Your correct Kevin, specifc gravity does change with temperature.
Specific gravity (sg) is a ratio of two densities, one being the density of pure water at 3.98 degrees C, (some say 4).
The definition of density is mass/volume
Because the volume changes due to thermal expansion and contraction that in of itself is caused by changes in temperature, specific gravity is temperature dependent.
(Did you know the last piece of the Golden Gate Bridge could only be fitting in place once the morning sun had warmed the metal, expanding it ever so?)
The key is knowing what standard your refractometer is calibrated at. The real challenge lies in the resolution of the refractometer.....i don't know about you guys, but I have problems telling 1.025 from 1.026 sometimes and guess on 1.0255. I won't even begin to think myself, or the instrument is that precise for anything further, and isn't.
So the real question is: how close is "close" enough for you?
From the below article link:
"The density of pure water at 20 °C is 0.998206 g/cm3, and at 60 °F it is 0.9990247 g/cm3. While these seem close to 1, and are often simply claimed to be 1.00 in many contexts, the difference can be substantial. For example, the specific gravity of natural seawater (S =35) is 1.0278 using the 3.98 °C standard, 1.0269 using the 60 °F standard, 1.0266 using the 20 °C standard, and 1.0264 using the 77 °F standard."-Randy Holmes-Farley
http://www.advancedaquarist.com/issues/jan2002/chemistry.htm
Here is your chart:
http://www.reefkeeping.com/issues/2004-07/rhf/index.php
And one on refractometers:
http://reefkeeping.com/issues/2006-12/rhf/index.php
With that said, I think the difference is far more precise than the average user with the average equipment can accuratly achieve to see the difference from 70-80 degrees.