The evaporation of small droplets of volatile liquids from solid surfaces d
epends on whether the initial contact angle is larger or less than 90 degre
es. In the latter case, for much of me evaporation time the contact radius
remains constant and the contact angle decreases. At equilibrium, the small
er the drop, the more it is possible to neglect gravity and the more the pr
ofile is expected to conform to a spherical cap shape. Recently published w
ork suggests that a singular flow progressively develops within the drop du
ring evaporation. This flow might create a pressure gradient and so result
in more flattening of the profile as the drop size reduces, in contradictio
n to expectations based on equilibrium ideas. In either case, it is importa
nt to develop methods to quantify confidence in a deduction of elliptical d
eviations from optically recorded droplet profiles. This paper discusses su
ch methods and illustrates the difficulties that can arise when the drop si
ze changes, but the absolute resolution of the system is fixed. In particul
ar, the difference between local variables, such as contact angle, cap heig
ht, and contact diameter, which depend on the precise location of the suppo
rting surface, and global variables such as radii of curvature and eccentri
city, is emphasized. The applicability of the ideas developed is not limite
d to evaporation experiments, but is also relevant to experiments on contac
t angle variation with drop volume.