Hostname: page-component-cd9895bd7-dzt6s Total loading time: 0 Render date: 2024-12-23T11:55:34.234Z Has data issue: false hasContentIssue false

Glaciological Literature

Published online by Cambridge University Press:  30 January 2017

Rights & Permissions [Opens in a new window]

Abstract

Type
Research Article
Copyright
Copyright © International Glaciological Society 1974

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 microfilming or photocopying.

References

Conferences

[Conference: Permafrost.] Permafrost. Second International Conference. 13–28 July 1973, Yakutsk, U.S.S.R,.North American contribution. Organizing Committee of Canada, National Research Council of Canada and United States Planning Committee, U.S. National Academy of Sciences, National Academy of Engineering, National Research Council. Washington, U.C., National Academy of Sciences, 1973. xi, 783 p. [For details of individual papers see elsewhere in this list.]Google Scholar
Kotlyakov, V. M., ed. Glyatsiogidroklimatologiya gornykh stran [Glaciohydroclimatology of highlands]. Rezid’taty Issledovaniy po Mezhdunarodnym Geofizkheskim Proyektam. Glyatsiologicheskiye Issledovaniya, No. 24, 1973, 199 p. [Papers presented at the fourth all-Union glaciological symposium, held in 1968 at Terskol in the Caucasus.]Google Scholar
Orvig, S., ed. Energy fluxes over polar surfaces: proceedings of the IAMAP/IAPSO/SCAR/ WMO Symposium, Moscow, 3–5 August 1971. Geneva, World Meteorological Organization, 1973. [viii], 299. P. (World Meteorological Organization, Technical Note No. 129; WMO, No. 361.) [For details of individual papers see elsewhere in this list.)Google Scholar
Péwé, T. L.Northeast Siberia—a report on the second International Conference on Permafrost. Arctic Bulletin, Vol. 1, No. 2, 1973, p. 39–36. [Account of conference, held in Yakutsk, 15–28 July 1973 and of field excursions, mentioning glaciological features observed.]Google Scholar

General

Govorukha, L. S.Glyatsiologicheskiye issledovaniya na lednikakh o. Desepshen v period raboty mezhdunaiod noy vulkanologicheskoy ekspeditsii [Glaciological research on Deception Island during the international vulcanology expedition]. Trudy Arkticheskogo i Antarkticheskogo Nauchno-Issledovatel’skogo Instituta, Tom 318, 1973, p. 8799. [1970 expedition.]Google Scholar
Lorius, C., and Vaugelade, J.International Antarctic Glaciological Project traverse, Dumont d’Urville to Vostok. Antarctic Journal of the United States, Vol. 8, No. 4, 1973, p. 171–72- [Describes 1972–73 activities.]Google Scholar
Murray, B.C., and Malin, M. C.Polar volatiles on Mars. Theory versus observation. Science, Vol. 182, No. 4111, 1973, p. 437–43. [Results of Mariner 9 mission used to discuss nature of polar caps on Mars.]CrossRefGoogle ScholarPubMed
Nunnally, N. R.ERTS-1 imagery and Arctic research: the systems and its operation. Arctic Bulletin. Vol. 1, No. 2, 1973, p. 3843. [General information, including observations currently being made of sea ice, snow cover and glaciers.]Google Scholar
Sekanina, Z.Existence of icy comet tails at large distances from the Sun. Astrophysical Letters, Vol. 14, No. 4, 1973 P 175–80. [Size distribution implies presence of clathrate hydrates.]Google Scholar
Siren, J. C.Radioactive wastes. Physics Today, Vol. 27, No. 2, 1974, p. 15, 67. [Comment on article by J. O. Blomeke, J. P. Nichols and W. C. McClain, ibid., Vol. 26, No. 8, 1973, p. 3643, which dismisses idea of disposing waste in ice sheets, with reply by authors stating why they so dismissed it.]Google Scholar
Ten Brink, N. W., and> Curl, J. E.Glaciology and glacial chronology in the South Shetland Islands. Antarctic Journal of the United States, Vol. 8, No. 4, 1973, p. 175–77- [Describes 1972–73 field work on Deception and Livingston Islands.]Google Scholar

Glaciological Instruments and Methods

Denton, G. H., and Karién, W.Lichenometry: its application to Holocene marine studies in southern Alaska and Swedish Lapland. Arctic and Alpine Research, Vol. 5, No. 4, 1973, p. 347–72. [Discusses techniques and problems in application of lichenometry.]10.2307/1550128CrossRefGoogle Scholar
Finsterwalder, Rüdioer. Begleitwort zur Karte des Vernagtferners 1: 10.000 vom Jahre 1969. zeitschrift für Gletscherkunde und Glazialgeologie, Bd. 8, Ht. 1–2, 1972, p. 510. [Presents map (in separate map supplement) composed from air photographs, conceived as a topographical map with geodetic and glaciological content. Explains methods of survey and discusses means of cartographic representation.]Google Scholar
Tōkairin, A.Kandenchi-shiki kan’i nessen hyōkō-kei ni tsuite [On the measurement of ice growth by hot-wire ice thickness meter]. Stppō, Vol. 35, No. 4, 1973, p. 169–72. [Description of hot-wire apparatus for measuring thickness of floating ice as a function of time. English summary, p. 172.]Google Scholar
Turner, F. M., and Radke, L. F.The design and evaluation of an airborne optical ice particle counter. Journal of Applied Meteorology, Vol. 13, No. 8, 1973, p. 1309–18. [Description of apparatus that uses birefringence of ice lo distinguish and reject water drops.]2.0.CO;2>CrossRefGoogle Scholar
Warner, G. G.The measurement of surface strain in glaciers using embedded resistance strain gages. Dissertation Abstracts International, B, Vol. 34, No. 6, 1973, p. 2648-B. [Description of gauges, which consist of five 10-foot (3 m) constantan wires and their testing in Ptarmigan Glacier, Alaska, and Cathedral Glacier, British Columbia, Canada. Abstract of Ph.D. thesis, Michigan State University, 1973. University Microfilms order no. 7329795.]Google Scholar
Weiss, H. V., and Bertink, K. K.Simultaneous determination of manganese, copper, arsenic, cadmium, antimony and mercury in glacial ice by radioactivation. Analytica Chimica Acta, Vol. 65, No. 2, 1973, p. 353–50. [Method described.]CrossRefGoogle Scholar

Physics of Ice

Anderson, D. M., and others. The water–ice phase composition of clay–water systems: I. The kaolinite–water system, [by] D. M. Anderson, A. R. Tice and A. Banin. Soil Science Society of America. Proceedings, Vol. 37, No. 6, 1973, p. 819–22. [After normalization to unit surface area, this system has higher unfrozen water content than any other clay–water system.]CrossRefGoogle Scholar
Bales, B. L., and others. Electron paramagnetic resonance and electron-nuclear double resonance line shape studies of trapped electrons in γ-irradiated deuterium-substituted 10M sodium hydroxide alkaline ice glass, by B. L. Bales, J. Helbert and L. Kevan. Journal of Physical Chemistry, Vol. 78, No. 3, 1974, p. 231–31. [Theoretical and experimental study of effect of deuteration.]CrossRefGoogle Scholar
Bernas, A., and Truong, Thu-Ba. Sur la luminescence stimulée de la glace polycrystalline irradiée par rayons γ.Comptes Rendus Hebdomadaires des Séances de l’Académie des Sciences (Paris), Sér. B, Tom. 277, No. 14, 1973, p. 391–94. [Luminescence of ice after γ-irradiation and optical bleaching attributed not to radicals or ions but to triplet state of water.]Google Scholar
Bilgram, J., and others. Perfection of zone refined ice single crystals, [by] J. Bilgram and H. Wenzl and G. Mair, Journal of Crystal Growth, Vol. 20, No. 4, 1973, p. 319–21. [Method of growing crystals as large as 3 l with dislocation density 103 cm−2.]CrossRefGoogle Scholar
Bosi, P., and others. On the problem of the vibrational spectrum and structure of ice Ih: lattice dynamical calculations, [by] P. Bosi, R. Turbino and G. Zerbi. Journal of Chemical Physics, Vol. 59, No. 9, 1973, p. 4578–86. [Lattice dynamical treatment of ordered ice Ih.]CrossRefGoogle Scholar
Bowman, M., and others. Forbidden matrix proton spin flip satellites in trapped electron EPR spectra, by M. Bowman, L. Kevan, R. N. Schwartz and B. L. Bales. Chemical Physics Letters, Vol. 22, No. 1, 1973, p. 1922. [Study on γ-irradiated frozen solutions of NaOH in H2O and NaOD in D2O.]CrossRefGoogle Scholar
Bychkov, V. Z., and others. Dielektricheskiye svoystva vody v oblasti fazovogo perekhoda zhidkost’–led [Dielectric properties of water in the liquid–ice phase transition region]. [By] V. Z. Rychkov, S. A. Fedulov, N. V. Mikhaylov. Zhurnal Fizicheskoy Khimii, Tom 48, Vyp. 2, 1974, p. 447–48. [Dielectric permittivity and loss tangent measured for ice and water through the phase transition, English translation in Russian Journal of Physical Chemistry, Vol. 48, No. 2, 1974.]Google Scholar
Byers, B. A.Secondary creep of polycrystalline ice under biaxial stress. Dissertation Abstracts International, B, Vol. 34, No. 5, 1973, p. 2101-B. [Experiments on thin-walled cylinders of randomly oriented polycrystalline ice used to confirm proportionality between deviatoric stress and corresponding creep rate at given value of second stress invariant. Abstract of Ph.D. thesis, University of Washington, 1973. University Microfilms order no. 73–27639.]Google Scholar
Cheeke, J. D. N., and others. Kapitza resistance of low acoustic impedance solids (ice and bismuth), by J. D. N. Cheeke, B. Hebral, J. Richard and R. R. Turkington. Physics Letters A. Vol. 46 a, No. 2, 1973, p. 8182. [Thermal resistance between ice and superfluid helium between 1–2 K is in agreement with theory.]CrossRefGoogle Scholar
Chen, M.-S., and others. Hopping of ions in ice, by M.-S. Chen and L. Onsager, J. Bonner and J. Nagle. Journal of Chemical Physics, Vol. 60, No. 2. 1974, p. 405–19. [Theory of proton tunnelling between water molecules in ice developed and compared with experimental mobilities.]CrossRefGoogle Scholar
Cohan, N. V., and Weissmann, M. A quantum electronic polaron model of the hydrated electron, Chemical Physics Letters, Vol. 22, No. 2, 1973, p. 287–90. [Calculation of ground state of hydrated electron in low temperature ice.]CrossRefGoogle Scholar
Crowe, R. W., and Santry, D. P.The polarization and dipole moment of lattice water in hydrogen bonded crystals. Chemical Physics Letters, Vol. 22, No. 1, 1973, p. 5255. [Calculation of dipole moments and charge distributions for H2O molecules in ice Ih and ice Ic.]CrossRefGoogle Scholar
Dabby, S. S.Ice–brine separation in a bed of aggregates of fine ice crystals. Dissertation Abstracts International, B, Vol. 34, No. 7, 1974, p. 3224-B. [Attempt to improve rate of washing in a freezing desalination plant by compacting ice crystals into aggregates. Abstract of Ph.D. thesis, Cornell University, 1973. University Microfilms order no. 73–31797.]Google Scholar
Duval, P.Fluage de la glace polycristalline pour les faibles contraintes. Comptes Rendus Hebdomadaires des Séances de l’Académie des Sciences (Paris), Sér, A, Tom. 277, No. 14, 1973, p. 703–16. [For low stresses, creep of polycrystalline ice depends on grain size, and for small grains transient creep disappears and steady-state creep is proportional to stress.]Google Scholar
Fang, J. K., and others. Role of proton–proton interactions in proton transfer processes in ice and water, [by] J. K. Fang, K. Godzik and G. L. Hofaeker. Berichte der Bunsengesellschaft für Physikalische Chemie, Bd. 77, Nr. 10–11, 1973, p. 980–90. [Dynamics of hydrated proton studied theoretically. Collective proton states deduced and their coupling to local modes discussed. New mechanism for proton mobility in water suggested.]Google Scholar
Fletcher, N. H.Dendritic growth of ice crystals. Journal of Crystal Growth, Vol. 20, No. 4, 1973, p. 268–72. [Theoretical explanation of dendritic branching of ice crystals grown from the vapour from – 10 to – 20° C.]CrossRefGoogle Scholar
Genaoiev, N. P.Reactivation of ice-forming PbI2 particles during heating. Dokludy Bolgarskoy Akodemii Nauk, Tom. 26, No. 8, 1973, p. 1025–27. [Laboratory studies show PbI2 particles are deactivated by heating to 300° C and only partially regenerated by subsequent moistening.]Google Scholar
Goroch, A. K. Astochastic theory of the stepwise growth of ice crystal surfaces. Dissertation Abstracts International, R Vol 34 No. 8, 1974, p. 3975-B. [Theory which predicts the peak in rate of advance of a step as a function of temperature. Abstract of Ph.D. thesis, University of Missouri–Rolla, 1973. University Microfilms order no 74–4347.]Google Scholar
Gosar, P.Note on the Hall effect in ice. Phvsics of Condensed Matter, Vol. 17, No. 3, 1974. p. 183–87. [Theoretical study shows Hall effect should be negligibly small if present picture of conduction processes a correct.]CrossRefGoogle Scholar
Griffiths, R. F., and Latham, J.Electrical corona from ice hvdrometeors. Quarterly Journal of the Royal Meteorological Society, Vol. 100, No. 424, 1974, p. 163–80. [Corona discharge observed from small ice particles provided temperature is above – 18° C. Possible role in thunderstorms discussed.]CrossRefGoogle Scholar
Guo, W. W.-W.Kinetics of ice crystal growth from the vapor. Dissertation Abstracts International, B, Vol. 34, No. 5, 1973, p. 2224-B. [Theoretical solution for growth of a spheroidal ice crystal from the vapour. Abstract of Ph.D. thesis. University of Denver, 1973. University Microfilms order no. 73–28020.]Google Scholar
Hardy, S., and Coriell, S. R.Surface tension and interface kinetics of ice crystals freezing and melting in sodium chloride solutions. Journal of Crystal Growth, Vol. 20, No. 4, 1973, p. 293300 [Measurements on growth and dissolution of cylindrical ice crystals used to deduce these parameters. Surface tension depends on impurity content of the ice.]CrossRefGoogle Scholar
Hasted, J. B.Aqueous dielectrics. London, Chapman and Hall, 1973. xiii, 302 p. (Studies in Chemical Physics.) [Chapters on the dielectric properties of ice, p. 100–16, applications to earth science, p. 256 –86, the latter containing sections on dielectric properties of snow, dielectric properties of naturally occurring ice. radio-echo depth sounding of polar ice.]Google Scholar
Hubmann, M.Formale aspekte eines Modelles von C. Jaccard für die elektrische Eigenschaften von Eis. Helvetica Physica Acta, Vol. 46, Fasc. 4, 1973. p. 421–22. [Experimental results used to deduce parameters in the theory of C. Jaccard, ibid., Vol. 32, Fasc. 2, 1959, p. 89–128.]Google Scholar
Huffman, P. J.Supersaturation dependence of ice nucleation by deposition for silver iodide and natural aerosols. Dissertation Abstracts International, B, Vol. 34, No. 5, 1973, p. 2224-B–25-B. [Laboratory observations. Results indicate this process is likely to be insignificant compared with nucleation via freezing for seeced clouds. Field observations of ice nucleus concentrations. Abstract of Ph.D. thesis, University of Wyoming, 1973. University Microfilms order no. 73–25552.]Google Scholar
Jones, D. R. H.Review: the free energies of solid–liquid interfaces. Journal of Materials Science, Vol. 9, No. 1, 1974, p. 117. [Includes review of work on ice–water and ice–brine interfacial energies.]CrossRefGoogle Scholar
Kroh, J., and Stradowski, C.Radiolvsis of alkaline ice containing additives. (In Dobó, J., and Hedvig, P., ed. Proceedings of the third Tihany Symposium on Radiation Chemistry. Vol. 2. Budapest. Akadémiai kiadó, 1972, p. 1173–80.) [Scavenging of mobile electrons by various negative ions and reactions of trapped electrons with these. Discussion, p. 1179–80.]Google Scholar
Mae, S., and Higashi, A.Effects of plastic deformation on the dielectric properties of ice. Crystal Lattice Dejects, Vol. 4, No, 4, 1973, p. 295308. [Debye dispersion unaffected by plastic deformation; space-charge dispersion has increased permittivity and decreased relaxation time. Explanation in terms of H3Ο+ ions released from dislocation jogs.]Google Scholar
Miloshev, G. N.New effect in freezing small waterdrops. Daklady Bolgarskoy Akademii Nauk, Tom. 26, No. 10, 1973, p. 1335–38. [Study of crystallization when wetting of solid nucleus is incomplete. Work for nucleus formation derived as function of drop radius.]Google Scholar
Nair, N. K., and Chio, H. T.Surface structure of ice at low temperature from adsorption studies. Malaysian Journal of Science, Vol. 1 (b), 1972. p. 163–72. [Adsorption of Ar, N and CO at 77 3 K studied. Data indicate lack of dipole field.]Google Scholar
Parravicini, G. P., and Resca, L.Electronic states and optical properties in cubic ice. Physical Review, B, Third Ser., Vol. 8, No. 6, 1973, p. 3009–23. [Electronic band structure derived for completely polarized ice Ic. Results for energy gap are in agreement with experimental values for cubic ice.]CrossRefGoogle Scholar
Perry, J.W. Complex refractive index of ice fog at a radio wavelength of 3 mm. Dissertation Abstracts Intel national, B, Vol. 34, No. 9, 1974, p. 4381-B. [Laboratory measurements for temperature range −30 to −48° C. Also measurements of complex dielectric permittivity of ice at 97 GHz. Abstract of Ph.D. thesis, University of Texas at Austin, 1973. University Microfilms order no. 74–5310.]Google Scholar
Perry, J. W., and Stariton, A. W.Revision of the dielectric constant of ice in the millimeter wave spectrum. Journal of Applied Physics, Vol. 44, No. 11, 1973, p. 5180. [Correction of values quoted by authors in an earlier paper, ibid., Vol.43, No. 2, 1972, p. 731–33.]10.1063/1.1662118CrossRefGoogle Scholar
Radke, L. F., and Hegg, D.The shattering of saline droplets upon crystallization. Journal de Recherches Atmosphériques, Vol. 6, 1972, p. 447–55. [Experiments on saline aerosols in a diffusion chamber imply existence of this effect. IGoogle Scholar
Ray, P. S.Broadband complex refractive indices of ice and water. Applied Optics, Vol. 11, No. 8, 1972, p. 1836–44. [Review of data over wide range of wavelengths and deduction of empirical model.]CrossRefGoogle Scholar
Rohatgi, P. K., and others. Dendritic structures produced on solidification of multicomponent aqueous solutions, [by] P. K. Rohatgi, E. J. Brush, S. M. Jain, C. M. Adams, Jr. Materials Science and Engineering, Vol. 13, No. 1, 1974, p. 318. [Dendrite structures studied as dependent on solute concentrations, diffusivity and local solidification time.]CrossRefGoogle Scholar
Rosinski, J., and others. Ice nucleation on radioactive and nonradioactive silver iodide particles, by J. Rosinski, G. Langer and C. T. Nagamoto, C. W. Thomas, J. A. Young and N. A. Wogman. Journal of Applied Meteorology, Vol. 12, No. 8, 1973, p. 1303–08. [Particles containing 131I were more efficient nuclei than non-radioactive ones.]2.0.CO;2>CrossRefGoogle Scholar
Rozental’, O. M.Voprosy obrazovaniya l’da v vode i rastvorakh. V. Upravleniye protsessom kristallizatsii s pomoshch’yu dobavok elektolita [Formation of ice in water and solutions. V. Control of crystallization using an electrolyte additive]. Zhurnal Fizicheskoy Khimii, Tom 47, Vyp. 12, 1973, p. 3043–45. [Addition of electrolytes decreases the freezing rate and affects polycrystallinity. English translation in Russian Journal of Physical Chemistry, Vol. 47, No. 12 1973 [pub. 1974].]Google Scholar
Rozental’, O. M.Voprosy obrazovaniya l’da v vode i rastvorakh. VI. Elektricheskiye faktory formirovaniya l’da [Formation of ice in water and solutions. VI. Electrical factors of ice formation]. Zhurnal Fizicheskoy Khimii, Tom 47, Vyp. 12, 1973, p. 3046–49. [Theory of ellipsoid form for ice crystals grown in an electric field. Earth’s field is sufficient to produce effect, but insignificant as regards nucleation. English translation in Russian Journal of Physical Chemistry, Vol. 47, No. 12, 1973 [pub. 1974].]Google Scholar
Ruckenstein, E.Positive and negative nucleation catalysis in crystallization. Journal of Colloid and Interface Science, Vol. 45, No. 1, 1973, p. 115–25. [Initially white light increases nucleating ability of Agi, but longer exposure produces a decrease. Explanation discussed.]CrossRefGoogle Scholar
Schaaf, J. W.The infrared reflectance of ice I. Dissertation Abstracts International, B, Vol. 34, No. 6, 1973, p. 2842-B. [Accurate measurement of absulute normal-incidence reflectance of ice at − 7° C. Abstract of Ph.D. thesis, Kansas State University, 1973. University Microfilms order no. 73–26372.]Google Scholar
Shubin, V. N., and others. Study of spectral and kinetic characteristics of short-lived particles in a solid phase, [by] V. N. Shubin, S. A. Kabakchi, T. E. Pernikova, Yu. I. Sharanin and P. I. Dolin. (In Dobó, J., and Hedvig, P., ed. Proceedings of the third Tihany Symposium on Radiation Chemistry. Vol. 2. Budapest, Akadémiai Kiadó, 1972, p. 1151–61.) [Ice irradiated with 5 MeV electrons and polaron yield and decay studied. Effect of dissolved KOH and of temperature. Discussion, p. 1160–61.]Google Scholar
Stewart, M. K.Hydrogen and oxygen isotope fractionation during crystallization of mirabilite and ice. Geochimica et Casmochimica Acta, Vol. 38, No. 1, 1974, p. 167–72. [Equilibrium fractionation factors between ice and 2.5 molal NaCl solution ai −10° C. Results are of use in assessing mirabilite as a climatic indicator.]CrossRefGoogle Scholar
Suzuki, M., and others. Rēdōmu-jō kōu yuki no jun-miri-ha ni yoru gensui [Studies of the attenuation of quasimiltimetre waves on a rain and snow covered radome]. [By] M. Suzuki, M. Ono [and] Y. Nomura. Seppyō, Vol. 35, No. 4, 1973, p. 192200. [Includes study of how snow accumulated on this dome and how this attenuates radar being transmitted through it. English summary, p. 200.]Google Scholar
Vassoille, R., and others. Comportement anélastique de la glace aux faibles fréquences de sollicitation, [par] R. Vassoille, J. Tatibouet, J. Perez et P.-F. Gobin. Comptes Rendus Hebdomadaires des Séances de l’Académie des Sciences (Paris), Sér. B, Tom. 278, No. 10, 1974, p. 409–12. [Low frequency internal friction measurements on ice give peaks at low temperature which separate molecule reorientation from grain boundary effects.]Google Scholar
Zagórskiy, Z. P., and Gkodkowski, J.Properties of the polycrystalline and glassy alkaline ice in the view of trapped electron mobilization by light. (In Dobó, J., and Hedvig, P., ed. Proceedings of the third Tihany Symposium on Radiation Chemistry. Vol. g. Budapest, Akadémiai Kiadó, 1972, p. 1413–20.) [Ice doped with NaOH used and dependence of effect on dose and on additives studied.]Google Scholar

