Q5: How have deliberate satellite intercepts affected the space debris environment?
On 11 January 2007, China conducted an anti-satellite test, intercepting their Fengyun-1C satellite with a surface-launched medium-range missile. The intercept occurred at an altitude of 862 km on a near-polar orbit, adding more than 3300 trackable objects to the US Space Surveillance Network catalogue, increasing its size by 25% in just one incident.
This was by far the worst break-up event in space history − some 3.5 times worse than the worst previous event. Owing to the high altitude of the collision event and the low ambient air density, the fragments will have long orbital lifetimes.
Satellites in Sun-synchronous orbits at around 800 km altitude still today experience an increased number of close conjunctions with debris objects. Roughly 30% of such events are caused by Fengyun-1C fragments.
On 21 February 2008, the United States intercepted their USA-193 satellite with a modified SM-3 missile. At the time of engagement, the target spacecraft was at an altitude of 249 km, on a near-circular orbit at 58.5º inclination. Owing to the low altitude, and the correspondingly high air drag, most of the generated fragments harmlessly reentered within one orbit.
Only 170 fragments entered the US catalogue within one month, and none were left by the end of 2008. In the short-term, however, the risk of penetration of the shields of the ISS’s crew modules by USA-193 fragments larger than 1 cm increased by about 30%.
Q6: Why does Earth's atmosphere have a positive effect on space debris?
Earth’s atmosphere causes air drag that extracts orbital energy, leading to a reduction in the orbital altitude and final reentry of a space object. Upper layers of the atmosphere are supported by lower layers, which are compressed under the weight of the air column above them. The air density increases, and hence the increase in drag due to air with decreasing altitude is progressive.
Changes in air density at a given orbital altitude are mainly driven by the Sun, which varies its activity in an 11-year cycle. Thus, every 11 years, lower parts of the atmosphere are heated and expand towards higher altitudes, where the air density increases, causing higher air drag on objects in space. As a consequence, space debris is periodically cleaned from the lower orbital regions, but these are subsequently replaced by debris objects descending from higher orbits.
After sufficient exposure to air drag, the object’s orbit decays, and the object enters Earth’s denser atmosphere, where the air drag converts orbital energy into heat. This heating process is normally sufficient to destroy any object. Approximately 20-40% of the mass of larger-size spacecraft or rocket bodies, or parts made of particularly high-melting steel or titanium alloys, may survive the reentry.
Q7: How many space debris objects are currently in orbit?
See “Space debris by the numbers” for the most recently updated figures from ESA’s Space Debris Office.
Any of these objects can cause harm to an operational spacecraft. For example, a collision with a 10-cm object would cause the catastrophic fragmentation of a typical satellite, a 1-cm object will most likely disable a spacecraft and penetrate the ISS shields, and a 1-mm object could destroy subsystems on a satellite.
Scientists generally agree that, for typical satellites, a collision having an energy-to-mass ratio exceeding 40 J/g will be catastrophic.
Q8: What is the Kessler Syndrome, and how can it be avoided?
At present, the majority of all space debris that can cause a catastrophic collision (i.e. larger than 10 cm) results from the more than 500 on-orbit fragmentation events that have happened in the course of spaceflight history.
However, simulations of the long-term evolution of the space debris environment indicate that within a few decades, generated collision fragments will start to dominate, at least in orbits around 800–1400 km altitude. This will be true even if all launch activities were to be discontinued now, which is an extremely unlikely development.
In the most probable scenario, fragments will initially collide with large, intact objects. Then, the resulting collision fragments will start to collide with other large, intact objects, and so on, and ultimately collision fragments will collide with collision fragments until all remaining objects are reduced to subcritical sizes.
This run-away, self-sustained, cascading collision process is most likely to commence at altitudes having high debris population densities and insufficient cleansing by air drag, which would be around 900 km and 1400 km.
These long-term simulations of the environment show how the extrapolation of current spaceflight trends in terms of:
adherence to space debris mitigation guidelines, and
the frequency of on-orbit breakups
will result in the exponential growth of the population of objects, with consequences for daily spacecraft operations.
The successful ‘passivation’ of all spacecraft, which would limit on-orbit breakups, and the widespread, i.e. more than 90%, adoption of effective disposal strategies at the end of missions would contribute to containing the population growth.
For the situation where large constellations of smaller satellites are present in low Earth orbit (LEO; typically, up to about 1000 km altitude), the IADC has conducted studies across all 13 space agency members. These have shown that a potentially stable evolution of the orbital environment is achieved only when the disposal rate is at least 95%, notably higher than the 90% needed for larger, ‘traditional’ satellites.
This runaway scenario is the ‘Kessler syndrome’ and was first postulated by NASA scientist Don Kessler in 1978.