FY 2007 Intercontinental Chemical Transport Experiment Ozonesonde Network Study (IONS) 2004: 2. Tropospheric ozone budgets and variability over northeastern North America Thompson, A.M., J.B. Stone, J. Witte, S.K. Miller, S.J. Oltmans, T.L. Kucsera, K.L. Ross, K.E. Pickering, J.T. Merrill, G. Forbes, D.W. Tarasick, E. Joseph, F.J. Schmidlin, W.W. McMillan, J. Warner, E.J. Hintsa, and J.E. Johnson J. Geophys. Res., 112, D12S13, doi: 10.1029/2006JD007670 (2007) Daily ozone soundings taken from the R/V Ronald H. Brown from 7 July through 11 August 2004 as part of the Intercontinental Chemical Transport Experiment (INTEX) Ozonesonde Network Study (IONS) are used to investigate the vertical structure of ozone over the Gulf of Maine and to characterize variability in sources of tropospheric ozone: stratosphere, regional convection and lightning, advection, and local boundary layer pollution. These soundings were part of a network of twelve IONS (http://croc.gsfc.nasa.gov/intex/ions.html) stations that launched ozonesonderadiosonde packages over the United States and maritime Canada during the INTEX/ International Consortium for Atmospheric Research on Transport and Transformation (ICARTT)/New England Air Quality Study (NEAQS) project from 1 July to 15 August 2004. Four of the IONS stations were in mid-Atlantic and northeast United States; four were in southeastern Canada. Although the INTEX/ICARTT goal was to examine pollution influences under stable high-pressure systems, northeastern North America (NENA) during IONS was dominated by weak frontal systems that mixed aged pollution and stratospheric ozone with ozone from more recent pollution and lightning. These sources are quantified to give tropospheric ozone budgets for individual soundings that are consistent with tracers and meteorological analyses. On average, for NENA stations in July-August 2004, tropospheric ozone was composed of the following: 10–15% each local boundary layer and regional sources (the latter including that due to lightningderived NO) and 20–25% stratospheric ozone, with the balance (~50%) a mixture of recently advected ozone and aged air of indeterminate origin. Feature Publications | Outstanding Scientific Publications Contact Sandra Bigley | Help
