Abstract
The accuracy of prediction of stable atmospheric boundary layers depends on the parameterization of the surface layer which is usually derived from the Monin-Obukhov similarity theory. In this article, several surface-layer models in the format of velocity and potential temperature Deacon numbers are compared with observations from CASES99, Cardington, and Halley datasets. The comparisons were hindered by a large amount of scatter within and among datasets. Tests utilizing R2 demonstrated that the quasi-normal scale elimination (QNSE) theory exhibits the best overall performance. Further proof of this was provided by 1D simulations with the Weather Research and Forecasting (WRF) model.
Original language | English |
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Pages (from-to) | 83-88 |
Number of pages | 6 |
Journal | Atmospheric Science Letters |
Volume | 16 |
Issue number | 1 |
DOIs | |
State | Published - 1 Jan 2015 |
Keywords
- Constant flux layer
- Deacon numbers
- Stable stratification
- Turbulence parameterization
ASJC Scopus subject areas
- Atmospheric Science