The thermal emission from boulders on (25143) Itokawa and general implications for the YORP effect
arXiv:1504.00566 · doi:10.1093/mnras/stv738
Abstract
Infrared radiation emitted from an asteroid surface causes a torque that can significantly affect rotational state of the asteroid. The influence of small topographic features on this phenomenon, called the YORP effect, seems to be of utmost importance. In this work, we show that a lateral heat diffusion in boulders of suitable sizes leads to an emergence of a local YORP effect which magnitude is comparable to the YORP effect due to the global shape. We solve a three-dimensional heat diffusion equation in a boulder and its surroundings by the finite element method, using the FreeFem++ code. The contribution to the total torque is inferred from the computed temperature distribution. Our general approach allows us to compute the torque induced by a realistic irregular boulder. For an idealized boulder, our result is consistent with an existing one-dimensional model. We also estimated (and extrapolated) a size distribution of boulders on (25143) Itokawa from close-up images of its surface. We realized that topographic features on Itokawa can potentially induce a torque corresponding to a rotational acceleration of the order 10^-7 rad day^-2 and can therefore explain the observed phase shift in light curves.
arXiv commentAccepted for publication in MNRAS
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- Rotation acceleration of asteroids (10115) 1992 SK, (1685) Toro, and (1620) Geographos due to the YORP effect
- The Global Surface Roughness of 25143 Itokawa
- Analytic model for tangential YORP
- The crater-induced YORP effect
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- A semi-analytical thermal model for craters with application to the crater-induced YORP effect
- Annihilation of Relative Equilibria in the Gravitational Field of Irregular-shaped Minor Celestial Bodies
- Analytic theory for the tangential YORP produced by the asteroid regolith
- Obliquity dependence of the tangential YORP
- A new equilibrium state for singly synchronous binary asteroids
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- Positive YORP effect induced by lateral heat conduction in a crater