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Dimorphos

Dimorphos is a small moonlet, approximately 160 meters (525 feet) in , that orbits the larger near-Earth Didymos every 11 hours and 23 minutes, forming a system approximately 1.2 kilometers (0.75 miles) across. Discovered through radar observations at the on November 23, 2003, Dimorphos was selected as the target for 's () mission due to its accessibility and the opportunity to measure changes in its orbit without posing any risk to . The spacecraft, launched in November 2021, intentionally collided with Dimorphos on September 26, 2022, at a speed of about 6.6 kilometers per second (4.1 miles per second), marking the first demonstration of the kinetic impact technique for planetary defense. This impact shortened Dimorphos's around Didymos by 33 minutes and 15 seconds—from its pre-impact duration of 11 hours and 55 minutes to approximately 11 hours and 22 minutes (as of March 2024)—exceeding the mission's success criteria by more than 25 times and confirming the method's effectiveness in altering an asteroid's trajectory. The collision ejected over a million kilograms of material into space, creating a comet-like tail and a large estimated at 50 meters (164 feet) wide, with boulders and debris observed drifting away via telescopes like Hubble. Spectroscopic observations indicate that Dimorphos shares a similar with Didymos, classified as an rich in silicates and metals, akin to meteorites, though pre-impact data suggested a boulder-strewn surface lacking fine . The impact changed the moonlet's shape from an oblate to a triaxial , with approximate dimensions of 177 m × 174 m × 116 m, and ongoing analyses from ground-based telescopes and the ESA's mission, launched in October 2024 and set to arrive in 2026, continue to refine understanding of its internal structure and the ejecta dynamics.

Discovery and nomenclature

Discovery

The binary nature of the near-Earth asteroid (65803) Didymos, serving as the primary body in the system, was first indicated through photometric observations conducted in November 2003 at the Ondřejov Observatory in the by Petr Pravec and Petr Kušnirák. Lightcurve analysis revealed periodic brightness variations consistent with mutual eclipses and occultations caused by a small companion orbiting the primary. These initial photometric findings were confirmed later that same month through radar observations using the by Jean-Luc Margot and collaborators, which directly imaged the binary configuration and resolved the . The provided the first direct of the companion's existence and enabled the estimation of its orbital parameters, including a semi-major axis of approximately 1.18 km. Detection proved difficult owing to the satellite's small size and low , which rendered it faint compared to Didymos and resulted in subtle lightcurve perturbations that demanded precise, extended observation campaigns to distinguish from rotational effects alone.

Naming

Upon its in 2003, the satellite of the asteroid was provisionally designated S/2003 (65803) 1, following the standard nomenclature for natural satellites of minor planets established by the (IAU). This designation reflected the year of observation and the parent body's number in the catalog. Informally, it was also referred to as Didymos I or Didymoon during early studies. The official name "Dimorphos" was approved by the IAU's for Small Bodies (WGSBN) on 23 June 2020, in recognition of its role as the target of NASA's (DART) and ESA's missions. The name was proposed by Kleomenis Tsiganis, a planetary scientist at and a member of the DART science team. Derived from the Greek word dimorphos, meaning "having two forms," it alludes to the satellite's anticipated change in orbital characteristics before and after the planned kinetic impact by DART in 2022. This naming complements the parent asteroid's designation as Didymos, from for "twin," which was chosen to highlight the nature of the system discovered in 1996. Together, the names emphasize the duality of the pair, both in their physical companionship and the transformative objectives of the planetary defense missions targeting them.

