Abstract
In this paper a simple model of the planetary boundary layer (PBL) is proposed. The surface layer is modeled according to established similarity theory. Above the surface layer a prognostic equation for the mixing length is introduced. The time-dependent mixing length is a function of the PBL characteristics, including the height of the capping inversion, the local friction velocity and the surface heat flux. In a preliminary experiment, the behavior of the PBL is compared with observations from the Great Plains Experiment.
| Original language | English |
|---|---|
| Journal | Journal of applied meteorology (1988) |
| Volume | 15 |
| Issue number | 9 |
| Pages (from-to) | 909-919 |
| ISSN | 0894-8763 |
| DOIs | |
| Publication status | Published - 1976 |
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