Regionalization of post-processed ensemble runoff forecasts

For many years, meteorological models have been run with perturbated initial conditions or parameters to produce ensemble forecasts that are used as a proxy of the uncertainty of the forecasts. However, the ensembles are usually both biased (the mean is systematically too high or too low, compare...

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Main Authors: J. O. Skøien, K. Bogner, P. Salamon, P. Smith, F. Pappenberger
Format: Article
Language:English
Published: Copernicus Publications 2016-05-01
Series:Proceedings of the International Association of Hydrological Sciences
Online Access:https://www.proc-iahs.net/373/109/2016/piahs-373-109-2016.pdf
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spelling doaj-7080b6c8af8e45cd863449977cd495f22020-11-24T23:15:29ZengCopernicus PublicationsProceedings of the International Association of Hydrological Sciences2199-89812199-899X2016-05-0137310911410.5194/piahs-373-109-2016Regionalization of post-processed ensemble runoff forecastsJ. O. Skøien0K. Bogner1P. Salamon2P. Smith3F. Pappenberger4European Commission, Joint Research Centre (JRC), Institute for Environment and Sustainability, Ispra, 21027 (VA), ItalySwiss Federal Institute WSL, Mountain Hydrology and Mass Movements, Birmensdorf, 8903, SwitzerlandEuropean Commission, Joint Research Centre (JRC), Institute for Environment and Sustainability, Ispra, 21027 (VA), ItalyEuropean Centre for Medium-Range Weather Forecasts, Reading, RG2 9AX, UKEuropean Centre for Medium-Range Weather Forecasts, Reading, RG2 9AX, UKFor many years, meteorological models have been run with perturbated initial conditions or parameters to produce ensemble forecasts that are used as a proxy of the uncertainty of the forecasts. However, the ensembles are usually both biased (the mean is systematically too high or too low, compared with the observed weather), and has dispersion errors (the ensemble variance indicates a too low or too high confidence in the forecast, compared with the observed weather). The ensembles are therefore commonly post-processed to correct for these shortcomings. Here we look at one of these techniques, referred to as Ensemble Model Output Statistics (EMOS) (Gneiting et al., 2005). Originally, the post-processing parameters were identified as a fixed set of parameters for a region. The application of our work is the European Flood Awareness System (<a href="http://www.efas.eu" target="_blank">http://www.efas.eu</a>), where a distributed model is run with meteorological ensembles as input. We are therefore dealing with a considerably larger data set than previous analyses. We also want to regionalize the parameters themselves for other locations than the calibration gauges. The post-processing parameters are therefore estimated for each calibration station, but with a spatial penalty for deviations from neighbouring stations, depending on the expected semivariance between the calibration catchment and these stations. The estimated post-processed parameters can then be used for regionalization of the postprocessing parameters also for uncalibrated locations using top-kriging in the rtop-package (Skøien et al., 2006, 2014). We will show results from cross-validation of the methodology and although our interest is mainly in identifying exceedance probabilities for certain return levels, we will also show how the rtop package can be used for creating a set of post-processed ensembles through simulations.https://www.proc-iahs.net/373/109/2016/piahs-373-109-2016.pdf
collection DOAJ
language English
format Article
sources DOAJ
author J. O. Skøien
K. Bogner
P. Salamon
P. Smith
F. Pappenberger
spellingShingle J. O. Skøien
K. Bogner
P. Salamon
P. Smith
F. Pappenberger
Regionalization of post-processed ensemble runoff forecasts
Proceedings of the International Association of Hydrological Sciences
author_facet J. O. Skøien
K. Bogner
P. Salamon
P. Smith
F. Pappenberger
author_sort J. O. Skøien
title Regionalization of post-processed ensemble runoff forecasts
title_short Regionalization of post-processed ensemble runoff forecasts
title_full Regionalization of post-processed ensemble runoff forecasts
title_fullStr Regionalization of post-processed ensemble runoff forecasts
title_full_unstemmed Regionalization of post-processed ensemble runoff forecasts
title_sort regionalization of post-processed ensemble runoff forecasts
publisher Copernicus Publications
series Proceedings of the International Association of Hydrological Sciences
issn 2199-8981
2199-899X
publishDate 2016-05-01
description For many years, meteorological models have been run with perturbated initial conditions or parameters to produce ensemble forecasts that are used as a proxy of the uncertainty of the forecasts. However, the ensembles are usually both biased (the mean is systematically too high or too low, compared with the observed weather), and has dispersion errors (the ensemble variance indicates a too low or too high confidence in the forecast, compared with the observed weather). The ensembles are therefore commonly post-processed to correct for these shortcomings. Here we look at one of these techniques, referred to as Ensemble Model Output Statistics (EMOS) (Gneiting et al., 2005). Originally, the post-processing parameters were identified as a fixed set of parameters for a region. The application of our work is the European Flood Awareness System (<a href="http://www.efas.eu" target="_blank">http://www.efas.eu</a>), where a distributed model is run with meteorological ensembles as input. We are therefore dealing with a considerably larger data set than previous analyses. We also want to regionalize the parameters themselves for other locations than the calibration gauges. The post-processing parameters are therefore estimated for each calibration station, but with a spatial penalty for deviations from neighbouring stations, depending on the expected semivariance between the calibration catchment and these stations. The estimated post-processed parameters can then be used for regionalization of the postprocessing parameters also for uncalibrated locations using top-kriging in the rtop-package (Skøien et al., 2006, 2014). We will show results from cross-validation of the methodology and although our interest is mainly in identifying exceedance probabilities for certain return levels, we will also show how the rtop package can be used for creating a set of post-processed ensembles through simulations.
url https://www.proc-iahs.net/373/109/2016/piahs-373-109-2016.pdf
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