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024 | 7 | _ | |a 10.1029/2012GL051912 |2 DOI |
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084 | _ | _ | |2 WoS |a Geosciences, Multidisciplinary |
100 | 1 | _ | |a Phillips, G.J. |b 0 |0 P:(DE-HGF)0 |
245 | _ | _ | |a Significant concentrations of nitryl chloride observed in rural continental Europe associated with the influence of sea salt chloride and anthropogenic emissions |
260 | _ | _ | |a Washington, DC |b American Geophysical Union |c 2012 |
300 | _ | _ | |a L10811 |
336 | 7 | _ | |a Journal Article |0 PUB:(DE-HGF)16 |2 PUB:(DE-HGF) |
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440 | _ | 0 | |a Geophysical Research Letters |x 0094-8276 |0 2249 |y L10811 |v 39 |
500 | _ | _ | |3 POF3_Assignment on 2016-02-29 |
500 | _ | _ | |a We acknowledge the ECMWF and the EU-funded project MACC for the sea salt optical depth forecast data (http://www.gmes-atmosphere.eu). We thank H. Bingemer and the staff and department of Geophysics of the Johann Wolfgang Goethe-University, Frankfurt am Main for logistical support and the use of the Taunus Observatory. We acknowledge the help and support of all PARADE participants and our colleagues in the department of atmospheric chemistry, MPIC. |
520 | _ | _ | |a We present the first measurements of nitryl chloride (ClNO2) over continental Europe. Significant quantities of ClNO2, up to 800 pptv, were measured at a mountaintop field site in Hessen, southwest Germany. ClNO2 was detected during the majority of nights between the 15th August and 16th September 2011, its largest mixing ratios being associated with air masses influenced by sea salt and anthropogenic NOx emissions. ClNO2 persisted in measurable quantities until early afternoons on days with low photolysis frequencies. As a consequence, early morning production rates of Cl atoms could significantly exceed the production of OH via ozone photolysis, likely leading to increased O-3 production. Citation: Phillips, G. J., M. J. Tang, J. Thieser, B. Brickwedde, G. Schuster, B. Bohn, J. Lelieveld, and J. N. Crowley (2012), Significant concentrations of nitryl chloride observed in rural continental Europe associated with the influence of sea salt chloride and anthropogenic emissions, Geophys. Res. Lett., 39, L10811, doi:10.1029/2012GL051912. |
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700 | 1 | _ | |a Brickwedde, B. |b 3 |0 P:(DE-HGF)0 |
700 | 1 | _ | |a Schuster, G. |b 4 |0 P:(DE-HGF)0 |
700 | 1 | _ | |a Bohn, B. |b 5 |u FZJ |0 P:(DE-Juel1)2693 |
700 | 1 | _ | |a Lelieveld, J. |b 6 |0 P:(DE-HGF)0 |
700 | 1 | _ | |a Crowley, J.N. |b 7 |0 P:(DE-HGF)0 |
773 | _ | _ | |a 10.1029/2012GL051912 |g Vol. 39 |q 39 |0 PERI:(DE-600)2021599-X |t Geophysical research letters |v 39 |y 2012 |x 0094-8276 |p L10811 |
856 | 7 | _ | |u http://dx.doi.org/10.1029/2012GL051912 |
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