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Glaciological Literature

Published online by Cambridge University Press:  30 January 2017

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Copyright © International Glaciological Society 1976

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 Literatme (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 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

International Association Of Hydraulic Research. M.A.G.I.simpozium. Led i yego vozdeystviye na gidro-tekhmckeshye sooruziya. [Tom 1.] Dopolnitel'nyye materialy.-[Tom 2.} Leningrad, SSSR, 26-29 sentyabrya 1972 [I.A.H.R.symposium. Ice and its action onh ydraulic structures. [Vol.1] Lectures, papers and discussion records of symposium, - [Vol. 2.] Leningrad, U.S.S.R., 26-29 September 1972. Leningrad, Vsesoyuznyy Nauchno-IIssledovatel skiy Institut Gidrolekhniki imcni B. Ye. Vedeneyeva, [1974], [1972]. 197 p.; 306p. [Second international symposium; first was held in Iceland, 1970. About 70 papers. English translation in two separate volumes.]Google Scholar

General Glaciology

Avers, R. Ç,jr., Oil spills in the Arctic Ocean: extent of spreading and possibility of large-scale thermal effects, [by] Ayers, R. C., Jahns, H. O., Glaeser, J. L. Science, Vol. 186, No. 4166, 1974 p 845–4, [Criticism of article by S. Martin and W. J. Campbell, ibid., Vol. 181, No. 4094, 1973, p. 5658. Reply by Martin and Campbell, p. 845–46.]Google Scholar
Kuroiwa, D. ed Kyokuchihyô shöhyö no butsuriteki kagakuteki kenkyû [Physical and chemical studies in ices [sic] from glaciers and ice sheets]. Monbushö Kagaku Kenpi Sögö Kenkü (A).(A). Hokukusho, [1973,] [pub.] 1974 [iv], 125 p. [Collection of papers. Contents: A. Higashi and H. Shöji, “Nankyoku hyöshö shinbunyö no rikigakuleki scishitsu [Mechanical properties of deep ice core samples obtained at Byrd station Antarctica]”, p. 1–13; D. Kuroiwa and T. Kawamura, “Jinköieki ni atsumitsu shila seppyö to nankyoku sepnyö no danseintsu to naibu masalsu [Elastic modulus and internal friction of artificially compressed snow and Antarctic snow and ice]”, p. 5–22; T. Yamada. “Mizuho kansoku-kyoten yori saishû sareta böringu koâ (fukasa 75 m) no közö. soshiki to tatcnami. yokonami no denpan sokudo to no kankci [Relation between sonic wave velocities and structures of core samples obtained at Mizuho camp, Antarctica]”, p. 223–27; S Mae and K Yamamoto, “Nankyoku hyöshö teibu no jikkentcki kenkyû (I). Kenkyü mokutcki to köatsü jikken söchi [An experimental apparatus for study of physical properties of ice under high pressure]” p. 29–32; 1J. Kuroiwa, Sefaseisu no atsumitsu ni tomonau yüdcnteki seishitsu [Change of dielectric properties of snow associated with uniaxial confined compression]”, p. 33–44; N. Maeno, “Investigations of electrical properties of deep ice cores obtained by drilling in Antarctica”, p. 45–56 (in English); T Yamada and T. Hasemi, Mizuho kansoku-kyoten ni okeru hyömen sekisetsu-sö no soshiki to netsudendôritsu to no kankei ni tsuite [On the relation between structure and thermal conductivity of sub-surface snow at Mizuho camp, Antarctica]”, p. 57–63; M. Muiozumi and S. Nakamura, “Kyokuchi hyôshôhyô no kagakuteki kenkyü [Chemical studies on ice cores from the Antarctic ice sheet]”, p. 65–75; Y. Endö “Tönankyoku tairiku no sekisetsu no atsumitsu [Densification of snow in south-east Antarctica]” p 77-83- K Kizaki Ice fabrics no kenkyushi to sono mondaiten [History of ice fabric study and related problems]" p. 85–93; M. Kumazawa, “Aisu faburikku no rironteki kenkyü [A theoretical study on ice fabrics]”, p. 95–97; G. Wakahama, “Nankyoku Amerii-dana hyö, Uiruksu-hyökyü oycibi Forugâ-misaki no shinsöhyö no kozo soshiki m tsuite [On ihe structure and texture of deep ice cores from Amery Ice Shelf, Wilkes Dome and Capa-Folger Antarctica]”, p. 99–108; M. Nakawo [i.e. Nakao] and S. Tanaka, “Tö nankyoku, heitö hy öga no böringu koä no kesshö shujiku höi bunpu ni tsuite [On the orientational distribution of c-axis of ice crystals of core samples]”, p. 109–13; S. Tanaka, “Köri no kesshö soshiki oyobi hyötai kêrö to faburikku patän no kisokusei ni tsuite [On the regularity of fabric patterns found in ice core samples]”, p. 115–19; M. Nakawo [i.e. Nakao] and G. Wakahama, “Arasuka-shü Makköu-hyöga chüryüiki no böiingu koä no kaiscki [Fabric studies of glacier ice obtained from McCall Glacier, Alaska]" p 121-25 ]Google Scholar
Lorius, C. Glaciological studies at dome C. Antarctic Journal of the United States, Vol. 10, No. 4, 1975, p. 159. [Preliminary results of mean annual temperature, annual snow accumulation, and mean isotopic content at 74° 39’ S., 123° 10’ E.JGoogle Scholar
Milton, D. J. Carbon dioxide hydrate and floods on Mars. Science, Vol. 183, No. 4125, 1974,p, 654–56. [Postulates floods at some past epoch when CO, 6H20 forming ground ice on Mars dissociated on pressure “release as cause of observed terrain features.]10.1126/science.183.4125.654CrossRefGoogle ScholarPubMed
Naruse, R. ed Glaciological research program in Mizuho Plateau—west Enderby Land, east Antarctica. Part 3, 1973-1974. Tokyo, National Institute of Polar Research, 1975. il., 121 p. (Japanese Antarctic Research Expedition. JARE Data Reports, No. 28 (Glaciology).) [Contents include: R. Naruse, “Outline of glaciological traverse in 1973-1974”, ?· 1-6; R. Naruse and K. Yokoyama, “Position, elevation and ice thickness of stations”, p. 747; K. Naruse, Movement of the ice sheet observed by a triangulation chain”, p. 4861 K Yokoyama “Net accumulation by stake measurements”, p. 6282.] 363Google Scholar
Sekanina, Z. Λ study of the icy tails of the distant comets. Icarus, Vol. 25, No. 2, 1975, p. 218–38. [Tests of this theory of composition of comet tails.]10.1016/0019-1035(75)90021-4CrossRefGoogle Scholar
ShimizU, H. ed. Glaciological research program in Mizuho Plateau—west Enderby Land, east Antarctica. Part 2,1969-1973. Tokyo, National Institute of Polar Research, 1975. ii, 235 p. (Japanese Antarctic Research Expedition. JARE Data Reports, No. 27 (Glaciology).) [Contents: T. Yamada, H. Narita, F. Okuhira H. Fukutani, 1 Fuiisawa and T Shiratsuchi, “Net accumulation of snow by stake measurements in Sâoya Coast—Mizuho Plateau in 1071-1073”, p. 1067; T. Yamada, “Stratigraphy of snow cover in Mizuho Plateau in 1971-1972”, p. 6883; M Nakawo [i.e. Nakao], “Variation of surface micro-relief of snow cover at Mizuho camp in 1971-1972“ p 84105; T, Yamada and H. Narita, “Drifting snow at Syowa station and Mizuho camp in 1971-1972”, p. 106113; T. Yamada, “Net radiation at the snow surface at Mizuho camp in 1971-1972”, p 114; T Yamada, “Snow temperature at Mizuho camp in 1971-1972”, p. 115–44; T. Yamada and H. Narita, “Snow temperature at 10 meters below the surface in Mizuho Plateau in 1971-1973”, p. 145; S. Kawaguchi, T. Yamada and H. Sasaki, “Surface meteorological condition in Mizuho Plateau in 1971-1972”, p. 146–61; H Shimizu, A. Yoshimura, R. Naruse, O. Watanabem M. Nakawo [i.e. Nakao] and F. Okuhira, “Movement of ice sheet and glaciers in Sôya Coast in 1972”, p. 162–74; A. Yoshimura and T. Kimura, “Surface topography of Mizuho camp area in 1970-1971”, p. 175–76; T. Yamada, “Thermal cracks in snow cover at Mizuho camp in 1971”, p. 177; T. Yamada, “Rising of water level in a drill hole in glacier ice, Sôya Coast in 1972”, p. 178–79; R. Naruse, “Density and hardness of snow in Mizuho Plateau in 1969-1970”, p. 180–86; O. Watanabe, “Density and hardness of snow in Mizuho Plateau—west Enderby Land in 1970-1971”, p. 187235.]Google Scholar

