Comets

Overview

Comets are celestial objects composed of frozen gases, rock, and dust. They are characterized by two tails as they orbit near the sun, whose radiation and solar wind vaporize and push gas and dust away from the comet. Comets serve as frozen archives of early solar system chemistry, and some models suggest they played a crucial role in bringing water to Earth during its formation.

Most comets come from two regions of leftover material from the formation of the sun and planets: the Kuiper Belt—a disc of material beyond Neptune, approximately 20 times wider than the asteroid belt—and the Oort Cloud—a spherical shell of icy objects orbiting between 5,000 and 100,000 times the Earth-sun distance. Minor gravitational disruptions can bring comets in these regions toward the inner solar system on highly elliptical orbits. Those originating from the Kuiper Belt can have orbits that repeat with periods of less than 200 years, while those from the Oort Cloud may have periods of about a million years.

Comets are named after the person, observatory, or mission that discovered them following a coded naming system developed by the International Astronomical Union. For example, I3/ATLAS was identified by the Asteroid Terrestrial-impact Last Alert System and is the third interstellar comet—from beyond the Oort Cloud—ever observed.

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