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Current climate change effects on the ground thermal regime in Central Yakutia

Research in Cold and Arid Regions 2014年第4期6卷 282-292页

作者： Stepan Varlamov yuri skachkov Pavel Skryabin Melnikov Permafrost Institute Siberian Branch of the Russian Academy of Sciences

The evolution of ground thermal state has been studied to assess impacts of current climatic warming on permafrost in Central Yakutia. The analysis of long-term data of regional weather stations has revealed one of the highest increasing trends in mean annual air temperature in northern Russia. A forecast of surface air temperature fluctuations has been made by applying a frequency analysis method. Monitoring of ground thermal conditions allows us to identify inter-annual and long-term variability among a wide range of natural conditions. Experimental research has indicated a long-term dynamics of ground thermal state evolution： ground temperatures at the depth of zero annual amplitude and seasonally thawed layer depth. Long-term variability of thaw depth shows near-zero to weak positive trends in small valleys in contrast to weak negative trends on slopes. With significant climatic warming, the thermal state of near-surface layers of permafrost demonstrates steadiness. Anthropogenic impacts on ground thermal regime in various terrain types have been qualitatively evaluated. Clear-cutting, ground cover stripping, and post-fire deforestation in inter-alas type terrains result in a significant increase of temperature and seasonal ground thaw depth, as well as adverse cryogenic processes. The dynamics of mean annual ground temperature in slash and burn sites have been evaluated in reference to stages of successive vegetation recovery.

关键词： permafrost active layer climate ground temperature regime natural landscapes disturbed landscapes

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Temperature monitoring from 2012 to 2019 in central part of Suntar-Khayat Ridge,Russia

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Journal of Mountain Science 2020年第10期17卷 2321-2338页

作者： Robert SYSOLYATIN Sergei SERIKOV Mikhai Yana TIKHONRAVOVA Vladimir ZHIZHIN Maria ROJINA Melnikov Permafrost Institute Yakutsk 677010Russia

In recent decades,research of the Alps,Qinghai-Tibet Plateau,and Cordillera have made great progress in understanding the phenomenon of *** the most part,this has been made possible due to temperature ***,the permafrost parameters in an area of more than 2 million square km of the mountainous regions of northeast Asia,for the most part,remain a blank spot in the scientific *** to the lack and insufficiency of factual materials,in 2012 the *** Permafrost Institute began to take temperature measurements in the upper part of the permafrost in the central part of the VerkhoyanKolyma uplands,namely the Suntar-Khayat *** article describes the temperature characteristics of air,surface and rocks of the active layer in the range of heights from 850 to 1821 m,in various landscape and topographic *** the observation period from 2012 to 2019,we obtained information on temperatures in the soils of the active layer at depths of 1 m,3 m,4 m,and 5 m and also air and surface temperature *** availability of data on automated monitoring of rock temperatures in the active layer and the upper horizons of the layer of annual heat rotations made it possible to substantiate the most typical conditions of the temperature conditions of the permafrost zone of the characterized *** parameters of permafrost existence and development are in favorable *** is shown in the analysis of temperature data of air,surface and active *** temperatures in the active layer of annual heat rotations are most clearly represented at a depth of 1 ***,on the territory of the mountain regions of Eastern Siberia,there are no more such sites for monitoring the temperature regime of *** on the permafrost parameters in the region will allow us to begin the process of creating new models or checking existing forecasts and the distribution of the temperature *** will also make it possible to eval

关键词： Air temperature Ground temperature Climate change Mountain permafrost Active layer thickness

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