Asteroid 1950 DA's Encounter with Earth in 2880: Physical Limits of Collision Probability Prediction

Author:

Giorgini J. D.1,Ostro S. J.1,Benner L. A. M.1,Chodas P. W.1,Chesley S. R.1,Hudson R. S.2,Nolan M. C.3,Klemola A. R.4,Standish E. M.1,Jurgens R. F.1,Rose R.1,Chamberlin A. B.1,Yeomans D. K.1,Margot J.-L.5

Affiliation:

1. Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA 91109–8099, USA.

2. School of Electrical Engineering and Computer Science, Washington State University, Pullman, WA 99164–2752, USA.

3. Arecibo Observatory, Arecibo, Puerto Rico 00612, USA.

4. Lick Observatory, University of California, Santa Cruz, CA 95064, USA.

5. California Institute of Technology, Pasadena, CA 91125, USA.

Abstract

Integration of the orbit of asteroid (29075) 1950 DA, which is based on radar and optical measurements spanning 51 years, reveals a 20-minute interval in March 2880 when there could be a nonnegligible probability of the 1-kilometer object colliding with Earth. Trajectory knowledge remains accurate until then because of extensive astrometric data, an inclined orbit geometry that reduces in-plane perturbations, and an orbit uncertainty space modulated by gravitational resonance. The approach distance uncertainty in 2880 is determined primarily by uncertainty in the accelerations arising from thermal re-radiation of solar energy absorbed by the asteroid. Those accelerations depend on the spin axis, composition, and surface properties of the asteroid, so that refining the collision probability may require direct inspection by a spacecraft.

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

Reference41 articles.

1. C. A. Wirtanen Minor Planet Circ. 416 (1950).

2. LONEOS Sky Survey Minor Planet Electron. Circ. 2001-A22 (2001).

3. C. M. Bardwell Minor Planet Electron. Circ. 2001-A26 (2001).

4. S. J. Ostro in Encyclopedia of Physical Science and Technology ed. 3 vol. 12 (Academic Press San Diego CA 2002) pp. 295–327.

5. Delay-Doppler corrections to the orbit at the start of the radar experiment were atypically small because of the long time interval spanned by preexisting optical astrometry which consisted of 119 plane-of-sky angular measurements reported by 15 different observing sites spanning 51 years. This optical astrometry and subsequent measurements are available from the Minor Planet Center Cambridge MA.

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