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Part of the book series: NATO Science Series ((ASEN2,volume 76))

Abstract

Probability of global climate wanning due to accumulation of greenhouse gases (dioxide carbon, methan et al.) in atmosphere is a problem of interest for mankind during last decades. [4, 18, 19, 22]. In case of climate warming forecasts realization one can expect significant changes in surface earth systems. Warming will inevitably result in corresponding response of permafrost which will begin to warm and melt. This will in turn cause irreversible landscape alternations, weakening of mechanical properties of superficial rocks, aggravation of all problems concerning reliability and stability of engineering structures. Investigation of the evolution of the temperature field in frozen rocks is becoming a topical problem in such situation.

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References

  1. Balobaev, V.T., Pavlov, A.V., Perlshtein, G.Z. et al. (1983) Thermophysical investigations of Siberian permafrost, Nauka, Novosibirsk, 214 p. (In Russian).

    Google Scholar 

  2. Balobaev, V.T. (1991) Geothermy of frozen zone of lithosphere of North Asia, Nauka, Novosibirsk, 194 p. (In Russian).

    Google Scholar 

  3. Balobaev, V.T. (1997) Global changes of climate and permafrost, Science and education, 2, p. 82–90 (In Russian).

    Google Scholar 

  4. Budyko, M.I. (1980) Climate in past andfuture, Hydrometeoizdat, Leningrad, 351 p. (In Russian).

    Google Scholar 

  5. Budyko, M.I., Ronov, A.B., Yanshin, A.L. (1985) History of atmosphere, Hydrometeoizdat, Leningrad, 209 p. (In Russian).

    Google Scholar 

  6. Devyatkin, V.N. (1993) Heat flow of Siberian permafrost, Nauka, Novosibirsk, 165 p. (In Russian).

    Google Scholar 

  7. Devyatkin, V.N. and An, V.V. (1994) Experimental confirmation of temperature increasing of lithosphere’s upper layer in West Siberia, in Borehole temperatures and climate change, Report of International Workshop, Geophysical Institute, Praha, p. 87–93.

    Google Scholar 

  8. Devyatkin, and An, V.V. (1998) On the relationship between thermal flows in frozen and underlying unfrozen rocks in the lithosphere of Sakha-Yakutia, Cryosphere of Earth, 1, p. 28–31 (In Russian).

    Google Scholar 

  9. Dorofeeva, R.P., Lysak, S.V., Duchkov, A.D. (1995) Terrestrial heat flow in Siberia and Mongolia, in Yamano, M. and Gupta, M. (eds.), Terrestrial heat flow and geothermal energy in Asia, M/S Oxford and IBH Publichers, New Delhi, pp. 251–279.

    Google Scholar 

  10. Duchkov, A.D., Lysak, S.V., Balobaev V.T. et al. (1987) Heat field in interior of Siberia, Nauka, Novosibirsk, 196 p.

    Google Scholar 

  11. Duchkov, A.D. (1991) Review of Siberian heat flow data, in V. Cermak and L. Rybach (eds.), Terrestrial heat flow and the lithosphere structure, Springer Verlag, Berlin, pp. 426–443.

    Chapter  Google Scholar 

  12. Duchkov, A.D., Balobaev, V.T., Volod’ko B.V. et al. (1994) Temperature, permafrost and radiogenic heat production in the Earth’ s crust of Northern Asia, UIGGM, Novosibirsk, 141 p. (In Russian).

    Google Scholar 

  13. Duchkov, A.D., Balobaev, V.T., Devyatkin, V.N. et al. (1995) Geothermal model of the West-Siberian permafrost, Russian Geology and Geophysics, 8, p. 69–79.

    Google Scholar 

  14. Duchkov, A.D., Sokolova, L.S., Balobaev, V.T. et al. (1997) Heat flow and geothermal field of Siberia, Russian Geology and Geophysics, 11, p. 1716–1729.

