Proxy-constrained modeled AMOC from 1450-1780 CE

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.

Resources

Name Format Description Link
0 http://data.europa.eu/88u/dataset/oai-zenodo-org-7648938
0 http://data.europa.eu/88u/dataset/oai-zenodo-org-7648938
0 http://data.europa.eu/88u/dataset/oai-zenodo-org-7648938
0 http://data.europa.eu/88u/dataset/oai-zenodo-org-7648938
0 http://data.europa.eu/88u/dataset/oai-zenodo-org-7648938
0 http://data.europa.eu/88u/dataset/oai-zenodo-org-7648938
0 http://data.europa.eu/88u/dataset/oai-zenodo-org-7648938
0 http://data.europa.eu/88u/dataset/oai-zenodo-org-7648938
0 http://data.europa.eu/88u/dataset/oai-zenodo-org-7648938
0 http://data.europa.eu/88u/dataset/oai-zenodo-org-7648938
0 http://data.europa.eu/88u/dataset/oai-zenodo-org-7648938

Tags

  • amoc,-proxy,-ensemble,-ocean

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