Can an Asteroid Really Destroy Earth in 800 Years?

GM (2/r - 1/a) ...where r is the distance from the focus - the Sun - to the perihelion (in meters), and a is the semimajor axis (in meters). The third root of the reciprocal of the semimajor axis (in inverse astronomical units) is the inverse of the perihelion distance (in inverse astronomical units). If you're dealing with an elliptical orbit, the perihelion distance will be the closest approach, and the aphelion distance will be the farthest distance from the focus. a = (rmax/(1+e)) + (rmin/(1-e)) If you're dealing with a
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Razi Abid
I have seen many movies relating to the destruction of the Earth from space rocks and asteroids. Sometimes I think our planet might be attacked by such things. Even more I heard that scientist have observed an asteroid heading to Earth and might crash after about 800 years. Can this ever happen?
 
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  • #2
That particular danger evaporated after astonomers recalculated the orbit. But sure, big rocks - way big - can and have hit the earth. It pretty well settled that the dinosaurs were done in by a comet or asteroid crash some 65 million year ago. And the modern theory of the moon's formation is based on the Earth getting a big whack from a near planet sized object back in the early formation days.

Can it happen in our time? Yes, but not very likely. The big guys are few and far between, and every one that did crash in the past is one that will never do that again. Obviously the whole two million years or so of homo sapiens has not been interrupted by a big crash.
 
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Jupiter is a big enough target that major impacts are probably pretty common. I am old enough to remember the excitement generated among astronomers by the comet Shoemaker-Levy hitting Jupiter. Big comet, big planet, big collision.
 
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people who interpret nostradamus are foolish. Did you follow the big flap about the King of Terrors that was supposed to come down on us in July 1999?
 
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SelfAdjoint, I missed that one I guess. I do remember that about a decade ago a Korean sect prepared for Christ's Second Coming, prophesied to be on some certain day, by among other things aborting pregnancies. That had to be Pat Robertson's ultimate nightmare.
 
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There are several dedicated searches underway to identify any threats from NEOs, PHAs, etc (Near Earth Objects, Potentially Hazardous Asteroids). This site is a good one for keeping track of news, searches, results and so on.

As SelfAdjoint noted, every now and then a NEO is observed with a preliminary orbit that has a low, but non-zero, probability of intersecting the Earth sometime in the next millenium. Subsequent work - in the next week or two - to refine the orbit has always reduced those probabilities to zero.

The post-discovery work is basically of two kinds - more observations, with more telescopes in different locations; and searches of old astronomical plates (before CCDs made them extinct, almost all astronomical images were made on glass plates covered in special photographic emulsion) and images. Often these searches will find 'pre-covery' images of the NEO, allowing a better orbit to be calculated. With the increasing availability of vast amounts of historical astronomical data via the internet, anyone with a broadband connection can do this research! Yes, even any PF member!

Well over 90% of all NEOs and PHAs will likely be identified in the next decade. Will we then be able to breath easy? No, because there's a class of potential homo sap (and all complex life on Earth) killers we aren't ever likely to identify - (new) comets.
 
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  • #9
Razi Abid said:
I have seen many movies relating to the destruction of the Earth from space rocks and asteroids. Sometimes I think our planet might be attacked by such things. Even more I heard that scientist have observed an asteroid heading to Earth and might crash after about 800 years. Can this ever happen?
800 years!? I'd like to know how anybody can accurately predict the cumulative perturbations of an Earth-crossing asteroid across that much time...accurately enough to predict a collision or a miss with Earth, that is.

I remember that JPL had to do a probability distribution for a 2001 XU encounter, and that wasn't anywhere near eight centuries. (2001 XU is an asteroid in an 8:33 tidal resonance with Earth, with a closest possible approach - for now - of 19,000 kilometers.)

An asteroid with an absolute magnitude (solar system scale) of 22.0 and a (typical) surface albedo of 0.13 will be about 150 meters in diameter. A difference of one magnitude corresponds to an increase or decrease in reflected power by the fifth root of 100, or 2.511886431.

For example, 2001-XU has an absolute magnitude of 19.01, and therefore...

Reflected power = 100^{(22-19.01)/5} = 15.7

...as compared to the reflected power from a 150-meter asteroid.

Reflected power varies according to surface area, which depends on the square of the average radius. So 2001-XU is about 3.96 times as wide as a 150-meter asteroid is. Its average radius is about 297 meters.

If we pretend that the asteroid is spherical, then the volume is 110 million cubic meters.

