geomorphology of the Rankin Inlet area, Keewatin, N.W. T., Canada. Biuletyn Peryglacjalny, No. 21, 1972, p. 12751. [Detailed description of features.]Google Scholar
Journaux, A., and Dresch, J. Phénomènes périglaciaires en Sibérie Orientale. Définition d’une nouvelle province périglaciaire actuelle. Bulletin de l’Association de Géographes Français, Nos. 395–96, 1972, p. 5773. [Describes periglacial phenomena such as frost cracks, ice wedges and soil veins in central Yakutskaya A.S.S.R.]Google Scholar
Jumikis, A. R. Three-dimensional influence values of disturbance distribution of temperature from heated structures on permafrost. Highway Research Record, No. 360, 1971, p. 3744. [Presents temperature influence values and graphs for evaluating and plotting quickly temperature fields in permafrost beneath heated rectangular structures.]Google Scholar
Kalyuzhnyy, I. L., and others. Teplofizicheskiy metod rascheta poter’ talykh vod na infil’tratsiyu v merzlyyu pochvu [A thermophysical method of calculating loss of thaw water due to infiltration into frozen soil]. [By] Kalyuzhnyy, I. L., Morosova, N. S., Pavlova, K. K., Romanov, V. V. Meteorologiya i Gidrologiya, 1972, No. 1, p. 7682. [Method described for calculating loss during first phase of infiltration. Conditions studied under which ice, formed from infiltrated water, can stop up the pores completely. English summary, p. 82.]Google Scholar
Kaplinat, T. N. Formy nachal’noy stadii obrazovaniya ledyanykh zhil [Forms of the first stage of the formation of glacial veins]. Merzlotnyye Issledovaniya, Vyp. 11, 1971, p. 16872. [Study made in flood-plain deposits along left bank tributary (Uyandina) of Indigirka river.]Google Scholar
Kerfoot, D. E. Thermal contraction cracks in an Arctic tundra environment. Arctic, Vol. 25, No. 2, 1972, p. 14250. [Field observations on bare and vegetated surfaces of low alluvial flats and sand-spits in the Mackenzie Delta area substantiate Lachenbruch’s theory of the development of frost crack patterns.]Google Scholar
Kononova, R. S., and others. Kriopegi—otritsatel’no temperaturnyye vody zemli [Cryopegs—waters of the earth below freezing point]. [By] Kononova, R. S., Neizvestnov, Ya. V., Tolstikhin, N. I., Tolstikhin, O. N. Merzlotnyye Issledovaniya, Vyp. 11, 1971, p. 7588. [Arctic, Antarctic and underground waters.]Google Scholar
Kudryavtsev, V. A., and Garagulya, L. S. Ob uteplyayushchem vliyanii pustot pod snegom na temperaturnyy rezhim pochvy [On the warming influence of air space under the snow on the temperature regime of the soil]. Merzlotnyye Issledovaniya, Vyp. 11, 1971, p. 3134. [Refers briefly to conditions in central Yakutiya and Eastern Siberia.]Google Scholar
Kudryavtsev, V. A., and Garagulya, L. S. O vliyanii zaholochennosti na formirovaniye temperaturnogo rezhima porod [The influence of marsh on the formation of the temperature regime of soils]. Merzlotnyye Issledovaniya, Vyp. 11, 1971, p. 3537.Google Scholar
Kulik, V. Ya. Priblizhennyy teoreticheskiy analiz nekotorykh sluchayev vpityvaniya vody v merzlyy grunt [An approximate theoretical analysis of some cases of water absorption in frozen soil]. Meteorologiya i Gidrologiya, 1972, No. 3, p. 8895. [Formulae derived and compared to field experiments. English summary, p. 95.]Google Scholar
