Atmospheric Chemistry and Physics Discussions www.atmos-chem-phys-discuss.net 1680-7367 1680-7375 8 4 2008 10.5194/acpd-8-13507-2008 http://www.atmos-chem-phys-discuss.net/8/13507/2008/ http://www.atmos-chem-phys-discuss.net/8/13507/2008/acpd-8-13507-2008.html http://www.atmos-chem-phys-discuss.net/8/13507/2008/acpd-8-13507-2008.pdf 13507 13553 2008-07-15 The ASSET intercomparison of stratosphere and lower mesosphere humidity analyses H. E. Thornton hazel.thornton@metoffice.gov.uk D. R. Jackson S. Bekki N. Bormann Q. Errera A. J. Geer W. A. Lahoz S. Rharmili Met Office, UK UPMC Univ Paris 06; CNRS; SA-IPSL, France European Centre for Medium-Range Weather Forecasts, UK Insitut d'Aéronomie Spatiale de Begique, BIRA–IASB, Belgium Norsk Institutt for Luftforskning, Norway This paper presents results from the first detailed intercomparison of stratosphere-lower mesosphere water vapour analyses; it builds on earlier results from the "Assimilation of ENVISAT Data" (ASSET) project. With the availability of high resolution, good quality Michelson Interferometer for Passive Atmospheric Sounding (MIPAS) water vapour profiles, the ability of four different atmospheric models to assimilate these data is tested. MIPAS data have been assimilated over September 2003 into the models of the European Centre for Medium Range Weather Forecasts (ECMWF), the Belgian Institute for Space and Aeronomy (BIRA-IASB), the French Service d'Aéronomie (SA-IPSL) and the UK Met Office. The resultant middle atmosphere humidity analyses are compared against independent satellite data from the Halogen Occultation Experiment (HALOE), the Polar Ozone and Aerosol Measurement (POAM III) and the Stratospheric Aerosol and Gas Experiment (SAGE II). The MIPAS water vapour profiles are generally well assimilated in the ECMWF, BIRA-IASB and SA systems, producing stratosphere-mesosphere water vapour fields where the main features compare favourably with the independent observations. However, the models are less capable of assimilating the MIPAS data where water vapour values are locally extreme or in regions of strong humidity gradients, such as the Southern Hemisphere lower stratosphere polar vortex. Differences in the analyses can be attributed to the choice of humidity control variable, how the background error covariance matrix is generated, the model resolution and its complexity, the degree of quality control of the observations and the use of observations near the model boundaries. Due to the poor performance of the Met Office analyses the results are not included in the intercomparison, but are discussed separately. The Met Office results highlight the pitfalls in humidity assimilation, and provide lessons that should be learnt by developers of stratospheric humidity assimilation systems. In particular, they underline the importance of the background error covariances in generating a realistic troposphere to mesosphere water vapour analysis. 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