Antarctic ice sheet discharge driven by atmosphere-ocean feedbacks at the Last Glacial Termination

Reconstructing the dynamic response of the Antarctic ice sheets to warming during the Last Glacial Termination (LGT; 18,000–11,650 yrs ago) allows us to disentangle ice-climate feedbacks that are key to improving future projections. Whilst the sequence of events during this period is reasonably well...

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Bibliografiset tiedot
Julkaisussa:Sci Rep
Päätekijät: Fogwill, C. J., Turney, C. S. M., Golledge, N. R., Etheridge, D. M., Rubino, M., Thornton, D. P., Baker, A., Woodward, J., Winter, K., van Ommen, T. D., Moy, A. D., Curran, M. A. J., Davies, S. M., Weber, M. E., Bird, M. I., Munksgaard, N. C., Menviel, L., Rootes, C. M., Ellis, B., Millman, H., Vohra, J., Rivera, A., Cooper, A.
Aineistotyyppi: Artigo
Kieli:Inglês
Julkaistu: Nature Publishing Group 2017
Aiheet:
Article
Linkit:https://ncbi.nlm.nih.gov/pmc/articles/PMC5215443/
https://ncbi.nlm.nih.gov/pubmed/28054598
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/srep39979
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