An observational study of the dryline

Abstract

This study presents analyses of data collected in the vicinity of a cloud-free dryline that occurred in western Oklahoma on 24 May 1989. Observations reveal sharp contrasts across the quasi-stationary, north-south dryline during midafternoon. Of greatest significance is a pronounced gradient of virtual potential temperature, although horizontal convergence and vorticity also maximize at the dryline. The environment of the 24 May dryline is dominated by vertical mixing that maintains a convective boundary layer (CBL) on both sides of the dryline. The dryline resembles a "mixing zone' containing varying proportions of hot, dry air to the west side and warm, moist air from the surface dryline location, then becomes a quasi-horizontal elevated moist layer above the CBL east of the dryline. -from Authors