Evaluation of a New Polarimetrically Based ZR Relation

V. N. Bringi Colorado State University, Fort Collins, Colorado

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Taiwen Tang Colorado State University, Fort Collins, Colorado

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V. Chandrasekar Colorado State University, Fort Collins, Colorado

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Abstract

A new polarimetrically based (or, pol-based) ZR relation of the form Z = aR1.5 is described and evaluated where the multiplicative coefficient a is continuously adjusted as the drop size distribution evolves in space and time. The methodology is based on previous studies involving estimation of the normalized gamma drop size distribution parameters (DSD) using radar measurements of Zh, Zdr, and Kdp. In moderate-to-intense rainfall, the retrieval of the DSD parameters are formulated to account for the effects of drop oscillations using the “effective” β concept where the axis ratio (r) versus D relation is assumed to be linear and of the form r = 1 − βD in the underlying raindrop shape model. Rayleigh scattering with analytic approximations are used to show that the β estimator in Gorgucci et al. (2000) based on Zh, Zdr, and Kdp is of the correct form. The changes in the effective β in a storm cell is studied as the cell evolves from the growth phase to the mature phase (with microburst and rain rates of around 100–120 mm h−1). The systematic shift in β with increasing rain rates in this cell is shown to be consistent with the collisional probability model results of Beard and Johnson (1984). For evaluation of the pol-based ZR relation, six storm events from the Tropical Rainfall Measuring Mission– Large-Scale Biosphere–Atmosphere (TRMM–LBA) experiment and Texas and Florida Underflights Experiment- B (TEFLUN-B) are analyzed using radar data from the NCAR–S-band Polarimetric (SPOL) radar and a network of gauges specially deployed for these two campaigns. For storm total accumulation, the new pol-based ZR algorithm gives a normalized bias of 6% (radar overestimate) and normalized standard error of 20%. The corresponding values for a conventional ZR relation (after stratiform/convective separation) are −18% and 24%. The pol-based ZR method continuously “tracks” the drop size distribution and so no classification of rain types is necessary.

Corresponding author address: V. N. Bringi, Colorado State University, Dept. of Electrical and Computer Engineering, Fort Collins, CO 80523. Email: bringi@engr.colostate.edu

Abstract

A new polarimetrically based (or, pol-based) ZR relation of the form Z = aR1.5 is described and evaluated where the multiplicative coefficient a is continuously adjusted as the drop size distribution evolves in space and time. The methodology is based on previous studies involving estimation of the normalized gamma drop size distribution parameters (DSD) using radar measurements of Zh, Zdr, and Kdp. In moderate-to-intense rainfall, the retrieval of the DSD parameters are formulated to account for the effects of drop oscillations using the “effective” β concept where the axis ratio (r) versus D relation is assumed to be linear and of the form r = 1 − βD in the underlying raindrop shape model. Rayleigh scattering with analytic approximations are used to show that the β estimator in Gorgucci et al. (2000) based on Zh, Zdr, and Kdp is of the correct form. The changes in the effective β in a storm cell is studied as the cell evolves from the growth phase to the mature phase (with microburst and rain rates of around 100–120 mm h−1). The systematic shift in β with increasing rain rates in this cell is shown to be consistent with the collisional probability model results of Beard and Johnson (1984). For evaluation of the pol-based ZR relation, six storm events from the Tropical Rainfall Measuring Mission– Large-Scale Biosphere–Atmosphere (TRMM–LBA) experiment and Texas and Florida Underflights Experiment- B (TEFLUN-B) are analyzed using radar data from the NCAR–S-band Polarimetric (SPOL) radar and a network of gauges specially deployed for these two campaigns. For storm total accumulation, the new pol-based ZR algorithm gives a normalized bias of 6% (radar overestimate) and normalized standard error of 20%. The corresponding values for a conventional ZR relation (after stratiform/convective separation) are −18% and 24%. The pol-based ZR method continuously “tracks” the drop size distribution and so no classification of rain types is necessary.

Corresponding author address: V. N. Bringi, Colorado State University, Dept. of Electrical and Computer Engineering, Fort Collins, CO 80523. Email: bringi@engr.colostate.edu

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  • Anagnostou, E., Morales C. A. , and Dinku T. , 2001: The use of TRMM precipitation radar observations in determining ground radar calibration biases. J. Atmos. Oceanic Technol, 18 , 616628.

    • Crossref
    • Search Google Scholar
    • Export Citation
  • Andsager, K., Beard K. V. , and Laird N. F. , 1999: Laboratory measurements of axis ratios for large raindrops. J. Atmos. Sci, 56 , 26732683.

    • Crossref
    • Search Google Scholar
    • Export Citation
  • Atlas, D., and Ulbrich C. W. , 1977: Path- and area- integrated rainfall measurement by microwave attenuation in 1–3 cm band. J. Appl. Meteor, 16 , 13221331.

    • Crossref
    • Search Google Scholar
    • Export Citation
  • Atlas, D., and Williams C. R. , 2003a: The anatomy of a continental tropical convective storm. J. Atmos. Sci, 60 , 315.

