HIGHLIGHTS
SUMMARY
A number of studies (e_g, Thornalley et_al 2018) have suggested a connectivity between density anomalies in the Labrador Sea and the strength of the Deep Western Boundary Current (DWBC) in the subtropics. Lozier et_al suggest that the apparent connectivity between the Labrador Sea and the subtropical AMOC is possible if: Labrador Sea density anomalies are signatures of density anomalies imported from the eastern subpolar gyre (Menary et_al 2020), where LNADW constituents originate; and/or Labrador Sea density anomalies exert a remote impact on water mass transformation in the eastern subpolar gyre. The authors identify . . .
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