Seasonal streamflow forecasts in the Ahlergaarde catchment, Denmark: the effect of preprocessing and post-processing on skill and statistical consistency
In the present study we analyze the effect of bias adjustments in both meteorological and streamflow forecasts on the skill and statistical consistency of monthly streamflow and yearly minimum daily flow forecasts. Both raw and preprocessed meteorological seasonal forecasts from the European Centre...
Gespeichert in:
Veröffentlicht in: | Hydrology and earth system sciences 2018-07, Vol.22 (7), p.3601-3617 |
---|---|
Hauptverfasser: | , , , , |
Format: | Artikel |
Sprache: | eng |
Schlagworte: | |
Online-Zugang: | Volltext |
Tags: |
Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
|
Zusammenfassung: | In the present study we analyze the
effect of bias adjustments in both meteorological and streamflow forecasts on
the skill and statistical consistency of monthly streamflow and yearly
minimum daily flow forecasts. Both raw and preprocessed meteorological seasonal forecasts from the European Centre for Medium-Range
Weather Forecasts (ECMWF) are used as inputs to a spatially distributed,
coupled surface–subsurface hydrological model based on the MIKE SHE code.
Streamflow predictions are then generated up to 7 months in advance. In
addition to this, we post-process streamflow predictions using an empirical
quantile mapping technique. Bias, skill and statistical consistency are the
qualities evaluated throughout the forecast-generating strategies and we
analyze where the different strategies fall short to improve them. ECMWF
System 4-based streamflow forecasts tend to show a lower accuracy level than
those generated with an ensemble of historical observations, a method
commonly known as ensemble streamflow prediction (ESP). This is particularly
true at longer lead times, for the dry season and for streamflow stations
that exhibit low hydrological model errors. Biases in the mean are better
removed by post-processing that in turn is reflected in the higher level of
statistical consistency. However, in general, the reduction of these biases
is not sufficient to ensure a higher level of accuracy than the ESP
forecasts. This is true for both monthly mean and minimum yearly streamflow
forecasts. We discuss the importance of including a better estimation of the
initial state of the catchment, which may increase the capability of the
system to forecast streamflow at longer leads. |
---|---|
ISSN: | 1607-7938 1027-5606 1607-7938 |
DOI: | 10.5194/hess-22-3601-2018 |