Laba, J. T. Viscoelastic properties of a laterally confined sand-ice system subjected to temperature increase. Highway Research Record, No. 360, 1971, p. 2636. [Equations derived for initial modulus of elasticity of a frozen sand layer, effect of temperature increase on the modulus of electricity, time-dependent coefficient of viscosity of a frozen sand-ice layer, and time-dependent functions of elastic strain and plastic strain.]Google Scholar
McCann, S. B., and others. Fluvial processes in a periglacial environment, Queen Elizabeth Islands, N.W.T., Canada, [by] McCann, S. B., Howarth, P. J. and Cogley, J. G. Institute of British Geographers. Transactions, No. 55, 1972, p. 6982. [Study of hydrological regime of two streams illustrates their geomorphological importance: 90% of annual run-off occurs in the spring snow melt flood and storm run-off is rapid in the presence of permafrost and the absence of vegetation.]Google Scholar
Maksimova, L. N., and Kondrat’yeva, K. A. O povtorno-zhilnykh l’dakh na vodorazdel’nykh sedlovinakh khr. Polousnogo [On reopened veined ice in the watershed saddles of Polousnyy Khrebet]. Merzlotnyye Issledovaniya, Vyp. 11, 1971, p. 16167.Google Scholar
Mangerud, J., and Skreden, S. A. Fossil ice wedges and ground wedges in sediments below till at Voss, western Norway. Norsk Geologisk Tidsskrift, Bd. 52, Ht. 1, 1972, p. 7396. [Description.]Google Scholar
Morgan, A. V. Late Wisconsinan ice-wedge polygons near Kitchener, Ontario, Canada. Canadian Journal of Earth Sciences, Vol. 9, No. 6, 1972, p. 60717. [Polygonal ground shown in air photographs. Trenching of a polygon exposed wedge-shaped sand and gravel infilled structures, interpreted as ice wedge casts.]Google Scholar
Pulinowa, M., and Pulina, M. Phénomènes cryogènes dans les grottes et gouffres des Tatras. Biuletyn Peryglacjalny, No. 21, 1972, p. 20135. [Describes cryogenic phenomena, including ice, now being formed in the periglacial climate of the caves and pits of the Polish part of the Tatry mountains.]Google Scholar
Seppälä, M. Pingo-like remnants in the Peltojärvi area of Finnish Lapland. Geografiska Annaler, Vol. 54A, No. 1, 1972, p. 3845. [Describes circular till ridges and suggests they are collapsed pingos.]Google Scholar
Sugden, D. Deglaciation and isostasy in the Sukkertoppen ice cap area, west Greenland. Arctic and Alpine Research, Vol. 4, No. 2, 1972, p. 97117. [Explains landforms associated with the disappearance of the inland ice, with the withdrawal of the local Sukkertoppen ice, and with the changing relative sea-level, and discusses the interrelationships between them.]Google Scholar
Szupryczyński, J., and Kozakski, S. Relief of the marginal zone of Sidujökull (Iceland). Bulletin de l’Académie Polonaise des Sciences. Série des Sciences Géologiques et Géographiques, Vol. 18, No. 4, 1970, p. 26978. [Four zones of end moraines and four outwash plain levels distinguished, and two types of proglacial valleys among the many examples found among the end moraines.]Google Scholar
Tufnell, L. Ploughing blocks with special reference to north-west England. Biuletyn Peryglacjalny, No. 21, 1972, p. 23770. [Describes varieties and movement of these blocks (angular rocks) which develop in areas experiencing a mildly periglacial climate. Currently developing blocks in the northern Pennines were observed.]Google Scholar
