  Cozar et al. (2012) used remotely-sensed data to link phytoplankton growth to
the net heat flux in both the northern and southern parts of Lake Victoria.
However, the latent and sensible heat fluxes were overestimated by ~26% by
assuming a constant air density of 1.3 kg m-3. As a result, the net heat flux
was underestimated, bringing into question conclusions regarding the convective
circulation.
