For a brief moment

 For a brief moment, atmospheric conditions align.

High above the clouds, sunlight passes through layers of ice crystals suspended in the upper atmosphere. Each crystal bends and separates the light at precise angles, distributing color outward while the source remains intensely white at the center.

This is light responding to geometry, altitude, and temperature — refraction, dispersion, and alignment occurring simultaneously. The colors do not surround the Sun by chance; they appear as a direct result of how light travels through ice-rich air above the cloud tops.

What makes this moment rare is the timing.

Such conditions occur infrequently and last only seconds before turbulence disrupts the symmetry and the atmosphere returns to a more typical state.

No signal.
No warning.
A short interval where structured patterns become visible — then dissipate.

This is not performance.
It is alignment, briefly observed.