## Abstract A new parametrization for the depth of the daytime entrainment zone is presented. It is derived from a simple energy budget, in which the eddy velocity in the mixed layer penetrating the overlying stable entrainment zone is taken to be proportional to the characteristic topβdown velocit
Lidar measurements of the atmospheric entrainment zone and the potential temperature jump across the top of the mixed layer
β Scribed by R. Boers; E. W. Eloranta
- Publisher
- Springer
- Year
- 1986
- Tongue
- English
- Weight
- 933 KB
- Volume
- 34
- Category
- Article
- ISSN
- 0006-8314
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β¦ Synopsis
Lidar measurements of the thickness of the atmospheric entrainment zone are presented. The measurements were obtained in central Illinois during 6 days of clear-air convection.
A new method was developed to monitor the potential temperature jump across the entrainment zone. A single early morning temperature sounding and continuous lidar measurements of the mixed-layer height provide potential temperature jump values which agree well with in situ observations.
Lidar measurements of the thickness of the entrainment zone normalized by mixed-layer depth are presented as a function of a 'convective' Richardson number; these values show reasonable agreement with published laboratory results. The lidar observations span a wider range of mixed-layer depths and contain higher values of the normalized entrainment rate (dh/dt)/ w* than those observed in tank studies. Both lidar and tank results show that simple parcel theory does not properly predict entrainment-zone thickness. During this experiment which examined mostly high entrainment conditions, the normalized entrainmentlayer thickness was linearly dependent on entrainment rate.
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