Proof of concept for turbulence measurements with the RPAS SUMO during the BLLAST campaign

被引:30
作者
Baserud, Line [1 ]
Reuder, Joachim [1 ]
Jonassen, Marius O. [1 ,2 ]
Kral, Stephan T. [1 ,2 ,3 ]
Paskyabi, Mostafa B. [1 ]
Lothon, Marie [4 ]
机构
[1] Univ Bergen, Inst Geophys, Allegaten 70, N-5007 Bergen, Norway
[2] UNIS, N-9171 Longyearbyen, Norway
[3] Finnish Meteorol Inst, Helsinki, Finland
[4] Univ Toulouse, CNRS, Lab Aerol, Toulouse, France
关键词
REMOTELY-PILOTED AIRCRAFT; METEOROLOGICAL OBSERVER SUMO; CONVECTIVE BOUNDARY-LAYER; UNMANNED AERIAL VEHICLE; LOWER TROPOSPHERE; VARIANCE MEASUREMENTS; MEASUREMENT SYSTEM; WIND LIDARS; TRANSITION; AFTERNOON;
D O I
10.5194/amt-9-4901-2016
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
The micro-RPAS (remotely piloted aircraft system) SUMO (Small Unmanned Meteorological Observer) equipped with a five-hole-probe (5HP) system for turbulent flow measurements was operated in 49 flight missions during the BLLAST (Boundary-Layer Late Afternoon and Sunset Turbulence) field campaign in 2011. Based on data sets from these flights, we investigate the potential and limitations of airborne velocity variance and TKE (turbulent kinetic energy) estimations by an RPAS with a take-off weight below 1 kg. The integration of the turbulence probe in the SUMO system was still in an early prototype stage during this campaign, and therefore extensive post-processing of the data was required. In order to be able to calculate the three-dimensional wind vector, flow probe measurements were first synchronized with the autopilot's attitude and velocity data. Clearly visible oscillations were detected in the resulting vertical velocity, w, even after correcting for the aircraft motion. The oscillations in w were identified as the result of an internal time shift between the inertial measurement unit (IMU) and the GPS sensors, leading to insufficient motion correction, especially for the vertical wind component, causing large values of sigma(w). Shifting the IMU 1-1.5 s forward in time with respect to the GPS yields a minimum for sigma(w) and maximum covariance between the IMU pitch angle and the GPS climb angle. The SUMO data show a good agreement to sonic anemometer data from a 60m tower for sigma(u), but show slightly higher values for sigma(v) and sigma(w). Vertical TKE profiles, obtained from consecutive flight legs at different altitudes, show reasonable results, both with respect to the overall TKE level and the temporal variation. A thorough discussion of the methods used and the identified uncertainties and limitations of the system for turbulence measurements is included and should help the developers and users of other systems with similar problems.
引用
收藏
页码:4901 / 4913
页数:13
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