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Authordc.contributor.authorSharma, Sanjib 
Authordc.contributor.authorSiddique, Ridwan 
Authordc.contributor.authorReed, Seann 
Authordc.contributor.authorAhnert, Peter 
Authordc.contributor.authorMendoza Zúñiga, Pablo Andrés 
Authordc.contributor.authorMejia, Alfonso 
Admission datedc.date.accessioned2018-07-17T20:22:56Z
Available datedc.date.available2018-07-17T20:22:56Z
Publication datedc.date.issued2018
Cita de ítemdc.identifier.citationHydrol. Earth Syst. Sci., 22, 1831–1849, 2018es_ES
Identifierdc.identifier.other10.5194/hess-22-1831-2018
Identifierdc.identifier.urihttps://repositorio.uchile.cl/handle/2250/149960
Abstractdc.description.abstractThe relative roles of statistical weather preprocessing and streamflow postprocessing in hydrological ensemble forecasting at short-to medium-range forecast lead times (day 1-7) are investigated. For this purpose, a regional hydrologic ensemble prediction system (RHEPS) is developed and implemented. The RHEPS is comprised of the following components: (i) hydrometeorological observations (multisensor precipitation estimates, gridded surface temperature, and gauged streamflow); (ii) weather ensemble forecasts (precipitation and near-surface temperature) from the National Centers for Environmental Prediction 11-member Global Ensemble Forecast System Re-forecast version 2 (GEFSRv2); (iii) NOAA's Hydrology Laboratory-Research Distributed Hydrologic Model (HL-RDHM); (iv) heteroscedastic censored logistic regression (HCLR) as the statistical preprocessor; (v) two statistical postprocessors, an autoregressive model with a single exogenous variable (ARX(1,1)) and quantile regression (QR); and (vi) a comprehensive verification strategy. To implement the RHEPS, 1 to 7 days weather forecasts from the GEFSRv2 are used to force HL-RDHM and generate raw ensemble streamflow forecasts. Forecasting experiments are conducted in four nested basins in the US Middle Atlantic region, ranging in size from 381 to 12 362 km(2). Results show that the HCLR preprocessed ensemble precipitation forecasts have greater skill than the raw forecasts. These improvements are more noticeable in the warm season at the longer lead times (>3 days). Both postprocessors, ARX(1,1) and QR, show gains in skill relative to the raw ensemble streamflow forecasts, particularly in the cool season, but QR outperforms ARX(1,1). The scenarios that implement preprocessing and postprocessing separately tend to perform similarly, although the postprocessing-alone scenario is often more effective. The scenario involving both preprocessing and postprocessing consistently outperforms the other scenarios. In some cases, however, the differences between this scenario and the scenario with postprocessing alone are not as significant. We conclude that implementing both preprocessing and postprocessing ensures the most skill improvements, but postprocessing alone can often be a competitive alternative.es_ES
Patrocinadordc.description.sponsorshipNOAA/NWS NA14NWS4680012es_ES
Lenguagedc.language.isoenes_ES
Publisherdc.publisherEuropean Geosciences Uniones_ES
Type of licensedc.rightsAttribution-NonCommercial-NoDerivs 3.0 Chile*
Link to Licensedc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/cl/*
Sourcedc.sourceHydrology and Earth System Scienceses_ES
Títulodc.titleRelative effects of statistical preprocessing and postprocessing on a regional hydrological ensemble prediction systemes_ES
Document typedc.typeArtículo de revista
Catalogueruchile.catalogadortjnes_ES
Indexationuchile.indexArtículo de publicación ISIes_ES


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Except where otherwise noted, this item's license is described as Attribution-NonCommercial-NoDerivs 3.0 Chile