• DocumentCode
    778030
  • Title

    Range adjustment for ground-based radar, derived with the spaceborne TRMM precipitation radar

  • Author

    Gabella, Marco ; Joss, Jürg ; Perona, Giovanni ; Michaelides, Silas

  • Author_Institution
    Dipt. di Elettronica, Politecnico di Torino, Italy
  • Volume
    44
  • Issue
    1
  • fYear
    2006
  • Firstpage
    126
  • Lastpage
    133
  • Abstract
    We show how the Tropical Rainfall Measuring Mission (TRMM) Precipitation Radar (TPR) can be used to monitor and adjust ground-based radar (GR) data, as a function of the distance from the radar site. Problems caused by the variability of precipitation and differences in sampling volume of the two instruments are reduced to a level that is achievable with, and acceptable for, the present analysis. Throughout the region under surveillance, TPR has poorer spatial resolution than GR. The sampling volume of the GR changes quite remarkably according to the range from the GR site: it increases with the square of the range. TPR, on the other hand, has similar sampling volumes in all the locations. The analysis is based on the average linear radar reflectivity, in circular rings around the GR site, , as a function of the range from the GR site. The GR/TPR ratio varies, for the Cyprus radar, on average from 2 dB, at 10 km, to -8 dB at 100 km. The average departure at the average range is considered to be mainly caused by the calibration of the GR. The range dependence of the GR/TPR ratio is significant and similar, in all the investigated cases. This is interpreted to be caused by the increasing sampling volume of the GR with range, combined with nonhomogeneous beam filling, e.g., at longer ranges of GR, the lower part of the volume could be in rain, whereas the upper part of the same pulse could be filled with snow, or even be without an echo. After correcting the GR data by using the derived averaged relationship, a significantly better agreement between the GR and TPR is found in all the overpasses analyzed. The agreement between the results of the two instruments is better for both the percentage of echo areas and the rain amount within each area. It is also better for the agreement of the GR with the gauges. In the absence of TPR data, it will be useful to investigate to what extent long-term, climatological data can be used to substitute TPR data.
  • Keywords
    atmospheric techniques; data acquisition; meteorological radar; microwave propagation; rain; remote sensing by radar; spaceborne radar; Cyprus radar; Tropical Rainfall Measuring Mission; atmospheric precipitation; calibration; climatological data; ground-based radar; linear radar reflectivity; meteorological radar; microwave radio propagation; nonhomogeneous beam filling; rain; range adjustment; spaceborne TRMM precipitation radar; spaceborne weather radar; spatial resolution; Calibration; Instruments; Monitoring; Radar measurements; Rain; Reflectivity; Sampling methods; Spaceborne radar; Spatial resolution; Surveillance; Meteorological radar; Tropical Rainfall Measuring Mission (TRMM); meteorology; microwave radio propagation meteorological factors; numerical analysis and verification; rain; spaceborne and ground-based weather radar;
  • fLanguage
    English
  • Journal_Title
    Geoscience and Remote Sensing, IEEE Transactions on
  • Publisher
    ieee
  • ISSN
    0196-2892
  • Type

    jour

  • DOI
    10.1109/TGRS.2005.858436
  • Filename
    1564402