Hostname: page-component-586b7cd67f-rcrh6 Total loading time: 0 Render date: 2024-11-24T23:34:07.824Z Has data issue: false hasContentIssue false

Glaciological Literature

Published online by Cambridge University Press:  30 January 2017

Rights & Permissions [Opens in a new window]

Abstract

Type
Other
Copyright
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
Steen, H. B. Holteng, J. Â. Radioluminescence of H20 and D20 ice. Journal of Chemical Physics, Vol. 63, No. 6, 1975, p. 2690–97. [Comparison between H20 and D2O samples used to deduce reasons for luminescence effects.]10.1063/1.431634CrossRefGoogle Scholar
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
Vereshchagin, L. F., O perekhode H20 v provodyashcheye sostoyaniye pri staticheskikh davlemyakh P = I Mbar]. [Transfer of H20 to the conducting state at static pressures P = I Mbar]. [By] Vere-shchagin, L.F., Yakovlev, Ye.N., Timofeyev, Yu.A.. Pisma u Zhurnal Eksperimentalnoy i Tearelicheskay Fiziki, Tom si, Vyp. 11, 1975, p. 643–45. [Resistivity found to drop by six orders of magnitude. Presumed phase transition, possibly to a metallic state, discussed. English translation in JETP Letters, Vol. 21, No. 11, 1975, p. 304·05·]Google Scholar
Vetrov, A. A., The spectrum of the intermolecular vibration of water, [by] Vetrov, A.A. Kondratov, O.I. Yukhnevich, G.V. Australian Journal of Chemistry, Vol. 28, No. 10, 1975, p. 2099–107. [Includes determination of force constants for ice.]CrossRefGoogle Scholar
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
Barry, R. G., Continental ice sheets: conditions for growth, [by] Barry, R.G. Andrews, J. T, Mahaffy, M A. Science, Vol. 190, No. 4318, 1975, p. 979–81. [Little Ice Age conditions in Canadian Arctic provide useful and sensitive analogue of glacial inception.]10.1126/science.190.4218.979CrossRefGoogle Scholar
Bjornsson, H. Explanation of jökulhlaups from Grimsvötn, Vainajökull, Iceland. Jökull, Ar 24, 1974 [pub.1 975l· P- 1-26. [Review of all available data. Primary cause is melting of ice in gothermal area. Icelandic summary, p. 2526.]Google Scholar
Brochu, M. Les trous à cryoconite du glacier Gilman (nord de l'Ile d'Ellesmère). Polarforschung, 45. Jahrg., Nr. 1, 1975, p. 3244. [Presents results of detailed observations on cryoconites on Eliesmere Island, N.W T., Canada.]Google Scholar
Budd, W. F., Raschet temperaturnogo profilya po dannym skvazhiny nastantsii Vostok [Estimation of temperature profile from data from the drill hole at Vostok station]. [By] Budd, W.F. Jenessen, D., Young, N.W. Informatsionnyy Byullete’ Sovetskoy Antarkticheskoy Ekspeditsii, No. 90, 1975, p. 5058.Google Scholar
Clough, J. W. Propagation of radio waves in the Antarctic ice sheet. Disseration Abstracts International B Vol. 35, No. 10, 1975, p. 4950-B [Discusses results obtained using wide-angle reflection measurements of velocity of propagation. Abstract of Ph.D. thesis, University of Wisconsin-Madison, 1974. University Microfilms order no. 74-30097.]Google Scholar
Clough, J. W. Robertson, J. D. RISP geophysical survey. Antarctic Journal of the United States, Vol. 10, No. 4, 1975,p. 153–55- [Survey included measurement of ice thickness and gravity, of horizontal gradients of ice thickness and gravity, seismic sounding of water depth beneath ice and studies of seismic and radio-wave velocities within ice shelf, all at several sites on Ross Ice Shelf.]Google Scholar
Clouch, J. W., RISP drill site survey, [by] Clough, J.W. Jezek, K.C., Robertson, J.D. Antarctic Journal of the United States, Vol. 10, No. 4 1975, p. 148–49. [Survey included radio-echo and seismic reflection soundings, seismic refraction profiles and radar survey of bottom crevasses.]Google Scholar
Dhar, O. N. Glaciers and their contribution to water resources. Vayu Mandal Bulletin of the Indian Meteorological Society (New Delhi), Vol. 4, No. 4, 1974, p. 104–06. [Brief description of glaciers in the Himalaya.]Google Scholar
Doake, C. S. M. Bottom sliding of a glacier measured from the surface. Nature, Vol. 257, No. 5529, 1975, p. 780–82. [Bottom sliding motion of Fleming Glacier, Graham Land, Antarctica, measured by comparison of surface velocities from survey and radio-echo techniques.]10.1038/257780a0CrossRefGoogle Scholar
Dressler, K. Fologrammetricheskiye raboty gruppy uchenykh GDR v semnadtsatoy sovetskoy antarkticheskoy ekspeditsii [Phologrammetric work of the German Democratic Republic scientists during the seventeenth Soviet Antarctic Expedition]. Informatsionnyy Byulleten' Sovetskoy Antarkticheskoy Ekspeditsii, No, 90, 1975, p. 5960. [Study of movement of glaciers in the Molodczhnaya area, 1972.] GARFIELD, D. E., and UEDA, Resurvey, H.T. of Byrd station drill hole.Antarctic Journal of the United States, Vol. 10, No. 4, 1975,p. 160. [To determine amount and direction of inclination and, hence, sub-surface flow patterns]Google Scholar
Holdswokth, G. Meserve Glacier. Wright Valley, Antarctica: part I. Basal processes. Ohio State University. Institute of Polar Studies. Report No. 37, 1974, xi, 104 p. [Discusses problem of glacier flow when temperature is below pressure-melting point.]Google Scholar
Hughes, T. J. The west Antarctic ice sheet: instability, disintegration, and initiation of ice ages Reviews of Geophysics and Space Physics, Vol. 13, No. 4, 1975, p. 502–26. [Previously issued as ISCAP Bulletin (University of Maine at Orono), No. 3, 1974.]10.1029/RG013i004p00502CrossRefGoogle Scholar
Iken, A. Glaciology, No. 5. Velocity fluctuations of an Arctic valley glacier, a study of the White Glacier, Axel Heiberg Island, Canadian Arctic Archipelago. Axel Heiberg Island Research Reports, McGill University, Montreal, 1974, vi. 116 P· [Velocity observed in relation to other phenomena, particularly water pressure in bottom conduits, during summers 1968-71.]Google Scholar
Ives, J. D. Glaciers of Baffin Island. Beaver, Outfit 306: 1, 1975, p. 3239. [Well-illustrated account of the role that these glaciers could play in heralding a new ice age.]Google Scholar
Karlen, W. Lichenometrisk datering i norra Skandinavien—metodens tillförlitlighet och regionala tillämpning.Appendix[by] Holm., S.-O. Stockholms Universitet. Naturgeografiska Institutionen. Forskningsrapporter, 22, 1975, 70 p. [Application of lichenometric dating method in northern Scandinavia; regional picture obtained of recent glacial fluctuations.]Google Scholar
Karsten, A. Stoker, M. Deformationsmessungen auf dem grönländischen Inlandeis während der Intern Glaziologischen Grönlandcxpedition 1974. Polarforschung, 45. Jahrg., Nr. 1, 1975, p. 4550. [Presents results of further measurements of deformation of Greenland ice sheet made at specified points.] KELLER, G. Glazitektonik als Wirkungsfeld exogener Dynamik. Eiszeitalter und Gegenwart, Bd. 25, 1975, p. 48–3. [Discusses dynamics of ice sheets.]Google Scholar
Kotlyakov, V. M. Lebedeva, I. M. "Kayushchiyesya" snega i l'dy, mekhanizm tkh obrazovaniya I indikatsionnoye znachemye [Penitentes of snow and ice, their formation and indication function]. Izvestiya Akademii Mauk SSSR. Seriya Geograficheskaya, 1975, No. 3, p. 2636. [Observations made 1969-73 in eastern Pamir, Tadzhikskaya A.S.S.R.]Google Scholar
Langway, C.C. Antarctic ice core studies. Antarctic Journal of the United States, Vol. 10. No. 4, 1975, p. 152153. [Describes core recovery from CRREL shallow drill.]Google Scholar
Lliboutry, L. A. Loi de glissement d'un glacier sans cavitation. Annules de Géophysique, Tom. 31, No. 2, 1975 p. 207–19. [Theory of sliding of glacier.] 'Google Scholar
Mayer, Z. Glyatsio-geodezicheskiye issledovaniya na lednike Kheysa v 1972 g. [Glacio-geodetic studies on Hays Glacier in 1972]. Informaisionnyy Byulleten' Sovetskoy Antarkticheskoy Ekspeditsii, No. 90, 1975, p. 6164. [Work on frontal movement of glacier.]Google Scholar
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