Physical characteristics

Size and shape

Prior to the DART impact, Dimorphos was modeled as an oblate with principal axes measuring approximately 177 m × 174 m × 133 m, corresponding to a volume-equivalent of about 160 m. These dimensions were derived from ground-based observations and lightcurve analysis conducted in the years leading up to the mission, revealing a compact, slightly flattened wider than it was tall. The irregular, non-spherical form suggested a rubble-pile structure, consistent with its low overall density and the gravitational aggregation of debris, though the surface appeared relatively smooth compared to more rugged small asteroids. Following the DART impact in September 2022, subsequent observations refined the shape model, indicating a subtle reshaping of Dimorphos into a more triaxial ellipsoid, often described as oblong or watermelon-like, with elongation along one axis. Updated photometric and radar data from 2023 and 2024, including analysis from the Hera mission planning, showed minimal change in overall volume, with a post-impact volume-equivalent diameter of approximately 160 m and negligible reduction (<0.01%) due to ejecta loss (~0.02% of mass); the shape change results from momentum transfer and internal reconfiguration rather than significant erosion. This slight alteration preserved the asteroid's compact scale while enhancing its elongated profile, highlighting the impact's role in redistributing surface material without substantially altering bulk dimensions. Dimorphos's pre- and post-impact morphology aligns with that of other small near-Earth asteroids, such as those in the 100–200 m range, which often exhibit elongated, rubble-pile forms resulting from rotational disruption and reaccumulation around a larger parent body like Didymos. Unlike more monolithic small bodies, its structure underscores the prevalence of loosely bound aggregates in this size class, where tidal and rotational forces maintain irregular yet stable shapes.

Surface features

The surface of Dimorphos is characterized by a predominantly smooth, boulder-strewn terrain with a scarcity of large craters, as documented through high-resolution imagery captured by the DART spacecraft's DRACO camera and the LICIACube CubeSat during the mission's approach and impact in September 2022. This topography suggests a relatively young surface, possibly resurfaced by ongoing processes related to its binary system dynamics, with boulders ranging from a few meters to over 6 meters in diameter dominating the landscape and indicating a rubble-pile composition. Crater size-frequency analysis indicates Dimorphos's surface age is approximately 300,000 years, consistent with its formation from Didymos debris (as of 2024). Notable among these features is an equatorial ridge, which may have formed through rotational instabilities or material accretion during Dimorphos's origin from the parent body Didymos approximately 300,000 years ago. Small impact craters, typically 10-20 meters in diameter, are sparsely distributed, with at least 12 identified in pre-impact images, reflecting limited exposure to major collisional events. The overlying regolith layer is estimated to be 1-10 meters thick, based on analyses of boulder tracks and surface mobility, supporting the interpretation of Dimorphos as a loosely aggregated body with minimal internal cohesion. Following the kinetic impact, significant alterations to the surface were observed, including the generation of a massive plume that extended tens of thousands of kilometers and redistributed material across the . At the impact site, located between two prominent boulders (Atabaque and Bodhran), a approximately 40-60 meters wide formed, accompanied by localized resurfacing due to the mobilization and redeposition of and boulders. These changes were inferred from variations, analyses, and imaging, with ground-based and observations from 2022 to 2024—such as those from Hubble and ESO facilities—revealing ongoing dispersal and subtle shape modifications consistent with global deformation. Approximately 37 large boulders (up to ~7 meters across) were observed ejected at speeds up to 52 meters per second, with additional smaller , further altering the surface texture without evidence of deep excavation. Dimorphos exhibits no signs of prominent geological activity, such as cryovolcanism or tectonic resurfacing, aligning with its structure as a low-strength, loose held together primarily by and weak inter-particle forces. This passive surface evolution underscores the asteroid's recent formation and the dominant role of external impacts and tidal interactions in shaping its .

Composition and density

Spectroscopic observations of Dimorphos in the visible to near-infrared (0.55–2.5 μm) indicate a surface consistent with L/LL ordinary chondrites, dominated by such as and . These spectra reveal absorption features around 1 μm and 2 μm attributable to the iron-bearing silicates in these analogs, with no strong evidence for significant hydrated minerals or organics on the surface. The reflectance properties align closely with those of the primary asteroid Didymos, suggesting a shared compositional . Post-impact analyses constrain the of Dimorphos to lower than ~2.4 /cm³ (range 1.5–2.4 /cm³), derived from orbital dynamics, volume measurements, and modeling. This low implies a highly porous internal structure, characteristic of a rubble-pile with macroporosity around 34–38%, indicating substantial void (20–40%) within loosely aggregated rocky material. The boulder population on the surface, modeled as having grain densities of 3.2–3.6 /cm³, further supports this porous framework, with limited cohesive strength (less than a few pascals). The estimated mass of Dimorphos is about 5 × 10⁹ kg, calculated from its and dimensions inferred via and lightcurve analysis prior to the impact. This value aligns with perturbations in the system's orbital parameters and post-impact ejecta modeling. Formation models propose that Dimorphos originated as a fragment of Didymos through rotational mass shedding, where rapid spin-up ejected that reaccumulated into the moonlet, consistent with its low metal content and primitive silicate-rich composition indicative of an early solar system . This process involved the loss of a small (~1%) of Didymos's , forming Dimorphos in its current orbit without significant capture from external . The rubble-pile structure and spectral similarity reinforce this evolution scenario over alternative captured-body hypotheses.

