The vertical velocity field and the convective plumes in the atmospheric boundary layer have been observed during morning hours with the acoustic Doppler sounder of the C.R.P.E. A method for plume determination using acoustic soundings in the well-mixed layer is presented. Using Telford's 1970 and M
Vertical velocity field in the convective boundary layer as observed with an acoustic Doppler sodar
โ Scribed by Odile Taconet; Alain Weill
- Publisher
- Springer
- Year
- 1982
- Tongue
- English
- Weight
- 814 KB
- Volume
- 23
- Category
- Article
- ISSN
- 0006-8314
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โฆ Synopsis
The morning development of the daytime convective boundary layer (CBL) during fine weather has been observed with an acoustic D2pler sodar of the C.R.P.E. In particular, the vertical profile of the vertical velocity third-order statistic W" has been obtained. This quantity is a maximum near 0.32, where z, is the height of the CBL. The histogram of vertical velocity in the CBL shows a relationship between W" and the convective velocity W. and is useful for convective plume determination.
๐ SIMILAR VOLUMES
Convective plume patterns, characteristic of clear sky and light wind daytime boundary layers over land, were observed for two nights with a &i-axial Doppler sodar operated in the central area of Rome during the summer of 1994. An urban heat island effect, combined with a continuation of a breeze fr