Land ice. Glaciers. Ice shelves

Aigelsreiter, H., and Neuer, E.Die Pasterze in den Jahren 1963–1970. Zeitschrift für Gletscherkunde and Glazialgeologie, Bd. 8, Ht. 1–2, 1972, p. 303–24. [Year-by-year detailed measurements on Pasterze and neighbouring glaciers (Austria) from 1963 to 1970.]Google Scholar
Ambach, W., Zum Strahlungshaushalt des grönländischen Inlandeises: vergleichende Studie im Akkumulationsund Ablationsgebiet. Polarforschung, Bd. 7, 43. Jahrg., Nr. 1–2, 1973, p. 1022. [Comparative study of radiation fluxes in areas of accumulation and ablation of the Greenland ice cap.]Google Scholar
Ambach, W., and others. Markierungsversuehe am innern Abfluss-system des Hintereisferners (Ötztaler Alpen), von W. Ambach, H. Behrens, H. Bergman und H. Moser. Zeitschrift für Gletscherkunde und Glazialgeologie, Bd. 8, Ht. 1–2, 1972, p. 137–45. [Discharge of melt water from glacier followed by dye method.]Google Scholar
Anderton, P. W.Structural glaciology of a glacier confluence, Kaskawulsh Glacier, Yukon Territory, Canada. Ohio State University. Institute of Polar Studies. Report No. 26, 1973, xii, 109 p. [Study of deformation of surface ice at confluence of north and central arms of glacier with particular reference to relationship between optic-axis fabrics of the ice and deformation.]Google Scholar
Aufdemberge, T. P.Energy balance studies over glacier and tundra surfaces, summer, 1969. Dissertation Abstracts International, B, Vol. 33, No. 5, 1972, p. 2141-B. [Studies on ice surface of glacier and on tundra at similar elevations and exposures showed most marked difference was due to effect of sensible and latent heat fluxes. Abstract of Ph.D. thesis, University of Michigan, 1971. University Microfilms order no. 72–28994.]Google Scholar
Beschel, R. E., and Weidick, A.Geobotanical and geomorphological reconnaissance in west Greenland, 1961. Arctic and Alpine Research, Vol. 5, No. 4, 1973, p. 311–19. [Study of plant succession in areas of recent glacier recession. Results interpreted to determine glacier behaviour where no documentation exists.]CrossRefGoogle Scholar
Bibron, R., and others. Extra-terrestrial 53Mn in Antarctic ice, [by] R. Bibron, R. Chesselet, G. Crozaz, G. Leger, J. P. Mennessier and E. [E.] Picciotto. Earth and Planetary Science Letters, Vol. 21, No. 2, 1974, p. 109–16. [Concludes that bulk of 53Mn found near “Plateau” station is associated with interplanetary dust in which it had been produced by the action of solar protons on iron.]CrossRefGoogle Scholar
Bittmann, O., and others. Die Ergebnisse der seismisclien Gletschermessungen am Obersten Pasterzenboden (Glocknergruppe) im Jahre 1970, von O. Bittmann, E. Brückl, G. Ganzl, F. J. Wallner. Arbeiten aus der Zentralanstalt für Meteorologie und Geodynamik, Ht. 11, 1973, 17 p. (Zeutralanstalt für Meteorologie und Geodynamik in Wien. Publikalion Nr. 201.) [Presents results of seismic refraction measurements of thickness of Pasterze glacier, Austria, 1970.]Google Scholar
Bray, J. R.Glacial advance relative to volcanic activity since 1500 a.d. Nature, Vol. 248, No. 5443, 1974. p. 4243. [Presents evidence suggesting that volcanic eruptions are followed by cold summers and then by glacier advances.]CrossRefGoogle Scholar
Brückl, E.Zusammenhange zwischen topographischen, elastischen und plastischen Grössen von Gletschern. Zeitschrift für Gletscherkunde und Glazialgeologie, Bd. 8, Ht. 1–2, 1972, p. 107–12. [Discusses results of investigation of 13 Austrian glaciers which yielded a statistical confirmation of certain relations between a characteristic parameter representing the flux of glacier ice per width of cross-section, the P-wave velocity of the ice, and the product of surface inclination and hydraulic radius.]Google Scholar
Brunner, K., and Rentsch, H.Die Änderungen von Fläche, Hölie und Volumen am Vernagt- und Guslarferner von 1889–1912-1938–1969. Zeitschrift für Gletscherkunde und Glazialgeologie, Bd. 8, Ht. 1–2, 1972, p. 1125. [Presents 3 maps (in separate map supplement) of this glacier system for 1889–1912, 1912–38 and 1938–69, each representing contour lines of glacier surveys. Changes in vertical shrinkage, volume and area allow individual behaviour of both glaciers to be analysed.]Google Scholar
Budd, W. F.The development of crystal orientation fabrics in moving ice. Zeitschrift fur Gletscherkundc und Glazialgeologie, Bd. 8, Ht. 1–2, 1972, p. 65105. [Examines problem of determining large-scale mean distribution of crystal orientation fabrics throughout ice mass.]Google Scholar
Corner, R. W. M., and SmithR. I, L. R. I, L.Botanical evidence of ice recession in the Argentine Islands. British Antarctic Survey Bulletin, No. 35, 1973, p. 8386. [Evidence of recent ice recession indicated by a band of relatively fresh, light-coloured rock, adjacent to the edge of the existing permanent ice, uncolonized by mosses or lichens.]Google Scholar
Desio, A., and others. Risultati di mezzo secolo di osservazioni sui ghiacciai del gruppo Ortles-Cevedale (Alpi Centrait), [by] A. Desio, S. Belloni, A, Giorcelli [and] G. Zanon. Consiglio Nazionale delle Ricerche. Commissione Incaricata di Coordinate la Partecipazione Italiana al Decennio Idrologico Internationale. Pubblicazione No. 6, 1973, 107 p.+ errata slip. [Results of half a century of investigation on the glaciers of the Ortles-Cevedale mountain group (central Alps); a summary of I ghiacciai del Gruppo Ortles-Cevedale (Alpi Centrali). Torino, Palazzo Carignano, 1967. Text also given in English.]Google Scholar
Dunbak, M.J.Glaciers and nutrients in Arctic fiords. Science, Vol. 182, No. 4110, 1972, p. 398. [Comments upon S, Apollonio’s study (ibid., Vol. 180, No. 4085, 1973, p. 491–93), and suggests that up-welling action of glaciers on water is more likely to affect nitrate concentration in the water than an erosive action.]CrossRefGoogle Scholar
Gangl., G., and others. Verhalten und Eisvolumen der Pasterze (Glocknergruppe) in Beziehung zu den klimatischen Bedingungen, von G. Gangl, G. Skoda und F. J. Wallner. Potarforschung, Bd. 7, 43. Jahrg., Nr. 1–2, 1973, p. 19. [Presents index for the annual ablation of this glacier (Austria) from study of temperature records dating back to 1887, Further retreat seems likely.]Google Scholar
Henriksen, N.Regional mapping and palaeomagnetic and glaciological investigations in the Scoresby Sund region, central east Greenland. Grønlands Geologiske Undersøgelse. Rapport, No. 55, 1973, p. 4247. [Mentions movement and calf ice production of major outlet glaciers.]Google Scholar
Hodge, S. M.The movement and basal sliding of the Nisqually Glacier, Mount Rainier. Dissertation Abstracts International, B, Vol. 33, No. 8, 1973, p. 3725-B. [Observations suggest that seasonal variations in the motion of a glacier are due to variations in the amount of basal sliding which is controlled by the amount of liquid water stored within the glacier. Abstract of Ph.D. thesis, University of Washington, 1972. University Microfilms order no. 73–3735.]Google Scholar
Hoinkes, H. C.Die Ausbrüche (surges) des Kolka-Gletsrhcrs in Nord-Ossetien, Zentraler Kaukasus. Zeitschrift für Gletscherkunde und Glazialgeologie, Bd. 8, Ht. 1–2, 197a, p. 253–70. [Describes 1969, 1902 and earlier surges of Lei link Kolka.]Google Scholar
Hooke, R. L.Flow near the margin of the Barnes Ice Cap, and the development of ice-cored moraines. Geological Society of America. Bulletin, Vol. 84, No. 12, 1973, p. 3929–48. [Observations indicate that clean ice beneath the debris bands is deformed superimposed ice formed at the margin by refreezing of percolating melt water and subsequently overridden during glacier advance.]2.0.CO;2>CrossRefGoogle Scholar
Hughes, T. J.Ice crater closure studies on Deception Island. Antarctic Journal of the United States, Vol. 8, No. 4, 1973, p. 172–75. [Reports 1972–73 studies on ice crater opened in 1970 at snout of glacier.]Google Scholar
Hughes, T. J.Is the west Antarctic ice sheet disintegrating? Journal of Geophysical Research, Vol. 78, No, 33. 1973, p. 7884–910. [Suggests that ice sheet has followed trend towards disintegration experienced by other continental ice sheets towards the end of the Pleistocene, and presents evidence that disintegration is continuing after a temporary advance]CrossRefGoogle Scholar
Hughes, T. J.An unstable tetrahedral mantle-convection model, continental drift, and polar ice sheets. Tectonophysics, Vol. 17, Nos. 1–2, 1973, p. 7388. [Points out value of the Antarctic ice sheet as a natural laboratory where models of mantle convection may be tested.]CrossRefGoogle Scholar
[International Hydrological Decade.] Combined heat, ice and water balances at selected glacier basins. Part II: specifications, standards and data exchange. A contribution to the International Hydrological Decade. [Paris], UNESCO/IASH, [c 1973]. 32 p. (Technical Papers in Hydrology, 5. Pt. II.) [Emphasis is on specification and standards for types, locations and timing of measurements, with particular attention given to heal balances.]Google Scholar
Kasser, P.Fluctuations of glaciers, 1965–1970. A contribution to the International Hydrological Decade. Compiled for the Permanent Service on the Fluctuations of Glaciers of the IUGG–FAGS/ICSU Paris, International Commission on Snow and Ice of the International Association of Hydrological Sciences and UNESCO, 1973. 357 p. + 7 maps. [Continues work of previous reports, with data from polar and non-polar glaciers all over the world.]Google Scholar
Kick, W.Auswerung photographischer Bilder für die Untersuchung und Messung von Gletscheränderungen mit Beispielen aus dem Kaukasus und dem Karakorum. Zeitschrift für Gletscherkunde und Glazialgeologie, Bd. 8, Ht. 1–2, 1972, p. 147–67. [Discusses value of photographs in providing information about glacier variations.]Google Scholar
Koerner, R. M., and others. δ18O profile in ice formed between the equilibrium and firn lines, [by] R. M. Koerner, W. S. B. Paterson, H. R. Krouse. Nature, Physical Science, Vol. 245, No. 148, 1973, p. 137–40. [Discusses problems peculiar to δ18O profiles from accumulation areas where strong melting occurs, and the palaeoclimatic value of these profiles, with reference to the Meighen Ice Cap, Canadian Arctic Archipelago.]CrossRefGoogle Scholar
Koptev, A. P.Zonal’noye raspredeleniye al’bedo podstilayushrhey poverkhnosti vostochnoy Antarktidy [Zonal distribution of the albedo of the underlying surface in eastern Antarctica]. Trudy Sovetskoy Antarkticheskoy Ekspeditsii, Tom 58. 1973, p. 146–60.Google Scholar
Kruchinin, Yu. A. Osnovnyye faktory prirodnoy differentsiatsii shel’fovykh lednikov Antarktidy [Basic factors in distinguishing natural differences in Antarctic ice shelves], Trudy Arkticheskogo i Antarkticheskogo Nauchno-Issledovatel’skogo Institute, Tom 318, 1973, p. 6986. [Attempt to divide Antarctica into natural regions.]Google Scholar
Lyon, G. L.Preliminary stable isotope analysis of drillhole ice at McMurdo station. Antarctic Journal of the United States, Vol. 8, No. 4, 1973, p. 160–62. [Discusses and interprets results. All samples bad low deuterium and 18O contents.]Google Scholar
Mcsaveney, M. J.Folding of cold ice. Antarctic Journal of the United States, Vol. 8, No. 6, 1973, p. 344–46. [Observations from Meserve Glacier, Wright Valley, and suggestions about formation.]Google Scholar
Mcsaveney, M. J.Recession of Meserve Glacier, Wright Valley, between 1966 and 1972. Antarctic Journal of the United States, Vol. 8, No. 6, 1973, p. 346–47. [Reports a probable retreat of 0.55 m.]Google Scholar
Maizels, J. K, Le glacier des Bossons. Quelques aspects caractéristiques de l’environnement proglaciaire. (Discussion sur les différentes façons dont le glacier affecte les températures proglaciaires, et sur le récent développement de la végétation.) Revue de Géographie Alpine, Tom. 61, Fasc. 3, 1973, p. 427–47 [Presents results of study of how the glacier affects the temperature of the proglacial valley and how the soil and vegetation has developed along the margin of the glacier since its last retreat in 1940.]Google Scholar
Miller, H.Ergebnisse von Messungen mit der Methode der Refraktions-Seismik auf dem Vernagt- und Guslarferner. Zeitschrift für Gletscherkunde and Glazialgeologie, Bd. 8, Ht. 1–2, 1972, p. 2741. [Presents results of measurements to determine the volume of ice and the bedrock topography of these two glaciers. Map (in separate map supplement) shows contours and geological nature of the bedrock.]Google Scholar
Oleson, O. B., and Reeh, N.Glaciological observations in the south-western Scoresby Sund region. A preliminary report. Grønlands Geologiske Undersøgelse. Rapport, No. 58, 1973, p. 4954. [Study of glaciers, mainly Vestfjord Gletscher, during organization’s expedition to east Greenland in 1972.]Google Scholar
Orheim, O.A 200 year record of glacier mass balance at Deception Island, southwest Atlantic Ocean, and its bearing on models of global climatic change. Dissertation Abstracts International, B, Vol. 33, No. 4, 1972, p. 1620-B–21-B. [Annual net mass balance variations from 1780 to present day were determined from ice stratigraphy in fissures and cracks after subglacial volcanic eruptions. Results discussed. Abstract of Ph.D. thesis, Ohio State University, 1972. University Microfilms order 110. 7227076.]Google Scholar
Patzeit, G. Gletscherschwankungen in der Venedigergruppe (Hohe Tauern) nach J. A. T. Young, Zeitschrift für Gletscherkunde und Glazialgeologie, Bd. 8, Ht. 1–2, 1972, p. 271–74. [Criticizes paper by Young, Arctic and Alpine Research, Vol. 4, No. 1, 1972, p. 73–83.]Google Scholar
Reinwarth, O.Untersuchungen zum Massenhaushalt des Vernagtferners (Ötztaler Alpen) 1965–1968. Zeitschrift für Gletscherkunde und Glazialgeologie, Bd. 8, Ht. 1–2, 1972, p. 4363. [Discusses principles, measurements and results of mass-balance studies and compares with corresponding values for Hintereis- and Laugtalerferner. Differences explained by different distribution of glacier area with altitude.]Google Scholar
Sanak, J.Pb-210 concentration in ice measured at South Pole station. Antarctic Journal of the United States, Vol. 8, No. 6, 1973, p. 339. [Result different from that of Picciotto (1962), using same method. Probably due to sampling to insufficient depth.]Google Scholar
Shirokov, K. P.Ispol’zovaniye aerometodov dlya vyyavleniya zakonomernostey neustanovivshegosya vetrovogo dreyfa l’da [Use of aerial methods for showing up conformity of unsteady wind drift of ice]. Trudy Gosudarstvennogo Okeanograficheskogo Instituta, Vyp. 117, 1973, p. 91100.Google Scholar
Smith, I. F.Gravity survey on Shoesmith Glacier, Horseshoe Island, Graham Land. British Antarctic Survey Bulletin, Nos. 33–34, 1973, p. 7782. [Intention of survey was to determine the thickness of the ice and the form of the rock ice interface, thereby deciding whether the island is bisected at sea-level as is suggested by its topography. This remains uncertain.]Google Scholar
Sobotovich, E. V., and others. Radiouglerod v lednikovoy vode Priel’brus’ya [Radiocarbon in the glacial water in the Mount Elbrus region]. [By] E. V. Sobotovich, N. N. Kovalyukh, G. N. Bondarenko, Yu. V. Kuznetsov. Geokhimiya, 1973, No. 4, p. 618–21. [CO2 removed from melt water from glaciers and used to provide radiocarbon ages of different glaciers.]Google Scholar
Souchez, R. A., and Lorrain, R. D.Influence de la désorption sur les propriétés chimiques de la glace profonde du glacier d’Argentière (Massif du Mont-Blanc). Comptes Rendus Hebdomadaires des Séances de l’Académie des Sciences (Paris), Sér. D, Tom. 276, No. 13, 1973, p. 1969–71. [Analysis of trace elements from various layers of ice from deep beneath this glacier used to discuss equilibrium of ions between interstitial water and adsorbed layer.]Google Scholar
Stengle, T. R., and others. Sampling of glacial snow for pesticide analysis on the high plateau glacier of Mount Logan, [by] T. R. Stengle, J. J. Lichtenberg, C. S. Houston. Arctic, Vol. 26, No. 4, 1973, p. 335–36. [Describes technique for sampling in hostile conditions.]CrossRefGoogle Scholar
Stupavsky, M., and Gravenor, C. P.Water release from the base of active glaciers. Geological Society of America, Bulletin, Vol. 85, No, 3, 1974, p, 433–36 [Mechanism suggested from laboratory experiments and adds validity to concept of continuous release.]2.0.CO;2>CrossRefGoogle Scholar
Theakstone, W. H., and others. Glacier studies in Nordland, Norway, 1971, [by] W. H. Theakstone, M. Hambrey, N. Τ. Knudsen. Aarhus Universitet. Geologisk Institut, Laboratoriet for Fysisk Geografi. Skrifter i Fysisk Geografi, Nr. 4, 1973, [96] leaves. [Study of Charles Rabots Bre.]Google Scholar
Thompson, L. G.Analysis of the concentration of microparticles in an ice core from Byrd station, Antarctica. Ohio State University. Institute of Polar Studies. Report No. 46, 1973, vii, 44 p. [Study of relationship between microparticle concentration and climate, by comparing concentrations arid size distribution with δ18O values of ice from same depth. Total concentration of microparticles was greatest in samples with largest negative δ18O values.]Google Scholar
Thompson, L. G., and others. Analysis of the concentration of microparticles in the long ice core from Byrd station, [by] L. G. Thompson, W. L, Hamilton, C. B. B. Bull. Antarctic Journal of the United States, Vol. 8, No. 6, 1973, p. 340–41. [Study of relation between microparticle concentrations and climate, by comparing the concentrations and size distributions with δ18O values of ice from the same depths.]Google Scholar
Toporkov, L. G.Ledovyye usloviya v rayone vygruzki trinadtsatoy ekspeditsii [Ice conditions in the areas where the thirteenth expedition landed]. Trudy Sovetskoy Antarkticheskoy Ekspeditsii, Tom 56, 1973, p. 108–12. [Presents results of research on fast ice in the Mirny region, snow patches near “Molodezhnaya”, and snow patches and snow cover of the Lazarev ice shelf.]Google Scholar

