Enhanced Mid‐depth Southward Transport in the Northeast Atlantic at the Last Glacial Maximum Despite a Weaker AMOC

This project was supported by the Australian Research Council. L. C. M., L. M., P. S., and J. Y. acknowledge funding from the Australian Research Council Grants DE150100107, DP180100048, DE150100223, FT140100993, FT180100606, and DP140101393. L. C. S. acknowledges support from NERC Grant NE/L006421/1.