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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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 |
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Open Polar |
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Zenodo |
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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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1766129573751160832 |