On 21 April 2013, during a co-ordinated Saturn auroral observing campaign, the northern and southern poles of the planet were observed from the NASA Infrared Telescope Facility (IRTF), Keck, and Hubble Space Telescope (HST) simultaneously with the Cassini infrared, visible, and ultraviolet remote sensing instruments. We present simultaneous multi-scale and mutli-wavelength analysis of the morphology of auroral emissions at Saturn. There is variability on every spatial and temporal scale analysed, and high spatial resolution observations distinguish variable features with sizes tens of km on the planet.The fine scale temporal and spatial features seen in the main oval itself show that complex structures present even during quiet solar wind conditions. We observe diffuse ultraviolet emissions southward of the southern midnight main oval that are not seen in the infrared.This implies a steep temperature gradient, ∼60 K over 2-4 • latitude equator wad of the main oval. Lower spatial resolution observations reveal broad-scale dynamics at both poles, variable over minutes to hours, the morphology of which is only partly consistent with a overlapping local-time fixed and co-rotating current systems. We also present the first direct comparison of simultaneous infrared, visible, and ultraviolet auroral emissions at Saturn. These emissions are co-located, even though the spatial scale and operational mode of each instrument are very different.