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- W87336321 abstract "Periglacial environments were dominated by aeolian processes periodically in the past but under present-day periglacial conditions, although contributing to local landscape development, are not as widespread. Wind speed, duration, efficiency in sediment transport, and sublimation mean that aeolian activity can take place even where substrates have high moisture contents or are frozen. Active layer processes and the hydrological regimes of rivers can act to replenish sediment availability. As a result, aeolian processes can lead, in addition to landscape elements common to other aeolian environments, to some more distinct to periglacial environments (e.g., elongated thaw lakes, glacier nourishment, and niveo-aeolian deposits)." @default.
- W87336321 created "2016-06-24" @default.
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- W87336321 date "2013-01-01" @default.
- W87336321 modified "2023-10-18" @default.
- W87336321 title "8.25 Aeolian Processes in Periglacial Environments" @default.
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- W87336321 doi "https://doi.org/10.1016/b978-0-12-374739-6.00219-0" @default.
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