Articles | Volume 7, issue 3
Nat. Hazards Earth Syst. Sci., 7, 391–398, 2007
https://doi.org/10.5194/nhess-7-391-2007

Special issue: Advances in radar, multi-sensor and hydrological modelling...

Nat. Hazards Earth Syst. Sci., 7, 391–398, 2007
https://doi.org/10.5194/nhess-7-391-2007

  08 Jun 2007

08 Jun 2007

Modelling of weather radar echoes from anomalous propagation using a hybrid parabolic equation method and NWP model data

D. Bebbington1, S. Rae1, J. Bech2,3, B. Codina3, and M. Picanyol3 D. Bebbington et al.
  • 1Dept. Electronic Systems Engineering, University of Essex, UK
  • 2Servei Meteorològic de Catalunya, Barcelona, Spain
  • 3Dept. d'Astronomia i Meteorologia, Universitat de Barcelona, Spain

Abstract. Contamination of weather radar echoes by anomalous propagation (anaprop) mechanisms remains a serious issue in quality control of radar precipitation estimates. Although significant progress has been made identifying clutter due to anaprop there is no unique method that solves the question of data reliability without removing genuine data. The work described here relates to the development of a software application that uses a numerical weather prediction (NWP) model to obtain the temperature, humidity and pressure fields to calculate the three dimensional structure of the atmospheric refractive index structure, from which a physically based prediction of the incidence of clutter can be made. This technique can be used in conjunction with existing methods for clutter removal by modifying parameters of detectors or filters according to the physical evidence for anomalous propagation conditions. The parabolic equation method (PEM) is a well established technique for solving the equations for beam propagation in a non-uniformly stratified atmosphere, but although intrinsically very efficient, is not sufficiently fast to be practicable for near real-time modelling of clutter over the entire area observed by a typical weather radar. We demonstrate a fast hybrid PEM technique that is capable of providing acceptable results in conjunction with a high-resolution terrain elevation model, using a standard desktop personal computer. We discuss the performance of the method and approaches for the improvement of the model profiles in the lowest levels of the troposphere.

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