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Glaciological Literature

Published online by Cambridge University Press:  30 January 2017

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Journal of Glaciology , Volume 13 , Issue 69 , 1974 , pp. 547 - 567
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. 87–99. [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. 38–43. [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. 36–43, 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. 5–10. [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. 73–29795.]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. 19–22. [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. 81–82. [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. 52–55. [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. 293–300 [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. 1–17. [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. 295–308. [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. 3–18. [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. 192–200. [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. 10–22. [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. 11–25. [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. 83–86. [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
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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
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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. 27–41. [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
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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
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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
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Smith, I. F.Gravity survey on Shoesmith Glacier, Horseshoe Island, Graham Land. British Antarctic Survey Bulletin, Nos. 33–34, 1973, p. 77–82. [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
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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
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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. 23–36. [Describes paths and limits of icebergs and their danger to shipping.]Google Scholar
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Blüthgen, J.Die Eisarten der Ostsee in ihrer geographischen Bedingtheit. Polarforschung, Bd. 7, 43. Jahrg., Nr. 1–2, 1973, p. 32–39. [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
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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
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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
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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. 45–52. [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
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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
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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
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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
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Thompson, T., and Udin, I.Isen i Östersjön; rutinistjänst och forskning. Ymer, Årg, 93, 1973, p. 60–82. [Describes activities of the Swedish ice reporting and forecasting service for the Baltic Sea.]Google Scholar
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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
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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. 1–12. [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
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Frost Action on Rocks and Soil. Frozen Ground. Permafrost

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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
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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
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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. 1–23.) [Presents and discusses results of micrometeorological measurements.]Google Scholar
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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. 69–100.) [Study of katabatic winds and their effect on the heat balance of the Antarctic ice sheet. Compares with trade winds.]Google Scholar
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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
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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. 48–67.) [Explains physical processes in air and soil in relation to their diurnal and seasonal variations.]Google Scholar
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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. 72–31310.]Google Scholar
Ambach, W.Probleme des freien Wassergehaltes der Schneedecke. Sicherheit in den Bergen. Jahrbuch (Wien), 1972, [pub.] 1973, p. 89–95. [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. 44–51. [Describes activities of the Institute of Arctic and Alpine Research, University of Colorado.]Google Scholar
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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. 52–61. [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. 799–802. [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. 62–68. [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. 41–52. [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. 29–36. [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. 69–74. [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. 493–508. [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. 29–36; M. Mellor, “Controlled release of avalanches by explosives”, p. 37–49: P. A. Schaerer, “Observations of avalanche impact pressures”, p. 51–54.]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. 80–89. [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. 898–900. [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. 75–79. [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. 37–43. [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