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Palsas are peat mounds with a permanently frozen peat and mineral soil core. They are a typical phenomenon in the polar and subpolar zone of discontinuous permafrost. One of their characteristics is having steep slopes that rise above the mire surface. This leads to the accumulation of large amounts of snow around them. The summits of the palsas are free…
Effects of climate change, Geographic distribution & Morphology
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palsas peat core mires pingos climate area permafrost layer ice several however change forms snow frozen surface temperature species water
| Subject | Predicate | Object | Confidence | Src |
|---|---|---|---|---|
| Palsa | is a | normal part of the cyclic development and | 0.90 | text |
| to preserve the newly formed permafrost.The overlying soil layer is gradually lifted up by frost heaving | instance of | Changes in surface moisture and vegetation will then be | 0.80 | text |
| a few following cold winters | instance of | can develop as a result of smaller variations in climatic conditions | 0.80 | text |
| Palsa | has effect | This | 0.60 | section |
| Palsa | has effect | European Union | 0.60 | section |
| Palsa | has effect | Although | 0.60 | section |
| Palsa | has effect | In | 0.60 | section |
| Palsa | has effect | It | 0.60 | section |
| Palsa | has effect | Without | 0.60 | section |
| Palsa | has effect | Northern Europe | 0.60 | section |
| Palsa | has effect | North European | 0.60 | section |
| Palsa | has effect | Finland | 0.60 | section |
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