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Glaciological Literature

Published online by Cambridge University Press:  21 June 2017

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Research Article
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Journal of Glaciology , Volume 18 , Issue 80 , 1977, pp. 523 - 546
Copyright
Copyright © International Glaciological Society 1977

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 Recent Polar Literature (supplement to 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 mi microfilming or photocopying.

Conferences

Bogorodskiy, V. V., and Gavrilo, V. P., ed. Fizicheskiye metody issledovaniye l’da i snega [Physical methods of ice and snow research]. Trudy Arkticheskogo i Antarkticheskogo Nauchhno-Issledovatel’skogo Instituta, Tom 326, 1975, [340] p. [Papers presented at symposium held in Leningrad, 1973. Contents include: V. V. Bogorodskiy, “Radiofizicheskiye metody issledovaniya l’da i snega [Radiophysical methods of ice and snow studies]”, p. 9–16; A. B. Babayev, V. P. Logachev, V. N. Parfent’yev, V. A. Fedorov and G. P. Shclomanova, “Radiolokatsionnyye ChM signaly, otrazhennyye ot ledovykh poverkhnostey i vozmozhnosti ikh modelirovaniya [Radar frequency-modulated signals reflected from ice surfaces and the possibility of modelling them]”, p. 17–20; A. Ye. Basharinov and A. A. Kurskaya, “Vliyaniye struktury l’da na yego radiatsionnyye kharakteristiki v SVCh diapazone [Ice structure and its effect on SHF emissivity]”, p. 21–23; V. V. Bogorodskiy, G. V. Trepov and B. A. Fedorov, “Rasprostraneniye radiovolnv gletcherakh [Radio-wave propagation in glaciers]”, p. 24–28; V. V. Bogorodskiy and V. P. Tripolnikov, “Radiozondirovaniye morskogo l’da [Radio-echo sounding of sea ice]”, p. 29–31; V. V. Bogorodskiy, A. I. Kozlov and L. T. Tuchkov, “Izluchatel’naya sposobnost’ ledyanykh, zemnykh i morskikh poverkhnostey. modeliruyemykh sloistoneodnorodnymi strukturami [Emissivity of ice, land and sea surfaces modelled by layered heterogeneous structures]", p. 32–38; J. W. Clough, “Izmereniya otrazhennykh signalov pri radiolokatsionnom zondirovanii v bol’shom diapazone uglov [Radio-sounding wide-angle reflection measurements]”, p. 39–44; J. W. Clough, “Depolyarizatsiya otrazhennykh radiosignalov [Depolarization of radio-echo returns]”, p. 45–50; M. I. Finkel’shteyn, V. A. Kutayev, V. G. Glushnev and E. I. Lazarev, “O distantsionnom izmerenii tolshchiny morskogo l’da metodami radiolokatsii [Remote radar measurements of sea ice thicknesses]”, p. 51–54; A. K. Zhebrovskiy, G. M. Strakhovskiy, V. N. Nedostayev and V. I. Stebin, “Elektricheskiye svoystva l’da, obrazovannogo v vakuume, i ikh vzaimosvyaz’ so strukturoy [Electrical properties of vacuum-deposited ice and their dependence on structure]”, p. 55–58; S. A. Vershinin, Ye. M. Kopaygorodskiy, V. V. Panov and Z. I. Shvayshteyn, “Davleniye l’da na otdel’no stoyashchiye opory po laboratoriymi naturiym ispytaniyam [Ice forces on separate supporting structures by laboratory and field tests]”, p. 59–65; H. Davis and R. Munis, “Vliyaniye solenosti morskogo l’da na opticheskuyu ekstinktsiyu sveta s dlinoy volny 6 328 Å [Correlation between the salinity of sea ice and extinction coefficient at 6 328 Å]”, p. 66–70; B. Ya. Gaytskhoki, “Opticheskiye kharakteristiki nekotorykh raznovidnostey yestestvennykh l’dov [Optical characteristics of some varieties of natural ice]”, p. 71–73; M. A. Kropotkin, “Apparatura dlya issledovaniya spektral’nogo otrazheniya zhidkoy vody v oblasti dlin voln ot 1 do 50 mkm [Instruments for the in vestigation of spectral reflection of liquid water in the range of wave lengths from 1 to 50 Mm]”, p. 74–79; V. Petera, “K voprosy izucheniya protsessa vozniknoveniya zaryadov na poverkhnosti razdela faz napravalenno zamerzayushchego 10–3 molyarnogo rastvora khlorida natriya [On the study of the process of charge generation at the phase interface of 10-3 molar solution of sodium chloride oriented during freezing]”, p. 80–89; L. B. Nekrasov, “Povedeniye l’da v bystroperemennykh elektromagnitnykh polyakh vysokoy napryazhennosti [The behaviour of ice in rapidly variable electromagnetic fields of high intensity]”, p. 90–93; B. V. Volod’ko, V. S. Yakupov, E. N. Akhmcdzyanov, V. M. Kalinin, V. O. Papitashvili and G. A. Sereda, “Magnitnaya s”yemka povtorno-zhil’nykh l’dov [Magnetic survey of ice wedges]”, p. 94–98; V. P. Melnikov and A. M. Snegirev, “Nizkochastotnaya polyarizatsiya l’da i merzlykh grubodispersnykh obrazovaniy [Low-frequency polarization of ice and frozen coarse-disperse formations]”, p. 99–103; S. M. Losev and Yu. A. Gorbunov, “Dinamika l’dov v pribrezhnykh rayonakh po dannym bokovoy radiolokatsionnoy s”yemki s samoleta [Coastal ice dynamics by SLAR observations]”, p. 104–13; A. I. Paramonov, Yu. A. Gorbunov and S. M. Losev. “Nablyudeniye za temperaturoy poverkhnosti morya s pomoshch’yu radiatsionnogo termometra s samoieta ledovoy razvedki [Observations of the surface temperature of the sea by airborne radiation thermometry]”, p. 114–20; V. P. Gavrilo and A. V. Gusev, “Primeneniye akusticheskikh metodov issledovaniya snega i l’da [Acoustic techniques in snow and ice studies]”, p. 121–27; V. V. Bogorodskiy, G. Ye. Smirnov and S. A. Smirnov, “Pogloshcheniye i rasseyaniye zvukovykh voln morskim l’dom [Attenuation and scattering of sound waves by sea ice]”, p. 128–34; N. A. Grubnik and O. V. Kudryavtsev, “Ob odnom metode izmereniya zatukhaniya zvuka v yestestvennom l’dy [A study of sound attenuation in natural ice]”, p. 135–36; V. N. Smirnov and Ye. M. Lin’kov, “Seysmicheskiye i naklonomernyye metody issledovaniya ledyanogo pokrova [Ice cover studies by seismic and tiltmeter methods]”, p. 137–42; I. M. Belousova, I. P. Ivanov and N. G. Firsov, “Izucheniye dinamiki lednikov s pomoshch’yu lazernogo deformografa [Glacier dynamics studies by laser deformograph]”, p. 143–46; V. V. Panov, A. V. Panyushkin, Yu. D. Sinochkin and Z. I. Shvayshteyn, “Eksperimental’noye izucheniye adgezii l’da v laboratoriykh i naturnykh usloviyakh [An experimental study of ice adhesion by laboratory and field tests]”, p. 147–54; N. A. Grubnik, V. I. Fomin and A. B. Shemyakin, “Izucheniye protsessa razrusheniya sloya l’da [A study of the process of ice layer destruction]”, p. 155–56; A. F. Wuori, “Mekhanicheskiye svoystva snega kak stroitel’nogo materiala [Mechanical properties of snow related to its use as a construction material]”, p. 157–64; I. M. Dolgin, N. N. Bryazgin and L. S. Petrov, “Snezhnyy pokrov Arktiki [Arctic snow cover]”, p. 165–70; S. I. Avdyushin [and 6 others], “Sposob izmereniya bol’shikh vlagozapasov v snezhnom pokrove po kosmicheskomu izlucheniyu [A technique to measure large moisture content in snow cover by cosmic radiation]”, p. 171–75; G. Abel’, “ Metody izmereniy prochnostnykh kharakteristik yestestvennogo i obrabotannogo snega [Techniques form easuring the strength characteristics of natural and processed snow]”, p. 176–86; A. Ya. Buzuyev, “Statisticheskaya otsenka prostranstvennogo raspredeleniya osnovnykh parametrov ledyanogo pokrova [Statistical evaluation of spatial distribution of the main parameters of the ice cover]”, p. 187–92; K. N. Korzhavin and A. B. Ivchenko, “Issledovaniye mekhanicheskikh svoystv presnovodnogo l’da pri medlennykh izmeneniyakh nagruzki [Study of mechanical properties of fresh-water ice with slowly variable load]”, p. 193–96; Yu. K. Zaretskiy, A. M. Fish, V. P. Gavrilo and A. V. Gusev, “Voprosy kratkovremennoy polzuchesti l’da i kinetika mikrotreshchinoobrazovaniya [On the short-term ice creep and micro-crack kinetics]”, p. 197–204; A. Ya. Ryvlin, “Naturnyye issledovaniya fiziko-mekhanicheskikh svoystv ledyanogo pokrova [Field tests of physical and mechanical properties of the ice cover]”, p. 205–09; D. Ye. Kheysin, V. A. Likhomanov and V. A. Kurdyumov, “Opredeleniye udel’noy energii razrusheniya i kontaktnykh davleniy pri udare tverdogo tela o led [Determination of specific failure energy and contact pressure on the impact of solid bodies on ice]”, p. 210–18; V. V. Bogorodskiy, V. P. Gavrilo and A. P. Polyakov, “Radiogidroakusticheskiy metod issledovaniya srednemasshtabnykh kharakteristik dinamiki morskikh l’dov [Radio-hydro-acoustical method to study meso-scale characteristics of sea-ice dynamics]”, p. 219–28.]

