Yu M Polishchuk
Biographic Data
| ID | 7991911 |
|---|---|
| NAME | Yu M Polishchuk |
| GIVEN NAMES | Yu M |
| FAMILY NAME | Polishchuk |
| SIGNATURE | POLISHCHUK Y M |
| AFFILIATIONS | Yugra State University |
| ORCID | 0000-0002-4944-4919 |
| VERIFIED | Yes |
| TOTAL WORKS | 3 |
| TOTAL CITATIONS | 0 |
| WORKS AS AUTHOR | 3 |
| WORKS AS EDITOR | 0 |
| FIRST PUBLICATION YEAR | 2008 |
| LATEST PUBLICATION YEAR | 2018 |
| H-INDEX | 0 |
Minor contribution of small thaw ponds to the pools of carbon and methane in the inland waters of the permafrost-affected part of the Western Siberian Lowland
Despite the potential importance of small (< 1000 m ^2 ) thaw ponds and thermokarst lakes in greenhouse gas (GHG) emissions from inland waters of high latitude and boreal regions, these features have not been fully inventoried and the volume of GHG and carbon in thermokarst lakes remains poorly constrained. This is especially true for the vast Western Siberia Lowland (WSL) which is subject to strong thermokarst activity. We assessed the number of…
Abrupt changes of thermokarst lakes in Western Siberia
Peatlands situated in a permafrost zone and consisting of thin layers of frozen peat, especially palsas in the sub‐arctic region of Western Siberia, are a very sensitive indicator of climatic changes, such that any changes of climate in the direction of warming lead to increased activity in a thermokarst process over extensive areas. Thermokarst lakes as an invariable element of the palsa mire complex are the most convenient object for distant mo…
One of the possible mechanisms of thermokarst lakes drainage in West‐Siberian North
During the 2008 expedition carried out within the framework of the Russian–French network project CAR‐WET‐SIB, one of the possible mechanisms of drainage of thermokarst lakes in the north of Western Siberia was revealed. The discovered natural process is significantly amplified by climate warming and gains special urgency in this regard
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One of the possible mechanisms of thermokarst lakes drainage in West‐Siberian North
During the 2008 expedition carried out within the framework of the Russian–French network project CAR‐WET‐SIB, one of the possible mechanisms of drainage of thermokarst lakes in the north of Western Siberia was revealed. The discovered natural process is significantly amplified by climate warming and gains special urgency in this regard
Abrupt changes of thermokarst lakes in Western Siberia
Peatlands situated in a permafrost zone and consisting of thin layers of frozen peat, especially palsas in the sub‐arctic region of Western Siberia, are a very sensitive indicator of climatic changes, such that any changes of climate in the direction of warming lead to increased activity in a thermokarst process over extensive areas. Thermokarst lakes as an invariable element of the palsa mire complex are the most convenient object for distant mo…
Minor contribution of small thaw ponds to the pools of carbon and methane in the inland waters of the permafrost-affected part of the Western Siberian Lowland
Despite the potential importance of small (< 1000 m ^2 ) thaw ponds and thermokarst lakes in greenhouse gas (GHG) emissions from inland waters of high latitude and boreal regions, these features have not been fully inventoried and the volume of GHG and carbon in thermokarst lakes remains poorly constrained. This is especially true for the vast Western Siberia Lowland (WSL) which is subject to strong thermokarst activity. We assessed the number of…
Climate change and permafrost (3 works) · Cryospheric studies and observations (3 works) · Ecology (3 works) · Environmental Science (3 works) · Geography (3 works) · Geology (3 works) · Oceanography (3 works) · Permafrost (3 works) · Physical geography (3 works) · Thermokarst (3 works)