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Figure 1a: Radar reflectivity indicates two linear snow bands at 5:19 UTC in southern
Oklahoma (one west-to-east oriented, the other southwest-to-northeast oriented).
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Figure 1b: Radar reflectivity indicates three snowbands at 9:15 UTC. The southwest-to-southeast-
oriented bands are quasi-stationary.
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Figure 1c: Radar reflectivity shows that the snow bands have begun moving eastward (14:11 UTC).
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Figure 2a: Small-to-slightly negative differential reflectivity values indicate ice and/or
snow at 5:19 UTC.
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Figure 2b: Small-to-slightly negative differential reflectivity values indicate ice and/or
snow at 9:15 UTC.
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Figure 2c: Small-to-slightly negative differential reflectivity values indicate ice and/or
snow at 14:11 UTC.
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Figure 3a: The hydrometeor classification algorithm classifies precipitation as dry snow
at 5:19 UTC.
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Figure 3b: The hydrometeor classification algorithm classifies precipitation as dry snow
at 9:15 UTC.
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Figure 3c: The hydrometeor classification algorithm classifies precipitation as dry snow
at 14:11 UTC.
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