Glaciological Instruments and Methods

Bogorodskiy, V. V. Radiozondirooaniye l'da [Radio sounding of ice]. Leningrad, Gidrometeoizdat, 1975. 64 p. [Short account of method as applied to glaciers, frozen ground, and fresh-water and sea ice.]Google Scholar
Garelik, I. S., Ispol'zovaniye matcrialov s"yemok so sputnikov dlya glyatsiologicheskikh issledovamy [The use of satellites in glaciological studies], [By] Garelik, I.S. Grinberg, A.M. Krenke, A. N . Izuestiya Akademii Nauk SSSR. Seriya Geograficheskaya, 1975, No. 1, p. 93101. [Based on satellite photographs of Altay and Tyan’-Shan’.]Google Scholar
Jairell, R. L. A sturdy probe for measuring deep snowdrifts. U.S. Dipt, of Agriculture. Forest Service. Research Note RM-301, 1975, 3 p. [Sections of hexagonal aluminium rod joined with pump couplings form rigid probe which will sample drifts as deep as 40 ft.],Google Scholar
Ramseier, R. O. Weaver, R. J. Floating ice thickness and structure determination—heated wire technique. Ottawa, Environment Canada. Inland Waters Directorate. Water Resources Branch, 1975. v, 8 p. (Technical Bulletin No 88.) [Quick means of making in situ thickness measurements on fresh-water and sea ice. Describes method and presents details of construction of gauge with engineering drawings.]Google Scholar
Rand, J. H. 100-meter ice cores from the South Pole and the Ross Ice Shelf. Antarctic Journal of the United Stales, Vol 10 No 4 1075 p. 150–51. [Describes operation of CRREL shallow drill.]Google Scholar
Slesarenko, YU YE. Ul'lrazvukovoy sposob opredeleniya fazovogo sostava ledyanykh obrazovanii iz morskoy vodv i raslvorov [Ultrasonic method of determining the phase composition of ice formations from sea-water and solutions]. (In Tsytovich, N.A., ed. Vtoraya Mezhdunarodnaya Konferentsiya po Merzlolovedmiyu. Dokladyisoobshcheniya.[Edited by] Tsytovich, N.A., Savel’yev, B.A., Votyakov, I.N. Vyp. 4. Yakutsk, Yakutskoye Knizhnoye Izdatel'stvo, 1973, p. 215–18.) [Propagation of ultrasonic waves in ice m sea-water determined and used to deduce phase composition.]Google Scholar
Stengle, T. R., Sampling of glacial snow for pesticide analysis: the high plateau glacier of Mt. Logan[by] Stengle, T.R. Lichtenberg, T.J. Houston., C.S. (In Bushneil, V.C., Marcus, M G., ed. Icefield Ranges Research Project. Scientific results. Vol. 4. New York, American Geographical Society; Montreal, Arctic Institute of North America, 1974, p. 225–26.) [Describes technique for obtaining samples free from contamination, under adverse conditions with simple equipment.]Google Scholar

