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Figure 1: Reflectivity at 3:09 UTC 14 September 2002.
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Figure 2: Differential Reflectivity at 3:09 UTC 14 September 2002.
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Figure 3: Correlation coefficient at 03:09 UTC 14 September 2002.
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Figure 4: Hydrometeor Classification Algorithm output at 3:09 UTC 14 September 2002.
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A number of meteorological and non-meteorological features exist
in the polarimetric data at 3:09 UTC 14 September 2002. The precipitation northeast
of KOUN is the remnants of the 13 September precipitation (Figs 1-4). A melting layer within the
precipitation is indicated by the area of high ZDR, low rhohv, and high reflectivity (Figs 1-3). A new convective line has developed
just west of KOUN, with a gust front ahead of its leading edge. This gust front is
evident in these data from 2:20-6:00 UTC, due, inpart, to the abundance of biological scatterers(Figs. 1-12). The bloom of low reflectivities around KOUN exemplies the presence of such
scatterers (esp. north of KOUN from 1:29-6:00 UTC). The hydrometeor classification
algorithm does a good job identifying these non-meteorological targets (Figs. 4,8,12). The "noisy" non-meteorological signal (especially northwest of the convective line) results from interference from another radar.
Following the passage of the convective line through central Oklahoma, flying creatures
are observed west of KOUN from 14:56-17:38 (Figs. 13-16). By 21 UTC, another convective
line has formed west of KOUN with a group of biological scatterers just ahead of it
(Figs. 17-20). As this line evolves, its downdrafts produce a gust front,
observed from 21:49-23:44 UTC (Figs. 21-28). Cell intensity and new cell growth ahead
of the line is enhanced by interactions between the gust front and inflow air (Figs. 25-28).