A recent report from the National Academy of Sciences points out that NASA has been tasked to locate 90 percent of the most deadly objects that could conceivably strike our planet. Yet only about a third of this assignment has been completed, and the money has yet to be found to complete the job. The agency calculates it needs about $800 million between now and 2020 to make the needed inventory, while $300 million would allow it to find most objects larger than 300 meters across.
The problem is that even the smaller sum is not available, and this AP story quotes space policy expert John Logsdon (George Washington University) as saying the money may never come through, calling the program “a bit of a lame duck.” In other words, there is not yet enough pressure on Congress to produce the needed funds. Meanwhile, asteroid detection remains a low priority for other governments as well, making this a problem we’re choosing to ignore in the absence of recent reminders of its potential.
Asteroid Numbers and Risk
The absence, at least, of recent reminders on Earth — we just saw what happened on Jupiter, with its admittedly larger gravitational well. The comet strike on that giant world reminds us of NASA’s current estimate that there are 20,000 objects — comets and asteroids — that are potential threats to our own world, each larger than 140 meters in diameter. We know the position of about a third of these. The AP story cites Lindley Johnson, manager of NASA’s Near Earth Object Program:
At the moment, NASA has identified about five near-Earth objects that pose better than a 1-in-a-million risk of hitting Earth and being big enough to cause serious damage, Johnson said. That number changes from time to time, as new asteroids are added and old ones are removed as information is gathered on their orbits.
The space rocks astronomers are keeping a closest eye on are a 430-foot (130-meter) diameter object that has a 1-in-3,000 chance of hitting Earth in 2048 and a much-talked about asteroid, Apophis, which is twice that size and has a one-in-43,000 chance of hitting in 2036, 2037 or 2069.
A New Asteroid Population Near Earth?
Meanwhile, an interesting paper by Takashi Ito (National Astronomical Observatory, Tokyo) and Renu Malhotra (University of Arizona) looks at the asymmetric distribution of craters on the lunar surface, questioning whether what we now know about near-Earth asteroids can account for what we see there. Various possibilities exist, including tidal forces breaking asteroids apart to create more numerous craters than we would expect, but there is also the possibility that there is an undetected population of objects co-orbiting with the Earth that has yet to be detected.
To study the issue, the authors simulated the orbital evolution of a large number of test particles representing near-Earth asteroids, working with one population made up of currently known NEAs, and one created as a synthetic group outside the known NEA orbital distribution. What emerged is interesting when weighed against lunar observations:
The NEA-like particles that we used in our numerical integrations, particularly the population A that does not include the particles with large random orbital velocity, have low relative velocity with respect to the Earth-Moon system. In other words, these particles are the “slowest” (relative to Earth) among all the known small body populations in the solar system.
Can the particles accurately model what we see on the Moon? The paper continues:
The fact that even these slow particles do not fully reproduce the asymmetric distribution of impacts as large as what is seen in the lunar crater record, suggests that there may exist a presently-unobserved population of small objects near the Earth’s orbit that have even lower average relative velocity than the currently known near-Earth asteroids do.
We end up with the possible existence of a population of slow objects orbiting the Sun close to the Earth-Moon system. Based on their simulations, the authors estimate the population of ‘slow NEAs’ as roughly fifty percent more than the fraction of known slow NEAs. The definition of ‘slow NEA’ is a near-Earth asteroid with a potential lunar impact velocity of less than 11 kilometers per second. These are objects, in other words, that are nearly co-orbiting with the Earth.
Observing Programs Not Optional
Do such objects exist? The authors note the need for more complete observational surveys of near-Earth asteroids to test their prediction. And they’re careful to run through the alternatives, which include (in addition to asteroid fragmentation) the possibility that future mapping missions will give us a better dataset regarding the crater asymmetry.
Whatever we learn about lunar cratering, this paper yanks our chain yet again — we need to learn much more about the objects that could do our planet harm. We’re finally approaching the technological stage when we could actually do something about a predicted impact. What remains to be seen is whether we’ll firm up our observing programs in time to put that technology to work in the event we spot something truly dangerous.
