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Data · dataset · 2024

IPSL-CM5A-LR GCM downscaled climate simulation for Marine Isotope Stage 3 over Europe.

Listed in Borealis

Initial data produced using the Atmosphere-Ocean General Circulation Model IPSL-CM5A-LR (Dufresne et al., 2013) at ∼1.9° latitude and 3.75° longitude spatial resolution to run two global climate simulations, one representing a typical MIS 3 stadial (cold) and the other a typical MIS 3 interstadial (warm).

Description

The boundary conditions are the same for both simulations and are described in Woillez et al. (2014), Le Mézo et al. (2017) and Lézine et al. (2023).

Astronomical forcing (precession, obliquity, eccentricity) is set with values for 46 kyr BP. Data were downscaled using a General Additive Model (Vrac et al., 2007, Latombe et al. 2017) obtaining temperature and precipitation data at a spatial scale of ~15 x 15 km . Cold model data are identified as M3I46F02 and warm model data are identified as MS3I46K2.

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Where it is published

Catalogue records · 1

Topics

Provenance · 1 source records, 12 field assertions
SourceKeyLast seenRaw
Borealisdoi:10.5683/SP3/JBZQKS12 d agoJSON v1
FieldAssertionExtractorEvidence
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concepts[field].dataverse_subject:earth-and-environmental-sciencessource · borealisdata caconnector:borealisdata_ca@1.0.0/subjects
concepts[field].local:field:earth-environmentalmapping · borealisdata caconnector:borealisdata_ca@1.0.0/subjects
concepts[field].local:field:ocean-atmosphericmapping · borealisdata caconnector:borealisdata_ca@1.0.0/subjects
concepts[method].local:method:climate-modelenrichment · borealisdata cakeyword-concept-rules@1.0.0title+description (65%)
concepts[method].local:method:simulationenrichment · borealisdata cakeyword-concept-rules@1.0.0title+description (75%)
created_datesource · borealisdata caconnector:borealisdata_ca@1.0.0
descriptionsource · borealisdata caconnector:borealisdata_ca@1.0.0/description
publication_datesource · borealisdata caconnector:borealisdata_ca@1.0.0
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version_labelsource · borealisdata caconnector:borealisdata_ca@1.0.0