Introduction Flashcards
Forecast (real-time forecast):
Estimation of a hydrometeorological variable for a specific time or a specific time period
Prognosis:
Estimation of a variabel for the future without relation to a specific time. This estimation is often associated with a probability.
Lead time
Difference between time when forecast is issued and future time for which variable is estimated. The forecast horizon is the maximum lead time (see Fig. 8.1).
Applications:
- Weather forecast (temperatur, precipitation, radiation, wind, etc.) for leisure, farming, water resources management, traffic, flight navigation, aviagion, etc. → meteorology
- Streamflow forecast (floods, droughts, inflow for dams) for water ressources management, navigation, hydro power, ecology, etc. → hydrology
- Water quality forecast (temperatur, O2-concentration, toxics for water ressources management, cooling water, ecology, disaster warning, etc. → water ressources management
Classification acc. to lead time:
- Shortest time forecast (Nowcasting):
- Lead time from minutes to a few hours
- Application for heavy storms, flash floods - Short time forecast:
- Lead time from hours to a few days
- Application e.g. for flood forecasting - Medium term forecast:
- Lead time from days to 2 weeks
- E.g. meteorological circulation pattern - Long term forecast:
- Lead time from weeks to months
- Application e.g. for low flow forecast
Ensemble-prediction:
(EPS-Ensemble-Prediction-System):
ensemble = a group of items viewed as a whole rather than individually.
Because of non-linearity of the systems and uncomplete knowledge an exact forecast is not possible
Different alternative forecasts can be used to assess the uncertainty
Ensembles are a set of alternative weather forecasts, valid for the same place and the same time
Uncertainty can be estimated by considering the frequency of certain states (e.g. 80% probability of precipitation)
Hydrological models can be driven with meteorological ensembles → ensemble flood prediction, gives e.g. uncertainty bands for discharge hydrographs or probabilities of threshold exceedings
Ensembles can be built by:
ensemble = a group of items viewed as a whole rather than individually.
a) Running several alternative models
b) Running the same model with different initial/ boundary conditions or model parameters
c) Combination of forecasts with different