Detecting Asteroid Collisions: 'Oumuamua & Radio Telescopes

In summary, an educated laymen would say that although science and technology have not found a way to detect a big asteroid collision with Earth, radio telescopes around the world should be able to detect an object of that size on course to hit Earth in due time.
  • #36
websterling said:
In the article they're talking about a signal from a 100W laser; entirely different physics involved.

With radar I think the limit for just detection of a 1km object is less than 1 AU, less than a 15 minute round trip time. For an object like Oumuamua it would be far less.

What are the basic technical and scientific hurdles for this 1km and less than 1 AU range/size limit?
 
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  • #37
roineust said:
What are the basic technical and scientific hurdles for this 1km and less than 1 AU range/size limit?

1) There's a limit to the transmitter power available.
2) Signal strength falls off as ##1/d^2##.
3) Dust covered rocky objects are poor reflectors.
4) 1km is rather small.
5) The return also falls off as ##1/d^2##.
 
  • #38
websterling said:
In the article they're talking about a signal from a 100W laser; entirely different physics involved.

With radar I think the limit for just detection of a 1km object is less than 1 AU, less than a 15 minute round trip time. For an object like Oumuamua it would be far less.

To which specific radar type, class or model were you referring to, which have these limits (1km 1 AU) and yet are the best currently available, for such an asteroid finding task? You meant hypothetical usable radars or ones that already exist as part of an asteroid detection system? You did mention that radars are already used to search for near Earth objects, you probably meant space derbies collision avoidance for the ISS or did you refer to other radars that search further away than space derbies? How come these radars are able to detect meteors, as you mentioned, while meteors are much smaller objects than asteroids? You meant only when meteors are as close to us as space derbies or less?

What i could find regarding radars and space derbies was Cobra Dane and EISCAT.
 
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  • #39
|Glitch| said:
It also helps if you are actually looking for them, which NASA wasn't prior to being given a congressional directive in 1998.
You ignored @nikkkom 's point, so I'll expand/repeat: Robotic/automated sky surveys were at best difficult and at worst impossible until at least the 1980s. But the capabilities expanded so fast that starting in the 1990s, amateurs regularly discover comets and asteroids. Many do their own automated sky surveys, discovering dozens or even hundreds. These days, hunting for such objects is so easy it is practically a race.

Sure, there is a a bit of a chicken-or-egg issue here, but what is certainly NOT a component of it is the implication that we could have found these thousands of objects in the 60s or 70s if we had simply decided to look. We could not have. And conversely, whether Congress was the cart or horse, a significant fraction of these objects were going to be found either way.

[edit] A quick google tells me that the first commercial CCD camera (100x100 pixels) was released in 1975 and the first telescope with a digital camera (pointed down ;) ) was launched into space in 1976. So I think it is fair to say that digital sky surveys were impossible until at least 1976.
 
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  • #40
russ_watters said:
You ignored @nikkkom 's point, so I'll expand/repeat: Robotic/automated sky surveys were at best difficult and at worst impossible until at least the 1980s. But the capabilities expanded so fast that starting in the 1990s, amateurs regularly discover comets and asteroids. Many do their own automated sky surveys, discovering dozens or even hundreds. These days, hunting for such objects is so easy it is practically a race.

Unfortunately (or not) those days have been over for years if you are talking about the amateurs due to the big automated surveys. It is only going to get even harder for the amateurs when LSST comes online and with GAIA's later data releases.

Most amateurs switched to followup observations or other areas like variable stars years ago. See for instance this article https://www.airspacemag.com/as-interview/aamps-interview-roy-tucker-112571/?all
 
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  • #41
russ_watters said:
You ignored @nikkkom 's point, so I'll expand/repeat: Robotic/automated sky surveys were at best difficult and at worst impossible until at least the 1980s. But the capabilities expanded so fast that starting in the 1990s, amateurs regularly discover comets and asteroids. Many do their own automated sky surveys, discovering dozens or even hundreds. These days, hunting for such objects is so easy it is practically a race.

Sure, there is a a bit of a chicken-or-egg issue here, but what is certainly NOT a component of it is the implication that we could have found these thousands of objects in the 60s or 70s if we had simply decided to look. We could not have. And conversely, whether Congress was the cart or horse, a significant fraction of these objects were going to be found either way.

