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Appropriate temporal resolution of precipitation data for discharge modelling in pre-alpine catchments
Univ Zurich, Dept Geog, Zurich, Switzerland.;Warsaw Univ Life Sci SGGW, Dept Hydraul Engn, Warsaw, Poland..ORCID-id: 0000-0002-5273-1038
Uppsala universitet, Teknisk-naturvetenskapliga vetenskapsområdet, Geovetenskapliga sektionen, Institutionen för geovetenskaper, Luft-, vatten- och landskapslära. Univ Zurich, Dept Geog, Zurich, Switzerland.ORCID-id: 0000-0002-6314-2124
2018 (engelsk)Inngår i: Hydrological Sciences Journal, ISSN 0262-6667, E-ISSN 2150-3435, Vol. 63, nr 1, s. 1-16Artikkel i tidsskrift (Fagfellevurdert) Published
Abstract [en]

Precipitation time series with high temporal resolution are desired for hydrological modelling and flood studies. Yet the choice of an appropriate resolution is not straightforward because the use of too high a temporal resolution increases the data requirements, computational costs and, presumably, associated uncertainty, while performance improvement may be indiscernible. In this study, the effect of averaging hourly precipitation on model performance and associated uncertainty is investigated using two data sources: station network precipitation (SNP) and radar-based precipitation (RBP). From these datasets, time series of different temporal resolutions were generated, and runoff was simulated for 13 pre-alpine catchments with a bucket-type model. Our results revealed that different temporal resolutions were required for an acceptable model performance depending on the catchment size and data source. These were 1-12h for small (16-59km(2)), 3-21h for medium (60-200km(2)), and 24h for large (200-939km(2)) catchments.

sted, utgiver, år, opplag, sider
TAYLOR & FRANCIS LTD , 2018. Vol. 63, nr 1, s. 1-16
Emneord [en]
radar-based precipitation, station network precipitation, averaging length, uncertainty, Bayesian methods, bucket-type model
HSV kategori
Identifikatorer
URN: urn:nbn:se:uu:diva-342455DOI: 10.1080/02626667.2017.1410279ISI: 000422685200001OAI: oai:DiVA.org:uu-342455DiVA, id: diva2:1185540
Tilgjengelig fra: 2018-02-26 Laget: 2018-02-26 Sist oppdatert: 2018-02-26bibliografisk kontrollert

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