Icebergs. Sea, River and Lake Ice

Afanas’yev, V. P.Ice pressure on vertical structures. Translated by V. Poppe. Canada. National Research Council. Technical Translation 1708, 1973, 6 p. [Translated from Transportnoye Stroitel’stuo, [Tom] 3, 1972, p. 47–48.•Suggests method for calculating ice loads due to moving ice fields on single marine hydro-engineering structures with vertical surfaces.]Google Scholar
Allison, I. F.A sample study of the energy fluxes preceding and accompanying the formation of Antarctic sea ice. (In Orvig, S., ed. Energy fluxes over polar surfaces …. Geneva, World Meteorological Organization, 1973, p. 115–32.) [Meteorological measurements made over annual sea ice, open water and new ice enable various terms in the energy balance equation lo be estimated and discussed for short periods representative of the pre-formation and formation of sea ice.]Google Scholar
Antonov, K.Aysbergi Arktiki i Antarktiki [Icebergs of the Arctic and Antarctic]. Morskoy Flot, 1973, No. 10, p. 2336. [Describes paths and limits of icebergs and their danger to shipping.]Google Scholar
Banke, E. G., and Smith., S. D.Wind stress on Arctic sea ice. Journal of Geophysical Research, Vol. 78, No. 33, 1973, p. 7871–83. [Presents results of experiments to determine wind drag coefficients and other boundary layer turbulence characteristics of sea ice in the Arctic Ocean and Robeson Channel, and discusses these and other earlier experiments in the same series.]CrossRefGoogle Scholar
Blüthgen, J.Die Eisarten der Ostsee in ihrer geographischen Bedingtheit. Polarforschung, Bd. 7, 43. Jahrg., Nr. 1–2, 1973, p. 3239. [Describes different types of sea ice occurring in the Baltic Sea and how they come to he formed. Compares with ice of polar seas.]Google Scholar
Bogorodskiy, V. V., and others. Electromagnetic and optic characteristics of sea ice, by V. V. Bogorodskiy, B. Ya. Gaytskhokiy and V. I. Tripolnikov. (In Orvig, S., ed. Energy fluxes over polar surfaces …. Geneva, World Meteorological Organization, 1973, p. 281–99.) [Discusses remote methods of measuring thickness of drifting sea ice and presents a photometric model of ice and snow-ice cover.]Google Scholar
Danecka-Palasz, R., and Kwapuliński, J. Ste{zdot}enie 90Sr w pokrywie lodowej limnicznych zbiorników powierzchniowyeh [Strontium-90 concentration in the ice cover of limnic surface reservoirs]. Acta Geophysica Polonica, Vol. 20, Nr. 3–4, 1972, p. 335–41 - [Results for two locations. English summary, p. 340–41.]Google Scholar
Derycke, R. J.Sea ice motions off Antarctica in the vicinity of the eastern Ross Sea as observed by satellite. Journal of Geophysical Research, Vol. 78, No. 36, 1973, p. 8873–79. [The sea ice displayed a highly variable motion when viewed over short time intervals. The generalized flow suggested a westward movement near shore as an effect of the Antarctic polar current.]CrossRefGoogle Scholar
Dionne, J.-C.How drift ice shapes the St, Lawrence. Canadian Geographical Journal, Vol. 88, No. 2, 1974, p. 49. [Well-illustrated popular account of the geological action of drift ice in this river estuary.]Google Scholar
Donchenko, R. V., ed. Obrazovaniye zatorov i zazhorov l’da na rekakh [The formation of ice jams and ice dams on rivers]. Gosudarstvennyy Ordena Trudovogo Krasnogo Znameni Gidrologicheskiy Institut. Trudy, Vyp. 201, 1973, 140 p. [Six articles with reference to rivers and reservoirs in the U.S.S.R.JGoogle Scholar
Dunbar, Moira. Ice regime and ice transport in Nares Strait. Arctic, Vol. 26, No. 4, 1973, p. 282–91. [Air observations and historical records suggest that date of consolidation of ice in strait is late. Contribution of Canadian channels to heat budget of Arctic Ocean by ice export may be greater than supposed.]CrossRefGoogle Scholar
[Floating Ice: Bearing Strength.] Ice is safe only in a glass. Canadian Mining Journal, Vol. 95, No. 1, 1974, p, 11. [Presents table showing load-carrying capacity of floating ice of various thicknesses for loads ranging from one person on skis to 7–8 ton truck.]Google Scholar
Gaskin., D. E.Icebergs south-east of New Zealand in 1967. (Note.) New Zealand Journal of Marine and Freshwater Research, Vol. 6, No. 3, 1972, p. 387–89. [Sightings of 85 icebergs in February and March are reported, with associated sea surface temperatures.]CrossRefGoogle Scholar
Griffin, O.M. Heat, mass, and momentum transfer during the inching of glacial ice in sea water. Journal of Heat Transfer, Vol. 95, No. 3, 1973, p. 317–23. [Integral methods of solution used for simultaneous calculation of momentum, thermal and mass diffusion boundary layers during steady-state melting of glacial ice in sea-water. Results used to model effects of temperature and salinity on the speed of sound near melting ice in sea-water.]CrossRefGoogle Scholar
Hult, J. L., and Ostrander, N. C.Antarctic icebergs as a global fresh water resource. Santa Monica, California, Rand Corporation, 1973. x, 83 p. (R-1255-NSF.) [Reviews possibility. Appendices on ice accumulation and loss in the Antarctic, controlling iceberg melting, cost, ice transport and models, and flow round a submerged moving body.]Google Scholar
Hult, J. C., and Ostrander, N. C.Applicability of ERTS for surveying Antarctic iceberg resources. Final report for period February–July 1973. Santa Monica, California, Rand Corporation, 1973. x, 50 p. (R-1354-NASA/NSF.) [Assesses potential of satellite observation.]Google Scholar
[International Hyokological Decade.] Guide to world inventory of sea, take and river ice. A contribution to the International Hydrological Decade. Paris, UNESCO/IAHS, 1972. 23 p. (Technical Papers in Hydrology, 9.) [Methods for standardization of data collection presented.]Google Scholar
Kan, T. K., and others. Sonar mapping of the underside of pack ice, [by] T. K. Kan, C. S. Clay and J. M. Berkson. Journal of Geophysical Research, Vol. 79, No. 3, 1974, p. 483–88. [Presents results of study of sea ice morphology. Estimates keel depth of ridges, and compares top and bottom features. Average ratio of peak top elevation to keel depth was 1: 7.6.]CrossRefGoogle Scholar
Keys, J. E.Data reduction system for 16 mm film records. Ottawa. Defence Research Board of Canada. Defence Research Establishment Ottawa, 1973. [iv], 6 p. (DREO Technical Note No. 73–14.) [A system for digitizing water current and ice floe position data recorded on 16 mm film was assembled from commercially available components. The system and its operation are described.]Google Scholar
Kiselev, Yu. G.Izucheniye sezonnykh izmeneniy uprugikh svoystv ledovogo pokrova v Arktike [Study of seasonal changes in elastic properties of the Arctic pack ice]. Geofizicheskiye Metody Razvedki v Arktike. Vyp. 6, 1971, p. 7982.Google Scholar
Kupetskiy, V. N.O biologicheskikh pokazatelyakh morskikh polyarnykh landshaftov [Biological factors of polar landscapes]. Trudy Arkticheskogo i Antarkticheskogo Nauchno-Issledovatel’skogo Institute, Tom 318, 1973, p. 4552. [Forecasts of future state of water and ice movements in Arctic seas can be based on a study of the movements of animals.]Google Scholar
Langleben, M. P.Albedo of ice-infested waters in the channels of the Canadian Archipelago. (In Orvig, S., ed. Energy fluxes over polar surfaces …. Geneva, World Meteorological Organization, 1973, p. 134–42.) [Study indicates that estimates of albedo of ice cover can be made on a synoptic scale from aircraft.]Google Scholar
Legen’Kov, A. P, “Mayny”, ikh sledy na molodykh l’dakh i konvektsiya [“Mayny”, signs of them on young ice and convection]. Okeanologiya, 1973, No. 5, p. 798800. [Study in Arctic seas of oval openings in ice (polynyas) and how they are formed.]Google Scholar
Legen’Kov, A. P.Termicheskiye naprazheniya i deformatsii ledyanogo ostrova deyfuyushchey stantsii “Severnyy polyus-19)” [Thermal stresses and deformations of the ice island SP-19]. Okeanologiya, 1973, No. 6, p. 975–80. [Calculations based on ice temperature and salinity data.]Google Scholar
Leont’yev, Ye. B. Ledovyye usloviya plavaniya d/e “Ob’” v Antarkticheskikh vodakh letom 1967/68 [Ice conditions during the voyage of the Ob’ in Antarctic waters in summer 1967–68]. Trudy Sovetskoy Antarkticheskoy Ekspeditsii, Tom 56, 1973, p. 103–07.Google Scholar
Mayer, W. G.Determination of transverse wave velocity in transition layer of sea ice from reflection of water-borne sound. Journal of Geophysical Research, Vol. 79, No. 6, 1974, p. 885–86. [Re-evaluation of M. P. Langleben’s data (ibid., Vol. 75, No. 27, 1970, p. 5243–46). Reply by Langleben, p. 886.]CrossRefGoogle Scholar
Milano, V. R.Ship resistance to continuous motion in ice. Dissertation Abstracts International. B, Vol. 33, No. 6, 1972, p. 2567-B–68-B. [Presents mathematical model which predicts the total energy lost by a given ship in moving a fixed distance through ice of known thickness. Compares well with field lests. Abstract of Ph.D. thesis, Stevens Institute of Technology, 1972. University Microfilms order no. 72–31170.]Google Scholar
Milne, A. R.Wind noise under winter ice fields. Journal of Geophysical Research, Vol. 79, No. 6, 1974, p. 803–09. [Explains mechanism of noise production.]CrossRefGoogle Scholar
Palmer, W. T.On the analysis of floating ice plates. Dissertation Abstracts International, B, Vol. 33, No. 6, 1972, p. 2637-B. [Discusses deformation of an ice plate floating on a liquid and the effect of vertical variation in its material properties. Effect of loads also discussed. Abstract of Ph.D. thesis, New York University, 1971. University Microfilms order no. 72–21787.]Google Scholar
Pounder, E. R., and others. Ice movement in the Gulf of St. Lawrence, by E. R. Pounder, O. M. Johannessen and B. D. Wright. (In Orvig, S., ed. Energy fluxes over polar surfaces …. Geneva, World Meteorological Organization, 1973, p. 249–80.) [Study of relations between wind and current fields and ice movement, resulting in deformational processes in the ice.]Google Scholar
Rango, A., and others. Observations of Arctic sea ice dynamics using the Earth Resources Technology Satellite (ERTS-1), [by] A. Rango, J. R. Greaves, R. J. DeRycke. Arctic, Vol. 26, No. 4, 1973, p. 337–39- [Demonstrates that ERTS-1 can be used to make synoptic observations of dynamic changes in Arctic sea ice and also to locate areas of sea ice that are melting and therefore likely to break up early.]CrossRefGoogle Scholar
Sager, G.Treib- und Packeis der polaren Meere. Seewirtschaft, Vol. 6, No. 1, 1974, p. 5155. [Discusses factors affecting formation of floating ice, mass balance of ice in polar seas, and ice and navigation in Arctic waters, referring to particular areas.]Google Scholar
Sergeyev, G. N.O prichine obrazovaniya vnutrivodnogo I’da u beregov Antarktidv [On a cause of underwater ice formation along Antarctic coasts]. Trudy Sovetskoy Antarkticheskoy Ekspeditsii, Tom 58, 1973, p. 161–66. [Theory that fresh water from beneath ice sheet mixes with colder salt ocean water to cause underwater ice formation.]Google Scholar
Shpaykher, A. O.Aysbergi Severnoy Atlantiki kak pokazatel’ krupnomasshtabnykh gidrometeorologicheskikh protsessov [North Atlantic icebergs as an index of large-scale hydrometeorological processes]. Trudy Arkticheskogo i Antarkticheskogo Nauchno-Issledovatel’skogo Instituta, Tom 318, 1973, p. 5368. [Icebergs studied off the coasts of Greenland and Newfoundland.]Google Scholar
Smirnov, V. N.Kolebaniya ledyanogo pokrova, obuslovlennyye vnutrennimi volnami ledovitogo okeana [Fluctuations of the ice sheet as a result of waves within the Arctic Ocean]. Doklady Akademii Nauk SSSR, Tom 206, No. 5, 1972, p. 1106–08.Google Scholar
Sovershayev, V. A.Ledovaya obstanovka na reyde Mirnogo v 1969/70 g. [Ice conditions in Mirny shipping lanes in 1969–70.] Trudy Sovetskoy Antarkticheskoy Ekspeditsii, Tom 58, 1973, p. 167–73.Google Scholar
Thompson, T., and Udin, I.Isen i Östersjön; rutinistjänst och forskning. Ymer, Årg, 93, 1973, p. 6082. [Describes activities of the Swedish ice reporting and forecasting service for the Baltic Sea.]Google Scholar
Tōkairin, A. Hoshajō moyō hyōmen no seisei kikō, I [Study on the radial pattern of an ice surface, I]. Seppyō, Vol. 35, No. 4, 1973, p. 173–79. [Pattern on lake ice due to channel of warm water gushing through accumulation of snow on lake surface. English summary, p. 179.]Google Scholar
Votintsev, K. K., and Grigor’yeva, E. N. K kharakteristike khimicheskogo sostava l’da i podlednoy vody ozer severnogo Kazakhstana [Characteristics of the chemical composition of ice and subglacial water of northern Kazakhstan lakes]. Doklady Akademii Nauk SSSR, Tom 211, No. 6, 1973, p. 1405–07.Google Scholar
Werner, J.Untersuchungen zur Wechselwirkung zwischen Windprofil und Meereisdecke in der kanadischen Arktis bei Pond Inlet, N.W.T. Polarforschung, Bd. 7, 43. Jahrg., Nr. 1–2, 1973, p. 2331. [Presents results of the interaction between wind profile and sea ice surface; roughness parameters are relatively small for undisturbed and snow-covered ice surfaces.]Google Scholar
Wolford, T. C. Iceberg drift. Dissertation Abstracts International, B, Vol. 33, No. 3, 1972, p. 1213-B. [Mathematical models developed. Abstract of Ph.D. thesis, Catholic University of America, 1972. University Microfilms order no. 72–23549.]Google Scholar