[edit] A quick google tells me that the first commercial CCD camera (100x100 pixels) was released in 1975 and the first telescope with a digital camera (pointed down ;) ) was launched into space in 1976. So I think it is fair to say that digital sky surveys were impossible until at least 1976.
@nikkkom 's point was irrelevant. I wasn't debating the efficiency of automated searches. You pretend as if nothing could be discovered prior to CCDs, when we know that is not true. Granted, it is not as "efficient" as an automated/robotic search, but we have taken photographs of the same part of the sky at different times and then compared them to see if anything moved. How do you think Pluto was discovered?

NASA is also a government agency that does what they are directed to do by both Congress and the President. It is not like they have the initiative (or an unlimited budget) to do whatever they please. If Congress does not direct NASA to locate NEOs, and does not provide funding for that purpose, then NASA will not locate NEOs. Which is what happened between 1958 and 1998.
 
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  • #42
|Glitch| said:
@nikkkom's point was irrelevant.

I feel hurt, distressed and also don't care :D
 
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  • #43
mfb said:
Even if we assume you manage to break the asteroid apart: So what? Now you have several smaller components that still fly towards Earth with the same combined energy. But instead of one area with a massive impact crater you get many impact craters scattered over a large area. You might even increase the damage it does.
Not to mention these fragments are highly radioactive. You've traded a sniper rifle for a plutonium shotgun.
 
  • #44
TeethWhitener said:
Not to mention these fragments are highly radioactive.

It would be low- or medium-reactive material, depending in the size of the warhead (the bigger the less radioactive). An explosion of the same size on Earth would produce more nuclear fallout and we had many of them in the past. The resulting increase of the background radiation would be an irrelevant side-effect of the impact. The main problem is in fact the fragmentation of the asteroid.
 
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  • #45
DrStupid said:
The main problem is in fact the fragmentation of the asteroid.

Non-fragmented asteroid is exponentially more destructive.
1-2 meter fragments will do no damage whatsoever.
20-meter fragments generally won't reach the surface too (a-la Chelyabinsk) but cause shockwave damage.
50-meter fragments can cause a city-scale destruction.
200-meter intact asteroid would leave about 5km diameter crater.
 
  • #46
64 scattered city-scale destruction areas (hard to evacuate) vs. one larger focused spot of destruction (possible to evacuate).
 
  • #47
230x35x35m asteroid can't be separated into 64 30m fragments. Maximum eight fragments.

Fragmentation at ~500km altitude means ~25 seconds to impact. If big fragments would have ~100m/s lateral velocities, they can drift apart by ~2.5 km only. The destruction will still be localized in about the same location, not spread across half a continent.
 
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  • #48
If you break it up that late it doesn’t matter anyway.

The number of fragments scales with the cube of the length scale. It doesn’t matter which shape you assume but be consistent - don’t switch in between.
 
  • #49
nikkkom said:
The destruction will still be localized in about the same location

And so will be the energy. Just the type of destruction will change. The larger the fragments the higher the ratio of mechanical effects (e.g. shock waves or seismic waves). The smaller the fragments the larger the ratio of radiative effects (e.g. heat radiation or emp). It depends on the circumstances which of them are more destructive. A direct hit could kill a city in any case.
 
  • #50
DrStupid said:
And so will be the energy. Just the type of destruction will change. The larger the fragments the higher the ratio of mechanical effects (e.g. shock waves or seismic waves). The smaller the fragments the larger the ratio of radiative effects (e.g. heat radiation or emp).

Exactly.
Energy in different forms has very different destructive potential.
For example, one kilogram of burning wood releases more energy than a hand grenade.

If you turn this asteroid into 1-5 meter fragments, on entry its energy will be converted almost entirely to light and shock waves in the air.
Light flash would be spectacular but won't be intense enough to do harm.
Shock waves would cause widespread window damage and may cause moderate structural damage in some buildings.
 
  • #51
nikkkom said:
Light flash would be spectacular but won't be intense enough to do harm.

We are talking about several Gt TNT equivalent. That would be sufficient to raise the temperature of the entire atmosphere within a 10 km radius around ground zero by some hundred K. The temperatures in the upper atmosphere, where most of the energy is initially released, would be much higher. A major part of the resulting heat radiation would pass the atmosphere and reach the ground, resulting in a second temperature peak at ground level. I don't believe that this would be harmless until I see a corresponding calculation.

nikkkom said:
Shock waves would cause widespread window damage and may cause moderate structural damage in some buildings.

Even the Chelyabinsk meteor caused widespread window damage and moderate structural damage in some buildings in Chelyabinsk which is 40 km away from ground zero. A direct hit with several thousand times the energy would raze the city to the ground and let it go up in flames.
 
