A Simulation Approach for Validation of a Brightband Correction Method

Marco Borga Department of Land and Agro-Forest Environment, University of Padova, Legnaro, Padova, Italy

Search for other papers by Marco Borga in
Current site
Google Scholar
PubMed
Close
,
Emmanouil N. Anagnostou Iowa Institute of Hydraulic Research, The University of Iowa, Iowa City, Iowa

Search for other papers by Emmanouil N. Anagnostou in
Current site
Google Scholar
PubMed
Close
, and
Witold F. Krajewski Iowa Institute of Hydraulic Research, The University of Iowa, Iowa City, Iowa

Search for other papers by Witold F. Krajewski in
Current site
Google Scholar
PubMed
Close
Restricted access

Abstract

Brightband effects are one of the more important causes of vertical variability of reflectivity and severely affect the accuracy of rainfall estimates from ground-based radar. Monte Carlo simulation experiments are performed to investigate the efficiency of a procedure for the correction of errors related to the vertical variability of reflectivity. The simulation model generates three-dimensional radar reflectivity fields. Brightband effects are simulated through a physically based model of melting-layer reflectivity observations. Sensitivity of the correction procedure for a number of different precipitation scenarios and radar systems is analyzed. Overall, the identification method is found to be a robust procedure for correction of brightband effects. Results indicate a dependence of the effectiveness of the correction procedure on mean altitude and spatial variability of the melting layer.

Corresponding author address: Dr. Marco Borga, DTeSAF, AGRIPOLIS, Via Romea, Legnaro, 35020 Padova, Italy.

Abstract

Brightband effects are one of the more important causes of vertical variability of reflectivity and severely affect the accuracy of rainfall estimates from ground-based radar. Monte Carlo simulation experiments are performed to investigate the efficiency of a procedure for the correction of errors related to the vertical variability of reflectivity. The simulation model generates three-dimensional radar reflectivity fields. Brightband effects are simulated through a physically based model of melting-layer reflectivity observations. Sensitivity of the correction procedure for a number of different precipitation scenarios and radar systems is analyzed. Overall, the identification method is found to be a robust procedure for correction of brightband effects. Results indicate a dependence of the effectiveness of the correction procedure on mean altitude and spatial variability of the melting layer.

Corresponding author address: Dr. Marco Borga, DTeSAF, AGRIPOLIS, Via Romea, Legnaro, 35020 Padova, Italy.

Save
  • Anagnostou, E. N., and W. F. Krajewski, 1996: Simulation of radar reflectivity fields: Algorithm formulation and evaluation. Water Resour. Res.,33(6), 1419–1429.

  • Andrieu, H., and J. D. Creutin, 1995: Identification of vertical profiles of radar reflectivities for hydrologicalapplications using an inverse method. Part I: Formulation. J. Appl. Meteor.,34, 225–239.

  • ——, G. Delrieu, and J. D. Creutin, 1995: Identification of vertical profiles of radar reflectivities for hydrological applications using an inverse method. Part II: Sensitivity analysis and case study. J. Appl. Meteor.,34, 240–259.

  • Atlas, D., M. Kerker, and W. Hitschfeld, 1953: Scattering and attenuation by nonspherical atmospheric particles. J. Atmos. Terr. Phys.,3, 108–119.

  • Austin, P. M., 1987: Relation between measured radar reflectivity and surface rainfall. Mon. Wea. Rev.,115, 1053–1070.

  • Battan, L. J., 1973: Radar Observation of the Atmosphere. University of Chicago Press, 324 pp.

  • Böhm, J. P., 1991: Sensitivity of computed radar reflectivities on various models of collisional growth. Preprints, 25th Conf. on Radar Meteorology, Paris, France, Amer. Meteor. Soc., 817–820.

  • Bohren, C. F., and L. J. Battan, 1980: Radar backscattering by inhomogeneous precipitation particles. J. Atmos. Sci.,37, 1821–1827.

