Last updated: September 2008
Radiance data from polar orbiting and geostationary satellites (ATOVS, AIRS/IASI, and SEVIRI) are used for LME (and its derivates) in order to improve forecast quality of LME and also quality of boundary values for subsequent models as LMK. Assimilation of level 1 radiance data is per- formed in two steps: Firstly, profiles (including screen level and skin values) of temperature and humidity are retrieved from the radiances using a 1DVar analysis approach. Secondly, these profiles are assimilated with the nudging scheme of the COSMO similarly to other conventional data.
Future domains of COSMO installations will include large parts of data sparse areas (e. g. north Atlantic for LME) for conventional data. The use of satellite radiances especially over sea has the potential to provide essential information in order to improve analyses and subsequent forecasts on the regional domain.
Prepare technical implementation for MSG data
Prepare technical implementation for ATOVS using developments for MSG
Adapt technical implementation and developments for AIRS/IASI
Setup monitoring: run implementation on a day by day basis and generate time series of observed minus background radiances for bias correction, evaluate statistics for selecting viable channels and adjusting observation errors
Cloud / rain detection and bias correction
Derive and tune background errors over sea and over land; assess use of MSG data over land
Validate usage of EMCWF climate values above LM model top for radiative transfer computation and compare it to extrapolation with statistical regression
Validate retrievals by comparing them to radiosonde data and to model profiles
Tune nudging of 1D-Var retrievals, nudging coefficients, etc (with case studies)