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Comparison of permafrost conditions in Canada and the USSR*

Published online by Cambridge University Press:  27 October 2009

Extract

Canada and the USSR together possess most of the territory in the Northern Hemisphere underlain by permafrost or perennially frozen ground. As about one half of the land area of each country is affected, the permafrost region of the Soviet Union is 2½ times larger than that of Canada. Outside mountainous regions, permafrost extends southward in Canada to the southern tip of James Bay at lat 51° N (Brown, in press). Permafrost extends farther south in eastern Asia, however, and occurs in Outer Mongolia and Manchuria to about lat 47° N Fig 1) (Baranov, 1959; Nekrasov, 1962).

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Articles
Copyright
Copyright © Cambridge University Press 1967

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References

Annersten, L. J. 1964. Investigations of permafrost in the vicinity of Knob Lake 1961–62. In: Bird, J. B., Ed. Permafrost studies in central Labrador-Ungava. McGill Sub-Arctic Research Papers, No 16, p 51137.Google Scholar
Balobayev, T. V. 1966. Usloviya formirovaniya temperatury i moshchnosti mnogoletnemerzlykh gornykh porod [Conditions of the formation of temperature and thickness of permafrost]. Materialy VIII Vsesoyuznogo Soveshchaniya po Geokriologii (Merzlotovedeniyu) [Proceedings of the VIII All-Union Interdepartmental Conference on Geocryology—Permafrost Studies], Vol 8, Yakutsk, p 149–57.Google Scholar
Baranov, I. Ya. 1959. Geograficheskoye rasprostraneniye sezonnopromerzayushchikh pochv i mnogoletnemerzlykh gornykh porod. [Geographical distribution of seasonally frozen ground]. In: Shvetsov, P. F., ed.: Osnovy geokriologii,(Moscow), Tom 1, p 193219. (Translated from the Russian in National Research Council of Canada Technical Translation 1121, 1964.)Google Scholar
Brewer, M. C. 1958. Some results of geothermal investigations of permafrost in northern Alaska. Transactions of the American Geophysical Union, Vol 39, No 1, p 1926.Google Scholar
Brewer, M. C. 1961. Temperature measurement studies, South Barrow Test Well 1; core tests and test wells, Barrow area, Alaska. US Geological Survey Professional Paper 305-K, p 596.Google Scholar
Brown, R. J. E. 1960. The distribution of permafrost and its relation to air temperature in Canada and the USSR. Arctic, Vol 13, No 3, p 163–77.CrossRefGoogle Scholar
Brown, R. J. E. 1965. Some observations on the influence of climate and terrain features on permafrost at Norman Wells, NWT, Canada. Canadian Journal of Earth Sciences, Vol 2, p 1531.CrossRefGoogle Scholar
Brown, R. J. E. 1966 a. Permafrost as an ecological factor in the Subarctic. UNESCO Symposium on the Ecology of Subarctic Regions, Otaniemi (Helsinki), Finland.Google Scholar
Brown, R. J. E. 1966 b. The relation between mean annual air and ground temperatures in the permafrost region of Canada. Proceedings of the International Permafrost Conference, Purdue University, p 241–46.Google Scholar
Brown, R. J. E. (in press). Permafrost map of Canada. Division of Building Research, National Research Council of Canada and Geological Survey of Canada.Google Scholar
Brown, W. G., Johnston, G. H. and Brown, R. J. E. 1964. Comparison of observed and calculated ground temperatures with permafrost distribution under a northern lake. Canadian Geotechnical Journal, Vol 1, No 3, p 147–54.CrossRefGoogle Scholar
Budyko, M. I. 1956. Teplovoy balans zemnoy poverkhnosti [The heat balance of the Earth's surface]. Leningrad: Gidrometeorologicheskoe Izdatel'stvo. (Translated from Russian by Office of Climatology, Washington, DC, 1958.)Google Scholar
Cook, F. A. 1958. Temperatures in permafrost at Resolute, NWT. Geographical Bulletin, No 12, p 518.Google Scholar
