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The monitoring and prediction of permafrost temperature, distribution and geocryological processes within russia under global climate changes

  • Glaciers, Permafrost, Porous Media
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Advances in Cold-Region Thermal Engineering and Sciences

Part of the book series: Lecture Notes in Physics ((LNP,volume 533))

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Abstract

The recent changes of climate and permafrost conditions are studied on the basis of the data of northern meteorological and permafrost stations located in various regions of Russia.

Everywhere on Russian territory a warming of the Climate and the upper part of the Permafrost was observed since the middle of 1960s. The Permafrost Monitoring data indicate an increase of the permafrost temperature for the last 15–20 years up to 2–1.5 °C in 3 m depth and up to 1 °C in 10 m depth. The probable increase of the temperature of the upper part of the permafrost of Western Siberia will amount to about 1 °C by 2020, and 1.5–2 °C by 2050.

Calculations (up to the year 2025) and small scale map-schemes of predicted permafrost thawing, distribution and changes of cryogenic cracking of the soils within Russia under a global climate warming were carried out. Predictions were done for peaty, clayey and sandy types. The zones of degrading and stable permafrost for different stow types and areas of decreasing frost soil cracking are identified within the territory of Russia.

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Kolumban Hutter Yongqi Wang Hans Beer

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© 1999 Springer-Verlag

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Pavlov, A., Grechishchev, S. (1999). The monitoring and prediction of permafrost temperature, distribution and geocryological processes within russia under global climate changes. In: Hutter, K., Wang, Y., Beer, H. (eds) Advances in Cold-Region Thermal Engineering and Sciences. Lecture Notes in Physics, vol 533. Springer, Berlin, Heidelberg. https://doi.org/10.1007/BFb0104207

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  • DOI: https://doi.org/10.1007/BFb0104207

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  • Publisher Name: Springer, Berlin, Heidelberg

  • Print ISBN: 978-3-540-66333-1

  • Online ISBN: 978-3-540-48410-3

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