Nitrogen dioxide and formaldehyde measurements from the GEOstationary Coastal and Air Pollution Events (GEO-CAPE) Airborne Simulator over Houston, Texas
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Published:2018-10-30
Issue:11
Volume:11
Page:5941-5964
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ISSN:1867-8548
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Container-title:Atmospheric Measurement Techniques
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language:en
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Short-container-title:Atmos. Meas. Tech.
Author:
Nowlan Caroline R.ORCID, Liu Xiong, Janz Scott J., Kowalewski Matthew G., Chance KellyORCID, Follette-Cook Melanie B., Fried Alan, González Abad GonzaloORCID, Herman Jay R.ORCID, Judd Laura M., Kwon Hyeong-AhnORCID, Loughner Christopher P., Pickering Kenneth E., Richter Dirk, Spinei Elena, Walega James, Weibring PetterORCID, Weinheimer Andrew J.
Abstract
Abstract. The GEOstationary Coastal and Air Pollution Events (GEO-CAPE)
Airborne Simulator (GCAS) was developed in support of NASA's decadal survey
GEO-CAPE geostationary satellite mission. GCAS is an airborne push-broom
remote-sensing instrument, consisting of two channels which make
hyperspectral measurements in the ultraviolet/visible (optimized for air
quality observations) and the visible–near infrared (optimized for ocean
color observations). The GCAS instrument participated in its first intensive
field campaign during the Deriving Information on Surface Conditions from
Column and Vertically Resolved Observations Relevant to Air Quality
(DISCOVER-AQ) campaign in Texas in September 2013. During this campaign, the
instrument flew on a King Air B-200 aircraft during 21 flights on 11 days to
make air quality observations over Houston, Texas. We present GCAS trace gas
retrievals of nitrogen dioxide (NO2) and formaldehyde
(CH2O), and compare these results with trace gas columns derived
from coincident in situ profile measurements of NO2 and
CH2O made by instruments on a P-3B aircraft, and with NO2
observations from ground-based Pandora spectrometers operating in direct-sun
and scattered light modes. GCAS tropospheric column measurements correlate
well spatially and temporally with columns estimated from the P-3B
measurements for both NO2 (r2=0.89) and CH2O
(r2=0.54) and with Pandora direct-sun (r2=0.85) and scattered light
(r2=0.94) observed NO2 columns. Coincident GCAS columns agree
in magnitude with NO2 and CH2O P-3B-observed columns to
within 10 % but are larger than scattered light Pandora tropospheric
NO2 columns by 33 % and direct-sun Pandora NO2
columns by 50 %.
Funder
National Aeronautics and Space Administration
Publisher
Copernicus GmbH
Subject
Atmospheric Science
Reference107 articles.
1. Aliwell, S. R., Van Roozendael, M., Johnston, P. V., Richter, A., Wagner, T.,
Arlander, D. W., Burrows, J. P., Fish, D. J., Jones, R. L., Tørnkvist,
K. K., Lambert, J.-C., Pfeilsticker, K., and Pundt, I.: Analysis for BrO in
zenith-sky spectra: An intercomparison exercise for analysis improvement,
J. Geophys. Res.-Atmos., 107, 4199,
https://doi.org/10.1029/2001JD000329, 2002. a 2. Baidar, S., Oetjen, H., Coburn, S., Dix, B., Ortega, I., Sinreich, R., and
Volkamer, R.: The CU Airborne MAX-DOAS instrument: vertical profiling of
aerosol extinction and trace gases, Atmos. Meas. Tech., 6, 719–739,
https://doi.org/10.5194/amt-6-719-2013, 2013. a 3. Barkley, M. P., Palmer, P. I., Kuhn, U., Kesselmeier, J., Chance, K., Kurosu,
T. P., Martin, R. V., Helmig, D., and Guenther, A.: Net ecosystem fluxes of
isoprene over tropical South America inferred from Global Ozone Monitoring
Experiment (GOME) observations of HCHO columns, J. Geophys. Res.-Atmos., 113, D20304, https://doi.org/10.1029/2008JD009863, 2008. a 4. Beirle, S., Lampel, J., Lerot, C., Sihler, H., and Wagner, T.: Parameterizing
the instrumental spectral response function and its changes by a
super-Gaussian and its derivatives, Atmos. Meas. Tech., 10, 581–598,
https://doi.org/10.5194/amt-10-581-2017, 2017. a 5. Boersma, K. F., Eskes, H. J., and Brinksma, E. J.: Error analysis for
tropospheric NO2 retrieval from space, J. Geophys. Res.-Atmos., 109, D04311,
https://doi.org/10.1029/2003JD003962, 2004. a, b, c
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