Sediment controls dynamic behavior of a Cordilleran Ice Stream at the Last Glacial Maximum

Sediment controls dynamic behavior of a Cordilleran Ice Stream at the Last Glacial Maximum

Tidewater glaciers in fjords can advance/retreat independent of climate due to stabilization by sediments at their termini. We show that an Alaskan paleo-ice stream behaved similarly on an open shelf, suggesting that increased sediment flux may delay catastrophic retreat of outlet glaciers in a warm...

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Autores principales: Ellen A. Cowan, Sarah D. Zellers, Juliane Müller, Maureen H. Walczak, Lindsay L. Worthington, Beth E. Caissie, Wesley A. Clary, John M. Jaeger, Sean P. S. Gulick, Jacob W. Pratt, Alan C. Mix, Stewart J. Fallon
Formato: article
Lenguaje:EN
Publicado: Nature Portfolio 2020
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Acceso en línea:https://doaj.org/article/40ccd9df2c0942419671f27be4935117
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https://doaj.org/article/40ccd9df2c0942419671f27be4935117

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