Versions Compared

Key

  • This line was added.
  • This line was removed.
  • Formatting was changed.

...

  • Large-scale cold outbreaks or heat waves lasting for (say) three days or more.
  • Intense synoptic-scale dynamic precipitation and extreme synoptic-scale winds.
  • Strong and organised convection.

The ENS is Ensembles are well equipped to forecast the first two types of anomalous events with the current resolution.  Extreme   Extreme convective features are less well captured but can, to some extent, be added by experienced forecasters, or via statistical interpretation schemes.

The Extreme Forecast Index (EFI) and  and Shift of Tails (SOT) have  have been developed to show forecasters how ongoing weather event probabilities relate to time-of-year dependant climatological conditions at every location. So these parameters also .   EFI and SOT parameters for CAPE and CAPE-shear have shown some noteworthy skill in foretelling of severe convective events that the IFS itself cannot predict directly.

These parameters have some general applicability for impact forecasting , because as they indirectly relate to local return periods across the globe, for different types of adverse weather. In this context forecasters will  Forecasters can also benefit from an understanding of the local resilience of man-made infrastructure in the face of natural hazards. Moreover, the recently added EFI and SOT parameters for CAPE and CAPE-shear have also shown some noteworthy skill in foretelling of severe convective events that the IFS itself cannot predict directly.

The forecaster’s role

Considerations of probabilityjumpiness, and the forecaster’s role apply in particular to extreme weather forecasting.  Calibrating or otherwise applying statistically based modifications to extreme weather events is very difficult because of their rarity.  However, forecasters can accumulate some experience of the IFS models’ capabilities from extreme weather events in neighbouring areas.  Complementary information, in particular forecasts from different NWP models and/or IFS runs, might motivate forecasters to upgrade or downgrade the probabilities.  Forecasters also have a unique role in supplying probability forecasts of events that are not explicitly covered by the ECMWF forecast products (e.g. thunderstorms).   Perhaps the most important task is to help end-users, such as regional and national authorities, to make the optimal decision about protective action.

...