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John L. Cintineo, Michael J. Pavolonis, Justin M. Sieglaff, Anthony Wimmers, Jason Brunner, and Willard Bellon

(patches E and F), strong cloud-edge brightness temperature gradients (patches B, C, D, and H), and warm clear air pixels around anvil clouds (patches F, H, I, and J). While robust overshooting tops and cold-U features have been known for decades to be associated with intense convection, it is encouraging that the CNN correctly learned and encoded elements of these features. Cloud-edge brightness temperature gradients are less known to be associated with intense convection, yet the model asserts that

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