Hostname: page-component-586b7cd67f-rcrh6 Total loading time: 0 Render date: 2024-11-22T06:12:21.940Z Has data issue: false hasContentIssue false
  • English
  • Français

Glaciological Literature

Published online by Cambridge University Press:  30 January 2017

Rights & Permissions [Opens in a new window]

Abstract

An abstract is not available for this content. As you have access to this content, full HTML content is provided on this page. A PDF of this content is also available in through the ‘Save PDF’ action button.
Type
Other
Information
Journal of Glaciology , Volume 1 , Issue 7 , 1950 , pp. 400 - 402
Copyright
Copyright © International Glaciological Society 1950

This bi-annual list of glaciological literature aims to cover the scientific aspects of snow and ice in all parts of the world. Attention is drawn to the bibliographies in each number of The Polar Record (Cambridge), which aim to cover the significant work dealing with expeditions, research, equipment and conditions of living in the Polar regions. Both journals, however, deal with Polar literature having specific glaciological interest and with general matters of a practical nature such as snowcraft.

Readers will greatly assist the Editor by notifying him of their own, or any other, publication of glaciological interest.

References

Ahlmann, Hans W:Son. Contribution of Polar expeditions to the science of glaciology. Polar Record, Vol. 5, Nos. 37, 38, 1949, p. 324–31.Google Scholar
Bartell, M. J. The relation of runoff to precipitation in the Sierra Nevada, California. Transactions American Geophysical Union, Vol. 30, No. 1, 1949, p. 89–97. [Method for estimating the amount of delayed runoff due to accumulated snow on a drainage area. Discusses precipitation-runoff relationship.]Google Scholar
Beracsaon, Tor. Nyare rön om nederbördens uppkumst och fördelning. Ymer, 69 Årg., Häfte 3, 1949, p. 161−88. [Advances in physics and geographical distribution of precipitation. English summary.]Google Scholar
Beniield, A. E. The effect of uplift and denudation on underground temperatures. Journal of Applied Physics, Vol. 20, No. 1. 1949, p. 66–70. [Uplift and denudation may increase heat flow from the earth by disturbing underground temperature gradient.]CrossRefGoogle Scholar
Brooks, C. E. P. The “end” of the Ice Age. Weather, Vol. 4, No. 9, 1949, p. 304. [Letter. End of latest glacial episode not a definite point of time.]Google Scholar
Brown, Andrew H. Sno-cats mechanize Oregon snow survey. National Geographic Magazine, Vol. 96, No. 4, 1949. p. 691–710, illus., map. [Journey in Tucker Sno-Cats, joint project of U.S. Soil Conservation Service and the Oregon Agricultural Experiment Station, along the crest of the Oregon Cascade Range, March-April 1948.]Google Scholar
Bryan, Kirk. Geologic implications of cryopedology. Journal of Geology, Vol. 97, No. 2, 1949, p. 101–04. [Introduction to Vol. 57, No. 2, devoted entirely to the study of Arctic phenomena and to the interpretation of similar phenomena when found in temperate regions.]CrossRefGoogle Scholar
Cailleux, Andre Thellier, Émile. Sur la détermination de la couche de sol gelé. Comptes Rendus Hebdomadaires des Séances de l’Académie des Sciences (Paris), Tome 224, 1947, p. 1174–75. [Describes a “cryopedometer,” a simple instrument for measuring the depth of frost in the ground.]Google Scholar
Christian, Francis G. The use of snow-surveys as an aid in flood-control operation of reservoirs. Transactions American Geophysical Union, 1944, Part 1, p. 155–65, diagrs. [Discussion of “The use of snow-surveys as an aid in flood-control operation of reservoirs,” by Fred Paget, Transactions American Geophysical Union, 1943, Part 3, p. 28–38; comments by L. Standish Hall and Ray K. Linsley, p. 160−65.]Google Scholar
Court., Arnold. Meteorological data for Little America III. Tabular and graphical results of observations made at the west base of the United States Antarctic Service Expedition of 1939–41. Monthly Weather Review, Supplement No. 48, 1949, 150 pages. [Includes snow observations and sub-surface temperatures by F. A. Wade.]Google Scholar
