Earth Syst. Sci. Data, 6, 105–115, 2014 Earth System www.earth-syst-sci-data.net/6/105/2014/ Science doi:10.5194/essd-6-105-2014 © Author(s) 2014. CC Attribution 3.0 License. Open Access Open Data Atmospheric ozone above Troll station, Antarctica observed by a ground based microwave radiometer M. Daae1,2, C. Straub1,3, P. J. Espy1,2, and D. A. Newnham4 1Norwegian University of Science and Technology, Department of Physics, Trondheim, Norway 2Birkeland Centre for Space Science, Bergen, Norway 3Institute of Applied Physics, University of Bern, Bern, Switzerland 4British Antarctic Survey, Cambridge, UK Correspondence to: M. Daae (
[email protected]) Received: 6 August 2013 – Published in Earth Syst. Sci. Data Discuss.: 5 September 2013 Revised: 11 February 2014 – Accepted: 16 February 2014 – Published: 21 March 2014 Abstract. This paper describes the stratospheric and mesospheric ozone profiles retrieved from spectral mea- surements of the 249.96 GHz O3 line, using the British Antarctic Survey’s ground-based Microwave Radiome- ter at Troll (BAS-MRT), Antarctica (72◦010 S, 02◦320 E, 62◦ Mlat). The instrument operated at Troll from February 2008 through January 2010, and hourly averaged spectra were used to retrieve approximately 20 ozone profiles per day. The ozone profiles cover the pressure range from 3 hPa to 0.02 hPa (approximately 38 to 72 km) which includes the topside of the stratospheric ozone layer and the peak of the tertiary maximum. Comparing the retrieved ozone volume mixing ratio (vmr) values to Aura/MLS and SD-WACCM shows no significant bias to within the instrumental uncertainties.