New trace gas climatology derived from the GEMS project
Assimilation of cloud-affected radiances for infra-red instruments
Improved assimilation of land-surface sensitive channels
Assimilation of total-column water vapour data from the MERIS instrument (over land)
Variational bias correction for ozone satellite data
Improved quality control (using Huber norm) of conventional observations
Improved background-error statistics for humidity; new humidity formulation in 4D- Var
Weak-constraint 4D- Var taking into account systematic model errors in the stratosphere
Further revision of the snow scheme (re-whitening, melting, ...)
Wave damping in wind input source term for ocean waves
Routine monitoring of soil moisture observations from Metop-A ASCAT
ENS
Revised stochastic physics
Meteorological impact
HRES
Northern hemisphere: statistically significant improvement in the tropospheric scores.
European: weaker statistical significance.
Southern hemisphere impact is essentially neutral.
An increased negative temperature bias is present at around 100 hPa. However, there is evidence that the quality of the analysis of temperature in the stratosphere has improved, as seen from an improved fit between observations and background fields.
The revision of the snow scheme has led to improved (colder) 2m-temperature in North America and Northern Asia in April and May.
Temperature over Europe is not significantly changed.
ENS
improved probabilistic scores for temperature at 850 hPa in the tropics.