Sodar estimates of surface heat flux and mixed layer depth compared with direct measurements |
| |
| Institution: | 1. Department of Cartography and Geoinformatics, Faculty of Geography, Lomonosov MSU, Leninskye Gory 1, Moscow 119234, Russia;2. Department of Meteorology and Climatology, Faculty of Geography, Lomonosov MSU, Leninskye Gory 1, Moscow 119234, Russia;1. Logistics Research Center, Shanghai Maritime University, Shanghai 200135, China;2. College of Transportation and Civil Engineering, Fujian Agriculture and Forestry University, Fuzhou 350002, China;3. School of Engineering, Sun Yat-sen University, Guangzhou, 510006, China;4. Institute of Physical Science and Engineering, Guangxi University, Nanning 530004, China;1. Graded S.p.A., Naples, Italy;2. Department of Engineering, University of Palermo, Italy;3. Horizonfirm S.r.l, Palermo, Italy;4. National & Kapodistrian University of Athens, Department of Physics, Greece;1. Center for Renewable Resources and Integration, Department of Mechanical and Aerospace Engineering, University of California, San Diego, United States;2. Department of Computer Science, Cornell Tech, New York, United States |
| |
| Abstract: | Similarity relationships for the convective boundary layer are used to derive surface heat flux and mixed layer depth from sodar measurements of the temperature structure parameter and the vertical velocity variance. Two different methods are presented and compared with direct measurements from the Öresund experiment which took place during the period 15 May–14 June 1984. The analyzed data were taken with two three-axis monostatic Doppler sodars manufactured by Sensitron, Sweden. Comparison with simultaneous direct measurements shows generally good agreement during convective conditions but also reveals some limitations of the methods. |
| |
| Keywords: | |
| 本文献已被 ScienceDirect 等数据库收录！ |
|
