Atmospheric Chemistry and Physics (Mar 2010)

Nocturnal nitrogen oxides at a rural mountain-site in south-western Germany

  • J. N. Crowley,
  • G. Schuster,
  • N. Pouvesle,
  • U. Parchatka,
  • H. Fischer,
  • B. Bonn,
  • H. Bingemer,
  • J. Lelieveld

Journal volume & issue
Vol. 10, no. 6
pp. 2795 – 2812

Abstract

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A new, two-channel instrument for simultaneous NO<sub>3</sub> and N<sub>2</sub>O<sub>5</sub> monitoring was used to make the first comprehensive set of nocturnal NO<sub>x</sub> measurements (NO, NO<sub>2</sub>, NO<sub>3</sub> and N<sub>2</sub>O<sub>5</sub>) at the Taunus Observatory, a rural mountain site (Kleiner Feldberg) in South-western Germany. In May 2008, NO<sub>3</sub> and N<sub>2</sub>O<sub>5</sub> mixing ratios were well above the instrumental detection limit (a few ppt) on all nights of the campaign and were characterised by large variability. The concentrations of NO<sub>3</sub>, N<sub>2</sub>O<sub>5</sub> and NO<sub>2</sub> were consistent with the equilibrium constant, <I>K</I><sub>2</sub>, defining the rates of formation and thermal dissociation of N<sub>2</sub>O<sub>5</sub>. A steady-state lifetime analysis is consistent with the loss of nocturnal NO<sub>x</sub> being dominated by the reaction of NO<sub>3</sub> with volatile organic compounds in this forested region, with N<sub>2</sub>O<sub>5</sub> uptake to aerosols of secondary importance. Analysis of a limited dataset obtained at high relative humidity indicated that the loss of N<sub>2</sub>O<sub>5</sub> by reaction with water vapour is less efficient (&gt;factor 3) than derived using laboratory kinetic data. The fraction of NO<sub>x</sub> present as NO<sub>3</sub> and N<sub>2</sub>O<sub>5</sub> reached ~20% on some nights, with night-time losses of NO<sub>x</sub> competing with daytime losses.