Contrasting the Penultimate Glacial Maximum and the Last Glacial Maximum (140 and 21 ka) using coupled climate–ice sheet modelling

<p>The configuration of the Northern Hemisphere ice sheets during the Penultimate Glacial Maximum differed to the Last Glacial Maximum. However, the reasons for this are not yet fully understood. These differences likely contributed to the varied deglaciation pathways experienced following the glaci...

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Autori principali:	V. L. Patterson, L. J. Gregoire, R. F. Ivanovic, N. Gandy, J. Owen, R. S. Smith, O. G. Pollard, L. C. Astfalck, P. J. Valdes
Natura:	Artigo
Lingua:	Inglês
Pubblicazione:	Copernicus Publications 2024-10-01
Serie:	Climate of the Past
Accesso online:	https://cp.copernicus.org/articles/20/2191/2024/cp-20-2191-2024.pdf
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