• fraction of incident radiation reflected by a surface or body
  • 0 (absorbs everything) to 1 (reflects everything)
  • Bond albedo: over all wavelengths and directions (the one used in energy balance)
  • geometric albedo: brightness at zero phase angle, relative to a flat, perfectly diffusing disk
  • Bond albedos: Earth ≈ 0.30, Venus ≈ 0.76, Moon ≈ 0.11
  • fresh snow ≈ 0.8, open ocean ≈ 0.06
  • ice-albedo feedback: less ice → darker surface → more sunlight absorbed → more melting (positive feedback)
  • role in a planet’s temperature: Stefan-Boltzmann law, zero-dimensional energy balance model