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Impact of Climate Change on the Ground Thermal Regime in the Lower Lena Region, Arctic Central Siberia

Author

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  • Pavel Konstantinov

    (Permafrost Landscapes Laboratory, Melnikov Permafrost Institute of the Siberian Branch of the RAS, 677010 Yakutsk, Russia
    Laboratory for Integrated Research of the Arctic Land-Shelf System, Tomsk State University, 634050 Tomsk, Russia)

  • Nikolai Basharin

    (Permafrost Landscapes Laboratory, Melnikov Permafrost Institute of the Siberian Branch of the RAS, 677010 Yakutsk, Russia
    Laboratory for Integrated Research of the Arctic Land-Shelf System, Tomsk State University, 634050 Tomsk, Russia)

  • Alexander Fedorov

    (Permafrost Landscapes Laboratory, Melnikov Permafrost Institute of the Siberian Branch of the RAS, 677010 Yakutsk, Russia)

  • Yoshihiro Iijima

    (Graduate School of Bioresources, Mie University, 1577 Kurimamachiya-cho, Tsu 514-8507, Japan)

  • Varvara Andreeva

    (Permafrost Landscapes Laboratory, Melnikov Permafrost Institute of the Siberian Branch of the RAS, 677010 Yakutsk, Russia
    Laboratory for Integrated Research of the Arctic Land-Shelf System, Tomsk State University, 634050 Tomsk, Russia)

  • Valerii Semenov

    (Permafrost Landscapes Laboratory, Melnikov Permafrost Institute of the Siberian Branch of the RAS, 677010 Yakutsk, Russia
    Laboratory for Integrated Research of the Arctic Land-Shelf System, Tomsk State University, 634050 Tomsk, Russia)

  • Nikolai Vasiliev

    (Permafrost Landscapes Laboratory, Melnikov Permafrost Institute of the Siberian Branch of the RAS, 677010 Yakutsk, Russia
    Laboratory for Integrated Research of the Arctic Land-Shelf System, Tomsk State University, 634050 Tomsk, Russia)

Abstract

This paper presents the results of 30 years of permafrost thermal monitoring in the Tiksi area in the eastern Russian Arctic. At a stone ridge site, the mean annual temperatures in the upper 30 m of the ground have increased by 1–2.4 °C compared to the first years of observations, with trends of °C/yr. At the same time, its change was uneven. In the last 20 years, the rate of increase has increased compared with the first decade of observations. At wet tundra sites in the foothill plain, the mean annual temperatures at the top of permafrost have increased by 2.4–2.6 °C between 2005 and 2022 at rates of 0.11–0.15 °C/yr, and the active layer thicknesses have increased at rates of 0.05–0.41 cm/yr.

Suggested Citation

  • Pavel Konstantinov & Nikolai Basharin & Alexander Fedorov & Yoshihiro Iijima & Varvara Andreeva & Valerii Semenov & Nikolai Vasiliev, 2022. "Impact of Climate Change on the Ground Thermal Regime in the Lower Lena Region, Arctic Central Siberia," Land, MDPI, vol. 12(1), pages 1-13, December.
    • Handle: RePEc:gam:jlands:v:12:y:2022:i:1:p:19-:d:1010202
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    References listed on IDEAS

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