3D wind observations with a compact mobile lidar based on tropo- and stratospheric aerosol backscatter

被引:3
|
作者
Mense, Thorben H. [1 ]
Hoeffner, Josef [1 ]
Baumgarten, Gerd [1 ]
Eixmann, Ronald [1 ]
Froh, Jan [1 ]
Mauer, Alsu [1 ]
Munk, Alexander [2 ]
Wing, Robin [1 ]
Luebken, Franz-Josef [1 ]
机构
[1] Univ Rostock, Leibniz Inst Atmospher Phys, Opt Soundings & Sounding Rockets, D-18225 Kuhlungsborn, Germany
[2] Fraunhofer Inst Laser Technol ILT, Nonlinear Opt & Tunable Lasers, D-52074 Aachen, Germany
关键词
DOPPLER WIND; AIRBORNE DEMONSTRATOR; TEMPERATURE-MEASUREMENTS; ATMOSPHERIC MEASUREMENTS; RADIOSONDE OBSERVATIONS; MIDDLE-ATMOSPHERE; VALIDATION; SYSTEM; PERFORMANCE; ALADIN;
D O I
10.5194/amt-17-1665-2024
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
We present the first measurements of simultaneous horizontal and vertical winds using a new lidar system developed at the Leibniz Institute of Atmospheric Physics in Kuhlungsborn, Germany (54.12 degrees N, 11.77 degrees E), for the concept of Vertical And Horizontal COverage by LIdars (VAHCOLI). We describe the technical details of a multi-field-of-view (MFOV) upgrade, which allows the measurement of wind dynamics in the transition region from microscale to mesoscale ( 10 3 - 10 4 m). The method was applied at the edge of a developing high-pressure region, covering altitudes between 3 and 25 km. Comparisons between the lidar measurements and data from the European Centre for Medium-Range Weather Forecasts (ECMWF) show excellent agreement for the meridional wind component along the north beam of the lidar, which is better than 0.30 +/- 0.33 m s - 1 , while along the south beam, a higher deviation with - 0.93 +/- 0.73 m s - 1 is observed. Measurements of vertical wind show a significant underestimation of this component by ECMWF. Comparison of Aeolus winds to the lidar winds projected to the Aeolus viewing direction shows good agreement, with results better than - 0.12 +/- 3.31 m s - 1 . The capability of the MFOV lidar to explore small-scale asymmetries in the wind field is shown by a comparison of the north and south field of view, where we observe a wind asymmetry in the meridional winds, which is also present in ECMWF but underestimated by a factor of approximately 4.
引用
收藏
页码:1665 / 1677
页数:13
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