The Impact of Signal Processing on the Range-Weighting Function for Weather Radars

Sebastián M. Torres Cooperative Institute for Mesoscale Meteorological Studies, University of Oklahoma, and NOAA/OAR/National Severe Storms Laboratory, Norman, Oklahoma

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Christopher D. Curtis Cooperative Institute for Mesoscale Meteorological Studies, University of Oklahoma, and NOAA/OAR/National Severe Storms Laboratory, Norman, Oklahoma

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Abstract

The range-weighting function (RWF) determines how individual scatterer contributions are weighted as a function of range to produce the meteorological data associated with a single resolution volume. The RWF is commonly defined in terms of the transmitter pulse envelope and the receiver filter impulse response, and it determines the radar range resolution. However, the effective RWF also depends on the range-time processing involved in producing estimates of meteorological variables. This is a third contributor to the RWF that has become more significant in recent years as advanced range-time processing techniques have become feasible for real-time implementation on modern radar systems. In this work, a new formulation of the RWF for weather radars that incorporates the impact of signal processing is proposed. Following the derivation based on a general signal processing model, typical scenarios are used to illustrate the variety of RWFs that can result from different range-time signal processing techniques. Finally, the RWF is used to measure range resolution and the range correlation of meteorological data.

Corresponding author address: Sebastián Torres, 120 David L. Boren Blvd., National Weather Center, Norman, OK 73072. E-mail: sebastian.torres@noaa.gov

Abstract

The range-weighting function (RWF) determines how individual scatterer contributions are weighted as a function of range to produce the meteorological data associated with a single resolution volume. The RWF is commonly defined in terms of the transmitter pulse envelope and the receiver filter impulse response, and it determines the radar range resolution. However, the effective RWF also depends on the range-time processing involved in producing estimates of meteorological variables. This is a third contributor to the RWF that has become more significant in recent years as advanced range-time processing techniques have become feasible for real-time implementation on modern radar systems. In this work, a new formulation of the RWF for weather radars that incorporates the impact of signal processing is proposed. Following the derivation based on a general signal processing model, typical scenarios are used to illustrate the variety of RWFs that can result from different range-time signal processing techniques. Finally, the RWF is used to measure range resolution and the range correlation of meteorological data.

Corresponding author address: Sebastián Torres, 120 David L. Boren Blvd., National Weather Center, Norman, OK 73072. E-mail: sebastian.torres@noaa.gov
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  • Bringi, V. N., and Chandrasekar V. , 2001: Polarimetric Doppler Weather Radar: Principles and Applications. Cambridge University Press, 636 pp.

  • Brown, R. A., Flickinger B. A. , Forren E. , Schultz D. M. , Sirmans D. , Spencer P. L. , Wood V. T. , and Ziegler C. L. , 2005: Improved detection of severe storms using experimental fine-resolution WSR-88D measurements. Wea. Forecasting, 20, 314.

    • Search Google Scholar
    • Export Citation
  • Bucci, N. J., and Urkowitz H. , 1993: Testing of Doppler tolerant range sidelobe suppression in pulse compression meteorological radar. Proc. IEEE National Radar Conf., Boston, MA, IEEE, 206–211.

  • Capsoni, C., and D’Amico M. , 1998: A physically based radar simulator. J. Atmos. Oceanic Technol., 15, 593598.

  • Cheong, B. L., Hoffman M. W. , and Palmer R. D. , 2004: Efficient atmospheric simulation for high-resolution radar imaging applications. J. Atmos. Oceanic Technol., 21, 374378.

    • Search Google Scholar
    • Export Citation
  • Cheong, B. L., Palmer R. D. , and Xue M. , 2008: A time series weather radar simulator based on high-resolution atmospheric models. J. Atmos. Oceanic Technol., 25, 230243.

    • Search Google Scholar
    • Export Citation
  • Chiuppesi, F., Galati G. , and Lombardi P. , 1980: Optimisation of rejection filters. IEE Proc. F Commun. Radar and Signal Process., 127, 354360.

    • Search Google Scholar
    • Export Citation
  • Curtis, C., and Torres S. , 2011: Adaptive range oversampling to achieve faster scanning on the National Weather Radar Testbed phased array radar. J. Atmos. Oceanic Technol., 28, 15811597.

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

  • Johnston, P. E., Hartten L. M. , Love C. H. , Carter D. A. , and Gage K. S. , 2002: Range errors in wind profiling caused by strong reflectivity gradients. J. Atmos. Oceanic Technol., 19, 934953.

    • Search Google Scholar
    • Export Citation
  • Li, X., He J. , Wang J. , and Si Z. , 2009: A robust capon method to improve weather radar range resolution using oversampling. Proc. 2009 Int. Conf. on Information Engineering and Computer Science, Wuhan, China, IEEE, 1–4.

  • Mudukutore, A. S., Chandrasekar V. , and Keeler R. J. , 1998: Pulse compression for weather radars. IEEE Trans. Geosci. Remote Sens., 36, 125142.

    • Search Google Scholar
    • Export Citation
  • Mueller, E. A., 1977: Statistics of high radar reflectivity gradients. J. Appl. Meteor., 16, 511513.

  • Torres, S., and Zrnić D. , 2003: Whitening in range to improve weather radar spectral moment estimates. Part I: Formulation and simulation. J. Atmos. Oceanic Technol., 20, 14331448.

    • Search Google Scholar
    • Export Citation
  • Torres, S., and Curtis C. D. , 2006: Design considerations for improved tornado detection using super-resolution data on the NEXRAD network. Preprints, Fourth European Conf. on Radar Meteorology and Hydrology (ERAD), Barcelona, Spain, ERAD, 92–95.

  • Torres, S., Curtis C. D. , and Cruz J. R. , 2004: Pseudowhitening of weather radar signals to improve spectral moment and polarimetric variable estimates at low signal-to-noise. IEEE Trans. Geosci. Remote Sens., 42, 941949.

    • Search Google Scholar
    • Export Citation
  • Unisys Corporation, 1991: Computer program development specification for signal processing program (B5, CPCI 02), DV1208261F. [Available from WSR-88D Radar Operations Center, 1200 Westheimer Dr., Norman, OK 73069.]

  • Wood, V. T., and Brown R. A. , 1997: Effects of radar sampling on single-Doppler velocity signatures of mesocyclones and tornadoes. Wea. Forecasting, 12, 928938.

    • Search Google Scholar
    • Export Citation
  • Yu, T.-Y., Zhang G. , Chalamalasetti A. , Doviak R. , and Zrnić D. , 2006: Resolution enhancement technique using range oversampling. J. Atmos. Oceanic Technol., 23, 228240.

    • Search Google Scholar
    • Export Citation
  • Zrnić, D. S., and Doviak R. J. , 1978: Matched filter criteria and range weighting for weather radar. IEEE Trans. Aerosp. Electron. Syst., AEC-14, 925930.

    • Search Google Scholar
    • Export Citation
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