Physics of Ice

Baies, B. L., Separation of isotropic and anisotropic hyperfine constants in disordered systems by analysis of electron paramagnetic resonance lines at two different microwave frequencies: applications to the molecular structure around excess electrons in y-irradiated 10M sodium hydroxde alkaline ice glass[by] Bales, B.L. Bowman, M.K., Kevan, L., Schwartz, R.N. Journal of Chemical Physics, Vol. 63, No. 7, 1975, p. 3008–14.Google Scholar
Benditkis, R. S., Issledovaniye vliyaniya rastvora nitrit-nitrata khlorida kal'tsiya na mekhanicheskiye svovstva l'dâ [Effect of a calcium chloride nitrite-nitrate solution on the mechanical properties of ice]. [By] Benditkis, R. S., Luzhnov, Yu.M. Lyapushkin, N.N. Zhurnal Fizicheskoy Khimii, Tom 49, Vyp. 8, 1975. p. 2157–58. [Abstract of paper deposited with VINITI. English translation in Russian Journal of Physical Chemistry, Vol. 49, No. 8, 1975,p. 1269.]Google Scholar
Bling, E. V., Proton dipolar spin-lattice releaxation in hexagonal ice, [BY] Blinc, R. Gränicher, H., Lahajnar, G., Zupančič, I.. Zeitschrift für Physik B, Vol. 22, No. 3, 1975,p. 21.-17. [Measurement * proton dipolar spin-lattice relaxation time gives results which agree with the vacancy diffusion theory.]Google Scholar
Browell, E. V. Anderson, R. C. Ultraviolet optical constants of water and ammonia ices. Journal of the Optical Society of America, Vol. 65. No. 8,. 1975, p. 919–26. [Refractive index and upper limit on absorption coefficient for ice Ih, amorphous ice and amorphous ammonia ice measured.]10.1364/JOSA.65.000919CrossRefGoogle Scholar
Budd, W. F. Matkjda, M. Nijiku-kuriipu asshuku m okeru takesshöhyö no sentaku-höise. nit suite [On preferred orientation of polyerystalline ice by biaxial creep]. Teion-kagaku: Low Temperature Science, Ser. A, [No.] 32, 1974, p. 261–65.Google Scholar
Chessin, H., Investigation of the pseudobinary solid solutions of AgI-Cul by means of X-ray diffraction, [by] Chessin, H., Passarelli, R.K., Yonnegut, B Inorganic Chemistry, Vol. 14, No. 10, 1975,p. 2551–52. [Effectiveness of solid solutions as ice nucleators increases with decreasing mismatch between (0001) plane of ice and (III plane of solution.]10.1021/ic50152a052CrossRefGoogle Scholar
Davis, B. L., An explanation for the unusual nucleating ability of aerosols produced from the AgI-NH4l-acetone system, by Davis, B.L. Johnson, L. R. Moeng., F, J. Journal of Applied Meteorology, Vol. 14, No. 5, 1975, p. 891–96. [Attributed to existence of a complex compound with better epitaxial fit to ice than AgI.]10.1175/1520-0450(1975)014<0891:AEFTUN>2.0.CO;22.0.CO;2>CrossRefGoogle Scholar
Dostovalov, B. N. Struktury, fazovyye perekhody i svoystva svobodnoy i svyazannoy vody [Structures, phase transitions and properties of free and bound water]. (In Tsytovich, N.A., ed. Vtoraya Mezkdunarod-naya Konferentsiya po Merzlolovtdeniyu. Daklady i soobshcheniya. [Edited by] Tsytovich, N. A., Savel, B.A.'yev; Votyakov, I.N. Vyp, 4.Yakutsk, Yakutskoye Knizhnoye Izdatel'stvo, 1973, p. 116–25.) [Theoretical model used to discuss structures of ice, water and water vapour.]Google Scholar
Ermolieff, A. Brillouin scattering in ice and deuteratcd ice as a function of temperature. Solid State Communications, Vol. 17, No. 8, 1975, p. 1013–16. [Elastic constants deduced from light scattering measurements from sound waves in ice. Anomalies observed between 70 and 130 K.]10.1016/0038-1098(75)90243-4CrossRefGoogle Scholar
Fukuda, Λ. Hyötankesshö no sosei nejiri henkei [Plastic torsion deformation of ice single crystals), Hokkaidö Daigaku Kogakubu Kenkyū Hnkoku 74, 1975, p. 7382. [Creep under alternating torsional stress. Results interpreted in terms of dislocation generation and movement.]Google Scholar
Fukuta, N. A. study of the mechanism of contact ire nuclcation. Journal of the Atmospheric Sciences, Vol. 32, No. 8, 1975,p. 603. [Nuclei acted 2-3 deg higher temperature on contact than if already immersed in drop.]10.1175/1520-0469(1975)032<1597:ASOTMO>2.0.CO;22.0.CO;2>CrossRefGoogle Scholar
Gagin, A. The ice phase in winter continental cumulus clouds. Journal of the Atmospheric Sciences, Vol. 3.a, No. 8, 1975, p. 1604–14. [Measurements from instrumented aircraft.]10.1175/1520-0469(1975)032<1604:TIPIWC>2.0.CO;22.0.CO;2>CrossRefGoogle Scholar
Golubev, V. N. Zavisimost' struktury I'da ot solenosti zamerzayushchey vody (Relation of ice structure to the salinity of freezing water]. (In Tsytovich, N.A., ed. Vtoraya Mezhdunaradnaya Konferentsiya pa Merzlotoveđcniyu. Doklady i soobshcheniya. [Edited by] Tsytovich, N.A. Savel, B.A.'yev; Votyakov, I.N. Vyp. 4.Yakutsk, Yakutskoye Knizhnoye Izdatel'stvo, 1973, p. 180–84.) [Relation between number of crystals and salinity found.]Google Scholar
Hhallett, J. Shkivastava, S. K. Nucleation of supercooled water by large single crystals of silver iodide. Journal de Recherches Atmosphériques, Vol. 6, Nos. 1-3, 1972, p. 223–36. [Effect of_various treatments on initial freezing temperature.]Google Scholar
Jelliek, H. H. G. Adhesion of ice frozen from dilute electrolyte solutions. (In Mittal, K.L., ed. Adsorption al interfaces. Papers from a symposium . . . at the 167th meeting of the American Chemical Society, Los Angeles, Calif., April 2-5, 1974. Washington, D.O., American Chemical Society, 1975, p. 348–60. (ACS Symposium Series, [No.] 8.) [Analysis of reported results implies adhesion is due to shearing an interfacial liquid solution layer.]Google Scholar
Kane, S. G., The kinetics of the secondary nucleation of ice: implications to the operation of continuous crystallizers, [by] Kane, S.G. Evans, T.W. Brian, P. L. T. Sarofim, A, F.. Desalination, Vol. 17, No. 1, 1975, p. 316. [Measurement of nucleation rates under wide range of conditions used to hypothesize mechanism of secondary nucleation.]10.1016/S0011-9164(00)84077-1CrossRefGoogle Scholar
Kino, W. D. Fletcher, N. H. Pressures and stresses in freezing water drops. Journal of Physics D, Vol. 6, No. 18, 1973,p, 2157–73.. [Calculation of pressure within freezing drop and comparison with experiments.]Google Scholar
Kolosov, A. P. Shvayshteyn, Z. I. Vliyaniye temperatury fronta kristallizatsii na strukturu I'da pri getero-gennom ledoobrazovanii [Effect of crystallization front temperature on ice structure in heterogeneous ice formation]. Trudy Arklicheskogo i Antarklicheskogo jXauchno-IssledovateVskogo Institute, Tom 317, 1975, p. 6166. [Study of crystal size and orientations during freezing.]Google Scholar
Kroh, D. Ron, A. The overtone spectra of H2O, D2O and mixtures of H20 in D20 ice. Chemical Physics Ltters, Vol. 36, No. 4, 1975, p. 527–30. [Absorption bands measured and interpreted].10.1016/0009-2614(75)80295-8CrossRefGoogle Scholar
Kut’kov, A. A. Shchegolev, V. A. O konformatsionnoy podvizhnnstil l'dopodobnogo karkasa i mekhanizme ireniya I'da [Conformational mobility of ice-like framework and mechanism of ice friction]. Trudy. Novocher-kasskogo Politekhnicheskogo Instituia, Tom 295, 1974, p. 821.Google Scholar
