Global Modeling of the Nitrate Radical (NO3)Forpresentand Pre-Industrial Scenarios
Atmospheric Research 164–165 (2015) 347–357 Contents lists available at ScienceDirect Atmospheric Research journal homepage: www.elsevier.com/locate/atmos Global modeling of the nitrate radical (NO3)forpresentand pre-industrial scenarios M.A.H. Khan a,M.C.Cookea,1, S.R. Utembe a,2, A.T. Archibald a,3,R.G.Derwentb,P.Xiaoa,C.J.Percivalc, M.E. Jenkin d, W.C. Morris a, D.E. Shallcross a,⁎ a Biogeochemistry Research Centre, School of Chemistry, University of Bristol, Cantock's Close, Bristol BS8 1TS, UK b rdscientific, Newbury, Berkshire, UK c The Centre for Atmospheric Science, The School of Earth, Atmospheric and Environmental Science, The University of Manchester, Simon Building, Brunswick Street, Manchester, M13 9PL, UK d Atmospheric Chemistry Services, Okehampton, Devon, EX20 4QB, UK article info abstract Article history: Increasing the complexity of the chemistry scheme in the global chemistry transport model STOCHEM to STOCHEM- Received 23 February 2015 CRI (Utembe et al., 2010) leads to an increase in NOx as well as ozone resulting in higher NO3 production over Received in revised form 26 May 2015 forested regions and regions impacted by anthropogenic emission. Peak NO3 is located over the continents near Accepted 8 June 2015 NO emission sources. NO is formed in the main by the reaction of NO with O ,andthesignificant losses of NO Available online 14 June 2015 x 3 2 3 3 are due to the photolysis and the reactions with NO and VOCs. Isoprene is an important biogenic VOC, and the possibility of HO recycling via isoprene chemistry and other mechanisms such as the reaction of RO with HO Keywords: x 2 2 STOCHEM-CRI has been investigated previously (Archibald et al., 2010a).
[Show full text]