Thomas, R. H. Eilers, D. H. Glaciological measurements on the Ross Ice Shelf. Antarctic Journal of the United States, Vol. 10, No. 4, 1975, p. 149–50. [Programme aimed at measuring ice strain-rates, snow accumulation rates, 10 m temperatures, and ice velocities at network of stations 50 km apart over entire ice Shelf].Google Scholar
Thompson, E. M. Thompson, L. G. Microparticles from the Byrd station deep ice core. Antarctic Journal of the United States, Vol. 10, No. 2, 1975, p. 4850. [Individual examination and analysis of microparticles indicate most particles deposited during Wisconsin are chemically dissimilar to those deposited since. Mentions implication of this in studies of past climates.]Google Scholar
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
Vivian, R. Les glaciers des Alpes Occidentales. Étude géographique. L emprise de la glaciation actuelle et ses fluctuations récentes · le rôle des eaux; l'aménagement du paysage montagnard par les glaciers. Grenoble, Imprimerie Allier, 1975. 513 P- [Glaciers of the western Alps. Part 1: inventory and regional variability; part 2: recent fluctuations; part 3: hydrology; part 4: geomorphological role.] Google Scholar
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
Hunkins, K. The oceanic boundary layer and stress beneath a drifting ice floe. Journal of Geophysical Research, Vol. 80, No. 24, 1975, p. 3425–33. [Modified Ekman spirals developed beneath ice in upper layer, depth 15-25 m, during AIDJEX pilot experiment under storm conditions with rapid ice drift. Momentum integral method used to evaluate ice-water stress from profiles of current velocity.]10.1029/JC080i024p03425CrossRefGoogle Scholar
Irwin, G. J. Ice pressures at the shore of Lincoln Bay. Ottawa, Dept. of National Defence. Research and Development Branch. Defence Research Establishment Ottawa, 1975. iv 1., 34 p. + errata sheet. (DREO Report No. 729.) [Study carried out during break-up in July in Robeson Channel area indicates ice floes grounding on shore should pose little threat to many types of shoreline installation.]Google Scholar
Ishida, T. Mensôkanpo ni yoru sogunhyö no ryüdö bekutoru no keisan [Calculation of flow vector of open pack ice by two-dimensional correlation method]. Teion-kagaku: Low Temperature Science, Ser. A, [No.] 32, 1974, p. 221–27. [English summary, p. 226–27.jGoogle Scholar
Konishi, R. Saito, M. The relationship between ice and weather conditions in the eastern Bering Sea. (In Hood, D. W., E. J., Kelley., 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, [e1974], p. 425–50. (Occasional Publication No. 2.))'370 [Results of 12 year study show ice in Bering Sea is influenced by changes occurring in weather conditions and sea currents in cycles of two years. Conversely, ice distribution influences course of atmospheric pressure and temperature in cyclic manner. Discussion, p. 449–50.]Google Scholar
La violette, P. E. Hubertz, J. M. Surface circulation patterns off the east coast of Greenland as deduced from satellite photographs of ice floes. Geophysical Research Letters, Vol. 2, No. 9, 1975, p. 400–02. [Paths of ice floes indicate presence of anticyclonic surface eddies.]CrossRefGoogle Scholar
Mcroy, C. P. Goering, J. J. The influence of ice on the primary productivity of the Bering Sea. (In Hood, D.W., Kelley, E. T., 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, [e1974], p. 403–21 Occasional Publication No. 2.)) [Presents support for hypothesis that ice cover increases total annual primary productivity of Bering Sea, measured by algal bloom. Discussion,p. 419.]Google Scholar
Maguire, R. J. Watkin, N. Effects of ice cover on dissolved oxygen m Silver Lake, Ontario. Ottawa, Environment Canada. Inland Waters Directorate. Water Resources Branch, 1975. v, 3 p. (Technical Bulletin No. 89.) [During winter, amount of dissolved oxygen decreased and level of H2S increased, probably due to prevention of atmospheric mixing by ice and snow cover.]Google Scholar
Maksimov, I. V. Lykova, V. V. O nekotorykh prichinakh vekovoy migratsu kromki plavuchikh l’dov i zony rasprostraneniya aysbergov v Yuzhnom okeane [Some causes of the secular migration of the sea ice edge and the zone of iceberg distribution in the Southern Ocean]. Informatsionnyy Byulleten' Sovetskoy Anlarkticheskay Ekspeditsii, No. 90, 1975, p. 1113. [Effects of changes in atmospheric circulation.]Google Scholar
Marko, J. R. Thomson, R. E, Spatially periodic lead patterns in the Canada basin sea ice: a possible relationship to planetary waves. Geophysical Research Letters, Vol. 2, No.10 , 1975, p. 431–34. [Suggests lead production is associated with current shears inherent to planetary type waves propagating in underlying water mass.]10.1029/GL002i010p00431CrossRefGoogle Scholar
Odriscoll, T. N. Bergy bit. Eastern South Pacific. Marine Observer, Vol. 45, No. 249, 1975,p. 104. [Observed 16 July 1974, 62 miles north of stated mean ice limit on Admiralty Chart No. 789.]Google Scholar
Plakhotnik, A. F. Fizicheskaya. okeanologiya. Kratkiy obzor vazhneyshikh issledomniy [Physical oceanography. A short survey of research]. Moscow, "Nauka”, 1973- 128 p. [Includes chapter on sea ice.]Google Scholar
Rodewaid, M. Die Tendenzwende in der Eisberg-Drift bei Neufundland. Meteorologische Abhandlungen, Neue Folge, Ser. B, Bd. 1, Ht. 3, 1975, 3 p. [Observations on general tendencies in iceberg movement near Newfoundland during recent years.]Google Scholar
Rothrock, D. A. The energetics of the plastic deformation of pack ice by ridging. Journal of Geophysical Research, Vol. 80, No. 33, 1975, p. 4514–19 (Generalizers energy arguments of Parmerter andCoon (AIDJEX Bulletin, No. 19, 1973, P. 59112)and thus develops plastic constitutive equation for real pack ice in which ice of many different thicknesses ridges simultaneously.].10.1029/JC080i033p04514CrossRefGoogle Scholar
Sanderson, R. M. Changes in the area of Arctic sea ice 1966 to 1974. Meteorological Magazine, Vol. 104, Mo. 1240 1975, p. 313–23. [In both winter and summer months, mean area for 1972-74 is slightly less than that for 1069- 71. Suggests decrease also applicable to two consecutive 4-year periods between 1967 and 1974.]Google Scholar
Savatyiksin, L. M. Ob osnovoy prichine grandioznykh oblomov shel'fovykh lednikov Antarktidy [On the main cause of immense calving of the ice shelf of Antarctica]. Informalsionnyy Byulleten' Sovetskoy Anlarkticheskay Ekspeditsii No 90 1975, p. 1822. [Effect of barometric waves on iceberg formation.]Google Scholar
Stringfr, W. J. Barrett, S. A. Katie's floeberg. Northern Engineer, Vol. 7, No. 1, 1975, p. 2630. [Describes growth and decay of stranded floeberg (collection of multi-year ice, mostly consisting of remains of large pressure ridge systems) at 72° N., 162° W., west of Barrow, Alaska, observed 1973-75.]Google Scholar
Tabata, T. Movement and deformation of drift ice as observed with sea ice radar. (In D. W., Hood, Kelley, E. J. edOceanography 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, [e1974], P. 373–82' (Occasional Publication No. 2.)) [Describes and presents some results from radar network constructed 10 observe distribution and movement of ice oil Okhotsk Sea coast of Hokkaido, Japan. Discussion, p. 381–82.]Google Scholar
Thornluke, A. S., The thickness distribution of sea ice, [by] Thorndike, A.S. Rothrock, D.A. Maykutarid, G.A., Colony, R. Journal of Geophysical Research, Vol. 80, No. 33, 1975, p. 4501–13 [Describes small-scale processes involved in producing and maintaining ice of different thicknesses and, from these, develops model to describe large-scale consequences.]10.1029/JC080i033p04501CrossRefGoogle Scholar
Tveit, J. Jnsulation against ice at measuring weirs. Nordic Hydrology, Vol. 5, No. 1, 1975, p. 3249. [Described development of simple method for insulating conventional V-weir.]10.2166/nh.1974.0002CrossRefGoogle Scholar