Kvlividze, V. L., Vliyaniye mezhfaznoy granitsy na plavlcniye I'da v geterogennykh sistemakh [Effect ?t the interphase boundary on the melting of ice in heterogeneous systems], [By] Kvlividze, V.I. Ananyan, A.A. Krasnushkin, A.V. Kurzayev, A.B. Svyazannaya Voda v Dispersnykh Sistemakh, Vyp. 3, 1974, p. 120–26. [Effect of interfacial properties between water and a solid on the freezing point, consequent liquid surface layer, and effect on freezing point in capillaries.]Google Scholar
Kvlividze, V. I., YaMR podirzhnoy fazy vody na poverkhnosti t'da [N.M.R. of the mobile water phase on the surface of ice]. [By] Kvlividze, V.J. Kiselev, V. F., Ushakova, L.A. Vestnik Moskouskogo Universiteta. Fizika i Astranamiya, Tom 15, No. 6, 1974, p. 736–38. [Confirmation that narrow signal is due to mobile water molecules on ice surface.]Google Scholar
Maeno, N. Kyokuchi no köri no denkheki-seishiisu. I [Electrical properties of polar ice. I], Teion-kagaku: Low Temperature Science, Ser. A, [No.] 32, 1974, p. 2538. [Cores from three Antarctic stations studied and differences discussed. English summary,p. 38.]Google Scholar
Mizuno, Y. X-sen topogurafu ni yoru shimo oyobi heihanhyö no kcsshô-kekkan nokenkyü [X-ray topographical studies on crystal defects in hoarfrost and tabular ice]. Teion-kagaku: Low Temperature Science, Ser. A, [No.] 32, 1974, p. 1324. [Dislocations observed With and Burgers vectors, also stacking faults on (0001) planes, Chemical etch pits more dense than dislocations. English summary, p. 2224.]Google Scholar
Moan, J. øvik, B. Electrons in shallow traps at 77 K. Chemical Physics Letters, Vol. 36, No. 1, 1975,p. 120–22. [Methanol ice glass at 77 K shows a relatively stable shallow trap. Stability may be due to partial crystallization.]10.1016/0009-2614(75)85702-2CrossRefGoogle Scholar
Narayana, P. A., Electron spin echo envelope modulation of trapped radicals in disordered glassy systems: application to the molecular structure around excess electrons in y-irradiated IOM sodium hydroxide alkaline ire glass, [by] Narayana, P.A. Bowman, M.K., Kevan, L., Yudanov, V.F. Tsvelkov, Yu.D.. Journal of Chemical Physics, Vol. 63, No. 8, 1975, p. 3365–71.CrossRefGoogle Scholar
Nishieata, K. Whalley, E. Thermal effects of the transformation ice III-IX. Bulletin of the National Research Laboratory of Metrology (Tokyo), No. 30, 1975, p. 17. [Calorimetry gives value which suggests ice IX is still significantly disordered.]Google Scholar
Oguro, M. Hyötankesshö-chu no ten'i ni yoru X-sen kaseki topogurafu-jô no zö konturasuto [Contrast of images on'X-ray topographs of dislocations in ice single crystals]. Hokkaido Daigaku Kogakubu Kenkyü Hokoku, 69, 1973, p. 137–46. [Theory of X-ray topographic imaging of dislocations in ice and causes of double-image phenomenon.]Google Scholar
Oguro, M. Yözai fujunbutsu o fukumu hyötankesshö no ikusei. Ten'i közö to fujunbulsu no sonzai jôtai [Growth of ice single crystals from dilute aqueous solutions by the modified Bridgman method. Distribution of impurities and structure of dislocations]. Hokkaidö Daigaku Kogakubu Kenkyü Hokoku, 74, 1975, p. 8394. [Crystals with NH3, NH4F and NaCl impurities studied.]Google Scholar
Panyushkin, A. V., Vliyaniye elektricheskogo polya na adgeziyu I'da k poverkhnosti perftorirovannogo gidrofobnogo sloya [Effect of an electric field on ice adhesion to the surface of a perfluorinated water-repellant coating], [By] Panyushkin, A.V. Sinochkin, Yu, D., Sergacheva, N.A. Trudy Arkticheskogo i Antarkticheskogo Nauchno-lsshiovateV skogo Instituta, Tom 317, 1975, p. 99102. [Hardening the finishing coat in an electric field produces surface with very low ice adhesion.) Poc, M.-M., and Roulleau, M. The ice nucleating properties of an ultrafine aerosol of pure silver iodide, journal of Applied Meteorology, Vol. 14, No. 6, 1975, p. 1146–50. [Found to be strangely inactive.]Google Scholar
Reisciiel, M. T. Ice nuclei from reactions involving lead, ammonia and iodine. Atmospheric Environment, Vol. 9, No. 10, 1975, p. 955–58. [Experiments show presence of ammonium ion increases number of active nuclei formed from PbO in iodide solutions.]10.1016/0004-6981(75)90106-7CrossRefGoogle Scholar
Ryan, B. F. The dependence of the growth of a spherical ice particle on the water drop spectrum. Journal de Recherches Atmosphériques, Vol. 6, No. 4, 1972, p. 673–77. [Theory shows that size distribution of water drops affects growth, not just mean radius.]Google Scholar
Scott, B. F. Interstitial and lattice substituted models of an expanded ice-In lattice. Theoretica Chimica Acta, Vol. 40, Fasc. i, 1975, p. 6170. [Theoretical study of ice Ih lattice of twelve molecules with H2, N2, 02, HF, CO2, H20, NH3 CH4 or CH20 molecules intcrstitially or HF, NH3, or H20 substitutionally.]10.1007/BF00547913CrossRefGoogle Scholar
Shigeo, U. K.öri ni okeru puroton dainamikkusu [Proton dynamics in ice). Bussei Kenkyü, [Vol]. 17, [No.] 2, 1971, p. C58-C63. [Hamiltonian for collective motion of protons in ice deduced on assumption that interaction with oxygen is only via their chemical bonding.)Google Scholar
Slusher, R. B. Derr, V. E. Temperature dependence and cross sections of some Stokes and anti-Stokes Raman lines in ice Ih. Applied Optics, Vol. 14, No. 9, 1975, p. 2116–20. [Raman scattering studied and new lines observed.]CrossRefGoogle Scholar
Steen, H. B. Radioluminescence of H20 and D20 ice. Spectral characteristics. Chemical Physics Letters, Vol. 35, No. 4, 1975, p. 508–10. [Differences in radiofluorescence, afterglow and thermoluminescente studied and interpreted.)10.1016/0009-2614(75)85653-3CrossRefGoogle Scholar
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Suzuki, S. Sösa-gata denshiken bikyö ni yoru köri no hyömen no kansatsu [Observation of ice surfaces by a scanning electron microscope]. Teion-kagaku: Low Temperature Science, Ser. A, [No.] 32, 1974, p. 112. [Observations using cooled stage on pure and NaCI-doped ice. English summary,p. 12.]Google Scholar
Truonc, T. B. The luminescence excitation spectrum of y-irradiated ethanol glasses at 77 K. Presence of an anion band: H-. Chemical Physics Letters, Vol. 35, No. 3, 1975, p. 426–30. [Includes ascription of band observed in polycrystalline ice and alkaline ices to H-.jCrossRefGoogle Scholar
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Voytkovskiy, K. D. Golubev, V. N. Zavisimost' mekhanitheskikh svoystv I'da ot usloviy yego obtazovaniya [Relation of the mechanical properties of ice to the conditions of its formation]. (In Tsytovich, N.A., ed. Vtoraya Mezhdunarodnaya Konferentsiya po Mer zlotovedemyu. Doklady i soobshcheniyo. [Edited by] Tsytovich, N.A. Savel, B.A.'yev, Votyakov, I.N. Vyp. 4. Yakutsk, Yakutskoye Knizhnoye Izdatel'stvo, 1973,p. 716) [Review of relation of mechanical properties to method of formation.]Google Scholar

