- Key People:
- Ernst Öpik
- Fred L. Whipple
- Related Topics:
- meteor shower
- bolide
- sporadic meteor
- fireball
- meteor stream
Most of the mass of the solar system resides in its larger bodies, the Sun and the planets. The planets move about the Sun in stable and well-separated orbits. It is almost certain that these orbits have undergone only minor changes since the formation of the solar system some 4.567 billion years ago. In addition, the planets are large enough to retain on their surfaces nearly all the debris excavated from craters produced by colliding bodies.
On the other hand, a smaller fraction of the mass of the solar system is in objects of such small size or in orbits so eccentric (elongated) that their physical survival or orbital stability has been in jeopardy throughout the history of the solar system. Most of these bodies are now found in either of two regions of the solar system—the asteroid belt, between the orbits of Mars and Jupiter, and the Kuiper belt and Oort cloud, which together extend from the orbit of Neptune out to distances typically more than 1,000 times as far. Small bodies would have been distributed throughout the early solar system, but most were rapidly swept up by the planets during a period that ended about four billion years ago. The flux of material from space that now falls on Earth (in the range of tens of thousands of tons per year) and other planets pales in comparison with this early intense bombardment. Since that time, large impacts have become relatively rare. Nevertheless, when they do occur, the results can be dramatic, as in the case of the impact of Comet Shoemaker-Levy 9 with Jupiter in 1994 or the impact of an asteroid or comet thought to be responsible for the extinction of the dinosaurs and other species at the end of the Cretaceous Period 65 million years ago.
For an object to hit Earth, it must be in an orbit which crosses that of Earth. In the case of the rocky asteroids and their fragments, a limited number of processes can put these bodies into Earth-crossing orbits. Collisions can inject material directly into such orbits, but a more efficient process involves gravitational resonances between asteroidal material and planets, particularly Jupiter. Dust particles can also be moved into an Earth-crossing orbit from the asteroid belt through interactions with solar radiation. The above-mentioned processes are discussed in greater detail in the section Directing meteoroids to Earth. In the outermost solar system, icy objects in the Kuiper belt and Oort cloud, which are believed to be the source reservoirs of comets, are perturbed into orbits that ultimately become Earth-crossing through gravitational interactions with Neptune or even with passing stars and interstellar clouds. When such a frozen body travels inside Jupiter’s orbit and approaches the Sun, it gives off gas and sheds small particles, typically taking on the characteristic appearance of a comet. Some of these particles remain in the vicinity of the comet’s orbit and may collide with Earth if the orbit is an Earth-crossing one. This process is further discussed above in the section Meteor showers.
The asteroid belt and the outermost solar system, therefore, can be thought of as long-lived though somewhat leaky reservoirs of meteoroidal material. They are long-lived enough to retain a significant quantity of primordial solar system material for 4.567 billion years but leaky enough to permit the escape of the observed quantity of Earth-crossing material. This quantity of Earth-crossing material represents an approximate steady-state balance between the input from the storage regions and the loss by ejection from the solar system, by collision with Earth, the Moon, and other planets and their satellites, or by impacts between meteoroids.
In addition to cometary and asteroidal sources, a very minor but identifiable fraction of the meteoroidal population comes from the Moon, Vesta, Mars, and possibly Mercury. From studies of meteorites, scientists believe that pieces of the surfaces of these bodies have been ejected into space by large impacts. They also know from the deep-space missions of the Galileo and Ulysses spacecraft that dust particles from outside the solar system are streaming through it as it orbits the centre of the Milky Way Galaxy. These interstellar grains are small and are traveling at high velocities (about 25 km per second) and thus have high kinetic energies, which must be dissipated as heat. Consequently, few are likely to survive atmospheric entry. Even if they do survive, they are rare and hard to discriminate among the much more abundant asteroidal and cometary dust. A meteor of interstellar origin has even been detected. On January 8, 2014, a meteor entered Earth’s atmosphere near Manus Island, Papua New Guinea, and subsequent analysis of its velocity and trajectory showed that it had come from outside the solar system.
