I'm going to look at the problem in a secondary-school way (which is what it deserves!)
Say you have a single column exactly 1 square meter in area.
The area will not change, because other water columns are immediately next to it.
The 0.00015 per degree C is then just a fractional increase in the depth (per degree C).
The interesting part is part (c), why the actual rise was much less than the expected rise. Some possibilities are (i) the spill-out effect, the lateral area of the ocean increases slightly when sea level rises, (ii) the time scale of deep ocean circulation, which is many hundreds of years, (iii) non-linearities in the seawater equation of state: perhaps the expansion coefficient is smaller where the pressure is great, or where the temperature is low to begin with, (iv) maybe a warmer atmosphere kept more of Earth's water in a vapor state. I leave it to you to evaluate these by doing some reading.