Next:
Stratus-Topped PBL
Up:
Atmospheric planetary boundary-layer research
Previous:
Surface-induced circulations.
Cloudy PBL
Stratus-Topped PBL
Cloud-top entrainment instability.
Other mechanisms for cloud dissipation.
Turbulent fluxes within the PBL.
Overlying free atmosphere.
PBL under Non-Precipitating Cumulus
PBL under Precipitating Cumulus
U.S. National Report to IUGG, 1991-1994
Rev. Geophys. Vol. 33 Suppl., © 1995 American Geophysical Union