Glacial. Geology

Aartolahti, T.Morphology, vegetation and development of Rokuanvaara, an esker and dune complex in Finland. Fennia, 127, 1973, 53 p. [Includes description of glacial relief of area.]Google Scholar
Andrews, J. T., and others. Holocene late glacial maximum and marine transgression in the eastern Canadian Arctic, [by] J. T. Andrews, A. Mears, G. H. Miller, D. R. Pheasant. Nature, Physical Science, Vol. 239, No. 96, 1972, p. 147–49. [Presents new data on age of major glacial readvance and marine transgression, and compares age of this and other major strandlines from northern Europe and the European Arctic.]CrossRefGoogle Scholar
Andrews, J. T., and others. Holocene sea level changes, Cumberland coast, northwest England: eustatic and glacio-isostatic movements, [by] J. T. Andrews, C. A. M. King and M. Stuiver. Geologie en Mijnbouw, Vol. 52, No. 1, 1973, p. 112. [Presents evidence for relative.sea-level movements along coast for period 9000 b.p. to present, and uses data to evaluate local glacio-isostatic recovery of region and world-wide eustatic sea-level changes.]Google Scholar
Beschel, R. E.Lichens as a measure of the age of recent moraines. Arctic and Alpine Research, Vol. 5, No. 4, 1973, p. 303–09. [Translation by W. Barr from Zeitschrift für Gletscherkunde und Glazialgeologie, Bd. 1, Ht. I, 1950, p. 152–61.]CrossRefGoogle Scholar
Binns, P. E., and others. Glacial and postglacial sedimentation in the Sea of the Hebrides, [by] P. E. Bums, R. Harland, M. J. Hughes. Nature, Vol. 248, No. 5451, 1974, p. 751–54. [Presents conclusions drawn from preliminary results of coring and drilling off the west coast of Scotland.]CrossRefGoogle Scholar
Bodéré, J.-C., and Guilcher, A.Extension de l’influence du glacier Vatna sur la formation des flèches littorales de la côte sud-est et est de l’Islande. Comptes Rendus Hebdomadaires des Séances de l’Académie des Sciences (Paris), Sér. D, Tom. 278, No. 14, 1974, p. 1805–07. [Discusses dependence of formation of spits along the south-east and east coasts of Iceland on the moraines and fluvio-glacial material from Vatnajökull.]Google Scholar
Bristow, G. R., and Cox, F. C., The Gipping Till: a reappraisal of East Anglian glacial stratigraphy. Journal of the Geological Society (London), Vol. 129, Pt. 1, 1973, p. 138. [Examines evidence for existence of this till and its associated glaciation.]Google Scholar
Brochu, M.La possibile presenza di ghiacci galleggianti nel Mediterraneo durante le glaciazioni Quaternarie e il loro ruolo geologico. Il Polo, An. 29, No. 4, 1973, p. 8488. [Discusses the possibility that floating ice occurred in the Mediterranean during the Quaternary, and that it transported sediments, later deposited on the sea floor.]Google Scholar
Büdel, J.Geomorphologische Polarforschung in Spitzbergen. Kurzbericht der Ergebnisse der Stauferland-Expedition 1959–1967. Zeitschrift für Gletscherkunde und Glazialgeologie, Bd. 8, Ht. 1–2, 1972, p. 283–94. [Discusses recent geomorphological work in Svalbard, particularly that of the Stauferland Expedition to Barentsøya, Edgeøya and Kong Karls Land. Extended English summary, p. 290–94.]Google Scholar
Carrara, P. E., and Andrews, J. T.Problems and application of lichenometry to geomorphic studies, San Juan Mountains, Colorado. Arctic and Alpine Research, Vol. 5, No. 4, 1973, p. 373–84. [Investigations of talus, protalus ramparts, rock glaciers and end moraines.]CrossRefGoogle Scholar
Carver, G. A.Glacial geology of the mountain lakes wilderness and adjacent parts of the Cascade Range, Oregon. Dissertation Abstracts international, B, Vol. 33, No. 12, Pt. 1, 1973, p. 5911-B. [Various deposits identified and differentiated. Abstract of Ph.D. thesis, University of Washington, 1972. University Micro films order no. 73–13803.]Google Scholar
Chapman, W. F.Glacial history of the northern part of the Hoback River basin, west-central Wyoming. Dissertation Abstracts International, B, Vol. 33, No. 5, 1972, p. 2150-B–51-B. [Discusses implications of examination of glacial deposits. Abstract of Ph.D. thesis, University of Michigan, 1972. University Microfilms order no, 72–29016.]Google Scholar
Charlesworth, J. K.Stages in the dissolution of the last ice-sheet in Ireland and the Irish Sea region. Proceedings of the Royal Irish Academy, Sect. B, Vol. 73, No. 5, 1973, p. 7986. [Reviews and assesses recent papers on extent and dissolution of Quaternary ice sheet.]Google Scholar
Danilov, I. D.Plastic and ruptural deformations in basin sediments. Biuletyn Peryglacjalny, No. 22, 1973, p. 329–37. [Studies of marine and lacustrine Pleistocene deposits in northern West Siberia and Pechora lowlands show that deformations are common and of several types, and are unrelated to permafrost pro cesses.]Google Scholar
Danilov, I. D.Subaqueous pseudomorphoses in Pleistocene deposits. Biuletyn Peryglacjalny, No. 23, 1973, p. 339–45. [Describes wedge-shaped formations, probably due to melting of ice veins and subsequent filling in of resulting spaces with mineral or peat substratum. May occur in several stages depending on climatic conditions.]Google Scholar
Denis, R.Late Quaternary geology and geomorphology in the Lake Maskinongé area, Québec. Uppsala Universitet. Naturgeografiska Institutionen. Rapport 28, 1974, 125 p. + 2 p. errata. [From a systematic analysis of data, the sequence of Quaternary events in this region may be reconstructed.]Google Scholar
Dilamarter, R. R. Areal variations of selected topographic variables on glacial drift sheets of different ages in Iowa, Dissertation Abstracts International, B, Vol. 33, No. 7, 1973, p. 3131-B–32-B. [Abstract of Ph.D. thesis, University of Iowa, 1972, University Microfilms order no. 73–614.]Google Scholar
Drake, L. D.Till fabric control by clast shape. Geological Society of America. Bulletin, Vol. 85, No. 2, 1974, p. 247–50. [Presents field data showing that pebble shape exerts a strong influence on its orientation in till.]2.0.CO;2>CrossRefGoogle Scholar
Fedorov, B. A.Podlednyy antarkticheskiy rel’yef v rayone stantsii Molodezhnoy [Subglacial Antarctic relief in the region of “Molodezhnaya” station]. Trudy Sovetskoy Antarkticheskoy Ekspeditsii, Tom 56, 1973, p. 121–24.Google Scholar
Flint, R. F.Present knowledge of late Cenozoic glaciation. Biuletyn Peryglacjalny, No. 23, 1973, p. 6770. [Brief review.]Google Scholar
Fliri, F., and others. Weitere Ergebnissc der Forschung am Bänderton von Baumkirchen (Inntal, Nordtirol), von F. Fliri, H. Felber und H. Hilscher. Zeitschrift für Gletscherkunde und Glazialgeologie, Bd. 8, Ht. 1–2, 1972, p. 203–13. [From investigations of laminated silts and clays it is possible to make some suggestions about the Würmian glaciation of the Inn valley.]Google Scholar
Foyer, M. B.Lichenometrical photography in the Kebnekaise mountains, Swedish Lapland. Arctic and Alpine Research, Vol. 5, No. 4, 1973, p. 321–22. [Describes how the growth rate is being established of lichens used in investigating absolute and relative chronologies of moraines.]CrossRefGoogle Scholar
Gangloff, P.Le milieu morphoclimatique tardiglaciaire dans la région de Montréal. Cahiers de Géographie de Québec, Vol. 17, No. 42, 1973, p. 415–48. [Presents results of study of glacial geology of region and discusses climatic implications.]CrossRefGoogle Scholar
Gemmell, A. M. D.The déglaciation of the island of Arran, Scotland. Institute of British Geographers. Transactions, No. 59, 1973, p. 2539. [Discusses sequence of events from major readvance of about 13500 b.p. until end of glacial period.]CrossRefGoogle Scholar
Gwyn, Q. H.The heavy mineral assemblages in tills and their use in distinguishing glacial lobes in the Great Lakes region. Dissertation Abstracts International, B, Vol. 33, No. 2, 1972, p. 785–8. [Possible to distinguish Huron, Georgian Bay and Ontario-Erie glacial lobes. Abstract of Ph.D. thesis, University of Western Ontario, 1971. Microfilm order from National Library of Canada, Ottawa.]Google Scholar
Hastenrath, S.Pleistocene snow line depression and atmospheric circulation in the New World tropics. (Summary.) Arctic and Alpine Research, Vol. 5, No. 3, Pt. 2, 1973, p. A181-A182. [Summarizes author’s field results, published previously between 1963 and 1971.]Google Scholar
Heuberger, H.Die Salzburger “Friedhofterrasse”—eine Schlernterrasse? Zeitschrift für Gletscherkunde und Glazialgeologie, Bd. 8, Ht. 1–2, 1972, p. 237–51. [Casts doubt on the suggestion that this gravel terrace is connected with moraines of local valley glaciers.]Google Scholar
Jochimsen, M.Does the size of lichen thalli really constitute a valid measure for dating glacial deposits? Arctic and Alpine Research, Vol. 5, No. 4, 1973, p. 417–24. [Critical discussion of Bechsel’s theory of lichenometry.]CrossRefGoogle Scholar
Kane, J., and others. Alpine glacial features of Mars, [by] J. Kane, J. Kasold, M. Suda, P. Metcalf, S. Caccamo. Nature, Vol. 244, No. 5410, 1973, p. 2021. [Describes and discusses features caused by glacial erosion.]CrossRefGoogle Scholar
Kazi, A., and Knill, J.Fissuring in glacial lake clays and tills on the Norfolk coast, United Kingdom. Engineering Geology, Vol. 7, No. 1, 1973, p. 3548. [Describes orientation and origin. Attitudes of fissures are geometrically related to stress conditions associated with glacial loading acid subsequent removal of overburden.]CrossRefGoogle Scholar
Krall, D. B.Till stratigraphy and Olean ice retreat in east-central New York. Dissertation Abstracts International, B, Vol. 33, No. 4, 1972, p. 1619-B. [Study of tills, moraines and drumlin morphology enables Quaternary deglaciation to be followed. Abstract of Ph.D. thesis, Rutgers University, 1972. University Microfilms order no. 72–27566.]Google Scholar
Kraus, E. B.Comparison between ice age and present general circulations. Nature, Vol. 245, No. 5421, 1973, p. 129–33. [Argues against assumption that ice ages were characterized by a more vigorous atmospheric circulation and by an increased meridional heat transport.]CrossRefGoogle Scholar
Lamarche, R. Y.Southeastward, northward, and westward ice movement in the Asbestos area of southern Quebec. Geological Society of America. Bulletin, Vol. 85, No. 3, 1974, p. 465–70. [Evidence of three major ice movements based on crag-and-tail striations.]2.0.CO;2>CrossRefGoogle Scholar
Lindsay, D. C.Estimates of lichen growth rates in the maritime Antarctic. Arctic and Alpine Research, Vol. 5, No. 4, 1973, p. 341–46. [Using growth rates estimated from lichens growing on introduced (dated) features on Signy Island, South Orkney Islands, the two most recent moraines of Orwell Glacier were dated. Growth rate of Rhizocarpon geographicum on this island is estimated to be about 16 mm in diameter per century.]Google Scholar
Lundqvist, J.Isavsmältningens förlopp i Jämtlands län. Sveriges Geologiska Undersökning. Avhandlingar och Uppsatser, Ser. C, Nr. 681, Årsbok 66, Nr, 12, 1973, 187 p. [Follows progress of deglaciation in county of Jämtland, central Sweden, based on study of moraines, glacio-fluvial formations and ice-dammed lakes. English summary, p. 170–84.]Google Scholar
Lyons, J. B., and Mielke, J. E.Holocene history of a portion of northernmost Ellesmere Island. Arctic, Vol. 26, No. 4, 1973, p. 314–23. [Presents new radiocarbon dates, relates these to post-glacial emergence and to growth of the Ward Hunt Ice Shelf and contiguous ice rises, and estimates thickness of Pleistocene ice.]Google Scholar
Mcelhinny, M. W., and others. Palaeomagnetic results and late Precambrian glaciations, [by] M. W. McElhinny, J. W. Giddings and B. J. J. Embleton. Nature, Vol. 248, No. 5449, 1974, p. 557–61. [Combined late Precambrien to early Palaeozoic polar wander path is derived for Gondwanaland, which suggests the latter existed at least 750 Ma ago. Widespread distribution of late Precambrian glaciations can be explained in terms of this polar migration.]CrossRefGoogle Scholar
Mahaney, W.Neoglacial chronology in the Fourth of July cirque, central Colorado Front Range. Geological Society of America. Bulletin, Vol. 84, No. 1, 1973, p. 161–70. [Lichenometrical, pedological and geological evidence used to establish chronology.]2.0.CO;2>CrossRefGoogle Scholar
Mahaney, W.Neoglacial chronology of the Fourth of July cirque, central Colorado Front Range: reply. Geological Society of America. Bulletin, Vol. 84, No. 11, 1973, p. 3767–72. [Comments upon J. Williams’s suggestions (ibid., p. 3761–65).]2.0.CO;2>CrossRefGoogle Scholar
Miller, C. D.Chronology of Neoglacial deposits in the northern Sawatch Range, Colorado. Arctic and Alpine Research, Vol. 5, No. 4, 1973, p. 385400. [Establishment of chronology of nick glacier development from lichenometry and geological evidence.]CrossRefGoogle Scholar
Millek, G. H.Variations in lichen growth from direct measurements: preliminary curves for Alectoria minuscula from eastern Baffin Island, N.W.T., Canada. Arctic and Alpine Research, Vol. 5, No. 4, 1973, p. 333–39. [Comments upon technique for dating Neoglacial moraine sequence.]Google Scholar
Mills, H. C., and Wells, P. D.Ice-shove deformation and glacial stratigraphy of Port Washington, Long Island. New York. Geological Society of America. Bulletin, Vol. 85, No. 3, 1974, p. 357–64. [Late Wisconsin ice advance caused thrust faulting and’ folding of Cretaceous and glacial strata. Further effects discussed.]2.0.CO;2>CrossRefGoogle Scholar
Molnia, B. F.Pleistocene ice rafting in the North Atlantic Ocean. Dissertation Abstracts International, B, Vol. 34, No. 1, 1973, p. 278-B. [Presents results of examination of age and nature of sediment samples, and discusses implications of these findings. Abstract of Ph.D. thesis, University of South Carolina, 1972. University Microfilms order no. 73–16313.]Google Scholar
Morgan, A. V.The Pleistocene geology of the area north and west of Wolverhampton, Staffordshire, England. Philosophical Transactions op the Royal Society of London, Ser. B, Vol. 265, No. 868, 1973, p. 233–97. [Detailed study of tills and deposits enables conclusions to be made about extent and dating of last glaciation of this area. Ice wedge casts and polygons indicate periglacial conditions which lasted until about 12500 b.p.]Google Scholar
Nikleb, L.Nov prilog poznavanju oledbe (Ein neuer Beitrag zur Kenntnis der Vereisung im Velebit Gebirge). Ceološki Vjesnik (Zagreb), Svezak 25 (Godište 1971), 1973, p. 109–12. [Comments upon the Pleistocene glaciation of the Velebit mountains, Yugoslavia. German summary, p. 112.]Google Scholar
Orengo, C.Glaciaire et tardiglaciaire des vallées de la Mirière, des Merveilles et de Fontanalbe (Alpes maritimes). Revue de Géographie Alpine, Tom. 61, Fasc. 4, 1973, p. 583–99. [Describes and interprets glacial morphology of these valleys.]CrossRefGoogle Scholar
Piper., J. D. A.Latitudinal extent of late Precambrian glaciations. Nature, Vol. 244, No. 5415, 1973, p. 342–44. [Comments upon extent at low latitudes.]CrossRefGoogle Scholar
Saunders, G. E, Vistulian periglacial environments in the Lleyn Peninsula. Biuletyn Peryglacjalny, No. 22, 1973, p. 357–69. [Climatic significance of periglacial phenomena in north-west Wales is considered in an attempt to assess the nature of the environments in which they were formed.]Google Scholar
Schnitker, D.Postglacial emergence of the Gulf of Maine. Geological Society of America. Bulletin, Vol. 85, No. 3, 1974, p. 491–94. [Summarizes evidence for a post-glacial strand of sea-level lower than at present and attempts to relate eustatic post-glacial sea-level rise with isostatic crustal movements.]2.0.CO;2>CrossRefGoogle Scholar
Schubert, C.Geomorphology and glacier retreat in the Pico Bolivar area, Sierra Nevada de Merida, Venezuela. Zeitschrift für Gletscherknnde und Glazidgeologie, Bd. 8, Ht. 1–2, 1972, p. 189202. [Describes glacial morphology of area. Maps, photographs and observations made between 1910 and 1972 suggest a rapid glacier retreat, reducing the ice-covered area by as much as 80%.]Google Scholar
Shcmerbakova, Ye. M. Drevneye oledeneniye Bol’shogo Kavkaza [Ancient glaciation of the Caucasus mountains], Moscow, Izdatel’stvo Moskovskogo Universiteta, 1973. 271 p. [Describes glacial geology of region.]Google Scholar
Shpolanskaya, N. A., and Yevseyev, V. P.Domed-hummocky peatbogs of the northern taiga in western Siberia. Biuletyn Peryglacjalny, No. 22, 1973, p. 271–83. [Field observations suggest these are relict formations of the late Holocene, developed as a result of water migration towards freezing soils and now degrading by the thawing from below of the frozen cores.]Google Scholar
Ten Brink, N. W.Glacio-isostasy: new data from west Greenland and geophysical implications. Geological Society of America. Bulletin, Vol. 85, No. 2, 1974, p. 219–28. [Examines process of post-glacial uplift as recorded by emerged marine features.]2.0.CO;2>CrossRefGoogle Scholar
[Till.] [Uppsala symposium on till and till stratigraphy, 1972.] Bulletin of the Geological Institutions of the University of Uppsala, New Ser., Vol. 5, 1973, 215 p. [Contains the following papers: L.-K. Kömgsson, “The Uppsala symposium on till and till stratigraphy”, p. 5; I. Th. Rosenqvist, “Sub-moraine deposits in Numedal”, p. 712; E. Roaldset, “Sub-till sediments in the Numedal valley, southern Norway”, p. 13–17; J. Lundqvist, “Dark bluish boulder-clay: a possible deposit from the first Würm glaciation”, p. 19–20; A. Berthelsen, “Weichselian ice advances and drift successions in Denmark”, p. 21–29; S. Sjørring, “Some problems in the till stratigraphy of the northeastern part of Sjaelland”, p. 31–35; L. A. Rasmussen, “The Quaternary stratigraphy and dislocations on Ven”, p. 37–39; K. S. Petersen, “Tills in dislocated drill deposits on the Røsnæs peninsula, northwestern Sjælland, Denmark”, p. 41–49: B. B. Broms, “The geotechnical aspects of moraine, p. 51–60; J. Hartlén, “The geotechnical characteristics of moraine clays related to their structure”, p. 61–68; O. Fr. Bergersen, “The roundness analysis of stones. A neglected aid in till studies”, p. 69–79; K. Garnes, “Till studies in the Gudbrandsdal area, eastern central Norway”, p. 81–92; H. Balmson, “Lithological investigations in some Danish boulder-clay profiles”, p. 93–109: K. Binzer, “Trace elements in Danish tills p. 111–15; J. Krüger, “Operator variance in orientation measurements in till macrofabric analyses. An experimental study”, p. 117–25; U. Thoregren, “A seismic refraction study of a complex accumulation in Ängersjö, southern Västerbotten”, p. 127–29; H. G. Johansson, “The genesis of the complex accumulation in Ängersjö. southern Västerbotten”, p. 131; H. Minell, “An investigation of drumlins in the Narvik area of Norway”, p. 133–38; Å. Hillefors, “The stratigraphy and genesis of stoss- and lee-side moraines”, p. 139–54• K Moreborg, “Limestone determinations of till in the Gävle region”, p. 155; K. Eriksson, “The distribution of some metals in different till fractions”, p. 157–64; N. Spjeldnæs, “Moraine stratigraphy, with examples from the basal Cambrian (‘Eocambrian’) and Ordovician glaciations”, p. 165–71; P. B. K-onradi, “Foraminiferas in some Danish glacial deposits”, p. 173–75; I. Marcussen, “Stones in Danish tills as a stratigraphical tool. A review”, p. 177–81; M. Markgren, “Problems of moraine stratigraphy”, p. 183–97; N.-A. Mörner, “Till stratigraphy in North America and northern Europe”, p. 199–207; E. Mohrén, “The drift beds of western Skåne in southern Sweden”, p. 209–15.]Google Scholar
Unwin, D. J.The distribution and orientation of curries in northern Snowdonia, Wales. Institute of British Geographers. Transactions, No. 58, 1973, p. 8597. [Analyses and describes significant regularities in attempt to identify factors controlling mountain glaciation.]CrossRefGoogle Scholar
Veyret, Y.Note préliminaire à l’étude morphologique des marges du glacier de l’Artense (Massif Central). Revue de Géographie Alpine, Tom. 61, Fasc. 2, 1973, p. 203–21. [Many glacio-fluvial formations were noted, but a sequence of events leading to their development was difficult to define.]CrossRefGoogle Scholar
Vorren, T. O.Glacial geology of the area between Jostedalsbreen and Jotunheimen, south Norway. Norges Geologiske Undersøkelse, Nr. 291, Bulletin 16, 1973, 46 p. [Reconstructs ice movement and course of deglaciation.]Google Scholar
Waitt, R. B., jr. Geomorphology and glacial geology of the Methow drainage basin, eastern North Cascade Range, Washington. Dissertation Abstracts International, B. Vol. 33, No. 12, Pt. 1, 1973, p. 5920-B–21-B. [Conclusions about the glaciation of this region are drawn from a study of the features. Abstract of Ph.D. thesis, University of Washington, 1972. University Microfilms order no. 73–13896.]Google Scholar
Webber, P. J., and Andrews, J. T.Lichenometry: a commentary. Arctic and Alpine Research, Vol. 5, No. 4, 1973, p. 295302. [Describes technique and applications, mainly to glacial geology.]CrossRefGoogle Scholar
Weymarn, J. von and Edwards, K. J.Interstadial site on the island of Lewis, Scotland. Nature, Vol. 246, No. 5434, 1973, p. 473–74. [Thin layer of organic detritus found beneath glacial till was radiocarbon dated to 27333 ± 2.40 b.p. Pollen analysis indicates a temperate climate.]CrossRefGoogle Scholar
Williams, J.Neoglacial chronology of the Fourth of July cirque, central Colorado Front Range: discussion. Geological Society of America. Bulletin, Vol. 84, No. 11, 1973, p. 3761–65. [Presents alternative interpretation and chronology to that of Mahaney (ibid., Vol. 84, No. 1, 1973, p. 161–70).]2.0.CO;2>CrossRefGoogle Scholar

