Rapidly-migrating and internally-generated knickpoints can control submarine channel evolution
The authors analyse 9 years of time-lapse surveys in Bute Inlet, British Columbia (CA), to show how an active submarine channel evolves. They show how channel evolution is controlled by fast upstream-migration of steep knickpoints, which are similar to waterfalls in rivers.
Guardado en:
Autores principales: | Maarten S. Heijnen, Michael A. Clare, Matthieu J. B. Cartigny, Peter J. Talling, Sophie Hage, D. Gwyn Lintern, Cooper Stacey, Daniel R. Parsons, Stephen M. Simmons, Ye Chen, Esther J. Sumner, Justin K. Dix, John E. Hughes Clarke |
---|---|
Formato: | article |
Lenguaje: | EN |
Publicado: |
Nature Portfolio
2020
|
Materias: | |
Acceso en línea: | https://doaj.org/article/ec7a423e3da249999882ceea1e6cfb11 |
Etiquetas: |
Agregar Etiqueta
Sin Etiquetas, Sea el primero en etiquetar este registro!
|
Ejemplares similares
-
Author Correction: Rapidly-migrating and internally-generated knickpoints can control submarine channel evolution
por: Maarten S. Heijnen, et al.
Publicado: (2020) -
Morphodynamics of submarine channel inception revealed by new experimental approach
por: Jan de Leeuw, et al.
Publicado: (2016) -
New flow relaxation mechanism explains scour fields at the end of submarine channels
por: F. Pohl, et al.
Publicado: (2019) -
Reconstructing the sediment concentration of a giant submarine gravity flow
por: Christopher John Stevenson, et al.
Publicado: (2018) -
Anatomy of subcritical submarine flows with a lutocline and an intermediate destruction layer
por: Jorge S. Salinas, et al.
Publicado: (2021)