Water tracks intensify surface energy and mass exchange in the Antarctic McMurdo Dry Valleys

The hydrologic cycle in the Antarctic McMurdo Dry Valleys (MDV) is mainly controlled by surface energy balance. Water tracks are channel-shaped high-moisture zones in the active layer of permafrost soils and are important solute and water pathways in the MDV. We evaluated the hypothesis that water t...

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Bibliographic Details
Published in:The Cryosphere
Main Authors: T. Linhardt, J. S. Levy, C. K. Thomas
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2019
Subjects:
geo
Ice
Online Access:https://doi.org/10.5194/tc-13-2203-2019
https://www.the-cryosphere.net/13/2203/2019/tc-13-2203-2019.pdf
https://doaj.org/article/d5bde354031c478ea3267ae8a23d81b6