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Regionalization of post-processed ensemble runoff forecasts

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Regionalization of post-processed ensemble runoff forecasts. / Skøien, Jon Olav; Bogner, Konrad; Salamon, Peter et al.
In: IAHS-AISH Proceedings and Reports, Vol. 373, 12.05.2016, p. 109-114.

Research output: Contribution to Journal/MagazineConference articlepeer-review

Harvard

Skøien, JO, Bogner, K, Salamon, P, Smith, P & Pappenberger, F 2016, 'Regionalization of post-processed ensemble runoff forecasts', IAHS-AISH Proceedings and Reports, vol. 373, pp. 109-114. https://doi.org/10.5194/piahs-373-109-2016

APA

Skøien, J. O., Bogner, K., Salamon, P., Smith, P., & Pappenberger, F. (2016). Regionalization of post-processed ensemble runoff forecasts. IAHS-AISH Proceedings and Reports, 373, 109-114. https://doi.org/10.5194/piahs-373-109-2016

Vancouver

Skøien JO, Bogner K, Salamon P, Smith P, Pappenberger F. Regionalization of post-processed ensemble runoff forecasts. IAHS-AISH Proceedings and Reports. 2016 May 12;373:109-114. doi: 10.5194/piahs-373-109-2016

Author

Skøien, Jon Olav ; Bogner, Konrad ; Salamon, Peter et al. / Regionalization of post-processed ensemble runoff forecasts. In: IAHS-AISH Proceedings and Reports. 2016 ; Vol. 373. pp. 109-114.

Bibtex

@article{172ff103fe2e4f96bf3b9f7c3377c811,
title = "Regionalization of post-processed ensemble runoff forecasts",
abstract = "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 (http://www.efas.eu), 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 (Sk{\o}ien 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.",
author = "Sk{\o}ien, {Jon Olav} and Konrad Bogner and Peter Salamon and Paul Smith and Florian Pappenberger",
year = "2016",
month = may,
day = "12",
doi = "10.5194/piahs-373-109-2016",
language = "English",
volume = "373",
pages = "109--114",
journal = "IAHS-AISH Proceedings and Reports",
issn = "0144-7815",
note = "7th International Water Resources Management Conference of IAHS-ICWRS 2016 ; Conference date: 18-05-2016 Through 20-05-2016",

}

RIS

TY - JOUR

T1 - Regionalization of post-processed ensemble runoff forecasts

AU - Skøien, Jon Olav

AU - Bogner, Konrad

AU - Salamon, Peter

AU - Smith, Paul

AU - Pappenberger, Florian

PY - 2016/5/12

Y1 - 2016/5/12

N2 - 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 (http://www.efas.eu), 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.

AB - 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 (http://www.efas.eu), 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.

U2 - 10.5194/piahs-373-109-2016

DO - 10.5194/piahs-373-109-2016

M3 - Conference article

AN - SCOPUS:85044543673

VL - 373

SP - 109

EP - 114

JO - IAHS-AISH Proceedings and Reports

JF - IAHS-AISH Proceedings and Reports

SN - 0144-7815

T2 - 7th International Water Resources Management Conference of IAHS-ICWRS 2016

Y2 - 18 May 2016 through 20 May 2016

ER -