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Figure 1: The radar reflectivity field at 2:11 UTC shows anomalous propagation north and east of KOUN.
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Figure 2: The radar reflectivity field at 4:19 UTC indicates precipitation ahead of a cold
front approaching OKC from the northwest.
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Figure 3: The mix of low and moderate differential reflectivity values associated with the
radar reflectivity field at 4:19 UTC suggests light snowfall combined with areas of larger, horizontally-oriented
aggregates.
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Figure 4: The field of high correlation coefficients with embedded lower correlation coefficients,
colocated with higher ZDRs (see Fig. 3) at 4:19 UTC suggests light snowfall combined with areas of larger, horizontally-oriented
aggregates.
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Figure 5: The "linear" band of low reflectivity moving away from KOUN 7:06 UTC suggests the passage
of the cold front through central Oklahoma.
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Figure 6: The "linear" band of ice crystals moving away from KOUN at 7:06 UTC suggests the
passage of the cold front through central Oklahoma.
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Figure 7: Northwest-to-southeast-oriented bands of low reflectivity exist in the vicinity
of KOUN at 14:12 UTC.
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Figure 8: A mix of small positive and negative differential reflectivity values associated
with the reflectivity image at 14:12 UTC indicate bands of ice crystals.
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Figure 9: The hydrometeor classification algorithm classifies the bands of ice crystals
as dry snow.
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