The paper is Ito and Malhotra, “Asymmetric impacts of near-Earth asteroids on the Moon,” submitted to Astronomy & Astrophysics (preprint).
Debris ejected into heliocentric orbits after being blown off Earth or the Moon could provide a population of low velocity meteoroids. Alternatively we’re seeing ‘drift’ from the L-point population which should approach the Earth-Moon system at very low relative velocity.
Hi Paul;
I could not be in better agreement with you regarding the last paragraph above. As our civilization ages, we will repeatedly run up against potential threats and game-changers such as asteriods, comets, supernova especially of blue hypergiant stars, and even the potential big rip that might result from an increasing universe expansion rate, among other concerns.
Luckily, the latter two examples are something we do not need to consider immeadiately except for the potential super nova of Eta Carinae in the coming centuries.
Asteriods and comets do pose a danger that should not be trivialized. I am a little dismayed at the conplacency of our space program when it comes to tracking these objects. And of course, the technology developed to divert or destroy an asteriod can be incorporated into the propulsion systems of faster manned interplanetary space craft.
One danger that will be very hard to avert, I am afraid, is the category of intrinsic (i.e. not coming from outside) geological dangers, I mean particularly the so-called super volcanic eruptions, such as Yellowstone. Of course volcanoes are the breathing of the planet, but sometimes she coughs. And Yellowstone is even more or less due, give or take another hundred millennia.
The low relative velocity will also make these objects harder to detect
which is a worry for the completeness of any survey.
Spend a few bucks to monitor NEOs or risk the chance of an impact
that could destroy an entire metropolis, kill millions, and cost trillions
of dollars.
Seems pretty obvious to me.
In Search of Dark Asteroids (and Other Sneaky Things)
NASA Science News for September 15, 2009
NASA is set to launch a sensitive new infrared telescope to seek out sneaky
things in the night sky — among them, dark asteroids that could pose a threat to Earth.
FULL STORY at
http://science.nasa.gov/headlines/y2009/15sep_ninjaastronomy.htm?list1094208
Dynamical erosion of the asteroid belt and implications for large impacts in the inner solar system
Authors: David A. Minton, Renu Malhotra
(Submitted on 21 Sep 2009)
Abstract: The cumulative effects of weak resonant and secular perturbations by the major planets produce chaotic behavior of asteroids on long timescales. Dynamical chaos is the dominant loss mechanism for asteroids with diameters D > 10 km in the current asteroid belt. In a numerical analysis of the long term evolution of test particles in the main asteroid belt region, we find that the dynamical loss history of test particles from this region is well described with a logarithmic decay law.
In our simulations the loss rate function that is established at t = 1 My persists with little deviation to at least t = 4 Gy. Our study indicates that the asteroid belt region has experienced a significant amount of depletion due to this dynamical erosion – having lost as much as ~50% of the large asteroids – since 1 My after the establishment of the current dynamical structure of the asteroid belt.
Because the dynamical depletion of asteroids from the main belt is approximately logarithmic, an equal amount of depletion occurred in the time interval 10-200 My as in 0.2-4 Gy, roughly ~30% of the current number of large asteroids in the main belt over each interval.
We find that asteroids escaping from the main belt due to dynamical chaos have an Earth impact probability of ~0.3%. Our model suggests that the rate of impacts from large asteroids has declined by a factor of 3 over the last 3 Gy, and that the present-day impact flux of D > 10 km objects on the terrestrial planets is roughly an order of magnitude less than estimates currently in use in crater chronologies and impact hazard risk assessments.
Comments: 39 pages, 12 figures, 3 tables
Subjects: Earth and Planetary Astrophysics (astro-ph.EP)
Cite as: arXiv:0909.3875v1 [astro-ph.EP]
Submission history
From: David Minton [view email]
[v1] Mon, 21 Sep 2009 23:03:31 GMT (4130kb)
http://arxiv.org/abs/0909.3875