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| Content Provider | Springer Nature Link |
|---|---|
| Author | Lothon, Marie Lenschow, Donald H. Mayor, Shane D. |
| Copyright Year | 2006 |
| Abstract | We utilized a Doppler lidar to measure integral scale and coherence of vertical velocity w in the daytime convective boundary layer (CBL). The high resolution 2 μm wavelength Doppler lidar developed by the NOAA Environmental Technology Laboratory was used to detect the mean radial velocity of aerosol particles. It operated continuously in the zenith-pointing mode for several days in the summer 1996 during the “Lidars in Flat Terrain” experiment over level farmland in central Illinois. We calculated profiles of w integral scales in both the alongwind and vertical directions from about 390 m height to the CBL top. In the middle of the mixed layer we found, from the ratio of the w integral scale in the vertical to that in the horizontal direction, that the w eddies are squashed by a factor of about 0.65 as compared to what would be the case for isotropic turbulence. Furthermore, there is a significant decrease of the vertical integral scale with height. The integral scale profiles and vertical coherence show that vertical velocity fluctuations in the CBL have a predictable anisotropic structure. We found no significant tilt of the thermal structures with height in the middle part of the CBL. |
| Starting Page | 521 |
| Ending Page | 536 |
| Page Count | 16 |
| File Format | |
| ISSN | 00068314 |
| Journal | Boundary-Layer Meteorology |
| Volume Number | 121 |
| Issue Number | 3 |
| e-ISSN | 15731472 |
| Language | English |
| Publisher | Kluwer Academic Publishers |
| Publisher Date | 2006-06-22 |
| Publisher Place | Dordrecht |
| Access Restriction | One Nation One Subscription (ONOS) |
| Subject Keyword | Coherence Convective boundary layer Integral scale Lidar Turbulence Atmospheric Protection/Air Quality Control/Air Pollution Meteorology/Climatology |
| Content Type | Text |
| Resource Type | Article |
| Subject | Atmospheric Science |
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