Fig. 6: Labrador Sea water thickness.
From: Subpolar gyre decadal variability explains the recent oxygenation in the Irminger Sea
Time series of the density layer thickness for σ0 intervals of 0.005 kg m−3 averaged within the core of the Irminger Sea (Fig. 1), a for the hydrographic profiles and b for the Argo data. Gray curves and points highlight the lower and upper boundaries of the Labrador Sea Water layer (LSW). Note that the x-axis is not evenly spaced in a, and that the longest gaps are marked with a blank space. In b, the vertical white lines indicate missing data for interpolation.
