A wind-tunnel study of sea breeze effects

摘要: A wind-tunnel simulation of the diffusion patterns in a sea breeze has been attempted. No attempt was made to reproduce recirculation that characterizes breeze, but results indicate low-level onshore flow well simulated for neutral, stable, unstable, and elevated inversion conditions. Velocity, turbulence, shear stress, temperature data were taken, spread emissions from ground-level sources investigated. Comparison is with theoretical predictions by Inoue open, countryside Pasquill. Agreement good. The comparison Pasquill's shows flows are shifted two categories towards more stable. discrepancy may be explained as lack mesoscale turbulence wind-tunnel.