Frost Action on Rocks and Soil. Frozen Ground. Permafrost

Alekseyev, M. N., and others. Sur les formations périglaciaires du Pléistocène dans la partie Nord de l’Asie Orientale, [by] M. N. Alekseyev, R. Ye. Giterman, L. V. Golubeva. Biuletyn Peryglacjalny, No. 23, 1973, p. 3750. [Outlines periglacial features of north-eastern U.S.S.R.]Google Scholar
Alter, A. J.Water supply and waste disposal concepts applicable in permafrost regions. Permafrost. Second International Conference. … 1973, 1973. p. 577–81. [General discussion of problems.]Google Scholar
Alvarez, R.Permafrost: relation between ice content and dielectric losses at 100° K. Earth and Planetary Science Letters, Vol. 20, No. 3, 1973, p. 409–14. [Results show feasibility of determining ice content in permafrost by electromagnetic means.]CrossRefGoogle Scholar
Anderson, D. M., and Morgenstern, N. R.Physics, chemistry, and mechanics of frozen ground: a review. Permafrost. Second International Conference. … 1973, 1973, p. 257–88. [Describes developments since 1963, with emphasis on studies in North America.]Google Scholar
Anderson, D. M., and Tice, A. R.Predicting unfrozen water contents in frozen soil from surface area measurements. Highway Research Record, No. 393, 1972, p. 12–18. [Empirical equation derived which is accurate enough for normal engineering requirements.]Google Scholar
Anderson, D. M., and others. An examination of Mariner 6 and 7 imagery for evidence of permafrost terrain on Mars, [by] D. M. Anderson and L. W. Gatto [and] F. C. Ugolini. Permafrost. Second International Conference. … 1973, 1973, p. 499508. [Permafrost terrain described and compared with similar features on Earth.]Google Scholar
Anderson, D. M., and others. The unfrozen water and the apparent specific heat capacity of frozen soils, [by] D. M. Anderson, A. R. Tice and H. L. McKim. Permafrost. Second International Conference. … 1973, 1973, p. 289–95. [Presents equation for predicting apparent specific heat capacity and cumulative heat absorption versus temperature curve of frozen soils from their water–ice phase composition data.]Google Scholar
Berg, R. L., and Aitken, G. W.Some passive methods of controlling geocryological conditions in roadway construction. Permafrost. Second International Conference. … 1973, 1973, p. 581–86. [Most effective technique was to paint the road white.]Google Scholar
Bertouille, H.Résolution simple de problèmes de thermo-cinétique dans les sols. Application à la cryoclastie. Biuletyn Peryglacjalny, No. 22, 1973, p. 747. [Study of frost fractures in soils. From examination of horizontal fossil cracks, it is possible to estimate the severity of Quaternary winters.]Google Scholar
Bird, E. C. F.The periglacial legacy in the landforms of the Weymouth lowland (south-central England). Biuletyn Peryglacjalny, No. 22, 1973, p. 315–21. [Effects of periglaciation, although limited, are evaluated and discussed.]Google Scholar
Birkeland, P. W.Use of relative age-dating methods in a stratigraphie study of rock glacier deposits, Mt. Sopris, Colorado. Arctic and Alpine Research, Vol. 5, No. 4, 1973, p. 401–16. [Data from lichens, rock weathering and soils were used and compared. No single method was adequate, but a combination of all three provided the best estimate of age.]CrossRefGoogle Scholar
Black, R. F.Growth of patterned ground in Victoria Land, Antarctica. Permafrost. Second International Conference. … 1973, 1973, p. 193203. [Presents results of measurements made at 14 sites over interval of 6–8 years, and discusses their significance. Most of the patterned ground here dates within the last 5000 years.]Google Scholar
Bout, P., and Godard, A.Aspects du modelé périglaciaire en Scandinavie du Nord. Problèmes de genèse, comparaisons. Biuletyn Peryglacjalny, No. 22, 1973, p. 4979. [Study of periglacial forms in northern Scandinavia, in particular, palsas, boulder pavements, stratified slope deposits, and boulder fields and runs.]Google Scholar
Brandt, G. H.Chemical additives to reduce frost heave and water accumulation in soils. Highway Research Record, No. 393, 1972, p. 3044. [Describes use of soil waterproofing chemicals in dry and moist soils, with particular reference to 4-tert-butylcatechol. Discussion, p, 48–44.]Google Scholar
Brown, J.Environmental considerations for the utilization of permafrost terrain. Permafrost. Second International Conference. … 1973, 1973, p. 587–90. [General discussion of the situation.]Google Scholar
Brown, R. J. E.Influence of climatic and terrain factors on ground temperatures at three locations in the permafrost region of Canada. Permafrost. Second International Conference.1973 1973, p. 2734. [Measurements made down to 15 m depth at Thompson, Manitoba, Yellowknife, Northwest Territories, and Devon Island, Queen Elizabeth Islands, Canadian Arctic Archipelago.]Google Scholar
Brown, R. J. E., and Péwé, T. L.Distribution of permafrost in North America and its relationship to the environment: a review, 1963–1973. Permafrost. Second International Conference. … 1973, 1973, p. 71100. [Extensive review of recent progress.]Google Scholar
Cailleux, A.Éolisations périglaciaires Quaternaires au Canada. Biuletyn Peryglacjalny, No. 22, 1973, p. 81115. [Discusses action of wind on soils and rocks during the Quaternary in Canada.]Google Scholar
Cailleux, A.Répartition et signification des différents critères d’éolisation périglaciaire. Biuletyn Peryglacjalny, No. 23, 1973, p. 5163. [Discusses effects of wind on periglacial features during the Quaternary.]Google Scholar
Chamberlain, E.Mechanical properties of frozen ground under high pressure. Permafrost. Second International Conference. … 1973, 1973, p. 295305. [Discusses and reports results of recent high-pressure triaxial compression tests and isothermal compressibility tests.]Google Scholar
Cohen, J.Β. Solid waste disposal in permafrost areas. Permafrost, Second International Conference. … 1973, 1973, p. 590–98. [General discussion of problems.]Google Scholar
Collard, M.Cryoturbations en forme de stries enracinées parallèles à la pente. Biuletyn Peryglacjalny, No. 22, 1973, p. 324–27. [Describes periglacial features in the form of stripes of debris running parallel to the slope of the ground which were observed in a trench excavated in the Belgian Ardennes and were probably formed during the Quaternary.]Google Scholar
Crampton, C. B. Alandscape zonation for the southern and central Mackenzie River valley based on terrain permafrost characteristics. Canadian Journal of Earth Sciences, Vol. 10, No. 12, 1973, p. 1843–54. [Describes method and how to interpret results.]CrossRefGoogle Scholar
Crampton, C. B., and Rutter, N. W.A geoecological terrain analysis of discontinuously frozen ground in the upper Mackenzie River valley, Canada. Permafrost. Second International Conference. … 1973, 1973, p. 101–05. [Describes various terrain conditions and how permafrost characteristics may be identified from air photographs.]Google Scholar
Crory, F. E.Settlement associated with the thawing of permafrost. Permafrost. Second International Conference. … 1973, 1973, p. 599607. [Discusses practical methods of determining and predicting settlement on thawing.]Google Scholar
Czudek, T., and Demek, J.The valley cryopediments in eastern Siberia. Biuletyn Peryglacjalty, No. 22, 1973, p. 117–30. [Study of present-day slope development in this area of continuous permafrost.]Google Scholar
Derbyshire, E.Periglacial phenomena in Tasmania. Biuletyn Peryglacjalny, No. 22, 1973, p. 131–48. [Study of talus, solifluction debris, rock glaciers, nivation cirques, protalus moraines and bedded screes of late Quaternary age and some presently active periglacial forms, and their climatic implications.]Google Scholar
Dingman, S. L.Effects of permafrost on stream flow characteristics in the discontinuous permafrost zone of central Alaska. Permafrost. Second International Conference. … 1973. 1973, p. 447–53. [Studies at Glenn Creek watershed, near Fairbanks.]Google Scholar
Dingman, S. L., and Koutz, F. R.Relations among vegetation, permafrost, and potential insolation in central Alaska. Arctic and Alpine Research, Vol. 6, No. 1 1974, 3747. [Detailed description of occurrence of permafrost and discussion of factors affecting this.]CrossRefGoogle Scholar
Dunn, J. R., and Hudec, P. P.Frost and sorption effects in argillaceous rocks. Highway Research Record, No. 393, 1972, p. 6578. [Concludes that sorptive interactions with water vapour or liquid water are more destructive of aggregate materials than is freezing and thawing.]Google Scholar
Esch, D. C.Control of permafrost degradation beneath a roadway by subgrade insulation, Permafrost. Second International Conference. … 1973, 1973, p. 608–22. [Roadway fill sections constructed over frozen peat subgrade with 5.1 and 10.2 cm layers of extruded polystyrene foam insulation board have performed well during three years, surface settlement being very small and uniform.]Google Scholar
Fahfy, B. D.Seasonal frost heave and frost penetration measurements in the Indian Peaks region of the Colorado Front Range. Arctic and Alpine Research, Vol. 6, No. 1, 1974, p. 6370. [Presents observations which show-that rates of frost heave were correlated in a weak but positive manner with rates of host penetration.]Google Scholar
Ferrians, O. J., jr., and Hobson, G. D.Mapping and predicting permafrost in North America: a review, 1963–1973. Permafrost. Second International Conference. … 1973, 1973, p. 479–98. [Canada and Alaska.]Google Scholar
French, H. M.Cryopediments on the chalk of southern England. Biuletyn Peryglacjalny, No. 22, 1973, p. 149–56, [Distinguishes between cryopediments and cryoplanation terraces, and discusses their presence in the dry chalk valleys where their preservation may reflect the lack of present-day fluvial modification.]Google Scholar
French, H. M.Mass-wasting at Sachs Harbour, Banks Island, N.W.T., Canada. Arctic and Alpine Research. Vol. 6, No. 1, 1974, p. 7178. [Rates of movement observed are similar to those in other periglacial environments: sub-surface between 1.4 and 1.7 cm/year and surface about 2.5 cm/year.]CrossRefGoogle Scholar
French, H. M., and Egginton, P.Thermokarst development, Banks Island, western Canadian Arctic. Permafrost. Second International Conference. … 1973, 1973, p. 203–12. [Description, based on recent field work.]Google Scholar
Fulwider, C. W.Thermal regime in an Arctic earthfill dam. Permafrost. Second International Conference. … 1973, 1973 1973, p. 622–28. [Presents details of construction and temperature conditions within this dam at Thule, Greenland, during a six-year period.]Google Scholar
Garg, O. P.In situ physicomechanical properties of permafrost using geophysical techniques. Permafrost. Second International Conference. … 1973, 1973, p. 508–17. [Possible to use seismic refraction resistivity surveys, but detailed laboratory investigations on variation of seismic velocities and resistivity as function of temperature are required for complete accuracy.]Google Scholar
Gaskin, D. A., and Stanley, L. E.Control of culvert icing. Permafrost. Second International Conference. … 1973, 1973, p. 629–36. [Describes field and laboratory studies using electric heat cables.]Google Scholar
George, W.Analysis of the proposed Little Chena River, earthfilled nonretention dam, Fairbanks, Alaska. Permafrost. Second International Conference. … 1973, 1973, p. 636–48. [Dam to be located in area of marginal permafrost and will be used only for temporary storage of water to prevent flooding. Presents plans and discusses problems.]Google Scholar
Gill, D.A spatial correlation between plant distribution and unfrozen ground within a region of discontinuous permafrost. Permafrost. Second International Conference. … 1973, 1973, p. 105–13. [Study of taliks and their effect on vegetation in the Mackenzie Delta.]Google Scholar
Gold, L. W., and Lachenbruch, A. H.Thermal conditions in permafrost—a review of North American literature. Permafrost. Second International Conference. … 1973, 1973, p. 325. [Discusses die surface boundary condition and subsurface thermal conditions. Appendix by L. E. Goodrich on use of computerized numerical methods for ground temperature calculations, p. 23–25.]Google Scholar
Granberg, H. B.Indirect mapping of the snowcover for permafrost prediction at Schefferville, Quebec. Permafrost. Second International Conference. … 1973, 1973, p. 113–20. [Two techniques have been found useful: the development of a statistical model and the use of sequences of air photographs.]Google Scholar
Granholm, H.Om frostens nedträngande i marken med särskild hänsyn till möjlighrten att förhindra tjälskador. Chalmers Tekniska Hogskolas Handlingar, Nr. 332, 1971, 83 p. [Study of frost penetration in soil with particular reference to prevention of frost damage to constructions. English summary, p. 80–81.]Google Scholar
Harris, A. R.Effect of deciduous, coniferous, and abandoned field cover on the hydrologie properties and frost morphology of frozen soil. Dissertation Absracts International, B, Vol. 33, No. 1, 1972, p. 16-B–17-B. [Abstract of Ph.D. thesis, University of Minnesota, 1972. University Microfilms order no. 72–20111.]Google Scholar
Hastenrath, S., and Wilkinson, J. Acontribution to the periglacial morphology of Lesotho, southern Africa. Biuletyn Peryglacjalny, No. 22, 1973, p. 157–67. [Describes active and fossil periglacial forms found between 1800 and 3485 m, and relates to climate.]Google Scholar
Heginbottom, J. A.Some effects of surface disturbance on the permafrost active layer at Inuvik, N.W.T., Canada. Permafrost. Second International Conference. … 1973, 1973, p. 649–57. [Factor that overrides all others in controlling effects of any terrain disturbance on the permafrost active layer is the intensity of any previous disturbance; variations due to différent original terrain conditions are much less.]Google Scholar
Heinek, A.Strength and compaction properties of frozen soil. National Swedish Building Research. Document, D11: 1972, 1972, [120] p. [Strength of frozen soil increased with decreasing temperature and increasing water content, while compaction decreased. Compaction improved by increasing compaction energy.]Google Scholar
Hennion, F. B., and Lobacz, E. F.Corps of Engineers technology related to design of pavements in areas of permafrost. Permafrost. Second International Conference. … 1973, 1973, p. 658–64. [Discusses problems in building roads in areas of permafrost.]Google Scholar
Hoar, C. L., and Clark, L. K.A sanitary service complex for villages in permafrost regions: a demonstration project at Wainwright, Alaska. Permafrost. Second International Conference. … 1973, 1973, p. 664–73. [Describes design and operation of central building containing source of community water supply, waste disposal system and laundry facility, with drive-through passage for vehicle making deliveries to and collections from homes in village of 350 inhabitants.]Google Scholar
Hoekstra, P., and Mcneill, D.Electromagnetic probing of permafrost. Permafrost. Second International Conference. … 1973, 1973, p. 517–26. [Describes use of ground and airborne low frequency electromagnetic sensors for mapping electrical resistivity of ground. Also summarizes existing knowledge of resistivity of permafrost with emphasis on temperature dependence.]Google Scholar
Hughes, T. J.Glacial permafrost and Pleistocene ice ages. Permafrost. Second International Conference. … 1973, 1973, p. 213–23. [Discusses past and present (predicted) glacial permafrost in the northern hemisphere.]Google Scholar
Hunter, J. A. M.The application of shallow seismic methods to mapping of frozen surficial materials. Permafrost. Second International Conference. … 1973, 1973, p. 527–35. [Methods successfully applied to permafrost studies. Depth less than 30 m.]Google Scholar
Ivanov, N. S., and others, ed. Eksperimental’nyye issledovaniya protsesson teploobmena v merzlykh gornykh porod [Experimental research into heat exchange processes in frozen rocks]. [Edited by]N. S. Ivanov,A. V. Pavlov. L. V. Chistotinov. Moscow, Izdatel’stvo “Nauka”, 1972. 178 p. [Collection of 24 articles.]Google Scholar
Ives, J. D.Permafrost and its relationship to other environmental parameters in a midlatitude, high-altitude setting, Front Range, Colorado Rocky Mountains. Permafrost. Second International Conference. … 1973, 1973, p. 121–25. [Present conclusions relating to this environment.]Google Scholar
Jahns, H. O., and others. Permafrost protection for pipelines, [by] H. O. Jahns, T. W. Miller, L. D. Power, W. P. Rickey, T. P. Taylor and J. A. Wheeler. Permafrost. Second International Conference. … 1973, 1973, p. 673–84. [Number of recommendations made.]Google Scholar
John, B. S.Vistulian periglacial phenomena in south-west Wales. Biuletyn Peryglacjalny, No. 22, 1973, p. 185212. [Presents four hypotheses concerning the development and preservation of periglacial phenomena in Pembrokeshire and relates to field evidence. Discussion, p. 211–12.]Google Scholar
Judge, A. S.Deep temperature observations in the Canadian north. Permafrost. Second International Conference. … 1973, 1973, p. 3540. [Results from borehole measurements show thickest permafrost recorded at Winter Harbour, Melville Island, at 530 m depth.]Google Scholar
Jumikis, A. R.Effect of porosity on amount of soil water transferred in a freezing silt. Permafrost. Second International Conference. … 1973, 1973, p. 305–10. [Results illustrate importance of porosity of freezing soil on the amount of soil moisture transferred by the thermo-osmotic flow process by way of the water-film mechanism from groundwater to the cold front.]Google Scholar
Kachadoorian, R., and Ferrians, O. J., jr. Permafrost-related engineering geology problems posed by the trans-Alaska pipeline. Permafrost. Second International Conference. … 1973, 1973, p. 684–87. [Outlines engineering problems in preserving the environment.]Google Scholar
Kane, D. L., and Slaughter, C. W.Recharge of a central Alaska lake by subpermafrost groundwater. Permafrost. Second International Conference. … 1973, 1973, p. 458–62. [Demonstrates existence of unfrozen ground beneath lake surrounded by permafrost and recharge of lake from sub-permafrost aquifers through this ground.]Google Scholar
Kane, D. L., and others. Groundwater pore pressures adjacent to subarctic streams, [by] D. L. Kane and R. F. Carlson [and] C. E. Bowers. Permafrost. Second International Conference. … 1973, 1973, p. 453–58. [Presents results of measurements over 12-month period of pore water pressure and boundary conditions in the vicinity of two sub-Arctic streams in a permafrost-dominated environment.]Google Scholar
Katasonov, E. M.Classification of frost-caused phenomena with references to the genesis of the sediments in central Yakutia. Biuletyn Peryglacjalny, No. 23, 1973, p. 7180. [Divides cryogenic phenomena into subterranean and correlated surface structures according to the conditions in which the deposits were accumulated and frozen.]Google Scholar
Katasonov, E. M.Present-day ground- and ice veins in the region of the middle Lena. Biuletyn Peryglacjalny, No. 23, 1973, p. 8189. [Observations on development of periglacial features in central Yakutiya throw light on conditions leading to the formation of similar features during the Pleistocene.]Google Scholar
Kliewer, R. M. Ageneral solution for the two dimensional, transient heat conduction problem in permafrost, using implicit, finite difference methods. Permafrost. Second International Conference. … 1973, 1973, p. 4151. [Presents computer programming technique for modelling mathematically a large class of problems involving the thermal response of a permafrost medium.]Google Scholar
Konishchev, V. N., and others. Cryogenic processes as reflected in ground microstructure, [by] V. N. Konishchev, M. A. Faustova, V. V. Rogov. Biuletyn Peryglacjalny, No. 22, 1973, p. 213–19. [Presents observations on the microstructure of clay rock subjected to repeated freezing and thawing with particular reference to loess-like cover of the Bol’shezemel’skaya Tundra, and describes features of glacial deposits which may be of a cryogenic nature.]Google Scholar
Kostyayev, A. G.Some rare varieties of stone circles. Biuletyn Peryglacjalny, No. 22, 1973, p. 347–52. [May be due to hydrodynamic action rather than to periglacial causes.]Google Scholar
Kuznecova, T. P.Special features of cryolithogenesis in the alluvial plains, central Yakutia. Biuletyn Peryglacjalny, No. 22, 1973, p. 221–31. [Describes some periglacial features in this area of continuous permafrost.]Google Scholar
Laba, J. T., and Aziz, K. A.Pressure-time relationship in laterally stressed frozen granular soils. Highway Research Record, No. 393, 1972, p. 7987. [Study of general tendency in which the lateral stress in frozen sand samples that were subjected to radial pressure at constant temperatures diminishes with time. Reduction in literal stress was correlated with temperature, degree of ice saturation, porosity, initial pressure and time.]Google Scholar
