The moon's orbit can be traced backwards in time to reveal that when the moon formed near the Earth, its orbit was inclined by approximately 10 degrees relative to the Earth's equator. Most other planetary satellites in the solar system have orbital inclinations smaller than 1 or 2 degrees. The cause of the moon's large orbital tilt has long been a mystery.
"The inclination problem had been one of the last remaining obstacles for the impact hypothesis of moon formation," says SwRI Institute Scientist Dr. William R. Ward. The widely favored "giant impact theory" proposes that a Mars-sized body collided with Earth 4.5 billion years ago, creating a hot disk of debris from which the moon accumulated. Previous models of the moon's formation from such a disk predict that the lunar orbit should have been nearly aligned with the Earth's equator, with only about a 1 degree tilt.
The new theory, published in the Feb. 17 issue of Nature, proposes that the moon acquired its large tilt soon after it formed because of a gravitational interaction with debris left over from the impact event. Modeling results presented in the paper, authored by Ward and SwRI planetary scientist Dr. Robin M. Canup, show that the moon could have acquired its 10 degree tilt as a consequence of the moon-forming impact.
To yield a lunar-sized moon, the giant impact must place about two lunar masses of material into an Earth-orbiting disk, according to Canup. In the model, debris particles in the inner regions of such a disk are prevented from coalescing by Earth's gravity, which tends to pull objects apart. Instead, the moon rapidly coalesces at the outer edge of the debris disk, at a distance of about 14,000 miles from the Earth. "The newly formed moon would have likely co-existed for some time with an inner disk of gas and debris left over from the impact," says Canup.
After the moon coalesced, its gravity would generate waves in the inner disk. The gravitational interaction of the moon with these waves would, in turn, modify the lunar orbit. The waves are launched at certain locations in the disk where the motions of disk particles are in resonance with the motion of the moon.
The waves generated at one such resonance -- where the orbital period of the moon is approximately three times that of the disk particles -- are called "bending waves," which corrugate the surface of the disk. The gravitational attraction between the moon and these rippled waves in the disk then acts to amplify the tilt of the moon's orbit.
Ward and Canup's model simulated the interaction of the moon and the inner debris disk, assuming that the moon formed in an orbit with only a 1 degree tilt. They found that the interaction of the moon with the bending waves it generates in such a disk can amplify the lunar inclination to values as high as 15 degrees before the disk dissipates. The required tilt of about 10 degrees can be achieved if the disk contained at least 25 to 50 percent of a lunar mass and persisted from decades to as long as a century. These values are consistent with those predicted by other models of the impact event.
"This theory explains the moon's anomalous orbital tilt as a natural consequence of its formation from a giant impact event," says Ward. "Rather than producing conflicting evidence, the lunar inclination may now represent an additional corroboration of the impact event," agrees Canup.
SwRI is an independent, nonprofit, applied research and development organization based in San Antonio, Texas, with more than 2,700 employees and an annual research volume of more than $300 million.
An image to support this story is available at http://www.swri.org/press/inline.htm
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