Simulations of ice volume across the late Pliocene (approx. 3.5 to 3 Myr ago) ...
The transient ice-sheet predictions are forced by multiple climate snapshots derived from a climate model set up with Late Pliocene boundary conditions, forced with different orbital forcing scenarios appropriate to two Marine Isotope Stages (MIS), MIS KM5c and K1. ... : Supplement to: de Boer, Bas;...
| Main Authors: | , , , , |
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| Format: | Dataset |
| Language: | English |
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PANGAEA
2017
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| Subjects: | |
| Online Access: | https://dx.doi.org/10.1594/pangaea.882047 https://doi.pangaea.de/10.1594/PANGAEA.882047 |
| Summary: | The transient ice-sheet predictions are forced by multiple climate snapshots derived from a climate model set up with Late Pliocene boundary conditions, forced with different orbital forcing scenarios appropriate to two Marine Isotope Stages (MIS), MIS KM5c and K1. ... : Supplement to: de Boer, Bas; Haywood, Alan M; Dolan, Aisling M; Hunter, Stephen J; Prescott, Caroline L (2017): The transient response of ice volume to orbital forcing during the warm Late Pliocene. Geophysical Research Letters ... |
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