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Figure 1: On 9 September 2002, at 14:55 UTC, the radar reflectivity field indicates
stratiform precipitation over southern Oklahoma.
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Figure 2: On 9 September 2002, at 14:55 UTC, the differential reflectivity field
indicates nearly spherical particles comprise the stratiform precipitation. The colocation
of such small ZDRs with low reflectivity suggests small droplets are observed.
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Figure 3: On 9 September 2002, at 14:55 UTC, the specific differential reflectivity
indicates light rain rates across most of southern Oklahoma.
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Figure 4: On 9 September 2002, at 14:55 UTC, the hydrometeor classfication algorithm
identifies mostly stratiform precipitation across southern Oklahoma.
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