This dramatic sky is the result of several atmospheric processes occurring simultaneously. The curved, layered cloud structure is characteristic of a supercell thunderstorm, where strong wind shear causes the storm to rotate and organize into spiral bands. The rainbow-like colors embedded in the cloud are not a typical rainbow, but a form of cloud iridescence, produced when sunlight is diffracted by tiny, uniformly sized water droplets or ice crystals within the cloud. Lightning visible beneath
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This dramatic sky is the result of several atmospheric processes occurring simultaneously. The curved, layered cloud structure is characteristic of a supercell thunderstorm, where strong wind shear causes the storm to rotate and organize into spiral bands. The rainbow-like colors embedded in the cloud are not a typical rainbow, but a form of cloud iridescence, produced when sunlight is diffracted by tiny, uniformly sized water droplets or ice crystals within the cloud. Lightning visible beneath
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