Vasiliyev, K. PSea-ice forecasting. (In Meteorological services to marine and coastal activities. Proceedings of the regional training seminar, Rome, 1-12 April 1974. Organized by the World Meteorological Organization under its participation in the United Nations Development Programme. Roma, Istituto di Fisica dell Atmosfera, Consigho Nazionale delle Ricerche, 1974, p. 267–92.) [Discusses factors that should be considered in long- and short-term forecasting of ice formation, decay and thickness.]Google Scholar
Wadhams, P. Airborne laser profiling of swell in an open ice field. Journal of Geophysical Research, Vol. 80, No. 33, 1975 p. 4520–28 [Profiles of swell entering drift ice off east coast of Newfoundland were made using Geodotite profiler mounted in ice patrol aircraft, concurrent infra-red imagery along track enabling floe size distribution to be recorded.]Google Scholar
Wakatsuchi, M. Kaihyô seicho to kaihyô kara no burainu no haishutsu ni kansuru jikken [Experiments on the growth of sea ice and the rejection of brine]. Teion-kagaku: Low Temperature Science, Ser. A, [No.] 32, 1974, p. 195205. [Results of unidirectional freezing of natural sea water (33% salinity) in the laboratory; air temperature -5 to — 30°C with constant wind speed. English summary, p. 204–05.]Google Scholar
Watanabe, K. Optical rectification of satellite pictures for sea-ice study. (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, [e1974], p. 595606. (Occasional Publication No. 2.)) [For precise studies in specific localities by individual investigators, the principle and mechanism of an optical rectifier is described.]Google Scholar
Yamadti [i.e. yamauchi], S. Ikeda, S. Ryûhyô Jôhô Scntâ no katsudô to sono köka [Activities of the iceberg information centre]. Suiro Tâhô: Hydrographie Bulletin, 1974, No. 95, p. 6168. [Describes operation of Japanese organization, mentioning shore stations which cover iceberg movements in northern coastal waters.]Google Scholar
Yevseyev, V. V. Opyt ispol'zovaniya sputnikovykh daimykh pri forsirovanii antarkticheskikh dreyfuyushchikh t'dov v navigatsiyu 1970-1971 gg. [Use of satellite data for forcing a passage through Antarctic pack ice during the navigation of 1970-71J. Informatsionnyy Byulleten' Sovetskoy Antarkticheskoy Ekspeditsii, No. 90, 1975, p. 102–04.Google Scholar
Yevseyev, V. V. O rasprostranenii morskikh antarkticheskikh l'dov po dannym sputnikovykh nahlyudeniy [On the distribution of Antarctic sea ice from satellite observational data]. Informatsionnyy Byulleten' Sovetskoy Antarkticheskoy Ekspeditsii, No. 90, 1975, p. 1417. [Data for 1970—71 compared with those for 1966 and 1969,]Google Scholar

Glacial Geology

Aario, R., Glacial landforms with special reference to drumlins and fluting in Koillismaa, Finland, by R. Aario, L. Forsström and P. Lahermo. Finland. Geological Survey. Bulletin 273, 1974, 30 p.Google Scholar
Aaktolahti, T. Two glacial mound fields in northern Savo, Finland. Fennia, 139, 1975, 23 p. [Detailed investigation of form and possible origins.]Google Scholar
Adam, D. P. Ice ages and the thermal equilibrium of the Earth, II. Quaternary Research, Vol. 5, No. 2, 1975, p. 161–71. [Discusses internal dynamics of glaciations.]10.1016/0033-5894(75)90021-6CrossRefGoogle Scholar
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
Bergstrom, B. Deglasiasjonsforlpet i Aurlandsdalen og omrädene omkring, Vest-Norge. Norges Geologiske Undersokelse, Nr. 317, 1975, p. 3368. [Reconstructs course of déglaciation in Aurlandsdalen, west Norway.]Google Scholar
Blake, W. jr., Studies of glacial history in the Queen Elizabeth Islands, Canadian Arctic Archipelago. Stockholms Vniversitet. Naturgeografiska Institutionen. Forskningsrapporter, 21, 1975, 14 p. [Summary of five papers submitted as doctoral dissertation, previously published in Canadian Journal of Earth Sciences, Vol. 7, No. 2, 1970, p. 634–64; ibid., Vol. 11, No. 8, 1974, p. 1025–42; Acta Universitatis Outuensis. Ser. A. Scientiae Rerum Naturalium, No. 3, Geologica, No. 1, 1972, p. 77–104; Naturaliste Canadien, Vol. 100, No. 1, 1973, p. 51–58; Geografiska Annaler, Vol. 57.?, Nos. 1-2, 1975, p. 1–71.]Google Scholar
Blank, R. G. Mmargolis, S. V. Pliocene climate and glacial history of Antarctica as revealed by southeast Indian Ocean deep-sea cores. Geological Society of America. Bulletin, Vol. 86.. No. 8, 1975, p. 1058–66. [Results include indication that there was increase in Antarctic glaciation and possible onset of permanent ice shelf about 3.8 million years B.P.]2.0.CO;2>CrossRefGoogle Scholar
Catterall, J. W. Further evidence of glaciation in the extreme Western Isles of Scotland: a note. Scottish Geographical Magazine, Vol. 91, No. 2, 1975, p. 122–24. [Observations on striations, till deposits and stone orientation in the Monarch Isles.]CrossRefGoogle Scholar
Clague, J. J. Glacier-flow patterns and the origin of late Wisconsinan till in the southern Rocky Mountain Trench, British Columbia. Geological Society of America, Bulletin, Vol. 86, No. 6, 1975, p. 721–31. [Determined by means of study of glacial landforms, till fabric and till composition.]10.1130/0016-7606(1975)86<721:GPATOO>2.0.CO;22.0.CO;2>CrossRefGoogle Scholar
Grozier, M. J. J. On the origin of the Peterborough drumlin field: testing the dilatancy theory. Canadian Geographer. Vol. 19, [No.] 3, 1975, p. 181–95. [Form, dimensions and pattern of drumlins and associated drift deposits in this field north of Lake Ontario can be satisfactorily explained in terms of drumlin-forming conditions suggested by theory.]10.1111/j.1541-0064.1975.tb01860.xCrossRefGoogle Scholar
Denton, G. H., Glacial history of the Ross Sea, [by] Denton, G.H. Borns, H, W., Grosswald, M, G.[i.e. Grosval'd] Stuiver, M., Nichols, R.L. Antarctic Journal of the United States, Vol. to, No, 4, '975· p. 160–64. [Describes field work, mainly mapping moraines.]Google Scholar
Donner, J. J. Jungner, H. Errors in the radiocarbon dating of deposits in Finland from the time of dglaciation. Bulletin of the Geological Society of Finland, No. 46, Pt, 2 1974, p. 139–44. [Indicates sources of errors which have made radiocarbon dates of sediments from area of Salpausselkä moraines and north of them appear too old.]10.17741/bgsf/46.2.006CrossRefGoogle Scholar
Dylik, J. The glacial complex in the notion of the late Genozoic cold ages. Biuletyn Peryglacjalny, No. 24, 1975, p. 219–31. [Discusses palaeoclimatology and Pleistocene glaciation.]Google Scholar
Fillon, R. H. Deglaciation of the Labrador continental shelf. Nature, Vol. 253, No. 5491, 1975, p. 429–31. [Evidence including moraines and glacial landforms shows extent of Quaternary glaciation in Hamilton Bank area and suggests déglaciation was in progress 9 000 B.P.]10.1038/253429a0CrossRefGoogle Scholar
Fischer, K. Die pleistozäne Vergletscherung und die Frage der Landscnkung im Bereich des Ghonos-Archipels/ Südchile. Eiszeitalter und Gegenwart, Bd. 25, 1975, p. 126–31. [Pleistocene glaciation of Patagonian Andes.]Google Scholar
Gajgalas, A. L., Moraine-like deposits in the periglacial zone, [by] Gajgalas, A, I., Karpukhin, S.S. Paramonova, N.N. Sudakova, N.G. Biuletyn Peryglacjalny, No. 24, 1975, p. 723. [Discusses difficulty of distinguishing glacial deposits from non-glacial deposits.]Google Scholar
GlÜckerT, G. Mindel- und rissciszcitlichc Endmoränen des Illervorlandglctschers. Eiszeitalter und Gegenwart, Bd. 25, 1975, p. 96106.. [Describes end moraines of this piedmont glacier which existed during Mindel and Riss glaciations in south-west Germany.]Google Scholar
Gluckert, G. On Pleistocene glaciations in the German alpine foreland. Bulletin of the Geological Society of Finland, No. 46, Pt. 2, 1974, p. 117–31. [Presents results of investigations of moraine and gravel formations.]10.17741/bgsf/46.2.004CrossRefGoogle Scholar
Gripp, K. Eisrandstudien ausgehend von Sermeq, SW-Grönland. Meddelelser om Grenland, Bd. 195, Nr, 8, 1975, [40] p. [Ice marginal studies in Sermilik region, west Greenland, in 1930.]Google Scholar
