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Pluto and its satellite, Charon (discovered in 1978; ref. 1), appear to form a double planet, rather than a hierarchical planet/satellite couple. Charon is about half Pluto's size and about one-eighth its mass. The precise radii of Pluto and Charon have remained uncertain, leading to large uncertainties on their densities. Although stellar occultations by Charon are in principle a powerful way of measuring its size, they are rare, as the satellite subtends less than 0.3 microradians (0.06 arcsec) on the sky. One occultation (in 1980) yielded a lower limit of 600 km for the satellite's radius, which was later refined to 601.5 km (ref. 4). Here we report observations from a multi-station stellar occultation by Charon, which we use to derive a radius, R(C) = 603.6 +/- 1.4 km (1sigma), and a density of rho = 1.71 +/- 0.08 g cm(-3). This occultation also provides upper limits of 110 and 15 (3sigma) nanobar for an atmosphere around Charon, assuming respectively a pure nitrogen or pure methane atmosphere.
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http://dx.doi.org/10.1038/nature04351 | DOI Listing |
Philos Trans A Math Phys Eng Sci
February 2025
Florida Space Institute, University of Central Florida, Orlando, FL, USA.
On 27 August 2023 (UTC), a new organization for occultation observations in East Asia was formed, the International Occultation Timing Association/East Asia (IOTA/EA). The goal of this organization is to promote and disseminate occultation observations in the East Asia region and to make occultation observations a useful tool and a partner for planetary exploration missions and other scientific research. The formation of IOTA/EA was triggered by the stellar eclipse observation campaign of (3200) Phaethon, which is the target of the JAXA DESTINY[Formula: see text] mission.
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February 2025
The Hakubi Center/Astronomical Observatory, Graduate School of Science, Kyoto University, Kitashirakawa-oiwake-cho, Sakyo-ku, Kyoto 606-8502, Japan.
The exploration of kilometre-sized trans-Neptunian objects (TNOs) is one of the ultimate goals in the search for the origin and evolution of the Solar System. However, such exploration is challenging because these small bodies are too faint to be directly detected. One potential avenue for detecting and investigating small and faint TNOs is the monitoring of stellar occultation events.
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February 2025
LIRA, CNRS, Observatoire de Paris, Université PSL, Sorbonne Université, Université Paris Cité, CY Cergy Paris Université, Meudon 92190, France.
Until about a decade ago, ring systems were only known to exist around giant planets. Each one of the four giant planets harbours its own distinctive and unique system of rings and inner satellites. The past decade has been marked by the unexpected discoveries of dense rings around small objects of the outer Solar System: the Centaur object Chariklo (and possibly Chiron), the dwarf planet Haumea and the trans-Neptunian object Quaoar.
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February 2025
Southwest Research Institute, 1301 Walnut St., Suite 400, Boulder, CO 80302, USA.
The process by which a system of non-luminous bodies form around a star is fundamental to understanding the origins of our own solar system and how it fits into the context of other systems we have begun to study around other stars. Some basics of solar system formation have emerged to describe the process by which dust and gas around a newly formed star evolve into what we see today. The combination of occultation observations and the flyby observations by New Horizons of the Cold-Classical Kuiper Belt Object (CCKBO), (498958) Arrokoth, has provided essential new constraints on formation models through its three-dimensional shape.
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February 2025
LESIA, Observatoire de Paris, Université PSL, Meudon 92195, France.
The observation of Earth-based stellar occultations by solar system planets and satellites has been used for decades to retrieve information on the physical properties of their atmospheres. From the variations of the stellar flux during ingress and egress and, in some favourable cases, from the central flash, one can infer the vertical density, pressure and temperature profiles around the half-light level (typically in the range of a few μbars), as well as zonal wind regimes and the presence of hazes. Earth-based occultations have been successfully applied to all planets and satellites surrounded by an atmosphere, and have delivered unique and significant information that are often complementary to the results obtained by planetary space missions.
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