Ladanyi, B., and Johnston, G. H.Evaluation of in situ creep properties of frozen soils with the pressuremeter. Permafrost. Second International Conference. … 1973, 1973, p. 310–18. [Field tests showed that the Ménard pressuremeter was suitable for use in conditions found at Thompson, Manitoba. Some problems in interpreting results are discussed.]Google Scholar
Lagarec, D.Éléments de la morphologie cryogène du golfe de Richmond, Nouveau-Québec. Cahiers de Géographie de Qtébec, Vol. 17, No. 42, 1973, p. 465–82. [Study of periglacial phenomena and major landforms of region enables classification of cryogenic and thermokarst features to be made.]CrossRefGoogle Scholar
Lagarec, D.Postglacial permafrost features in eastern Canada. Permafrost. Second International Conference. … 1973, 1973, p. 126–31. [Study of landforms, especially polygons, associated with former existence of permafrost, mainly in Quebec.]Google Scholar
Lange, G. R.Investigation of sampling perennially frozen alluvial gravel by core drilling. Permafrost. Second International Conference. … 1973, 1973, p. 535–41. [Practical problems.]Google Scholar
Larson, D. B., and others. Shock-wave studies of ice and two frozen soils, [by] D. B. Larson, G. D. Bearson and J. R. Taylor. Permafrost. Second International Conference.... 1973, 1973, 318–25. [Investigates loading and unloading characteristics of frozen materials in stress range 0–15 kbar and thus determines the effect that reaction kinetics and a soil matrix have upon the equations of state of frozen materials.]Google Scholar
Leschagk, L. A., and others. Potential use of airborne dual-channel infrared scanning to detect massive ice in permafrost, [by] L. A. LeSchack, F. H. Morse, W. R. Brimley, Jr., N. G. Ryan and R. B. Ryan. Permafrost. Second International Conference. … 1973, 1973, p. 542–49. [Method is possible for detecting ice in upper 2.5 to 3 m of permafrost.]Google Scholar
Lewellen, R. LThe occurrence and characteristics of nearshore permafrost, northern Alaska. Permafrost. Second International Conference. … 1973, 1973, p. 131–36. [Study, based on field measurements, of under-sea permafrost between Cape Beaufort and Demarcation Point.]Google Scholar
Linell, K. A.Long-term effects of vegetative cover on permafrost stability in an area of discontinuous permafrost. Permafrost. Second International Conference. … 1973, 1973, p. 688–93. [At Fairbanks, Alaska, (permafrost 30 m deep) only the undisturbed tree-covered test section remained free from permafrost degradation over 20 years’ observation. In cleared and stripped sections, degradation still continues.]Google Scholar
Linell, K. A.Risk of uncontrolled flow from wells through permafrost. Permafrost. Second International Conference. … 1973, 1973, p. 462–68. [Describes case history from Fairbanks, Alaska, when water well was drilled in 1946, and discusses how subsequent events might have been prevented.]Google Scholar
Linell, K. A., and Johnston, G. H.Engineering design and construction in permafrost regions: a review. Permafrost. Second International Conference. … 1973, 1973, p. 553–75. [North America.]Google Scholar
Long, E. L.Designing friction piles for increased stability at lower installed cost in permafrost. Permafrost. Second International Conference. … 1973, 1973, p. 693–99. [Recommendations made, based on author’s and others’ work.]Google Scholar
Luscher, U., and Afifi, S. S.Thaw consolidation of Alaskan silts and granular soils. Permafrost. Second International Conference. … 1973, 1973, p. 335–34. [Presents results of extensive laboratory investigations.]Google Scholar
Mc Gaw, R.Frost heaving versus depth to water table. Highway Research Record, No. 393, 1972, p. 4555. [Describes laboratory investigation of the influence of water (able depth on the freezing characteristics of four soil types ranging from gravelly sand to sandy clay.]Google Scholar
Mc Ginnis, L. D., and others. Geophysical identification of frozen and unfrozen ground, Antarctica, [by] L. D. McGinnis, K. Nakao, C. C. Clark. Permafrost. Second International Conference. … 1973, 1973, p. 136–46. [Studies in the dry valleys of Victoria Land revealed abnormally thin permafrost with respect to climate, probably due to presence of solar-heated lakes and to high water and soil salinities.]Google Scholar
Mackay, J. R.Problems in the origin of massive icy beds, western Arctic, Canada. Permafrost. Second International Conference. … 1973, 1973, p. 223–28. [Considers that massive bodies of segregated ice could grow at depth, in the same manner as that of segregated ice in pingos.]Google Scholar
Mackay, J. R., and Black, R. F.Origin, composition, and structure of perennially frozen ground and ground ice: a review. Permafrost. Second International Conference.... 1973, 1973, 185–92. [Mainly with reference to North America.]Google Scholar
Mackay, J. R., and Mathews, W. H.Needle ice striped ground. Arctic and Alpine Research, Vol. 6, No. 1, 1974, p. 7984. [Stripe orientations shown to develop parallel to shadows cast by sun when needle ice, with soil cap, thaws and collapses.]CrossRefGoogle Scholar
Mcvee, C. V.Permafrost considerations in land use planning management. Permafrost. Second International Conference. … 1973, 1973, p. 146–51 [General discussion of problems.]Google Scholar
Mainini, G.Osservazioni scientifiche nel distretto di Angrnagssalik, Groenlandia orientale. Il Polo, An. 29, No. 4, 1973, p. 8998. [Includes results of studies of frozen ground.]Google Scholar
Martini, A.Experimental investigations of frost weathering on granites. Stadia Geographica, 33, 1973, p. 6166. [Discusses results of laboratory studies.]Google Scholar
Mellor, M.Mechanical properties of rocks at low temperatures. Permafrost. Second International Conference. … 1973, 1973, p. 334–44. [Emphasizes importance of pore size and water content, which can affect strength and deformability.]Google Scholar
Mel’Nikov, P. I., and others. Geotermicheskiye issledovaniya v tsentral’noy Yakutii [Geothermal research in central Yakutiya]. [By] P. I. Mel’nikov, V. T. Balobayev, I. M. Kutasov, V. N. Devyatkin. Geologiya i Geofizika, 1972, No. 12, p. 134–37. [Study of heat flow from frozen and thawed zones.]Google Scholar
Miller, R. D.Freezing and heaving of saturated and unsaturated soils. Highway Research Record, No. 393. 1972, p. 111. [Theoretical considerations.]Google Scholar
Miller, R. D.Soil freezing in relation to pore water pressure and temperature. Permafrost. Second International Conference. … 1973, 1973, p. 344–52. [Mathematical analysis.]Google Scholar
Moore, D. G.Nitrate movement in freezing or frozen soils. Dissertation Abstracts International, B, Vol. 33, No. 7, 1973, p. 2888-B. [Laboratory and field investigations of effect of various temperatures and temperature gradients on nitrate movement in several types of soil. Abstract of Ph.D. thesis, South Dakota State University, 1972. University Microfilms order no. 7233333.]Google Scholar
Murrmann, R. P.Ionic mobility in permafrost. Permafrost. Second International Conference. … 1973, 1973, p, 352–59. [Was investigated directly by determining sodium ion diffusion coefficients and indirectly by measuring electrical conductance. Results define diffusion rates, determine how soil parameters affect ion migration, and provide information about the nature of unfrozen water in frozen soil.]Google Scholar
Nakano, Y., and Froula, N. H.Sound and shock transmission in frozen soils. Permafrost. Second International Conference. … 1973, 1973, p. 359–09. [Presents and interprets results of investigation by ultrasonic technique, and discusses behaviour of frozen soils under shock compression by use of gas gun.]Google Scholar
Nicholson, F. H., and Granberg, H. B.Permafrost and snowcover relationships near Schefferville. Permafrost. Second International Conference. … 1973, 1973, p. 151–58. [Studies at site in Quebec underlain by discontinuous permafrost showed that snow is the most important factor controlling permafrost distribution in this area, and there is a linear relationship between ground temperatures and snow depth.]Google Scholar
Nicholson, F. H., and Thom, B. G.Studies at the Timmins 4 permafrost experimental site. Permafrost. Second International Conference. … 1973, 1973, p. 159–66. [Describes research at this site underlain by discontinuous permafrost near Schefferville, Quebec.]Google Scholar
Nixon, J. F., and Morgenstern, N. R.Practical extensions to a theory of consolidation for thawing soils. Permafrost. Second International Conference. … 1973, 1973, p. 369–77. [Considers problems where thaw depth is not simply proportional to the square root of time, and problems where the change of void ratio of the soil bears a semi-logarithmic relationship with the change in effective stress.]Google Scholar
Nixon, J. F., and Morgenstern, N. R.Thaw-consolidation tests on undisturbed fine-grained permafrost. Canadian Geotechnical Journal, Vol. 11, No. 1, 1974, p. 202–14. [Settlements, pore water pressures and rates of thaw were measured in a series of tests on undisturbed Arctic soils. Results were interpreted in the light of current theories of heat transfer and thaw-consolidation.]CrossRefGoogle Scholar
Outcalt, S. I.A simulai ion sensitivity analysis of the needle ice growth environment. Permafrost. Second International Conference. … 1973, 1973, p. 228–34. [Points out both practical and theoretical value of this analysis.]Google Scholar
Penner, E.Influence of freezing rate on frost heaving. Highway Research Record, No. 393, 1972, p. 5664. [Stresses importance of the rate at which the soil is frozen and its effect on mobilizing moisture flow.]Google Scholar
Pettibone, H. C.Stability of an underground room in frozen gravel. Permafrost. Second International Conference. … 1973, 1973, p. 699706. [Discusses mine construction in frozen gravel, and problems encountered in year-round operation when temperatures are above freezing in summer.]Google Scholar
Péwé, T. L., and Sellmann, P. V.Geochemistry of permafrost and Quaternary stratigraphy. Permafrost. Second International Conference. … 1973, 1973, p. 166–70. [Preliminary analyses of frozen sediments and ice from northern and central Alaska suggest that the chemical investigation of frozen ground holds great potential for gross correlations in permafrost regions.]Google Scholar
Pissart, A.Les études expérimentales de l’action du gel voie de recherche d’avenir. Biuletyn Peryglacjalny, No. 22, 1973, p. 233–47. [Reviews recent experimental work on the formation of periglacial features.]Google Scholar
Pissart, A.Résultats d’expériences sur l’action du gel dans le sol. Biuletyn Peryglacjalny, No. 23, 1973, p. 101–13. [Describes laboratory experiments.]Google Scholar
Popov, A. I.Genetic systematics of periglacial formations. Biuletyn Peryglacjalny, No. 83, 1973, p. 115–24. [Discusses properties and types of cryolilhogenesis, and describes forms of thermokar.st.]Google Scholar
Price, L. W.Rates of mass wasting in the Ruby Range, Yukon Territory. Permafrost. Second International Conference. … 1973, 1973, p. 235–45. [Rates appear to be less than those recorded for other solifluctional areas, about 1–3 cm/year.]Google Scholar
Radd, F. J., and Oektle, D. H.Experimental pressure studies of frost heave mechanisms and the growth-fusion behavior of ice. Permafrost. Second International Conference. … 1973, 1973, p. 377–84-[Experimental and theoretical studies of basic frost heave mechanisms. Shows that ice lens formation is simply a special form of crystal growth.]Google Scholar
Raynal, R.Quelques vues d’ensemble à propos du périglaciaire pléistocène des régions riveraines de la Méditerranée occidentale. Biuletyn Periglacjatny, No. 22, 1973, p. 249–56. [Reviews recent periglacial evidence on the Pleistocene of areas bordering on the western Mediterranean.]Google Scholar
Reed, S. C., and Buzzell, T. D.A sewage-treatment concept for permafrost areas. Permafrost. Second International Conference. … 1973, 1973, p. 706–12. [Describes effective inexpensive single-tank treatment system.]Google Scholar
Richter, H. G.Main lines of the regional structure of periglacial facies on the territory of the G.D.R. Biuletyn Peryglacjalny, No. 23, 1973, p. 125–33. [Describes the pattern of periglacial facies formed at the time of the Vistula glaciation in what is now known as the German Democratic Republic.]Google Scholar
Romanovskiy, N. N.Regularities in formation of frost-fissures and development of frost-fissure polygons. Biuletyn Peryglacjalny, No. 23, 1973, p. 237–77. [Study of development of frost cracks.]Google Scholar
Rowley, R. K., and others. Vertical and lateral pile load tests in permafrost, [by] R. K. Rowley and G. H. Watson [and] B. Ladanyi. Permafrost. Second International Conference. … 1973, 1973, p. 712–21. [Analyses mathematically problems of constructing piles for supporting pipelines in frozen ground.]Google Scholar
Ryan, W. L.Design and construction of practical sanitation facilities for small Alaskan communities. Permafrost. Second International Conference. … 1973, 1973, p. 721–30. [Describes and discusses some of the installations currently in use and makes some general conclusions.]Google Scholar
Sayles, F. H.Triaxial and creep tests on frozen Ottawa sand. Permafrost. Second International Conference....1973, 1973, p. 384–91. [Study of effects of hydrostatic confining pressure and rate of applied load on strength and deformation characteristics of frozen sands and assessment of relative influence of cohesion of ice matrix versus friction between particles of sand.]Google Scholar
Sellmann, P. V., and Brown, J.Stratigraphy and diagenesis of perennially frozen sediments in the Barrow. Alaska, region. Permafrost. Second International Conference. … 1973, 1973, p. 171–81. [Investigations enable conclusions to be made about the late Quaternary history of the northern Alaskan Arctic coastal plain.]Google Scholar
Sherman, R. G.A groundwater supply for an oil camp near Prudhoe Bay, Arctic Alaska. Permafrost. Second International Conference. … 1973, 1973, p. 469–72. [Tests show that a year-round supply of water exists in an alluvial aquifer beneath a large Arctic stream.]Google Scholar
Sisko, R. K.Osobennosti sczonnotalogo sloya Novostbirskogo arkhipelaga [Features of the seasonally thawed layer of the Novosibirsk archipelago]. Trudy Arkticheskogo i Antarkticheskogo.Nauchno-Issledovatel’skogo Institute, Tom 318, 1973, p. 100–13. [Detailed study of local factors affecting thawing of ground.]Google Scholar
Smith, M. W., and Hwang, C. T.Thermal disturbance due to channel shifting, Mackenzie Delta, N.W.T., Canada. Permafrost. Second International Conference. … 1973, 1973, p. 5160. [Study of geomorphological pattern of permafrost distribution under shifting river channel and analysis of problem quantitatively in framework of heat conduction theory.]Google Scholar
Smith, N., and Berg, R.Encountering massive ground ice during road construction in central Alaska. Permafrost. Second International Conference. … 1973, 1973, p. 730–36. [Presents recommendations for making cuts through ice-rich soils.]Google Scholar
Smith, N., and others. The use of polyurethane foam plastics in the construction of expedient roads on permafrost in central Alaska, [by] N. Smith, R. Berg and L. Muller. Permafrost. Second International Conference. … 1973, 1973, p. 736–45. [Discusses the construction of roads destined for short-term use.]Google Scholar
Smith, W. S., and others. Sample disturbance and thaw consolidation of a deep sand permafrost, [by] W. S. Smith and K. Nair [and] R. E. Smith. Permafrost. Second International Conference. … 1973, 1973, p. 392400. [Effects of sample disturbance may have a significant influence on laboratory test results obtained with permafrost cores recovered from great depth (300440 m).]Google Scholar
Soloviyev, P. A.Thermokarst phenomena and landforms due to frost heaving in central Yakutia, Biuletyn Peryglacjalny, No. 23, 1973, p. 135–55. [Detailed descriptions.]Google Scholar
Steer, T. L., and others. Effects of ground-ice variability and resulting thaw settlements on buried warm-oil pipelines, [by] T. L. Speer, G. H. Watson and R. K. Rowley. Permafrost. Second International Conference. … 1973, 1973, p. 746–52. [Describes and discusses field and laboratory tests to determine the type and variability of ground ice occurring in permafrost soils and to establish limiting pipe burial criteria.]Google Scholar
Stevens, H. W.Viscoelastic properties of frozen soil under vibratory loads. Permafrost. Second International Conference. … 1973, 1973, p. 400–09. [Presents method of analysis and describes laboratory tests on frozen soils subjected to steady-state sinusoidal vibration in the longitudinal or compression mode and in the torsional or shear mode. Discusses results.]Google Scholar
Sutherland, H. B., and Gaskin, P. N.Pore water and heaving pressures developed in partially frozen soils. Permafrost. Second International Conference. … 1973, 1973, p. 409–19. [Compares predicted and actual values of pressures associated with a growing ice lens.]Google Scholar
Tedrow, J. C. F.Polar soil classification and the periglacial problem. Biuletyn Peryglacjalny, No. 22, 1973, p. 285–94. [Reviews present classification and suggests further taxonomic units.]Google Scholar
Thomson, S., and Lobacz, E. F.Shear strength at a thaw interface. Permafrost. Second International Conférence. … 1973, 1973, p. 419–26. [Compares strength characteristics assessed by laboratory tests with those observed in direct shear tests in which a frozen-thawed interface coincided with the shear plane imposed by the direct shear apparatus.]Google Scholar
Tobiasson, W.Performance of the Thule hangar soil cooling systems. Permafrost. Second International Conference. … 1973, 1973, p. 752–58. [Discusses experiences in ducted soil cooling systems gained at Thule airbase, north-west Greenland. Groundwater in the active layer was one particular problem.]Google Scholar
Tsvetkova, S. G., ed. Problemy geokriologii [Problems of geocryology]. Novosibirsk, Izdatel’stvo “Nauka”, 1973. 108 p. [Eleven articles.]Google Scholar
Tumel’, N. V.Temperature-controlled formation of cryogenic structure of permafrost of the Bolšezemelskaya Tundra. Biuletyn Peryglacjalny, No. 22, 1973, p. 295313. [Reviews earlier work in this area and presents some new ideas.]Google Scholar
Ugolini, F. C., and others. Soil development and patterned ground evolution in Beacon Valley, Antarctica, [by] F. C. Ugolini, J. G. Bockheim, D. M. Anderson. Permafrost. Second International Conference. … 1973, 1973, p. 246–54. [Detailed study in southern Victoria Land.]Google Scholar
Viereck, L. A.Ecological effects of river flooding and forest fires on permafrost in the taiga of Alaska. Permafrost. Second International Conference. … 1973,1973, p. 6067. [Long-lasting effects described.]Google Scholar
Vietoris, L.Über den Blockgletscher des Äusseren Hocheoenkars. Zeitschrift für Gletscherkunde und Glazialgeologie, Bd. 8, Ht. 1–2, 1972, p. 169–88. [Interprets measurements made between 1951 and 1970 on this rock glacier, and discusses its nature and formation.]Google Scholar
Walker, H. J.The nature of the sea water-fresh water interface during breakup in the Colville River delta, Alaska. Permafrost. Second International Conference. … 1973, 1973, p. 473–76. [Position and nature of interface was established with a salinometer and the volume of displaced sea water was calculated for period of breakup flooding. Method usable for any river that ceases flow for period.]Google Scholar
Watson, G. H., and others. Performance of a warm-oil pipeline buried in permafrost, [by] G. H. Watson and R. K. Rowley [and] W. A. Slusarchuk. Permafrost. Second International Conference. … 1973, 1973, p. 759–66. [Observations on settlement when oil was circulated at 71° C.]Google Scholar
Wein, R. W., and Bliss, L. C.Biological considerations for construction in the Canadian permafrost region. Permafrost. Second International Conference. … 1973, 1973, p. 767–70. [Review of problems.]Google Scholar
Williams, J. R., and Van Everdingen, R. O.Groundwater investigations in permafrost regions of North America: a review. Permafrost. Second International Conference. … 1973, 1973, p. 435–46.Google Scholar
Williams, P. J.Use of the ice-water surface tension concept in engineering practice. Highway Research Record, No. 393, 1972, p. 1929. [Discusses prediction of susceptibility of soils to frost heave and prediction of phase composition and, hence, thermal properties of frozen soils, and relates to engineering practice.]Google Scholar
Woodcock, A. H.Permafrost and climatology of a Hawaii volcano crater. Arctic and Alpine Research, Vol. 6, No. 1, 1974, p. 4962. [Describes and discusses occurrence of permafrost extending to 10 m depth at altitude of 4 140 m and mean annual air temperature of 3.6° C.]CrossRefGoogle Scholar
Yong, R. N., and others. Some aspects of surficial salt treatment for attenuation of frost heaving, [by] R. N. Yong, J. C. Osier and P. V. Janiga. Permafrost. Second International Conference. … 1973, 1973, p. 426–32. [Describes preliminary results obtained from two-year field study that will enable a complete analysis of the salt treatment problem to be made.]Google Scholar

