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Impact of abrupt sea ice loss on Greenland water isotopes during the last glacial period

Greenland ice cores provide excellent evidence of past abrupt climate changes. However, there is no universally accepted theory of how and why these Dansgaard–Oeschger (DO) events occur. Several mechanisms have been proposed to explain DO events, including sea ice, ice shelf buildup, ice sheets, atm...

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Detalles Bibliográficos
Autores principales: Sime, Louise C., Hopcroft, Peter O., Rhodes, Rachael H.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: National Academy of Sciences 2019
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6410777/
https://www.ncbi.nlm.nih.gov/pubmed/30760586
http://dx.doi.org/10.1073/pnas.1807261116