| contributor author | Kiemle, C. | |
| contributor author | Kästner, M. | |
| contributor author | Ehret, C. | |
| date accessioned | 2017-06-09T14:00:04Z | |
| date available | 2017-06-09T14:00:04Z | |
| date copyright | 1995/08/01 | |
| date issued | 1995 | |
| identifier issn | 0739-0572 | |
| identifier other | ams-1068.pdf | |
| identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4145823 | |
| description abstract | The convective boundary layer has been investigated with an airborne differential absorption lidar (DIAL) during the EFEDA (European Field Experiment in a Desertification Threatened Area) campaign in June 1991 over middle Spain. For the first time, airborne DIAL water vapor measurements resolving the structure of a convection cell are presented. On 28 June, an interesting boundary layer structure has been found in the lidar aerosol and water vapor measurements, showing a wave structure with a wavelength of 4.5 km and an amplitude of 100?450 m in the residual layer. Additional radiosonde data and the analysis of the synoptic situation reveal that this wave structure is part of a wind shear-driven gravity wave. | |
| publisher | American Meteorological Society | |
| title | The Convective Boundary Layer Structure from Lidar and Radiosonde Measurements during the EFEDA '91 Campaign | |
| type | Journal Paper | |
| journal volume | 12 | |
| journal issue | 4 | |
| journal title | Journal of Atmospheric and Oceanic Technology | |
| identifier doi | 10.1175/1520-0426(1995)012<0771:TCBLSF>2.0.CO;2 | |
| journal fristpage | 771 | |
| journal lastpage | 782 | |
| tree | Journal of Atmospheric and Oceanic Technology:;1995:;volume( 012 ):;issue: 004 | |
| contenttype | Fulltext | |
