Near-Earth Asteroids: Charting Celestial Threats
In 2011, NASA's NEOWISE infrared mission revised the estimated number of mid-sized near-Earth objects (140 m to 1 km) downward, from about 35,000 to about 19,500 objects. Since then, surveys have continued: today, more than 41,000 near-Earth objects are known, across all sizes.
In this inner solar system diagram, the green dots represent planets.
Object sizes are not to scale.
Image source: NASA/JPL-Caltech (new window)
Scientific summary
This Astronoo article presents an in-depth analysis of the monitoring of near-Earth asteroids, those celestial bodies whose orbits cross that of Earth. Drawing on data from detection programs such as Pan-STARRS, the Catalina Sky Survey, ATLAS, and, since 2025, the Vera C. Rubin Observatory, the study details the methods of detection, dynamic mapping, and risk assessment. The chaotic dynamics of these objects, influenced by gravitational perturbations and the Yarkovsky effect, make their tracking complex, as illustrated by the case of asteroid 2024 YR4. The article highlights the importance of databases like JPL's SBDB and the future infrared space mission NEO Surveyor (launch planned for late 2027) in filling observational blind spots, particularly near the Sun. Precise and continuous sky charting is presented as a crucial issue for planetary security.
Why is charting near-Earth asteroids so crucial for our safety?
This article is dedicated to charting near-Earth asteroids, celestial objects that orbit in our planetary neighborhood. But why is such vigilance essential? The answer lies in the potential threat these bodies pose to our planet. With over 41,000 near-Earth objects cataloged to date and a much larger number still undetected—tens of millions of objects smaller than 30 meters are estimated to remain undiscovered—precise knowledge of their trajectories is our primary defense against a devastating impact. A 140-meter asteroid, classified as "potentially hazardous," could release energy far exceeding that of a conventional nuclear explosion. Dynamic charting of these objects is not just a simple list of positions; it incorporates complex physical models, parallax corrections, and orbital integrations to anticipate their movements over decades or even centuries. This article explores the tools, challenges, and limits of this surveillance, showing that each new observation refines our understanding of the impact risk and strengthens our ability to respond to the unexpected.
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Intruders in our orbital neighborhood
Definition and stakes of near-Earth objects
Near-Earth Asteroids (NEAs) are celestial bodies whose orbits approach that of Earth, with a perihelion of less than 1.3 astronomical units. Their known number now exceeds 41,000, a total that grows each year as surveys become more sensitive. Among them, Potentially Hazardous Asteroids (PHAs) are those whose minimum orbital intersection distance with Earth (MOID) is less than 0.05 AU, and whose estimated diameter is greater than 140 m: there are about 2,550 of them as of late August 2026, according to the JPL database. An impact with such an object could release energy on the order of several hundred megatons of TNT, enough to devastate an entire region.
How are near-Earth objects detected?
Detection programs and how they work
Detection programs such as Pan-STARRS, the Catalina Sky Survey, ATLAS (Asteroid Terrestrial-impact Last Alert System), and, since it began operations in 2025, the Vera C. Rubin Observatory in Chile, continuously scan the celestial vault to detect objects moving rapidly from a geocentric perspective. The analysis relies on comparing successive images using motion detection algorithms. Rubin, with its 8.4-meter telescope and 3.2-gigapixel camera, has already identified several thousand new Solar System objects in its first months of operation and is expected to significantly accelerate the census of mid-sized near-Earth objects. Once identified, a near-Earth object is observed over several days to refine its orbit using Kepler's equations and gravitational perturbations.
Building the celestial map of near-Earth objects
Methods and tools for dynamic charting
Charting near-Earth objects involves projecting their real-time position onto the celestial sphere in equatorial coordinates (right ascension \(\alpha\), declination \(\delta\)). Each point corresponds to the apparent position of a given asteroid at time \(t\), corrected for parallax and atmospheric refraction effects. The chart evolves continuously with Earth's rotation and the heliocentric motion of the objects.