Land ice. Glaciers. Ice shelves

Barkov, N. I., Izotopno-kislorodnyye issledovaniya 500-metrovogo ledyanogo kerna iz skvazhiny stantsii Vostok [Oxygen isotope studies of a 500 m ice core from a drill hole at Vostnk station],[By] Barkov, N.I. Gordiyenko, F.G. Y Korotkevich, e.S. Kotlyakov, V.M. Informatsionnyy Byulleten' Sovetskoy Antarkti-cheskoy Ekspeditsii, No. 90, 1975,p. 3949-Google Scholar
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Portmann, J. P. Notices glaciologiqucs. Aperçu historique 1 (1880-1900). Les Alpes. Revue du Club Alpin Suisse, 51e An., 3e Trimestre, 1975, p. 182–88. [Describes first conception and organization of reports on "Les variations périodiques des glaciers des Alpes”, which have been published in Les Alpes from 1880 to the present day.]Google Scholar
Robin, G.DE Q. Radio-echo sounding of the Antarctic ice sheet. Antarctic Journal of the United States, Vol. 10, No. 4, 1975,p. 157–59- [Describes fourth season of radio-echo sounding, mainly bottom topography, of International Antarctic Glaciological Project area, Marie Byrd Land, and Ross Ice Shelf.]Google Scholar
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Tómasson, H. Grimsvatnahlaup 1972, mechanism and sediment discharge. Jökull, Ár 24, 1974 [pub. 1975], p. 2739. [Discharge estimated as 2 km3 containing about 29.5 X 106 tons sediment. Discusses complex mechanism. Icelandic summary, p. 3839.]Google Scholar
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Wakahama, G. Hasemi, T. Akyokuchi kanreihyôga ni okeru jôsekihyô no seisei ni tsuite [Formation of superimposed ice in sub-polar glaciers]. Teian-kagaku: Low Temperature Science, Ser. A, [No.] 32, 1974, p. 161–74. [Formed by freezing of melt water which has percolated down through glacier to be arrested by underlying impermeable ice layer. Important factor in mass budget studies. English summary,p. 172–74·]Google Scholar
Wakahama, G., Arasuka-shû Makkôru-hyôga-genryûiki ni okeru sekisetsu no hyögahyo eno tenka [Field studies on the transformation processes of snow into glacier ice in the accumulation area of McCall Glacier Alaska]. [By] Wakahama, G., Kuroiwa, D., Benson, C.S. Teion-kagaku: Low Temperature Science, Ser. A, [No.] 32, 1974,p. 143–59· [Examines transformation processes in this sub-polar glacier and compares with those occurring in polar and temperate glaciers. English summary, p. 158–59.]Google Scholar
Weaver, R. L. "Boas" Glacier (Baffin Island, N.W.T., Canada) mass balance for the five budget years 1909 to 1974 Arctic and Alpine Research, Vol. 7, No. 3, 1975, p. 279–84. [Presents estimates of specific winter, summer, and net balance for the 1972-73 and 1971-72 budget years and summarizes net balance for 1969 to 1975 period.]CrossRefGoogle Scholar
Weidick, A. Estimates on the mass balance changes of the inland ice since Wisconsin-Weichsel. Grenlands Geologiske Undersegelse. Rapport Nr. 68, 1975, 21 p. [Discusses changes in mass balance of Greenland ice sheet during change from pleniglacial to post-glacial equilibrium.]Google Scholar
Weiss, H., The chemical composition of a Greenland glacier,[by] Weiss, H., Bertine, K., Koide, M. Goldberg, E.D. Geochimica et Cosmochimica Ada, Vol. 39, No. 1, 1975, p. 110. [Water from dated strata was analysed for contents of various chemical elements. Notable increase in S04 during past decade attributed to combustion of fossil fuels.].10.1016/0016-7037(75)90180-5CrossRefGoogle Scholar
Whillans, I. M. The surface mass-balance of Marie Byrd Land, Antarctica: data interpretation and application. Ohio State University. Institute of Polar Studies. Report No. 51, 1975, vii 1., 86 p. [Develops precise and accurate calculation based on measurements made with poles; includes corrections for snow and firn settling and for migration of anchoring position along pole.]Google Scholar
Zatsepin, YE N. Otsenka moshchnosti lednikov arkhipelaga Severnaya Zemlya po geonzicheskim dannym [Estimate of depth of glaciers of Severnaya Zemlya archipelago using geophysical data]. Geofieuheskiye Melody Razvedki v Arklike, Vyp. 8, 1973, p. 98100. [Gives depths of individual glaciers.]Google Scholar

