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. 2023 Oct 10;11:e16208. doi: 10.7717/peerj.16208

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© 2023 Possenti et al.

This is an open access article distributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, reproduction and adaptation in any medium and for any purpose provided that it is properly attributed. For attribution, the original author(s), title, publication source (PeerJ) and either DOI or URL of the article must be cited.

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Volumetric flow rate in Sverdrup of the Atlantic Meridional Overturning Circulation (AMOC) derived in the CESM2 using CMIP6 climate models for two different climate scenarios SSP5-8.5 (in blue) and SSP2-4.5 (in red) at 26.5° N smoothed using a 5-year moving median vs top 200 m median of the predicted SPL_tot between 475 and 500 km distance for the Northwest Atlantic Ocean (45° N 40° W) from a single bulker. The regression equations are: for SSP5-8.5: SPL_tot (dB re 1 μPa) = −1.2 ± 0.1AMOC + 85.7 ± 0.8 (R² = 0.8) and for SSP2-4.5: SPL_tot (dB re 1 μPa) = −1.2 ± 0.1AMOC + 87.9 ± 0.8 (R² = 0.87).