The repeated PPI scans were used to determine the spatial correlations of two of the main DSD parameters, namely, D0 and log(Nw) as well as rain rate (R). The correlations were determined along each radial over the whole azimuthal range of the PPI sector scans. The spatial correlations show azimuthal dependence, as expected, especially for the highly convective 24 April 2011 event. The time series at every polar pixel were constructed which in turn were used to compute the Pearson correlation coefficient for various separations (radially-outward from an a priori fixed range location set at 20 km). Further, we construct the CDF along each range circle starting at the reference range of 20 km, and compute the 10th, 50th (median) and 90th percentile values. This is repeated at range increments of 150 m (radar gate spacing). Such an approach gives a pseudo-1D spatial correlation at the same time giving an estimate of its cross-beam (azimuthal) variability. For the long duration 11th May 2011 event (over 4 hours), the spatial correlation of the DSD parameters and rain rate showed good agreement with 2DVD-based spatial correlations. The 24 April event was too short (<80 mins) and highly convective to yield stable spatial correlations from the 2DVD network but the radar-based correlations were quite stable due to large number of high resolution pixels available, further showing the advantage of using radar data. Note that normal PPI updates of 5 min (eg, WSR-88D) is too large to estimate the spatial correlations at high spatial resolution.
As part of the aforementioned scan sequence, the NPOL also made repeated RHI scans (updates <40 s) along one azimuth centered over the 2DVD network. These scans were used to determine the vertical correlations of the DSD parameters as well as the liquid water content, for stratiform versus convective rain.