Accelerating growth of HFC-227ea (1,1,1,2,3,3,3-heptafluoropropane) in the atmosphere

We report the first measurements of 1,1,1,2,3,3,3-heptafluoropropane (HFC-227ea), a substitute for ozone depleting compounds, in air samples originating from remote regions of the atmosphere and present evidence for its accelerating growth. Observed mixing ratios ranged from below 0.01 ppt in deep f...

Full description

Bibliographic Details
Main Authors: Laube, J.C., Martinerie, P., Witrant, E., Blunier, T., Schwander, J., Brenninkmeijer, C.A.M., Schuck, T.J., Bolder, M., Rockmann, T., van der Veen, C., Bönisch, H., Engel, A., Mills, G.P., Newland, M.J., Oram, D.E., Reeves, C.E., Sturges, W.T.
Other Authors: Marine and Atmospheric Research, Sub Algemeen Marine & Atmospheric Res, Sub Atmospheric physics and chemistry
Format: Article in Journal/Newspaper
Language:English
Published: 2010
Subjects:
Online Access:https://dspace.library.uu.nl/handle/1874/203008
Description
Summary:We report the first measurements of 1,1,1,2,3,3,3-heptafluoropropane (HFC-227ea), a substitute for ozone depleting compounds, in air samples originating from remote regions of the atmosphere and present evidence for its accelerating growth. Observed mixing ratios ranged from below 0.01 ppt in deep firn air to 0.59 ppt in the current northern mid-latitudinal upper troposphere. Firn air samples collected in Greenland were used to reconstruct a history of atmospheric abundance. Year-on-year increases were deduced, with acceleration in the growth rate from 0.029 ppt per year in 2000 to 0.056 ppt per year in 2007. Upper tropospheric air samples provide evidence for a continuing growth until late 2009. Furthermore we calculated a stratospheric lifetime of 370 years from measurements of air samples collected on board high altitude aircraft and balloons. Emission estimates were determined from the reconstructed atmospheric trend and suggest that current "bottom-up" estimates of global emissions for 2005 are too high by a factor of three.