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Barotropic seiches in a perennially ice‐covered lake, East Antarctica

Abstract Water movement in ice‐covered lakes is known to be driven by wind, sediment heat flux, solar radiation, saline density flows, and advective stream discharge. In large ice‐covered lakes, wind‐induced oscillations have been found to play a major role in horizontal flows. Here, we report recur...

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Principais autores: Devin N. Castendyk, Hilary A. Dugan, Hugh A. Gallagher, Nimish Pujara, Peter T. Doran, John C. Priscu, W. Berry Lyons
Formato: Artigo
Idioma:Inglês
Publicado em: Wiley 2022-02-01
coleção:Limnology and Oceanography Letters
Acesso em linha:https://doi.org/10.1002/lol2.10226
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