Quantifying the effect of the Drake Passage opening on the Eocene Ocean

Fuente: PANGAEA
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Bibliographische Detailangaben
Hauptverfasser: Donnadieu, Yannick, Toumoulin, Agathe, Ladant, Jean-Baptiste, Batenburg, Sietske J, Poblete, Fernando, Dupont-Nivet, Guillaume
Format: Dataset Open Access
Sprache:en
Veröffentlicht: PANGAEA 2020
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author Donnadieu, Yannick
Toumoulin, Agathe
Ladant, Jean-Baptiste
Batenburg, Sietske J
Poblete, Fernando
Dupont-Nivet, Guillaume
author_facet Donnadieu, Yannick
Toumoulin, Agathe
Ladant, Jean-Baptiste
Batenburg, Sietske J
Poblete, Fernando
Dupont-Nivet, Guillaume
collection Datos científicos de ciencias marinas y ambientales
contents This dataset combines the oceanic and atmospheric outputs from various experiments modelling the Drake Passage opening during the Eocene (Toumoulin et al. 2020, Paleoceanography and Paleoclimatology). It includes 4 simulations with a 40 Ma paleogeography, a 1120 ppm pCO2 and different depths of the Drake Passage (0, 100, 1000, 2500m). Experiments were performed with the general circulation model IPSL-CM5A2. Each of these simulations ran for 4000 years until a quasi-equilibrium state (deep ocean temperature change <0.1°C/century). Data are monthly averages over the last 100 years.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_915802
institution PANGAEA
language en
publishDate 2020
publisher PANGAEA
record_format pangaea
spellingShingle Quantifying the effect of the Drake Passage opening on the Eocene Ocean
Donnadieu, Yannick
Toumoulin, Agathe
Ladant, Jean-Baptiste
Batenburg, Sietske J
Poblete, Fernando
Dupont-Nivet, Guillaume
Antarctic Circumpolar Current; climate; Eocene; File content; File format; File name; File size; general circulation model; Ocean Gateways; Paleoclimate; Uniform resource locator/link to file
This dataset combines the oceanic and atmospheric outputs from various experiments modelling the Drake Passage opening during the Eocene (Toumoulin et al. 2020, Paleoceanography and Paleoclimatology). It includes 4 simulations with a 40 Ma paleogeography, a 1120 ppm pCO2 and different depths of the Drake Passage (0, 100, 1000, 2500m). Experiments were performed with the general circulation model IPSL-CM5A2. Each of these simulations ran for 4000 years until a quasi-equilibrium state (deep ocean temperature change <0.1°C/century). Data are monthly averages over the last 100 years.
title Quantifying the effect of the Drake Passage opening on the Eocene Ocean
topic Antarctic Circumpolar Current; climate; Eocene; File content; File format; File name; File size; general circulation model; Ocean Gateways; Paleoclimate; Uniform resource locator/link to file
url https://doi.org/10.1594/PANGAEA.915802