The use of NO₂ absorption cross section temperature sensitivity to derive NO₂ profile temperature and stratospheric–tropospheric column partitioning from visible direct-sun DOAS measurements

• Main Authors: E. Spinei, A. Cede, W. H. Swartz, J. Herman, G. H. Mount
• Format: Article
• Language: English
• Published: Copernicus Publications 2014-12-01
• Series: Atmospheric Measurement Techniques
• Online Access: http://www.atmos-meas-tech.net/7/4299/2014/amt-7-4299-2014.pdf
• ISSN: 1867-1381; 1867-8548

This paper presents a temperature sensitivity method (TESEM) to accurately calculate total vertical NO₂ column, atmospheric slant NO₂ profile-weighted temperature (<i>T</i>), and to separate stratospheric and tropospheric columns from direct-sun (DS), ground-based measurements using the retrieved <i>T</i>. TESEM is based on differential optical absorption spectroscopy (DOAS) fitting of the linear temperature-dependent NO₂ absorption cross section, σ (<i>T</i>), regression model (Vandaele et al., 2003). Separation between stratospheric and tropospheric columns is based on the primarily bimodal vertical distribution of NO₂ and an assumption that stratospheric effective temperature can be represented by temperature at 27 km ± 3 K, and tropospheric effective temperature is equal to surface temperature within 3–5 K. These assumptions were derived from the Global Modeling Initiative (GMI) chemistry-transport model (CTM) simulations over two northern midlatitude sites in 2011. <br><br> TESEM was applied to the Washington State University Multi-Function DOAS instrument (MFDOAS) measurements at four midlatitude locations with low and moderate NO₂ anthropogenic emissions: (1) the Jet Propulsion Laboratory's Table Mountain Facility (JPL-TMF), CA, USA (34.38° N/117.68° W); (2) Pullman, WA, USA (46.73° N/117.17° W); (3) Greenbelt, MD, USA (38.99° N/76.84° W); and (4) Cabauw, the Netherlands (51.97° N/4.93° E) during July 2007, June–July 2009, July–August and October 2011, November 2012–May 2013, respectively. NO₂ <i>T</i> and total, stratospheric, and tropospheric NO₂ vertical columns were determined over each site.