Estimating subsurface horizontal and vertical velocities from sea-surface temperature

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Ocean Circulation Kinetic Energy: Reservoirs, Sources, and Sinks (2009, background): “Observations show that KE is surface intensified at scales smaller than the first deformation radius (Ferrari and Rudnick, 2001; LaCasce and Mahadevan, 2006) and support the notion that the ocean surface is a primary location for transfer of energy to small scales and hence dissipation.”
Reconstructing the Ocean's Interior from Surface Data (2013, background): “Surface heating/cooling can modify the surface signature of near-surface density anomalies, changing possibly both their strength and lateral structure (LaCasce and Mahadevan 2006).”
Do Altimeter Wavenumber Spectra Agree with the Interior or Surface Quasigeostrophic Theory (2008, methodology): “1995), has been recently revisited to describe the dynamics of the upper-oceanic layers (Lapeyre and Klein 2006a; LaCasce and Mahadevan 2006; IsernFontanet et al. 2006).”
Three‐dimensional reconstruction of oceanic mesoscale currents from surface information (2008, methodology): “This approach has been already tested in idealized numerical simulations [Lapeyre and Klein, 2006; LaCasce and Mahadevan, 2006], in situ measurements [LaCasce and Mahadevan, 2006] and remotely sensed data [Isern-Fontanet et al.”