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

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_...

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Bibliographic Details
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
Description
Summary: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

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