  • #52
DrStupid said:
>> Light flash would be spectacular but won't be intense enough to do harm.

We are talking about several Gt TNT equivalent. That would be sufficient to raise the temperature of the entire atmosphere within a 10 km radius around ground zero by some hundred K.

...if all of it is absorbed. Which does not happen.

A direct hit with several thousand times the energy

This particular asteroid would not have "several thousand times the energy" of Chelyabinsk event. More like about 50 times more energy. (Chelyabinsk bolide estimated to be ~20m, Oumuamua is ~230m x 35m x 35m).
 
  • #53
nikkkom said:
..if all of it is absorbed. Which does not happen.
The energy is still there - if it doesn't get absorbed by the atmosphere that just means it directly reaches the ground and heats that.

230*35*35/203=35. If we give the asteroid 3 times the speed it has 315 times the energy. If we give it 8 times the speed it has 2200 times the energy. Not necessarily thousands of times, but the difference is still huge.
 
  • #54
mfb said:
The energy is still there - if it doesn't get absorbed by the atmosphere that just means it directly reaches the ground and heats that.

Half of the energy which has been converted to light goes up straight to space and has no effect. The other half shines onto the ground, and part of that (on average 30%) gets reflected.
 
  • #55
nikkkom said:
This particular asteroid would not have "several thousand times the energy" of Chelyabinsk event. More like about 50 times more energy. (Chelyabinsk bolide estimated to be ~20m, Oumuamua is ~230m x 35m x 35m).

With 230m x 35m x 35m Oumuamua has a volume of about 2.8·105 m³ and with a density of 1500 kg/m³ a mass of 4.2·108 kg. With a speed of 50 km/s this results in a kinetic energy of 5.3·1017 J which corresponds to 1.3 Gt TNT eqivalent. That's like 25 Tsar bombs (50 Mt) or 2500 times the energy of the Chelyabinsk meteor (500 kt). What makes you think the resulting destructions at ground zero would be similar to a single Chelyabinsk meteor in a distance of 40 km?
 
  • #56
DrStupid said:
What makes you think the resulting destructions at ground zero would be similar to a single Chelyabinsk meteor in a distance of 40 km?

Nothing makes me think so. I said no such thing.

I said that nuking this asteroid in space is (a) probably possible even with today's tech, and definitely possible if we'd finance a R&D program for nuclear-tipped asteroid interceptors; and (b) does significantly reduce the effects. The effects will still be severe, but many times less so than if we just let it impact the ground intact.
 
  • #57
This paper, which studies the deflection and fragmentation of a near-Earth asteroid, may be of interest: http://web.gps.caltech.edu/~sue/TJA_LindhurstLabWebsite/ListPublications/Papers_pdf/Seismo_1621.pdf

Note that "fragmentation" here refers to the strategy of breaking up the asteroid so that the majority of its fragments are either too small to pose a threat to Earth or miss Earth completely. Interestingly, the paper claims that a surface burst is not more effective than a "stand-off" burst, which is detonated at a distance from the asteroid.

nikkkom said:
I said that nuking this asteroid in space is (a) probably possible even with today's tech, and definitely possible if we'd finance a R&D program for nuclear-tipped asteroid interceptors;

A short search on google netted me this paper: https://ntrs.nasa.gov/archive/nasa/casi.ntrs.nasa.gov/20150011479.pdf
It discusses the suborbital interception and fragmentation of an asteroid with very short warning times using modern ICBM's. Interception of an asteroid at further distances is probably not possible without a specialized launch vehicle. I don't think ICBM's have enough fuel to escape Earth's orbit and reach their target. We certainly have the technology to create a launch vehicle and weapon system capable of intercepting and deflecting/fragmenting potential threats, we just haven't had the push to do so.
 
  • #58
Drakkith said:
...google netted me this paper:
Lol, not bad... . :wink:

Intended... ?
 
  • #59
OCR said:
Lol, not bad... . :wink:

Intended... ?

Sorry, I'm not sure what you're asking me.
 
  • #60
Drakkith said:
Sorry, I'm not sure what you're asking me.
No worries ... I thought you might have made an intended pun. . :oops:
 
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  • #61
nikkkom said:
Nothing makes me think so. I said no such thing.

You said it in #50:

nikkkom said:
Light flash would be spectacular but won't be intense enough to do harm.
Shock waves would cause widespread window damage and may cause moderate structural damage in some buildings.

