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Thomas Meunier, Enric Pallàs Sanz, Miguel Tenreiro, José Ochoa, Angel Ruiz Angulo, and Christian Buckingham

.e., having increased spice) anomaly between the 24.5 and 26.5 kg m −3 isopycnals ( Fig. 1 ). Since the Yucatan Strait is the GoM’s only entrance for subsurface water, the thermohaline anomalies found in LCE’s cores have a large impact on the GCW characteristics ( Vidal et al. 1992 ; Elliott 1982 ; Meunier et al. 2018b ). GCW is believed to be transformed SUW, through surface heat fluxes, river discharge, evaporation, precipitation, and diapycnal mixing ( Hamilton et al. 2018 ). Of particular interest

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