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THE YARKOVSKY AND YORP EFFECTS: Implications for Asteroid Dynamics

W. F. BottkeSouthwest Research Institute, Boulder, Colorado 80302;David VokrouhlickýInstitute of Astronomy, Charles University, 18000 Prague 8, Czech RepublicDavid Parry RubincamNASA Goddard Space Flight Center, Greenbelt, Maryland 20771David NesvornýSouthwest Research Institute, Boulder, Colorado 80302;
2006en
ABI

Abstract

The Yarkovsky and YORP (Yarkovsky-O'Keefe-Radzievskii-Paddack) effects are thermal radiation forces and torques that cause small objects to undergo semimajor axis drift and spin vector modifications, respectively, as a function of their spin, orbit, and material properties. These mechanisms help to (a) deliver asteroids (and meteoroids) with diameter D < 40 km from their source locations in the main belt to chaotic resonance zones capable of transporting this material to Earth-crossing orbits; (b) disperse asteroid families, with drifting bodies jumping or becoming trapped in mean-motion and secular resonances within the main belt; (c) modify the rotation rates and obliquities of D < 40 km asteroids; and (d) allow asteroids to enter into spin-orbit resonances, which affect the evolution of their spin vectors and feedback into the Yarkovsky-driven semimajor axis evolution. Accordingly, we suggest that nongravitational forces should now be considered as important as collisions and gravitational perturbations to our overall understanding of asteroid evolution.

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