That's exactly what happened in Chelyabinsk.

nikkkom said:
and (b) does significantly reduce the effects.

Egain, I don't believe that until I see a corresponding calculation.
 
  • #62
i guess people are not relating to my 'why not radar?' question, because somehow by just bringing this up, is demonstrated a lack of even basic understanding of how astronomical equipment is used for that goal. But yet can anyone please try and explain in simple words, how far away is current technology from being able to detect by radar at least 2 months ahead, an asteroid coming at an angle that optical and infrared means are unable to detect ? Or are optical and infrared means still a better possibility and if so, what improvements are needed to be able to do that in a case such as with 'Oumuamua? i mean, people are talking here about nukes and other very late time to impact options, but why does no one discusses ways to make it an earlier detection case? Is much earlier detection such an impossibility?
 
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  • #63
You need three things to discover an asteroid:

1) it has to be bright enough to be visible
2) it has to be in the field of view

These two sound trivial, but the combination is not. Hubble can see objects with an apparent magnitude of 31.5, about 10 billion times fainter than what we can see with the naked eye. But to do that it has to look at a tiny region, just 1/(30 million) of the sky, for one month. To cover the whole sky that way we would need 30 million Hubble telescopes - that doesn't work.
There are telescopes with larger fields of view and they typically operate with shorter exposure times. They can cover larger regions of the sky, but at a much lower sensitivity.
Radar astronomy is flexible, you can either use a wide beam and a very short range (for Earth orbits?) or a narrow beam and a still quite short range (to track asteroids nearby), but you still have the trade-off other methods have. You don't get a reasonable range at a reasonable field of view to detect new things. You can only track known things, and even then only if they are nearby or huge (e. g. planets).

Hubble should be able to follow Oumuamua well into the outer solar system, but to discover it at this distance Hubble would have had to make images of a very small region of the sky just by accident. Many asteroid detections were the result of these accidents - but you never get a comprehensive list that way.

3) It has to be recognized as asteroid.
Most spots of light that appear in telescope images are stars. If you just have a single image (e.g. from Hubble), you don't recognize asteroids in it. You need multiple images taken at different times. Everything that moves is nearby, everything that does not move notably is far away.

The Large Synoptic Survey Telescope is currently under construction. Once completed in ~2021 it will monitor the whole sky (apart from a small region near Polaris) every few days. It will increase our chance to detect something before it could hit Earth a lot.

Gaia is an interesting case. Its main focus is on objects outside the solar system, in particular mapping about 1 billion stars and other objects. To do that, it scans the whole sky where each spot comes into view typically once per month. Stars will appear at nearly the same spot every time, but near Earth asteroids move a lot during that time - they will appear at random-looking spots during the observation campaign. It will need clever algorithms to associate these spots to orbits of different asteroids. The list of stars can also help other telescopes. If they see spots of light, they can check the Gaia database if these correspond to known stars.
 
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  • #64
mfb said:
1) it has to be bright enough to be visible
2) it has to be in the field of view

Can you expand on objects coming from the direction of the sun, and the ability of existing equipment such as Gaia and possible future equipment, to detect in such a case?
 
  • #65
That is challenging for all telescopes. Most near Earth asteroids should typically be not too close to the Sun during some time in their orbit, for extrasolar asteroids that is not necessarily true (but they are very rare). Gaia is expected to find various asteroids closer to the Sun that were missed in previous surveys. Its scanning procedure includes measurements down to a 45 degree angle with respect to the Sun (source: page 6).

Sentinel was a concept of a telescope in a Venus-like orbit. That way all the potentially dangerous asteroids would have been far away from the Sun as seen by the telescope. Didn't get funded.
 
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  • #66
roineust said:
A reasonably read and educated laymen, would response to a claim that science and technology still have no means to detect a big asteroid collision with earth, by saying that according to what he read and saw in communication channels reliable enough, an object of that size on course to hit earth, should be detected by radio telescopes around the world, in due time. Then comes into our solar system 'Oumuamua, which is detected only on 19 October 2017. Please let me on your thoughts and knowledge regarding this subject.

'Oumuamua (A/2017 U1) was brighter than apparent magnitude +22 only between 2 September 2017 and 13 September 2017. It wasn't an obvious night-sky object by any stretch of the imagination.

