Eine Plattform für die Wissenschaft: Bauingenieurwesen, Architektur und Urbanistik
Assessing 32-Day Hydrological Ensemble Forecasts in the Lake Champlain–Richelieu River Watershed
This paper explored various configurations of the ensemble Kalman filter, the GR4J hydrological model, and the Global Environmental Multiscale (GEM) atmospheric model in order to maximize the skill of ensemble hydrological forecasts for the Lake Champlain–Richelieu River watershed. In open-loop mode, the hydrological model represented very well the observed streamflow (Nash–Sutcliffe value above 90%). It sufficed to assimilate hydrological data to obtain a reliable and skillful analysis of streamflow; assimilation of snow water equivalent (SWE) information did not bring additional benefits. In forecast mode, the opposite was true: hydrological assimilation alone did not improve forecast performance, but assimilating SWE data improved reliability and skill of forecasts with lead times of 15 days to 1 month. The impact of SWE assimilation also depended on the quality of the precipitation analysis. It therefore is recommended to use SWE assimilation for monthly forecasting, especially if the precipitation data used to drive the hydrological model are biased.
Assessing 32-Day Hydrological Ensemble Forecasts in the Lake Champlain–Richelieu River Watershed
This paper explored various configurations of the ensemble Kalman filter, the GR4J hydrological model, and the Global Environmental Multiscale (GEM) atmospheric model in order to maximize the skill of ensemble hydrological forecasts for the Lake Champlain–Richelieu River watershed. In open-loop mode, the hydrological model represented very well the observed streamflow (Nash–Sutcliffe value above 90%). It sufficed to assimilate hydrological data to obtain a reliable and skillful analysis of streamflow; assimilation of snow water equivalent (SWE) information did not bring additional benefits. In forecast mode, the opposite was true: hydrological assimilation alone did not improve forecast performance, but assimilating SWE data improved reliability and skill of forecasts with lead times of 15 days to 1 month. The impact of SWE assimilation also depended on the quality of the precipitation analysis. It therefore is recommended to use SWE assimilation for monthly forecasting, especially if the precipitation data used to drive the hydrological model are biased.
Assessing 32-Day Hydrological Ensemble Forecasts in the Lake Champlain–Richelieu River Watershed
Abaza, Mabrouk (Autor:in) / Fortin, Vincent (Autor:in) / Gaborit, Étienne (Autor:in) / Bélair, Stéphane (Autor:in) / Garnaud, Camille (Autor:in)
16.07.2020
Aufsatz (Zeitschrift)
Elektronische Ressource
Unbekannt
Analysis of Lake Champlain/Richelieu River's historical 2011 flood
Online Contents | 2016
|Engineering Index Backfile | 1932
|Ensemble Hydrological Forecasts for the Upper Rhone River Basin
British Library Conference Proceedings | 2009
|Engineering Index Backfile | 1929
|Engineering Index Backfile | 1933
|