Icebergs. Sea, River and Lake Ice

Alekseyev, G. V., O postanovke nablyudeniy za potokami tepla i vlagi, tayaniyem i narastaniyem I'da na poverkhnosti razvodîy i molodykh l'dov v Arkticheskom basseyne [Organization of observation of heat and moisture flows, thawing and accumulation of ice on the surface of polynyas and young ice in the Arctic basin][By] Alekseyev, G V., Zablotskiy, G.A. Makshtas, A.P. Trudy Arkttckeskogo i Antarkttcheskogo Nauchno-hsledovateVskogo Instiluta, Tom 321, 1975. P. 143–47- [Emphasizes importance of part played by polynyas in ice regime of Arctic basin.]Google Scholar
Arya, S. P. S. A drag partition theory for determining the large-scale roughness parameter and wind stress on the Arctic pack ice. Journal of Geophysical Research, Vol. 80, No. 24, 1975,p. 3447–54· [Simple drag partition theory developed for classical problem of boundary layer flows over regular arrays of two- or three-dimensional roughness elements.].10.1029/JC080i024p03447CrossRefGoogle Scholar
Bfnson, C. S. Osterkamp, T. E. Underwater ice formation in rivers as a vehicle for sediment transport. (In Hood, D W., Kelley, E. J., ed. Oceanography of the Bering Sea with emphasis on renewable resources. Inter-national symposium for Bering Sea study, Hakodate, Japan, 31 January-4 February 1972.,.. Fairbanks Alaska Institute of Marine Science, University of Alaska, [c1974] P-401-02. (Occasional Publication No. 2.)) [Abstract only. Role of anchor and frazil ice. Discussion,p. 402.].Google Scholar
Biggs, A W. Remote sensing of surface properties.(In Ince, A. N., ed. Electromagnetic wave propagation involving irregular surfaces and inhomogeneous media. Papers and discussions presented at the Electromagnetic Wave Propagation Panel Symposium held in The Hague, Netherlands, 25-29 March, 1974. [Neuilly sur Seine], North Atlantic Treaty Organization Advisory Group for Aerospace Research and Development, 1975, p. 13-1–13-12. (AGARD Conference Proceedings No. 144.)) [Reviews some experimental techniques used in remote sensing of ocean surfaces, polar sea ice, and vegetation.]Google Scholar
Biggs, A. W. Volume scattering from ice and water in inhomngeneous terrain. (In Ince, A. N., ed. Electromagnetic wave propagation involving irregular surfaces and inhomogeneous media. Papers and discussions presented at the Electromagnetic Wave Propagation Panel Symposium held in The Hague, Neetherlands, 25-29 March, 1974. [Neuilly sur Seine], North Atlantic Treaty Organization. Advisory Group for Aerospace Research and Development, 1975 P. 16-1–16-13. (AGARD Conference Proceedings No. 144.)) [Considers volume scattering from Arctic sea ice and terrain (glacier snow) with varying amounts of water.]Google Scholar
Brooks, P. N. The influence of static mechanical properties on the resistance of fresh-water ice to ballistic penetration. Quebec, Dcpt. of National Defence, Research and Development Branch. Defence Research Establishment Valcartier, 1975. iiI., 29 p. (DREV Report 4032/75.) [Experimental investigation of penetration response of various types of fresh-water ice having different quasi-static mechanical properties, and whether mechanical properties correlate with ballistic behaviour.]Google Scholar
Carter, L. J. Icebergs and oil tankers: USGS glaciologists are concerned. Science, Vol. 190, No. 4215, [1975, p. 641–43. [Discusses possible danger to oil tankers from icebergs discharging from Columbia Glacier, near Valdez, Alaska.]CrossRefGoogle Scholar
Chaykina, S. A. Model' dreyfa l'da v Arkticheskom basseyne [A model of the drift of ice in the Arctic basin]. Trudy Arkticheshogo i Antarkticheskogo Nauchno-Issledouatel'skogo Instituta, Tom 321, 1975,p, 125–32.. [Atmospheric influence.]Google Scholar
Farengol'ts, I. V. Nablyudeniya s pomoshch'yu frantsuzskoy clektronnoy apparatury i sputnika "EOL" [Observations by means of French electronic apparatus and the satellite EOLE]. Informalsionnyy Byulleten' Sovetskoy Antarkticheskoy Ekspeditsii, No. 90, 1975, p. 105–09. [The EOLE iceberg programme, 1973.]Google Scholar
Fay, F. H. The role of ice in the ecology of marine mammals of the Bering Sea. (In Hood, D. W., Kelley, E. J., ed. Oceanography of the Bering Sea with emphasis on renewable resources. International symposium for Bering Sea study, Hakodate, Japan, 31 January-4 February 1972., Fairbanks, Alaska, Institute of Marine Science University of Alaska, [1974], p. 383–99.. (Occasional Publication No. 2.)) [Quality and quantity of ice as important in habitat selection as are terrain and vegetation to terrestrial mammals.]Google Scholar
Foss, S. D. An approximate solution to the moving boundary problem associated with the freezing and melting of lake ice. Dissertation Abstracts International, B, Vol. 35, No. 8, 1975, p. 3893-B. [Ice depths observed during experimental study agreed quite well with mathematical predictions. Abstract of Ph.D. thesis, University of New Hampshire, 1974. University Microfilms order no. 75-1655.]Google Scholar
Frederkino, R. Gold, L. W. Experimental study of edge loading of ice plates. Canadian Geotechnical Journal, Vol. 12, No. 4, 1975, p. 456–63. [Investigates effect of plate thickness and indentor width on maximum force that develops during ductile deformation of columnar-grained ice plates subjected to edge-loading.]10.1139/t75-053CrossRefGoogle Scholar
Fujino, K. Öl, M. Ryühyö rfidä bunkainö nosokutei. III. Hyôteki no gansuiritsu to hansha-kyodo no kankei [Measurement of the resolving capability of drift ice radar. III. Relation between the water content of the target and its reflective power]. Teion-kagaku: Low Temperature Science, Ser. A, [No.] 32, 1974, p. 229–33. [Concludes that intensity of radar echo from target is influenced by conductivity of material covering target. English summary,p. 233.]Google Scholar
Fujino, K., Joatsu kara 100 bars made no kaisui sekihyfj ondo [The freezing point of sea water at pressures up to 100 barsj. [By] Fujino, K., Lewis, E.L. Perkin, R.G. Teion-kagaku: Low Temperature Science Ser. A, [No.] 32, 1974, p. 185–94. [Measured in salinity range 18% < S < 35% at atmospheric pressure, showing results consistently lower than Hansen's (1904) values. English summary, p. 193–94.]Google Scholar
Gold, L. W. Blackstrap Lake ice cover parking lot: ice bridges of the James Bay project: salvage of heavy construction equipment by a floating ice bridge: discussion. Canadian Geotechnical Journal, Vol. 12, No. 3, 1975. P. 441–44. [Comments upon three recent articles in this journal: Vol. 11, No. 4, 1974 p. 490508; ibid., p. 599619; Vol. 12, No. 1, 1975, p. 5859.]10.1139/t75-048CrossRefGoogle Scholar
Gray, D. H. Propagation velocity of Decca frequency transmissions over sea ice. Canadian Surveyor, Vol. 29, No. 3, 1975, p. 277–88. [Discusses results of test comparing secondary phase lag effect of sea ice and sea water in Amundsen Gulf, Canadian Arctic.]10.1139/tcs-1975-0036CrossRefGoogle Scholar
Hasehi, T., Usui ittöhyö no seichô ni tsuite [On the growth of thin winter ice], Teion-kagaku: Low Temperature Science, Ser. A, [No.] 32, 1974, p. 207–19. [Model predicts growth curves which are in good agreement with observed changes. English summary, p. 218–19.]Google Scholar
Hisida [i.e. HISHIDA], M. Nankyoku shûrensen to nankyoku kansokusen no hyökai ni okeru ködö nissû to no kankei ni tsuite [On the correlation between the Antarctic Convergence line and the number of operational days of the Antarctic observation vessel in the frozen sea]. Suiro Yôhô: Hydrographie Bulletin, 1974, No. 95, p. 2530· [Deals with factors affecting formation of sea ice and effect of Antarctic Convergence.]Google Scholar
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Glacial Geology

