Non-closure of the surface energy balance explained by phase difference between vertical velocity and scalars of large atmospheric eddies
It is now accepted that large-scale turbulent eddies impact the widely reported non-closure of the surface energy balance when latent and sensible heat fluxes are measured using the eddy covariance method in the atmospheric surface layer (ASL).However, a mechanistic link between large eddies and non-closure of the surface energy balance remains a s