The Role of Atlantic Basin Geometry in Meridional Overturning Circulation

Climatology data for manuscript: "The Role of Atlantic Basin Geometry in Meridional Overturning Circulation" We present idealized simulations to explore how the shape of eastern and western continental boundaries along the Atlantic influence the Atlantic Meridional Overturning Circulation...

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Main Author: Ragen, Sarah
Format: Dataset
Language:unknown
Published: Zenodo 2021
Subjects:
Online Access:https://dx.doi.org/10.5281/zenodo.5544531
https://zenodo.org/record/5544531
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spelling ftdatacite:10.5281/zenodo.5544531 2023-05-15T18:18:00+02:00 The Role of Atlantic Basin Geometry in Meridional Overturning Circulation Ragen, Sarah 2021 https://dx.doi.org/10.5281/zenodo.5544531 https://zenodo.org/record/5544531 unknown Zenodo https://dx.doi.org/10.5281/zenodo.5544530 Open Access Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 info:eu-repo/semantics/openAccess CC-BY dataset Dataset 2021 ftdatacite https://doi.org/10.5281/zenodo.5544531 https://doi.org/10.5281/zenodo.5544530 2021-11-05T12:55:41Z Climatology data for manuscript: "The Role of Atlantic Basin Geometry in Meridional Overturning Circulation" We present idealized simulations to explore how the shape of eastern and western continental boundaries along the Atlantic influence the Atlantic Meridional Overturning Circulation (AMOC). We use a state-of-the art ocean—sea-ice model (MOM6 and SIS2) with idealized, zonally-symmetric surface forcing and a range of idealized continental configurations with a large, Pacific-like basin and a small, Atlantic-like basin. We perform simulations with five coastline geometries along the Atlantic-like basin that range from coastlines that are straight to coastlines shaped like the coasts of the American and African continents. Dataset Sea ice DataCite Metadata Store (German National Library of Science and Technology) Pacific
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language unknown
description Climatology data for manuscript: "The Role of Atlantic Basin Geometry in Meridional Overturning Circulation" We present idealized simulations to explore how the shape of eastern and western continental boundaries along the Atlantic influence the Atlantic Meridional Overturning Circulation (AMOC). We use a state-of-the art ocean—sea-ice model (MOM6 and SIS2) with idealized, zonally-symmetric surface forcing and a range of idealized continental configurations with a large, Pacific-like basin and a small, Atlantic-like basin. We perform simulations with five coastline geometries along the Atlantic-like basin that range from coastlines that are straight to coastlines shaped like the coasts of the American and African continents.
format Dataset
author Ragen, Sarah
spellingShingle Ragen, Sarah
The Role of Atlantic Basin Geometry in Meridional Overturning Circulation
author_facet Ragen, Sarah
author_sort Ragen, Sarah
title The Role of Atlantic Basin Geometry in Meridional Overturning Circulation
title_short The Role of Atlantic Basin Geometry in Meridional Overturning Circulation
title_full The Role of Atlantic Basin Geometry in Meridional Overturning Circulation
title_fullStr The Role of Atlantic Basin Geometry in Meridional Overturning Circulation
title_full_unstemmed The Role of Atlantic Basin Geometry in Meridional Overturning Circulation
title_sort role of atlantic basin geometry in meridional overturning circulation
publisher Zenodo
publishDate 2021
url https://dx.doi.org/10.5281/zenodo.5544531
https://zenodo.org/record/5544531
geographic Pacific
geographic_facet Pacific
genre Sea ice
genre_facet Sea ice
op_relation https://dx.doi.org/10.5281/zenodo.5544530
op_rights Open Access
Creative Commons Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/legalcode
cc-by-4.0
info:eu-repo/semantics/openAccess
op_rightsnorm CC-BY
op_doi https://doi.org/10.5281/zenodo.5544531
https://doi.org/10.5281/zenodo.5544530
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