... computation for the Moon as we did for the Earth we have: Io (1 - AMoon ) = T 4 Moon , (19) where the Moon's albedo is lower ... The Moon's effective temperature TMoon = 274 K is higher than the Earth's because of the Moon's lower albedo. ...
82. http://www.mso.anu.edu.au/~kcf/pubs_top20/54.pdf
... 1 E. Berger,5 T. Piran,1 ,6 A. M. Soderb erg,1 S. B. Cenko,1 P. B. Cameron,1 A. Gal-Yam,1 M. M. Kasliwal,1 D.-S. Moon,1 F. A. Harrison,1 arXiv:astro-ph/0510110v1 5 Oct 2005 E. Nakar,1 B. P. Schmidt,7 , B. Penprase,8 R. A. Chevalier,9 P. Kumar,10 K. Roth ...
83. http://www.mso.anu.edu.au/~charley/papers/LineweaverChopra2012.pdf
... include Jupiter's moons Europa, Ganymede, and Callisto and Saturn's moons Titan and ... moons seems to scale with the mass of the host planet, the most massive planets in ...
84. http://www.mso.anu.edu.au/~charley/papers/ChopraLineweaverASSC09v3.pdf
... The Moon-forming life at that time [67]. any inferences about years after the Moon impact 4.5 billion years ago would have sterilised Earth of any extant LUCA probably existed 4.2 ± 0.4 billion years ago [68]. ...
85. http://www.mso.anu.edu.au/pfrancis/comets/comets.pdf
... E.M. & Stewart, A.I.F. 1996, Earth, Moon & Planets, 72, 243 Bronshten, V. 2000, A&A ... 2003, Icarus, 161, 17 Jewitt, D. 2003, Earth, Moon & Planets, 92, 465 Jewitt, D.C ...