Ekhart, E. Die Niederschlagsverteilung in den Alpen nach dem Anornalienprinzip. Geografiska Annaler, Årg. 30. Haft. 3–4, 1948, P. 728–39. [Critical examination of the distribution of precipitation in the Alps with the aid of the principle of anomalies.]Google Scholar
Emery, K. O. Topography and sediments of the Arctic basin. Journal of Geology, Vol. 57, No 5, 1949, p. 512–21. [Includes note on distribution of Pleistocene glaciers; map of Arctic ice boundaries.]Google Scholar
Fraser, D. Production of ice-crystal clouds by seeding. Nature, Vol. 164, No. 4161, 1949, p. 179–80. [Note from the Flight Research Section, National Research Council, Ottawa; discusses limitations of the process.]CrossRefGoogle Scholar
Garstka, Walter U. Interpretation of snow surveys. Transactions American Geophysical Union, Vol. 30, No. 3, 1949, p. 412–20. [Method for forecast of seasonal water yield based on snow-survey data.]Google Scholar
[Glacier Research.] Glacier research. Connections with climate, minerals and metals. Science To-day, Vol. 6, No. 151, 1949, p. 301–03. [Summary of recent research.]Google Scholar
Gripp, Karl. Glazialmorphologie und geologische Kartierung. Zeitschrift der Deutschen Geologischen Gesellsrhaft, Bd. 99, 1947 (1949), p. 190–205. [Criticism of geological maps of east Holstein on the basis of glaciomorphology.]Google Scholar
Honda, Kotaro. Formation of frozen rain-drops and the condition of ice-crusted trees. Nature, Vol. 164, No. 4161, 1949, p. 180. [Pressure of ice in frozen rain-drops and on ice-encrusted trees keeps internal water liquid.]CrossRefGoogle Scholar
Jenness, John L. Permafrost in Canada. Origin and distribution of permanently frozen ground with special reference to Canada. Arctic. Journal Arctic Institute of North America, Vol. 2, No. 1, 1949, p. 13–27, illus., maps, diagrs.Google Scholar
Kanavinš, Edvigs. Eisverh[illnine in Osteuropa und die angewandten Massnahmen zur Beeinflussung der Eisbildung und des Eisganges in der Düna (Daugava). Riga, Verlag der Generaldirektion der Technik und des Verkehrs, 1944. 40 pages, illus., diagrs. [Investigation of ice conditions in the Daugava during the winters 1941–42 and 1942–43; discusses influence of general ice conditions in the eastern Baltic.]Google Scholar
Kinzl, Hans. Die Vergletscherung in der Südhalfte der Cordillera Blanca (Peru). Zeitschrift für Gletscherkunde und Glazialgeologie (Vienna), Bd. 1, Ht. 1, 1949, p. 1–28. [Glaciation in the southern sector of the Cordillera Blanca; with stereo-photogrammetric map 1: 100,000.]Google Scholar
Klæboe, H. Hydrological conditions in Norway. Norsk Geografisk Tidsskrift, Bind 12, Hefte 1, 1948, p. 21−31. [Lecturr at the congress of the International Union of Geodesy and Geophysics at Oslo, 1948.]Google Scholar
Klebelsberg, R. Von. Alpengletscher jetzt und einst. Berge und Heimat (Oesterreichischer Alpenverein), Jahrg. 3. Heft 7, 1948, p. 172–5. [Traces extent of alpine glacierization in recent times.]Google Scholar
Klebelsberg, R. Von. Spuren eiszeitlicher Lokalvergletscherung in den Luganer Bergen (Südschweiz). Zeitschrift für Gletscherkunde und Glazialgeologie (Vienna), Bd, 1, Ht. 1, 1949, p. 79–83. [Traces of local Pleistocene glaciation in the Lugano district.]Google Scholar
Klein, S. Restzeugen alter Vereisungen auf der oberbayerischen Hochebene westlich München. Zeitschrift für Gletscherkunde und Glazialgeologie, Bd. 1, Ht. 1, 1949, p. 74–78. [Evidences of glaciation in the Bavarian highlands west of Munich.]Google Scholar
Kohler, M. A. Linsley, R. K. Recent developments in water supply forecasting from precipitation. Transactions American Geophysical Union, Vol. 30, No. 3, 1949, p. 427–36. [Details of methods developed by U.S. Weather Bureau in its programme of water supply forecasting.]Google Scholar
Krintzsky, E. L. Origin of pimple mounds. American Journal of Science, Vol. 247, No. 10, 1949, p. 706–14. [Remains of dunes and hillocks formed under a variety of conditions including glacial outwash.]Google Scholar
Lavrova, M. A. Osnovnye etapy chetvertichnoy istorii Kol’skogo poluostrova lzvestiya Vsesoyuznogo Geograficheskogo Obshchestva (Moscow, Leningrad), Tom 79, No. 1, 1947, p. 21–38. [Study of last two glaciations and interglacial period between them, based mainly on data obtained since 1935. Copy in Foreign Office Research Department, London.]Google Scholar
