Summary
We present low-resolution turbulence proles of the atmosphere above Dome C, Antarctica, measured with the MASS instrument during 25 nights in March { May 2004. Except for the lowest layer, Dome C has signicantly less turbulence than Cerro Tololo and Cerro Pachon. In particular, the integrated turbulence at 16 km is always less than the median values at the two Chilean sites. From these proles we evaluate the photometric noise produced by scintillation, and the atmospheric contribution to the error budget in narrow-angle dierential astrometry. In comparison with the two mid-latitude sites in Chile, Dome C oers a potential gain of about 3:6 in both photometric precision (for long integrations) and narrow-angle astrometry precision. These gain estimates are preliminary, being computed with average wind-speed proles, but the validity of our approach is conrmed by independent data. Although the data from Dome C cover a fairly limited time frame, they lend strong support to expectations that Dome C will offer signicant advantages for photometric and astrometric studies.