Determining long time‐scale hyporheic zone flow paths in Antarctic streams

Abstract In the McMurdo Dry Valleys of Antarctica, glaciers are the source of meltwater during the austral summer, and the streams and adjacent hyporheic zones constitute the entire physical watershed; there are no hillslope processes in these systems. Hyporheic zones can extend several metres from...

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Bibliographic Details
Published in:Hydrological Processes
Main Authors: Gooseff, Michael N., McKnight, Diane M., Runkel, Robert L., Vaughn, Bruce H.
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2003
Subjects:
Online Access:http://dx.doi.org/10.1002/hyp.1210
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fhyp.1210
https://onlinelibrary.wiley.com/doi/pdf/10.1002/hyp.1210