The Small Whiskbroom Imager for atmospheric compositioN monitorinG (SWING) and its operations from an unmanned aerial vehicle (UAV) during the AROMAT campaign
The Small Whiskbroom Imager for atmospheric compositioN monitorinG (SWING) is a compact remote sensing instrument dedicated to mapping trace gases from an unmanned aerial vehicle (UAV). SWING is based on a compact visible spectrometer and a scanning mirror to collect scattered sunlight. Its weight,...
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Veröffentlicht in: | Atmospheric measurement techniques 2018-01, Vol.11 (1), p.551-567 |
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Sprache: | eng |
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Zusammenfassung: | The Small Whiskbroom Imager for atmospheric compositioN monitorinG (SWING) is
a compact remote sensing instrument dedicated to mapping trace gases from an
unmanned aerial vehicle (UAV). SWING is based on a compact visible
spectrometer and a scanning mirror to collect scattered sunlight. Its weight,
size, and power consumption are respectively 920 g,
27 cm × 12 cm × 8 cm, and 6 W. SWING was
developed in parallel with a 2.5 m flying-wing UAV. This unmanned
aircraft is electrically powered, has a typical airspeed of
100 km h−1, and can operate at a maximum altitude of
3 km. We present SWING-UAV experiments performed in Romania on 11 September 2014
during the Airborne ROmanian Measurements of Aerosols and Trace gases
(AROMAT) campaign, which was dedicated to test newly developed instruments in
the context of air quality satellite validation. The UAV was operated up to
700 m above ground, in the vicinity of the large power plant of
Turceni (44.67∘ N, 23.41∘ E; 116 ma.s.l.). These
SWING-UAV flights were coincident with another airborne experiment using the
Airborne imaging differential optical absorption spectroscopy (DOAS)
instrument for Measurements of Atmospheric Pollution (AirMAP), and with
ground-based DOAS, lidar, and balloon-borne in situ observations. The spectra recorded during the SWING-UAV flights are analysed with the DOAS
technique. This analysis reveals NO2 differential slant column
densities (DSCDs) up to 13±0.6×1016 molec cm−2.
These NO2 DSCDs are converted to vertical column densities (VCDs) by
estimating air mass factors. The resulting NO2 VCDs are up to
4.7±0.4×1016 molec cm−2. The water vapour DSCD
measurements, up to 8±0.15×1022 molec cm−2, are used
to estimate a volume mixing ratio of water vapour in the boundary layer of
0.013±0.002 mol mol−1. These geophysical quantities are
validated with the coincident measurements. |
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ISSN: | 1867-8548 1867-1381 1867-8548 |
DOI: | 10.5194/amt-11-551-2018 |