📝 SummarXiv

Abstract

Turbulent flows close beneath a free water surface are of central importance in the Earth system, yet remain relatively little studied with many open questions. We study the degree of correlation between surface motion and sub-surface velocities, comparing data from direct numerical simulation to a new experimental setup where the free-surface motion and sub-surface velocity field are measured simultaneously in a jet-stirred tank. A previous study showed a close correlation between the time series of mean-square surface divergence and the surface features (Babiker \& al., 2023 \emph{J.~Fluid Mech.} {\bf 964}, R2); we find that the normalised cross-correlation between mean-square horizontal divergence at vertical position $z$ ($\beta(z)=\partial_xu+\partial_yv$, with $z$ the vertical coordinate and $u,v$ the velocity in horizontal directions $x,y$, respectively) and relative surface area covered by persistent surface features (`dimples' and `scars') decreases slowly with depth but remains significant even two integral scales beneath the surface. Although turbulent Reynolds numbers differ by an order of magnitude between simulation and experiment, the same scaling and behaviour is found for all quantities we consider when scaled by the integral scale. Our results demonstrate that although surface-to-bulk correlations may appear weak when covariance between surface and velocity quantities is made point-to-point for the full surface, conditional quantities guided by visible surface features can yield significant information about the largest, most energetic flow events even beyond the blockage layer.