Atmospheric Chemistry and Physics Discussions www.atmos-chem-phys-discuss.net 1680-7367 1680-7375 6 1 2006 10.5194/acpd-6-701-2006 http://www.atmos-chem-phys-discuss.net/6/701/2006/ http://www.atmos-chem-phys-discuss.net/6/701/2006/acpd-6-701-2006.html http://www.atmos-chem-phys-discuss.net/6/701/2006/acpd-6-701-2006.pdf 701 754 2006-01-24 20th Century trends and budget implications of trihalomethanes and dihalomethanes inferred from North GRIP firn air D. R. Worton W. T. Sturges J. Schwander R. Mulvaney J.-M. Barnola J. Chappellaz School of Environmental Sciences, University of East Anglia, Norwich, NR4 7TJ, UK Physics Institute, University of Berne, Berne, Switzerland British Antarctic Survey, Natural Environment Research Council, Cambridge, UK CNRS Laboratoire de Glaciologie et Geophysique de l’Environnement, Saint Martin d’Heres, France Four trihalomethane (THM; CHCl₃, CHBrCl₂, CHBr₂Cl and CHBr₃) and two dihalomethane (DHM; CH₂BrCl and CH₂Br₂) trace gases have been measured in air extracted from polar firn collected at the North Greenland Icecore Project (NGRIP) site. CHCl₃ was also measured in firn air from Devon Island (DI), Canada, Dronning Maud Land (DML), Antarctica and Dome Concordia (Dome C), Antarctica. All of these species are believed to be almost entirely of natural origin except for CHCl₃ where anthropogenic sources have been reported to contribute ~10% to the global burden. A 2-D atmospheric model was run for CHCl₃ using reported emission estimates to produce historical atmospheric trends at the three firn sites, which were then input into a firn diffusion model to produce concentration depth profiles that were compared against the measurements. The anthropogenic emissions were modified in order to give the best model fit to the firn data at NGRIP, Dome C and DML. As a result, the contribution of CHCl₃ from anthropogenic sources, mainly from pulp and paper manufacture, to the total chloroform budget appears to have been considerably underestimated and was likely to have been close to ~40% at the maximum in atmospheric CHCl₃ concentrations around 1990, declining to ~19% at the beginning of the 21st Century. We also show that the atmospheric burden of the brominated THM's in the northern hemisphere have increased over the 20th Century while CH₂Br₂ has remained constant over time implying that it is entirely of natural origin.