Meteorological and Climatological Glaciology

Borisenkov, Ye.P., and Chernukhin, M. Sh. Estimation of the energy balance elements of the polar zone of the northern hemisphere (north of 50° N). (In Orvig, S., ed. Energy faxes over polar surfaces.… Geneva, World Meteorological Organization, 1973, p. 219–43.) [Most distinct patterns observed in winter, when intense flow of heat is directed into polar zone from the Pacific. Cold flow from Arctic observed over Eurasia and North America.]Google Scholar
Fletcher, J. O., and others. Numerical simulation of the influence of Arctic sea ice on climate, by J. O. Fletcher, Υ. Mintz, A. Arakawa and T. Fox. (In Orvig, S., ed. Energy fluxes over polar surfaces.... Geneva, World Meteorological Organization, 1973, p. 181218.) [Comparison between time-averaged distributions of atmospheric variables in two numerical atmospheric general circulation experiments, one with and one without ice over the Arctic Ocean.]Google Scholar
Hess, M.A method of determining the influence of mountain glaciers on the climate. Arctic and Alpine Research, Vol. 5, No. 3, Pt. 2, 1973, p. A183-A186. [Develops linear equations relating mean monthly temperatures to other temperature-related climatic elements and uses these to demonstrate degree of influence of glaciers on climate. Shows that climate as a whole can be changed if there is a change in the mean monthly temperature.]Google Scholar
Hobbs, P. V., and Farber, R. T.Fragmentation of ice particles in clouds. Journal de Recherches Atmosphériques, Vol. 6, 1972, p. 246–58. [Evidence for this fragmentation and discussion of possible mechanisms.]Google Scholar
Hobbs, P. V., and others. Collection of ice particles from aircraft using detectors, [by] P. V. Hobbs, R. J. Farber and R. G. Joppa. Journal of Applied Meteorology, Vol. 12, No. 3, 1973, p. 522–28. [Design, evaluation and field testing of two devices which can collect delicate ice crystals from aircraft.]2.0.CO;2>CrossRefGoogle Scholar
Holmgren, B.The energy exchange in the superimposed ice zone of the Devon Island ice cap in summer. (In Orvig, S., ed. Energy fluxes over polar surfaces.... Geneva, World Meteorological Organization, 1973, p. 123.) [Presents and discusses results of micrometeorological measurements.]Google Scholar
Hunt, G. E. Radiative properties of terrestrial clouds at visible and infra-red thermal window wavelengths, Quarterly Journal of the Royal Meteorological Society, Vol. 99, No. 430, 1973, p. 346–69. [Theory including ice clouds.]Google Scholar
Jayaweera, K. O. L. F., and Ohtake, T.Properties of columnar ice crystals precipitating from cloud layers. Journal of the Atmospheric Sciences, Vol. 31, No. 1, 1974, p. 280–86. [Crystals collected, photographed, and weighed. Habit similar to laboratory grown crystals. Bundles form by growth of secondary crystals on prism faces.]2.0.CO;2>CrossRefGoogle Scholar
Kuhn, M.Spectral energy distribution in shortwave fluxes over the east Antarctic plateau. (In Orvig, S., ed. Energy fluxes over polar surfaces.... Geneva, World Meteorological Organization, 1973, p. 2447.) [Radiation fluxes in the spectral range below 4 μ were used to characterize the scattering and absorbing processes in the Antarctic atmosphere; results are discussed.]Google Scholar
Mandrioli, P., and others. Distribution of microorganisms in hailstones, [by] P. Mandrioli, G. L. Puppi, N. Bagni, F. Prodi. Nature, Vol. 246, No. 5433, 1973, p. 416–17. [Number and type of germinating microorganisms and their radial variation in a 7 cm hailstone.]CrossRefGoogle Scholar
Mason, B. J.Production of ice crystals in slightly supercooled cumulus. Nature, Vol. 245, No. 5436, 1973, p. 451–53. [Letter. Discussion of theoretical explanation of existence of ice crystals in such clouds in terms of growth of rimed pellets which shed ice splinters.]CrossRefGoogle Scholar
Pitter, R. L.An experimental and numerical investigation of the evolution of ice particles in atmospheric clouds. Dissertation Abstracts international, B, Vol. 34, No. 6, 1973, p. 2841-B. [Experiments in cloud tunnel and theoretical calculations of crystal growth. Abstract of Ph.D. thesis, University of California, Los Angeles, 1973. University Microfilms order no. 73–28748.]Google Scholar
Pogosyan, Kh. P.The effect of large-scale tropospheric processes upon the geopotential field variations and the stratospheric air circulation. (In Orvig, S., ed. Energy fluxes over polar surfaces.... Geneva, World Meteorological Organization, 1973, p. 244–48.) [Shows that stratospheric warmings occur in the northern hemisphere as a result of localized meridional processes originating in the troposphere. These conditions are not available in the southern hemisphere.]Google Scholar
Radok, U.On the energetics of surface winds over the Antarctic ice cap. (In Orvig, S., ed. Energy fluxes over polar surfaces.... Geneva, World Meteorological Organization, 1973, p. 69100.) [Study of katabatic winds and their effect on the heat balance of the Antarctic ice sheet. Compares with trade winds.]Google Scholar
Schemenauer, R. S.The corrective mass-transfer of snow crystals, conical graupel and conical small hail modes. Dissertation Abstracts International, B, Vol. 34, No. 8, 1974, p. 3976-B. [Experiments to study mass transfer by diffusion and convection to models of snow, graupel and hail. Abstract of Ph.D. thesis, University of Toronto, 1972.]Google Scholar
Thompson, D. C.Surface heat balance and climate in an ice-free area of Antarctica. (In Orvig, S., ed. Energy fluxes over polar surfaces.... Geneva, World Meteorological Organization, 1973, p. 167–79.) [Presents results from two years’ continuous observations in Wright Valley.]Google Scholar
Vinje, Τ. E. On wind and temperature profiles above an Antarctic ice shelf. (In Orvig, S., ed. Energy fluxes over polar surfaces.... Geneva, World Meteorological Organization, 1973, p. 101–14.) [Discusses results of measurements of wind speed and temperature made 27 m above surface.]Google Scholar
Vowinckel, E., and Orvig, S.Synoptic energy budgets from the Beaufort Sea. (In Orvig, S., ed. Energy fluxes over polar surfaces.… Geneva, World Meteorological Organization, 1973, p. 143–66.) [Results of investigation of oasis effect, based on surface and upper air observations from drifting ice station.]Google Scholar
Wendler, G.Some measurements of the diurnal variation of the heat balance in central Alaska. (In Orvig, S., ed. Energy fluxes over polar surfaces.... Geneva, World Meteorological Organization, 1973, p. 4867.) [Explains physical processes in air and soil in relation to their diurnal and seasonal variations.]Google Scholar
Young, S. B., and Schofield, E. K.Pollen evidence for late Quaternary climate changes on Kerguelen Islands. Nature, Vol. 245, No. 5429, 1973, p. 311–12. [Discusses, in the light of studies on Îies Kerguelen, the suggestion that late-glacial and post-glacial changes in climate and vegetation were synchronous in the northern and southern hemispheres.]CrossRefGoogle Scholar

