you have an incoming flux at perihelion of:<br />1366 W/m² / 0.307² = 14500 W/m²<br />If you could really have a 99% albedo body, you would absorb only 1% ie 145 W/m2 and have, assuming an IR emissivity epsilon of 0.98 (smooth clean ice), a radiative flux balance:<br />145 W/m2 = absorbed flux = reemitted flux = epsilon.sigma.T4<br />(assuming no heat flux from the interior)<br />Hence T=226K.<br /><br />For people in doubt, note that the same calculation with 12% Bond albedo and an epsilon of 0.9 gives 707K.<br /><br />The point is to keep an actual 99% albedo! This may be possible on Enceladus only because of ultra-flat surface of ice thanks to resurfacing. Ageing of your surface will quickly increase the absorptivity (decrease the albedo).<br /><br />273K corresponds to an albedo of 0.9825! <br /><br />Also, 226K is "above" sublimation of ice in vacuum. To get a reasonably negligible sublimation rate, you should be below 170K.<br />You would satisfy this condition on your "instantly teleported Enceladus" above 71° latitude at perihelion, and above 43° latitude at aphelion.<br /><br />Best regards.<br /><br />