Cargando…
A new global ice sheet reconstruction for the past 80 000 years
The evolution of past global ice sheets is highly uncertain. One example is the missing ice problem during the Last Glacial Maximum (LGM, 26 000-19 000 years before present) – an apparent 8-28 m discrepancy between far-field sea level indicators and modelled sea level from ice sheet reconstructions....
Autores principales: | Gowan, Evan J., Zhang, Xu, Khosravi, Sara, Rovere, Alessio, Stocchi, Paolo, Hughes, Anna L. C., Gyllencreutz, Richard, Mangerud, Jan, Svendsen, John-Inge, Lohmann, Gerrit |
---|---|
Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
Nature Publishing Group UK
2021
|
Materias: | |
Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7902671/ https://www.ncbi.nlm.nih.gov/pubmed/33623046 http://dx.doi.org/10.1038/s41467-021-21469-w |
Ejemplares similares
-
Reply to: Towards solving the missing ice problem and the importance of rigorous model data comparisons
por: Gowan, Evan J., et al.
Publicado: (2022) -
Impact of paleoclimate on present and future evolution of the Greenland Ice Sheet
por: Yang, Hu, et al.
Publicado: (2022) -
The silicon cycle impacted by past ice sheets
por: Hawkings, Jon R., et al.
Publicado: (2018) -
Reconciling glacial Antarctic water stable isotopes with ice sheet topography and the isotopic paleothermometer
por: Werner, Martin, et al.
Publicado: (2018) -
Past continental shelf evolution increased Antarctic ice sheet sensitivity to climatic conditions
por: Colleoni, Florence, et al.
Publicado: (2018)