Orbital and rotational properties

Orbit around Didymos

Dimorphos orbits its , Didymos, in a synchronous, near-circular path characterized by a semi-major axis of 1.19 ± 0.03 km and an of approximately 0.04. This configuration results in an of 11.9217 ± 0.0002 hours, during which Dimorphos completes one full revolution around Didymos. The lies nearly in the equatorial plane of Didymos, promoting long-term stability through interactions that maintain the secondary's position relative to the primary. The synchronous nature of the means Dimorphos maintains the same face toward Didymos throughout its cycle, a state achieved via in the . This locking contributes to the overall dynamics of the Didymos-Dimorphos pair, where the mutual of 11.92 hours contrasts with Didymos's faster of about 2.26 hours, influencing the system's photometric variability and gravitational interactions. The slight introduces minor variations in distance, but the remains stable without significant perturbations prior to external intervention. Following the mission's kinetic impact on September 26, 2022, the of Dimorphos was shortened by 33.25 ± 0.025 minutes as of 2024 measurements from ground-based lightcurve and observations, reducing the period to approximately 11 hours 22 minutes. Recent 2025 studies indicate an additional ~30-second shortening due to ongoing system evolution toward , for a total change of approximately 33 minutes 45 seconds as of October 2025. This alteration also reduced the semi-major axis to 1.144 ± 0.070 and initially induced a post-impact of about 0.028 ± 0.016, which decayed to near zero within ~70 days, though the retained its overall synchronous and stable characteristics.

Rotation

Dimorphos rotates with a period synchronous to its orbital period around Didymos (11.92 hours pre-impact), as expected from in the , confirmed by pre-impact lightcurve analysis of mutual events observed between 2003 and 2021. This synchronization indicates , where the same hemisphere of Dimorphos consistently faces Didymos throughout its orbit. The of Dimorphos is closely aligned with the vector of the , exhibiting a small obliquity that supports stable . The position is at 320.6° and −78.6°, corresponding to a inclination of 168.6° relative to the plane, or an effective tilt of approximately 11° from alignment with the pole. Pre-impact observations and dynamical models reveal no significant tumbling or non-principal , consistent with the equilibrium expected from interactions in a mature system. The stability arises from the close proximity and mutual gravitational influence between Didymos and Dimorphos, which dampen any deviations from synchronous over time. Following the impact in September 2022, numerical simulations predict a minor excitation of Dimorphos's spin state due to transfer from the collision and , potentially introducing non-principal axis or tumbling (with roll up to 45°, pitch up to 20°, yaw up to 25°) while maintaining an average synchronous ; however, such depends on post-impact ratios and may not occur at estimated values. Ground-based lightcurve observations post-impact, including 2024-2025 data, confirm no drastic change beyond the orbital alteration, with overall rotational stability observed despite potential minor perturbations from reshaping.