  • ——, and ——, 1982: Radar backscattering of microwaves by spongy ice spheres. J. Atmos. Sci.,39, 2623–2629.

  • Borga, M., E. N. Anagnostou, and W. F. Krajewski, 1995: Validation of a method for vertical profile of reflectivity identification through bright band simulation. Proc. III Int. Symp. on Hydrological Applications of Weather Radar, Sao Paolo, Brazil, IAHR, 331–343.

  • Bourrel, L., H. Sauvageot, J. J. Vidal, D. Dartus, and J. P. Dupouyet, 1994: Radar measurement of precipitation in cold mountainous areas: The Garonne basin. Hydrol. Sci. J.,39, 369–389.

  • Collier, C. G., 1986: Accuracy of rainfall estimates by radar, Part I: Calibration by telemetering raingauges. J. Hydrol.,83, 207–223.

  • Ekpenyong, B. E., and R. C. Srivastava, 1970: Radar characteristics of the melting layer—A theoretical study. Preprints, 14th Conf. on Radar Meteorology, Tucson, AZ, Amer. Meteor. Soc., 161–166.

  • Fabry, F., 1996: On the determination of scale ranges for precipitation fields. J. Geophys. Res.,101 (D8), 12819–12826.

  • ——, G. L. Austin, and D. Tees, 1992: The accuracy of rainfall estimations by radar as a function of range. Quart. J. Roy. Meteor. Soc.,118, 435–453.

  • ——, A. Bellon, and I. Zawadzki, 1994a: Long term observations of the melting layer using vertically pointing radar. Stormy Weather Group Scientific Rep. MW101, McGill University, Montreal, 65 pp.

  • ——, ——, M. R. Duncan, and G. L. Austin, 1994b: High resolution rainfall measurements by radar for very small basins: The sampling problem reexamined. J. Hydrol,161, 415–428.

  • Gray, W. R., 1991: Vertical profile corrections based on EOF analysis of operational data. Preprints, 25th. Conf. on Radar Meteorology, Paris, France, Amer. Meteor. Soc., 824–827.

  • Gunn, K. L. S., and J. S. Marshall, 1958: The distribution with size of aggregate snow flakes. J. Meteor.,15, 452–461.

  • Hardaker, P. J., 1991: The derivation of relationships between bright band parameters and surface rainfall rate at weather radar frequencies. Department of Mathematics Rep., University of Essex, United Kingdom, 9pp.

  • ——, K. Tilford, C. G. Collier, I. D. Cluckie, and A. R. Holt, 1992: A study of experimentally measured and theoretically derived vertical reflectivity profiles at X-band. URSI Comm. F., Ravenscar, United Kingdom, 2.3.1.–2.3.3.

  • ——, A. R. Holt, and C. G. Collier, 1995: A melting layer model and its use in correcting for the bright band in single polarization radar echoes. Quart. J. Roy. Meteor. Soc.,121, 495–525.

  • Harrold, T. W., and P. G. Kitchingam, 1975: Measurement of surface rainfall using radar when the beam intersects the melting layer. Preprints, 16th Conf. on Radar Meteorology, Boston, MA, Amer. Meteor. Soc., 473–478.

  • Joss, J., and A. Waldvogel, 1990: Precipitation measurements and hydrology. Radar in Meteorology. D. Atlas, Ed., Amer. Meteor. Soc., 577–606.

  • ——, and R. Lee, 1995: The application of radar-gauge comparisons to operational precipitation profile corrections. J. Appl. Meteor.,34, 2612–2630.

  • ——, R. Cavalli, and R. K. Crane, 1974: Good agreement between theory and experiments for attenuation data. J. Rech. Atmos.,8, 299–318.

  • Kitchen, M., and R. M. Blackall, 1992: Representativeness errors in comparisons between radar and gauge measurements of rainfall. J. Hydrol.,134, 13–33.

  • ——, and P. M. Jackson, 1993: Weather radar performance at long range—Simulated and observed. J. Appl. Meteor.,32, 975–985.