Frankenstein, G. E., ed. Proceedings, third intemational symposium on ice problems, 18–21 August 1975, Hanover, New Hampshire. [Hanover, N.H.], International Association of Hydraulic Research. Committee on Ice Problems, 1975. v, 627 p. [Contents include: V. V. Balanin, “Probngation of inland navigation terms in the U.S.S.R.”, p. 5–14; W. E. Webb and W. F. Blair, “Ice problems in locks and canals on the St. Lawrence River”, p. 15–24; E. Tesaker, “Accumulation of frazil ice in an intake reservoir”, p. 25–38; F. Boulanger, E. Dumalo, D. Le Van and L. Racicot, “Ice control study, Lake St. Francis–Beauharnois Canal, Quebec-Canada”, p. 39–48; J. J. Peter and T. V. Kotras, “Simulation of lock operations during winter ice months”, p. 49–58; D. J. Calkins and lVI. Melior, “Cost comparisons for lock wall deicing”, p. 59–67; V. Aleksandrov, V. V. Balanin, G. Onipchenko and V. Tronin, “Inland navigation and maintenance of hydraulic structures at negative air temperature in ice-bound conditions”, p. 69–79; J. V. Danys, “Ice movement control by the artificial islands in Lac St. Pierre”, p. 81–91; G. Tsang, “A field study of ice piling on shores and the associated hydro-meteorological parameters”, p. 93–110; C. Argiroff, “Planning the Great Lakes-St. Lawrence Seaway navigation season extension program”, p. 111–25; B. Michel and D. Bérenger, “Algorithm for accelerated growth of ice in a ship’s track”, p. 127–32; G. D. Ashton, “Experimental evaluation of bubbler-induced heat transfer coefficients”, p. 133–42; J. F. Kennedy, “Ice-jam mechanics”, p. 143–64; P. H. Burgi, “Hydraulic model studies of ice booms to co ntrol river ice”, p. 165–73; I. N. Sokolov and Ya. L. Gotlib, “Ice jam control upstream and downstream from hydro power plants”, p. 175–78; H. S. Uzuner, “Stability of ice blocks beneath an ice cover”, p. 179–85; E. V. Kanavin, “Water velocity in open and frozen rivers : control of ice production”, p. 187–99; T. E. Osterkamp, “Observations of Tanana River ice”, p. 201–09; T. O’D. Hanley and B. Michel, “Temperature patterns during the formation of border ice and frazil in a laboratory tank”, p. 211–21; V. V. Degtyarev, I. P. Butyagin and V. K. Morgunov, “Investigations of ice jams on the Siberian rivers and measures taken to prevent them”, p. 223–32; J. M. Maríusson, S. Freysteinsson and E. B. Elíasson, “Ice jam control. Experience from the Burfell power plant, Iceland”, p. 233–42; E. Zsilák, “Some new relatiomhips of the jammed ice motion”, p. 243–51; B. Michel and R. Abdelnour, “Break-up of a solid river ice cover”, p. 253–59; R. Gerard, “Preliminary observations of spring ice jams in Alberta”, p. 261–77; P. Rozsnyoí and I. Pados, “Regulation of the development of ice-barriers in the reach of the Tisza River above the barrage of Tiszalök for a secure winter operation of the barrage”, p. 279–88; R. R. Rumer, Jr., C. H. Atkinson and S. T. Lavender, “Effects of Lake Erie-Niagara River ice boom on the ice regime of Lake Erie”, p. 289–99; T. O’D. Hanley, “A note on the mechanism of frazil initiation”, p. 301–04; P. Larsen, “Notes on the stability of floating ice blocks”, p. 305–14; K. R. Croasdale, “Ice forces on marine structures”, p. 315–37; P. Tryde, “Intermittent forces acting on inclined wedges”, p. 339–43; M. Määtänen, “Ice forces and vibrational behaviour of bottom-founded steel lighthouses”, p. 345–55; T. Carstens and R. C. Byrd, “The oscillating icebreaking platform”, p. 357–59; A. Assur, “Problems in ice engineering”, p. 361–72; J. Schwarz, “On the flexural strength and elasticity of saline ice”, p. 373–86; L. J. Zabilansky, D. E. Nevel and F. D. Haynes, “Ice forces on simulated structures”, p. 387–95; R. E. Perham and L. Racicot, “Forces on an ice boom in the Beauharnois Canal”, p. 397–407; R. J. Hodek and J. C. Doud, “Instrumented piles for the measurement of ice-uplift forces”, p. 409–17; A. D. Kerr, “Ice forces on structures due to a change of the water level”, p. 419–27; Ken-ichi Hirayama, J. Schwarz and Han Chin Mu, “Ice forces on vertical piles: indentation and penetration”, p. 429–45; F. G. Bercha and J. V. Danys, “Prediction of ice forces on conical offshore structures”, p. 447–58; M. Metge, A. Strilehuk and P. Trofimenkoff, “On recording stresses in ice”, p. 459–68; Yu. V. Dolgopolov, V. P. Afanas’yev, V. A. Koren’kov and D. F. Panfilov, “Effect of hummocked ice on the piers of marine hydraulic structures”, p. 469–77; A. Traetteberg, L. W. Gold and R. [M. W.] Frederking, “The strain rate and temperature dependence of Young’s modulus of ice”, p. 479–86; A. I. Pekhovich, V. M. Zhidkikh, I. N. Shatalina and S. M. Aleynikov, “Control of the thickness and strength of the ice cover”, p. 487–98; D. V. Reddy, P. S. Cheema, A. S. J. Swamidas and A. K. Haldar, “Stochastic response of a three-dimensional offshore tower to ice forces”, p. 499–514; K. D. Vaudrey and M. G. Katona, “Viscoelastic finite element analysis of sea ice sheets”, p. 515–25; R. J. Evans and D. A. Rothrock, “Stress fields in pack ice”, p. 527–39; W. D. Hibler III, W. B. Tucker III and W. F. Weeks, “Measurement of sea ice drift far from shore using LANDSAT and aerial photogrammetric imagery”, p. 541–54; G. D. Rose, D. M. Masterson and C. E. Friesen, “Some measurements of laterally-loaded ice sheets”, p. 555–66; D. L. Kane, R. F. Carlson and R. D. Seifert, “Alaskan Arctic coast ice and snow dynamics as viewed by the NOAA satellites”, p. 567–77; V. M. Sinyavskaya and P. G. Dik, “Field studies of ice action on structures”, p. 579–88; R. Gerard, “A simple field measure of ice strength”, p. 589–600; International Association of Hydraulic Research. Committee on Ice Problems, “Report of task-committee on standardizing testing methods for ice”, p. 607–18.]

