Thermohaline structure and circulation beneath the Langhovde Glacier ice shelf in East Antarctica

Basal melting of ice shelves is considered to be the principal driver of recent ice mass loss in Antarctica. Nevertheless, in-situ oceanic data covering the extensive areas of a subshelf cavity are sparse. Here we show comprehensive structures of temperature, salinity and current measured in January...

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Detalles Bibliográficos
Autores principales: Minowa, Masahiro, Sugiyama, Shin, Ito, Masato, Yamane, Shiori, Aoki, Shigeru
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2021
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8270922/
https://www.ncbi.nlm.nih.gov/pubmed/34244489
http://dx.doi.org/10.1038/s41467-021-23534-w

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8270922/
https://www.ncbi.nlm.nih.gov/pubmed/34244489
http://dx.doi.org/10.1038/s41467-021-23534-w

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