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- W2184670384 abstract "Long-term studies of vegetation and permafrost have been carried out in northern Siberia since 1962. Stationary plots were established both in natural and disturbed environments. The observations covered natural zones ranging from typical tundra to northern taiga. However, the longest series of observations was for northern taiga. These investigations have documented the influence of vegetation removal and its recovery after disruption on active layer thickness, soil temperature and moisture, and cryogenic processes. On the basis of the characteristics of vegetation recovery, the cryogenic geosystems (Melnikov, 1988) may be divided into three categories with different geocryological conditions. The first category embraces geosystems with the most rapid recovery of vegetation and minimal changes in permafrost. The second category encompasses geosystems with a slow rate of vegetation recovery and larger changes in permafrost. The third category embraces geosystems with an incompletely restored vegetation and the greatest changes in permafrost." @default.
- W2184670384 created "2016-06-24" @default.
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- W2184670384 date "1998-01-01" @default.
- W2184670384 modified "2023-09-27" @default.
- W2184670384 title "IMPACT OF VEGETATION REMOVAL AND ITS RECOVERY AFTER DISTURBANCE ON PERMAFROST" @default.
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