OH, HO2 and RO2 Radical and OH Reactivity Observations during the Summertime in Beijing: High In-Situ Ozone Production and Evidence of a Missing OH Source.
Lisa Whalley1,2, Chunxiang Ye3, Eloise Slater3, Robert Woodward-Massey3, James D Lee4,5, Freya Anne Squires6, James R Hopkins5,6, Rachel Dunmore6, Marvin Shaw5,6, Jacqueline Hamilton7, Alistair C Lewis8,9, Leigh Crilley10, Louisa J Kramer10, William Bloss10 and Dwayne E Heard2,3, (1)University of Leeds, School of Chemistry, Leeds, LS2, United Kingdom, (2)National Centre for Atmospheric Science, Leeds, United Kingdom, (3)University of Leeds, School of Chemistry, Leeds, United Kingdom, (4)University of York, Wolfson Atmospheric Chemistry Laboratories, York, YO10, United Kingdom, (5)National Centre for Atmospheric Science, York, United Kingdom, (6)University of York, Wolfson Atmospheric Chemistry Laboratories, Department of Chemistry, York, United Kingdom, (7)University of York, Department of Chemistry, York, United Kingdom, (8)University of York, Wolfson Atmospheric Chemistry Laboratories, York, United Kingdom, (9)National Centre for Atmospheric Science, Wolfson Atmospheric Chemistry Laboratories, Department of Chemistry, York, United Kingdom, (10)University of Birmingham, School of Geography, Earth and Environmental Sciences, Birmingham, United Kingdom