Major near-Earth objects close to Earth
Monitoring recent and upcoming passages
The detection of near-Earth asteroids has intensified significantly in recent years: programs like the Catalina Sky Survey or the ATLAS system discover new objects almost every night, and the Vera C. Rubin Observatory has been reinforcing this pace since 2025. As of late August 2026, the JPL cataloged about 2,550 potentially hazardous asteroids, and nearly 870 near-Earth objects larger than one kilometer in diameter are now cataloged, representing about 90% of the estimated population for that size class. The table below presents some documented close passages, whose parameters sometimes change from one observation to the next; for up-to-date data, the CNEOS close approach database (new window) remains the reference to consult.
| Asteroid name | Passage date | Distance (LD) | Estimated diameter (m) |
|---|---|---|---|
| 2026 EG1 | 12 March 2026 | ~0.83 | 10 – 22 |
| 2024 YR4 | 17 December 2028 (flyby, no impact) | > 1 | ~60 |
| 99942 Apophis | 13 April 2029 | ~0.083 | 340 – 450 |
N.B. :
LD = lunar distance = 384,400 km. A distance of 0.05 LD corresponds to about 19,220 km, comparable to the altitude of geostationary satellites. Diameters of recently discovered small objects remain estimates derived from their absolute magnitude and an assumed albedo; they are subject to revision upon further observations (radar or infrared).
The fundamental tool is the JPL SBDB (Small Body Database) (new window). From the orbital elements: the semi-major axis a (orbit size), eccentricity e (orbit shape), inclination i (orientation relative to the ecliptic plane), longitude of the ascending node Ω, argument of perihelion ω, and mean anomaly M (object's position on its orbit), it is possible to calculate the position (x, y, z) of an object in a barycentric reference frame (origin at the Solar System's center of mass) and project it into equatorial coordinates (right ascension and declination) to locate the asteroid in our night sky.
Case study: 2024 YR4, a lesson in dynamic charting
How an apparent threat dissipated under the weight of observations
Asteroid 2024 YR4, discovered on 27 December 2024 by the ATLAS telescope in Chile, perfectly illustrates how a dynamic map is built and corrected over time with measurements. On 31 December 2024, the object was placed on NASA's automated Sentry monitoring list, as its impact probability with Earth on 22 December 2032 had exceeded the 1% notification threshold. Estimates would later temporarily climb to about 3%, a record for an object of this size (about 60 meters in diameter), placing 2024 YR4 at the top of the Torino Scale for several weeks. A collision scenario with the Moon was even briefly considered.
Additional observations, notably with the James Webb Space Telescope, significantly refined the object's orbit: the uncertainty corridor narrowed until it completely excluded Earth from the possible trajectory in 2032, reducing the impact risk to a probability on the order of 0.001%. The risk of a lunar impact was also ruled out, as the object will pass more than 20,000 km from the Moon. This episode concretely demonstrates the very principle of dynamic charting: each new astrometric measurement reduces the cloud of possible trajectories (Monte Carlo method) until the uncertainty becomes negligible. 2024 YR4 will pass near Earth again on 17 December 2028, providing another opportunity to observe it without any concern.
From surveillance to action: the beginnings of planetary defense
Testing our ability to deflect an asteroid
Charting is not enough: we must also be able to act if a dangerous object were ever detected. NASA's DART (Double Asteroid Redirection Test) mission demonstrated in September 2022 that a kinetic impactor could alter the orbital period of a small body, by striking the satellite Dimorphos of the binary asteroid Didymos. The exceptional flyby of Apophis in April 2029 will be an opportunity to go further: the European Space Agency is preparing the Ramses mission (Rapid Apophis Mission for Space Safety), designed to rendezvous with the asteroid before its closest approach to Earth to observe in real time the effects of Earth's tidal forces on its internal structure, rotation, and surface. This type of characterization mission complements detection programs: knowing where a near-Earth object is does not reveal its internal cohesion, a decisive parameter for designing an effective deflection strategy.