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Ashwell, I. Y. Glacial and late glacial processes in western Iceland. Geografiska Annaler, Vol. 57.?, Nos. 3-4, 1975. p. 225–45.- [Suggests major superficial features formed by floating ice shelf, which provided environment for sedimentation of glacial marine drift deposits.]10.1080/04353676.1975.11879918CrossRefGoogle Scholar
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Price, R. J. The glaciation of west central Scotland—a review. Scottish Geographical Magazine, Vol. 91, No. 3, 1975, p. 134–45.· [Major problems relating to last glaciation that remain to be solved are primarily concerned with chronology of déglaciation and interpretation of stratigraphy.]10.1080/00369227508736314CrossRefGoogle Scholar
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Rapp, A. Some views on the Ordovician palaeoglaciation in Saharan Africa. Geologiska Föreningens i Stockholm Förhandlingar, Vol. 97, Pt. 2, No. 561, 1975,p, 142–50.. [Reviews work of French and Algerian scientists from 1961 to 1971.]CrossRefGoogle Scholar
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Roshöff, K. A probable glaciogenic sediment in the Särv Nappe, central Swedish Caledonides. Geologiska Föreningens i Stockholm Förhandlingar, Vol. 97, Pt. 2, No. 561, 1975, p. 192–95. [Describes diamictite, probably of Varangian age.]10.1080/11035897509454972CrossRefGoogle Scholar
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Rudmark, L. The dglaciation at Kalmarsund, south-eastern Sweden. Sveriges Geologiska Undersökning, Avhand-lingar och Uppsatser, Scr. C, Nr. 713, Ärsbok 69. Nr. 5. 1975. 88 p. [Special attention paid to glacial striae, highest shore-line and varvcd glacial clay.]Google Scholar
Saunderson, H. C. A comparison of empirical and theoretical frequency distributions for two-dimensional palaeocurrent data from the Brampton esker and associated sediments. Geografiska Annaler. Vol. 57.A, Nos. 3-4, 1975, p. 189200. [Brampton esker, near Toronto, Canada.)CrossRefGoogle Scholar
Scott, W. E. Quaternary glacial and volcanic environments, Mctolius River area, Oregon. Dissertation Abstracts International. B, Vol. 35, No. 7. 1975. p. 3396-B. [Latest Pleistocene glaciation was multiple; Neoglacial activity also recorded. Past glacier margins reconstructed from evidence. Abstract of Ph.D. thesis, University of Washington, 1974. University Microfilms order no. 74-29497.]Google Scholar
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Sommerhoff, G. Glaziale Gestaltung und marine Überformung der Schelf bänke vor SW-Grönland. Morpho-genetische Ergebnisse einer Fernreliefanalyse. Polarforschung, 45. Jahrg., Nr. l, 1975, p. 2331. [Results indicate bottom topography of shelf banks is due to accumulation of glacial deposits and marine abrasion.]Google Scholar
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Frost Action on Rocks and Sol Frozen Ground. Permafrost

