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
Main Authors: Menviel, Laurie, Capron, Emilie, Tarasov, Lev, Abe-Ouchi, Ayako
Format: Dataset
Language:unknown
Published: UNSW Sydney 2019
Subjects:
paleoclimate
PMIP4
deglaciation
ice-sheet
Greenland
Antarc*
Antarctica
Ice Sheet
Online Access:https://dx.doi.org/10.26190/5d0c0c0bd1f26
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 ... : The data is described in Menviel et al., 2019, Geoscientific Model Development, "The penultimate deglaciation: protocol for PMIP4 transient numerical simulations between 140 and 127°ka, version 1.0", https://doi.org/10.5194/gmd-2019-41 as well as on the PMIP4 wiki:https://pmip4.lsce.ipsl.fr/doku.php/exp_design:degla_t2 ...

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