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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University of New South Wales
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ftands:oai:ands.org.au::1957055 2023-05-15T13:38:54+02:00 The penultimate deglaciation: protocol for PMIP4 transient numerical simulations between 140 and 127 ka, version 1.0 Dr Laurie Menviel (hasPrincipalInvestigator) Dr Laurie Menviel (hasCollector) The University of New South Wales (isManagedBy) University of New South Wales (isManagedBy) 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 unknown University of New South Wales https://researchdata.edu.au/the-penultimate-deglaciation-version-10/1957055 http://hdl.handle.net/1959.4/resource/collection/resdatac_874/1 https://doi.org/10.26190/5d0c0c0bd1f26 https://www.unsworks.unsw.edu.au/ 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 dataset ftands https://doi.org/10.26190/5d0c0c0bd1f26 2023-01-30T23:21:52Z 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 Dataset Antarc* Antarctica Greenland Ice Sheet Research Data Australia (Australian National Data Service - ANDS) Greenland |
institution |
Open Polar |
collection |
Research Data Australia (Australian National Data Service - ANDS) |
op_collection_id |
ftands |
language |
unknown |
topic |
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 |
spellingShingle |
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 The penultimate deglaciation: protocol for PMIP4 transient numerical simulations between 140 and 127 ka, version 1.0 |
topic_facet |
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 |
description |
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 |
author2 |
Dr Laurie Menviel (hasPrincipalInvestigator) Dr Laurie Menviel (hasCollector) The University of New South Wales (isManagedBy) University of New South Wales (isManagedBy) |
format |
Dataset |
title |
The penultimate deglaciation: protocol for PMIP4 transient numerical simulations between 140 and 127 ka, version 1.0 |
title_short |
The penultimate deglaciation: protocol for PMIP4 transient numerical simulations between 140 and 127 ka, version 1.0 |
title_full |
The penultimate deglaciation: protocol for PMIP4 transient numerical simulations between 140 and 127 ka, version 1.0 |
title_fullStr |
The penultimate deglaciation: protocol for PMIP4 transient numerical simulations between 140 and 127 ka, version 1.0 |
title_full_unstemmed |
The penultimate deglaciation: protocol for PMIP4 transient numerical simulations between 140 and 127 ka, version 1.0 |
title_sort |
penultimate deglaciation: protocol for pmip4 transient numerical simulations between 140 and 127 ka, version 1.0 |
publisher |
University of New South Wales |
url |
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 |
geographic |
Greenland |
geographic_facet |
Greenland |
genre |
Antarc* Antarctica Greenland Ice Sheet |
genre_facet |
Antarc* Antarctica Greenland Ice Sheet |
op_source |
https://www.unsworks.unsw.edu.au/ |
op_relation |
https://researchdata.edu.au/the-penultimate-deglaciation-version-10/1957055 http://hdl.handle.net/1959.4/resource/collection/resdatac_874/1 https://doi.org/10.26190/5d0c0c0bd1f26 |
op_doi |
https://doi.org/10.26190/5d0c0c0bd1f26 |
_version_ |
1766112297460170752 |