Proxy-constrained modeled AMOC from 1450-1780 CE

The Atlantic Meridional Overturning Circulation (AMOC) has profound impacts on the climate of the North Atlantic and the global climate at large. It plays a significant role in redistributing heat and freshwater around the globe. Real-time AMOC measurement began in 2004, providing monthly observatio...

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Bibliographic Details
Main Author: Eric Samakinwa
Format: Dataset
Language:English
Published: 2023
Subjects:
Online Access:https://zenodo.org/record/7648938
https://doi.org/10.5281/zenodo.7648938
id ftzenodo:oai:zenodo.org:7648938
record_format openpolar
spelling ftzenodo:oai:zenodo.org:7648938 2023-05-15T17:31:48+02:00 Proxy-constrained modeled AMOC from 1450-1780 CE Eric Samakinwa 2023-02-17 https://zenodo.org/record/7648938 https://doi.org/10.5281/zenodo.7648938 eng eng info:eu-repo/grantAgreement/EC/H2020/787574/ doi:10.5281/zenodo.7648937 https://zenodo.org/record/7648938 https://doi.org/10.5281/zenodo.7648938 oai:zenodo.org:7648938 info:eu-repo/semantics/openAccess https://creativecommons.org/licenses/by/4.0/legalcode AMOC Proxy ensemble Ocean info:eu-repo/semantics/other dataset 2023 ftzenodo https://doi.org/10.5281/zenodo.764893810.5281/zenodo.7648937 2023-03-11T04:24:00Z The Atlantic Meridional Overturning Circulation (AMOC) has profound impacts on the climate of the North Atlantic and the global climate at large. It plays a significant role in redistributing heat and freshwater around the globe. Real-time AMOC measurement began in 2004, providing monthly observation of the stream function. Although this observation exhibits large intra-to-multi-annual variability, the records are too short to make inferences about intra-annual AMOC variability. Here, we present a 10-member ensemble simulated AMOC from a stand-alone ocean model MPI-OM. We nudge the ocean model in the surface to proxy the reconstructed SST of Samakinwa et al., 2021, thereby leading to a proxy-constrained Modeled AMOC for the period 1450 - 1780 CE. Dataset North Atlantic Zenodo
institution Open Polar
collection Zenodo
op_collection_id ftzenodo
language English
topic AMOC
Proxy
ensemble
Ocean
spellingShingle AMOC
Proxy
ensemble
Ocean
Eric Samakinwa
Proxy-constrained modeled AMOC from 1450-1780 CE
topic_facet AMOC
Proxy
ensemble
Ocean
description The Atlantic Meridional Overturning Circulation (AMOC) has profound impacts on the climate of the North Atlantic and the global climate at large. It plays a significant role in redistributing heat and freshwater around the globe. Real-time AMOC measurement began in 2004, providing monthly observation of the stream function. Although this observation exhibits large intra-to-multi-annual variability, the records are too short to make inferences about intra-annual AMOC variability. Here, we present a 10-member ensemble simulated AMOC from a stand-alone ocean model MPI-OM. We nudge the ocean model in the surface to proxy the reconstructed SST of Samakinwa et al., 2021, thereby leading to a proxy-constrained Modeled AMOC for the period 1450 - 1780 CE.
format Dataset
author Eric Samakinwa
author_facet Eric Samakinwa
author_sort Eric Samakinwa
title Proxy-constrained modeled AMOC from 1450-1780 CE
title_short Proxy-constrained modeled AMOC from 1450-1780 CE
title_full Proxy-constrained modeled AMOC from 1450-1780 CE
title_fullStr Proxy-constrained modeled AMOC from 1450-1780 CE
title_full_unstemmed Proxy-constrained modeled AMOC from 1450-1780 CE
title_sort proxy-constrained modeled amoc from 1450-1780 ce
publishDate 2023
url https://zenodo.org/record/7648938
https://doi.org/10.5281/zenodo.7648938
genre North Atlantic
genre_facet North Atlantic
op_relation info:eu-repo/grantAgreement/EC/H2020/787574/
doi:10.5281/zenodo.7648937
https://zenodo.org/record/7648938
https://doi.org/10.5281/zenodo.7648938
oai:zenodo.org:7648938
op_rights info:eu-repo/semantics/openAccess
https://creativecommons.org/licenses/by/4.0/legalcode
op_doi https://doi.org/10.5281/zenodo.764893810.5281/zenodo.7648937
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