References

General glaciology

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Glaciological instruments and methods

Annan, A. P., and Davis, J. L. Impulse radar sounding in permafrost. Radio Science, Vol. 11, No. 4, 1976, p. 383–94. [Describes field testing of techniques in Tuktoyaktuk region of Mackenzie delta, Northwest Territories, Canada.]CrossRefGoogle Scholar
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Fukazawa, D. Dokuritsu-jūtaku ni okeru rakka-yane-yuki no yūsetsu shōri-hō [Method of melting snow sliding down the roof of an isolated building]. Seppyō, Vol. 38, No. 4, 1976, p. 188–95. [River water used to wash down slabs of snow from galvanized iron roof. English summary, p. 195.]Google Scholar
Getker, M. I., and Shentsis, I. D. Metodika opredeleniya optimal’nogo nabora snegopunktov dlya prognozov stoka gornykh rek [Methods of determination of the optimum number of snow survey points for forecasting mountain river run-off]. Materialy Glyalsiologicheskikh Issledovaniy. Khronika. Obsuzhdeniya, Vyp. 26, 1976, p. 184–93. [Describes method and applies to three river basins in Soviet Central Asia. English summary, p. 193.]Google Scholar
Grakovich, V. F. Metodika obrabotki glyatsiologicheskikh dannykh na EVM [Methods of computer handling of glaciological data]. Materialy Glyalsiologicheskikh Issledovaniy. Khronika. Obsuzhdelliya, Vyp. 25, 1976, p. 214–19. [Suggests methods. English summary, p. 219.]Google Scholar
Heimbach, J. A. jr., and others. A suggested technique for the analysis of airborne continuous ice nucleus data, [by]. Heimbach, J. A. Jr., Super, A. B. and McPartland, J. T. Journal of Applied Meteorology, Vol. 16, No. 3, 1977, p. 255–61. [Method of reducing data taking account of the large response times of these instruments.]Google Scholar
Hibler, W. D. III, and others. Techniques for studying sea ice drift and deformation at sites far from land using LANDSAT imagery, [by] Hibler, W. D. III, Tucker, W. B. III and Weeks, W. F. Proceedings of the tenth International Symposium on Remote Sensing of Environment ... 1975. ... Ann Arbor, Center for Remote Sensing Information and Analysis, Environmental Research Institute of Michigan, Vol. 1, [1975], p. 595–609. [Describes and discusses techniques to be used where there is no stationary land feature as point of reference.]Google Scholar
Hnatiuk, J., and Randall, A. G. Determination of permafrost thickness in wells in northern Canada. Canadian Journal of Earth Sciences, Vol. 14, No. 3, 1977, p. 375–83. [Compares and disc usses methods.]Google Scholar
Maksimov, N. V. Sovershenstvovaniye metodov ucheta osadkov v gorakh s pomoshch’yu summarnykh osadkomerav novykh konstruktsiy [Development of methods of measuring precipitation in mountains with the aid of newly designed gauges]. Materialy Glyatsiologicheskikh Issledovaniy. Khronika. Obsuzhdeniye, Vyp. 25, 1976, p. 220–22. [Describes and compares gauges. English summary, p. 222.]Google Scholar
Melnikov, V. P., and Guennadinik [i.e. Gennadlnik], B. I. La polarisation provoquée des roches co ngelées. Inter-Nord, Nos. 13–14, 1974, p. 87–98. [Discusses use of induced polarization method for investigating rock-pore-space structure in cryogenic fermations.]Google Scholar
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Tanaka, K., and others. Kōkenshutsu setsuryōkei no kōan to sono jikken hōkoku [Design of snow gauge using photoelectric effects]. [By] Tanaka, K. Yamaki, M. Masuda, S. Seppyō, Vol. 38, No. 4, 1976, p. 171–77. [Describes instrument used for estimating quantity of melt water flowing into reservoir during thawing season, in connection with hydroelectric power generation. English summary, p. 177.]Google Scholar
Turner, F. M. The design, construction and evaluation of an automatic airborne device for counting ice particles in clouds. Disserlation Abstracts Internalional, B, Vol. 37, No. 2, 1976, p. 913-B. [Abstract of Ph.D. thesis, University of Washington, 1975. University Microfilms order no. 76–17665.]Google Scholar
Watanabe, S., and others. Sekisetsu idō-ryō no ichi sokutei hōhō [A method for measuring snow gliding]. [By] Watanabe, S. Ōzeki, Y. Saeki, M. Seppyō, Vol. 38, No. 4, 1976, p. 196–97. [Describes simple device, tested over two winter seasons, for measuring snow movement down a slope.]Google Scholar
Wiensnet, D. R. Remote sensing and its application to hydrology. (In Rodda, J. C., ed. Facets of hydrology. London, New York, etc., John Wiley and Sons, [e 1976], p. 37–59.) [Chapter in survey of hydrology. Includes remote sensing of snow and ice.]Google Scholar
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Yemel’yanov, Yu. N., and others. O tochnosti izmereniya snegozapasov na gornykh Iednikakh [On the accuracy of measurement of snow storage on mountain glaciers]. [By] Yemel’yanov, Yu. N. Zhidkov, V. A. Nozdryukhin, V. K. Materialy Glyatsiologicheskikh Issledovaniy. Khronika. Obsuzhdeniya, Vyp. 26, 1976, p. 239–45. [Assesses accuracy of surveys from data obtained from Lednik Abramov, Kirgizskaya S.S.R. English summary, p. 245.]Google Scholar
Young, G. J. A portable profiling snow gauge; results of field tests on glaciers. Proceedings of the Western Snow Conference, 44th annual meeting, 1976, p. 7–11. [Instrument was satisfactory for measuring water equivalents of glacier snow-packs, but not so successful as a profiling instrument.]Google Scholar

