At the dramatic conclusion of the season's first thunderstorm, the base of a passing cloud takes on mountainous topography. Meteorologists use the term mammatus to describe these distinctive formations. Warm, moist air in the thundercloud rises in a typical convective updraft. It strikes a layer of cooler, dry air in the atmosphere above and spreads outward to produce an anvil-shaped cloud. Ice crystals fall to the bottom of the cloud where they sublimate, changing state directly from ice to water vapor. As this cool air sinks in pockets across the base of the cloud, localized, reverse convection currents are set up—the puffballs that give mammatus clouds their texture.

Autumn weather is as changeable as a teenager's moods. On Sunday night a heavy bank of clouds rolled in just as the Harvest Moon began to peek over the eastern horizon. The low pressure system parked over our heads and remained in place for two days, bringing two inches of much-needed rain.

Wednesday dawned fresh and golden. By early afternoon warmer air had caused unusual cloud formations to build up. Altoculumulus undulatus clouds are named for their resemblance to rippling wave trains along