Wednesday, 12 January 2000
The determination of the height of the Planetary Boundary Layer (PBL)
is important for accurate transport and diffusion modeling. The PBL height
determines the direction and speed of pollution movement, as well as the
vertical depth over which the effluent will be mixed. Many methods
are used by different models to deduce the height of the PBL from observed
upper-air soundings. Fewer methods utilize output from mesoscale numerical
weather prediction models (e.g., MM5, RAMS, COAMPS) to determine PBL
heights, mainly because the wide use of these models for transport and diffusion
modeling has only recently begun. We plan to present results of a study in
which PBL heights computed from a variety of methods are compared and
contrasted. The methods to be included are a combination of subjective (i.e.,
human) and objective schemes using both observed upper-air data and model
forecast data produced by the Regional Atmospheric Modeling System (RAMS). PBL
heights determined using the prognostic fields of turbulent kinetic energy
(TKE) available from RAMS will also be included in the study to determine the
applicability of this technique.
- Indicates paper has been withdrawn from meeting
- Indicates an Award Winner