Sub-aerial talik formation observed across the discontinuous permafrost zone of Alaska
Talik formation has long been acknowledged as an important mechanism of permafrost degradation. Currently, a lack of in situ observations has left a critical gap in our understanding of how ongoing climate change may influence future sub-aerial talik formation in areas unaffected by water bodies or...
| Published in: | Nature geoscience Vol. 15, № 6. P. 475-481 |
|---|---|
| Other Authors: | Farquharson, Louise M., Romanovsky, Vladimir E., Kholodov, Alexander, Nicolsky, Dmitry |
| Format: | Article |
| Language: | English |
| Subjects: | |
| Online Access: | http://vital.lib.tsu.ru/vital/access/manager/Repository/koha:001001121 |
Similar Items
- Organic and organo-mineral colloids in discontinuous permafrost zone
- Thermokarst lake waters across the permafrost zones of western Siberia
- Seasonal dynamics of organic carbon and metals in thermokarst lakes from the discontinuous permafrost zone of western Siberia
- Biogeochemistry of organic carbon, CO2, CH4, and trace elements in thermokarst water bodies in discontinuous permafrost zones of Western Siberia
- Trace element transport in western Siberian rivers across a permafrost gradient