Gripp, K. Untermoräne—Grundmoräne—Grundmoränenlandsrhaft. Eiszeitalter und Gegenwart, Bd. 25, 1975, P- 5-9- [Deals with development of moraines. JGoogle Scholar
Hastenkath, S. Spuren pleistozäner Vereisung in den Altos de Cuchumatanes, Guatemala. Eiszeitalter und Gegenwart, Bd. 25, 1975, p. 25—34· IDcscrihes moraines and relates to Pleistocene glaciation.]Google Scholar
Hero, D. G. Glacial and volcanic geology of the Ruiz-Tolima volcanic complex Cordillera Central, Colombia. Dissertation Abstracts International, B, Vol. 35, No. 8, 1975, p. 3986-B. [Reconstruction of Pleistocene ice caps and snowlines possible. Abstract of Ph.D. thesis, University of Washington, 1974. University Microfilms order no. 75-3994·]Google Scholar
Hormann, K. Ein neues Modell des würmzeitlichen Inn-Chiemsecglctschers. Überschiebung des Inngletschers über den Tiroler Achengietscher bis in Bereiche des heutigen Chicmsees. Eiszeitalter und Gegenwart, Bd. 35, 1975 p. 3547.- [Discusses non-simultaneous advance and retreat of adjoining Inn- and Achen-(or Chiemsee-)gletscher during Wurm period.]Google Scholar
Hyvärinen, H. Ekonen, M. Mannerjäätikön sulamisvaiheen aikainen uomasto Koarvikoddsin maastossa inarissa [Glacial drainage channels near Koarvikodds in Finnish Lapland]. Terra, Vol. 87.. No, 9, 1975, p. 8794. [Describes system of Quaternary glacial drainage channels, and discusses origin and classification. English abstract,p. 87.]Google Scholar
Johnson, P. G. Recent crevasse fillings at the terminus of the Donjek Glacier, St. Elias Mountains, Yukon Territory. Quaestiones Geographkae (Poznan), No. 2, 1975, p. 5359. [Small ridges of till close to terminus identified as crevasse fillings formed prior to 1969 surge.]Google Scholar
Kind, N. V. Glaciations in the Verkhoyansk mountains and their place in the radiocarbon geochronology of the Siberian late Anthropogene. Biuletyn Peryglacjatny, No. 24, 1975, p. 4154. [Discusses chronology of Pleistocene glaciation of this part of Siberia.]Google Scholar
Kozarski, S. Oriented kettle holes in outwash plains. Quaestiones Geographkae (Poznan), No. 2, 1975, p. 99112.[Occurrence in north-west Poland compared with similar kettle holes in Spitsbergen.]Google Scholar
Mccrea, W. H. Ice ages and the galaxy. Nature, Vol. 255, No. 5510, 1975, p. 607–09. [Passage of solar system through dust lane bordering spiral arm of galaxy may cause temporary variation of sun's radiation and so lead to ice epoch on Earth.]10.1038/255607a0CrossRefGoogle Scholar
Mathews, W. H. Ccnozoic erosion and erosion surfaces of eastern North America. American Journal of Snence, Vol. 275, No. 7, 1975, p. 818–24. [Data on Tertiary sediments on floor of western Atlantic Ocean permit new appraisal of post-Cretaceous erosion on adjacent land.]10.2475/ajs.275.7.818CrossRefGoogle Scholar
Mayewski, P. A. Glacial geologic investigation of upper Rennick Glacier region, northern Victoria Land. Antarctic Journal of the United States, Vol. io, No. 4, 1975, p. 164–66. [Describes field investigations to study glacial history and compare with other areas.]Google Scholar
Metzger, K. Ein Beitrag zur Gliederung der eiszeitlichen Ablagerungen im Trauntal bei Wels/Oberösterreich. Eiszeitalter und Gegenwart, Bd. 25, 1975, p. 1024. [Describes glacial deposits in this part of Austria and relates to Quaternary history.] NGoogle Scholar
Newell, R. E. Changes in the poleward energy flux by the atmosphere and ocean as a possible cause for ire ages. Quaternary Research, Vol. 4, No. 2, 1974,p. 117–27- [Discusses new theory.]CrossRefGoogle Scholar
Ólzafsdóttir, Þ. Jökulgaröur á sjávarbotni út af Breiöafiröi [A moraine ridge on the Iceland shelf, west of Breiöafjoröur], Náttúrfrsingurinn, Ár 45, Ht. [I], 1975, p. 3136. [Thought to represent maximum advance of Weichselian ice sheet in area. English summary,p. 36.]Google Scholar
Porter, S. C. Equilibrium-line altitudes of late Quaternary glaciers in the Southern Alps, New Zealand. Quaternary Research, Vol. 5, No. 1, 1975, p. 2747. [Results of calculations compared with present-day values obtained from field studies and air photography, and used to provide measure of gross difference in climate between present and earlier periods of glacial readvance.]CrossRefGoogle Scholar
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
Rains, R. B. Selby, M. J. Relatively young moraines of the Webb Glacier, Barwick Valley, Victoria Land, Antarctica. (In Stokes, E., ed: Proceedings of the seventh New Zealand Geography Conference, Hamilton, August 1972.[Christchurch], New Zealand Geographical Society, 1973,p. 235–45- (Conference Series No. 7.)) [Discusses modes of origin of moraines, and offers tentative interpretation of late history of glacier.]Google Scholar
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
Reed, M. A. Cordilleran and Laurcntide multiple glaciation, west central Alberta, Canada. Canadian Journal of Earth Sciences, Vol. 12, No. 9, 1975, p. 14931515. [Surficial deposits of area mapped and glacial history of area discussed. Evidence for four, possibly five, glaciations.]10.1139/e75-136CrossRefGoogle Scholar
Ritchot, G. Essais de géomorphologie structurale. Québec, Presses de l'Université Laval, 1975. [xx], 388 p. (Travaux du Département de Géographie de l'Université Laval, 3.) [Ch. 6 is largely concerned with glacial geology and periglacial effects, with reference to Canada.]Google Scholar
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
Rotnicki, K. Stratigraphie evidences of the survival of Riss glaciotectonic structures and forms in the marginal zone of the maximum extent of the last glaciation. Quaestiones Geographicae (Poznań), No. 2, 1975,p. 113–37· [Discusses relation of marginal forms of last glaciation to older glaciotectonic forms.]Google Scholar
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
Selby, M. J. The termini and moraines of glaciers in the McMurdo dry valleys, Antarctica. (In Stokes, E., ed. Proceedings of the seventh. New Zealand Geography Conference, Hamilton, August 1972. [Christchurch], New Zealand Geographical Society, 1973, p. 247–57. (Conference Series No, 7.)) [Discusses problem posed by presence of moraines and polar glaciers in relation to past history of glaciers.]Google Scholar
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
Soyez, D., Geomorfologiska tnvcnteringar och deglaciationsstudier i Dalarna och Västerbotten. Stockholms Universitel. Naturgeografiska Institutionen. Forskningsrapporter, 18, 1974, II l [Geomorphological mapping and study of retreat of Quaternary ice in north-west Dalarna, central Sweden, and Västerbotten mountain region, north Sweden. Based on articles published in ibid., II, 1971 and Geografiska Annaler, Vol. 56.A Nos. 1-2, 1974, p. 171. German summary, p. 910.]Google Scholar
Stufavsky, M. Gravenor, C. P. Magnetic fabric around boulders in till. Geological Society of America. Bulletin, Vol. 86, No. II, 1975,p. 1534–36- [Study of variation in magnetic till fabric enabled conclusions to be made about flow of ice around boulders.]10.1130/0016-7606(1975)86<1534:MFABIT>2.0.CO;22.0.CO;2>CrossRefGoogle Scholar
Ten brink, N. W. Holocene history of the Greenland ice sheet based on radiocarbon-dated moraines in west Greenland. Meddelelser om Grenland, Bd. 201, Nr. 4, 1975, 44 p. [Field work in Sendre Stramfjord area. Ice sheet retreated about 125 km during Holocene in this region.]Google Scholar
Young, J. A. T. Ice wastage in Glen Feshie, Inverness-shire. Scottish Geographical Magazine, Vol. 91, No. 2, 1975, p. 91101. [Sequence of glacial events established in this region of Scotland. Movement of ice sheet from south-west to north-east indicated; glacial drainage channels and eskers trace out sequence of progressive ice wastage from higher to lower ground.]CrossRefGoogle Scholar

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