'Oumuamua's orbital elements

semimajor axis, a

a = −1.279792859772851 AU

eccentricity, e
e = 1.199512371721525

inclination to ecliptic, i
i = 122.6867065669057°

longitude of the ascending node, Ω
Ω = 24.59910692499587°

argument of the perihelion, ω
ω = 241.7023929688934°

time of perihelion passage, T
T = 2458005.9912606976 JD = 9 September 2017 @ 11:47:24.9 UT

The reduction of Keplerian orbital elements to position and velocity, for a specified time-of-interest, t.
For Hyperbolic Orbits.


mean anomaly, M, at time-of-interest t (for hyperbolic orbits)
M = 0.01720209895 (t−T) √[1/(−a)³]

eccentric anomaly, u, at time-of-interest t (for hyperbolic orbits)

u = 0.0
U = 999.9
while |u−U| > 1e-12:
U = u
f₀ = e sinh(U) − U − M
f₁ = e cosh(U) − 1
f₂ = e sinh(U)
f₃ = e cosh(U)
d₁ = −f₀ / f₁
d₂ = −f₀ / (f₁ + ½ d₁f₂)
d₃ = −f₀ / (f₁ + ½ d₁f₂ + ⅙ d₂² f₃)
u = U + d₃

heliocentric distance, r, at time-of-interest t (for hyperbolic orbits)
r = a (1 − e cosh u)

true anomaly, θ, at time-of-interest t (for hyperbolic orbits)

if M≥0, then
θ = arccos[(e − cosh u) / (e cosh u − 1)]
if M<0, then
θ = −arccos[(e − cosh u)/(e cosh u − 1)]

position in heliocentric ecliptic coordinates, [x, y, z], at time-of-interest t

x'' = r cos θ
y'' = r sin θ

x' = x'' cos ω − y'' sin ω
y' = x'' sin ω + y'' cos ω

x = x' cos Ω − y' cos i sin Ω
y = x' sin Ω + y' cos i cos Ω
z = y' sin i

velocity in heliocentric ecliptic coordinates, [Vx, Vy, Vz], at time-of-interest t (for hyperbolic orbits)

k = 29784.6918325927 m/s

Vx'' = k (a/r) √[1/(−a)] sinh u
Vy'' = −k (a/r) √[(1−e²)/a] cosh u

(Enter a and r in astronomical units. Their dimensions have already been extracted and converted into the constant k.)

Vx' = Vx'' cos ω − Vy'' sin ω
Vy' = Vx'' sin ω + Vy'' cos ω

Vx = Vx' cos Ω − Vy' cos i sin Ω
Vy = Vx' sin Ω + Vy' cos i cos Ω
Vz = Vy' sin iJust to be complete about things, here's...The reduction of Keplerian orbital elements to position and velocity, for a specified time-of-interest, t.
For Elliptical Orbits.


mean anomaly, M, at time-of-interest t (for elliptical orbits)

P = 365.256898326 a¹·⁵
m₀ = (t−T) / P
M = 2π [m₀ − integer(m₀)]

eccentric anomaly, u, at time-of-interest t (for elliptical orbits)

u = M + (e − e³/8 + e⁵/192) sin(M) + (e² − e⁴/6) sin(2M) + (3e³/8 − 27e⁵/128) sin(3M) + (e⁴/3) sin(4M)
U = 999.9
while |u−U| > 1e-12:
U = u
f₀ = U − e sin U − M
f₁ = 1 − e cos U
f₂ = e sin U
f₃ = e cos U
d₁ = −f₀ / f₁
d₂ = −f₀ / (f₁ + ½ d₁f₂)
d₃ = −f₀ / (f₁ + ½ d₁f₂ + ⅙ d₂² f₃)
u = U + d₃

true anomaly, θ, at time-of-interest t (for elliptical orbits)

x'' = a (−e + cos u)
y'' = a √(1−e²) sin u
θ = arctan(y,x)

(arctan is the two-dimensional arctangent function in which y=sin θ and x=cos θ.)

heliocentric distance, r, at time-of-interest t (for elliptical orbits)
r = √[ (x'')² + (y'')² ]

position in heliocentric ecliptic coordinates, [x, y, z], at time-of-interest t

x' = x'' cos ω − y'' sin ω
y' = x'' sin ω + y'' cos ω

x = x' cos Ω − y' cos i sin Ω
y = x' sin Ω + y' cos i cos Ω
z = y' sin i

velocity in heliocentric ecliptic coordinates, [Vx, Vy, Vz], at time-of-interest t (for elliptical orbits)


k = 29784.6918325927 m/s

Vx = −k sin θ / √[a(1−e²)]
Vy = k (e + cos θ) / √[a(1−e²)]

(Enter a in astronomical units. Its dimensions have already been extracted and converted into the constant k.)

