- Climate change and permafrost
- Geological Studies and Exploration
- Methane Hydrates and Related Phenomena
- Paleontology and Stratigraphy of Fossils
- Arctic and Antarctic ice dynamics
- Geology and Paleoclimatology Research
- Ionosphere and magnetosphere dynamics
- Mining and Gasification Technologies
- Earthquake Detection and Analysis
- Geotechnical and Geomechanical Engineering
- Cryospheric studies and observations
- Coal and Coke Industries Research
- Engineering and Environmental Studies
- Marine and environmental studies
Earth Cryosphere Institute
2019-2024
Permafrost is a key element of the cryosphere and an essential climate variable in Global Climate Observing System. There no remote-sensing method available to reliably monitor permafrost thermal state. To estimate distribution at hemispheric scale, we employ equilibrium state model for temperature top (TTOP model) 2000–2016 period, driven by remotely-sensed land surface temperatures, down-scaled ERA-Interim reanalysis data, tundra wetness classes landcover map from ESA Landcover Change...
Monitoring of the thickness active layer within lake-marsh type terrain in northern taiga was carried out at three sites organized 1997, 2013 and 2022. In these areas, two types tracts are distinguished: frozen peat bogs swampy runoff hollows with a lowered roof permafrost (the cross-section is same type, only difference peat). The work methodology complied unified protocol international CALM program. Additionally, surface settlement assessed (based on leveling from local benchmark),...