The FG5 series absolute gravimeters have an estimated instrumental acc
uracy of 1-2 muGal (1-2 x 10(-8) ms-2). A number of instrument compari
sons were conducted with six FG5 instruments over a period of 9 months
; the predecessor series JILA4 instrument was also used. The standard
deviation of mean g values (averaged over 24-48 h), as observed by dif
ferent instruments, is 1.8 muGal. Observations taken within 48 h typic
ally agree within 2 muGal, and the maximum observed disagreement is 6
muGal for two observations taken 37 days apart. Individual data sets o
f 100-250 measurements (16-42 min duration) show minimum standard devi
ations of 7-8 muGal, placing an upper bound on instrument noise. The d
ata are not corrected for local water-table effects or regional atmosp
heric loading, and thus the observed repeatability is probably an unde
restimate of the instrument accuracy. The observed instrument agreemen
t is consistent with the instrumental accuracy estimate. Ignoring defi
ciencies in modeling environmental gravity signals, this accuracy leve
l should allow resolution of vertical motions at the sub-centimeter le
vel.