Holocene reconfiguration and readvance of the East Antarctic Ice Sheet
Ice sheets are vulnerable to changes in the environment where ice discharges into the ocean. Here, the authors show that, in spite of widespread retreat following the last glacial maximum, a sub-sector of the East Antarctic Ice Sheet in the Ross Sea underwent sustained readvance.
Guardado en:
Autores principales: | Sarah L. Greenwood, Lauren M. Simkins, Anna Ruth W. Halberstadt, Lindsay O. Prothro, John B. Anderson |
---|---|
Formato: | article |
Lenguaje: | EN |
Publicado: |
Nature Portfolio
2018
|
Materias: | |
Acceso en línea: | https://doaj.org/article/c3b4133e9c9c4c2495f408d757060cfe |
Etiquetas: |
Agregar Etiqueta
Sin Etiquetas, Sea el primero en etiquetar este registro!
|
Ejemplares similares
-
Mid-Holocene pulse of thinning in the Weddell Sea sector of the West Antarctic ice sheet
por: Andrew S. Hein, et al.
Publicado: (2016) -
Windblown Pliocene diatoms and East Antarctic Ice Sheet retreat
por: Reed P. Scherer, et al.
Publicado: (2016) -
The paradigm shift in Antarctic ice sheet modelling
por: Frank Pattyn
Publicado: (2018) -
The prescience of paleoclimatology and the future of the Antarctic ice sheet
por: Eric J. Steig, et al.
Publicado: (2018) -
Solid Earth change and the evolution of the Antarctic Ice Sheet
por: Pippa L. Whitehouse, et al.
Publicado: (2019)