  • Atlas, D., and Williams C. R. , 2003b: Physical origin of a microburst seen by radar profiler. Preprints, 31st Conf. on Radar Meteorology, Seattle, WA, Amer. Meteor. Soc., 551–554.

    • Search Google Scholar
    • Export Citation
  • Atlas, D., Srivastava R. C. , and Sekhon R. S. , 1973: Doppler radar characteristics of precipitation at vertical incidence. Rev. Geophys. Space Phys, 2 , 135.

    • Search Google Scholar
    • Export Citation
  • Beard, K. V., 1984: Oscillation modes for predicting raindrop axis and backscattering ratios. Radio Sci, 19 , 6774.

  • Beard, K. V., and Jameson A. R. , 1983: Raindrop canting. J. Atmos. Sci, 40 , 448454.

  • Beard, K. V., and Johnson D. B. , 1984: Raindrop axial and backscatter ratios using a collisional probability model. Geophys. Res. Lett, 11 , 6568.

    • Crossref
    • Search Google Scholar
    • Export Citation
  • Beard, K. V., and Chuang C. , 1987: A new model for the equilibrium shape of raindrops. J. Atmos. Sci, 44 , 15091524.

  • Beard, K. V., and Kubesh R. J. , 1991: Laboratory measurements of small raindrop distortion. Part II: Oscillation frequencies and modes. J. Atmos. Sci, 48 , 22452264.

    • Crossref
    • Search Google Scholar
    • Export Citation
  • Brandes, E. A., Zhang G. , and Vivekanandan J. , 2002: Experiments in rainfall estimation with a polarimetric radar in a subtropical environment. J. Appl. Meteor, 41 , 674685.

    • Crossref
    • Search Google Scholar
    • Export Citation
  • Brandes, E. A., Zhang G. , and Vivekanandan J. , 2003: An evaluation of a drop distribution- based polarimetric radar rainfall estimator. J. Appl. Meteor, 42 , 652660.

    • Crossref
    • Search Google Scholar
    • Export Citation
  • Bringi, V. N., and Chandrasekar V. , 2001: Polarimetric Doppler Weather Radar Principles and Applications. Cambridge University Press, 636 pp.

    • Search Google Scholar
    • Export Citation
  • Bringi, V. N., Huang G. , Chandrasekar V. , and Keenan T. D. , 2001a: An areal rainfall estimator using differential propagation phase: Evaluation using a C-band radar and a dense gage network in the Tropics. J. Atmos. Oceanic Technol, 18 , 18101818.

    • Crossref
    • Search Google Scholar
    • Export Citation
  • Bringi, V. N., Keenan T. D. , and Chandrasekar V. , 2001b: Correcting C-band radar reflectivity and differential reflectivity data for rain attenuation: A self-consistent method with constraints. Trans. IEEE Geosci. Remote Sens, 39 , 19061915.

    • Crossref
    • Search Google Scholar
    • Export Citation
  • Bringi, V. N., Huang G. , and Chandrasekar V. , 2002: A methodology for estimating the parameters of a gamma raindrop size distribution model from polarimetric radar data: Application to a squall-line event from the TRMM/Brazil campaign. J. Atmos. Oceanic Technol, 19 , 633645.

    • Crossref
    • Search Google Scholar
    • Export Citation
  • Bringi, V. N., Chandrasekar V. , Hubbert J. , Gorgucci E. , Randeu W. L. , and Schoenhuber M. , 2003: Raindrop size distribution in different climatic regimes from disdrometer and dual-polarized radar analysis. J. Atmos. Sci, 60 , 354365.

    • Crossref
    • Search Google Scholar
    • Export Citation
  • Carbone, R. E., and Nelson L. D. , 1978: The evolution of raindrop spectra in warm-based convective storms as observed and numerically modeled. J. Atmos. Sci, 35 , 23022314.

    • Crossref
    • Search Google Scholar
    • Export Citation
  • Doviak, R. J., and Zrnić D. S. , 1993: Doppler Radar and Weather Observations. 2d ed. Academic Press, 562 pp.

  • Gorgucci, E., Scarchilli G. , Chandrasekar V. , and Bringi V. N. , 2000: Measurement of mean raindrop shape from polarimetric radar observations. J. Atmos. Sci, 57 , 34063413.

    • Crossref
    • Search Google Scholar
    • Export Citation
  • Gorgucci, E., Scarchilli G. , Chandrasekar V. , and Bringi V. N. , 2001: Rainfall estimation from polarimetric radar measurements: Composite algorithms independent of raindrop shape–size relation. J. Atmos. Oceanic Technol, 18 , 17731786.

    • Crossref
    • Search Google Scholar
    • Export Citation
  • Gorgucci, E., Chandrasekar V. , Bringi V. N. , and Scarchilli G. , 2002: Estimation of raindrop size distribution parameters from polarimetric radar measurements. J. Atmos. Sci, 59 , 23732384.

    • Crossref
    • Search Google Scholar
    • Export Citation
  • Hubbert, J., and Bringi V. N. , 1995: An iterative filtering technique for the analysis of copolar differential phase and dual-frequency radar measurements. J. Atmos. Oceanic Technol, 12 , 643648.

