Can Deep Groundwater Influx be Detected from the Geochemistry of Thermokarst Lakes in Arctic Alaska?
In the continuous permafrost zone, unfrozen ground may exist beneath large lakes and streams. Sub‐lake taliks that extend through permafrost provide a potential conduit for subpermafrost groundwater to reach the surface, increasing dissolved ion concentrations in lake water. Twenty‐eight lakes on th...
Published in: | Permafrost and Periglacial Processes |
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Main Authors: | , , , |
Format: | Article in Journal/Newspaper |
Language: | unknown |
Subjects: | |
Online Access: | https://doi.org/10.1002/ppp.1895 |