Wang, M.-C., and Roderick, G. L. Frost behavior of compacted soils. Highway Research Record, No. 360, 1971. p. 925. [Effect of a unidirectional penetration of freezing temperature from the top under a temperature gradient of 0.7 deg/cm on depth and rate of frost penetration, moisture migration due to freezing, frost heaving, and development of ice segregation.]Google Scholar
Yershov, E. D. Ob upravlenii glubinoy sezonnogo ottaivaniya (promerzaniya) porod v prakticheskikh tselyakh [On the control of the depth of thawing (freezing) of soils in practical terms]. Merzlotnyye Issledovaniya, Vyp. 11, 1971, p. 10815. [Experiments in Anadyrskaya Nizmennost’.]Google Scholar

Meteorological and Climatological Glaciology

Auer, A. H., jr. Distribution of graupel and hail with size. Monthly Weather Review, Vol. 100, No. 5, 1972’ p. 32528. [Observations on size and concentration of graupel and hail in untreated convective clouds over Wyoming, U.S.A.]Google Scholar
Isaac, G. A., and Douglas, R. H. Another “time lag” in the activation of atmospheric ice nuclei. Journal of Applied Meteorology, Vol. 11, No. 3, 1972, p. 49093. [Examines parameters affecting nucleation and how well laboratory cloud simulates natural one.]Google Scholar
Jayaweera, K. O. L. F. An equivalent disc for calculating the terminal velocity of plate-like ice crystals. Journal of the Atmospheric Sciences, Vol. 29, No. 3, 1972, p. 59698. [Model experiments with metal plates in glycerol-water mixture.]Google Scholar
Jayaweera, K. O. L. F., and Ryan, B. F. Terminal velocities of ice crystals. Quarterly Journal of the Royal Meteorological Society, Vol. 98, No. 415, 1972, p. 19397. [Measurements for plate-like and columnar crystals agree well with theory.]Google Scholar
List, R., and others. Air bubbles in hailstones, [by] List, R., Murray, W. A. and Dyck, C. Journal of the Atmospheric Sciences, Vol. 29, No. 5, 1972, p. 91620. [Bubble size distributions and bubble concentration measured and used to correlate with icing conditions during growth.]Google Scholar
Mathews, L. A., and others. Rate of solution of ice nuclei in water drops and its effect on nucleation, [by] Mathews, L. A., Reed, D. W., St.-Amand, P. and Stirlon, R. J. Journal of Applied Meteorology, Vol. 11, No. 5, 1972, p. 81317. [Calculation of lifetime of nuclei in water droplets due to dissolution.]Google Scholar
Mossop, S. C., and others. Ice crystal concentrations in cumulus and stratocumulus clouds, by Mossop, S. C., Cottis, R. E. and Bartlett, B. M. Quarterly Journal of the Royal Meteorological Society, Vol. 98, No. 415, 1972, p. 10523. [Measurements show concentrations much higher than those of ice nuclei. Discussion of enhancement mechanisms.]Google Scholar
Rosinski, J., and others. On the ejection of microdroplets from the surface of a freezing water drop, by Rosinski, J., Langer, G. and Nagamoto, C. T. Journal of Applied Meteorology, Vol. 11, No. 2, 1972, p. 40506. [Presents evidence to show that this does not occur, contrary to R. J. Cheng’s results (Science, Vol. 170, No. 3965, 1970, p. 139596).]Google Scholar
Tricker, R. A. R. Observations on certain features to be seen in a photograph of haloes taken by Dr. Emil Schulthess in Antarctica. Quarterly Journal of the Royal Meteorological Society, Vol. 98, No. 417, 1972, p. 54262. [Theory of formation of ares by refraction in rotating ice crystals.]Google Scholar

Snow

