Subglacial brine flow and wind-induced internal waves in Lake Bonney, Antarctica
© Copyright Antarctic Science Ltd 2020. Brine beneath Taylor Glacier has been proposed to enter the proglacial west lobe of Lake Bonney (WLB) as well as from Blood Falls, a surface discharge point at the Taylor Glacier terminus. The brine strongly influences the geochemistry of the water column of W...
Published in: | Antarctic Science |
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Main Authors: | , , , |
Format: | Text |
Language: | unknown |
Published: |
LSU Digital Commons
2020
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Subjects: | |
Online Access: | https://digitalcommons.lsu.edu/geo_pubs/578 https://doi.org/10.1017/S0954102020000036 |