Geophysical studies were carried out in goal to study the permafrost-hydrogeological conditions of the aufeis
glade (area more than 7 km2
) of the Anmangynda River Basin. For this purpose, the following methods were used:
ground penetrating radar sounding, electrical resistivity tomography, transient electromagnetic method and contactless
measurement of the electric field with grounding through capacitive coupling. The information was obtained on the
characteristics of the aufeis in 2021: the average and maximum thickness of the ice was 1,35 m and 4,35 m, the area and
volume of the aufeis was 3,73 km2 and 3,56 million m3
, respectively. The depth of the seasonal frozen layer was
determined (average 4,5 m, maximum 6 m) and the correlation with the ice thickness was revealed. The geoelectric
signs of large deep taliks and the boundaries of shallow suprapermafrost taliks have been established.