Cross-correlation of consecutive Doppler images is one of the most common
techniques used to detect surface differential rotation (hereafter DR) on
spotted stars. The disadvantage of a single cross-correlation is, however, that
the expected DR pattern can be overwhelmed by sudden changes in the apparent
spot configuration. Another way to reconstruct the image shear using Doppler
imaging is to include a predefined latitude-dependent rotation law in the
inversion code (`sheared image method'). However, special but not unusual spot
distributions, such like a large polar cap or an equatorial belt (e.g., small
random spots evenly distributed along the equator), can distort the rotation
profile similarly as the DR does, consequently, yielding incorrect measure of
the DR from the sheared image method. To avoid these problems, the technique of
measuring DR from averaged cross-correlations using time-series Doppler images
(`ACCORD') is introduced and the reliability of this tool is demonstrated on
artificial data.Comment: 2 pages, 2 figures, to be appeared in 'Magnetic Fields Throughout the
Stellar Evolution', Proc. IAU Symp. 302, (26-30 Aug 2013, Biarritz, France