Flint, R. F. 1957. Glacial and Pleistocene geology. New York, John Wiley and Sons Inc.Google Scholar
Fraser, J. K. 1956. Physiographic notes on features in the Mackenzie Delta area. Canadian Geographer, No 8, p 1823.Google Scholar
Hemstock, R. A. 1949. Permafrost at Norman Wells, NWT. Calgary, Imperial Oil Ltd.Google Scholar
Hughes, O. L. 1965. Geological Survey of Canada. (Personal communication.)Google Scholar
Hustich, I. 1966. On the forest-tundra and the northern tree-lines. In: Reports from the Kevo Subarctic Research Station, 3. Annales Universitatis Turkuensis, Series A, II, 36, p 747.Google Scholar
Katasonov, Ye. M. 1961. Merzloto-fatsial'nyy analiz kak metod izucheniya mnogoletnemerzlykh chetvertichnykh otlozheniy [Frozen ground facies analysis as a method of studying pe rennially frozen Quaternary deposits]. Report of the Vlth International Congress on Quaternary Research, Warsaw, Vol IV, p 103–09.Google Scholar
Katasonov, Ye. M. 1966. Institut Merzlotovedeniya, Sibirskoye Otdeleniye AN SSSR [Permafrost Institute, Siberian Division, Academy of Sciences of the USSR], Yakutsk (personal communication).Google Scholar
Legget, R. F., Brown, R. J. E. and Johnston, G. H. 1966. Alluvial fan formation near Aklavik, Northwest Territories, Canada. Bulletin of the Geological Society of America, Vol 77, p 1530.CrossRefGoogle Scholar
Mel'nikov, P. I. 1959. O zakonomernostyakh rasprostraneniya i razvitiya merzlykh pochv i gornykh porod v basseyne r. Leny [Mechanisms of distribution and development of frozen soil and rock in the Lena river basin]. VII Mezhduvedomstvennoye Soveshchaniye po Merzlotovedeniyu [VII Interdepartmental Permafrost Conference]. Izdatel'stvo Akademii Nauk SSSR, p 91102.Google Scholar
Misener, A. D. 1955. Heat flow and depth of permafrost at Resolute Bay, Cornwallis Island, NWT, Canada. Transactions of the American Geophysical Union, Vol 36, No 6, p 1055–60.Google Scholar
Nekrasov, I. A. 1962. Geokriologiya—nauka o merzlykh tolshchakh zemli [Geocryology— science of the frozen masses of the Earth]. Priroda, No 2, p 1926.Google Scholar
Shumskiy, P. A. 1964. Principles of structural glaciology. New York, Dover Publications Inc. (Translated from the Russian by David Kraus.)Google Scholar
Solov'yev, P. A. 1962. Alasnyy rel'yef tsentral'noy Yakutii i yego proiskhozhdeniye [Alas relief in central Yakutia and its origin]. In: Grave, N. A., ed.: Mnogoletnemerzlyye porody i soputstvuyushchiye im yavleniya na territorii Yakutskoy ASSR. Moscow, p 3853.Google Scholar
Solov'yev, P. A. 1963. Alasnyye doliny Yakutii [Alas valleys of Yakutia]. In: Katasonov, Ye. M., ed.: Usloviya i osobennosti razvitiya merzlykh tolshch v Sibiri i na Severo-Vostoke. Moscow, p 8090.Google Scholar
Sumgin, M. I., Kachurin, S. P., Tolstikhin, N. I. and Tumel', V. F. 1940. Obshcheye merzlotovedeniye [General permafrost studies]. Moscow.Google Scholar
Tikhomirov, B. A. 1958. Nekotoryye voprosy dinamiki poverkhnostnykh obrazovaniy Arktiki v svyazi s genezisom bugrov-baydzharakhov [Problems concerning the dynamics of Arctic surface features in connection with the genesis of cemetery mounds]. Reprint from Problemy Fizicheskoy Geografii, p 285312.Google Scholar
Tolstikhin, O. N. 1965. O vliyanii noveyshey tektoniki na formirovaniye i raspredeleniye naledey v severo-vostochnoy Yakutii [Influence of recent tectonic activity on nalyed formation and distribution in northeastern Yakutia]. Geologiya i Geofizika (Novosibirsk), No 9, p 75–83.Google Scholar
Tolstikhin, O. N. 1966. O nekotorykh lineynykh zonakh formirovaniya naledey na territorii severo-vostochnoy Yakutii [Lineation of nalyed formation zones in northeastern Yakutia]. Materialy VIII Vsesoyuznogo Soveshchaniya po Geokriologii (Merzlotovedeniyu) [Proceedings of the VIII All-Union Interdepartmental Conference on Geocryology— Permafrost Studies], Vol 3, Yakutsk, p 218–25.Google Scholar