Alkire, B. D., Improving low temperature compaction of a granular soil, [by] Alkire, B.D. Haas, W.M. Kaderabek, T.J. Canadian Geotechnkal Journal, Vol. 12, No. 4, 1975, p. 527–30. [Dry density of silly sand compacted below 0°C can be improved by using CaCl2 as additive.]10.1139/t75-059CrossRefGoogle Scholar
Barsch, D. King, L. An attempt to date fossil rock glaciers in Grison, Swiss Alps. (A preliminary note.) Quaestiones Geographical (Poznań), No. 2, 1975, p. 514. [Radiocarbon dating of organic material suggests rock glaciers near present timber line are 2 500 yr inactive or fossil.]Google Scholar
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
Bout, P. Le périglaciaire du Massif Central de la France. Biuletyn Peryglacjalny, No. 24, 1975, p. 187210. [Presents evidence showing that at onset of Quaternary, this region showed effects of periglacial climate]Google Scholar
Boyd, D. W. Computing freezing and thawing degree-days from monthly temperatures. Canada. National Research Council. Division of Building Research. Technical Paper No. 444, 1975, [29] p. [Development of equation and reasons for rejecting alternatives are discussed.]Google Scholar
Brockie, W. J. Experimental frost-shattering. (In Stokes, E., ed. Proceedings of the seventh New Zealand Geography Conference, Hamilton, August 1972. [Christchurch], New Zealand Geographical Society, 1973, p. 177–86. (Conference Series No, 7.)) [Attempts to relate qualitative results to specific landscape situations.]Google Scholar
Clapperton, C. M. Further observations on the stone runs of the Falkland Islands. Biuletyn Peryglacjalny, No. 24, 1975, p. 211–17. [Presents evidence supporting theory that stone runs were derived by frost-shattering and moved by solifluction. Suggests probable sequence of landform evolution leading to development.]Google Scholar
Danilov, I. D. Plastovyye l'dy v subakval'nykh otlozheniyakh severa Zapadnoy Sibiri [Stratified ice in subaqueous deposits in the north of Western Siberia]. Prirodnyye Usloviya Zapadnoy Sibiri, Vyp. 5, 1975, p. 205–15. [Describes horizontal beds of ice and vertical veins in permanently frozen rocks.]Google Scholar
Dionne, J.-C. Bibliographie annotée sur les formes et structures périglaciaires fossiles au Canada méridional. Biuletyn Peryglacjalny, No. 24, 1975, p. 369–71.Google Scholar
[Effects Of Frozen Ground On Roads.] Road research. Frost action on roads. Proceedings of the symposium on frost action on roads held at the Norwegian Road Research Laboratory in Oslo on 1st, 2nd and 3rd October 1973. [Paris], Organisation for Economic Co-operation and Development, [c1974]. 229 p. [Summaries of 54 papers and discussions at each session.]Google Scholar
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
Golte, W. Heine, K. Fossile Riesen-Eiskeilnctze am Nicderrhoin. Eiszeitaller und Gegenwart, Bd. 25, 1975, p. 132–40. [Describes fossil ice wedge polygons in lower Rhine valley.]Google Scholar
Hedges, J., Multiple cycles of crynplanation on Sugarloaf Mountain, Maryland. Biutetyn Peryglacjainy, No. 24, 1975 p. 233–43. [Mountain was widely though superficially modified by episodes of periglaeial climate during Pleistocene. Landforms described.]Google Scholar
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
Hoekstra, P., Ground and airborne resistivity surveys of permafrost near Fairbanks, Alaska, [by] Hoekstra, P., Sellmann, P.V. Delaney., A. Geophysics, Vol. 40, No. 4, 1975, p. 641–56. [Discusses VLF (very low frequency) surveys.]CrossRefGoogle Scholar
Hyvärinen, H. Ritchie, J. G. Pollen stratigraphy of Mackenzie pingo sediments, N.W.T., Canada. Arctic and Alpine Research, Vol. 7, No. 3, 1975, p. 261–72. [Growth of two eroded pingos was probably initiated about 2 500 years ago.]10.2307/1550001CrossRefGoogle Scholar
Nnstanes, B. Svalbard lufthavn. Hangar og kontrolltârn. Frost i ford, No. 15. 1975, p. 3137. [Describes construction of hangar and control tower at civil air-field near Longyearbyen, Spitsbergen, with reference to difficulties encountered through presence of permafrost. English summary, p. 3537.JGoogle Scholar
Jersak, J. Frost fissures in loess deposits. Biuletyn Peryglacjainy, No. 24, 1975, p. 245–58. [Describes and discusses formation of these polygonal fissures, with examples from Poland.]Google Scholar
Katasonov, E. M. Frozen-ground and facial analysis of Pleistocene deposits and paleogeography of central Yakutia. Biuletyn Peryglacjainy. No. 24, 1975, p. 3340 [Follows development of permafrost since Pleistocene in this region.]Google Scholar
Kinosita [i.e. Kinoshita], S. ed. Arasuka Kanada-hokubu no eikyû tôdo ni okeru kanrei chikei oyobi seibulsu kankyo no sogo chosa. Shown 4g-nen 6—γ gatsu [Joint studies on physical and biological environments in the permafrost, Alaska and north Canada. June to July, 1974]. Sapporo, Institute of Low Temperature Science, Hokkaido University, 1975. [iv], 143 p. [Contains the following papers: S. Kinosita [i.e. Kinoshita], "Eikyü tödo-ken gakujutsu chösa no sösetsu [General outline of joint studies on physical and biological environments in the permafrost]”, p. 132 (English summary,p. 3132); S. Kinosita [i.e. Kinoshita], Y. Suzuki, K Horiguchi, M. Fukuda, "Eikyü tödo hyösöbu no danmen kansoku [Core samplings in the upper layer of permafrost]”, p. 3361 (English summary, p. 61); M. Fukuda, "Eikyû tôdo chüki no chikei hattatsu to dai-yonki chishi [Quaternary histories of landform development in permafrost]”, p. 6284 (English summary,p. 8384); K. Horiguchi, "Eikyü tôdo hyôsôdo no kagakuteki seishitsu toku ni sanseido ni tsuite [Chemical properties, especially pri, of the upper layer of permafrost]”, p. 8594 (English summary,p. 9394); A. Sakai and S. Yoshida, M. Saitô, "Eikyû tôdo chitai ni okeru shinrin sliokusei no scitai teki tokuchô [Ecological characteristics of forests on permafrost]”, p. 95126 (English summary,p. 125–2(1); K. Tannn, "Eikyû tôdo to dojö döbutsu [Permafrost and invertebrates]”, p. 127–43 (English summary,p. 142–43).]Google Scholar
Kinosita [i.e. Kinoshita], S., Tomakomai ni okeru tôjô kansoku (Shöwa 48-49 nen tôki) [Frost heave in Tomakomai (1973-74)]. [By] Kinosita [i.e. Kinoshita], S., Suzuki, Y., Horiguchi, K., Fukuda, M., Inoue, M.. Teion-kagaku: Low Temperature Science, Ser. A, [No.] 32, 1974, p. 251–60. [Observations near Hokkaido. Minimum air temperature — 21.8°C. English summary,p. 260.]Google Scholar
Konokovskiy, A. K. Rezhimy merzlotnykh poymennykh pochv doliny Leny [Regimes of frozen soil of flood terraces of the Lena valley]. Novosibirsk, “Nauka”, 1974- 168 p. [Includes hydrological and chemical regimes; effect of using fertilisers.]Google Scholar
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
Kostyayev, A. G. The periglaeial zone of western Eurasian plains. Biuletyn Peryglacjainy, No. 24, 1975, p. 5568. [Describes what one would expect to find in this zone.]Google Scholar
Krayev, V. F. On the periglaeial character of the Ukrainian loesses. Biuletyn Periglacjalny, No. 24, 1975, p. 6970. [Summarizes concept.]Google Scholar
Ladanyi, B. Bearing capacity of strip footings in frozen soils. Canadian Geotechnical Journal, Vol. 12, No. 3, 1975, p. 393407. [Discusses basic requirements for determination of allowable bearing pressure for frozen soils, and shows how creep settlement and failure of strip footing in frozen soil can be predicted by use of simple mathematical model of an expanding cylindrical cavity.]10.1139/t75-043CrossRefGoogle Scholar
Mcartkur, J. L. Some observations on periglaeial morphogenesis in the Southern Alps, New Zealand. Gea-grafiska Annaler, Vol. 57.A, Nos. 3-4, 1975, p. 213–24. [Shows that main components of land surface in study area were produced during glaeial-periglacial episodes of late Pleistocene. Describes landforms and discusses nature of slope development.]CrossRefGoogle Scholar
Magkay, J. R. The closing of ice-wedge cracks in permafrost, Garry Island, Northwest Territories. Canadian Journal of Earth Sciences, Vol. 12, No. 9, 1975, p. 1668–74. [Describes simple gauge to measure in situ closing of thermal contraction cracks, Mean annual ice vein increment is probably less than 20% of mean winter crack width.]CrossRefGoogle Scholar
