Mystery of disappearing asteroids solved
A new study finds that most asteroids and comets are destroyed in a drawn out, long hot fizzle, much farther from the Sun than previously thought.
Ever since it was realized that asteroid and comet impacts are a real and present danger to the survival of life on Earth, it was thought that most of those objects end their existence in a dramatic final plunge into the Sun. A new study finds instead that most of those objects are destroyed in a drawn out, long hot fizzle, much farther from the Sun than previously thought. This surprising new discovery explains several puzzling observations that have been reported in recent years.
An international team composed of researchers from Finland, France, the United States, and the Czech Republic originally set out to construct a state-of-the-art model of the near-Earth-object (NEO) population that is needed for planning future asteroid surveys and spacecraft missions. The model describes the NEOs’ orbit distribution and estimates the number of NEOs of different sizes.
The vast majority of NEOs originate in the doughnut-shaped main asteroid belt between the orbits of Mars and Jupiter. The orbit of a main-belt asteroid slowly changes as it is pushed by the uneven release of excess solar heat from the asteroid’s surface. The asteroid’s orbit eventually interacts with the orbital motions of Jupiter and Saturn, changing the trajectory to bring the asteroid close to Earth. An asteroid is classified as an NEO when its smallest distance from the Sun during an orbit is less than 1.3 times the average Earth-Sun distance.
The team used the properties of almost 9,000 NEOs detected in about 100,000 images acquired over about eight years by the Catalina Sky Survey (CSS) near Tucson, Arizona, to construct the new population model. One of the most challenging problems facing the team was computing which asteroids they could actually detect. An asteroid appears as a moving point of light against a background of fixed stars but detecting it on an image depends on two factors — how bright it is and how fast it seems to be moving. If the telescope isn’t looking at the right location at the right time when an asteroid is bright enough and slow enough to be detected, we simply may never find that asteroid.
Robert Jedicke, a team member at the University of Hawaii Institute for Astronomy developed the software needed to compute how likely it was for asteroids on different orbits to have been detected by the Catalina Sky Survey. This calculation required a detailed understanding of the operations of the telescope and detector systems and a tremendous amount of computing time even with novel, fast mathematical techniques. The team produced the best-ever model of the NEO population by combining this information with the CSS data and theoretical models of the orbit distributions of NEOs that originate in different parts of the main belt.
But they noticed that their model had a problem — it predicted that there should be almost 10 times more objects on orbits that approach the Sun to within 10 solar diameters. The team then spent a year verifying their calculations before they came to the conclusion that the problem was not in their analysis but in their assumptions of how the solar system works.
Mikael Granvik from the University of Helsinki hypothesized that their model would better match the observations if NEOs are destroyed close to the Sun but long before an actual collision. The team tested this idea and found an excellent agreement between the model and the observed population of NEOs when they eliminated asteroids that spend too much time within about 10 solar diameters of the Sun. “The discovery that asteroids must be breaking up when they approach too close to the Sun was surprising and that’s why we spent so much time verifying our calculations,” said Jedicke.
The team’s discovery helps to explain several other discrepancies between observations and predictions of the distribution of small objects in our solar system. Meteors, commonly known as shooting stars, are tiny bits of dust and rock that are dislodged from the surfaces of asteroids and comets that then end their lives burning up as they enter our atmosphere when they appear as fast moving bright flashes of light in the night sky. They travel in streams that follow the path of their parent object, but astronomers have been unable to match most of the meteor streams with any known object. This study suggests that the parent objects were completely destroyed when they came too close to the Sun — leaving behind streams of meteors but no parent NEOs. They also found that darker asteroids are destroyed farther from the Sun than brighter ones, explaining an earlier discovery that NEOs that approach closer to the Sun are brighter than those that keep their distance. The fact that dark objects are more easily destroyed implies that dark and bright asteroids have a different internal composition and structure.
According to Granvik, their discovery of the catastrophic loss of asteroids before a collision with the Sun allows planetary scientists to understand a variety of recent observations from a new perspective but also leads to a more profound advance in asteroid science: “Perhaps the most intriguing outcome of this study is that it is now possible to test models of asteroid interiors simply by keeping track of their orbits and sizes. This is truly remarkable and was completely unexpected when we first started constructing the new NEO model.”