Observations of the Labrador Sea eddy field

By Jonathan M. Lilly, P. Rhines, F. Schott, Kara L. Lavender, J. Lazier, U. Send, Eric D'Asaro. 2003

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Higher-Order Properties of Analytic Wavelets (2008, background): “On the other hand, the analytic wavelet transform can also be useful for application to very time-localized structure s [3], particularly if these features may appear as either locally even (symmetric) or locally odd (asymmetric) [ 4 ].”
On the Connection between Dense Water Formation, Overturning, and Poleward Heat Transport in a Convective Basin* (2006, background): “This exchange is thought to be dominated by mesoscale eddies, as supported by observations (Lilly et al. 1999; Prater 2002; Lilly et al. 2003), and by the numerical simulations (from idealized to more realistic) of Khatiwala and Visbeck (2000), Spall (2004), Katsman et al. (2004), and Eden and…”
The Irminger Gyre: Circulation, convection, and interannual variability (2011, background): “Lateral exchange between the boundary current and the interior, typically in the form of mesoscale eddies, has been extensively investigated in the eastern Labrador Sea (e.g. Lilly et al., 2003; Straneo, 2006).”