Nitrogen dioxide and formaldehyde measurements from the GEOstationary Coastal...

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Nowlan, C., X. Liu, S. Janz, M. Kowalewski, K. Chance, M. B. Follette-Cook, A. Fried, G. G. Abad, J. R. Herman, L. Judd, H. Kwon, C. P. Loughner, K. E. Pickering, D. Richter, E. Spinei, J. G. Walega, P. Weibring, and A. Weinheimer (2018), Nitrogen dioxide and formaldehyde measurements from the GEOstationary Coastal and Air Pollution Events (GEO-CAPE) Airborne Simulator over Houston, Texas, Atmos. Meas. Tech., 11, 5941-5964, doi:10.5194/amt-11-5941-2018.
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 pushbroom 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 (CH2 O), and compare these results with trace gas columns derived from coincident in situ profile measurements of NO2 and CH2 O 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 (r 2 = 0.89) and CH2 O (r 2 = 0.54) and with Pandora direct-sun (r 2 = 0.85) and scattered light (r 2 = 0.94) observed NO2 columns. Coincident GCAS columns agree in magnitude with NO2 and CH2 O P-3B-observed columns to within 10 % but are larger than scattered light

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