Anderson, H. W. Storage and delivery of rainfall and snowmelt water as related to forest environments. (In Powell, J. M., and Nolasco, C. F., ed. Proceedings of the third Forest Microclimate Symposium, Kananaskis Forest Experiment Station, Seebe, Alberta, September 23–26, 1969. Calgary, Alberta, Dept. of Fisheries and Forestry, Canadian Forestry Service, Alberta/Territories Region, 1970, p. 5167.) [Review, summarizing what can be done to modify snow storage and control snow melt in forest management.]Google Scholar
Belov, V. F. Opticheskiy metod opredeleniya perenosa snega [Optic method of determining snow movement]. Antarktika. Doklady Komissii, 1969, [pub.] 1971, p. 15770.Google Scholar
Belov, V. F., and others. Balans snezhnoy poverkhnosti i raspredeleniye snezhuogo i ledovogo pokrovov v zalive Alasheyeva [The balance of snow surface and the distribution of snow and ice cover in Alasheyev Bight]. [By] Belov, V. F., Kornilov, N. A., Chikovskiy, S. S., Baranov, Ya. P. Antarktika. Doklady Komissii, 1969, [pub.] 1071, p. 14456. [Study made in 1968 near “Molodezhnaya” station.]Google Scholar
Bergström, S. Snösmaltningen i Lappträskets representativa område som funktion av lufttemperaturen. Sveriges Meteorologiska och Hydrologiska Institut. Hydrologiska Byrån. Notiser och Preliminära Rapporter. Serie Hydrologi, No. 18, 1972, 27 p. [Snow melt as a function of air temperature. Measurements in Lappträsket region, north Sweden, as part of IHD programme.]Google Scholar
Bordovskaya, L. I. K voprosu o sinopticheskikh usloviyakh letnikh snegopadov nad Altayem [On the problem of synoptic conditions of summer snowfalls over Altay]. Materialy Glyatsiologicheskikh Issledovaniy. Khronika. Obsuzhdeniya, Vyp. 18, 1971, p. 18990.Google Scholar
Bories, S., and Thirriot, C. Phénomènes de convection naturelle dans la neige et les aquifères. (In Quator zième Congrès de l’Association Internationale de Recherches Hydrauliques 29 août-3 septembre 1971. La recherche hydraulique et son impact sur l’environnement. Comptes-rendus. Vol. 1. [Paris], Société Hydrotechnique de France, [1971], p. 28390. (Rapport A-34.)) [Includes a study of the movement of air in a snow layer when low ambient nocturnal temperatures impose a downward thermal gradient.]Google Scholar
Bortenschlager, S., and others. Vergleich von Pollenspektren im Akkumulationsgebiet des Kesselwandferners (Otztaler Alpen), [von] Bortenschlager, S. Ambach, W. Eisner, H. Bericht des Naturwissenschaftlich-medizinischen Vereins in Innsbruck, Bd. 58, 1970, p. 12530. [Old and new snow show significant differences in pollen content and the horizon formed by summer melting may be seen clearly in the vertical pollen profile.]Google Scholar
Carlson, P. E., and Marshall, J. S. Measurement of snowfall by radar. Journal of Applied Meteorology, Vol. 11, No. 3, 1972, p. 494500. [Radar returns from a layer at 1 500 m were converted to snowfall rates and summed over 36 h to obtain a map of snowfall amount.]Google Scholar
Cubley, S., and others. The tundra microclimates during snow-melt at Barrow, Alaska, [by] Cubley, S., Parker, S., Trabant, D., Benson, C. S. and Weller, G. Proceedings [of the] 22nd Alaska Science Conference, College, Alaska, August 17 to 19, 1971, 1971, p. 29. [Abstract. Observation of changes during period from end of May, snow cover 38 cm deep, to end of June, after complete disappearance of snow.]Google Scholar
Dijk, T. van, and Weg, W. F. van der. Het conserveren van sneeuwkristallen. Hemel en Dampkring, Jaarg. 70, Afl. 4, 1972, p. 11117.Google Scholar
