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6 - Planetary Defence

Published online by Cambridge University Press:  06 April 2023

Michael Byers
Affiliation:
University of British Columbia, Vancouver
Aaron Boley
Affiliation:
University of British Columbia, Vancouver

Summary

Some 66 billion years ago, a cataclysmic collision between the Earth and an asteroid ten to 15 kilometres in diameter caused the extinction of the non-avian dinosaurs. In 1908, an asteroid 50 to 70 metres in diameter levelled over 2,000 square kilometres of forest in Siberia, while in 2013 an asteroid 19 metres in diameter produced a shockwave over Chelyabinsk, Russia, sending over a thousand people to the hospital. The field of ‘planetary defence’ involves the detection, characterisation, risk assessment and, if necessary, deflection of asteroids and comets that have the potential to strike Earth. Yet there has been a lack of high-level diplomacy on this issue. In particular, the low probability of a major Earth impact happening in our lifetime makes planetary defence a low priority for political leaders, despite the existential consequences of impacts and their eventual certainty of occurring. There is also a shortage of widely agreed international law, including on the potential use of nuclear explosive devices for deflecting asteroids. Most importantly, there is a lack of agreement on who is responsible for vetting the science, assessing the risks and making decisions if Earth were faced with an actual impact threat. Is it the United Nations Security Council that decides? What if a Security Council decision is blocked by one of its veto-holding permanent members? Would a state that acted unilaterally be excused any illegality because of the necessity of its actions, according to the international law on ‘state responsibility’?

Information

Figure 0

Figure 6.1 Lake Manicouagan was created by a five-kilometre-diameter asteroid approximately 214 million years ago. Located in Quebec, Canada, it is approximately 100 kilometres across, with the reservoir ring being approximately 70 kilometres across.

This image was taken by the European Space Agency’s Sentinel-2 satellite.
Figure 1

Figure 6.2 Alan B Chamberlin, ‘Fireball and bolide data: Fireballs reported by US government sensors (1988-Apr-15 to 2022-Apr-21)’, (April 2022), Center for Near Earth Object Studies, online: cneos.jpl.nasa.gov/fireballs. A fireball is a very bright meteor, reaching a brightness comparable to that of the planet Venus, while a bolide is a bright fireball that explodes.

Figure 2

Figure 6.3 Near-Earth asteroid discovery plot, cumulative over time. The upward slope is due to the completeness of catalogued objects still being low for smaller bodies.

Figure 3

Figure 6.4

Figure 4

Figure 6.4

Figure 5

Figure 6.5 B-plane showing simulation results of different deflection scenarios for the hypothetical impactor 2019 PDC. The B-plane co-ordinates are in units of Earth radii. The solid circle represents the cross section of Earth, and the dashed line is Earth’s effective cross section when including gravitational focusing. Each point represents where the hypothetical 2019 PDC passed through the B-plane – if the point is within the dashed circle, then the impactor would have hit Earth. The central point represents no deflection attempt. Starting from the uppermost point moving downward, the deflections used are Δv= –10, –8, –6, –4, –2, 0, 2, 4, 6, 8, 10 millimetres per second. Each Δv was applied 7.7 years before the potential impact, with the results roughly consistent with the approximate relation in the text.

Figure produced in collaboration with Edmond Ng.
Figure 6

Figure 6.6 Comet 67P/Churyumov–Gerasimenko, in a mosaic of four photographs from ESA’s Rosetta spacecraft. The comet, which appears to be two icy bodies weakly held together, is about 4.3 by 4.1 kilometres at its longest and widest dimensions. One of Rosetta’s many discoveries was that the isotopic signature of the water on the comet is quite different from that on Earth, which suggests that Earth’s oceans did not come from comets like 67P.47

Figure 7

Figure 6.7 The area of expected damage due to an airburst from a 60-metre asteroid, arranged by increasing severity. The region of ‘severe’ damage is enclosed by the region of ‘serious’ damage, and so forth. Regions need not be circular, and they depend on several factors. The term ‘overpressure’ refers to the pressure, in pounds per square inch (psi), in excess of the ambient pressure prior to the arrival of the blast wave. From Barbara Jennings, ‘Day 5 at Risk Critical Infrastructure Effects’ (paper delivered at the 6th Planetary Defense Conference, College Park, Maryland, 29 April–3 May 2019), NASA, online: cneos.jpl.nasa.gov/pd/cs/pdc19/pdc19_briefing5c.pdf.

Figure 8

Figure 6.8 Keyhole map for the 2029 flyby of Apophis. The x axis shows the change in the ζ co-ordinate on the B-plane, relative to the location of the nominal orbit. The y axis shows the closest to Earth that Apophis would come after the 2029 encounter for the next 100 years upon passing through the noted location on the B-plane. The downward spikes represent the orbital structure. Spikes that get within about 10 per cent of Earth’s radius will collide with Earth in that 100-year timeframe, depending on the amount of gravitational focusing (which draws the asteroid even closer to the planet). The broad downward dip with multiple spikes is an example of a ‘keyhole complex’, where there is the potential for multiple keyholes to reside. To a very high degree of certainty, the orbit of Apophis will not pass through a keyhole in 2029.

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  • Planetary Defence
  • Michael Byers, University of British Columbia, Vancouver, Aaron Boley, University of British Columbia, Vancouver
  • Book: Who Owns Outer Space?
  • Online publication: 06 April 2023
  • Chapter DOI: https://doi.org/10.1017/9781108597135.007
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  • Planetary Defence
  • Michael Byers, University of British Columbia, Vancouver, Aaron Boley, University of British Columbia, Vancouver
  • Book: Who Owns Outer Space?
  • Online publication: 06 April 2023
  • Chapter DOI: https://doi.org/10.1017/9781108597135.007
Available formats
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  • Planetary Defence
  • Michael Byers, University of British Columbia, Vancouver, Aaron Boley, University of British Columbia, Vancouver
  • Book: Who Owns Outer Space?
  • Online publication: 06 April 2023
  • Chapter DOI: https://doi.org/10.1017/9781108597135.007
Available formats
×