Lehmann, H. Periglaziale Züge im Formenschatz der Veluwe. Erdkunde, Bd. 2, Lfg. 1/3, 1948, p. 69–79, maps. [Examination of unsolved geomorphological problems in the Veluwe area of Holland, with reference to its periglacial position in the Pleistocene glaciation.]CrossRefGoogle Scholar
Lehmann, H. Über Periglaziale Erscheinungen in der Ümgebung von Bonn. Erdkunde, Bd. 2, Lfg. 1/3, 1948, p. 186–90, illus. [Examination of periglacial features in the Bonn area, Germany.]Google Scholar
Lundqvist, G. Norrlands jordarter. Sveriges Geologiska Undersókning, Avhandlingar och Uppsatser, Ser. C, No. 457, Årsbok 37, No. 6, 1943, 166 pages, illus., maps, tables, diagrs. [The Quaternary deposits of Norrland, north and central Sweden.]Google Scholar
Lundqvist, G. Dubbla moranen i Boliden. Sverige: Geologiska Undersókning, Avhandlingar och Uppsatser, Ser. C, No. 471, Årsbok 39, 1945, 10 pages, illus., diagrs. [The “double moraine” in glacial deposits at Boliden, north Sweden; author holds that the upper “moraine” was formed when water flowed in and out of a lagoon there.]Google Scholar
Manley, Gordon. Fanaråken: the mountain station in Norway. Weather, Vol. 4, No. 11, 1949, p. 352–54 [Meteorological data including precipitation and temperature, the latter in comparison with Ben Nevis.]Google Scholar
Miller, Maynard Malcolm. Progress report of the Juneau Ice Field research project 1948. New York, American Geographical Society, 1949. [vi], 108 p., illus., maps. [Alaska. Includes account of glaciological and meteorological research and recommendations for future work.]Google Scholar
Morawetz, Siechard. Die Postglaziale Wärmezeit und die Vergletscherung der zentralen Ostalpen. Zeitschrift fiar Gletscherkunde und Glazialgeologie (Vienna), Bd. 1, Ht. 1, 1949, p. 63–69. [Post-glacial climatic amelioration and the glaciation of the central Eastern Alps.]Google Scholar
Murri, Carlo Alfredo. Variabilité del sole e periodi di glaciazione. Il Polo (Macerata), Anno 4, 1948, p. 1–3.Google Scholar
Östman, C. J. Den svåra isvintern 1939–1940. Statens Meteorologisk-Hydrografiska Anstalt, Meddelanden, Serien Uppsatser, No. 33, 1940, 25 p., illus., maps. [Survey of ice conditions on Swedish coasts during the cold winter 1939–40. ice thickness in different harbours; photographs of ice formations; English summary.]Google Scholar
Östman, C. J. Isvintem 1940–41. En jämförelse med 1939–40. Statens Meteorologisk-Hydrografska Anstalt, Meddelanden, Serien Uppsatser, No. 38, 1941, 10 p. [Comparison of cold winters 1940–41 and 1939–40; maps of ice conditions in the Baltic; English summary.]Google Scholar
Paschinger, V. Profiländerungen der Pasterze (Glocknergruppe) 1848–1942. Zeitschrift für Gletscherkunde und Glazialgeologie (Vienna), Bd. 1, Ht. 1, 1949, p. 39–55. [Profile changes on the Pasterzenkees.]Google Scholar
Paschincer, V. Die Firnrnoräne der Pasterze. Zeitschrift für Gletscherkunde rind Glazialgeologie (Vienna), Bd. 1, Ht. 1, 1949, p. 56–62.Google Scholar
Poser, Hans. Boden- und Klimaverhältnisse in Mittel- und Westeuropa während der Wurmeiszeit. Erdkunde, Bd. 2, Lfg. 1/3, 1948, p. 53–68, maps, tables. [Abridged version of author’s studies of permanently frozen soil in west and central Europe during the Würm glaciation, with a view to reconstructing climate.]Google Scholar
Renaud, André. Nos glaciers. Neuchâtel, Delachaux et Niestlé, [1947], 44 pages. (Cahiers d’enseignement pratique, 48.) [Instructional monograph on Swiss glaciers.]Google Scholar
Richmond, Gerald M. Stone nets, stone stripes, and soil stripes in the Wind River Mountains, Wyoming. Journal of Geology, Vol. 57, No. 2, 1949. p. 143–53. [Considers that most of the stone stripes result from solifluction acting on stone nets.]CrossRefGoogle Scholar
Richter, Hans. Photograrnmeter in Arktis und Antarktis. Polarforschung, Jahrg. 15, Heft 1/2, 1945, p. 1–5. [Technique of photogrammetric surveys.]Google Scholar
Rikhter, G. D. Snezhny pokrov, yego formirovanie i svoystva. [Snow cover, its formation and properties.] Moscow, Leningrad, Izdatel’stvo Akademii Nauk SSSR [Publishing House of the Academy of Sciences of the U.S.S.R.], 1945. 120 p., maps, tables, diagrs., 22 cm. [Formation of snow cover, its physical properties, influence on visibility, drifting action and thawing; features of snow cover in U.S.S.R. by regions.]Google Scholar