    Google Scholar 

  15. Ershov, E.D. (ed.) (1996) Geocryology map of former USSR, Moscow State University, Moscow (In Russian).

    Google Scholar 

  16. Ershov, E.D. (ed.) (1989) Geocryology of USSR: West Siberia, Nedra, Moscow, 454 p. (In Russian).

    Google Scholar 

  17. Ershov, E.D. (ed.) (1989) Geocryology of USSR: Middle Siberia, Nedra, Moscow, 414 p. (In Russian).

    Google Scholar 

  18. Gruz, G.V. and Khmelevtsova, S.S. (eds.) (1981) Ehergy and climate, Hydrometeoizdat, Leningrag, 304 p. (in Russian).

    Google Scholar 

  19. Hansen, J.E., Russel, G., Ring, D. et al. (1983) Efficient three-dimensional global models for climatic studies: models I and II, Monthly Weather Rev., 111, 609–622.

    Article  Google Scholar 

  20. Kondratieva, I.A., Khurutzky, S.F. and Romanovsky, N.N. (1993) Changes in the extent of permafrost during the late Qurternary period in the territory of the former Soviet Union, Permafrost and periglacial processes, 4, 113–119.

    Article  Google Scholar 

  21. Klyashtorin, L.B. (1998) Long-term climate change and main commercial fish production in the Atlantic and Pacific, Ficheries Research, 754, 1–11.

    Google Scholar 

  22. Manabe, S. and Wetherald, R.T. (1975) The effect of doubling the CO2 concentration on the climate of a general circulation model, J. Atmos. Sci, 32, 3–15.

    Article  CAS  Google Scholar 

  23. Melnikov, P.I., Kamenskii, R.M. and Pavlov, A.V. (1993) Monitoring of permafrost, Bulletin of RAS, p. 1090–1095 (In Russian).

    Google Scholar 

  24. Mitchell, J.F.B, Manabe, S, Meleshko, V., and Tokioka, T. (1990) Equilibrium climate changes and its implications for the future, Climate change: The JPCC Sei. Assess. Report of working group I of the Intergovernmental panel on climate change, Cambridge Univ. press, N.-Y., p. 131–172.

    Google Scholar 

  25. Pavlov, A.V. (1997) Permafrost-climatic monitoring of Russia: methodology, results of observation and forecast, Cryosphere of Earth, 1, p. 47–58 (In Russian).

    Google Scholar 

  26. Rusakov, V.G., and Egorov, A.S. (1996) Temperature monitoring of upper layer of permafrost, in Influence of climate on frozen landshafts in Central Yakutia. Publ. House of Permafrost Institute SB RAS, Yakutsk, p. 57–67 (In Russian).

    Google Scholar 

  27. Skorbilin, N.A. (1994) Dynamics of air temperature regime by meteorological data in West Siberia, in Borehole temperatures and climate change. Report of International Workshop, Geophysical Institute, Praha, p. 95–99.

    Google Scholar 

  28. Skorbilin, N.A. (1997) About the tendency in evolution of the seasonally frozen ground zone of West Siberia for the nearest decades, Cryosphere of Earth, 1, p. 66–68 (In Russian).

    Google Scholar 

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© 2001 Springer Science+Business Media Dordrecht

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Duchkov, A.D., Balobaev, V.T. (2001). Geothermal studies of permafrost response to global natural changes. In: Paepe, R., Melnikov, V.P., Van Overloop, E., Gorokhov, V.D. (eds) Permafrost Response on Economic Development, Environmental Security and Natural Resources. NATO Science Series, vol 76. Springer, Dordrecht. https://doi.org/10.1007/978-94-010-0684-2_21

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  • DOI: https://doi.org/10.1007/978-94-010-0684-2_21

  • Publisher Name: Springer, Dordrecht

  • Print ISBN: 978-0-7923-6784-0

  • Online ISBN: 978-94-010-0684-2

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