Exploration and scientific study

Ground-based and telescopic observations

Ground-based and telescopic observations of Dimorphos before the mission focused on techniques to infer its physical and orbital properties within the Didymos . These efforts, spanning imaging, photometry, and , provided essential constraints on Dimorphos's , , , and , though limited by the moonlet's faintness and small relative to Didymos. Radar observations played a key role in resolving the binary structure and estimating shapes. The captured the first images of the system on November 23–24, 2003, using delay-Doppler imaging at 12.6 cm wavelength, which confirmed Dimorphos's presence by detecting separate echoes from the primary and secondary components during close approach. These data yielded an initial estimate of Dimorphos's at approximately 160 m and revealed its orbital motion around Didymos. Photometric lightcurve campaigns over multiple apparitions further characterized Dimorphos's and , including refinements from observations in and later. Observations from 2003 to , coordinated by Petr Pravec at Ondřejov Observatory and involving facilities like , analyzed composite lightcurves of the system to detect mutual events such as eclipses and occultations. These events, occurring when Dimorphos passed in front of or behind Didymos, allowed determination of the moonlet's sidereal of 11.92 hours and low of 0.03 ± 0.01, with Dimorphos in synchronous . Extensive coverage during the 2019–2020 apparitions, using telescopes from 0.6 m to 10 m apertures, refined these parameters to uncertainties below 1 second for the period, essential for targeting, and enabled a shape model of Dimorphos as an oblate spheroid approximately 170 m in . The mutual parameters included Dimorphos's semi-major axis of about 1.2 . Spectroscopic observations classified the Didymos system, with spectra dominated by the primary, as S-type based on visible and near-infrared features indicative of ordinary chondrite-like silicates. Pre-DART near-IR spectra from NASA's Infrared Telescope Facility (IRTF) showed a moderately red slope consistent with S-complex asteroids, while (VLT) observations with X-Shooter in 2021 confirmed the through absorption bands near 1 and 2 μm linked to and . No distinct pre-impact spectrum of Dimorphos alone was obtained due to its flux contribution being less than 5% of the system total. Despite these advances, ground-based methods faced inherent limitations, including radar resolutions of approximately 30 m per pixel that precluded detailed surface mapping or boulder-scale features on Dimorphos. Photometric and spectroscopic data also suffered from blending with Didymos, restricting insights into the moonlet's individual composition and geology until spacecraft flybys.

DART mission

The Double Asteroid Redirection Test (DART) was a NASA planetary defense demonstration mission designed to test kinetic impact as a method for altering the trajectory of a potentially hazardous asteroid. Launched on November 24, 2021, aboard a SpaceX Falcon 9 rocket from Vandenberg Space Force Base in California, the mission targeted the binary asteroid system (65803) Didymos and its moonlet Dimorphos. The spacecraft traveled for nearly 10 months before arriving at the target system on September 26, 2022, when it intentionally collided with Dimorphos at a relative speed of approximately 6.6 km/s, about 11 million kilometers from Earth. This impact marked the first deliberate alteration of an asteroid's orbit by human means, validating the kinetic impactor technique for future deflection efforts against near-Earth objects. The spacecraft, developed and operated by the () under NASA's , was a box-shaped impactor with a mass of approximately 610 kg at launch, including about 110 kg of propellant for trajectory corrections. Key to its success was the Didymos Reconnaissance and Asteroid Camera for Optical navigation (), a high-resolution imager based on the Long Range Reconnaissance Imager from the mission, which enabled autonomous navigation via the SMART Nav system during the final approach. captured images down to seconds before , providing real-time data on Dimorphos's size, shape, and surface features to refine targeting. Accompanying the main spacecraft was LICIACube, a 6U developed by the (ASI) in collaboration with Argotec, deployed from on September 11, 2022—about 15 days prior to impact—to observe the collision from a safe distance of roughly 50-55 km. Equipped with two optical cameras (LEIA and LUKE) for visible and near-infrared imaging, LICIACube documented the ejecta plume, crater formation, and early dynamical effects on Dimorphos, complementing DRACO's onboard observations. The impact occurred in Dimorphos's southern hemisphere, as confirmed by the sequence of images transmitted in the final minutes, which revealed a rugged surface dominated by a dense field with over 950 identifiable boulders ranging from decimeters to several meters across. These images, streamed live to , showed the spacecraft's approach toward a of irregular rocks and possible ridges, highlighting the moonlet's loosely consolidated rubble-pile suitable for transfer during deflection. The mission's execution achieved its core objective, demonstrating that a like could successfully navigate to and strike a small, fast-moving target with precision.

