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intermediate

The Yarkovsky and YORP Effects

D. Vokrouhlický et al. (2015)

Published
Jan 1, 2015
Journal
Asteroids IV
DOI
10.2458/azu_uapress_9780816532131-ch027

At a Glance

Comprehensive review of how thermal radiation forces/torques (Yarkovsky, YORP, BYORP) drive asteroid orbits, spins, and binaries.

Summary

This chapter synthesizes the modern theory, measurement techniques, and scientific uses of the Yarkovsky (orbital drift) and YORP/BYORP (spin and binary-orbit evolution) effects, which are now central to small-body dynamics. It highlights why Yarkovsky is comparatively robust to model (often spherical/1D thermal models suffice) while YORP is intrinsically sensitive to fine-scale topography, self-heating, and 3D heat transport—making prediction harder and motivating “stochastic/self-limited YORP” ideas. Using full-text case studies and detection catalogs (e.g., Bennu’s extremely precise Yarkovsky drift; a short list of firm YORP detections; BYORP non-detections consistent with tide–BYORP equilibrium), it shows how these subtle forces constrain asteroid density/thermal inertia, shape and internal structure, and even impact probabilities. The review also connects these effects to population-level outcomes such as NEA retrograde-spin excess, asteroid-family age dating via Yarkovsky spreading, spin-axis clustering (Slivan states), and binary formation/evolution pathways driven by YORP/BYORP plus tides.

Method Snapshot

Analytical scaling theory plus thermophysical/radiative recoil modeling, tied to orbit/rotation-state estimation from radar and long-arc optical photometry.

Background

Celestial mechanics and basic heat transfer/thermophysics for small Solar System bodies.