E. Andersson et al., USE OF CLOUD-CLEARED RADIANCES IN 3-DIMENSIONAL 4-DIMENSIONAL VARIATIONAL DATA ASSIMILATION, Quarterly Journal of the Royal Meteorological Society, 120(517), 1994, pp. 627-653
The direct use of TOVS (TIROS Operational Vertical Sounder) cloud-clea
red radiances in a three/four-dimensional variational data assimilatio
n scheme is described. This scheme uses a fast radiative transfer mode
l and its adjoint. Radiances are used together with all the other obse
rvational data. Global spectral fields of mass, wind and humidity are
analysed simultaneously under certain mass/wind balance constraints wh
ich control the degree to which gravity waves enter into the analysis.
In this way the need for a subsequent initialization is avoided. The
scheme thus combines retrieval, analysis and initialization in one ste
p and makes it possible to achieve a more optimal combination of the i
nformation contained in the radiances, the conventional data and the b
ackground (a six-hour forecast). At spectral truncation T63, a global
three-dimensional variational analysis (3D-Var) of TOVS radiances and
conventional data is compared with the ECMWF operational Optimum Inter
polation scheme, which uses TOVS radiance information in the form of p
rofiles of temperature and humidity, retrieved using a one-dimensional
variational method. The results of 3D-Var are in good agreement with
the operational analysis at the same resolution. In an application of
the four-dimensional scheme (4D-Var), data covering a period of 24 hou
rs were used simultaneously. In 4D-Var consistency in time is ensured
through the evolution of the forecast model and its adjoint. Using the
adiabatic version of the ECMWF forecast model (spectral resolution T4
2) we show that 4D-Var is able to extract additional information from
the dynamics of the model. In particular we show an impact on the trop
ical wind field from the use of the humidity-sensitive TOVS channels.