Dry deposition of NOx to grass in rural east Anglia |
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| Affiliation: | 1. State Key Laboratory of Severe Weather & CMA Key Laboratory of Atmospheric Chemistry, Chinese Academy of Meteorological Sciences, Beijing 100081, China;2. China Waterborne Transport Research Institute, Beijing 100088, China;3. CMA Meteorological Observation Centre, Beijing 100081, China;4. Shangdianzi Regional Air Background Station, Beijing, Meteorological Bureau, Beijing 101507, China;5. Meteorological Bureau of Shijiazhuang, Shijiazhuang 050081, China;1. Institute of Geophysics, University of Tehran, Tehran, Iran;2. Iranian National Institute for Oceanography and Atmospheric Science, Tehran, Iran;1. Key Laboratory of Mesoscale Severe Weather, Ministry of Education, Nanjing University, Nanjing 210023, China;2. School of Atmospheric Sciences, Nanjing University, Nanjing 210023, China;3. Department of Atmospheric Science, Yunnan University, Kunming 650091, China;1. Samara National Research University, Samara, 443086, Russia;2. Department of Mechanical Engineering, University of California at Berkeley, Berkeley, California, 94720-1740, U.S.A.;3. Department of Chemistry and Biochemistry, Florida International University, Miami, FL, 33199, U.S.A. |
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| Abstract: | A single set of analytical instruments was utilised, with a two-level sampling system, to determine the dry deposition of NOx by the gradient method over a cut-grass field during day-time in the spring. The range of deposition velocities is around O.1–0.6 cm s−1, and the bulk surface resistance range is about O.8–5.6 s cm−1. |
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