The authors describe and present early results from the July-August 19
96 Lidars in Flat Terrain (LIFT) experiment. LIFT was a boundary layer
experiment that made use of recently developed Doppler, aerosol backs
catter, and ozone lidars, along with radars and surface instrumentatio
n, to study the structure and evolution of the convective boundary lay
er over the very flat terrain of central Illinois. Scientific goals in
clude measurement of fluxes of heat, moisture, and momentum; vertical
velocity statistics; study of entrainment and boundary layer height; a
nd observation of organized coherent structures. The data collected wi
ll also be used to evaluate the performance of these new lidars and co
mpare measurements of velocity and boundary layer height to those obta
ined from nearby radar wind profilers. LIFT was a companion to the Fla
tland96 experiment, described by Angevine et al.