We investigate theoretically and experimentally the evaporation of liquid
disks in the presence of natural convection due to a density difference between
the vapor and the surrounding gas. From the analogy between thermal convection
above a heated disk and our system, we derive scaling laws to describe the
evaporation rate. The local evaporation rate depends on the presence of a
boundary layer in the gas phase such that the total evaporation rate is given
by a combination of different scaling contributions, which reflect the
structure of the boundary layer. We compare our theoretical predictions to
experiments performed with water in an environment controlled in humidity,
which validate our approach