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This research evaluates how landscape structure and subaerial taliks influence runoff characteristics of small rivers in continuous permafrost.

Cryogenic Landscapes and Runoff of Small Rivers in the Middle Part of the Lena River Basin, Central Yakutia

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Randomized trial evaluates runoff dynamics in small rivers of permafrost zones, highlighting landscape impact on water supply.

This research evaluates how landscape structure and subaerial taliks influence runoff characteristics of small rivers in continuous permafrost.
Correlation analysis methods were applied alongside experimental study results and standard hydrological observations.
Two small watersheds with differing landscape structures were compared for long-term water balance components.
Pine forests on sandy deposits maintained stable water supply due to non-freezing groundwater reserves.
Low evaporation rates in these landscapes contributed to regulated runoff, largely independent from weather variations.
Taliks replenished by precipitation aided in sustaining water flow throughout various seasons.

Lebedeva et al. (2026) studied this question.

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View Full Paper

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Authors

Randomized trial evaluates runoff dynamics in small rivers of permafrost zones, highlighting landscape impact on water supply.

This research evaluates how landscape structure and subaerial taliks influence runoff characteristics of small rivers in continuous permafrost.
Correlation analysis methods were applied alongside experimental study results and standard hydrological observations.
Two small watersheds with differing landscape structures were compared for long-term water balance components.
Pine forests on sandy deposits maintained stable water supply due to non-freezing groundwater reserves.
Low evaporation rates in these landscapes contributed to regulated runoff, largely independent from weather variations.
Taliks replenished by precipitation aided in sustaining water flow throughout various seasons.

Lebedeva et al. (2026) studied this question.

View Full Paper

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