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BrO vertical column BIRA-IASB
Jul 2002 to Dec 2005 *)     
IFE/IUP Bremen
Jan 2003 to April 2012 *)     
SAO
on request        
BrO profile IFE/IUP Bremen
Sep 2002 to April 2012 *)  p.valid
MPI Mainz/IUP Heidelberg
Sep 2002 to April 2012 *)  p. valid.
Environment Canada
on request   demonstrated
*): some restrictions on data use, see product details (click on institute)
BrO profile by IFE/IUP Bremen (last update: 12 Jul 2010)
validation summary Comparisons of BrO vertical profiles retrieved at IUP Bremen from SCIAMACHY limb measurements (version 3.2) to the results obtained from ground-based measurements are presented by Hendrick et al. 2009. The latter results are obtained at IASB-BIRA applying the profiling algorithm to ground-based zenith sky measurements of the scattered solar light. The comparison reveal a good agreement between both techniques. In the altitude range between 15 and 27 km the retrieved BrO profiles are found to agree better than 20%. Due to data availability issues comparisons are only done for three selected locations, namely, over Harestua (60N), OHP (45N), and Lauder (45S) ground stations.
available data September 2002 - April 2012. Data is available via the SCIA-ARC website. Restrictions for data use do apply.
point of contact Alexei Rozanov
algorithm description The algorithm is described in the Algorithm Document.
product details All details can be be found in the Product Specification Document v3.0 (or v1.1).
validation results The SCIA-ARC website also lists preliminary validation results.


SCIAMACHY BrO profile (IFE) validation literature:
  • Multi-year comparison of stratospheric BrO vertical profiles retrieved from SCIAMACHY limb and ground-based UV-visible measurements
    Hendrick, F., A. Rozanov, P.V. Johnston, H. Bovensmann, M. De Maziere, C. Fayt, C. Hermans, K. Kreher, W. Lotz, B.M. Sinnhuber, N. Theys, A. Thomas, J.P. Burrows and M. Van Roozendael
    Abstract/Article: Atmospheric Measurement Techniques 2, 273-285, 2009
    Product: BrO profile
    Institute: IUP/IFE, University of Bremen
    Method: Vertical profiles of stratospheric BrO retrieved daily from SCIAMACHY limb scatter data are copmpared to ground-based UV-visible observations performed at three gound based measuring sites in the 15 to 27 km altitude range for various periods, respectivel

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