Relating ocean temperatures to frontal ablation rates at Svalbard tidewater glaciers: Insights from glacier proximal datasets

Fjord-terminating glaciers in Svalbard lose mass through submarine melt and calving (collectively: frontal ablation), and surface melt. With the recently observed Atlantification of water masses in the Barents Sea, warmer waters enter these fjords and may reach glacier fronts, where their role in ac...

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Detalles Bibliográficos
Autores principales: Holmes, Felicity A., Kirchner, Nina, Kuttenkeuler, Jakob, Krützfeldt, Jari, Noormets, Riko
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2019
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6603002/
https://www.ncbi.nlm.nih.gov/pubmed/31263126
http://dx.doi.org/10.1038/s41598-019-45077-3

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6603002/
https://www.ncbi.nlm.nih.gov/pubmed/31263126
http://dx.doi.org/10.1038/s41598-019-45077-3

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