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, wh
โฆ LIBER โฆ
Structure of the vertical velocity field analyzed with a Doppler Sodar
โ Scribed by Angelo Ricotta; Massimo Berico; Salvatore Mazzola
- Publisher
- Springer
- Year
- 1983
- Tongue
- English
- Weight
- 765 KB
- Volume
- 27
- Category
- Article
- ISSN
- 0006-8314
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