Dolov, M. A. Nekotoryye voprosy teplofiziki snega [Some thermal properties of snow]. Materialy Glyatsiologicheskikh Issledovaniy. Khronika. Obsuzhdeniya, Vyp. 17, 1970, p. 10614. [Laboratory investigations described. English summary, p. 170.]Google Scholar
Getker, M. I., and others. Izmenchivost’ vysoty snezhnogo pokrova v gorakh zapadnogo Tyan’-Shan’ [Snow cover depth variation in the western Tyan’-Shan’ mountains]. [By] Getker, M. I., Kanayev, L. A., Chirkova, A. A. Materialy Glyatsiologicheskikh Issledovaniy. Khronika. Obsuzhdeniya, Vyp. 17, 1970, p. 12430. [Analysis of observations from remote sites in different climatic areas; effect of exposure, height and relief of area considered. English summary, p. 171.]Google Scholar
Golding, D. L. Computer mapping of the Marmot Creek snowpack and the influence of topographic and forest stand variables on the pack. (In Powell, J. M., and Nolasco, C. F., ed. Proceedings of the third Forest Microclimate Symposium, Kananaskis Forest Experiment Station, Seebe, Alberta, September 23–26, 1969. Calgary, Alberta, Dept. of Fisheries and Forestry, Canadian Forestry Service, Alberta/Territories Region, 1970, p. 7683.) [Studies on snow accumulation and melt from this experimental watershed.]Google Scholar
Jail, M., and Vivian, R. Les glissements de terrain et les éboulements dans les Alpes françaises du Nord en 1970. Étude physique et problèmes posés par ces phénomènes. Revue de Géographie Alpine, Tom. 59, Fasc. 4, 1971, p. 473502. [Following many avalanches in the northern French Alps during the winter of 1969–70, numerous landslides occurred in spring 1970. These are described and discussed with particular reference to the one at Assy.]Google Scholar
Jiusto, J. E., and Kaplan, M. L. Snowfall from lake-effect storms. Monthly Weather Review, Vol. 100, No. 1, 1972, p. 6266. [Attempt to define snowfall patterns associated with these storms and to correlate snowfall depth and density with relevant variables.]Google Scholar
Khmelevskoy, I. F. Raspredeleniye snegozapasov v lesnoy zone mezhdurech’ya Obi i Irtysha i ikh izmenchivost’ vo vremeni [Distribution of snow pack in the forest zone between the Ob’ and the Irtysh rivers and its variability with time]. Materialy Glyatsiologicheskikh Issledovaniy. Khronika. Obsuzhdeniya, Vyp. 17, 1970, p. 23140. [English summary, p. 240.]Google Scholar
Khodakov, V. G., and Tsvetkov, D. G. Opyt izmereniya tolshchiny snezhnogo pokrova v gorakh stereofoto-grammetricheskim metodom [Experience in measuring snow depth in mountains by the stereophotogrammetric method]. Materialy Glyatsiologicheskikh Issledovaniy. Khronika. Obsuzhdeniya, Vyp. 17, 1970, p. 32836. [Preliminary results show considerable promise. English summary, p. 336.]Google Scholar
Koblents, Ya. P. Vliyaniye uklona poverkhnosti lednika na raspredeleniye snezhnogo pokrova [The influence of glacier slope on snow cover distribution]. Informatsionnyy Byulleten’ Sovetskoy Antarkticheskoy Ekspeditsii, No. 82, 1971, p. 5763. [Observations near “Molodezhnaya” station.]Google Scholar
Koblents, Ya. P., and others. O prakticheskom ispol’zovanii snezhnikov pribrezhnoy zony v svyazi s osobennostyami ikh formirovaniya (po nablyudeniyam v zalive Alasheyeva) [The practical use of snow-patches in the coastal zone in connection with features of their formation (from observations in Alasheyev Bight)]. [By] Koblents, Ya. P. Pshchelko, S. A., Fedotov, V. I. Trudy Sovetskoy Antarkticheskoy Ekspeditsii, Tom 57, 1971, p. 23545. [Snow-patches on fast ice.]Google Scholar