Impact effects and orbital changes

The impact on September 26, 2022, generated a prominent plume from Dimorphos, consisting of dust and boulders expelled at high velocities. Observations from the SOAR Telescope in captured the plume forming a comet-like tail exceeding 10,000 kilometers in length shortly after impact, with the tail extending up to 70,000 kilometers over subsequent weeks as material continued to disperse. The ejected mass was estimated at 1.3–2.2 × 10^7 kilograms, equivalent to 0.3–0.5% of Dimorphos's total mass assuming a of 2,400 kg/m³, significantly enhancing the overall transfer beyond the spacecraft's direct . This contributed to a momentum amplification factor of 2–4, as the plume's pushed Dimorphos more effectively than the impactor alone. The did not produce a traditional deep but instead caused widespread surface disruption due to Dimorphos's highly porous, rubble-pile . Hydrocode simulations indicate the excavation spanned approximately 40–60 meters in , with excavated to depths of about 15 meters, though the low (a few Pascals to tens of kilopascals) led to shallow features and extensive redistribution rather than a confined bowl-shaped . Global reshaping occurred as recoiling boulders and debris, totaling up to 8% of the asteroid's mass moving below , altered Dimorphos's overall form from a near-spheroidal shape to one with increased elongation, potentially raising its from 1.02 to 1.2. Ground-based observations from 2022 to 2025, including lightcurve photometry from telescopes like SOAR, confirmed the impact's orbital perturbations around Didymos. The mutual shortened by 33.0 ± 1.0 minutes, from 11 hours 55 minutes to about 11 hours 22 minutes, with the post-impact orbit becoming slightly eccentric at e ≈ 0.028 ± 0.016. This change, validated through mutual event timing and , implies a velocity reduction of 2.70 ± 0.10 mm/s for Dimorphos. The momentum enhancement factor β, defined as the ratio of total momentum transferred to the impactor's momentum, was determined to be 3.6 ± 0.6 based on plume modeling and orbital , assuming Dimorphos's of 2,400 kg/m³; broader ranges yield β between 2.2 and 4.9. This value demonstrates the efficacy of kinetic impactors for deflection, as the ejecta plume amplified the effect by a factor exceeding 3, providing critical for future planetary defense strategies.

Future missions

The European Space Agency's (ESA) Hera mission represents the primary planned follow-up to NASA's impact on Dimorphos, aimed at conducting a detailed in-situ of the system. Launched on , 2024, aboard a rocket from , is scheduled to arrive at the Didymos-Dimorphos system in November 2026, an earlier timeline than initially planned due to refined trajectories informed by post-DART data analysis. The mission, part of ESA's Space Safety Programme, will orbit Didymos and perform close-proximity observations of Dimorphos over approximately six months to characterize the kinetic impact site's effects and validate planetary defense techniques. Hera carries two CubeSats for extended monitoring: Milani, which will conduct and to analyze surface composition, and , equipped with the low-frequency instrument for subsurface sounding to probe Dimorphos's internal structure, gravity field, and potential site properties. is designed to detach and attempt a controlled on Dimorphos, providing the first measurements inside an . These CubeSats will enable detailed studies beyond Hera's main orbiter capabilities, including radio experiments to augment and determinations. Key objectives include high-resolution mapping of the impact crater on Dimorphos to assess its size, shape, and distribution; precise measurement of Dimorphos's and through orbital tracking and radio to evaluate momentum transfer efficiency from the ; and analysis of the system's dynamics, including any lingering plume remnants and changes in orbital parameters. These investigations build on 's precursor demonstration of deflection by kinetic impactor. As of November 2025, remains on track following a successful Mars flyby in March 2025, which provided gravitational assist and imaging opportunities of the planet and its moon Deimos. has contributed through the selection of participating scientists in 2024 to support and instrument calibration, enhancing international collaboration on the mission. No additional standalone missions to Dimorphos are currently approved beyond and its CubeSats, though proposals for future extended monitoring via smallsats have been discussed in planetary defense planning.

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