Snow

Abdul-Halim, R. K.Interaction of water quality, rainfall and snowmelt on soil salinity using sensors and samples. Dissertation Abstracts International, B, Vol. 33, No. 6, 1972, p. 2435-B–36-B. [Study of changes in salinity of a 70 cm soil profile for furrow-irrigated Zea mays L. under semi-arid climate of 45 cm average annual précipitation for two years. Abstract of Ph.D. thesis, Colorado State University, 1972. University Microfilms order no. 7231310.]Google Scholar
Ambach, W.Probleme des freien Wassergehaltes der Schneedecke. Sicherheit in den Bergen. Jahrbuch (Wien), 1972, [pub.] 1973, p. 8995. [Describes briefly methods for measuring the amount of free water contained in snow cover, and the relation between free water content and avalanche occurrence.]Google Scholar
Ambach, W., and Denoth, A.Studies on the dielectric properties of snow. Zeitschrift für Cletscherkunde und Glazialgeologie, Bd. 8, Ht. 1–2, 1972, p. 113–23. [Relations are established between dielectric constant, density and free water content of snow samples of various structures.]Google Scholar
Ambach, W., and others. Isotopic oxygen composition of firn, old snow and precipitation in alpine regions, by W. Ambach, H. Eisner and K. Pesst. Zeitschrift für Gletscherkunde und Glazialgeologie, Bd. 8, Ht. 1–2, 1972, p. 125–35-[Results of studies on firn cores, new snow and rain, all collected at different altitudes. Shown that snow layers could be identified within a snow pack by changes in isotopic composition during accumulation and ablation.Google Scholar
Armstrong, R. L.Avalanche studies in the San Juan Mountains of southwestern Colorado. Proceedings of the Western Snow Conference, 41st annual meeting. 1973, p. 4451. [Describes activities of the Institute of Arctic and Alpine Research, University of Colorado.]Google Scholar
[Avalanches.] Avalanche classification. Hydrological Sciences Bulletin, Vol. 18, No. 4, 1973, 391402. [Proposal of the Working Group on Avalanche Classification of the International Commission on Snow and Ice.]CrossRefGoogle Scholar
Bartos, L. R., and Rechard, P. A.Snow sampling technique on a small subalpine watershed. Proceedings of the Western Snow Conference, 41st annual meeting, 1973, p. 5261. [Discusses the advantages of a transect method of snow measurements. Snow density was uniform and required only a few measurements: more depth measurements were required.]Google Scholar
Booth, B.J.A simplified snow predictor. Meteorological Magazine, Vol. 102, No. 1216, 1973, p. 332–40. [Effectiveness of dew-point temperature as a snow predictor is reconsidered, and a simplified snow index suggested.]Google Scholar
Coyne, P. I., and Kelley, J. J.Variations in carbon dioxide across an Arctic snowpack during spring. Journal of Geophysical Research, Vol. 79, No. 6, 1974, p. 799802. [Subnivean CO2 was continually higher than ambient CO2 during period 1 May to 9 June 1971 near Barrow, Alaska. Reasons discussed.]CrossRefGoogle Scholar
Crook., A. G., and Freeman, T. G.A comparison of techniques of sampling the Arctic-subarctic snowpack in Alaska, Proceedings of the Western Snow Conference, 41st annual meeting, 1973, p. 6268. [Compares Bowman and CRREL snow samplers, and shows how data collected by one method may be adjusted to conform to values obtained by the other.]Google Scholar
Elgmork, K., and others. Polluted snow in southern Norway during the winters 1968–1971, [by] K. Elgmork, A. Hagen and A. Langeland. Environmental Pollution, Vol. 4, No. 1, 1973, p. 4152. [Study of snow profile shows correlation between greyish colour and acidity.]CrossRefGoogle Scholar
Gary, H. L. Growth of Engelmann spruce [Picea engelmanni) unaffected by increased snowpack. Arctic and Alpine Research, Vol. 6, No. 1. 1974, p. 2936. [Observations in New Mexico suggest that weather modification programmes will have little detrimental effect on radial growth of existing forests.]Google Scholar
George, T. A., and Mcandrew, D. W.Snow load analysis and recreational uses of snow data. Proceedings of the Western Snow Conference, 41st annual meeting, 1973, p. 6974. [Describes work in Nevada and Oregon.]Google Scholar
Henrirsem, A.Quantitative chemical analysis of snow. Vatten, Årg. 28, 5, 1972, p. 409–12. [Results used to estimate total yearly fall-out of various substances in southern Norway.]Google Scholar
Holroyd, E. W., III. The meso- and microscale structure of Great Lakes snowstorm bands—a synthesis of ground measurements, radar data, and satellite observations. Dissertation Abstracts International, B, Vol. 33, No. 6, 1972, p. 2747-B. [Includes detailed study of snow crystals in storms. Abstract of Ph.D. thesis, State University of New York at Albany, 1971. University Microfilms order no. 72–31774.]Google Scholar
Humphrey, J. H.Numerical prediction of snowpack temperatures in the eastside Sierra Nevada using a surface energy balance model. Dissertation Abstracts international, B, Vol. 33, No. 12, Pt. 1, 1973, p. 5942-B. [Predicted temperatures were usually within 10% of those observed at representative sites. Abstract of Ph.D. thesis, University of Nevada, Reno, 1972. University Microfilms order no, 73–15293.]Google Scholar
Ikoue, M., and Matsuda, M.Daisetsu-san Yukikabe sekkei ni okeru shitsuryō shūshi no kenkyū [Mass balance study of the Yukikabe perennial snow patch in the Daisetsu mountains]. Seppyō, Vol. 35, No. 4, 1973, p. 180–91. [English summary, p. 190–91.]Google Scholar
ΙSHIZΑΚA, Y. On materials of solid particles contained in snow and rain water: part 2. Journal of the Meteorological Society of Japan, Vol. 51, No. 5, 1973, p. 325–36. [Snow from Hokuriku coast of Japan contained loess particles blown from Hwang Ho region, China, across the Sea of Japan.]CrossRefGoogle Scholar
Isyumov, N.An approach to the prediction of snow loads. Dissertation Abstracts International, B, Vol. 33, No. 2, 1972. p. 704-B. [Describes assessment of snow loads on roofs from the balance between loads added by individual snowfalls and amounts removed by various natural depletion mechanisms. Abstract of Ph.D. thesis, University of Western Ontario, 1971. Microfilm order from National Library of Canada, Ottawa.]Google Scholar
Judson, A., and Erickson, B. J.Predicting avalanche intensity from weather data: a statistical analysis. U.S, Dept. of Agriculture. Forest Service. Research Paper RM-112, 1973, [ii], 12 p. [Weather and avalanche data from 23 avalanche paths were analysed by univariate techniques, which resulted in a simple two-parameter storm index that effectively predicts the number of avalanches expected on the 23 paths.]Google Scholar
Kikuchi, K.On the polarity of the electric charges on snow crystals of the various shapes. Journal of the Meteorological Society of Japan, Vol. 51, No. 5, 1973. p. 337–45. [Discusses observations on falling snow crystals made at “Syowa” station, Antarctica, where the electric polarity of dendrite, sector and plate crystals was found to be negative and that of column, bullet and side plane crystals was positive, depending on temperature of growth.]CrossRefGoogle Scholar
Moser, H., and others. Messungen des Deuterium- und Tritiumgehaltes von Schnee-, Eis- und Schmelzwasserproben des Hintereisferners (Ötztaler Alpen), von H. Moser, W. Rauert, W. Stichler und W. Ambach, H. Eisner, Zeitschrift für Gletscherkunde und Glazialgeologie, Bd. 8, Ht. 1–2, 1972, p. 275–81. [Relation established between isotope content and altitude of sampling site. Deuterium content significantly higher than in previous year. Results discussed.]Google Scholar
Norem, H.Snøvern. [Cslo], Yrkesopplæringsrådet for Håndverk og Industri. Universitetsforlaget, 1972. 35 p. [Countermeasures against damage and blocking of roads by avalanches and drifting snow.]Google Scholar
O’Neill, A.D. J. The energetics of shallow prairie snowpacks. Dissertation Abstracts International, B, Vol. 34, No. 2, 1973, p. 748-B. [Investigation into the development of a snow melt model applicable to the Canadian prairies. Abstract of Ph.D. thesis, University of Saskatchewan, 1973. University Microfilms order no. 73–18664.]Google Scholar
Owens, M. S., und Warburton, J. A.Analysis of iodine in Antarctic snow. Antarctic Journal of the United States, Vol. 8, No. 6, 1973, p. 343–44. [Preliminary data indicate that iodine concentration ai inland stations is lower than that previously reported for coastal snow in polar regions.]Google Scholar
Payette, S., and others. Relations neige-végétation dans la toundra forestière du Nouveau-Québec, Baie d’Hudson, [par] S. Payette, L. Filion et J. Ouzilleau. Naturaliste Canadien, Vol. 100, No. 5, 1973, p. 493508. [Herbaceous and cryptogamic formations have denser and more variable depth of snow cover than shrubs and trees. Pattern of snow distribution is discussed in relation to topography and soil conditions in this region.]Google Scholar
Perla, R. I., ed. Advances in North American avalanche technology: 1972 symposium. U.S. Dept. of Agriculture. Forest Service. General Technical Report RM-3, 1973, [iv], 54 p. [Contains the following papers: W. St. Lawrence and C. Bradley, “Ultrasonic emissions in snow”, p. 1–6; C. B. Brown, R. J. Evans and D. McClung, “Incorporation of glide, and creep measurements into snow slab mechanics”, p. 7–13; J. O. Curtis and F. W. Smith, “Material properly and boundary condition effects on stresses in avalanche snowpacks”. p. 14–23; T. E. Lang and R. L. Brown, “On the mechanics of the hard slab avalanche”, p. 24 28; R. A. Sommerfeld, “Statistical problems in snow mechanics”, p. 2936; M. Mellor, “Controlled release of avalanches by explosives”, p. 3749: P. A. Schaerer, “Observations of avalanche impact pressures”, p. 5154.]Google Scholar
Poulin, A. O.On the thermal nature and sensing of snow-covered Arctic terrain. Dissertation Abstracts International, B, Vol. 33, No. 7, 1973, p. 3067-B–68-B. [Describes winter air imagery experiments showing that sea and lake ice and snow depth, as well as other features, may be identified by means of temperature differences. Abstract of Ph.D. thesis, McGill University, 1972. Microfilm order from National Library of Canada, Ottawa.]Google Scholar
Sasteford, H.S., jr. Management of windblown alpine snows. Dissertation Abstracts International, B, Vol. 33, No. 12, Pt. 1, 1973, p. 5943-B. [Run-off from alpine cirques may be augmented successfully by applying a management effort to the wind-blown snow deposits along the ridge line. Abstract of Ph.D. thesis, Colorado State University, 1972. University Microfilms order no. 73–13046.]Google Scholar
Schaefer, D. G., and Nikleva, S. N.Mean precipitation and snowfall maps for a mountainous area of potential urban development. Proceedings of the Western Snow Conference, 41st annual meeting, 1973, p. 8089. [Study of climate north and west of Vancouver, Canada. Discusses problems of heavy rain and budgeting for snow removal.]Google Scholar
Schokni, T. R.Picture of the month. Autumn snow storms in the plains. Monthly Weather Review, Vol. 101, Νο. 12, 1973, p. 898900. [Observations made by satellite over the Great Plains of the United States.]2.3.CO;2>CrossRefGoogle Scholar
Schultz, R. W.Snowmelt lysimeters perform well in cold temperatures in central Colorado. U.S. Dept. of Agriculture. Forest Service. Research Note RM-247, 8 p. [Describes and discusses performance of lysimeters.]Google Scholar
Schultz, R. W.The use of snowmelt lysimeters for estimating the temporal and spatial distribution of snowmelt at Fraser experimental forest, Colorado. Dissertation Abstracts International, B, Vol. 33, No. 5, 1972, p. 2182-B. [Abstract of Ph.D. thesis. University of Michigan, 1972. University Microfilms order no. 72–29197.]Google Scholar
Smith, A. H.Picture of the month. Snow covers the southland. Monthly Weather Review, Vol. 101, No. 8, 1973, p. 654–55. [The NOAA 2 VHRR (visible) data of 10 and 11 February 1973 reveal, in detail, the structure of a major storm with resulting snow cover over the south-eastern United States.]2.3.CO;2>CrossRefGoogle Scholar
Sulahria, M. B.Prediction of water retentive capacity of high elevation snowpacks on the east side of the Sierra Nevada. Dissertation Abstracts International, B, Vol. 33, No. 12, Pt. 1, 1973, p. 5943-B. [Abstract of Ph.D. thesis, University of Nevada, 1972. University Microfilms order no. 73–12903.]Google Scholar
Tabler, R. D.Evaporation losses of windblown snow, and the potential for recovery. Proceedings of the Western Snow Conference, 41st annual meeting, 1973, p. 7579. [Demonstrates the size of losses from wind-blown snow by sublimation, and shows how this amount may be estimated. Importance of snow fences stressed.]Google Scholar
Truman, J. C.Wave propagation in snow. American Journal of Physics, Vol. 41, No. 2, 1973, p. 282–83. [Describes swishing sound and occasionally visible receding wave front caused by walking in snow, and discusses conditions of occurrence.]CrossRefGoogle Scholar
Veverka, J.The photometric properties of natural snow and of snow-covered planets. Icarus, Vol. 20, No. 3, 1973, p. 304–10. [Using the white light measurements of Knowles Middleton and Mungall, the Minnaert constants k and B 0 are derived for six types of snow surfaces for phase angles up to 80° and are used to estimate some parameters of smooth snow-covered planets.]CrossRefGoogle Scholar
Warburton, J. A., and others. Silver concentrations in Antarctic snow and fini, [by] J. A. Warburton, G. O. Linkletter and L. G. Young. Antarctic Journal of the United States, Vol. 8, No. 6, 1973, p. 342–43. [Average concentration was 8 × 10−13 g silver/ml.]Google Scholar
Ward, J. C.Water pollution potential of snowfall on spent oil shale residues. Proceedings of the Western Snow Conference, 41st annual meeting, 1973, p. 3743. [Factors in concentration and composition of water pollution from residue are cumulative volume, porosity of residue, soil moisture content, snow melt rate and fraction of snow melt water appearing as run-off. Overland flow water quality model presented.]Google Scholar
Woo, Ming-ko. Numerical simulation of snow hydrology for management purposes. Dissertation Abstracts International, B, Vol. 33, No. 8, 1973, p. 3758-B. [Describes method of estimating snow storage and melt water release for small coastal mountain basins in the temperate forest zone of south-western British Columbia. Microfilm order from National Library of Canada, Ottawa.]Google Scholar