Multicolor CCD images at selected wavelengths from 370 to (900 \mathrm{~nm}) obtained at Pic-du-Midi Observatory during four different phases of the development of Saturn's equatorial disturbance are used to analyze its photometric properties. Three epochs and four morphologically different regions were studied: October 5,1990 , the source of the event, the Great White Spot properly; October 6 and 8,1990 , an undisturbed area in the same latitude far away from the GWS; November 17, 1990, the mature phase of the planetary disturbance; and July 7, 1991, the declined phase, but still active, disturbance. The absolute spectral reflectivity of the GWS single feature showed a marked increase at all wavelengths with respect to the undisturbed neighbourings. A simple interpretation of these data indicates that optically thick cloud tops in the GWS nucleus were located at average pressures (\sim 200 \mathrm{mbar}, \sim) two scale heights above the expected ammonia cloud deck at (\sim 1.8) bar. The particles forming the GWS were very bright in the red and less contaminated by the blue absorbing impurities. Limb to limb scans at latitudes (5^{\circ}), (13^{\circ}), and (20^{\circ} \mathrm{N}) are used to characterize the temporal spectral dependence of the Minnaert's limb darkening coefficient (K) and the normalized albedo ((I / F){0}). Pronounced increases in (K) and ((I / F){0}) were noted at continuum wavelengths in November 1990, but only moderate changes were apparent in July 1991 (both with respect to the undisturbed area observed in early October 1990). The particles constituting the upper cloud of the disturbance during its mature phase in November 1990 showed changes in their vertical distribution, and had a higher single-scattering albedo at blue and yellow wavelengths, and were more forward scattering than those which normally form the equatorial haze and cloud of Saturn. O 1994 Academic Press, Inc.