Rogstad, Olaf. Breenes virkning på den nyttbare vannmengde ved kraftverkene i Glåma. Norsk Geografxsk Tidsskrift, Bind 12, Hefte 1, 1948, p. 9–20. [The influence of glaciers on the water supply to power plants in Glåma.]Google Scholar
[Sea Ice.] Merkblatt für die Eiserkundung durch Flugzeuge. Ausgabe für Nordsee, Ostsee und Schwarzes Meer. Bearbeitet von der Deutschen Seewarte. Berlin, Oberkommando der Kriegsmarine, 1942. 25 pages, illus., 21 cm. (Nr. 2199). [Well-illustrated description of forms of ice in North Sea, Baltic, and Black Sea for aircraft reconnaissance.]Google Scholar
[Sea Ice.] Radar detection of floating ice. 1946 ice season. U.S. Coast Guard Bulletin, No. 32, 1947, p. 178–88. [Brief account of experiments on radar detection of floating ice, 1944–45; results of work, 1945–46; experiments with airborne radar.]Google Scholar
Simojoki, Heikki. Über den Zeitpunkt des Entstehens und des Verschwindens der dauernden Schneedecke in Finnland. Fennia, 70, No. 3, 1947, 31 pages, maps, tables, diagrs. [On the time of appearance and disappearance of snow cover in Finland.]Google Scholar
Smith, H. T. U. Periglacial features in the driftless area of southern Wisconsin. Journal of Geology, Vol. 57, No. 2, 1949, p. 196–215.CrossRefGoogle Scholar
Stefansson, Vilhjaimur. Bibliography of Arctic books. Explorers Journal, Vol. 26, No. 1, 1947–48, p. 15–16,23–24, 30; No. 2, 1948, p. 13–15; Nos. 3&4, 1948, p. 46–48. [Reprintedd from Shelesnyak, M. C. Across the top of the world. A discussion of the Arctic. Washington, D.C., Office of Naval Research, 1947. p. 49–71.]Google Scholar
Streiff-Becker, R. Der Bächfirn. Die Alpen, Bd. 25, No. 7, 1949, p. 264–66. [This area in lee of prevailing winds collects snow therefrom and is described as a “Windgletscher.”]Google Scholar
Troll, Carl. Der Subnivale oder periglaziale Zyklus der Denudation. Erdkunde, Band 2, Lief. 1/3, 1948, p. 1–21. [Discusses soil frost formations and solifluction processes.]Google Scholar
Troll, Carl. Schmelzung und Verdunstung von Eis und Schnee in ihrem Verhältnis zur geographischen Verbreitung der Ablationsformen. Erdkunde, Band 3, Lief. 1, 1949, p. 18–29. [Brings up to date the author’s previous work on ablation and ablation forma.]Google Scholar
Varbschi, Volkmar. Der grosse Aletsch. Berge und Heimat (Oesterreichischer Alpenverein), Jahrg. 3, Heft 7, 1948, p. 188–92, maps. [General and glaciological description.]Google Scholar
Wallén, Carl Christian. Glacial-meteorological investigations on the Krirsa Glacier in Swedish Lappland 1942–1948. Geografiska Annoter, Årg. 30, Haft. 3–4, 1948, p. 451–672, illus., maps, tables, diagrs. [Kärsajökel. Meteorological conditions, accumulation, ablation, heat-balance at glacier surface, dependence of ablation on different meteorological factors.]Google Scholar
Wegener, Kurt. Die Ursachen der Abtragung (Ablation) der Gletscher. Zeitschrift für Gletscherkunde und Glazialgeologie (Vienna), Bd. 1, Ht. 1, 1949, p. 71–74. [Causes of glacial ablation.]Google Scholar
Wennberg, Gunnar. Tifferentialoirelser i inlandsisen. Sista istiden i Danmark, Skåne och Östersjön. Lund, 1949. 201+46 p., illus. [Variations in limits of ice sheet over Skåne, Denmark, and the Baltic Sea during Pleistocene glaciation.]Google Scholar
Wood, Walter A. Project “Snow comice.” The establishment of the Seward glacial research station. Arctic. Journal Arctic Institute of North America, Vol. 1, No. 2, 1948, p. 107–12, illus. [Describes glaciological and meteorological programmes and other scientific studies. The area of operations is the drainage basin of the Seward Glacier.]Google Scholar
Wundt, W. Relieftheorie, Niederschlagstheorie und Theorie der kosmischen Nebel als Erklärung für die Entstehung der Eiszeiten. Meteorologische Zeitschrift, Bd. 60, Heft 8, 1943, p. 274 – 81. [Examination of origin of Pleistocene glaciation with reference to the theories of pre-glacial land uplift, of precipitation and its connection with temperature change and a review of difficulties arising from the theory of cosmic obscuration.]Google Scholar