Airborne wind lidar observations over the North Atlantic in 2016 for the pre-launch validation of the satellite mission Aeolus
In preparation of the satellite mission Aeolus carried out by the European Space Agency, airborne wind lidar observations have been performed in the frame of the North Atlantic Waveguide and Downstream Impact Experiment (NAWDEX), employing the prototype of the satellite instrument, the ALADIN Ai...
Main Authors: | , , , , , , , |
---|---|
Format: | Article |
Language: | English |
Published: |
Copernicus Publications
2018-06-01
|
Series: | Atmospheric Measurement Techniques |
Online Access: | https://www.atmos-meas-tech.net/11/3297/2018/amt-11-3297-2018.pdf |
Summary: | In preparation of the satellite mission Aeolus carried
out by the European Space Agency, airborne wind lidar observations have been
performed in the frame of the North Atlantic Waveguide and Downstream Impact
Experiment (NAWDEX), employing the prototype of the satellite instrument,
the ALADIN Airborne Demonstrator (A2D). The direct-detection Doppler wind
lidar system is composed of a frequency-stabilized Nd:YAG laser operating at
355 nm, a Cassegrain telescope and a dual-channel receiver. The latter
incorporates a Fizeau interferometer and two sequential Fabry–Pérot
interferometers to measure line-of-sight (LOS) wind speeds by analysing both
Mie and Rayleigh backscatter signals. The benefit of the complementary
design is demonstrated by airborne observations of strong wind shear related
to the jet stream over the North Atlantic on 27 September and 4 October
2016, yielding high data coverage in diverse atmospheric conditions. The
paper also highlights the relevance of accurate ground detection for the
Rayleigh and Mie response calibration and wind retrieval. Using a detection
scheme developed for the NAWDEX campaign, the obtained ground return signals
are exploited for the correction of systematic wind errors. Validation of
the instrument performance and retrieval algorithms was conducted by
comparison with DLR's coherent wind lidar which was operated in parallel,
showing a systematic error of the A2D LOS winds of less than
0.5 m s<sup>−1</sup> and random errors from 1.5
(Mie) to 2.7 m s<sup>−1</sup> (Rayleigh). |
---|---|
ISSN: | 1867-1381 1867-8548 |