Spatial variations in the geochemistry of glacial meltwater streams in the Taylor Valley, Antarctica

Abstract Streams in the McMurdo Dry Valleys, Antarctica, flow during the summer melt season (4–12 weeks) when air temperatures are close to the freezing point of water. Because of the low precipitation rates, streams originate from glacial meltwater and flow to closed-basin lakes on the valley floor...

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Bibliographic Details
Published in:Antarctic Science
Main Authors: Welch, Kathleen A., Lyons, W. Berry, Whisner, Carla, Gardner, Christopher B., Gooseff, Michael N., McKnight, Diane M., Priscu, John C.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 2010
Subjects:
Online Access:http://dx.doi.org/10.1017/s0954102010000702
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0954102010000702