Physics of ice

Andrews, D. A., and Newton, G. The stopping power of heavy ice for low energy (10–30 keV) deuterons. Journal of Physics D, Vol. 10, No. 6, 1977, p. 845–50. [Yields for D (d, n)T on a D2O ice target give stopping power lower than gas target values.]CrossRefGoogle Scholar
Barnaal, D., and others. Study of HF doped ice by pulsed NMR, [by] Barnaal, D. Kopp, M. [and] Loew, I. J. Journal of Chemical Physics, Vol. 65, No. 12, 1976, p. 5495–506. [Spin-lattice relaxation times determined as function of temperature and HF content and results interpreted in terms of defects induced by HF.]Google Scholar
Bartley, D. L. Monolayer ledges on basalice surfaces. Journal of Chemical Physics, Vol. 66, No. 3, 1977, p. 1063–66. [Analysis of classes of ledges and probabilities of jumps.]CrossRefGoogle Scholar
Bendell, M. S., and Gebhart, B. Heat transfer and ice-melting in ambient water near its density extremum. International Journal of Heat and Mass Tranfer, Vol. 19, No. 10, 1976, p. 1081–87. [Effect of changing temperature of water on natural convective now over vertical ice slab.]Google Scholar
Cecciii, R. Temperature dependent potential differences in ice crystals. Atti della Società Naturalisti e Matematici di Modena, Vol. 105, 1974, p. 153–58. [Measurement of potential differences on polycrystalline ice gives results that cannot be attributed to thermoelastic effect alone.]Google Scholar
Choularton, T. W., and Latham, J. Measurements of the deposition coefficient for ice, and its application to cirrus seeding. Quarterly Journal of the Royal Meteorological Society, Vol. 103, No. 436, 1977, p. 307–18. [Two techniques used to measure coefficient for deposition of water vapour molecules onto ice from distilled water and dilute HCl solutions. Results used to calculate distance cirrus crystals will fall below cloud base.]Google Scholar
Claus, R., and others. The proton distribution in ice-Ih investigated by light scattering. [by] Claus, R. and Plagge, W. Bilgram, J. Zeitschrift für Naturforschung, Teil a. Bd. 31a. Ht. 12, 1976, p. 1526–31. [Lack of phonon directional dispersion shows absence of ferroelectric domains of order of light wavelength. Depolarization ratio of phonons is isotropic implying statistically random proton distribution.]Google Scholar
Duval, P. Lois du fluage transitoire ou permanent de la glace polycristalline pour divers états de contrainte. Annales de Géophysique, Tom. 32, No. 4, 1976 [pub. 1977]. p. 335–50. [Creep tests under triaxial conditions confirm a power law relation in volving only one invariant for steady-state creep. Reversible component of logarithmic creep observed, also an Andrade transient component.]Google Scholar
Ermolleff, A., and others. Temperature dependence of the 306 and 227 cm-1 Raman lines in hexagonal ice between 250 and 80 K, [by] Ermolieff, A. and Chosson, A. Faure, P. Journal de Physique, Tom. 37, No. 12, 1976. p. 1457–59. [Search for coupling between acoustic and optic phonons in region of anomalous elastic behaviour reveals no sign of any equivalent anomalies.]Google Scholar
Fennema, O. R. Water and ice. (In Fennema, O. R., ed. Principles of food science. Part 1. food chemistry. New York and Basel, Marcel Dekker Inc., [e 1976], p. 13–39. (Food Science : a Series of Monographs, Vol. 4.)) [Review of properties of ice and water of relevance to food science.]Google Scholar
Ferraro, J. R. Some comments on solid state selection rules. Applied Spectroscopy, Vol. 30, No. 3, 1976, p. 369. [Problems in use of these rules, based on space-time average space groups, to predict experimental results. Ice Ih used as example.]Google Scholar
Filatova, Ye. V., and Filatov, A. O. Struktura metastabil’nykh faz vystro zamorozhennykh vodykh mincral’nykh dispersiy [Structure of metastable phases of quickly frozen aqueous mineral dispersions]. Kolloidnyy Zhurnal. Tom 38, Vyp. 6. 1976, p. 1203–05. [X-ray diffraction studies of rapidly frozen dispersions confirm existence of a metastable phase or phases of a nomalous ice. English summary, p. 1205.]Google Scholar
Franks, F. Water, ice and solutions of simple molecules. (In Duckworth, R. B., ed. Water relations of foods. Proceedings of an international symposium held in Glasgow, September 1974. London, etc., Academic Press, [e 1975], p. 3–22.) [Review of properties of water and ice and their relevance to food systems.]Google Scholar
Fukuta, N., and Armstrong, J. A. A new method for precision measurements of the deposition coefficient of water vapor onto ice. (In Becker, M., and Fiebig, M., ed. Rarefied gas dynamics. Proceedings of the ninth International Symposium (on Rarified Gas Dynamics), 1974, Vol. 2, [1975]. p. C.5–1—C.5–10.) [Method using cleavage of glacier ice single crystals and measuring temperature changes when crack width is less than mean free path of saturated water vapour.]Google Scholar
Gilpin, R. R. The effects of dendritic ice formation in water pipes. International Journal of Heat and Mass Transfer, Vol. 20, No. 6, 1977, p. 693–99. [Freezing of quiescent water in pipes usually nucleates at a supercooling of 4–6 deg and gives a dendritic structure which can give flow blockage with only a small frozen fraction.]CrossRefGoogle Scholar
Gorbunov, B. Z., and others. Issledovaniye zavisimosti l’doobrazuyushchey aktivnosti aerozolya yodistogo serebra ot dispersnosti [Ice-forming activity of silver iodide aerosols versus dispersal composition of aerosols at various temperatures of fog]. [By] Gorbunov, B. Z. Kakutkina, N. A. Koutsenogiy, K. P. Makarov, V. I. Izvestiya Akademiya Nank SSSR. Fizika Atmosfery i Okeana, Tom 12, No. 12, 1976, p. 1295–1302. [Study of ice-forming ability for different mean particle sizes and temperatures. English abstract, p. 1302.]Google Scholar
Haltenorth, H., and Klinger, J. Solubility of hydrofluoric acid in ice Ih single crystals. Solid State Communications, Vol. 21, No. 6, 1977, p. 533–35. [Saturation concentrations measured in boundary layer near the HF doping zone of ice crystals from 180 to 270 K. Most of the HF may be in small-angle boundaries or other perturbations.]CrossRefGoogle Scholar
Hardy, S. C. A grain boundary groove measurement of the surface tension between ice and water. Philosophical Magazine, Eighth Ser., Vol. 35, No. 2, 1977, p. 471–84. [Equilibrium state of grain-boundary grooves observed at an interface stabilized by a temperature gradient. Surface tension found to be 29. 1 ± 0.8 mJ m-2.]Google Scholar
