NASA's UltraViolet Imager, an instrument on the Polar spacecraft,
captured this image of the aurora borealis' distribution across
the North Pole on April 6, 1996. Remarkably, it shows auroral
activity in both the night and day hemispheres of Earth at the
same time—the daytime side being the Western Hemisphere,
which is visible in the lower part of the image. Though reflected
sunlight would drown out the daytime aurora in a visible light
image, ultraviolet light picks it up. The intensity of the
aurora's concentration is color-coded from purple (weakest)
through blue, green, yellow, and red (strongest). A sub-aurora,
the large red area that appears in the upper part of the image,
displays mostly in the night sky.