If we assume that the average density is 3000 kilograms per cubic meter (typical for rock), the mass is about 330 billion kilograms. (No attempt at precision is being made here; this is just a ballpark calculation.)

Here's an equation that I put together to let you reach the impact energy directly.

K = 1.26 megatons TNT { 100^[0.3 (22-MAG)] } V^2

Where K is kinetic energy, MAG is the asteroid's absolute magnitude, and V is the asteroid's speed relative to Earth at impact, in kilometers per second.

The equation implicitly assumes that the asteroid reflects 13% of incident sunlight. You would discover the relative speed by reducing the orbital elements for Earth and for the asteroid to obtain the velocity vectors of each at the moment of impact, viz...

*** top of velocity calculation section ***

a : semimajor axis of the orbit
e : eccentricity of the orbit

1 astronomical unit = 1.49597870691E+11 meters

GMsun = 1.32712440018E+20 m^3 sec^-2

The canonical velocity in a hyperbolic orbit, in general, is found from

Vx’’’ = -(a/r) { GMsun / a }^0.5 sinh u

Vy’’’ = +(a/r) { GMsun / a }^0.5 (e^2 - 1)^0.5 cosh u

Vz’’’ = 0

Where u is the eccentric anomaly and r is the current distance from the sun.

The canonical velocity in an elliptical orbit, in general, is found from

Vx’’’ = -sin Q { GMsun / [ a (1-e^2) ] }^0.5

Vy’’’ = (e + cos Q) { GMsun / [ a (1-e^2) ] }^0.5

Vz’’’ = 0

Where Q is the true anomaly.

The triple-primed vectors would be rotated (negatively) by the angular elements of the orbit (w,i,L) to heliocentric ecliptic coordinates.

Rotation by the argument of the perihelion, w.

Vx'' = Vx''' cos w - Vy''' sin w

Vy'' = Vx''' sin w + Vy''' cos w

Vz'' = Vz''' = 0

Rotation by the inclination, i.

Vx' = Vx''

Vy' = Vy'' cos i

Vz' = Vy'' sin i

Rotation by the longitude of ascending node, L.

Vx = Vx' cos L - Vy' sin L

Vy = Vx' sin L + Vy' cos L

Vz = Vz'

The unprimed vector [Vx, Vy, Vz] is the velocity in the orbit, referred to heliocentric ecliptic coordinates.

*** end of velocity calculation section ***

The impact speed will be the magnitude of the vector difference between the HEC velocity of the asteroid and the HEC velocity of the Earth.

If 2001-XU ever hits Earth, it will be moving at 28.9 km/sec, which corresponds to an impact energy of 2.76+20 Joules, which is equivalent to 65,600 megatons TNT (or 65.6 gigatons). This kind of thing might, possibly, you know, destroy the world.

Modeling asteroid impact effects.
http://www.lpl.arizona.edu/impacteffects/

Asteroid orbital elements.
http://ssd.jpl.nasa.gov/sb_elem.html
http://arnold.usno.navy.mil/murison/Asteroids/OrbitalElements.html

Jerry Abbott
 
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1. What is the difference between an asteroid and a space rock?

An asteroid is a small rocky object that orbits the sun, while a space rock is a general term used to describe any small, rocky object in space including asteroids, meteoroids, and comets. Asteroids are typically larger and have a more defined orbit, while space rocks can vary in size and trajectory.

2. How do asteroids and space rocks form?

Asteroids and space rocks are believed to form from the leftover debris of the early solar system. As planets and other objects formed, there was leftover material that did not coalesce into larger bodies. This material then formed into smaller objects such as asteroids and space rocks.

3. Can asteroids and space rocks collide with Earth?

Yes, asteroids and space rocks can collide with Earth. In fact, Earth is hit by thousands of tons of space debris every day. Most of these objects are small and burn up in our atmosphere. However, larger objects can cause damage and even extinction events if they collide with Earth.

4. How are asteroids and space rocks studied?

Scientists study asteroids and space rocks through various methods such as ground-based telescopes, spacecraft missions, and meteorite analysis. By studying the composition, size, and trajectory of these objects, scientists can learn more about the formation and evolution of our solar system.

5. Is there a risk of an asteroid or space rock impacting Earth in the future?

While the probability of a large asteroid or space rock impacting Earth is low, it is still a possibility. NASA and other space agencies are constantly monitoring space objects and developing strategies to mitigate any potential impact. However, it is important for continued research and observation to better understand and prepare for any future impacts.

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