Ice-stream demise dynamically conditioned by trough shape and bed strength

Ice sheet mass loss is currently dominated by fast-flowing glaciers (ice streams) terminating in the ocean as ice shelves and resting on beds below sea level. The factors controlling ice-stream flow and retreat over longer time scales (>100 years), especially the role of three-dimensional bed sha...

Popoln opis

Shranjeno v:
Bibliografske podrobnosti
izdano v:Sci Adv
Main Authors: Bradwell, Tom, Small, David, Fabel, Derek, Smedley, Rachel K., Clark, Chris D., Saher, Margot H., Callard, S. Louise, Chiverrell, Richard C., Dove, Dayton, Moreton, Steven G., Roberts, David H., Duller, Geoff A. T., Ó Cofaigh, Colm
Format: Artigo
Jezik:Inglês
Izdano: American Association for the Advancement of Science 2019
Teme:
Research Articles
Online dostop:https://ncbi.nlm.nih.gov/pmc/articles/PMC6498188/
https://ncbi.nlm.nih.gov/pubmed/31058217
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1126/sciadv.aau1380
Oznake: Označite
Brez oznak, prvi označite!

Podobne knjige/članki