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A comparison between gauge and radar precipitation time\u2010series records for the event indicated discrepancies between data sources, particularly in areas of higher elevation. The HEC\u2010HMS rainfall\u2010runoff model was selected to assess the accuracy of the precipitation to simulate river flows for the extreme event. Gauge, radar and gauge\u2010corrected radar rainfall were used as model inputs. Universal cokriging was used to geostatistically interpolate gauge data with radar and elevation data as covariates. This interpolated layer was used to calculate the mean\u2010field bias and correct the radar composites. Results indicated that gauge\u2010 and gauge\u2010corrected radar\u2010driven models replicated flows adequately for the extreme event. Gauge\u2010corrected flow predictions produced an increase in flow prediction accuracy when compared with the raw radar, yet predictions were comparative in accuracy to those using the interpolated gauge network. Subsequent investigations suggested this was due to an adequate spatial and temporal resolution of the precipitation gauge network within the Severn Uplands. Results suggested that the six rain gauges could adequately represent precipitation variability of the Severn Uplands to predict flows at an approximately equal accuracy to that obtained by radar. Temporally, radar produced an increase in flow prediction accuracy in mountainous reaches once the gauge time step was in excessive of an hourly interval. Copyright \u00a9 2010 John Wiley &amp; Sons, Ltd.<\/jats:p>","DOI":"10.1002\/hyp.7869","type":"journal-article","created":{"date-parts":[[2010,10,8]],"date-time":"2010-10-08T04:40:29Z","timestamp":1286512829000},"page":"795-810","source":"Crossref","is-referenced-by-count":40,"title":["A comparison of gauge and radar precipitation data for simulating an extreme hydrological event in the Severn Uplands, UK"],"prefix":"10.1002","volume":"25","author":[{"given":"Eloise M.","family":"Biggs","sequence":"first","affiliation":[],"role":[{"vocabulary":"crossref","role":"author"}]},{"given":"Peter M.","family":"Atkinson","sequence":"additional","affiliation":[],"role":[{"vocabulary":"crossref","role":"author"}]}],"member":"311","published-online":{"date-parts":[[2010,10,8]]},"reference":[{"key":"e_1_2_11_2_1","doi-asserted-by":"publisher","DOI":"10.3354\/cr014115"},{"key":"e_1_2_11_3_1","doi-asserted-by":"publisher","DOI":"10.1175\/1520-0426(1999)016<0206:UQOMAR>2.0.CO;2"},{"key":"e_1_2_11_4_1","doi-asserted-by":"publisher","DOI":"10.1016\/S0022-1694(96)03202-7"},{"key":"e_1_2_11_5_1","doi-asserted-by":"publisher","DOI":"10.3354\/cr028031"},{"key":"e_1_2_11_6_1","doi-asserted-by":"publisher","DOI":"10.1016\/0022-1694(94)02590-8"},{"key":"e_1_2_11_7_1","doi-asserted-by":"publisher","DOI":"10.5194\/hess-2-265-1998"},{"key":"e_1_2_11_8_1","doi-asserted-by":"publisher","DOI":"10.5194\/hess-2-283-1998"},{"key":"e_1_2_11_9_1","first-page":"360","volume-title":"Rainfall\u2010Runoff Modelling: The Primer","author":"Beven KJ","year":"2001"},{"key":"e_1_2_11_10_1","doi-asserted-by":"publisher","DOI":"10.1016\/S0022-1694(02)00137-3"},{"key":"e_1_2_11_11_1","doi-asserted-by":"publisher","DOI":"10.1029\/1999JD900270"},{"key":"e_1_2_11_12_1","doi-asserted-by":"publisher","DOI":"10.1023\/A:1012734519752"},{"key":"e_1_2_11_13_1","doi-asserted-by":"publisher","DOI":"10.1016\/j.jhydrol.2004.03.042"},{"key":"e_1_2_11_14_1","doi-asserted-by":"crossref","unstructured":"CharleyWJ.1988.The estimation of rainfall for flood forecasting using radar and rain gage data. 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