Limits of current surveillance
Missing objects and blind spots
Objects smaller than 50 m still often evade detection, like the Chelyabinsk meteor (2013), which was about 20 m in size. Their low absolute magnitude (\(H>25\)) makes them difficult to detect except at very close approach. Furthermore, regions near the Sun (near zero elongation) remain unobservable from the ground, a limitation that only space-based infrared observation can overcome. NASA's NEO Surveyor mission, an infrared telescope dedicated to this task with launch planned no earlier than September 2027 from Cape Canaveral, is precisely designed to fill this blind spot by observing from the Sun-Earth L1 Lagrange point; it aims to discover two-thirds of the yet-undiscovered near-Earth objects larger than 140 m by the end of its five-year nominal mission.
Why a dynamic map is essential
Anticipating the chaotic dynamics of near-Earth objects
The dynamics of near-Earth objects are chaotic in the long term. Small gravitational perturbations from the giant planets can significantly alter their orbits (including the Yarkovsky effect). A dynamic map allows for the recalculation of impact probabilities with each new astrometric measurement, using the automated Sentry (NASA/JPL) and Aegis (ESA) systems. Nominal orbits and trajectory clouds (Monte Carlo integration) are then compared to Earth's future position, as demonstrated by the case of 2024 YR4.
Anticipating the unexpected
Vigilance as the key to planetary security
Monitoring near-Earth objects is one of the few scientific fields where every day counts for planetary security. Building an accurate and dynamic map of the sky is a physical, mathematical, and technological necessity. It is not the size of the object that makes it dangerous, but our ability to see it coming in time. Charting the invisible is ensuring our vigilance in a perpetually moving cosmos.
References
- CNEOS - Center for Near Earth Object Studies, NASA/JPL (new window)
- CNEOS - Close Approach Data Table (real-time close approaches) (new window)
- JPL Small-Body Database Lookup (SBDB) (new window)
- NASA/JPL (2011). NASA Space Telescope Finds Fewer Asteroids Near Earth (new window)
- NASA Science - NEO Surveyor Mission (new window)
- NASA Science - Apophis Facts (new window)
- ESA - Presentation of the Ramses mission to asteroid Apophis (new window)
- Vera C. Rubin Observatory (new window)
FAQ: Everything you need to know about near-Earth asteroids
What is a near-Earth asteroid?
A near-Earth asteroid is a celestial body whose orbit around the Sun brings it close to Earth's orbit. These objects are closely monitored because they represent a potential impact threat. Their size can range from a few meters to several kilometers for the largest ones, but it is the intermediate-sized ones (over 140 m) that are classified as "potentially hazardous" when their orbit approaches sufficiently close to Earth's.
How do scientists detect near-Earth asteroids?
Detection relies on systematic surveys of the night sky, such as Pan-STARRS, the Catalina Sky Survey, ATLAS, and, since 2025, the Vera C. Rubin Observatory. These programs use wide-field telescopes to take successive images of the same region of the sky. A moving asteroid appears as a point that shifts between images. Computer algorithms then compare these images to identify moving objects, which are subsequently confirmed by follow-up observations and reported to the Minor Planet Center (MPC).
What is the difference between a near-Earth asteroid and a PHA?
Not all near-Earth objects are considered hazardous. The acronym PHA (Potentially Hazardous Asteroid) refers to a subset whose orbit approaches within 0.05 astronomical units (about 7.5 million km) of Earth and whose estimated diameter exceeds 140 meters. These criteria define an object large enough to cause regional damage in the event of an impact.
Can near-Earth asteroids deviate from their trajectory?
Yes, their trajectory is influenced by several factors: gravitational perturbations from planets (especially Jupiter), the Yarkovsky effect (a thrust due to infrared thermal emission), close encounters with Earth itself (such as during Apophis's flyby in 2029), and collisions with other small bodies. These effects make their dynamics complex and chaotic over the long term, justifying continuous monitoring and regular updates of their orbits, as shown by the case of 2024 YR4.
What would happen if a large asteroid were detected on a collision course?
If an impact were confirmed, several deflection strategies could be considered. NASA's DART (Double Asteroid Redirection Test) mission demonstrated in 2022 that it is possible to alter an asteroid's orbit via kinetic impact. Other methods, such as surface nuclear explosion or the use of gravitational tractors, are also being studied, while the future European Ramses mission aims to deepen our knowledge of the internal structure of such objects. The goal is to have a range of responses tailored to the size and available warning time.
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