  • Klaassen, W., 1988: Radar observations and simulations of the melting layer of precipitation. J. Atmos. Sci.,45, 3741–3753.

  • Koistinen, J., 1991: Operational correction of radar rainfall errors due to the vertical profile of reflectivity. Preprints, 25th Conf. on Radar Meteorology, Paris, France, Amer. Meteor. Soc., 91–96.

  • Krajewski, W. F., R. Raghavan, and V. Chandrasekar, 1993: Physically based simulation of radar rainfall data using a space–time rainfall model. J. Appl. Meteor.,32, 268–282.

  • Lhermitte, R. M., and D. Atlas, 1963: Doppler fall speed and particle growth in stratiform precipitation. Preprints, Tenth Conf. on Radar Meteorology, Washington, DC, Amer. Meteor. Soc., 297–302.

  • Mantoglou, A., and J. L. Wilson, 1982: The turning band method for simulation of random fields using line generation by a spectral method. Water Resour. Res.,18 (5), 1379–1394.

  • Matsuo, T., and Y. Sasyo, 1981: Melting of snowflakes below freezing level in the atmosphere. J. Meteor. Soc. Japan,59, 10–24.

  • Maxwell-Garnet, J. C., 1904: Colors in metal glasses and in metallic films. Philos. Trans. Roy. Soc. London,A203, 385–420.

  • Mie, G., 1908: Beiträge zur Optik trüber Medien, speziell kolloidaler Metallösungen (Contribution to the optics of suspended media, specifically colloidal metal suspensions). Ann. Phys.,25, 377–445.

  • Mitra, S. K., O. Vohl, M. Ahr, and H. R. Pruppacher, 1990: A wind tunnel and theoretical study of the melting behavior of atmospheric particles. IV: Experiment and theory for snow flakes. J. Atmos. Sci.,47, 584–591.

  • Ohtake, T., 1969: Observations of the size distributions of hydrometeors through the melting layer. J. Atmos. Sci.,26, 545–557.

  • Rodriguez-Iturbe, I., and P. S. Eagleson, 1987: Mathematical models of rainstorm events in space and time. Water Resour. Res.,23 (1), 181–190.

  • Russchenberg, H. W. J., 1992: Ground-Based Remote Sensing of Precipitation using a Multi-Polarized FM-CW Doppler Radar. Delft University Press, 206 pp.

  • Smith, C. J., 1986: The reduction of errors caused by bright band in quantitative rainfall measurements made using radar. J. Atmos. Oceanic Technol.,3, 129–141.

  • Steiner, M., R. A. Houze Jr., and S. E. Yuter, 1995: Climatological characterization of three-dimensional storm structure from operational radar and rain gauge data. J. Appl. Meteor.,34, 1978–2007.

  • Stewart, R. E., J. D. Marwitz, J. C. Pace, and R. E. Carbone, 1984: Characteristics through the melting layer of stratiform clouds. J. Atmos. Sci.,22, 3227–3237.

  • Tarantola, A., and B. Valette, 1982: Inverse problems: Quest for information. J. Geophys.,50, 159–170.

  • Ulbrich, C. W., 1983: Natural variations in the analytical form of the raindrop size distribution. J. Climate Appl. Meteor.,22, 1764–1775.

  • Willis, P. T., and A. J. Heymsfield, 1989: Structure of the melting layer in mesoscale convective system stratiform precipitation. J. Atmos. Sci.,46, 2008–2025.

  • Yokoyama, T., and H. Tanaka, 1984: Microphysical processes of melting snow flakes detected by two-wavelength radar. Part I. Principle of measurement based on model calculation. J. Meteor. Soc. Japan,62, 650–667.

  • Zawadzki, I., 1975: On radar-rain gage comparison. J. Appl. Meteor.,14, 1430–1436.

All Time Past Year Past 30 Days
Abstract Views 0 0 0
Full Text Views 278 77 6
PDF Downloads 69 34 4