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Published bySherman Julian Horton Modified over 9 years ago
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Presentation to the Inter-Agency Committee for Hydrological Uses of Radar Data, University of Bristol, 5 August 2004 C.G.Collier University of Salford
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Combining and comparing rainfall observing systems in hydrological modelling of a rural catchment G.L.Robbins 1, M.Grum 2 and C.G.Collier 1 1 Univ. Salford 2 PH-Consult, Denmark
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Rainfall measurements relative strengths.
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A simple model which, one step ahead, predicts the rainfall intensity to be a weighting of its immediate own current value with its neighbours
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Schematic of a simple catchment model
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Croal catchment and hydrometeorological network
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Rainfall, observed river flow and forecast hydrographs after various time steps 13 September 2001
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Error in peak flow magnitude and time of occurrence of peak flow
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Assimilation of Doppler radial winds into a high resolution NWP model F.A.Rihan 1, C.G.Collier 1, S.P.Ballard 2 and S.J.Swarbrick 2 1 University of Salford 2 JCMM, Met Office
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Impact of a strong velocity gradient across the pulse volume and instrumental noise on the Doppler wind spectrum
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Schematic representation showing a convergence line moving from left to right. Gaussian noise represents the measurement error
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Chilbolton (300m & 4 km res.) and 1 km NWP model radial winds 1 July 2003. Model at two elevations
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Model radial winds at 4 km resoln.
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Next steps Met Office to complete 3D-var (later 4D- Var) assimilation system Observing System Simulation Experiments (OSSEs)
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