The morning transition between the stable nocturnal situation and the daytime convective boundary layer (CBL) is of interest both for basic understanding and for initializing prognostic models. While the morning growth phase of the CBL has been studied in detail, relatively little has been published on the transition itself. In this paper, conventional observations of surface temperature, humidity, and fluxes and data from a meteorological tower are combined with measurements of the onset of convection by boundary layer wind profilers to explore the timing and behavior of the transition period. The transition is defined here as the period between sunrise and the time at which the depth of convection reaches about 200 m AGL. Diagnostic relationships based on surface heat flux, temperature difference between 2 m and 200 m, and bulk Richardson number are explored. The transition is found to be enabled by surface heating relaxing the surface stability, while the warming of the layer between 2 m and 200 m is in large part due to shear­driven entrainment.