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Article detail · 2013

Understanding the role of the ground surface in HONO vertical structure High resolution vertical profiles during NACHTT 11

YÖKSİS OpenAlex Open access · bronze SJR Q1 JCR Q1 Citations 219 Top 10% Percentile 98.2% FWCI 8.25
Year
2013
Type
article

Data source split

  • YÖKSİS YÖKSİS article record
  • YÖKSİS venue Journal of Geophysical Research: Atmospheres
  • Catalog match (ISSN) Journal of Geophysical Research: Atmospheres
  • OpenAlex OpenAlex enrichment (abstract, citations, topics)

Abstract

OpenAlex · English

A negative‐ion proton‐transfer chemical ionization mass spectrometer was deployed on a mobile tower‐mounted platform during Nitrogen, Aerosol Composition, and Halogens on a Tall Tower (NACHTT) to measure nitrous acid (HONO) in the winter of 2011. High resolution vertical profiles revealed (i) HONO gradients in nocturnal boundary layers, (ii) ground surface dominates HONO production by heterogeneous uptake of NO2, (iii) significant quantities of HONO may be deposited to the ground surface at night, (iv) daytime gradients indicative of ground HONO production or emission, and (v) an estimated surface HONO reservoir comparable or larger than integrated daytime HONO surface production. Nocturnal integrated column observations of HONO and NO2 allowed direct evaluation of nocturnal ground surface uptake coefficients for these species (γNO2, surf = 2 × 10−6 to 1.6 × 10−5 and γHONO, surf = 2 × 10−5 to 2 × 10−4). A chemical model showed that the unknown source of HONO was highest in the morning, 4 × 106 molecules cm−3 s−1 (600 pptv h−1), declined throughout the day, and minimized near 1 × 106 molecules cm−3 s−1 (165 pptv h−1). The quantity of surface‐deposited HONO was also modeled, showing that HONO deposited to the surface at night was at least 25%, and likely in excess of 100%, of the calculated unknown daytime HONO source. These results suggest that if nocturnally deposited HONO forms a conservative surface reservoir, which can be released the following day, a significant fraction of the daytime HONO source can be explained for the NACHTT observations.

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Citations

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219 citations

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Authors

  1. T VandenBoer
  2. SS Brown
  3. JG Murphy
  4. WC Keene
  5. C Young
  6. AAP Pszenny
  7. S Kim
  8. C Warneke
  9. JA de Gouw
  10. JR Maben
  11. NL Wagner
  12. T Riedel
  13. JA Thornton
  14. DE Wolfe
  15. WP Dube
  16. FATMA ÖZTÜRK BOĞAZİÇİ ÜNİVERSİTESİ
  17. CA Brock
  18. N Grossberg
  19. B Lefer
  20. B Lerner
  21. AM Middlebrook
  22. JM Roberts