THE IMPACT OF CLIMATE CHANGE AND FLUCTUATIONS IN THE DEPTH OF SEASONAL THAWING ON THE WATER BALANCE OF SMALL RIVERS OF THE PERMAFROST ZONE OF THE NORTH-EAST OF RUSSIA

* — page under construction


Observational data

Anadyrsky district of Chukotka Autonomous Okrug

Monitoring of ice content of the seasonally thawed layer
  1. Ice content of the seasonally thawed layer (sampled may-June 2018: Kazachka river valley, stream Promyslovy);
  2. Ice content of the seasonally thawed layer (sampled may-June 2019: Kazachka river valley, stream Promyslovy);
  3. Ice content of the seasonally thawed layer (sampled may-June 2020: Kazachka river valley, stream Promyslovy).
Materials of permafrost-hydrometric survey
  1. The depth of seasonal thawing and humidity of the seasonal thaw layer of the Ugolnaya-Dionisia river basin (July 2019);
  2. Flow, temperature, mineralization and pH reaction of water of 2-3 orders of magnitude in the basin of the Ugolnaya-Dionysiya river (July 2019).
Monitoring of the runoff of an supra permafrost aquifer
  1. The Plot Is Right Dionysius;
  2. The plot of stream Yagodny
  3. The plot of stream Shumny
Monitoring the temperature and humidity of the seasonally thawed layer
  1. The Plot Is Right Dionysius;
  2. The plot of stream Yagodny
  3. The plot of stream Shumny

Hydrology and hydrometry river basin Ugolnaya-Dionysiya

  1. Platform Dionysy
  2. Platform Kruglaya
  3. Platform Onemen (Rogozhny)

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