Precipitation and temperature ensemble forecasts from single-value forecasts

To perform an objective validation of the database, the forecasts of the Solar Forecast Similarity method have been compared to the measurements from nine BSRN stations:

This last step does NOT require that all indicator be converted - best if only a small percent need to be reacted to make the change visible.. Note the

follows from Rouch6's theorem thatf has exactly one l-point on the ring domain la,lq-Ll2=lzl=la,lqu2... positive

Figure 10: RMSE in W m −2 against the maximal number of members chosen from each center ensemble; (blue: no sorting), (green: sorting full ensemble), (red: sorting by center),

Figure 9 shows the relative value of the ECMWF EPS (ECEPS) and the control forecast (ECL) for the total range of C/L ratios (0 to 1). For each C/L, the statistical sig- nificance of

The model included a turbulence parameterization (Cuxart et al., 2000), a mi- crophysical scheme that predicts the evolution of the mix- ing ratios of six water species (water

The numerical solution of the temperature for the radiative heat transfer model (4.2) at steady state, with a buffer inside the fluid zone (top) and a buffer partially outside the

These space forms are isometric quotients S n (r)/Γ of round spheres and naturally carry a unit Hopf vector field which is critical for the volume functional.. So, in contrast with