Gunar A.Yu. 1,3, Koshurnikov A.V.1,2, Balikhin E.I. 1,2, Rosenberg V.V. 2  

THERMOMETRY RESULTS IN THE FIRST WELLS OF THE STATE GEOCRYOLOGICAL MONITORING SYSTEM IN SPITSBERGEN AND NORILSK 

Relief and Quaternary deposits of the Arctic, Subarctic and North-West Russia. Issue 11.

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doi: 10.24412/2687-1092-2024-11-501-506

Лицензия Creative Commons

1LLC MSU-Geophysics, Moscow, Russia

 2 Lomonosov Moscow State University, Moscow, Russia,

3Arctic and Antarctic Research Institute, St. Petersburg, Russia 

 

     

Abstract. The article provides an analysis of the obtained data of thermometric observations in the wells of Barentsburg and Norilsk. In both areas, there is a noticeable increase in the average annual air temperature, but the nature of the thermometric curves for these areas is completely different, which indicates that geocryological conditions can in some cases successfully resist climate warming. The data analysis of the site with a trend for climate warming (Barentsburg) and the site with an agrading layer of permafrost is presented. The article provides an approach to obtaining additional information from the results of temperature observations in monitoring wells.

Keywords: thermometry, climate warming, temperature shift, thermal modeling

 

 


 

 

REFERENCES:

General permafrost studies / edited by Kudryavtsev V.A. M.: Publishing House of Moscow. Unita, 1978. 463 p.

Pesotsky D.G. The influence of the content of unfrozen water in frozen rocks on the formation of their temperature regime: Master's thesis. Funds of the Department of Geocryology. Moscow State University. 2013.

Climate Center of Roshydromet. URL: https://cc.voeikovmgo.ru/ru/klimat/cmip6hr (accessed 11/24/2024).

 

 

Cite this article:

Gunar A.Yu., Koshurnikov A.V., Balikhin E.I., Rosenberg V.V. Thermometry results in the first wells of the State Geocryological monitoring system // Relief and Quaternary deposits of the Arctic, Subarctic and North-West Russia. 2024. Issue 11. P. 501-506. doi: 10.24412/2687-1092-2024-11-501-506

 



 


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