28 March 1995 A revision to the definition of
tropopause for the humidity analysis was introduced.
4 April 1995 A new
version of the forecast model (IFS cycle13r4) was implemented including:
- new prognostic cloud scheme;
- smoothed mean orography and new subgrid orography parametrization;
- modified quasi-regular (reduced) Gaussian grid.
Specific humidity on model levels and pressure levels
was changed from spherical harmonic to quasi regular Gaussian grid field.
In addition, three new quasi-regular Gaussian grid fields on model levels
were introduced: cloud liquid water content, cloud ice water content
and cloud cover. Fields of low, medium, high and total cloud cover continue
to be produced, but convective cloud cover is no longer produced.
This change led to much improved representation of
cloud cover, with large reductions from the previous systematic negative
biases, especially during the day. A significant reduction in summertime
warm bias of two-metre temperature, was achieved. The change improves
the precipitation forecast, with smoother precipitation patterns and
reduced spin-up problems in the early range of the forecast.
In addition, the parametrization of the ocean surface
albedo has been changed to better represent the variation of reflectivity
with solar zenith angle.
An article from the ECMWF Newsletter describing
these changes is given in pdf
(396
KB) file.
28 November 1995 A revised form of the continuity
equation was implemented in the forecast model, resulting in a reduction
of noise in all lower tropospheric fields previously experienced near
mountains. In particular, the fields of mean sea level pressure, geopotential
height and temperature are smoother, and the near surface wind is better
represented.