Michel, J. P. Périglaciaire des environs de Paris. Biuletyn Peryglacjalny, No. 24, 1975, p. 259352. [Describes landforms associated with periglacial conditions occurring during Quaternary in France,]Google Scholar
Mühleisen, R. Lämmle, A. Neue Untersuchungen zur Entstehung von Kammeis (Haareis). Meteorologische Rundschau. Jahrg. 28, Ht. 2, 1975, p. 5560. [Laboratory experiments suggest osmotic pressure in wood or soil pores is responsible for extrusion of ice needles when air temperature is o° to — 4°C]Google Scholar
Nixon, J. F. The role of convective heat transport in the thawing of frozen soils. Canadian Geotechnical Journal, Vol. 12, No. 3, 1975, p. 425–29. [Describes solution Tor one-dimensional thawing problem which accounts for migration of melt water to soil surface.]CrossRefGoogle Scholar
Pennex, E., Thermal conductivity laboratory studies of some Mackenzie Highway soils, [by] Penner, E., Johnston, G.H. Goodrich, L. E. . Canadian Geotechnical Journal, Vol. 12, No. 3. 1975, p. 271–88. [At low values of moisture contents, thermal conductivity for seven of the ten soils was less in frozen slate than in unfrozen. This was reversed at higher moisture contents.]CrossRefGoogle Scholar
Remizov, I. N. Kovalev, P. V. Fossil traces of permafrost in the Ukraine and their palcogeographic significance. Biuletyn Peryglacjalny, No. 24, 1975, p, 71. [Summary. Lists points of interest.]Google Scholar
Rowley, R. K., Prediction of pile performance in permafrost under lateral load, [by] Rowley, R.K., Watson, G.H. Ladanyi, B. . Canadian Geotechnical Journal, Vol. 12, No. 4, 1975, p. 510–23. [Describes field tests at Inuvik, N.W.T., and compares predicted and observed pile behaviour.)10.1139/t75-057CrossRefGoogle Scholar
Ryckborst, H. On the origin of pingos. Journal of Hydrology, Vol. 26, Nos. 3-4, 1975, p. 303–14. [Presents uniform theory of formation, in contrast to previous freezing-expansion theories.]10.1016/0022-1694(75)90011-6CrossRefGoogle Scholar
Schunke, E. Frostpaltenmakropolygonc im westlichen Zentral-Island, ihre klimatischen und edaphischen Bedingungen. Eiszeitalter und Gegenwart, Bd. 25, 1975, p. 157–65. [Discusses climatic significance of frost crack macropolygons (diameter 15-35 mm) in vicinity of Hofs- and LangjökuU, west central Iceland.]Google Scholar
Shpolyanskaya, N. A. Prognoz razvitiya vechnoy merzloty Zapadnoy Sibiri v svyazi s vekovymi kolebaniyami klimata [Forecast of development of permafrost in Western Siberia in relation to former climate changes]. Prirodnyye Usloviya Zapadnoy Sibiri, Vyp. 5, 1975, p. 174204.Google Scholar
Slusarchuk, W. A. Watson, G. H. Thermal conductivity of some ice-rich permafrost soils. Canadian Geotechnical Journal, Vol. 12, No. 3, 1975, p. 413–24. [Presents values for thermal conductivity of frozen and thawed ice-rich permafrost soils measured under field and laboratory conditions with a cylindrical heat source.]CrossRefGoogle Scholar
Smith, M. W. Microclimatic influences on ground temperatures and permafrost distribution, Mackenzie Delta, Northwest Territories. Canadian Journal of Earth Sciences, Vol. 12, No. 8, 1975, p. 1421–38. [Demonstrates importance of local seasonal surface factors, such as vegetation and snow cover, on variations in thermal regime of ground.]CrossRefGoogle Scholar
Sukhodrovskiy, V. L. Particularités de l'évolution des versants dans les régions de pcrgclisoi. Biuletyn Peryglacjalny, No. 24, 1975, p. 7380. [Slope formation in periglacial regions.] Tικκανεν, M., and HKIKKINEN. O. Glasiaalikarstin aiheuttamia muotoja Vardoaivilia | Formations produced by karst on Vardoaivi fell, Finnish Lapland], Terra, Vol. 87, No. 2, 1975. p. 95103. [Describes ring ridges, mounds and kettle holes, and discusses mode of formation. English abstract,p. 95.]Google Scholar
Trofimov, V. T. Martynov, A. P. O plyvunnykh i tiksotropnykh svoystvakh pylevatykh porod sloya sezonnogo ottaivaniya poluostrova Yamal [On flow and thixotropic properties of powdered rock of seasonally thawing layers of Poluostrov Yamal]. Prirodnyye Usloviya ^apadnoy Sibiri, Vyp. 5, 1975, p. 263–72.Google Scholar
Trofimov, V. T., Osnovnyye zakonomcrnosti rasprostraneniya, s'troyeniya tolshch i temperatury mnogoletnemerzlykh porod poluostrov Yamal [Basic conformity of distribution, structure of strata and temperature of frozen rocks of Poluostrov YamalJ. [By] Trofimov, V.T. Y Badu, u.B. Varcnyshev, V.B. Kudryashov, V.G. Lur'ye, I. S., Firsov, N.G. Prirodnyye Usloviya Zapadnoy Sibiri, Vyp. 5, 1975, p. 123–73.Google Scholar
Tufnüll, L. Hummocky microrelief in the Moor House area of the northern Pennines, England. Biuletyn Peryglacjalny, No. 24, 1975, p. 353–68. L Periglacial features of thufur type.]Google Scholar
Tyktikov, A. P. Dinamika vechnoy merzloty vblizi yeye yuzhnoy gianitsy v Zapadnoy Sibiri v zvyazi s razvitiyem rastiternosli [Dynamics of permafrost towards its southern limit in Western Siberia in connection with the growth ?Γ vegetation]. Prirodnyye Usloviya Zapadnoy Sibiri, Vyp. 5, 1975, p. 99102.Google Scholar
Vasil'yev, Y. M. Malnikova, M. G. Frost-protective layers made of stabilized soils. Frost i Jord, No. 15, 1975· P· 45 [Cement-treated soils as preventive measure against frost heaving.]Google Scholar
Vvelichko, A. A. Paragenesis of a cryogenic (periglacial) zone. Biuletyn Peryglacjalny, No. 24, 1975, p. 89110. [Discusses formation of periglacial zones, in particular, effect of climate.]Google Scholar
Yevseyev, V. P. K voprosu o zakonomernostyakh rasprostraneniya migratsionnykh bugrov pucheniya na severe Zapadnoy Sibiri i Pechorskoy nizmennosti [On conformity of the distribution of migratory pingos in the north of Western Siberia and the Pechora lowland], Prirodnyye Usloviya Zapadnoy Sibiri, Vyp. 5, 1975, p. 216–27.Google Scholar

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
Graerel, T. E. Franey, J. P. Field measurements of submicron aerosol washout by snow. Geophysical Research Letters, Vol. 2, No. 8, 1975, p. 325–28. [Comparison of results with those previously derived for rain wash-out indicate that snow scavenging is about 28 to 50 times more efficient per equivalent water content.]Google Scholar
Hallett, J. Influence of cloud dynamics on the relationship between ice nucleus measurement and ice crystal concentration. Journal de Recherches Atmosphériques, Vol. 6, Nos. 1-3, 1972, p. 213–21.Google Scholar
Hobbs, P. V. The nature of winter clouds and precipitation in the Cascade Mountains and their modification by artificial seeding. Part I: natural conditions. Journal of Applied Meteorology, Vol. 14, No. 5, 1975, p. 783804. [Includes study of ice and snow particles in clouds and on the ground.]2.0.CO;2>CrossRefGoogle Scholar
Hobbs, P. V. The nature of winter clouds and precipitation in the Cascade Mountains and their modification by artificial seeding. Part III: case studies of the effects of seeding. Journal of Applied Meteorology, Vol. 14, No. 5, 1975,p. 819–58-10.1175/1520-0450(1975)014<0819:TNOWCA>2.0.CO;22.0.CO;2>CrossRefGoogle Scholar
Hobbs, P. V. Rauke, L. F. The nature of winter clouds and precipitation in the Cascade Mountains and their modification by artificial seeding. Part II: techniques for the physical evaluation of seeding. Journal of Applied Meteorology, Vol. 14, No. 5, 1975, p. 805–18.Google Scholar
Hogan, A. W. Klkuch, K. Aerosols and precipitation at the South Pole. Antarctic Journal of the United Mates, Vol. 10, No. 4, 1975, p. 190–91. [Discusses several exceptionally heavy periods of ice crystal precipitation in 1974-7 5; structures of crystals were investigated.].Google Scholar
HöGSTRöm, U. Wet fallout of sulfurous pollutants emitted from a city during rain or snow. Atmospheric Environment, Vol. 8, No. 12, 1974, p. 12911303. [Pollutants deposited in range 50-100 km, mostly as sulphate. Experiment conducted at Uppsala, Sweden.]CrossRefGoogle ScholarPubMed
