The intra-day variable source 0917+624 displays annual changes in its
timescale of variability. This is explained in terms of a scintillation model
in which changes in the variability timescale are due to changes in the
relative velocity of the scintillation pattern as the Earth orbits the sun.
(see also astro-ph/0102050)Comment: 4 pages, 1 figure. Accepted for A&A Letter