Hubbard, K. G. Parameterization of depositional ice growth. Journal of Applied Meteorology, Vol. 16, No. 2, 1977, p. 177–82. [Parameterized equation developed and compared with a more detailed model.]Google Scholar
Hubmann, M. Ein universeller Zusammenhang zwischen den Parametern der dielektrischen Dispersion von Eis Ih. Helvetica Physica Acta, Vol. 50, Fasc. 2, 1977, p. 151. [Abstract only. Relation between dielectric dispersion strength and the ratio of low-frequency to high-frequency conductivity.]Google Scholar
Joncich, D. M. The plastic behavior of predeformed ice crystals. Dissertation Abstracts International, B, Vol. 37, No. 10, 1977, p. 5186-B-87-B. [Creep, constant strain-rate, and stress relaxation tests on ice pre-deformed at a higher stress to give a constant dislocation density. Results consistent with proton rearrangement in dislocation stress field as proposed by Weertman. Abstract of Ph.D. thesis, University of Illinois at Urbana–Champaign, 1976. University Microfilms order no. 77–9042.]Google Scholar
Kallungal, J. P., and Barduhn, A. J. Growth rate of an ice crystal in subcooled pure water. AIChE Journal (American Institute of Chemical Engineers), Vol. 23, No. 3, 1977, p. 294–303. [Data on growth rate in a-axis direction in qui escent and slow-Aowing water shows thermal natural convection to be an important mechanism. For slow or zero flow, steady growth is only observed horizontally or upwards. With high flow rates the growth ∝υ1/2ΔT3/2.]CrossRefGoogle Scholar
Kevan, L., and others. Silver atom solvation and desolvation in ice matrices : electron spin resonance studies of radiation-produced silver a toms formed at 4 K, by Kevan, L. Hase, H. Kawabata, K. Journal of Chelllical Physics, Vol. 66, No. 8, 1977, p. 3834–45. [New primary site found and attributed to Ag ion solution. This converts at 77 K to an Ag atom solvation site which can be desolvated optically at 4.2 K.]Google Scholar
Lacmann, R. Zur Deutung der Wachstumsformen des Eises. Zeitschrift für Physikalische Chemie (Wiesbaden), Neue Folge, 104. Bd., Ht. 1–3, 1977, p. 1–10. [Theory of temperature variation of development of ice crystals from the vapour based on a transitional quasi-liquid layer on the surface.]Google Scholar
Lavis, D. A. An exact matrix calculation for a two-dimensional model of the steam-water-ice system: bulk and boundary properties. Journal of Physics A, Vol. 9, No. 12, 1976, p. 2077–95. [Theoretical model.]Google Scholar
Lin, Y., and others. Compartmentalization of NaCl in frozen solutions of antifreeze glycoproteins, [by] Lin, Y. Raymond, J. A. Duman, J. G. and DeVries, A. L. Cryobiology, Vol. 13, No. 3, 1976, p. 334–40. [Experiments to study whether glycoproteins from Antarctic fish prevent concentration of NaCl during freezing. Effect due to spicular structure of ice from this solution which compartmentalizes brine pockets.]Google ScholarPubMed
Maï, C., and others. Dislocations et propriétés physico-mécaniques de la glace Ih, par Maï, C. Perez, J. Rivière, R. Tatibouet, J. et Vassoille, R. Annales de Physique, Quinzième Série, Vol. 2, No. 2, 1977, p. 91–118. [Review of characteristics of dislocations in ice and their influence on physical and mechanical properties.]Google Scholar
Matteson, S., and others. Physical-state effect in the stopping cross section of H2O ice and vapor for 0.3–2.0-MeV ∝ particles, [by] Matteson, S. Powers, D. and Chan, E. K. Physical Review A, Third Ser., Vol. 15, No. 3, 1977, p. 856–64. [Cross-section of vapour found to be (4–12)% higher than that of ice. Difference attributed to changes in modes of electronic excitation in the molecule due to aggregation.]Google Scholar
Michaeli, G. A study of the growth processes of small ice crystals under simulated cloud conditions. Dissertation Abstracts International, B, Vol. 37, No. 7, 1977, p. 3477-B-78-B. [Laboratory study of growth and fall rate of freely-falling ice crystals nucleated either by a chilled rod or by AgI nuclei. Abstract of Ph.D. thesis, Hebrew University of Jerusalem, 1976. University Microfilms order no. 76–30289.]Google Scholar
Mizuno, Y. Ekkisu-sen niyoru kōri no kūzō no kansetsu [X-ray topographic observation of vapour figures in single crystals of ice). Teion-kagaku: Low Temperature Science, Ser. A, [No.] 33, 1975, p. 17–27. [Samples of Mendenhall Glacier ice showed high dislocation density around vapour figures. English summary, p. 26–27.]Google Scholar
Mogensen, O. E., and Eldrup, M. On the vaca ncy concentration in ice. Physics Letters A, Vol. 60A, No. 4, 1977, p. 325–26. [Vacancy concentration deduced from diffusion data reaches at least 10-6 near melting point.]Google Scholar
Montefinale, T., and Papee, H. M. Thresholds of bulk contact ice nucleation of some photosensitive surfaces. Journal of Colloid and Interface Science, Vol. 59, No. 2, 1977, p. 337–41. [Measured for Cu2S, Ag2S, MoS2, CdS and results interpreted in terms of hygroscopic sites formed by chemical transitions.]Google Scholar
Ozüm, B., and Kirwan, D. J. Impurities in ice crystals grown from stirred solutions. AIChE Symposium Series (American Institute of Chemical Engineers), Vol. 72, No. 153, 1976, p. 1–6. [Observations in NaCI and sucrose solutions. Solute incorporations due to trapping in dendritic interface.]Google Scholar
Pitter, R. L. A reexamination of riming on thin ice plates. Journal of the Atmospheric Sciences, Vol. 34, No. 4, 1977, p. 684–85. [Revision of earlier paper by Pitter and Pruppacher, H. R. (ibid., Vol. 31, No. 2, 1974, p. 551–59) to include local Reynolds-number effects shows higher collision efficiencies with the larger drops.]Google Scholar
Prince, R. H. Low-temperature diffusion of electrons in ice. Evidence for polaron bands. Physica Status Solidi B, Vol. 78, No. 1, 1976, p. 271–76. [Hopping activation energy for localized polaron states measured as 0.065 eV. Below c. 125 K polaron band motion observed. Relevance of fluorescence and thermoluminescence in ice.]Google Scholar
Prince, R. H., and Floyd, G. R. Production of ionized clusters by electron bombardment of condensed polar solvents. Chemical Physics Letters, Vol. 43, No. 2, 1976, p. 326–31. [Mass spectra of products interpreted. Includes ice.]Google Scholar
