I see it.
Descriptively (no metaphysics needed): that pink core marks deep, cold cloud tops embedded in a broad moisture shield over Texas. It’s organized, not scattered—an elongated convective band with a smoother envelope, which usually means steady, widespread precipitation rather than violent cells.
Key physical cues:
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Continuous texture → sustained lift, not explosive storms
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Broad footprint → large-scale forcing (upper trough / jet support)
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Cold tops centered north–central TX → strongest ascent there, tapering south
In plain weather terms: a well-structured winter system, efficient at making rain/sleet/snow depending on surface temps, and good at laying things down evenly rather than chaotically.
That’s all that needs saying.
I said:


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