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@ARTICLE{Li:20012,
      author       = {Li, X. and Brauers, T. and Häseler, R. and Bohn, B. and
                      Fuchs, H. and Hofzumahaus, A. and Holland, F. and Lou, S.
                      and Lu, K.D. and Rohrer, F. and Hu, M. and Zeng, L.M. and
                      Zhang, Y.H. and Garland, R.M. and Su, H. and Nowak, A. and
                      Wiedensohler, A. and Takegawa, N. and Shao, M. and Wahner,
                      A.},
      title        = {{E}xploring the atmospheric chemistry of nitrous acid
                      ({HONO}) at a rural site in {S}outhern {C}hina},
      journal      = {Atmospheric chemistry and physics},
      volume       = {12},
      issn         = {1680-7316},
      address      = {Katlenburg-Lindau},
      publisher    = {EGU},
      reportid     = {PreJuSER-20012},
      pages        = {1497 - 1513},
      year         = {2012},
      note         = {This work was supported by the China National Basic
                      Research and Development Program 2002CB410801, and the
                      National High Technology Research and Development Program of
                      China (863 Program) 2006AA06A301.},
      abstract     = {We performed measurements of nitrous acid (HONO) during the
                      PRIDE-PRD2006 campaign in the Pearl River Delta region 60 km
                      north of Guangzhou, China, for 4 weeks in June 2006. HONO
                      was measured by a LOPAP in-situ instrument which was setup
                      in one of the campaign supersites along with a variety of
                      instruments measuring hydroxyl radicals, trace gases,
                      aerosols, and meteorological parameters. Maximum diurnal
                      HONO mixing ratios of 1-5 ppb were observed during the
                      nights. We found that the nighttime build-up of HONO can be
                      attributed to the heterogeneous NO2 to HONO conversion on
                      ground surfaces and the OH + NO reaction. In addition to
                      elevated nighttime mixing ratios, measured noontime values
                      of approximate to 200 ppt indicate the existence of a
                      daytime source higher than the OH + NO -> HONO reaction.
                      Using the simultaneously recorded OH, NO, and HONO
                      photolysis frequency, a daytime additional source strength
                      of HONO (P-M) was calculated to be 0.77 ppb h(-1) on
                      average. This value compares well to previous measurements
                      in other environments. Our analysis of P-M provides evidence
                      that the photolysis of HNO3 adsorbed on ground surfaces
                      contributes to the HONO formation.},
      keywords     = {J (WoSType)},
      cin          = {IEK-8},
      ddc          = {550},
      cid          = {I:(DE-Juel1)IEK-8-20101013},
      pnm          = {Atmosphäre und Klima},
      pid          = {G:(DE-Juel1)FUEK491},
      shelfmark    = {Meteorology $\&$ Atmospheric Sciences},
      typ          = {PUB:(DE-HGF)16},
      UT           = {WOS:000300656500017},
      doi          = {10.5194/acp-12-1497-2012},
      url          = {https://juser.fz-juelich.de/record/20012},
}