Cargando…
Ocean-induced melt volume directly paces ice loss from Pine Island Glacier
The spatial distribution of ocean-induced melting beneath buttressing ice shelves is often cited as an important factor controlling Antarctica’s sea-level contribution. Using numerical simulations, we investigate the relative sensitivity of grounded-ice loss to the spatial distribution and overall v...
Autores principales: | Joughin, Ian, Shapero, Daniel, Dutrieux, Pierre, Smith, Ben |
---|---|
Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
American Association for the Advancement of Science
2021
|
Materias: | |
Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8535793/ https://www.ncbi.nlm.nih.gov/pubmed/34678060 http://dx.doi.org/10.1126/sciadv.abi5738 |
Ejemplares similares
-
Ice-shelf retreat drives recent Pine Island Glacier speedup
por: Joughin, Ian, et al.
Publicado: (2021) -
Direct observations of melting, freezing, and ocean circulation in an ice shelf basal crevasse
por: Washam, Peter, et al.
Publicado: (2023) -
Complex motion of Greenland Ice Sheet outlet glaciers with basal temperate ice
por: Law, Robert, et al.
Publicado: (2023) -
Internal tsunamigenesis and ocean mixing driven by glacier calving in Antarctica
por: Meredith, Michael P., et al.
Publicado: (2022) -
Contemporary ice sheet thinning drives subglacial groundwater exfiltration with potential feedbacks on glacier flow
por: Robel, Alexander A., et al.
Publicado: (2023)