Kry, P. R. List, R. Aerodynamic torques on rotating oblate spheroids. Physics of Fluids, Vol, 17, No. o, 1974, p. 1087–92. [Measurements of relevance to hail.]10.1063/1.1694847CrossRefGoogle Scholar
Kry, P. R. List, R. Angular motions of freely falling spheroidal hailstone models. Physics of Fluids, Vol. 17, No. 6, 1974, p. 1093–1012. [Theory.]Google Scholar
Morgan, G. M. Towery, N. G. Small-scale variability of hail and its significance lor hail prevention experiments Journal of Applied Meteorology. Vol. 14, No. 5, 1975, p. 763–70. [Studies of small-scale variability of hail.]2.0.CO;2>CrossRefGoogle Scholar
Mossop, S. C. The role of ice nucleus measurements in studies of ice particle formation in natural clouds. Journal de Recherches Atmosphériques, Vol. 6, Nos. 1-3, 197a, p. 377–89.Google Scholar
OIîTAKE, T. Ice crystal precipitation at the South Pole. Antarctic Journal of the UmtedStates, Vol. 10, No. 4. 1975,p. 191. [Preliminary results of studies of atmospheric ice crystals from cloudless skies to understand mechanism of production and influence on climate.]Google Scholar
Oono, N. Sentai-chakuhyô ni kansuru kenkyü. IV. Sentai-chakuhyô-jôken no tôkei-bunsetsu [Studies on ice accumulation on ships. IV. Statistical analysis of ship icing conditions]. Teion-kagaku: Low Temperature Science, Ser. A, [No.] 32, 1974, p. 235–42. [Data collected from fishing vessels during three winters. Results presented and discussed. English summary, p. 241–42.]Google Scholar
Plooster, M. N. Fukuta, N. A numerical model of precipitation from seeded and unseeded cold orographie clouds. Journal of Applied Meteorology, Vol. 14, No. 5, 1975, p. 859–67. [Calculation of rate of precipitation at ground level.]10.1175/1520-0450(1975)014<0859:ANMOPF>2.0.CO;22.0.CO;2>CrossRefGoogle Scholar
Reinking, R. F. Formation ofgraupel. Journal of Applied Meteorology, Vol. 14, No. 5, 1975,p. 745–54- [Measurements of sizes and concentrations of graupel and snow crystals in seeded and untreated winter storms. Mechanism of graupel development discussed.]2.0.CO;2>CrossRefGoogle Scholar
Sawada, T. Nihon kinkai no sentai chakuhyö [Ice accretion on ships in Japanese coastal waters]. Hakodate Kaiyô Kishôdai ïôhô; Bulletin of the Hakodate Marine Observatory, No. 18, | Article No.] 10, 1975, 15 p. [Discusses ice accretion on ships in Japanese coastal waters, methods of forecasting the likelihood of accretion, and future problems.]Google Scholar
Shellard, H. C. The meteorological aspects of ice accretion on ships. Geneva, World Meteorological Organization, 1974. xiv, 34 p. (World Meteorological Organization. Reports on Marine Science Affairs. Report No. 10. (WMO-No. 397.)) [Review.].Google Scholar
Van valin, C. C., Formation of cloud and ice nuclei by the combustion of crude oil, [by] C. C., Van Valin., Pueschel, R.F., Parungo, F.P. Journal of Applied Meteorology, Vol. 14, No. 6, 1975, p. 1200–03. [Order of magnitude increase in ice nuclei in smoke plume from oil-well fire thought to be due to clay minerals.]Google Scholar
Weiss, R. R. Hobbs, P. V. Determination of dominant solid precipitation particle growth processes with a vertically pointing Doppler radar. (In 16th Radar Meteorology Conference. Sponsored by the American Meteorological Society, April SÎ-if, /075, Houston, Texas. Boston, American Meteorological Society, [1975], p. 410–14.) [Measurement of fall speeds used to deduce whether particles are growing from vapour or by riming and to detect effects of cloud seeding.]Google Scholar
Zavarina, M. V. Kopanev, I. D. , erf. Meteorologicheskiye nagruzki na sooruzheniya [Meteorological loading of buildings]. Glavnaya Geofitkheskaya Obsermloriya. Trudy, Vyp. 333, 1974. [136] P- [Sixteen articles on glazed frost and ice deposits.]Google Scholar

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
Akitaya, E. Shamen-sekisetsu no kyodô no kenkyü. HI. Setsujimen de no yuki no ido (guraido) [Studies ol the behaviour of snow cover on mountain slope. III. The movement (glide) of snow in contact with the ground surface]. Teion-kagaku: Low Temperature Science, Ser. A, [No.] 32, 1974, p. 97104. [Describes method of measurement of glide and derives equation. English summary, p. 103–04.]Google Scholar
Beroströ, M. S. The development oiasnow routine for the HBV-2 model. Nordic Hydrology, Vol. o, No. 2, 1975, p. 7392. [Describes development of snow routine for this rainfall-run-off model. Shows application of model to forested basin in central Sweden.]Google Scholar
Cehak, K. Statistische Schneekarten für Österreich. Zbornik Meteoroloikih i Hidroloskih Radova (Beograd), Broj 5, 1974, p. 307–10. [Deals with maps relating to snowfall in Austria.]Google Scholar
De fcreitas, C. R. Estimation of the disruptive impact of snowfalls in urban areas. Journal of Applied Meteorology, Vol. 14, No. 6, 1975, p. 1166–73. [Assesses variable characteristics of snowfalls in terms of their effect on severity of disruption, focusing on five urban areas of Canada.]2.0.CO;2>CrossRefGoogle Scholar
Delsol, F. La prévision des avalanches. Un colloque de Γ????? à Briançon. La Météorologie, Sér. 6, 1975, No. 1, p. 9596. [Colloquy on safety in mountains, held 24 April 1975, included section on forecasting of avalanches.]Google Scholar
Dirmhirn, I. Eaton, F. D, Some characteristics of the albedo of snow. Journal of Applied Meteorology, Vol. 14, No. 3, 1975, p. 375–79. [Discusses effect of the specular component on accuracy of estimations of albedo of large areas.]2.0.CO;2>CrossRefGoogle Scholar
Endö, Y. Akitaya, E. Shamen-sekisetsu no katsudö-jikken (yohö) [Experimental studies on snow gliding]. Teion-kagaku: Low Température Science. Ser. A, [No. ] 32. 1974, p. 267–72. [Observations made on south-facing slopes near Hokkaido.]Google Scholar
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
Huzioka [i.e. FUJIOKA], T. Shamen-sekisetsu no kyodô no kenkyû. IV. Shamen-sekiseisu-nai no ôryoku [Studies of the behaviour of snow cover on mountain slope. IV. Stress in snow cover]. Teion-kagaku: Law Temperature Science, Ser. A, [No.J 32, 1974, p. 105–12. [Calculated on assumption that finite homogeneous strain is exerted on creeping movement of snow. English summary, p. 111–12.]Google Scholar
Itö, T. Kajikawa, M. Akita no gösetsu to seppyö saigai ni kansuru chôsa kenkyû [Investigations on heavy snow and snow disaster in Akita prefecture]. Seppyö, Vol. 37, No. 2, 1975, p. 5566. [Describes regional characteristics of snow events (snow storms, hail storms, frost, avalanches) and presents observations on snow depth in Akita. English summary,p. 66.]Google Scholar
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
Kobayashi, S. Ishida, T. Jifubukiji ni okeru kazc no ranryü. Ill, Hajo setsumen keiseiji no kansoku-rei [On the wind turbulence during drifting snow. III. Example of observation when snow wave is forming], Teion-kagaku: Low Temperature Science, Ser. A, |No.] 32, 1974,p, 8187.. [Observations made on snow wave formed when wind of speed > 7 m/s blew after new snow had accumulated to depth 20 cm. English summary, p. 8687.]Google Scholar
Lauscher, A. Lauscher, F. Die Zeitpunkte grösster Schneehöhe in den Ostalpenländern. Wetter und Üben, Jahrg. 27, Ht. 1-2, 1975, p. 2630. [Relates date of maximum snow depth to height above sea-level in eastern Alps.]Google Scholar
LemmalÄ, R. Kuusisto, E. Evaporation-condensation and snowmclt measurements in Finland. Nordic Hydrology, Vol. 5, No. 1, 1975, p. 6474. [Presents observations made in southern Finland, 1968-73, and discusses results and factors affecting them.]CrossRefGoogle Scholar
Lovie, C. Les bassins du Torrent des Glaciers et du Versoycn; réflexions sur un domaine très propice aux avalanches de neige. Centre Universitaire de Savoie. Centre de Recherches sur la Neige et les Avalanches (Albertville), 1975, LNo.J 1, 37 p. [Discusses geomorphological effects of avalanches in this part of Haute Tarentaise, Savoie, France.]Google Scholar