Vx' = Vx'' cos ω − Vy'' sin ω
Vy' = Vx'' sin ω + Vy'' cos ω

Vx = Vx' cos Ω − Vy' cos i sin Ω
Vy = Vx' sin Ω + Vy' cos i cos Ω
Vz = Vy' sin i
 
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  • #67
The Barringer impactor (near Winslow, Arizona) was a nickel-iron meteorite and is estimated to have been only 50 meters in diameter. It left a hole 500 feet deep and about 3/4ths of a mile in diameter. Obviously, it did not blow up on entry to the atmosphere. Impact energy was about 10 megatons. Had such a meteorite impacted near a modern metropolitan area, well, the destruction would have been horrendous. Depending on the composition of Oumuamua, had it impacted, it could have been even more devastating, although not an extinction level event.
 
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  • #68
I forgot what I was leading up to. Using that algorithm, you can calculate that 'Oumuamua was 0.16162 AU from Earth at closest approach at 18h UT on 14 October 2017, where its speed relative to Earth was 60.225 km/sec.

On 14 October 2017, Earth's orbital elements were:

a = 1.000000394110650 AU
e = 0.0166942736943211
i = 0.0024086539688206°
Ω = 174.0573387205077°
ω = 288.8352443931458°
T = 2458122.078193375841 JD
 
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  • #69
Dr_Zinj said:
The Barringer impactor (near Winslow, Arizona) was a nickel-iron meteorite and is estimated to have been only 50 meters in diameter. It left a hole 500 feet deep and about 3/4ths of a mile in diameter. Obviously, it did not blow up on entry to the atmosphere. Impact energy was about 10 megatons. Had such a meteorite impacted near a modern metropolitan area, well, the destruction would have been horrendous. Depending on the composition of Oumuamua, had it impacted, it could have been even more devastating, although not an extinction level event.
The speed of the object is also important. A 30 meter in diameter nickel/iron meteor (8.391 g/cm3) approaching Earth at an angle of 45° will explode in the atmosphere if its speed is in excess of 40 km/s, releasing 9.49 x 1016 Joules of energy (22.7 MegaTons TNT). But that exact same meteorite will impact with the Earth's surface if its speed is 20 km/s or less. At 20 km/s a 30 meter in diameter nickel/iron meteorite would create a final crater about 890 meters (just over half a mile) in diameter and release 6.96 x 1015 Joules of energy (1.66 MegaTons TNT) upon striking the ground.

Oumuamua's speed as it flew past Earth was ~47 km/s. They also suspect that Oumuamua is made of metal rich rock because of its elongated shape and the fact that it did not display a cometary tail as it made its closest approach to the sun. Assuming Oumuamua has the density of iron (7.874 g/cm3), traveling at 47 km/s and impacting Earth at an angle of 45°, this would be the effect:
  • The meteorite begins to break up at an altitude of 31,300 meters (103,000 feet).
  • The meteorite strikes the surface at a velocity of 28.8 km/s. The impact energy is 3.52 x 1017 Joules of energy (8.41 MegaTons TNT). The broken projectile fragments strike the ground in an ellipse of 446 meters by 315 meters.
  • The initial crater is 2.03 km (1.26 miles) in diameter and 716 meters (2,350 feet) deep. The final crater will be 2.53 km (1.57 miles) and 539 meters (1,770 feet) deep. Roughly half of the melt remains in the crater.
  • The seismic effects at a distance of 100 km from the impact would be approximately a magnitude 5.9 that would arrive about 20 seconds after impact.
  • Ejecta would begin arriving 100 km from the impact site 2.4 minutes after impact and be 1.53 cm (0.604 inches) in diameter on average.
  • The air blast would arrive 100 km from the impact site 5.05 minutes after impact. The peak overpressure would be 2,870 Pa (0.408 psi) with a maximum wind speed of 6.69 m/s (15 mph) and be accompanied by a 69 dB blast (the sound of heavy traffic).
If such an impact were to occur in downtown Los Angeles, there would be 1,251,290 estimated fatalities and 1,845,600 estimated injured. Everything from San Fernando to Anaheim, and from Santa Monica to Pomona would be destroyed. Anyone within 16.5 miles (859 square miles) of the impact would suffer third degree burns, or worse.
 
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  • #70
Reducing the speed by a factor 2 (assuming you used 40 km/s) shouldn’t reduce the energy by a factor of more than 10 unless you are not considering the full energy.
 
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