Kolomyts, E. G. Rost kristallov pri konstruktivnom metamorfizme snezhnoy tolshchi [The growth of crystals under constructive metamorphism in snow pack]. Materialy Glyatsiologicheskikh Issledovaniy. Khronika. Obsuzhdeniya, Vyp. 17, 1970, p. 11424. [Describes growth of secondary crystals in deposited snow in a continental climate. English summary, p. 170.]Google Scholar
Kopanev, I. D. Metody izucheniya snezhnogo pokrova [Methods of studying snow cover]. Leningrad, Gidrometeorologicheskoye Izdatel’stvo, 1971. 226 p. [English summary, p. 2.]Google Scholar
Kuindzhi, V. B., and Khodakov, V. G. Tayaniye snezhnika Khadatinskogo [The melting of the Khadata snow-drift]. Materialy Glyatsiologicheskikh Issledovaniy. Khronika. Obsuzhdeniya, Vyp. 18, 1971, p. 18387. [Tyumenskaya Oblast’.]Google Scholar
McCann, S. B., and Cogley, J. G. Hydrological observations on a small Arctic catchment, Devon Island. Canadian Journal of Earth Sciences, Vol. 9, No. 4, 1972, p. 36165. [Study of drainage basin of “Jason’s Creek”, flowing into Radstock Bay.]Google Scholar
Makeyev, V. M. Snezhnaya lavina [Snow avalanche]. Informatsionnyy Byulleten’ Sovetskoy Antarkticheskoy Ekspeditsii, No. 82, 1971, p. 9192. [Observations in Vassfjellet, Dronning Maud Land.]Google Scholar
Matviyenko, V. S. O vozmozhnosti priblizhennoy otsenki vetrovogo rezhima po formam snezhnogo mikrorel’yefa [An approximate estimation of a wind regime from snow microrelief forms]. Materialy Glyatsiologicheskikh Issledovaniy. Khronika. Obsuzhdeniya, Vyp. 17, 1970, p. 13037. [Major factor in the generation of snow microrelief forms is the saturation rate by snow particles of a drifting snow current. English summary, p. 171.]Google Scholar
Mayo, L. R. Self-mixing antifreeze solution for precipitation gages. Journal of Applied Meteorology, Vol. 11, No. 2, 1972, p. 40004. [Methanol-glycol mixture plus water or ice provides simple low-maintenance method of preventing freezing in gauges that receive large amounts of snow.]Google Scholar
Murozumi, M. Minami noyuki kita noyuki [Snows in the southern and northern polar regions]. Kyokuchi: Polar News, Vol. 7, No. 2, 1972, p. 4852.Google Scholar
Persson, M. Hydrologiska undersokningar i Lapptraskets representativa omnråde. Rapport 2. Snömätningar med snörör och snökuddar. Sveriges Meteorologiska och Hydrologiska Institut. Hydrologiska Byrån. Notiser och Preliminära Rapporter. Serie Hydrologi, No. 13, 1971, 32 leaves. [Snow measurements in Lappträsket region, north Sweden, by means of snow samplers and pressure pillows. Part of IHD programme. English summary on separate slip.]Google Scholar
Pont, A. Mattmark: les causes présumées de la chute catastrophique de 1965. Les Alpes. Revue du Club Alpin Suisse, 48 e An., 2e Trimestre, 1972, p. 12428. [Suggests cause of Swiss avalanche catastrophe.]Google Scholar
Rodda, J. C. Report on precipitation. A ‘state of the art’ report prepared on behalf of the Committee on Precipitation and presented at the General Assembly of the Association, Moscow, 1971. Bulletin de l’Association Internationale d’Hydrologie Scientifique, 16 e An., No. 4, 1971, p. 3747. [Includes measurement of snowfall.]Google Scholar