Alekseyev, V. P. Naledi Leno-Amurskogo mezhdurech'ya [Naleds of the Lena-Amur interfluve]. Sibirskiy Geograficheskiy Sbornik, 10, 1975, p. 46127. [Survey of studies on formation and distribution of naleds in area.]Google Scholar
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Berg, I. Flyplassprosjektet pâ Svalbard. Anleggstekniskc arbcidcr. Frost i Jord, No. 15, 1975, p. 2329. [Describes construction of civil air-field near Longyearbyen, Spitsbergen. From June to September only, thawing depth of soil may be 50-100 cm. English summary, p. 2829.]Google Scholar
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Fahey, B. D. Nonsorted circle development in a Colorado alpine location. Geografiska Annaler, Vol. 57.A, Nos. 3-4, 1975, p. 153–64. [Examines characteristics, origin, development and dynamics of group of non-sorted circles produced by seasonal frost heaving and discusses age relations with other periglacial features in area.]CrossRefGoogle Scholar
Fukuda, M. Tôketsu-yukai ni yoru ganseki no fûka [Rock weathering by freeze-thaw cycles]. Teion-kagaku: Low Temperature Science, Ser. A, [No.] 32, 1974, p. 243–49. [Describes field work and results. English summary,p. 249.]Google Scholar
Fukuda, M. Inoue, M. Tôjô shita tsuchi no közö to danseiha-sokudo [Structure of frost-heaved soil and velocity of comprcssivc waves]. Teion-kagaku: Low Temperature Science, Ser. A, [No.] 32, 1974, p. 283–86.Google Scholar
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Heidmann, L. J. Predicting frost heaving susceptibility of Arizona soils. U.S. Dept. of Agriculture. Forest Service. Research Note RM-295, 1975, 7 p. [Study to identify frosl-susceptible soils. By using variables of bulk density, sand content and calcium, equation was constructed which accounted for 83% of total variation in heaving.]Google Scholar
Heidmann, L. J. Thokud, D. B. Effect of bulk density on frost heaving of six soils in Arizona, U.S. Dept. of Agriculture. Forest Service. Research. Note RM-293, 1975,4ρ· [For all soils and depths, frost heaving increased with bulk density.]Google Scholar
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Korsunskiy, M. B., Thermal insulation of motorway subgrades using foam plastic, by Korsun, M.B.-skiy, Gayvoronskiy, V.N. Rossovskiy, P.D. Frost i Jord, No. 15, 1975, p. 3944. [Avoidance of Trost heaving of roads.]Google Scholar
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Meteorological and Climatological Glaciology

Changnon, S. A., Design of a hall [sic,i.e hail] suppression project for Illinois, [by] Changnon, S.A. Morgan, G.M., Achtemeier, G.L. Towery, N.G. Grosh, R.C. Journal of Applied Meteorology, Vol. 14, No. 5, 1975, p. 771–82..2.0.CO;2>CrossRefGoogle Scholar
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Snow

Abbi, S. D. S. Pareek, R. S. Meteorological aspects of the occurrence of avalanches. Vayu Mandai: Bulletin 'of the Indian Meteorological Society (New Delhi), Vol. 4, No. 4, 1974, p. 101–03. 106. [Discusses prediction with reference to meteorological conditions in the Himalaya.]Google Scholar
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Fujii, T. Kojima, K. Tsumi-katamerareta yuki no shösetsu no okure [Delay in ablation of artificially packed part of snow cover]. Teion-kagaku: Low Temperature Science, Ser. A, [No.] 32, 1974, p. 129–41. [Mechanism of delay studied by observations of experimentally packed paths and undisturbed snow. Compression and density discussed. English summary, p. 140–41.]Google Scholar
Grasty, R. L. Snow-water equivalent measurement using natural gamma emission, Nordic Hydrology, Vol. 4, No. 1, 1975, p. 116. [Attenuation by snow of gamma radiation emitted by potassium, uranium and thorium depends on water equivalent of snow layer. Snow-water equivalents up to 18 cm may be measured to accuracy of 2 cm.]CrossRefGoogle Scholar
Herb, H. Schneefeldsprengungen mit einer Ringsprengseilbahn zur Sicherung von Skiabfahrten. Zbornik Meteoroloikih i Hidroloikih Radova (Beograd), Broj 5, 1974, p. 329–32. (Describes device used in Bavarian Alps for releasing avalanches by explosives.)Google Scholar
Hooan, A. W. Collection of drifting snow by a track-roughened surface. Journal of Applied Meteorology, Vol. 14, No. 3, 1975, p. 428–29. [Presents observations on creation of surface drag by vehicle tracks in the Antarctic; this slows wind velocity near ground and causes precipitation of windhorne ice particles.]Google Scholar
Hoinkes, H. C. Siogas, L. Innsbrucker Winter seit 1890-91. Wetter und Leben, Jahrg. 27, Ht. 1-2, 1975, p. 314. [Data from 84 winters investigated statistically, including snow cover and snow depth.]Google Scholar
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Judson, A. Avalanche warnings: content and dissemination. U.S. Dept. of Agriculture. Forest Service. Research Note RM-291, 1975, 8 p. [Discusses how to warn the public of dangerous conditions when travelling outside controlled areas.]Google Scholar
Khodakov, V. G. Rol' snezhnogo pokrova v prirode landshaftov Severa i yego fizicheskiyc svoystva [The role of snow cover in natural landscapes of the north and its physical properties]. Izvestiya Akademii Nauk SSSR. Seriya Geograficheskaya, 1975, No. 1, p. 1726. [Properties and effects of snow cover in Polyarnyy Ural.]Google Scholar
Kobayashi, D., Yp setsuki ni okeru kasenryüiki no suion. I [Stream temperature during the snow melt season. I]. [By] Kobayashi, D., Aburakawa Kojima, H.K. Ishikawa, N.. Teion-kagaku: Low Temperature Science, Ser. A, [No.] 32, 1974., p. 279–82.Google Scholar
Kobayashi, S. Saiküron-gata jifubukikei to hikidashibakagata jifubuki kei nohikaku [A comparison between cyclone-type and chest-of-drawer-type drift collectors]. Teion-kagaku: Low Temperature Science, Ser. A, [No.] 32, 1974, p. 8995. [Compares efficiency of two types of snow drift collectors. English summary, P- 95.]Google Scholar
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Petrov, V. N. Atmosfernoye pitaniye kdnikovogo pokrova Antarktidy {Atmospheric feeding of the Antarctic ice sheet]. Leningrad, Gidrometeoizdat, 1975. 152 p. [Deals with features of snow accumulation in Antarctica.]Google Scholar
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