    • Crossref
    • Search Google Scholar
    • Export Citation
  • Jameson, A. R., 1989: Theoretical analysis and meteorological interpretation of the role of raindrop shape on microwave attenuation and propagation phase shifts: Implication for the radar measurement of rain. J. Atmos. Oceanic Technol, 6 , 7688.

    • Crossref
    • Search Google Scholar
    • Export Citation
  • Le Bouar, E., Testud J. , and Keenan T. D. , 2001: Validation of the rain profiling algorithm “ZPHI” from the C-band polarimetric weather radar in Darwin. J. Atmos. Oceanic Technol, 18 , 18191837.

    • Crossref
    • Search Google Scholar
    • Export Citation
  • Matrosov, S. Y., Clark K. A. , Martner B. E. , and Tokay A. , 2002: X- band polarimetric radar measurements of rainfall. J. Appl. Meteor, 41 , 941952.

    • Crossref
    • Search Google Scholar
    • Export Citation
  • May, P., Keenan T. , Zrnić D. , Carey L. D. , and Rutledge S. A. , 1999: Polarimetric radar measurements of tropical rain at a 5-cm wavelength. J. Appl. Meteor, 38 , 750765.

    • Crossref
    • Search Google Scholar
    • Export Citation
  • Pruppacher, H. R., and Beard K. V. , 1970: A wind tunnel investigation of the internal circulation and shape of water drops falling at terminal velocity in air. Quart. J. Roy. Meteor. Soc, 96 , 247256.

    • Crossref
    • Search Google Scholar
    • Export Citation
  • Ryzhkov, A. V., and Zrnić D. S. , 1996: Assessment of rainfall measurement that uses specific differential phase. J. Appl. Meteor, 35 , 20802090.

    • Crossref
    • Search Google Scholar
    • Export Citation
  • Ryzhkov, A. V., Zrnić D. , and Atlas D. , 1997: Polarimetrically tuned R(Z) relations and comparison of radar rainfall methods. J. Appl. Meteor, 36 , 340349.

    • Crossref
    • Search Google Scholar
    • Export Citation
  • Ryzhkov, A. V., Zrnić D. , and Fulton R. , 2000: Areal rainfall estimates using differential phase. J. Appl. Meteor, 39 , 263268.

    • Crossref
    • Search Google Scholar
    • Export Citation
  • Ryzhkov, A. V., Giangrande S. , and Schuur T. J. , 2003: Rainfall estimation with a polarimetric prototype of the operational WSR-88D radar. Preprint, 31st Conf. on Radar Meteorology, Seattle, WA, Amer. Meteor. Soc., 208–211.

    • Search Google Scholar
    • Export Citation
  • Sekhon, R. S., and Srivastava R. C. , 1971: Doppler radar observations of drop-size distributions in a thunderstorm. J. Atmos. Sci, 28 , 983994.

    • Crossref
    • Search Google Scholar
    • Export Citation
  • Steiner, M., and Smith J. A. , 1998: Convective versus stratiform rainfall: An ice-microphysical and kinematic conceptual model. Atmos. Res, 47 , –48. 317326.

    • Search Google Scholar
    • Export Citation
  • Testud, J., Le Bouar E. , Obligis E. , and Ali-Mehenni M. , 2000: The rain profiling algorithm applied to polarimetric weather radar. J. Atmos. Oceanic Technol, 17 , 322356.

    • Search Google Scholar
    • Export Citation
  • Testud, J., Oury S. , Amayenc P. , and Black R. A. , 2001: The concept of “normalized” distributions to describe raindrop spectra: A tool for cloud physics and cloud remote sensing. J. Appl. Meteor, 40 , 11181140.

    • Crossref
    • Search Google Scholar
    • Export Citation
  • Tokay, A., and Beard K. V. , 1996: A field study of raindrop oscillations. Part I: Observation of size spectra and evaluation of oscillation causes. J. Appl. Meteor, 35 , 16711687.

    • Crossref
    • Search Google Scholar
    • Export Citation
  • Tokay, A., and Short D. A. , 1996: Evidence from tropical raindrop spectra of the origin of rain from stratiform versus convective clouds. J. Appl. Meteor, 35 , 355371.

    • Crossref
    • Search Google Scholar
    • Export Citation
  • Willis, P. T., 1984: Functional fits to some observed drop size distributions and parameterization of rain. J. Atmos. Sci, 41 , 16481661.

    • Crossref
    • Search Google Scholar
    • Export Citation
  • Zawadzki, I., 1984: Factors affecting the precision of radar measurements of rain. Preprints, 22d Conf. on Radar Meteorology, Zurich, Switzerland, Amer. Meteor. Soc., 251–256.

    • Search Google Scholar
    • Export Citation
  • Zhang, G., Vivekanandan J. , and Brandes E. , 2001: A method for estimating rain rate and drop size distribution from polarimetric radar measurements. IEEE Trans. Geosci. Remote Sens, 39 , 830841.

    • Crossref
    • Search Google Scholar
    • Export Citation
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