## Abstract Vertical profiles of the latent heat flux in a convective boundary layer (CBL) are obtained for the first time over complex terrain with airborne water vapour differential absorption lidar and Doppler wind lidar. During the Convective and Orographicallyβinduced Precipitation Study (COPS
Lidar observations of flow variability over complex terrain
β Scribed by A. Barkwith; C. G. Collier
- Publisher
- John Wiley and Sons
- Year
- 2011
- Tongue
- English
- Weight
- 705 KB
- Volume
- 18
- Category
- Article
- ISSN
- 1350-4827
- DOI
- 10.1002/met.244
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β¦ Synopsis
Abstract
This paper examines one way in which remote sensing instrumentation can be used to advance our understanding of the interactions between complex terrain and the atmospheric boundary layer (ABL). When mean flow speed is of moderate strength and the ABL is stable, mechanical effects will dominate thermal effects in modifying flow speed and direction. Boundary layer measurements were made using the scanning Salford 10 Β΅m pulsed CO~2~ Doppler lidar during the 2005 Convective Storm Initiation Project (CSIP), above the heterogeneous orography that surrounds Faccombe, Hampshire, UK. A new method of detecting boundary layer flow perturbations was developed and successfully applied to the lidar data, giving a clearer insight into flow modification that occurs above complex terrain. Copyright Β© 2011 Royal Meteorological Society
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