Significant concentrations of nitryl chloride observed in rural continental Europe associated with the influence of sea salt chloride and anthropogenic emissions

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 2...

Full description

Saved in:
Bibliographic Details
Published inGeophysical research letters Vol. 39; no. 10
Main Authors Phillips, G. J., Tang, M. J., Thieser, J., Brickwedde, B., Schuster, G., Bohn, B., Lelieveld, J., Crowley, J. N.
Format Journal Article
LanguageEnglish
Published Washington, DC Blackwell Publishing Ltd 28.05.2012
American Geophysical Union
John Wiley & Sons, Inc
Subjects
Online AccessGet full text

Cover

Loading…
More Information
Summary: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 O3 production. Key Points Nitryl chloride exists in significant mixing fractions over Europe Nitryl chloride is likely of marine origin, deriving from aged sea salt and N2O5 Nitryl chloride is a significant radical source in early morning
Bibliography:ArticleID:2012GL051912
ark:/67375/WNG-LR3M7SSN-6
istex:429C6418B405D0F6726928A748D4FFB5C10B9E10
ObjectType-Article-1
SourceType-Scholarly Journals-1
ObjectType-Feature-2
content type line 23
ISSN:0094-8276
1944-8007
DOI:10.1029/2012GL051912