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Sediment transport drives tidewater glacier periodicity

Most of Earth’s glaciers are retreating, but some tidewater glaciers are advancing despite increasing temperatures and contrary to their neighbors. This can be explained by the coupling of ice and sediment dynamics: a shoal forms at the glacier terminus, reducing ice discharge and causing advance to...

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Detalles Bibliográficos
Autores principales: Brinkerhoff, Douglas, Truffer, Martin, Aschwanden, Andy
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2017
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5522421/
https://www.ncbi.nlm.nih.gov/pubmed/28733603
http://dx.doi.org/10.1038/s41467-017-00095-5