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...

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Bibliographic Details
Published in:Antarctic Science
Main Authors: Lawrence, Jade P., Doran, Peter T., Winslow, Luke A., Priscu, John C.
Format: Text
Language:unknown
Published: LSU Digital Commons 2020
Subjects:
Online Access:https://digitalcommons.lsu.edu/geo_pubs/578
https://doi.org/10.1017/S0954102020000036