Bibcode
DellaGiustina, D. N. ; C. A. Bennett; K. Becker; D. R. Golish; L. Le Corre; D. A. Cook; K. L. Edmundson; M. Chojnacki; S. S. Sutton; M. P. Milazzo; B. Carcich; M. C. Nolan; N. Habib; K. N. Burke; T. Becker; P. H. Smith; K. J. Walsh; K. Getzandanner; D. R. Wibben; J. M. Leonard; M. M. Westermann; A. T. Polit; J. N. Kidd Jr; C. W. Hergenrother; W. V. Boynton; J. Backer; S. Sides; J. Mapel; K. Berry; H. Roper; C. Drouet d'Aubigny; B. Rizk; M. K. Crombie; E. K. Kinney‐Spano; de León J.; J. L. Rizos; Licandro J.; H. C. Campins; B. E. Clark; H. L. Enos; D. S. Lauretta
Referencia bibliográfica
Earth and Space Science
Fecha de publicación:
12
2018
Número de citas
23
Número de citas referidas
22
Descripción
The OSIRIS‐REx Asteroid Sample Return Mission is the third mission in National Aeronautics and Space Administration (NASA)'s New Frontiers Program and is the first U.S. mission to return samples from an asteroid to Earth. The most important decision ahead of the OSIRIS‐REx team is the selection of a prime sample‐site on the surface of asteroid (101955) Bennu. Mission success hinges on identifying a site that is safe and has regolith that can readily be ingested by the spacecraft's sampling mechanism. To inform this mission‐critical decision, the surface of Bennu is mapped using the OSIRIS‐REx Camera Suite and the images are used to develop several foundational data products. Acquiring the necessary inputs to these data products requires observational strategies that are defined specifically to overcome the challenges associated with mapping a small irregular body. We present these strategies in the context of assessing candidate sample sites at Bennu according to a framework of decisions regarding the relative safety, sampleability, and scientific value across the asteroid's surface. To create data products that aid these assessments, we describe the best practices developed by the OSIRIS‐REx team for image‐based mapping of irregular small bodies. We emphasize the importance of using 3‐D shape models and the ability to work in body‐fixed rectangular coordinates when dealing with planetary surfaces that cannot be uniquely addressed by body‐fixed latitude and longitude.