Mcginnis, D. F. jr., Snew depth and snow extent using VHRR data from the NOAA-2 satellite, by McGinnis, D.F. Jr., Pritchard, J.A., Wiesnet, D.R. Washington, D.C., U.S. Dept. of Commerce. National Oceanic and Atmospheric Administration, National Environmental Satellite Service, 1975. ii, 10 p. (NOAA Technical Memorandum NESS 63.) [Describes testing of hypothesis that the brightness of snow received as reflected radiation by visible-band sensors on satellites is a possible indication of snow depth.]Google Scholar
Martinec, J. Subsurface flow from snowmelt traced by tritium. Water Resources Research, Vol. 11, No. 3, 1975, p, 40,6 gB. [Offers explanation of apparent discrepancy between small velocities of sub-surface (low and watershed response. Environmental tritium in hydrological cycle provides evidence for new insight into runoff mechanism,]CrossRefGoogle Scholar
Meyer, L. Organisation en France des systèmes de prévision du risque d'avalanches. £bornik Meteorolos'kih i Hidroloikik Radova (Beograd), Broj 5, 1974, p. 363–65. [Describes system of forecasting of avalanche risk in France.]Google Scholar
Moskalev, Yu. D. Glyatsiologiya Sredncy Azii. Laviny LGlaciology of Central Asia. Avalanches]. Sredne-aziatskiy Regional'nyy Nauchno-lssUdomteVskiy Gidromeleorologkheskiy institut. Trudy, Vyp. 15(96), 1974, 159 p. [Collected articles on avalanches and protection against them.]Google Scholar
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
Plancher, G. Estimation de la rétention nivale lors des précipitations extrêmes à l'origine des crues dans les bassins versants de haute montagne Zbornik Meteoroloskik i Hidroioskih Radova (Beograd), Broj 5, 1974: p. 345–49. [Deals with risk of floods from heavy snowfalls in high mountains.]Google Scholar
Plas, J. Contribution à l'étude statistique enneigement—avalanches dans les Alpes françaises. Zbornik Meteorolos'kih i Hidroioskih Radova (Beograd), Broj 5, 1974, p. 353–56. [Discusses use of statistical data on snowfall in studying occurrence of avalanches.]Google Scholar
Puhakka, T. On the Z R relationship in snowfall. Geophyska. Vol. 13, No. 2, 1974, p. 121–42. [Measurement of snowfall by radar.]Google Scholar
Regelin, W. L. WallmO, O. C. Carbon black increases snowmelt and forage availability on deer winter range in Colorado. U.S. Dept. aj Agriculture. Forest Service. Research Note RM-296, 1975, 4 p, [Using carbon black on slopes with southern exposure, over 40 cm of snow was melted to bare ground in February when air temperature averaged — 8.8°C during daylight hours. Snow density unaltered.]Google Scholar
Sanak, J. Lorius, C. Geochemistry at the South Pole. Antarctic Journal of the United States, Vol. 10, No. 4, 1975, p. 159-fio. [Outlines work, mainly lead content, on snow samples.]Google Scholar
Shimizu, H., Kurobe-kyökoku kösoku-nadare no kenkyû. Ill [Study of high-speed avalanche in Kurobe canyon. III]. [By] Shimizu., H., Huzioka [i.e. Fujioka]., T., Akitaya, E., Narita, H., Nakagawa, M., Kawada, K. . Teion-kagaku: Low Temperature Science, Ser. A, [No.] 32, 1974, p. 113–27. [Presents conclusions drawn from detailed studies of avalanches in this area of Honshu, Japan. English summary, p. 126–27.]Google Scholar
Solomon, R. M., Snowmelt runoff efficiencies on Arizona watersheds, [by] Solomon, R.M. Ffolliott, P.F. Baker, M.B. Jr., Gottfried, G.J. Thompson, J. R.. University of Arizona. Agricultural Experiment Station. Research Report 274, 1975, [ii], 50 p. [Compares efficiencies for several watersheds in different vegetation zones. Includes study of variables.]Google Scholar
Stfinhäusser, H. Zur Bilanz des unterirdischen Wassers in alpinen Einzugsgebieten. Zbornik Meteorolos'kih i Hidroioskih Radova (Beograd), Broj 5, 1974, p. 367–70. [Includes contribution of melt water from snow and ice to water balance in Alpine basins.]Google Scholar
Vrba, M. Spusta, V. Lavinovy katastr Krkonos [Avalanche survey and map of Krkonosc mountains]. Opera Corcontka (Vrchlabi, Czechoslovakia), 12, 1975, p. 6590. [Presents map and descriptions of avalanche fields situated in Czech territory of this mountain chain. English summary, p. 8689.]Google Scholar
Wakahama, G., Hokkyoku chiiki no sekisctsu chôsa (1973 nen 3 gatsu) [Observations of snow cover in Arctic regions (March 1973)]. [By] Wakahama, G., Akitaya, E., Tabata., T. Teion-kagaku: Low Temperature Science, Ser. A, [No.J 32, 1974, p. 175–84. [Snow cover on sea ice compared with that on lake ice and frozen ground. English summary, p. 183–84.]Google Scholar
Warbukton, J. A., Influence of precipitation-forming mechanisms on the chemistry of the Ross Ice Shelf, [by] Warburton, J. A., Linkletter, G. O., Owens, M.S., Trachte, D, A.. Antarctic Journal of the United States, Vol. 10, No. 4, 1975,p. 147. [Preliminary observations on atmospheric scavenging by snow crystals.]Google Scholar
Weiss, H. V. A review of lead, sulfur, selenium and mercury in permanent snowfields. Berkowitz{in, J.B., ed. Marine electrochemistry, edited by Berkowitz{in, J.B. [and 6 others]. Princeton, N.J., Electrochemical Society, Inc., [CI973], p. 385–99.) [Increases in impurity content of snow in Greenland by up to factor of 500 due to human activity.]Google Scholar
Williams, K. Avalanche fatalities in the United States, 1950-75. U.S. Dept. of Agriculture. Forest Service. Research Note RM-300, 1975, 4 p. [Fatalities are increasing: in past 5 years, average number of deaths was 12 per winter, twice the 25 year average. Mainly holiday-makers.]Google Scholar
Woo, Ming-ko, Laymaker, H. O. Alpine streamflow response to snowpack thickness and extent. Geografiska Annaler, Vol. 57.A, Nos. 3-4, 1975, p. 201–12. [Presents results of investigation of snow melt and melt water discharge in small alpine basin in Coast Mountains, British Columbia, Canada, during spring when contrast between thick and shallow pack was evident.]10.1080/04353676.1975.11879916CrossRefGoogle Scholar
Yamada, T., Daisetsusan-Asahidake no shinringenkai yori kabu no sekisctsu no kansoku [Observation of snow accumulation below the forest line at Asahi-dakc on Mt. Daisetsuj. [By] Yamada, T., Hasemi, T., Izumi, K., Sato, A.. Teion-kagaku: Low Temperature Science, Ser. A, [No.] 32, 1974, p. 273–77.Google Scholar
Yamada, T., Sekisetsu-soshiki no ihösei to danseiha no dcnpan-rendo oyobi netsudendôritsu ni tsuite [On the dependencies of the velocities of P- and S-waves and the thermal conductivity of snow upon the texture of snow]. [By] Yamada, T., Hasemi, T., Izumi, K., Satô, A..Teion-kagaku: Low Temperature Science, Ser. A, [No.] 32, 1974, p. 7180. [Samples of new snow, fine-grained compact snow and depth hoar were examined, using vertical and horizontal sections. English summary, p. 7980.]Google Scholar
Yoshida, T. Sekiyu-zuke roshi ni yori motometa yuki no rёdâ hansha keisû to kôsui kyôdo no kankei [The relation between radar reflectivity and snowfall intensity by kerosene-soaked filter paper method]. Kishöchö Kenkyüjihö: Journal of Meteorological Research, Vol. 27, No. 3, 1975, p. 107–11. [Use of kerosene has eliminated problem of how to prevent snow-flakes breaking upon impact on filler paper. English summary,p. 107.]Google Scholar
Yosida, Z. [i.e, Yoshiua, J.] Purau joselsu no riron. 1. Ryüdö-gata kösoku-purau zen-en keage [Theoretical studies on snow removal by a plough. I. Flow-type kick up of snow caused by a plough moving at high speeds]. Teion-kagaku: Low Temperature Science, Ser. A, [No.] 32, 1974, p. 3953. [Derives formulae for velocity of snow after kick up. English summary, p. 5253.]Google Scholar
Yosida, Z. [i.e. Yoshida, J.] Purau josetsu no riron. II. Hisan-gata kösoku-purau zen-en keage [Theoretical studies on snow removal by a plough. II. Spray-type kick up of snow caused by a plough moving at high speeds]. Teion-kagaku: Low Temperature Science. Ser.A, [No.] 32, 1974. p.5570. [English summarv, p. 6870.]Google Scholar