The penultimate deglaciation: protocol for PMIP4 transient numerical simulations between 140 and 127 ka, version 1.0

• Other Authors: Dr Laurie Menviel (hasPrincipalInvestigator), Dr Laurie Menviel (hasCollector), The University of New South Wales (isManagedBy), University of New South Wales (isManagedBy)
• Format: Dataset
• Language: unknown
• Published: University of New South Wales
• Subjects: paleoclimate; PMIP4; deglaciation; ice-sheet; Palaeoclimatology; EARTH SCIENCES; PHYSICAL GEOGRAPHY AND ENVIRONMENTAL GEOSCIENCE; Chemical Oceanography; OCEANOGRAPHY; Climate Change Processes; ATMOSPHERIC SCIENCES; Climate Variability (excl. Social Impacts); ENVIRONMENT; CLIMATE AND CLIMATE CHANGE; Expanding Knowledge in the Earth Sciences; EXPANDING KNOWLEDGE; Physical and Chemical Conditions of Water in Marine Environments; PHYSICAL AND CHEMICAL CONDITIONS OF WATER; Greenland; Antarc*; Antarctica; Ice Sheet
• Online Access: https://doi.org/10.26190/5d0c0c0bd1f26; https://researchdata.edu.au/the-penultimate-deglaciation-version-10/1957055; http://hdl.handle.net/1959.4/resource/collection/resdatac_874/1

Continental ice-sheets and meltwater forcing necessary to perform transient simulations of the penultimate deglaciation. TopoIcem-140-122k.nc gives the combined ice-sheet forcing (North America, Eurasia, Greenland, and Antarctica) over the period 140ka to 122ka, needed to perform the simulations nh_abe2013_01.nc gives the Northern Hemisphere ice-sheet evolution over the period 140ka to 120ka from Abe Ouchi et al., 2013. T2-fwfFlux.txt gives the meltwater input scenarios