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• W1676070361 abstract "Western Siberia is a large region with mostly flat relief, that lead to the formation of a multitude of interconnected natural objects large and small rivers streams, large floodplains, lakes, bogs etc. . Flooded areas and bogs also act as a buffer zone, providing a dampening sponge effect on the water redistribution within the river system. Large area covered by rivers and wetlands results in high rate of evaporation compared to any other large boreal watershed. Two contrasting processes are actually occurring in the Southern and Northern parts of the region. In the south, there is a progressive swamping which leads to forest death. In the north, there is a thermokarst activity or thawing permafrost in palsas of sub-arctic zone of Western Siberia." @default.
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• W1676070361 date "2010-05-01" @default.
• W1676070361 modified "2023-09-26" @default.
• W1676070361 title "Seasonal and interannual changes of hydrological regime of the Western Siberia" @default.
• W1676070361 hasPublicationYear "2010" @default.
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