Rybak, O. L. Osobennosti formirovaniya i raspredeleniya snezhnogo pokrova v gornotayezhnoy zone yuga vostochnoy Sibiri [Snow cover formation and distribution peculiarities in mountainous taiga zone in the south of Eastern Siberia]. Materialy Glyatsiologicheskikh Issledovaniy. Khronika. Obsuzhdeniya, Vyp. 17. 1970, p. 13742. [Effect of temperature and altitude. Eastern Sayan and south Prebaykal’ye, Buryat-Mongol’skaya A.S.S.R. English summary, p. 171.]Google Scholar
Samukashvili, R. D. O vliyanii zacherneniya poverkhnosti snezhnogo pokrova na velichiny spektral’nykh potokov pronikayushchey radiatsii [Effect of blackening snow cover surface on spectral fluxes of penetrating radiation]. Materialy Glyatsiologicheskikh Issledovaniy. Khronika. Obsuzhdeniya, Vyp. 17, 1970, p. 10005. [A layer of black powder 1 cm thick prevented snow from melting. English summary, p. 170.]Google Scholar
Santeford, H. S., jr., and others Snowmelt energy exchange in the Lake Superior region, [by] Santeford, H. S. Jr., Alger, G. R. and Meier, J. G. Water Resources Research, Vol. 8, No. 2, 1972, p. 39097. [Stresses importance of effect of geothermal heat in determining snow melt in this region.]Google Scholar
Shamont’yev, V. A. Snegonakopleniye v krayevoy chasti antarkticheskogo lednikovogo pokrova na uchastke Mirnyy—105-y kilometr v 1966–1968 gg. [Snow accumulation in the marginal part of the Antarctic ice cover in the Mirny area—105 km in 1966–68]. Trudy Sovetskoy Antarkticheskoy Ekspeditsii, Tom 55, 1972, p. 15257. [Observations along Mirny-“Vostock” line.]Google Scholar
Snyder, F., and others, ed. Flood studies: an international guide for collection and processing of data. A contribution to the International Hydrological Decade. Edited by F. Snyder, A. Sokolov and K. Szesztay. Paris, UNESCO, 1971, 49 p. (Technical Papers in Hydrology, 8.) [Determination of flood flows from rain and snow melt and methods of estimating maximum flow.]Google Scholar
Tabler, R. D., and Veal, D. L. Effect of snow fence height on wind speed. Bulletin de l’Association Internationale d’Hydrologie Scientifique, 16 e An., No. 4. 1971, p. 4956. [Deals with the potential of snow fences for inducing snow accumulation as a means of increasing water yield from windswept areas.]Google Scholar
Vilenskiy, V. D., and Yemel’yanov, V. V. Opredeleniye skorosti snegonakopleniya v rayone stantsii Vostok s pomoshch’yu Pb210 [Determination of snow accumulation in the “Vostok” station region with the help of 210Pb]. Informatsionnyy Byulleten’ Sovetskoy Antarkticheskoy Ekspeditsii, No. 82, 1971, p. 1721.Google Scholar
Vinogradov, O. N. Nakopleniye snega na profile Mirnyy-stantsiya Vostok (po rezul’tatam nablyudeniy 1964 i 1969 gg.) [Snow accumulation along the profile Mirny-“Vostok” station (from results of observations in 1964 and 1969)]. Materialy Glyatsiologicheskikh Issledovaniy. Khronika. Obsuzhdeniya, Vyp. 17, 1970, p. 21622. [English summary, p. 222.]Google Scholar
Wasserman, S. E., and Monte, D. J. A relationship between snow accumulation and snow intensity as determined from visibility. Journal of Applied Meteorology, Vol. 11, No. 2, 1972, p. 38588. [Describes satisfactory method for estimating hourly snow accumulation from observations of snow intensity or visibility.]Google Scholar
Zalikhanov, M. Ch. K raspredeleniyu snezhnogo pokrova v gorakh Severnoy Osetii [On the distribution of snow cover in the mountains of Severnoya Osetiya]. Materialy Glyatsiologicheskikh Issledovaniy. Khronika. Obsuzhdeniya, Vyp. 18, 1971, p. 17477. [A.S.S.R. on north of Caucasus.]Google Scholar