Probabilistic flood forecasting on the Rhone River: evaluation with ensemble and analogue-based precipitation forecasts
Hydrological ensemble forecasting performances are analysed over 5 basins up to 2000 km2 in the French Upper Rhone region. Streamflow forecasts are issued at an hourly time step from lumped ARX rainfall-runoff models forced by different precipitation forecasts. Ensemble meteorological forecasts from...
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2016-01-01
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Online Access: | http://dx.doi.org/10.1051/e3sconf/20160718011 |
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doaj-99637c281ad347e984a413a06326da402021-03-02T07:34:36ZengEDP SciencesE3S Web of Conferences2267-12422016-01-0171801110.1051/e3sconf/20160718011e3sconf_flood2016_18011Probabilistic flood forecasting on the Rhone River: evaluation with ensemble and analogue-based precipitation forecastsBellier Joseph0Zin Isabella1Siblot Stanislas2Bontron Guillaume3Université Grenoble Alpes, Laboratoire d’étude des Transferts en Hydrologie et EnvironnementUniversité Grenoble Alpes, Laboratoire d’étude des Transferts en Hydrologie et EnvironnementCompagnie Nationale du RhôneCompagnie Nationale du RhôneHydrological ensemble forecasting performances are analysed over 5 basins up to 2000 km2 in the French Upper Rhone region. Streamflow forecasts are issued at an hourly time step from lumped ARX rainfall-runoff models forced by different precipitation forecasts. Ensemble meteorological forecasts from ECMWF and NCEP are considered, as well as analogue-based forecasts fed by their corresponding control forecast. Analogue forecasts are rearranged using an adaptation of the Schaake-Shuffle method in order to ensure the temporal coherence. A new evaluation approach is proposed, separating forecasting performances on peak amplitudes and peak timings for high flow events. Evaluation is conducted against both simulated and observed streamflow (so that relative meteorological and hydrological uncertainties can be assessed), by means of CRPS and rank histograms, over the 2007-2014 period. Results show a general agreement of the forecasting performances when averaged over the 5 basins. However, ensemble-based and analogue-based streamflow forecasts produce a different signature on peak events in terms of bias, spread and reliability. Strengths and weaknesses of both approaches are discussed as well as potential improvements, notably towards their merging.http://dx.doi.org/10.1051/e3sconf/20160718011 |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Bellier Joseph Zin Isabella Siblot Stanislas Bontron Guillaume |
spellingShingle |
Bellier Joseph Zin Isabella Siblot Stanislas Bontron Guillaume Probabilistic flood forecasting on the Rhone River: evaluation with ensemble and analogue-based precipitation forecasts E3S Web of Conferences |
author_facet |
Bellier Joseph Zin Isabella Siblot Stanislas Bontron Guillaume |
author_sort |
Bellier Joseph |
title |
Probabilistic flood forecasting on the Rhone River: evaluation with ensemble and analogue-based precipitation forecasts |
title_short |
Probabilistic flood forecasting on the Rhone River: evaluation with ensemble and analogue-based precipitation forecasts |
title_full |
Probabilistic flood forecasting on the Rhone River: evaluation with ensemble and analogue-based precipitation forecasts |
title_fullStr |
Probabilistic flood forecasting on the Rhone River: evaluation with ensemble and analogue-based precipitation forecasts |
title_full_unstemmed |
Probabilistic flood forecasting on the Rhone River: evaluation with ensemble and analogue-based precipitation forecasts |
title_sort |
probabilistic flood forecasting on the rhone river: evaluation with ensemble and analogue-based precipitation forecasts |
publisher |
EDP Sciences |
series |
E3S Web of Conferences |
issn |
2267-1242 |
publishDate |
2016-01-01 |
description |
Hydrological ensemble forecasting performances are analysed over 5 basins up to 2000 km2 in the French Upper Rhone region. Streamflow forecasts are issued at an hourly time step from lumped ARX rainfall-runoff models forced by different precipitation forecasts. Ensemble meteorological forecasts from ECMWF and NCEP are considered, as well as analogue-based forecasts fed by their corresponding control forecast. Analogue forecasts are rearranged using an adaptation of the Schaake-Shuffle method in order to ensure the temporal coherence. A new evaluation approach is proposed, separating forecasting performances on peak amplitudes and peak timings for high flow events. Evaluation is conducted against both simulated and observed streamflow (so that relative meteorological and hydrological uncertainties can be assessed), by means of CRPS and rank histograms, over the 2007-2014 period. Results show a general agreement of the forecasting performances when averaged over the 5 basins. However, ensemble-based and analogue-based streamflow forecasts produce a different signature on peak events in terms of bias, spread and reliability. Strengths and weaknesses of both approaches are discussed as well as potential improvements, notably towards their merging. |
url |
http://dx.doi.org/10.1051/e3sconf/20160718011 |
work_keys_str_mv |
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