Raymond, J. A. Adsorption inhibition as a mechanism of freezing resistance in polar fishes. Dissertation Abstracts International, B, Vol. 37, No. 4, 1976, p. 1579-B. [Physical process of this inhibition studied. When solutions of antifreezes were frozen, the antifreezes were partially incorporated in the ice and strongly influenced growth habit. Model of action proposed and possible uses discussed. Abstract of Ph.D. thesis, University of California, San Diego, 1976. University Microfilms order no. 76–23143.]Google Scholar
Rennie, G. K., and Cufford, J. Melting of ice in porous solids. Journal of the Chemical Society. Faraday Transactions I, Vol. 73, Pt. 4, 1977, p. 680–89. [Differential scanning calorimetry used. At low water contents (<3 monolayers) no freezing or melting observed. With more water a single melting peak was seen until pores filled completely above which two peaks were found.]Google Scholar
Resca, L., and Resta, R. Energy bands in cubicice. Ab initio calculation using the method of linear combination of molecular orbitals. Physica Status Solidi (B), Vol. 81, No. 1, 1977, p. 129–38. [Theoretiol calculation by LCMO method. Results compared with experimental data.]Google Scholar
Saitoh, T. Natural convection heat transfer from a horizontal ice cylinder. Applied Scientific Research, Vol. 32, No. 4, 1976 [pub. 1977], p. 429–51. [Heat-transfer studied when passing through the maximum density point both experimentally and theoretically. At about 6°C an instability of flow occurs.]Google Scholar
Sassen, K. Optical backscattering from near-spherical water, ice, and mixed phase drops. Applied Optics, Vol. 16, No. 5, 1977, p. 1332–41. [Experimental study.]CrossRefGoogle ScholarPubMed
Schmidt, P., and Walzel-Wiesentreu, P. Ausfrieren von Eis an vibrierten Kühlflächen. Chemie Ingenieur Technik, 49. Jahrg., Nr. 2, 1977, p. 169. [Study of growth of ice from an aqueous solution ming a vibrating cold surface. Summary cf a 40 p. manuscript obtainable as photocopy or microfiche MS 451/77 from Verlag Chemie.]Google Scholar
Schnell, R. C. Bacteria acting as natural ice nucleants at temperatures approaching - 1°C. Bulletin of the American Meteorological Society, Vol. 57, No. 11, 1976, p. 1356. [Letter. Bacterial ice nucleants can be important and some bacteria may reduce plant resistance to freezing. Control of these may be economically important.]Google Scholar
Schuster, P., and others, ed. The hydrogen bond. Recent developments in theory and experiments, [edited by] Schuster, P. Zundel, G. Sandorfy, C. Amsterdam, etc., North Holland Publishing Co., 1976. 3 vols : viii, 390; 391–888; 889–1549 p. [Review of present knowledge of hydrogen bonding with reference to ice in many chapters, in particular: ch. 7, “Hydrogen bond statistics”, by Perram, J. W.; ch. 19, “Incoherent neutron scattering experiments on hydrogen bonded systems”, by Janik, J. A.; ch. 20, “Dielectricproperties of hydrogen bonded systems”, by Sobezyk, L. Engelhardt, H. and Bunzl, K.; ch. 27, “Hydrogen bonds in systems of adsorbed molecules”, by Knözinger, H.; ch. 29, “The hydrogen bond in ice”, by Whalley, E.]Google Scholar
Shibaguchi, T., and others. Electronicstructures of water and ice, by Shibaguchi, T. Onuki, H. and Onaka, R. Journal of the Physical Society of Japan, Vol. 42, No. 1, 1977, p. 152–58. [Ultraviolet and X-ray photoelectron spectroscopy and vacuum ultraviolet absorption spectroscopy used to deduce electronic band structure of ice.]Google Scholar
Simons, G. A. Aerodynamic shattering of ice crystals in hypersonic flight. AIAA Journal (American Institute of Aeronautics and Astronautics), Vol. 14, No. 11, 1976, p. 1563–70. [Theoretical study to assess relative kinetic energy of an ice crystal on impact. Fragments continue to shatter and prevent entry of shock-layer gas.]Google Scholar
Suzuki, S. Sōsakei denshi-kenbikyō ni yoru kōri no hyōmen no kansatsu. 2. Reikyaku ni tomonau shika no ōscn [Observation of ice surfaces by a scanning electron microscope. 2. Contamination on ice crystal surface]. Teioll-kagaku: Low Temperature Science, Ser. A, [No.] 33, 1975, p. 1–9. [To observe ice in the electron microscope it has to be cooled to liquid nitrogen temperature. Despite the vacuum in the chamber. a film of contaminants forms on the ice over 60–100 min. English summary, p. 8–9.]Google Scholar
Suzuki, S. Sōsakei denshi-kenbikyō ni yoru kōri no hyōmen no kansatsu. 3. Kōri no furakutogurafii [Observation of ice surfaces by a scanning electron microscope. 3. Fractography of ice crystal]. Teioll-kagaku: Low Temperature Science, Ser. A, [No.] 33, 1975. p. 11–15. [High resolution and high depth of focus used to study fracture surface immediately after fiacturing on cold stage. English summary, p. 14–15.]Google Scholar
Takahashi, T., and Wakahama, G. Kōri no netsuōryoku no sokutei [A study on thermal. stresses in ice]. Teion-kagaku : Low Temperature Science, Ser. A, [No.] 33, 1975, p. 29–37. [Observations of thermal stresses induced in cylinders of ice immersed in a kerosene bath. Results for different kinds of polycrystalline ice and for single crystals. English summary, p. 36–37.]Google Scholar
Tovbin, M. V., and others. Vliyaniye adsorbtsionnogo modifitsirovaniya poverkhnosti kristallicheskikh veshchestv na ikh l’doobrazuyshchuyu aktivnost’ [Influence of adsorption modification of the surface of crystalline substances on their ice-forming activity). [By] Tovbin, M. V. Chesha, I. I. Gel’man, L. A. Kolloidnyy Zhurnal, Tom 39, Vyp. 1, 1977, p. 213–15. [Ice-forming reagents can be produced by surface modification of inactive materials by producing a mosaic surface-layer structure which optimizes the hydrophilic-hydrophobic balance. English summary, p. 215.]Google Scholar
Turner, J. S. Laboratory experiments on double-diffusive instabilities. Advances in Chemical Physics, Vol. 32, 1975, p. 135–49. [Study of convective motions in fluids with heat and salinity gradients or two solutes. Includes effect of inserting a slab of ice vertically into a previously stable salinity gradient.]Google Scholar
Viaud, P. R. Theoreti cal and experimental study of stationary profiles of a water-ice mobile solidification interface. Advances in Chemical Physics, Vol. 32, 1975, p. 163–205. [Stability criteri on developed. Coupling between thermal conditions and interface behaviour described.]Google Scholar

