Abstract
The convective boundary-layer scaling expressions presented by Wyngaard and LeMone (1980) are compared with predictions from a turbulence closure model. We first examine a model experiment involving a clear-air, convectively driven boundary layer overland. The model results agree well with scaling expressions and observations in the lower boundary layer and near the inversion. In the mid-boundary layer region, however, the closure model underestimates the temperature structure parameter CT2 and overestimates the humidity structure parameter Cq2. A cloud-topped marine boundary layer is examined in a second experiment which uses AMTEX data. Order-of-magnitude differences are found here between interfacial-layer scaling expressions and closure model predictions. Potential sources of this disagreement are discussed.
Keywords
Related Publications
Refractive Index Structure Parameters: Time-Dependent Calculations Using a Numerical Boundary-Layer Model
A second-moment turbulence closure model is used to investigate the make-up of the refractive structure parameter Cn2 for acoustic, optical and microwave radiation. For these di...
The Moist Boundary Layer with a Higher Order Turbulence Closure Model
A one-dimensional higher order turbulence closure model is used to investigate moisture structure within the diurnally varying planetary boundary layer. The diurnal character of...
Development and Testing of a Surface Flux and Planetary Boundary Layer Model for Application in Mesoscale Models
Abstract Although the development of soil, vegetation, and atmosphere interaction models has been driven primarily by the need for accurate simulations of long-term energy and m...
Some effects of suspended sediment stratification on an oceanic bottom boundary layer
A suspended‐sediment‐induced, stably stratified oceanic bottom boundary layer is examined with the Mellor‐Yamada level II turbulence closure model. The boundary layer equations ...
A Reynolds stress model of turbulence and its application to thin shear flows
The paper provides a model of turbulence which effects closure through approximated transport equations for the Reynolds stress tensor $\overline{u_iu_j}$ and for the turbulence...
Publication Info
- Year
- 1981
- Type
- article
- Volume
- 38
- Issue
- 4
- Pages
- 751-761
- Citations
- 12
- Access
- Closed
External Links
Social Impact
Social media, news, blog, policy document mentions
Citation Metrics
Cite This
Identifiers
- DOI
- 10.1175/1520-0469(1981)038<0751:cospse>2.0.co;2