Steven J. Ostro

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Steven J. Ostro is an American scientist specializing in radar astronomy. He works at NASA's Jet Propulsion Laboratory. Ostro has led radar observations of numerous asteroids, as well as the moons of Jupiter and Saturn, Saturn's rings, and Mars and its satellites. As of May 2008, Ostro and his collaborators have detected 222 near-Earth asteroids (including 130 potentially hazardous objects and 24 binaries) and 118 main belt objects with radar[1].

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[edit] Education and Employment

Ostro received his undergraduate degree in ceramic science from Rutgers University in 1969, a masters in engineering physics from Cornell in 1974, and his PhD in planetary science from MIT in 1978. At MIT, Ostro was advised by Gordon Pettingill and studied the radar scattering properties of the Galilean satellites using the Arecibo Observatory.

After completing his graduate work, Ostro served as an assistant professor at Cornell before moving to JPL in 1984.

Currently, Ostro heads JPL's Asteroid Radar group, and is also a member of the Cassini–Huygens RADAR team, studying the moons of Saturn.

[edit] Asteroid Radar Astronomy

Animation of 1999 KW4, a binary near-Earth asteroid observed by Ostro and his collaborators. This shape model was obtained by inversion of radar images.
Animation of 1999 KW4, a binary near-Earth asteroid observed by Ostro and his collaborators. This shape model was obtained by inversion of radar images.

Much of Ostro's career has focused on the development of asteroid radar astronomy. In early experiments, such as the first radar detection of Ceres, radar observations of asteroids were restricted to measurements of Doppler shifts and radar cross-sections [2]. Beginning in the early 1980's, Ostro led the development of radar imaging and shape-reconstruction techniques, first determining only outer limits of targets' shapes, then deriving three-dimensional shape models[3]. From August 19 to 22 of 1989, Ostro and Scott Hudson observed the contact binary 4769 Castalia from the Arecibo Observatory, producing the first resolved radar images of an asteroid, which they later used to construct a model of the object.

Following the further development of imaging and shape reconstruction techniques by Ostro, Hudson, and Christopher Magri and the upgrade of Arecibo in the mid-1990s, the number of radar observations has increased dramatically[4].

Notable asteroids observed by Ostro include:

  • 216 Kleopatra - a large main-belt asteroid, the first asteroid confirmed to have a surface composition of nickel-iron.
  • 1986 DA - the first near-Earth asteroid confirmed to be metallic. The estimated amount of platinum-group metals in 1986 DA is comparable to that in the Bushveld Igneous Complex, the largest source on Earth's surface.
  • 4179 Toutatis - a contact binary asteroid that is in a non-principal axis rotation state.
  • 1998 JM8 - a large near-Earth asteroid that rotates very slowly.
  • 1998 KY26 - a very small (30 m wide) asteroid that spins so quickly that it has negative effective gravity.
  • 1999 KW4 - one of the first binary near-Earth asteroids known. The shape of the primary (alpha) has been determined by the orbital evolution of the secondary (beta), which is in turn coupled to the system's orbit around the Sun by radiation forces.

In these dynamical studies, Ostro has worked extensively with Daniel J. Scheeres of the University of Colorado and his students.

  • 1950 DA - an approximately 1-km wide asteroid with a possible Earth impact in 2880 (initially studied by Ostro, Jon Giorgini, Lance Benner, and Scott Hudson).
  • 99942 Apophis - a near-Earth asteroid that will pass within geosynchronous orbit in 2029. Radar astrometry from observations by Ostro's group have been essential to predicting Apophis' trajectory.

Radar provides extremely accurate measurement of the positions and velocities of target objects, and such astrometry of near-Earth objects has been recognized as crucial to dealing with the impact hazard. In many cases, radar astrometry has excluded possible Earth impacts from trajectory predictions years before optical astrometry would have been able to do so.

[edit] Work on other objects

Ostro has continued to work on radar observations of the icy satellites of Jupiter and Saturn, particularly with the Cassini-Huygens RADAR instrument, and measured the thickness of the coating of dark organics that forms the dark side of Iapetus.

Radar observations of Mars' moons, Phobos and Deimos, have refined knowledge of their orbits and show that their surfaces are coated with very low density (~1 g/cm3) material, most likely fine-grain dust, to a depth of several meters.

[edit] Asteroid impact hazard

Ostro was an early participant in discussion of the asteroid impact hazard, placing particular emphasis on the need to characterize asteroids before any deflection attempt. In a paper with Carl Sagan, Ostro noted that while the asteroid impact hazard is a long-term risk to any civilization, the risk associated with maintaining an active deflection program is higher, because it is just as easy to deflect an asteroid to impact Earth as to prevent it from doing so [5]. Ostro advocates for continued funding of the Arecibo Planetary Radar, on both hazard and scientific grounds.

[edit] Awards and honors

Ostro received the Gerard P. Kuiper Prize from the Division for Planetary Sciences of the American Astronomical Society in 2003.

The asteroid 3169 Ostro is named in his honor.

[edit] References

  1. ^ http://echo.jpl.nasa.gov/asteroids/asteroid_radar_highlights.txt
  2. ^ Ostro, S.J. et al. 1979. Radar observations of asteroid 1 Ceres. Icarus 40, 355-358
  3. ^ Ostro, S.J. et al. 1988. Asteroid shapes from radar echo spectra: A new theoretical approach. Icarus 73, 15-24
  4. ^ echo.jpl.nasa.gov
  5. ^ S.J. Ostro and Carl Sagan. 1994. Cosmic Collisions and Galactic Civilizations

[edit] External links