Land ice. Glaciers. Ice shelves

Atlas, L. E., and others. Reki basseyna oz. Karakul’.—Basseyn verkhov’yev r. Markansu [River basins of Ozeru Karakul’.—Basin of the upper reaches of the river Markansu). [By] Atlas, L. E. Barnakova, G. M. Rototayeva, O. V. Katalog lednikov SSSR [Catalogue of glaciers of the U.S.S.R.], Tom 14, Vyp. 3, Chast’ 18, 19, 1975, [80] p. [Part of I.H.D. catalogue giving details of what is known of glaciers in this part of Central Asia. The Tom and Vyp. numbers correspond with those of Resursy poverkhnostnykh vod SSSR [Surface water resources of the U.S.S.R.].]Google Scholar
Barkov, N. I., and others. Izotopnyye issledovaniya ledyanogo kerna so stantsii Vostok (Antarktida) do glubiny 950 m [Isotopic studies of an ice core from Vostok station (Antarctica) to a depth of 950 m]. [By] Barkov, N. I. Gordiyenko, F. G. Korotkevich, Ye. S. Kotlyakov, V. M. Doklady Akademii Nauk S.S.S.R., Tom 230, No. 3, 1976, p. 656–59. [18O profile.]Google Scholar
Berri, B. L., and Golubev, G. N. Opyt primeneniya rezistivimetrii v gidrologii lednikov [Experiments in application of measurements of electrical conductivity in glacier hydrology]. Materialy Glyatsiologicheskikh Issledovaniy. Khronika. Obsuzlzdeniya, Vyp. 25, 1976, p. 96–105. [Field work on Lednik Dzhankuat, Caucasus. English summary, p. 104–05.]Google Scholar
Björnsson, H. Subglacial water reservoirs, jökulhlaups and volcanic eruptions. Jökull, Ár 25, 1975 [pub. 1976], p. 1–14. [Discusses causes of jökulhlaups with references to particular events in Iceland. Icelandic summary, p. 12–14.]Google Scholar
Björnsson, H., and others. A 1976 radio echo sounding expedition to the Vatnajökull ice cap, Iceland, by Björnsson, H. Ferrari, R. L. Miller, K. J. and Owen, G. Polar Record, Vol. 18, No. 115, 1977, p. 375–77. [Results of first year of two-year project to develop apparatus suitable for temperate ice.]Google Scholar
Boyarskiy, V. I., and Shalygin, A. M. Radiolokatsionnaya s”yemka podlednogo rel’yefa devyatnadtsatoy Sovetskoy antarkticheskoy ekspeditsiyey [Radio-echo sounding survey of sub-ice relief during the nineteenth Soviet Antarctic expedition]. Informatsionnyy Byulleten’ Sovetskoy Antarkticheskoy Ekspeditsii, No. 92, 1976, p. 18–23.Google Scholar
Bull, C. B. B. The disposal of rad ioactive wastes in the Antarctic ice sheet. Notes on a meeting held at the Scott Polar Research Institute, Cambridge, on 25 September 1974. I.U.G.G. Chronicle, No. 102, 1975, p. 163–67.Google Scholar
Cherkasov, P. A. Basseyny rek Khorgosa, Useka [Basins of the rivers Khorgosa and Useka]. Katalog lednikov SSSR [Catalogue of glaciers of the U.S.S.R.], Tom 13, Vyp. 2, Chast’ 4, 1975, [84] p. [Part of I.H.D. catalogue giving details of what is known of glaciers in this part of Kazakhstan. The Tom and Vyp. numbers correspond with those of Resursy poverkhnostnykh vod SSSR [Surface water resources of the U.S.S.R.].]Google Scholar
Chernova, L. P., and Chernov, A. A. Otsenka rasseyaniya energii dlya ploskoy modeli lednika [Estimation of the dispersion of energy for a two-dimensional glacier model]. Materialy Glyatsiologicheskikh Issledovaniy. Khronika. Obsuzhdeniya, Vyp. 25, 1976, p. 175–77. [English summary, p. 177.]Google Scholar
Clough, J. W. Electromagnetic lateral waves observed by earth-sounding radars. Geophysics, Vol. 41, No. 6A, 1976, p. 1126–32. [Discusses example recorded on Ross Ice Shelf, Antarctica.]Google Scholar
Colvill, A. J. Cambridge east Greenland expedition, 1976. Polar Record, Vol. 18, No. 115, 1977, p. 378–79. [Results of survey of Roslin Gletscher, Stauning Alper.]CrossRefGoogle Scholar
Davidovich, N. V. Nekotoryye cherty mikroklimatichcskikh razlichiy v firnovoy oblasti gornogo lednika [On some peculiarities of microclimate difference, in the firn area of a mountain glacier]. Materialy Glyatsiologicheskikh Issledouaniy. Khronika. Obsuzlzdeniya, Vyp. 25, 1976, p. 84–90. [Study of microclimate of Lednik Marukh, Caucasm. English summary, p. 89–90.]Google Scholar
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Icebergs. Sea, River and Lake Ice

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Glacial Geology

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Chuklenkova, I. N. O rasprostranenii pokrovnogo oledeneniya na severe russkoy ravniny v pozdnem pleystotsene (analiz morfometricheskikh dannykh) [On the spreading of the ice sheet in the northern areas of the Russian plain (interpretation of morphometric data)]. Materialy Glyatsiologicheskikh Issledovaniy. Khronika. Obsuzlideniya, Vyp. 25, 1976, p. 196–99. [English summary, p. 199.]Google Scholar
Drozdowski, E. Penultimate period of deglaciation in the Grudziadz basin, lower Vistula river valley : an interstadial-like interval of the middle Würm. Geographia Polonica, 31, 1975, p. 213–35. [Reconstructs processes of down-wating by studies of landforms and deposits.)Google Scholar
Gillberg, G. Drumlins in southern Sweden. Bulletin of the Geological Institutions of the University of Uppsala, New Series, Vol. 6, p. 125–89. [Describes large number of drumlins in this area and discusses their formation.]Google Scholar
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Harmon, R. S. Late Pleistocene glacial chronology of the South Nahanni River region, Northwest Territories, Canada. Michigan Academician, Vol. 9, No. 2, 1976, p. 147–56. [Identified by means of speleothems.]Google Scholar
Hays, J. D., and others. Variations in the Earth’s orbit: pacemaker of the ice ages, [by) Hays, J. D. Imbrie, J. Shackleton, N. J. Science, Vol. 194, No. 4270, 1976, p. 1121–32. [Concludes that changes in Earth’s orbit are cause of succession of Quaternary ice ages and predicts long-term trend over next several thousand years is toward extensive glaciation of northern hemisphere.]Google Scholar
Hillefors, Å. Contribution to the knowledge of the chronology of the deglaciation of western Sweden with special reference to the Gothenburg moraine. Svensk Geografisk Årsbok, Årg. 51, 1975, p. 70–81. [Suggests moraine was formed owing to oscillations of inland ice during late Dryas and between late Dryas and Böiling interstadial.)Google Scholar
Hughes, T. J., and others. Was there a Jate-Würm Arctic ice sheet? [By] Hughes, T. J. and Denton, G. H. Grosswald, M. G. [i.e. Grosval’d]. Nature, Vol. 266, No. 5603, 1977, p. 596–602. [Simplification and synthesis of late-Würm northern hemisphere glaciation is possible by postulating Arctic ice sheet that behaved as single dynamicsys tem.]Google Scholar
Ivanovskiy, L. N. Drevnelednikovyy rel’yef i drevneye oledeneniye gor Sibiri i Dal’nego Vostoka [Ancient glacial relief and ancient glaciation of mountains in Siberia and the far east]. Izvestiya Vsesoyluznogo Geograficheskogo Obshchestva, Tom 108, Vyp. 2, 1976, p. 116–22.Google Scholar
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Janossy, D. The influence of the glaciations on the microvertebrate fauna in the periglacia l area in Europe. Geologiska Föreningens i Stockholm Förhandlingar, Vol. 98, Pt. 4, No. 567, 1976, p. 291–96. [Refers to conditions in Hungary.)Google Scholar
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Johnson, C. B. Characteristics and mechanics of formation of glacial arcuate abrasion cracks. Dissertation Abstracts International, B, Vol. 36, No. 11, 1976, p. 5476-B. [Interpretation of four basic types. Abstract of Ph.D. thesis, Pennsylvania State University, 1975. University Microfilms order no. 76-10738.]Google Scholar
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Karczewski, A. Morphology and textural–structural features of ground and hummocky moraine in the Paistunturit area, Finnish Lapland. Reports from the Kevo Subarctic Research Station, Vol. 12, 1975, p. 34–44. [Includes attempt to define type and character of deglaciation in area.]Google Scholar
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Klajnert, Z. Struktura form szczelinowych akumulowanych w warunkach martwego lodu i jej związek z dynamiką procesów deglacjacji na podstawie badań w południowej Zelandii (Dania) i w Polsce środkowej [Interrelation between the structure of crevasse filling forms accumulated in dead ice and the dynamics of deglaciation processes on the basis of investigation carried out in South Zealand (Denmark) and in central Poland]. Acta Geographica Lodziensia, Nr. 37, 1976, p. 53–72. [Discusses development of eskers and kames. English summary, p. 71–72.]Google Scholar
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Lapshin, A. V. Izmeneniye ob”yema kontinental’nogo oledeneniya zemli za posledniye 35 tysyach let [Changes in the volume of continental glaciation of the Earth for the last 35 000 years]. Materialy Glyatsiologicheskikh Issledovaniy. Khronika. Obsuzhdeniya, Vyp. 25, 1976, p. 39–44. [Considered on basis of sea-level fluctuations. English summary, p. 44.]Google Scholar
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Frost Action on Rocks and Soil. Frozen Ground. Permafrost

