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.

Bibliographic Details
Main Authors: de Boer, Bas, Haywood, Alan M, Dolan, Aisling M, Hunter, Stephen J, Prescott, Caroline L
Format: Dataset
Language:English
Published: PANGAEA 2017
Subjects:
Ice Sheet
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.882047
https://doi.org/10.1594/PANGAEA.882047
Description
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.

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