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Data from: Non-linear climatic response to the weakening of the Atlantic meridional overturning circulation during glacial times

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Jun 03, 2026 version files 4.92 GB

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Abstract

The climatic response to the weakening of the Atlantic Meridional Overturning Circulation (AMOC) is investigated under glacial conditions representative of Heinrich Stadial 5 (at 49,000 years ago) using a fully coupled Earth System Model (ACCESS-ESM1.5). Three North Atlantic freshwater forcing experiments are conducted using the ACCESS-ESM1.5 model to evaluate the climate response to different magnitudes of AMOC weakening. This dataset includes all the model outputs used in this study.