Aguirre-Pente, J. Aperçu sur le problème de la congélation des sols. Inter-Nord, Nos. 13–14, 1974, p. 323–26. [Brief outline of problems and recent studies in permafrost research.] Google Scholar
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Anderson, D. M. Department of the Army, Cold Regions Research and Engineering Laboratory. Biuletyn Peryglacjalny, No. 26, 1976, p. 148–52. [Describes research carried out at CRREL, with particular reference to periglacial phenomena.] Google Scholar
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Daniels, J. J., and others. Computer-assisted interpretation of electromagnetic soundings over a permafrost section, [by] Daniels, J. J., Keller, G. V. and Jacobson, J. J.. Geophysics, Vol. 41, No. 4, 1976, p. 752–65. [Procedure used to interpret two-locp electromagnetic soundings made along Arctic Slope of Alaska to determine permafrost thickness and character.] Google Scholar
Donnay, J., and others. Observations sur photos aériennes de structures périglaciaires en Ardenne centrale, [par] Donnay, J., Macar, P., Ozer, A. et Pissart, A.. Biuletyn Peryglccjalny, No. 26, 1976, p. 205–09. [Describes fossil periglacial phenomena observed by means of air photographs in Belgium.] Google Scholar
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[Frozen Ground.] Dix ans de recherches au Centre de Céomorphologie. Centre National de la Recherche Scientifique. Centre de Géomorphologie de Caen. Bulletin No. 21, 1976, 95 p. [Includes: Journaux, A. and. Coutard, J. P. “Les expériences sur l’action du gel dans les sols”. p. 13–20; Lautridou, J. P. “Les expériences de cryoclastie”, p. 21–28; Caniard, L. de Boissoudy, A. and Bertouille, H. “Étude du comportement d’une structure routière soumise à des cycles de gel-dégel en simulation expérimentale à la station de gel de Cacn”, p. 63–72; Bertouille, H. “Études théoriques et propositions expérimentales”, p. 73–77.]Google Scholar
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Higashi, A. Ice Research Laboratory, Department of Applied Physics, Hokkaido University, Sapporc, Japan. Biuletyn Peryglacjalny, No. 26, 1976, p. 114–17. [Describes recent research on periglacial phenomena conducted in this laboratory.]Google Scholar
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Ladanyi, B. Université de Montréal, École Polytechnique, Centre d’Ingénierie Nordique. Biuletyn Peryglacjalny, No. 26, 1976, p. 153–58. [Research at the Centre is mainly into northern engineering with emphasis on frozen ground mechanics.]Google Scholar
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Mackay, J. R. Probing for the bottom of the active layer. Project 680047. Canada. Geological Survey. Paper 77-1A, 1977, p. 327–28. [Can be located in icy and ice-bonded soils by “feel”, but not in fine-grained soils free of ice lenses.]Google Scholar
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Mackay, J. R. The widths of ice wedges. Project 680047. Canada. Geological Survey. Paper 77-1A, 1977, p. 43–44. [Apparent width is about 50% greater than true width; apparent height is usually true.]Google Scholar
Meneghel, M. Alcune nisure su fenomeni di soliflusso osservati presso il passo Pordoi (Dolomiti ). Bollettino del Comitato Glaciologico Italiano, Ser. 2, No. 24, 1976, p. 9–21. [Although solifluction near this pass seems to be active still, some mud tongues were probably formed in period when climate could have caused periglacial environment.]Google Scholar
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Pissart, A. Université de Liège. Biuletyn Peryglacjalny, No. 26, 1976, p. 118–27. [Describes research into periglacial processes carried out at this university in the Laboratoire de Géologie et Géographie Physique.]Google Scholar
Poppe, V. N., and Brown, R. J. E. Russian–English glossary of permafrost terms. Canada. National Research Council. Associate Committee on Geotechnical Research. Technical Memorandum No. 117, 1976, iii 1., 25 leaves. [Russian terms given in Cyrillic script.]Google Scholar
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Meteorological and Climatological Glaciology

Allison, I., and Kruss, P. Estimation of recent climate change in Irian Jaya by numerical modeling of its tropical glaciers. Arctic and Alpine Research. Vol. 9, No. 1, 1977, p. 49–60. [Carstensz and Meren glaciers, Papua New Guinea.]Google Scholar
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Snow

Adams, W. P. Areal differentiation of snow cover in east central Ontario. Water ResourccS Research, Vol. 12, No. 6, 1976, p. 1226–34. [Studies variation of depth, mean density, and water equivalent among seven vegetation types in area where vegetation is dominant control of areal variation of snow cover.]Google Scholar
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Yong, R. N., and Fukue, M. Compression shear performance of snow. McGill University. Dept. of Civil Engineering and Applied Mechanics. Soil Mechanics Research Laboratory. Soil Mechanics Series No. 35, 1976, i 1., 30 leaves. [Related to behaviour of wheels on snow.]Google Scholar